Sample records for observed pressure profiles

  1. Pressure profiles of plasmas confined in the field of a dipole magnet

    NASA Astrophysics Data System (ADS)

    Davis, Matthew Stiles

    total electron population. When the dipole was magnetically levitated the plasma density increased substantially because particle losses to the mechanical supports were eliminated so particles could only be lost via slower cross-field transport processes. The pressure profile was observed to be broader during levitated operation than it was during supported operation, and the pressure appeared to be contained in both a thermal population and an energetic electron population. X-ray spectra indicated that the X-rays came from a similar hot electron population during levitated and supported operation; however, the hot electron fraction was an order of magnitude smaller during levitated operation (<3% of the total electron population). Pressure gradients for both supported and levitated plasmas were compared to the MHD limit. Levitated plasmas had pressure profiles that were (i) steeper than, (ii) shallower than, or (iii) near the MHD limit dependent on plasma conditions. However, those profiles that exceeded the MHD limit were observed to have larger fractions of energetic electrons. When the dipole magnet was supported, high pressure plasmas always had profiles that exceeded the MHD interchange stability limit, but the high pressure in these plasmas appeared to arise entirely from a population of energetic trapped electrons.

  2. Pressure profiles of sport compression stockings.

    PubMed

    Reich-Schupke, Stefanie; Surhoff, Stefan; Stücker, Markus

    2016-05-01

    While sport compression stockings (SCS) have become increasingly popular, there is no regulatory norm as exists for medical compression stockings (MCS). The objective of this pilot study was to compare five SCS with respect to their pressure profiles ex vivo and in vivo, and in relation to German standards for MCS (RAL norm). In vivo (10 competitive athletes; standardized procedure using the Kikuhime pressure monitor) and ex vivo (tested at the Hohenstein Institute) pressure profiles were tested for the following products: CEP Running Progressive Socks, Falke Running Energizing, Sigvaris Performance, X-Socks Speed Metal Energizer, and 2XU Compression Race Socks. Ex vivo ankle pressures of CEP (25.6 mmHg) and 2XU (23.2 mmHg) corresponded to class 2 MCS; that of Sigvaris (20.8 mmHg), to class 1 MCS. The remaining SCS achieved lower pressure values. The pressure gradients showed marked differences, and did not meet MCS standards. Average in vivo pressures were higher for 2XU, CEP, and Sigvaris than for Falke and X-Socks. However, in vivo values for all SCS were below those of class 1 MCS. None of the SCS showed the decreasing pressure gradient (from distal to proximal) required for MCS. In vivo and ex vivo pressure profiles of all SCS examined showed marked heterogeneity, and did not meet MCS standards. Consequently, the clinical and practical effects of SCS cannot be compared, either. It would therefore be desirable to establish a classification that allows for the categorization and comparison of various SCS as well as their selection based on individual preferences and needs (high vs. low pressure, progressive vs. degressive profile). © 2016 Deutsche Dermatologische Gesellschaft (DDG). Published by John Wiley & Sons Ltd.

  3. Rotor with Flattened Exit Pressure Profile

    NASA Technical Reports Server (NTRS)

    Baltas, Constantine (Inventor); Prasad, Dilip (Inventor); Gallagher, Edward J. (Inventor)

    2015-01-01

    A rotor blade comprises an airfoil extending radially from a root section to a tip section and axially from a leading edge to a trailing edge, the leading and trailing edges defining a curvature therebetween. The curvature determines a relative exit angle at a relative span height between the root section and the tip section, based on an incident flow velocity at the leading edge of the airfoil and a rotational velocity at the relative span height. In operation of the rotor blade, the relative exit angle determines a substantially flat exit pressure ratio profile for relative span heights from 75% to 95%, wherein the exit pressure ratio profile is constant within a tolerance of 10% of a maximum value of the exit pressure ratio profile.

  4. Observation of pressure variation in the cavitation region of submerged journal bearings

    NASA Technical Reports Server (NTRS)

    Etsion, I.; Ludwig, L. P.

    1980-01-01

    Visual observations and pressure measurements in the cavitation zone of a submerged journal bearing are described. Tests were performed at various shaft speeds and ambient pressure levels. Some photographs of the cavitation region are presented showing strong reverse flow at the downstream end of the region. Pressure profiles are presented showing significant pressure variations inside the cavitation zone, contrary to common assumptions of constant cavitation pressure.

  5. Association between abnormal nocturnal blood pressure profile and dementia in Parkinson's disease.

    PubMed

    Tanaka, Ryota; Shimo, Yasushi; Yamashiro, Kazuo; Ogawa, Takashi; Nishioka, Kenya; Oyama, Genko; Umemura, Atsushi; Hattori, Nobutaka

    2018-01-01

    Circadian blood pressure alterations are frequently observed in Parkinson's disease, but the association between these changes and dementia in the condition remains unclear. Here, we assess the relationship between abnormal nocturnal blood pressure profiles and dementia in Parkinson's disease. We enrolled 137 patients with Parkinson's disease, who underwent 24 h ambulatory blood pressure monitoring, following cognitive and clinical assessment. Twenty-seven patients (19.7%) were diagnosed with dementia in this cohort. We observed significant associations of dementia with age, male gender, Hoehn-Yahr (H-Y) stage, diabetes mellitus, history of stroke, presence of cerebrovascular lesions on MRI, and orthostatic hypotension. Univariate logistic regression analysis showed that among the patterns of nocturnal blood pressure profiles, the riser pattern was significantly associated with dementia (OR 11.6, 95%CI: 2.14-215.0, P < 0.01), and this trend was observed after adjusting for all confounding factors except orthostatic hypotension (OR 19.2, 95%CI: 1.12-1960.3, P = 0.04). However, coexistence of a riser pattern and orthostatic hypotension was related to a higher prevalence of dementia (45.2%) than was a riser pattern alone (9.5%). Furthermore, coexistence of a riser pattern and orthostatic hypotension was significantly more associated with dementia than was a riser pattern alone, even after adjusting for confounders (OR 1625.1, 95%CI: 21.9-1343909.5, P < 0.01). Our results suggest a relationship between a riser pattern coexisting with orthostatic hypotension and dementia in Parkinson's disease. Further prospective studies are warranted to investigate whether abnormal nocturnal blood pressure profiles predict dementia in Parkinson's disease. Copyright © 2017 Elsevier Ltd. All rights reserved.

  6. Application of a Self-Similar Pressure Profile to Sunyaev-Zeldovich Effect Data from Galaxy Clusters

    NASA Technical Reports Server (NTRS)

    Mroczkowski, Tony; Bonamente, Max; Carlstrom, John E.; Culverhouse, Thomas L.; Greer, Christopher; Hawkins, David; Hennessy, Ryan; Joy, Marshall; Lamb, James W.; Leitch, Erik M.; hide

    2009-01-01

    We investigate the utility of a new, self-similar pressure profile for fitting Sunyaev-Zel'dovich (SZ) effect observations of galaxy clusters. Current SZ imaging instruments-such as the Sunyaev-Zel'dovich Array (SZA)- are capable of probing clusters over a large range in a physical scale. A model is therefore required that can accurately describe a cluster's pressure profile over a broad range of radii from the core of the cluster out to a significant fraction of the virial radius. In the analysis presented here, we fit a radial pressure profile derived from simulations and detailed X-ray analysis of relaxed clusters to SZA observations of three clusters with exceptionally high-quality X-ray data: A1835, A1914, and CL J1226.9+3332. From the joint analysis of the SZ and X-ray data, we derive physical properties such as gas mass, total mass, gas fraction and the intrinsic, integrated Compton y-parameter. We find that parameters derived from the joint fit to the SZ and X-ray data agree well with a detailed, independent X-ray-only analysis of the same clusters. In particular, we find that, when combined with X-ray imaging data, this new pressure profile yields an independent electron radial temperature profile that is in good agreement with spectroscopic X-ray measurements.

  7. Theory and discretization of ideal magnetohydrodynamic equilibria with fractal pressure profiles

    NASA Astrophysics Data System (ADS)

    Kraus, B. F.; Hudson, S. R.

    2017-09-01

    In three-dimensional ideal magnetohydrodynamics, closed flux surfaces cannot maintain both rational rotational-transform and pressure gradients, as these features together produce unphysical, infinite currents. A proposed set of equilibria nullifies these currents by flattening the pressure on sufficiently wide intervals around each rational surface. Such rational surfaces exist at every scale, which characterizes the pressure profile as self-similar and thus fractal. The pressure profile is approximated numerically by considering a finite number of rational regions and analyzed mathematically by classifying the irrational numbers that support gradients into subsets. Applying these results to a given rotational-transform profile in cylindrical geometry, we find magnetic field and current density profiles compatible with the fractal pressure.

  8. Radial pressure profiles in a cold‐flow gas‐solid vortex reactor

    PubMed Central

    Pantzali, Maria N.; Kovacevic, Jelena Z.; Marin, Guy B.; Shtern, Vladimir N.

    2015-01-01

    A unique normalized radial pressure profile characterizes the bed of a gas‐solid vortex reactor over a range of particle densities and sizes, solid capacities, and gas flow rates: 950–1240 kg/m3, 1–2 mm, 2 kg to maximum solids capacity, and 0.4–0.8 Nm3/s (corresponding to gas injection velocities of 55–110 m/s), respectively. The combined momentum conservation equations of both gas and solid phases predict this pressure profile when accounting for the corresponding measured particle velocities. The pressure profiles for a given type of particles and a given solids loading but for different gas injection velocities merge into a single curve when normalizing the pressures with the pressure value downstream of the bed. The normalized—with respect to the overall pressure drop—pressure profiles for different gas injection velocities in particle‐free flow merge in a unique profile. © 2015 The Authors AIChE Journal published by Wiley Periodicals, Inc. on behalf of American Institute of Chemical Engineers AIChE J, 61: 4114–4125, 2015 PMID:27667827

  9. Theory and discretization of ideal magnetohydrodynamic equilibria with fractal pressure profiles

    DOE PAGES

    Kraus, B. F.; Hudson, S. R.

    2017-09-29

    In three-dimensional ideal magnetohydrodynamics, closed flux surfaces cannot maintain both rational rotational-transform and pressure gradients, as these features together produce unphysical, infinite currents. A proposed set of equilibria nullifies these currents by flattening the pressure on sufficiently wide intervals around each rational surface. Such rational surfaces exist at every scale, which characterizes the pressure profile as self-similar and thus fractal. The pressure profile is approximated numerically by considering a finite number of rational regions and analyzed mathematically by classifying the irrational numbers that support gradients into subsets. As a result, applying these results to a given rotational-transform profile in cylindricalmore » geometry, we find magnetic field and current density profiles compatible with the fractal pressure.« less

  10. Theory and discretization of ideal magnetohydrodynamic equilibria with fractal pressure profiles

    DOE Office of Scientific and Technical Information (OSTI.GOV)

    Kraus, B. F.; Hudson, S. R.

    In three-dimensional ideal magnetohydrodynamics, closed flux surfaces cannot maintain both rational rotational-transform and pressure gradients, as these features together produce unphysical, infinite currents. A proposed set of equilibria nullifies these currents by flattening the pressure on sufficiently wide intervals around each rational surface. Such rational surfaces exist at every scale, which characterizes the pressure profile as self-similar and thus fractal. The pressure profile is approximated numerically by considering a finite number of rational regions and analyzed mathematically by classifying the irrational numbers that support gradients into subsets. As a result, applying these results to a given rotational-transform profile in cylindricalmore » geometry, we find magnetic field and current density profiles compatible with the fractal pressure.« less

  11. Ambulatory blood pressure profiles in familial dysautonomia.

    PubMed

    Goldberg, Lior; Bar-Aluma, Bat-El; Krauthammer, Alex; Efrati, Ori; Sharabi, Yehonatan

    2018-02-12

    Familial dysautonomia (FD) is a rare genetic disease that involves extreme blood pressure fluctuations secondary to afferent baroreflex failure. The diurnal blood pressure profile, including the average, variability, and day-night difference, may have implications for long-term end organ damage. The purpose of this study was to describe the circadian pattern of blood pressure in the FD population and relationships with renal and pulmonary function, use of medications, and overall disability. We analyzed 24-h ambulatory blood pressure monitoring recordings in 22 patients with FD. Information about medications, disease severity, renal function (estimated glomerular filtration, eGFR), pulmonary function (forced expiratory volume in 1 s, FEV1) and an index of blood pressure variability (standard deviation of systolic pressure) were analyzed. The mean (± SEM) 24-h blood pressure was 115 ± 5.6/72 ± 2.0 mmHg. The diurnal blood pressure variability was high (daytime systolic pressure standard deviation 22.4 ± 1.5 mmHg, nighttime 17.2 ± 1.6), with a high frequency of a non-dipping pattern (16 patients, 73%). eGFR, use of medications, FEV1, and disability scores were unrelated to the degree of blood pressure variability or to dipping status. This FD cohort had normal average 24-h blood pressure, fluctuating blood pressure, and a high frequency of non-dippers. Although there was evidence of renal dysfunction based on eGFR and proteinuria, the ABPM profile was unrelated to the measures of end organ dysfunction or to reported disability.

  12. An Electronic Pressure Profile Display system for aeronautic test facilities

    NASA Technical Reports Server (NTRS)

    Woike, Mark R.

    1990-01-01

    The NASA Lewis Research Center has installed an Electronic Pressure Profile Display system. This system provides for the real-time display of pressure readings on high resolution graphics monitors. The Electronic Pressure Profile Display system will replace manometer banks currently used in aeronautic test facilities. The Electronic Pressure Profile Display system consists of an industrial type Digital Pressure Transmitter (DPI) unit which interfaces with a host computer. The host computer collects the pressure data from the DPI unit, converts it into engineering units, and displays the readings on a high resolution graphics monitor in bar graph format. Software was developed to accomplish the above tasks and also draw facility diagrams as background information on the displays. Data transfer between host computer and DPT unit is done with serial communications. Up to 64 channels are displayed with one second update time. This paper describes the system configuration, its features, and its advantages over existing systems.

  13. An electronic pressure profile display system for aeronautic test facilities

    NASA Technical Reports Server (NTRS)

    Woike, Mark R.

    1990-01-01

    The NASA Lewis Research Center has installed an Electronic Pressure Profile Display system. This system provides for the real-time display of pressure readings on high resolution graphics monitors. The Electronic Pressure Profile Display system will replace manometer banks currently used in aeronautic test facilities. The Electronic Pressure Profile Display system consists of an industrial type Digital Pressure Transmitter (DPT) unit which interfaces with a host computer. The host computer collects the pressure data from the DPT unit, converts it into engineering units, and displays the readings on a high resolution graphics monitor in bar graph format. Software was developed to accomplish the above tasks and also draw facility diagrams as background information on the displays. Data transfer between host computer and DPT unit is done with serial communications. Up to 64 channels are displayed with one second update time. This paper describes the system configuration, its features, and its advantages over existing systems.

  14. Radial profiles of velocity and pressure for condensation-induced hurricanes

    NASA Astrophysics Data System (ADS)

    Makarieva, A. M.; Gorshkov, V. G.

    2011-02-01

    The Bernoulli integral in the form of an algebraic equation is obtained for the hurricane air flow as the sum of the kinetic energy of wind and the condensational potential energy. With an account for the eye rotation energy and the decrease of angular momentum towards the hurricane center it is shown that the theoretical profiles of pressure and velocity agree well with observations for intense hurricanes. The previous order of magnitude estimates obtained in pole approximation are confirmed.

  15. Effect of continuous positive airway pressure on blood pressure and metabolic profile in women with sleep apnoea.

    PubMed

    Campos-Rodriguez, Francisco; Gonzalez-Martinez, Monica; Sanchez-Armengol, Angeles; Jurado-Gamez, Bernabe; Cordero-Guevara, Jose; Reyes-Nuñez, Nuria; Troncoso, Maria F; Abad-Fernandez, Araceli; Teran-Santos, Joaquin; Caballero-Rodriguez, Julian; Martin-Romero, Mercedes; Encabo-Motiño, Ana; Sacristan-Bou, Lirios; Navarro-Esteva, Javier; Somoza-Gonzalez, Maria; Masa, Juan F; Sanchez-Quiroga, Maria A; Jara-Chinarro, Beatriz; Orosa-Bertol, Belen; Martinez-Garcia, Miguel A

    2017-08-01

    Continuous positive airway pressure (CPAP) reduces blood pressure levels in hypertensive patients with obstructive sleep apnoea (OSA). However, the role of CPAP in blood pressure and the metabolic profile in women has not yet been assessed. In this study we investigated the effect of CPAP on blood pressure levels and the glucose and lipid profile in women with moderate-to-severe OSA.A multicentre, open-label, randomised controlled trial was conducted in 307 women diagnosed with moderate-to-severe OSA (apnoea-hypopnoea index ≥15 events·h -1 ) in 19 Spanish Sleep Units. Women were randomised to CPAP (n=151) or conservative treatment (n=156) for 12 weeks. Changes in office blood pressure measures as well as in the glucose and lipid profile were assessed in both groups.Compared with the control group, the CPAP group achieved a significantly greater decrease in diastolic blood pressure (-2.04 mmHg, 95% CI -4.02- -0.05; p=0.045), and a nonsignificantly greater decrease in systolic blood pressure (-1.54 mmHg, 95% CI -4.58-1.51; p=0.32) and mean blood pressure (-1.90 mmHg, 95% CI -4.0-0.31; p=0.084). CPAP therapy did not change any of the metabolic variables assessed.In women with moderate-to-severe OSA, 12 weeks of CPAP therapy improved blood pressure, especially diastolic blood pressure, but did not change the metabolic profile, compared with conservative treatment. Copyright ©ERS 2017.

  16. Effect of continuous positive airway pressure on blood pressure and metabolic profile in women with sleep apnoea

    PubMed Central

    Gonzalez-Martinez, Monica; Sanchez-Armengol, Angeles; Jurado-Gamez, Bernabe; Cordero-Guevara, Jose; Reyes-Nuñez, Nuria; Troncoso, Maria F.; Abad-Fernandez, Araceli; Teran-Santos, Joaquin; Caballero-Rodriguez, Julian; Martin-Romero, Mercedes; Encabo-Motiño, Ana; Sacristan-Bou, Lirios; Navarro-Esteva, Javier; Somoza-Gonzalez, Maria; Masa, Juan F.; Sanchez-Quiroga, Maria A.; Jara-Chinarro, Beatriz; Orosa-Bertol, Belen; Martinez-Garcia, Miguel A.

    2017-01-01

    Continuous positive airway pressure (CPAP) reduces blood pressure levels in hypertensive patients with obstructive sleep apnoea (OSA). However, the role of CPAP in blood pressure and the metabolic profile in women has not yet been assessed. In this study we investigated the effect of CPAP on blood pressure levels and the glucose and lipid profile in women with moderate-to-severe OSA. A multicentre, open-label, randomised controlled trial was conducted in 307 women diagnosed with moderate-to-severe OSA (apnoea–hypopnoea index ≥15 events·h–1) in 19 Spanish Sleep Units. Women were randomised to CPAP (n=151) or conservative treatment (n=156) for 12 weeks. Changes in office blood pressure measures as well as in the glucose and lipid profile were assessed in both groups. Compared with the control group, the CPAP group achieved a significantly greater decrease in diastolic blood pressure (−2.04 mmHg, 95% CI −4.02– −0.05; p=0.045), and a nonsignificantly greater decrease in systolic blood pressure (−1.54 mmHg, 95% CI −4.58–1.51; p=0.32) and mean blood pressure (−1.90 mmHg, 95% CI −4.0–0.31; p=0.084). CPAP therapy did not change any of the metabolic variables assessed. In women with moderate-to-severe OSA, 12 weeks of CPAP therapy improved blood pressure, especially diastolic blood pressure, but did not change the metabolic profile, compared with conservative treatment. PMID:28798089

  17. Pressure and velocity profiles in a static mechanical hemilarynx model

    NASA Astrophysics Data System (ADS)

    Alipour, Fariborz; Scherer, Ronald C.

    2002-12-01

    This study examined pressure and velocity profiles in a hemilarynx mechanical model of phonation. The glottal section had parallel walls and was fabricated from hard plastic. Twelve pressure taps were created in the vocal fold surface and connected to a differential pressure transducer through a pressure switch. The glottal gap was measured with feeler gauges and the uniform glottal duct was verified by use of a laser system. Eight pressure transducers were placed in the flat wall opposite the vocal fold. Hot-wire anemometry was used to obtain velocity profiles upstream and downstream of the glottis. The results indicate that the pressure distribution on the vocal fold surface was consistent with pressure change along a parallel duct, whereas the pressures on the opposite flat wall typically were lower (by 8%-40% of the transglottal pressure just past mid-glottis). The upstream velocity profiles were symmetric regardless of the constriction shape and size. The jet flow downstream of the glottis was turbulent even for laminar upstream conditions. The front of the jet was consistently approximately 1.5 mm from the flat wall for glottal gaps of 0.4, 0.8 and 1.2 mm. The turbulence intensity also remained approximately at the same location of about 4 mm from the flat wall for the two larger gaps.

  18. Pressure and velocity profiles in a static mechanical hemilarynx model.

    PubMed

    Alipour, Fariborz; Scherer, Ronald C

    2002-12-01

    This study examined pressure and velocity profiles in a hemilarynx mechanical model of phonation. The glottal section had parallel walls and was fabricated from hard plastic. Twelve pressure taps were created in the vocal fold surface and connected to a differential pressure transducer through a pressure switch. The glottal gap was measured with feeler gauges and the uniform glottal duct was verified by use of a laser system. Eight pressure transducers were placed in the flat wall opposite the vocal fold. Hot-wire anemometry was used to obtain velocity profiles upstream and downstream of the glottis. The results indicate that the pressure distribution on the vocal fold surface was consistent with pressure change along a parallel duct, whereas the pressures on the opposite flat wall typically were lower (by 8%-40% of the transglottal pressure just past mid-glottis). The upstream velocity profiles were symmetric regardless of the constriction shape and size. The jet flow downstream of the glottis was turbulent even for laminar upstream conditions. The front of the jet was consistently approximately 1.5 mm from the flat wall for glottal gaps of 0.4, 0.8 and 1.2 mm. The turbulence intensity also remained approximately at the same location of about 4 mm from the flat wall for the two larger gaps.

  19. Differential absorption lidar measurements of atmospheric temperature and pressure profiles

    NASA Technical Reports Server (NTRS)

    Korb, C. L.

    1981-01-01

    The theory and methodology of using differential absorption lidar techniques for the remote measurement of atmospheric pressure profiles, surface pressure, and temperature profiles from ground, air, and space-based platforms are presented. Pressure measurements are effected by means of high resolution measurement of absorption at the edges of the oxygen A band lines where absorption is pressure dependent due to collisional line broadening. Temperature is assessed using measurements of the absorption at the center of the oxygen A band line originating from a quantum state with high ground state energy. The population of the state is temperature dependent, allowing determination of the temperature through the Boltzmann term. The results of simulations of the techniques using Voigt profile and variational analysis are reported for ground-based, airborne, and Shuttle-based systems. Accuracies in the 0.5-1.0 K and 0.1-0.3% range are projected.

  20. Pressure Support in Galaxy Disks: Impact on Rotation Curves and Dark Matter Density Profiles

    NASA Astrophysics Data System (ADS)

    Dalcanton, Julianne J.; Stilp, Adrienne M.

    2010-09-01

    Rotation curves constrain a galaxy's underlying mass density profile, under the assumption that the observed rotation produces a centripetal force that exactly balances the inward force of gravity. However, most rotation curves are measured using emission lines from gas, which can experience additional forces due to pressure. In realistic galaxy disks, the gas pressure declines with radius, providing additional radial support to the disk. The measured tangential rotation speed will therefore tend to lag the true circular velocity of a test particle. The gas pressure is dominated by turbulence, and we evaluate its likely amplitude from recent estimates of the gas velocity dispersion and surface density. We show that where the amplitude of the rotation curve is comparable to the characteristic velocities of the interstellar turbulence, pressure support may lead to underestimates of the mass density of the underlying dark matter halo and the inner slope of its density profile. These effects may be significant for galaxies with rotation speeds lsim75 km s-1 but are unlikely to be significant in higher-mass galaxies. We find that pressure support can be sustained over long timescales, because any reduction in support due to the conversion of gas into stars is compensated for by an inward flow of gas. However, we point to many uncertainties in assessing the importance of pressure support in real or simulated galaxies. Thus, while pressure support may help to alleviate possible tensions between rotation curve observations and ΛCDM on kiloparsec scales, it should not be viewed as a definitive solution at this time.

  1. Comparison of theoretical and observed pressure profiles in geothermal wells

    DOE Office of Scientific and Technical Information (OSTI.GOV)

    Marquez M, R.

    Two-phase water-steam flow conditions in geothermal wells are studied aimed at predicting pressure drops in these wells. Five prediction methods were selected to be analyzed and compared with each other and with actual pressure measurements. These five correlations were tested on five wells: three in New Zealand, one in Mexico, and one in the Philippines.

  2. Reconstruction of Pressure Profile Evolution during Levitated Dipole Experiments

    NASA Astrophysics Data System (ADS)

    Mauel, M.; Garnier, D.; Boxer, A.; Ellsworth, J.; Kesner, J.

    2008-11-01

    Magnetic levitation of the LDX superconducting dipole causes significant changes in the measured diamagnetic flux and what appears to be an isotropic plasma pressure profile (p˜p||). This poster describes the reconstruction of plasma current and plasma pressure profiles from external measurements of the equilibrium magnetic field, which vary substantially as a function of time depending upon variations in neutral pressure and multifrequency ECRH power levels. Previous free-boundary reconstructions of plasma equilibrium showed the plasma to be anisotropic and highly peaked at the location of the cyclotron resonance of the microwave heating sources. Reconstructions of the peaked plasma pressures confined by a levitated dipole incorporate the small axial motion of the dipole (±5 mm), time varying levitation coil currents, eddy currents flowing in the vacuum vessel, constant magnetic flux linking the superconductor, and new flux loops located near the hot plasma in order to closely couple to plasma current and dipole current variations. I. Karim, et al., J. Fusion Energy, 26 (2007) 99.

  3. High temperature- and high pressure-processed garlic improves lipid profiles in rats fed high cholesterol diets.

    PubMed

    Sohn, Chan Wok; Kim, Hyunae; You, Bo Ram; Kim, Min Jee; Kim, Hyo Jin; Lee, Ji Yeon; Sok, Dai-Eun; Kim, Jin Hee; Lee, Kun Jong; Kim, Mee Ree

    2012-05-01

    Garlic protects against degenerative diseases such as hyperlipidemia and cardiovascular diseases. However, raw garlic has a strong pungency, which is unpleasant. In this study, we examined the effect of high temperature/high pressure-processed garlic on plasma lipid profiles in rats. Sprague-Dawley rats were fed a normal control diet, a high cholesterol (0.5% cholesterol) diet (HCD) only, or a high cholesterol diet supplemented with 0.5% high temperature/high pressure-processed garlic (HCP) or raw garlic (HCR) for 10 weeks. The body weights of the rats fed the garlic-supplemented diets decreased, mostly because of reduced fat pad weights. Plasma levels of total cholesterol (TC), low-density lipoprotein cholesterol, and triglyceride (TG) in the HCP and HCR groups decreased significantly compared with those in the HCD group. Additionally, fecal TC and TG increased significantly in the HCP and HCR groups. It is notable that no significant differences in plasma or fecal lipid profiles were observed between the HCP and HCR groups. High temperature/high pressure-processed garlic contained a higher amount of S-allyl cysteine than raw garlic (P<.05). The results suggest that high temperature/high pressure-processed garlic may be useful as a functional food to improve lipid profiles.

  4. High Temperature- and High Pressure-Processed Garlic Improves Lipid Profiles in Rats Fed High Cholesterol Diets

    PubMed Central

    Sohn, Chan Wok; Kim, Hyunae; You, Bo Ram; Kim, Min Jee; Kim, Hyo Jin; Lee, Ji Yeon; Sok, Dai-Eun; Kim, Jin Hee; Lee, Kun Jong

    2012-01-01

    Abstract Garlic protects against degenerative diseases such as hyperlipidemia and cardiovascular diseases. However, raw garlic has a strong pungency, which is unpleasant. In this study, we examined the effect of high temperature/high pressure-processed garlic on plasma lipid profiles in rats. Sprague–Dawley rats were fed a normal control diet, a high cholesterol (0.5% cholesterol) diet (HCD) only, or a high cholesterol diet supplemented with 0.5% high temperature/high pressure-processed garlic (HCP) or raw garlic (HCR) for 10 weeks. The body weights of the rats fed the garlic-supplemented diets decreased, mostly because of reduced fat pad weights. Plasma levels of total cholesterol (TC), low-density lipoprotein cholesterol, and triglyceride (TG) in the HCP and HCR groups decreased significantly compared with those in the HCD group. Additionally, fecal TC and TG increased significantly in the HCP and HCR groups. It is notable that no significant differences in plasma or fecal lipid profiles were observed between the HCP and HCR groups. High temperature/high pressure-processed garlic contained a higher amount of S-allyl cysteine than raw garlic (P<.05). The results suggest that high temperature/high pressure-processed garlic may be useful as a functional food to improve lipid profiles. PMID:22404600

  5. Linear pressure profile estimation along a penstock associated with transients due to severe defects

    NASA Astrophysics Data System (ADS)

    Kueny, J. L.; Combes, G.; Lourenço, M.; Clary, V.; Ballester, J. L.

    2014-03-01

    The purpose of this article is to show how the pressure load profile along a penstock of an hydroplant and the corresponding flow rate is obtained from the pressure signal using a code called ACHYL CF. In particular the paper will present how it is possible to reconstruct the history of the incident after a strong transient state, in the case of two plants with Pelton turbines and one DSPCF device on a branch of the circuit. For plant1 the DSPCF device observes an overrun of the maximal allowed pressure after the filling of the injector branch and for plant_2, a strong transient leads to the rupture of the penstock.

  6. Calibration of Raman lidar water vapor profiles by means of AERONET photometer observations and GDAS meteorological data

    NASA Astrophysics Data System (ADS)

    Dai, Guangyao; Althausen, Dietrich; Hofer, Julian; Engelmann, Ronny; Seifert, Patric; Bühl, Johannes; Mamouri, Rodanthi-Elisavet; Wu, Songhua; Ansmann, Albert

    2018-05-01

    We present a practical method to continuously calibrate Raman lidar observations of water vapor mixing ratio profiles. The water vapor profile measured with the multiwavelength polarization Raman lidar PollyXT is calibrated by means of co-located AErosol RObotic NETwork (AERONET) sun photometer observations and Global Data Assimilation System (GDAS) temperature and pressure profiles. This method is applied to lidar observations conducted during the Cyprus Cloud Aerosol and Rain Experiment (CyCARE) in Limassol, Cyprus. We use the GDAS temperature and pressure profiles to retrieve the water vapor density. In the next step, the precipitable water vapor from the lidar observations is used for the calibration of the lidar measurements with the sun photometer measurements. The retrieved calibrated water vapor mixing ratio from the lidar measurements has a relative uncertainty of 11 % in which the error is mainly caused by the error of the sun photometer measurements. During CyCARE, nine measurement cases with cloud-free and stable meteorological conditions are selected to calculate the precipitable water vapor from the lidar and the sun photometer observations. The ratio of these two precipitable water vapor values yields the water vapor calibration constant. The calibration constant for the PollyXT Raman lidar is 6.56 g kg-1 ± 0.72 g kg-1 (with a statistical uncertainty of 0.08 g kg-1 and an instrumental uncertainty of 0.72 g kg-1). To check the quality of the water vapor calibration, the water vapor mixing ratio profiles from the simultaneous nighttime observations with Raman lidar and Vaisala radiosonde sounding are compared. The correlation of the water vapor mixing ratios from these two instruments is determined by using all of the 19 simultaneous nighttime measurements during CyCARE. Excellent agreement with the slope of 1.01 and the R2 of 0.99 is found. One example is presented to demonstrate the full

  7. Numerical Investigation of Pressure Profile in Hydrodynamic Lubrication Thrust Bearing.

    PubMed

    Najar, Farooq Ahmad; Harmain, G A

    2014-01-01

    Reynolds equation is solved using finite difference method (FDM) on the surface of the tilting pad to find the pressure distribution in the lubricant oil film. Different pressure profiles with grid independence are described. The present work evaluates pressure at various locations after performing a thorough grid refinement. In recent similar works, this aspect has not been addressed. However, present study shows that it can have significant effect on the pressure profile. Results of a sector shaped pad are presented and it is shown that the maximum average value of pressure is 12% (approximately) greater than the previous results. Grid independence occurs after 24 × 24 grids. A parameter "ψ" has been proposed to provide convenient indicator of obtaining grid independent results. ψ = |(P refinedgrid - P Refrence-grid)/P refinedgrid|, ψ ≤ ε, where "ε" can be fixed to a convenient value and a constant minimum film thickness value of 75 μm is used in present study. This important parameter is highlighted in the present work; the location of the peak pressure zone in terms of (r, θ) coordinates is getting shifted by changing the grid size which will help the designer and experimentalist to conveniently determine the position of pressure measurement probe.

  8. Numerical Investigation of Pressure Profile in Hydrodynamic Lubrication Thrust Bearing

    PubMed Central

    Najar, Farooq Ahmad; Harmain, G. A.

    2014-01-01

    Reynolds equation is solved using finite difference method (FDM) on the surface of the tilting pad to find the pressure distribution in the lubricant oil film. Different pressure profiles with grid independence are described. The present work evaluates pressure at various locations after performing a thorough grid refinement. In recent similar works, this aspect has not been addressed. However, present study shows that it can have significant effect on the pressure profile. Results of a sector shaped pad are presented and it is shown that the maximum average value of pressure is 12% (approximately) greater than the previous results. Grid independence occurs after 24 × 24 grids. A parameter “ψ” has been proposed to provide convenient indicator of obtaining grid independent results. ψ = |(P refinedgrid − P Refrence-grid)/P refinedgrid|, ψ ≤ ε, where “ε” can be fixed to a convenient value and a constant minimum film thickness value of 75 μm is used in present study. This important parameter is highlighted in the present work; the location of the peak pressure zone in terms of (r, θ) coordinates is getting shifted by changing the grid size which will help the designer and experimentalist to conveniently determine the position of pressure measurement probe. PMID:27350977

  9. Capillary pressure curves for low permeability chalk obtained by NMR imaging of core saturation profiles

    DOE Office of Scientific and Technical Information (OSTI.GOV)

    Norgaard, J.V.; Olsen, D.; Springer, N.

    1995-12-31

    A new technique for obtaining water-oil capillary pressure curves, based on NMR imaging of the saturation distribution in flooded cores is presented. In this technique, a steady state fluid saturation profile is developed by flooding the core at a constant flow rate. At the steady state situation where the saturation distribution no longer changes, the local pressure difference between the wetting and non-wetting phases represents the capillary pressure. The saturation profile is measured using an NMR technique and for a drainage case, the pressure in the non-wetting phase is calculated numerically. The paper presents the NMR technique and the proceduremore » for calculating the pressure distribution in the sample. Inhomogeneous samples produce irregular saturation profiles, which may be interpreted in terms of variation in permeability, porosity, and capillary pressure. Capillary pressure curves for North Sea chalk obtained by the new technique show good agreement with capillary pressure curves obtained by traditional techniques.« less

  10. Complete temperature profiles in ultra-high-pressure liquid chromatography columns.

    PubMed

    Gritti, Fabrice; Guiochon, Georges

    2008-07-01

    The temperature profiles were calculated along and across seven packed columns (lengths 30, 50, 100, and 150 mm, i.d., 1 and 2.1 mm, all packed with Acquity UPLC, BEH-C 18 particles, average d(p) approximately 1.7 microm) and their stainless steel tubes (o.d. 4.53 and 6.35 mm). These columns were kept horizontal and sheltered from forced air convection (i.e., under still air conditions), at room temperature. They were all percolated with pure acetonitrile, either under the maximum pressure drop (1034 bar) or at the maximum flow rate (2 mL/min) permitted by the chromatograph. The heat balance equation of chromatographic columns was discretized and solved numerically with minimum approximation. Both the compressibility and the thermal expansion of the eluent were taken into account. The boundary conditions were determined from the experimental measurements of the column inlet pressure and of the temperature profile along the column wall, which were made with a precision better than +/-0.1 K. These calculation results provide the 3-D temperature profiles along and across the columns. The axial and radial temperature gradients are discussed in relationship with the experimental conditions used. The temperature map obtained permits a prediction of the chromatographic data obtained under a very high pressure gradient.

  11. Microstructure, microbial profile and quality characteristics of high-pressure-treated chicken nuggets.

    PubMed

    Devatkal, Suresh; Anurag, Rahul; Jaganath, Bindu; Rao, Srinivasa

    2015-10-01

    High-pressure processing (300 MPa for 5 min) as a non-thermal post-processing intervention was employed to improve the shelf life and qualities of cooked refrigerated chicken nuggets. Pomegranate peel extract (1%) was also used as a source of natural antioxidant and antimicrobial in chicken nuggets. Microstructure, microbial profile, instrumental colour, texture profile and lipid oxidation were evaluated. High-pressure treatment and pomegranate peel extract did not influence significantly the colour and textural properties of cooked chicken nuggets. Thiobarbituric acid reactive substance values significantly (p < 0.05) increased in pressure-treated nuggets. Microstructural studies revealed shrinkage in the structure and loosening of the dense network of meat emulsion due to high-pressure treatment. Pressure treatment resulted in a reduction of 2-3.0 log10 cfu/g in total plate count and Enterobacteriaceae count. Molecular characterization studies revealed that Enterobacter amnigenus and Enterobacter sp. in control and Bacillus licheniformis, Enterococcus gallinarum and Acinetobacter baumannii in high-pressure-treated chicken nuggets were the major spoilage bacteria. © The Author(s) 2014.

  12. Influence of pelvic floor muscle contraction on the profile of vaginal closure pressure in continent and stress urinary incontinent women.

    PubMed

    Shishido, Keiichi; Peng, Qiyu; Jones, Ruth; Omata, Sadao; Constantinou, Christos E

    2008-05-01

    We characterized the vaginal pressure profile as a representation of closure forces along the length and circumference of the vaginal wall. Vaginal pressure profile data were used to test the hypothesis that the strength of pelvic floor muscle contractions differs significantly between continent women and women with stress urinary incontinence. Vaginal pressure profile recordings were made in 23 continent subjects and in 10 patients with stress urinary incontinence. The recordings characterized closure forces along the entire length of the vagina and identified differences among the anterior, posterior, left and right sides of the vaginal wall. Using a novel, directionally sensitive vaginal probe we made vaginal pressure profile measurements with the women at rest and during pelvic floor muscle contraction while supine. The nature of the vaginal pressure profile was characterized in terms of force distribution in the anterior and posterior vaginal walls, which was significantly greater than that on the left and right sides. The continent group had significant greater maximum pressure than the stress urinary incontinence group on the posterior side at rest (mean +/- SE 3.4 +/- 0.3 vs 2.01 +/- 0.36 N/cm(2)) and during pelvic floor muscle contraction (4.18 +/- 0.26 vs 2.25 +/- 0.41 N/cm(2)). The activity pressure difference between the posterior and anterior vaginal walls in the continent group was significantly increased when the pelvic floor muscles contracted vs that at rest (3.29 +/- 0.21 vs 2.45 +/- 0.26 N/cm(2)). However, the change observed in the stress urinary incontinence group was not significant (1.85 +/- 0.38 vs 1.35 +/- 0.27 N/cm(2)). The results demonstrate that the voluntary pelvic floor muscles impose significant closure forces along the vaginal wall of continent women but not in women with stress urinary incontinence. The implication of these findings is that extrinsic urethral closure pressure is insufficiently augmented by pelvic floor muscle

  13. Pressure profiles of the BRing based on the simulation used in the CSRm

    NASA Astrophysics Data System (ADS)

    Wang, J. C.; Li, P.; Yang, J. C.; Yuan, Y. J.; Wu, B.; Chai, Z.; Luo, C.; Dong, Z. Q.; Zheng, W. H.; Zhao, H.; Ruan, S.; Wang, G.; Liu, J.; Chen, X.; Wang, K. D.; Qin, Z. M.; Yin, B.

    2017-07-01

    HIAF-BRing, a new multipurpose accelerator facility of the High Intensity heavy-ion Accelerator Facility project, requires an extremely high vacuum lower than 10-11 mbar to fulfill the requirements of radioactive beam physics and high energy density physics. To achieve the required process pressure, the bench-marked codes of VAKTRAK and Molflow+ are used to simulate the pressure profiles of the BRing system. In order to ensure the accuracy of the implementation of VAKTRAK, the computational results are verified by measured pressure data and compared with a new simulation code BOLIDE on the current synchrotron CSRm. Since the verification of VAKTRAK has been done, the pressure profiles of the BRing are calculated with different parameters such as conductance, out-gassing rates and pumping speeds. According to the computational results, the optimal parameters are selected to achieve the required pressure for the BRing.

  14. Atmospheric pressure and temperature profiling using near IR differential absorption lidar

    NASA Technical Reports Server (NTRS)

    Korb, C. L.; Schwemmer, G. K.; Dombrowski, M.; Weng, C. Y.

    1983-01-01

    The present investigation is concerned with differential absorption lidar techniques for remotely measuring the atmospheric temperature and pressure profile, surface pressure, and cloud top pressure-height. The procedure used in determining the pressure is based on the conduction of high-resolution measurements of absorption in the wings of lines in the oxygen A band. Absorption with respect to these areas is highly pressure sensitive in connection with the mechanism of collisional line broadening. The method of temperature measurement utilizes a determination of the absorption at the center of a selected line in the oxygen A band which originates from a quantum state with high ground state energy.

  15. Tuning Spatial Profiles of Selection Pressure to Modulate the Evolution of Drug Resistance

    NASA Astrophysics Data System (ADS)

    De Jong, Maxwell G.; Wood, Kevin B.

    2018-06-01

    Spatial heterogeneity plays an important role in the evolution of drug resistance. While recent studies have indicated that spatial gradients of selection pressure can accelerate resistance evolution, much less is known about evolution in more complex spatial profiles. Here we use a stochastic toy model of drug resistance to investigate how different spatial profiles of selection pressure impact the time to fixation of a resistant allele. Using mean first passage time calculations, we show that spatial heterogeneity accelerates resistance evolution when the rate of spatial migration is sufficiently large relative to mutation but slows fixation for small migration rates. Interestingly, there exists an intermediate regime—characterized by comparable rates of migration and mutation—in which the rate of fixation can be either accelerated or decelerated depending on the spatial profile, even when spatially averaged selection pressure remains constant. Finally, we demonstrate that optimal tuning of the spatial profile can dramatically slow the spread and fixation of resistant subpopulations, even in the absence of a fitness cost for resistance. Our results may lay the groundwork for optimized, spatially resolved drug dosing strategies for mitigating the effects of drug resistance.

  16. [Features of diurnal profile of blood pressure in workers having serum aromatic hydrocarbons level].

    PubMed

    Baĭdina, A S; Safonova, M A; Alekseev, V B

    2012-01-01

    Features of diurnal profile of blood pressure in workers having serum level of benzol and ethylbenzene are high systolic and diastolic arterial blood pressure during the day, index of systolic arterial pressure time and index diastolic arterial pressure time was also high. These features should be considered in anti-hypertensives prescription.

  17. Association of physical activity and physical fitness with blood pressure profile in Gujarati Indian adolescents.

    PubMed

    Shaikh, Wasim A; Patel, Minal C; Singh, S K

    2011-01-01

    The current study was conducted to determine how physical activity level and physical fitness affects the blood pressure profile of Gujarati Indian adolescents so as to help in developing preventive strategies for the local population as ethnic differences exist in the aetiopathogenesis of hypertension. A cross-sectional study was conducted on 485 Gujarati Indian adolescent boys and girls of age group 16-19 years. Physical activity level was assessed using Johnson Space Center/NASA Physical Activity Rating Scale and VO2 max was used to assess the physical fitness. Body composition was assessed in terms of Body Mass Index, Fat Mass Index and Waist Circumference. Blood Pressure was measured by oscillometry. One-way ANOVA was used to study if any significant differences (P<0.05) existed in the blood pressure profile between the high, moderate and low physical activity groups. Pearson's correlation coefficient was determined to assess the relationship between VO2 max and blood pressure profile. In girls, physical activity level was not found to have a significant effect on the blood pressure profile. In boys, systolic blood pressure and mean arterial pressure were found to be significantly higher in Moderate Physical Activity Group as compared to Low Physical Activity Group. PVO2 max was found to have a significant negative correlationship with SBP, DBP and MAP in girls and a significant negative correlationship with SBP, PP and MAP in boys. It could thus be concluded that a better physical fitness rather than a higher physical activity level could keep the blood pressure in check in the Gujarati Indian adolescents.

  18. Critical Analysis of Different Methods to Retrieve Atmosphere Humidity Profiles from GNSS Radio Occultation Observations

    NASA Astrophysics Data System (ADS)

    Vespe, Francesco; Benedetto, Catia

    2013-04-01

    The huge amount of GPS Radio Occultation (RO) observations currently available thanks to space mission like COSMIC, CHAMP, GRACE, TERRASAR-X etc., have greatly encouraged the research of new algorithms suitable to extract humidity, temperature and pressure profiles of the atmosphere in a more and more precise way. For what concern the humidity profiles in these last years two different approaches have been widely proved and applied: the "Simple" and the 1DVAR methods. The Simple methods essentially determine dry refractivity profiles from temperature analysis profiles and hydrostatic equation. Then the dry refractivity is subtracted from RO refractivity to achieve the wet component. Finally from the wet refractivity is achieved humidity. The 1DVAR approach combines RO observations with profiles given by the background models with both the terms weighted with the inverse of covariance matrix. The advantage of "Simple" methods is that they are not affected by bias due to the background models. We have proposed in the past the BPV approach to retrieve humidity. Our approach can be classified among the "Simple" methods. The BPV approach works with dry atmospheric CIRA-Q models which depend on latitude, DoY and height. The dry CIRA-Q refractivity profile is selected estimating the involved parameters in a non linear least square fashion achieved by fitting RO observed bending angles through the stratosphere. The BPV as well as all the other "Simple" methods, has as drawback the unphysical occurrence of negative "humidity". Thus we propose to apply a modulated weighting of the fit residuals just to minimize the effects of this inconvenient. After a proper tuning of the approach, we plan to present the results of the validation.

  19. Validation of 10-year SAO OMI Ozone Profile (PROFOZ) product using ozonesonde observations

    NASA Astrophysics Data System (ADS)

    Huang, Guanyu; Liu, Xiong; Chance, Kelly; Yang, Kai; Bhartia, Pawan K.; Cai, Zhaonan; Allaart, Marc; Ancellet, Gérard; Calpini, Bertrand; Coetzee, Gerrie J. R.; Cuevas-Agulló, Emilio; Cupeiro, Manuel; De Backer, Hugo; Dubey, Manvendra K.; Fuelberg, Henry E.; Fujiwara, Masatomo; Godin-Beekmann, Sophie; Hall, Tristan J.; Johnson, Bryan; Joseph, Everette; Kivi, Rigel; Kois, Bogumil; Komala, Ninong; König-Langlo, Gert; Laneve, Giovanni; Leblanc, Thierry; Marchand, Marion; Minschwaner, Kenneth R.; Morris, Gary; Newchurch, Michael J.; Ogino, Shin-Ya; Ohkawara, Nozomu; Piters, Ankie J. M.; Posny, Françoise; Querel, Richard; Scheele, Rinus; Schmidlin, Frank J.; Schnell, Russell C.; Schrems, Otto; Selkirk, Henry; Shiotani, Masato; Skrivánková, Pavla; Stübi, René; Taha, Ghassan; Tarasick, David W.; Thompson, Anne M.; Thouret, Valérie; Tully, Matthew B.; Van Malderen, Roeland; Vömel, Holger; von der Gathen, Peter; Witte, Jacquelyn C.; Yela, Margarita

    2017-07-01

    We validate the Ozone Monitoring Instrument (OMI) Ozone Profile (PROFOZ) product from October 2004 through December 2014 retrieved by the Smithsonian Astrophysical Observatory (SAO) algorithm against ozonesonde observations. We also evaluate the effects of OMI row anomaly (RA) on the retrieval by dividing the dataset into before and after the occurrence of serious OMI RA, i.e., pre-RA (2004-2008) and post-RA (2009-2014). The retrieval shows good agreement with ozonesondes in the tropics and midlatitudes and for pressure < ˜ 50 hPa in the high latitudes. It demonstrates clear improvement over the a priori down to the lower troposphere in the tropics and down to an average of ˜ 550 (300) hPa at middle (high) latitudes. In the tropics and midlatitudes, the profile mean biases (MBs) are less than 6 %, and the standard deviations (SDs) range from 5 to 10 % for pressure < ˜ 50 hPa to less than 18 % (27 %) in the tropics (midlatitudes) for pressure > ˜ 50 hPa after applying OMI averaging kernels to ozonesonde data. The MBs of the stratospheric ozone column (SOC, the ozone column from the tropopause pressure to the ozonesonde burst pressure) are within 2 % with SDs of < 5 % and the MBs of the tropospheric ozone column (TOC) are within 6 % with SDs of 15 %. In the high latitudes, the profile MBs are within 10 % with SDs of 5-15 % for pressure < ˜ 50 hPa but increase to 30 % with SDs as great as 40 % for pressure > ˜ 50 hPa. The SOC MBs increase up to 3 % with SDs as great as 6 % and the TOC SDs increase up to 30 %. The comparison generally degrades at larger solar zenith angles (SZA) due to weaker signals and additional sources of error, leading to worse performance at high latitudes and during the midlatitude winter. Agreement also degrades with increasing cloudiness for pressure > ˜ 100 hPa and varies with cross-track position, especially with large MBs and SDs at extreme off-nadir positions. In the tropics and midlatitudes, the post-RA comparison is considerably

  20. Effects of sub-lethal high-pressure homogenization treatment on the outermost cellular structures and the volatile-molecule profiles of two strains of probiotic lactobacilli.

    PubMed

    Tabanelli, Giulia; Vernocchi, Pamela; Patrignani, Francesca; Del Chierico, Federica; Putignani, Lorenza; Vinderola, Gabriel; Reinheimer, Jorge A; Gardini, Fausto; Lanciotti, Rosalba

    2015-01-01

    Applying sub-lethal levels of high-pressure homogenization (HPH) to lactic acid bacteria has been proposed as a method of enhancing some of their functional properties. Because the principal targets of HPH are the cell-surface structures, the aim of this study was to examine the effect of sub-lethal HPH treatment on the outermost cellular structures and the proteomic profiles of two known probiotic bacterial strains. Moreover, the effect of HPH treatment on the metabolism of probiotic cells within a dairy product during its refrigerated storage was investigated using SPME-GC-MS. Transmission electron microscopy was used to examine the microstructural changes in the outermost cellular structures due to HPH treatment. These alterations may be involved in the changes in some of the technological and functional properties of the strains that were observed after pressure treatment. Moreover, the proteomic profiles of the probiotic strains treated with HPH and incubated at 37°C for various periods showed different peptide patterns compared with those of the untreated cells. In addition, there were differences in the peaks that were observed in the low-mass spectral region (2000-3000 Da) of the spectral profiles of the control and treated samples. Due to pressure treatment, the volatile-molecule profiles of buttermilk inoculated with treated or control cells and stored at 4°C for 30 days exhibited overall changes in the aroma profile and in the production of molecules that improved its sensory profile, although the two different species imparted specific fingerprints to the product. The results of this study will contribute to understanding the changes that occur in the outermost cellular structures and the metabolism of LAB in response to HPH treatment. The findings of this investigation may contribute to elucidating the relationships between these changes and the alterations of the technological and functional properties of LAB induced by pressure treatment.

  1. Simulating Pressure Profiles for the Free-Electron Laser Photoemission Gun Using Molflow+

    NASA Astrophysics Data System (ADS)

    Song, Diego; Hernandez-Garcia, Carlos

    2012-10-01

    The Jefferson Lab Free Electron Laser (FEL) generates tunable laser light by passing a relativistic electron beam generated in a high-voltage DC electron gun with a semiconducting photocathode through a magnetic undulator. The electron gun is in stringent vacuum conditions in order to guarantee photocathode longevity. Considering an upgrade of the electron gun, this project consists of simulating pressure profiles to determine if the novel design meets the electron gun vacuum requirements. The method of simulation employs the software Molflow+, developed by R. Kersevan at the Organisation Europ'eene pour la Recherche Nucl'eaire (CERN), which uses the test-particle Monte Carlo method to simulate molecular flows in 3D structures. Pressure is obtained along specified chamber axes. Results are then compared to measured pressure values from the existing gun for validation. Outgassing rates, surface area, and pressure were found to be proportionally related. The simulations indicate that the upgrade gun vacuum chamber requires more pumping compared to its predecessor, while it holds similar vacuum conditions. The ability to simulate pressure profiles through tools like Molflow+, allows researchers to optimize vacuum systems during the engineering process.

  2. Functional morphology of the lower esophageal sphincter and crural diaphragm determined by three-dimensional high-resolution esophago-gastric junction pressure profile and CT imaging.

    PubMed

    Mittal, Ravinder K; Zifan, Ali; Kumar, Dushyant; Ledgerwood-Lee, Melissa; Ruppert, Erika; Ghahremani, Gary

    2017-09-01

    greater curvature. The pressure profile revealed circular and axial pressure asymmetry, with greatest pressure and shortest cranio-caudal length on the left (close to the angle of His). The CD contraction with tidal and forced inspiration increases pressure in the cranial half of the LES pressure profile, and it was placed horizontally across the recording. The CD, esophagus, and stomach were outlined in the CT scan images to construct a 3-D anatomy of the region; it revealed that the hiatus (CD) is placed obliquely across the esophagus; however, because of the bend of the esophagus to the left at the upper edge of the hiatus, the two were placed at right angle to each other, which resulted in a horizontal pressure profile of the CD on the LES. Our observations suggest a unique shape of the LES, CD, and the anatomical relationship between the two, which provides a possible explanation as to why the LES pressure shows circumferential and axial asymmetry. Our findings have implication for the length and circumferential orientation of myotomy incision required for the ablation of LES pressure in achalasia esophagus. NEW & NOTEWORTHY We used computed tomography scan imaging with three-dimensional esophago-gastric junction (EGJ) pressure recordings to determine functional morphology of the lower esophageal sphincter (LES) and crural diaphragm and its relationship to EGJ anatomy. The LES pressure profile was unique with the LES length longer and pressures lower toward the lesser curvature of the stomach, as compared with the greater curvature. Our findings have implications for the length and circumferential orientation of myotomy incision required for the ablation of LES pressure in the achalasia esophagus. Copyright © 2017 the American Physiological Society.

  3. Seasonal Variations in the CO Line Profile and the Retrieved Thermal/Pressure Structures in the Atmosphere of Mars

    NASA Astrophysics Data System (ADS)

    Khayat, Alain; Villanueva, G. L.; Mumma, M. J.; Riesen, T. E.; Tokunaga, A. T.

    2013-10-01

    We report retrievals of temperature vertical profiles up to 100 km over Tharsis and Syrtis regions on Mars obtained by inverting the strong rotational (3-2) line of carbon monoxide (CO) at 346 GHz. Observations of CO were made from mid Northern Spring to early Northern Summer on Mars (Ls= 36°-108°, 23 Nov, 2011 - 13 May, 2012) using the Caltech Submillimeter Observatory's (CSO) high-resolution heterodyne receiver (Barney) on top of Mauna Kea, Hawai'i. The temperature profiles were derived using our radiative transfer model that considers the latest spectroscopic constants for CO collisionally broadened by CO2. We observe notable changes of the line profile for different dates, which are directly related to seasonal variations in the thermal/pressure structure of the atmosphere. The seasonal variability of the martian CO line profile, the extracted temperature profiles, and comparisons with modeled profiles from the Mars Climate Database (Lewis et al, 1999) will be presented. We gratefully acknowledge support from the NASA Planetary Astronomy Program , NASA Astrobiology Institute, Planetary Atmospheres programs. This material is based upon work at the Caltech Submillimeter Observatory, which is operated by the California Institute of Technology under cooperative agreement with the National Science Foundation, grant number AST-0838261.

  4. Monitoring pressure profiles across an airfoil with a fiber Bragg grating sensor array

    NASA Astrophysics Data System (ADS)

    Papageorgiou, Anthony W.; Parkinson, Luke A.; Karas, Andrew R.; Hansen, Kristy L.; Arkwright, John W.

    2018-02-01

    Fluid flow over an airfoil section creates a pressure difference across the upper and lower surfaces, thus generating lift. Successful wing design is a combination of engineering design and experience in the field, with subtleties in design and manufacture having significant impact on the amount of lift produced. Current methods of airfoil optimization and validation typically involve computational fluid dynamics (CFD) and extensive wind tunnel testing with pressure sensors embedded into the airfoil to measure the pressure over the wing. Monitoring pressure along an airfoil in a wind tunnel is typically achieved using surface pressure taps that consist of hollow tubes running from the surface of the airfoil to individual pressure sensors external to the tunnel. These pressure taps are complex to configure and not ideal for in-flight testing. Fiber Bragg grating (FBG) pressure sensing arrays provide a highly viable option for both wind tunnel and inflight pressure measurement. We present a fiber optic sensor array that can detect positive and negative pressure suitable for validating CFD models of airfoil profile sections. The sensing array presented here consists of 6 independent sensing elements, each capable of a pressure resolution of less than 10 Pa over the range of 70 kPa to 120 kPa. The device has been tested with the sensor array attached to a 90mm chord length airfoil section subjected to low velocity flow. Results show that the arrays are capable of accurately detecting variations of the pressure profile along the airfoil as the angle of attack is varied from zero to the point at which stall occurs.

  5. Theoretical model of ice nucleation induced by acoustic cavitation. Part 1: Pressure and temperature profiles around a single bubble.

    PubMed

    Cogné, C; Labouret, S; Peczalski, R; Louisnard, O; Baillon, F; Espitalier, F

    2016-03-01

    This paper deals with the inertial cavitation of a single gas bubble in a liquid submitted to an ultrasonic wave. The aim was to calculate accurately the pressure and temperature at the bubble wall and in the liquid adjacent to the wall just before and just after the collapse. Two different approaches were proposed for modeling the heat transfer between the ambient liquid and the gas: the simplified approach (A) with liquid acting as perfect heat sink, the rigorous approach (B) with liquid acting as a normal heat conducting medium. The time profiles of the bubble radius, gas temperature, interface temperature and pressure corresponding to the above models were compared and important differences were observed excepted for the bubble size. The exact pressure and temperature distributions in the liquid corresponding to the second model (B) were also presented. These profiles are necessary for the prediction of any physical phenomena occurring around the cavitation bubble, with possible applications to sono-crystallization. Copyright © 2015 Elsevier B.V. All rights reserved.

  6. Experimental Studies of Low-Pressure Turbine Flows and Flow Control. Streamwise Pressure Profiles and Velocity Profiles

    NASA Technical Reports Server (NTRS)

    Volino, Ralph

    2012-01-01

    faculties. The geometry corresponded to "Pak B" LPT airfoil. The test section simulated LPT flow in a passage. Three experimental studies were performed: (a) Boundary layer measurements for ten baseline cases under high and low freestream turbulence conditions at five Reynolds numbers of 25,000, 50,000, 100,000, 200,000, and 300,000, based on passage exit velocity and suction surface wetted length; (b) Passive flow control studies with three thicknesses of two-dimensional bars, and two heights of three-dimensional circular cylinders with different spanwise separations, at same flow conditions as the 10 baseline cases; (c) Active flow control with oscillating synthetic (zero net mass flow) vortex generator jets, for one case with low freestream turbulence and a low Reynolds number of 25,000. The Passive flow control was successful at controlling the separation problem at low Reynolds numbers, with varying degrees of success from case to case and varying levels of impact at higher Reynolds numbers. The active flow control successfully eliminated the large separation problem for the low Reynolds number case. Very detailed data was acquired using hot-wire anemometry, including single and two velocity components, integral boundary layer quantities, turbulence statistics and spectra, turbulent shear stresses and their spectra, and intermittency, documenting transition, separation and reattachment. Models were constructed to correlate the results. The report includes a summary of the work performed and reprints of the publications describing the various studies. The folders in this supplement contain processed data in ASCII format. Streamwise pressure profiles and velocity profiles are included. The velocity profiles were acquired using single sensor and cross sensor hot-wire probes which were traversed from the wall to the freestream at various streamwise locations. In some of the flow control cases (3D Trips and Jets) profiles were acquired at multiple spanwise locations.

  7. Ram Pressure Stripping: Observations Meet Simulations

    NASA Astrophysics Data System (ADS)

    Past, Matthew; Ruszkowski, Mateusz; Sharon, Keren

    2017-01-01

    Ram pressure stripping occurs when a galaxy falls into the potential well of a cluster, removing gas and dust as the galaxy travels through the intracluster medium. This interaction leads to filamentary gas tails stretching behind the galaxy and plays an important role in galaxy evolution. Previously, these “jellyfish” galaxies had only been observed in nearby clusters, but recently, higher redshift (z > 0.3) examples have been found from HST data imaging.Recent work has shown that cosmic rays injected by supernovae can cause galactic disks to thicken due to cosmic ray pressure. We run three-dimensional magneto-hydrodynamical simulations of ram pressure stripping including cosmic rays to compare to previous models. We study how the efficiency of the ram pressure stripping of the gas, and the morphology of the filamentary tails, depend on the magnitude of the cosmic ray pressure support. We generate mock X-ray images and radio polarization data. Simultaneously, we perform an exhaustive search of the HST archive to increase the sample of jellyfish galaxies and compare selected cases to simulations.

  8. Real-time measurement of the vaginal pressure profile using an optical-fiber-based instrumented speculum.

    PubMed

    Parkinson, Luke A; Gargett, Caroline E; Young, Natharnia; Rosamilia, Anna; Vashi, Aditya V; Werkmeister, Jerome A; Papageorgiou, Anthony W; Arkwright, John W

    2016-12-01

    Pelvic organ prolapse (POP) occurs when changes to the pelvic organ support structures cause descent or herniation of the pelvic organs into the vagina. Clinical evaluation of POP is a series of manual measurements known as the pelvic organ prolapse quantification (POP-Q) score. However, it fails to identify the mechanism causing POP and relies on the skills of the practitioner. We report on a modified vaginal speculum incorporating a double-helix fiber-Bragg grating structure for distributed pressure measurements along the length of the vagina and include preliminary data in an ovine model of prolapse. Vaginal pressure profiles were recorded at 10 Hz as the speculum was dilated incrementally up to 20 mm. At 10-mm dilation, nulliparous sheep showed higher mean pressures ( 102 ± 46 ?? mmHg ) than parous sheep ( 39 ± 23 ?? mmHg ) ( P = 0.02 ), attributable largely to the proximal (cervical) end of the vagina. In addition to overall pressure variations, we observed a difference in the distribution of pressure that related to POP-Q measurements adapted for the ovine anatomy, showing increased tissue laxity in the upper anterior vagina for parous ewes. We demonstrate the utility of the fiber-optic instrumented speculum for rapid distributed measurement of vaginal support.

  9. Real-time measurement of the vaginal pressure profile using an optical-fiber-based instrumented speculum

    NASA Astrophysics Data System (ADS)

    Parkinson, Luke A.; Gargett, Caroline E.; Young, Natharnia; Rosamilia, Anna; Vashi, Aditya V.; Werkmeister, Jerome A.; Papageorgiou, Anthony W.; Arkwright, John W.

    2016-12-01

    Pelvic organ prolapse (POP) occurs when changes to the pelvic organ support structures cause descent or herniation of the pelvic organs into the vagina. Clinical evaluation of POP is a series of manual measurements known as the pelvic organ prolapse quantification (POP-Q) score. However, it fails to identify the mechanism causing POP and relies on the skills of the practitioner. We report on a modified vaginal speculum incorporating a double-helix fiber-Bragg grating structure for distributed pressure measurements along the length of the vagina and include preliminary data in an ovine model of prolapse. Vaginal pressure profiles were recorded at 10 Hz as the speculum was dilated incrementally up to 20 mm. At 10-mm dilation, nulliparous sheep showed higher mean pressures (102±46 mmHg) than parous sheep (39±23 mmHg) (P=0.02), attributable largely to the proximal (cervical) end of the vagina. In addition to overall pressure variations, we observed a difference in the distribution of pressure that related to POP-Q measurements adapted for the ovine anatomy, showing increased tissue laxity in the upper anterior vagina for parous ewes. We demonstrate the utility of the fiber-optic instrumented speculum for rapid distributed measurement of vaginal support.

  10. Measurements of the vertical profile of water vapor abundance in the Martian atmosphere from Mars Observer

    NASA Technical Reports Server (NTRS)

    Schofield, J. T.; Mccleese, Daniel J.

    1988-01-01

    An analysis is presented of the Pressure Modulator Infrared Radiometer (PMIRR) capabilities along with how the vertical profiles of water vapor will be obtained. The PMIRR will employ filter and pressure modulation radiometry using nine spectral channels, in both limb scanning and nadir sounding modes, to obtain daily, global maps of temperature, dust extinction, condensate extinction, and water vapor mixing ratio profiles as a function of pressure to half scale height or 5 km vertical resolution. Surface thermal properties will also be mapped, and the polar radiactive balance will be monitored.

  11. The urethral pressure profiles in continent and stress-incontinent women.

    PubMed

    Henriksson, L; Andersson, K E; Ulmsten, U

    1979-01-01

    Simultaneous urethrocystometry, including recording of the urethral pressure profile, was performed in 127 women aged 30 to 69 years; 42 of the women were free from urologic disorders and 85 had stress incontinence of urine. Both groups were subgrouped according to age. The results in the continent and the incontinent women were analyzed separately, in order to disclose any age-related changes. The data within each decade of age were also comparatively analyzed. In the bladder pressure at rest no age-related changes were found, and the readings were similar in the continent and the incontinent women. The maximum urethral pressure fell significantly with rising age in both groups and was significantly reduced in stress incontinence. The urethral closure pressure showed variations similar to those in the maximum urethral pressure. No lower limit of urethral closure pressure that definitely predisposed to stress incontinence could be established. The functional length of the urethra diminished significantly with rising age in the continent, but not in the incontinent women. The absolute length of the urethra did not show such diminution. Both the functional and the absolute urethral length were significantly less in the incontinent than in the continent women in the age groups between 30 and 49 years.

  12. Observations of wave-induced pore pressure gradients and bed level response on a surf zone sandbar

    NASA Astrophysics Data System (ADS)

    Anderson, Dylan; Cox, Dan; Mieras, Ryan; Puleo, Jack A.; Hsu, Tian-Jian

    2017-06-01

    Horizontal and vertical pressure gradients may be important physical mechanisms contributing to onshore sediment transport beneath steep, near-breaking waves in the surf zone. A barred beach was constructed in a large-scale laboratory wave flume with a fixed profile containing a mobile sediment layer on the crest of the sandbar. Horizontal and vertical pore pressure gradients were obtained by finite differences of measurements from an array of pressure transducers buried within the upper several centimeters of the bed. Colocated observations of erosion depth were made during asymmetric wave trials with wave heights between 0.10 and 0.98 m, consistently resulting in onshore sheet flow sediment transport. The pore pressure gradient vector within the bed exhibited temporal rotations during each wave cycle, directed predominantly upward under the trough and then rapidly rotating onshore and downward as the wavefront passed. The magnitude of the pore pressure gradient during each phase of rotation was correlated with local wave steepness and relative depth. Momentary bed failures as deep as 20 grain diameters were coincident with sharp increases in the onshore-directed pore pressure gradients, but occurred at horizontal pressure gradients less than theoretical critical values for initiation of the motion for compact beds. An expression combining the effects of both horizontal and vertical pore pressure gradients with bed shear stress and soil stability is used to determine that failure of the bed is initiated at nonnegligible values of both forces.Plain Language SummaryThe <span class="hlt">pressure</span> gradient present within the seabed beneath breaking waves may be an important physical mechanism transporting sediment. A large-scale laboratory was used to replicate realistic surfzone conditions in controlled tests, allowing for horizontal and vertical <span class="hlt">pressure</span> gradient magnitudes and the resulting sediment bed response to be <span class="hlt">observed</span> with</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2015AGUFMIN11F1808C','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2015AGUFMIN11F1808C"><span>TOLNet Data Format for Lidar Ozone <span class="hlt">Profile</span> & Surface <span class="hlt">Observations</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Chen, G.; Aknan, A. A.; Newchurch, M.; Leblanc, T.</p> <p>2015-12-01</p> <p>The Tropospheric Ozone Lidar Network (TOLNet) is an interagency initiative started by NASA, NOAA, and EPA in 2011. TOLNet currently has six Lidars and one ozonesonde station. TOLNet provides high-resolution spatio-temporal measurements of tropospheric (surface to tropopause) ozone and aerosol vertical <span class="hlt">profiles</span> to address fundamental air-quality science questions. The TOLNet data format was developed by TOLNet members as a community standard for reporting ozone <span class="hlt">profile</span> <span class="hlt">observations</span>. The development of this new format was primarily based on the existing NDAAC (Network for the Detection of Atmospheric Composition Change) format and ICARTT (International Consortium for Atmospheric Research on Transport and Transformation) format. The main goal is to present the Lidar <span class="hlt">observations</span> in self-describing and easy-to-use data files. The TOLNet format is an ASCII format containing a general file header, individual <span class="hlt">profile</span> headers, and the <span class="hlt">profile</span> data. The last two components repeat for all <span class="hlt">profiles</span> recorded in the file. The TOLNet format is both human and machine readable as it adopts standard metadata entries and fixed variable names. In addition, software has been developed to check for format compliance. To be presented is a detailed description of the TOLNet format protocol and scanning software.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://www.dtic.mil/docs/citations/AD1018036','DTIC-ST'); return false;" href="http://www.dtic.mil/docs/citations/AD1018036"><span>Code Description for Generation of Meteorological Height and <span class="hlt">Pressure</span> Level and Layer <span class="hlt">Profiles</span></span></a></p> <p><a target="_blank" href="http://www.dtic.mil/">DTIC Science & Technology</a></p> <p></p> <p>2016-06-01</p> <p>defined by user input height or <span class="hlt">pressure</span> levels. It can process input <span class="hlt">profiles</span> from sensing systems such as radiosonde, lidar, or wind <span class="hlt">profiling</span> radar...nearly the same way, but the split between wind and temperature/humidity (TH) special levels leads to some changes to one other routine. If changes are...top of the sounding, sometimes the moisture, the thermal, both thermal and moisture, and/or the wind data are missing. Missing data items in the</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/12545631','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/12545631"><span>[Ejaculatory <span class="hlt">profile</span>: a <span class="hlt">pressure</span> of 5 meters H2O at the level of the bladder neck during ejaculation].</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Hugonnet, Christophe L; Böhlen, Dominik; Schmid, Hans-Peter</p> <p>2002-12-01</p> <p>The existence of a <span class="hlt">pressure</span> gradient in order to prevent retrograde ejaculation in men with no ejaculatory disorders has always been postulated, but without any scientific evidence. The <span class="hlt">profile</span> of the prostatic urethra was recorded during ejaculation in 5 men with no ejaculatory disorders using a 10 F balloon catheter with 16 <span class="hlt">pressure</span> channels, situated in pairs every 5 mm, starting just below the balloon in the bladder neck and extending as far as the external urethral sphincter. The <span class="hlt">pressure</span> in the proximal part of the proximal urethra was 500 cm H2O in the five men, but this <span class="hlt">pressure</span> did not exceed 400 cm H2O distally as far as the colliculus seminalis. The authors present a new method for recording the urethral <span class="hlt">pressure</span> <span class="hlt">profile</span> during ejaculation (ejaculatory <span class="hlt">profile</span>). This study provides a better understanding of the mechanisms of normal ejaculation and could be useful for the evaluation of disorders of ejaculation.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/19870000849','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/19870000849"><span>Airborne Lidar measurements of the atmospheric <span class="hlt">pressure</span> <span class="hlt">profile</span> with tunable Alexandrite lasers</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Korb, C. L.; Schwemmer, G. K.; Dombrowski, M.; Milrod, J.; Walden, H.</p> <p>1986-01-01</p> <p>The first remote measurements of the atmospheric <span class="hlt">pressure</span> <span class="hlt">profile</span> made from an airborne platform are described. The measurements utilize a differential absorption lidar and tunable solid state Alexandrite lasers. The <span class="hlt">pressure</span> measurement technique uses a high resolution oxygen A band where the absorption is highly <span class="hlt">pressure</span> sensitive due to collision broadening. Absorption troughs and regions of minimum absorption were used between pairs of stongly absorption lines for these measurements. The trough technique allows the measurement to be greatly desensitized to the effects of laser frequency instabilities. The lidar system was set up to measure <span class="hlt">pressure</span> with the on-line laser tuned to the absorption trough at 13147.3/cm and with the reference laser tuned to a nonabsorbing frequency near 13170.0/cm. The lidar signal returns were sampled with a 200 range gate (30 vertical resoltion) and averaged over 100 shots.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/25522744','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/25522744"><span>Plasma lipid <span class="hlt">profile</span> in Nigerians with high--normal blood <span class="hlt">pressure</span>.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Saidu, Hadiza; Karaye, Kamilu Musa; Okeahialam, Basil N</p> <p>2014-12-18</p> <p>High blood <span class="hlt">pressure</span> levels have been associated with elevated atherogenic blood lipid fraction, but epidemiological surveys often give inconsistent results across population sub-groups. To determine the extent to which there are differences in lipid <span class="hlt">profile</span> based on blood <span class="hlt">pressure</span> levels, we assessed lipid <span class="hlt">profile</span> of subjects with high-normal blood <span class="hlt">pressure</span> and compared with those of hypertensives and optimally normal blood <span class="hlt">pressure</span>. The study was a cross-sectional comparative study conducted at Aminu Kano Teaching Hospital, Kano, Nigeria. Fasting lipid levels were examined among randomly selected patients with optimally normal blood <span class="hlt">pressure</span> (group 1), high-normal blood <span class="hlt">pressure</span> (group 2) and those with hypertension (group 3). Optimal blood <span class="hlt">pressure</span> was defined as systolic blood <span class="hlt">pressure</span> (SBP) of <120 mmHg/or diastolic blood <span class="hlt">pressure</span> (DBP) of <80 mmHg; and high-normal blood <span class="hlt">pressure</span> as SBP of 130-139 mmHg and/or DBP of 85-89 mmHg. A total of 300 subjects were studied, 100 in each group. The mean age of subjects in group 1 was 27.32±8.20 years and 60% were female, while that of group 2 was 34.04±6.25 years, and 53% were female, and that for group 3 was 52.81±13.3 years and 56% were female. The mean total cholesterol (TC) for subjects in group1 (3.96±0.40 mmol/L) was significantly lower than levels in group2 (4.55±1.01 mmol/L); P=<0.001. Subjects in group 3 (5.20±1.88 mmol/L), however had statistically significant higher mean TC when compared with group 2; (P=0.03). The difference between the groups for low density lipoprotein cholesterol (LDL-C) and triglycerides (TG) followed the same pattern as that of TC, with statistically significant increasing trend across the blood <span class="hlt">pressure</span> categories. Levels of high density lipoprotein cholesterol (HDL-C) were however similar across the three groups (group 2 versus group 1; P=0.49, group 2 versus group 3; P=0.9). Increased TC (>5.2 mmol/L) was absent in group1, but found among 11% of group2 subjects and 40% of</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://ntrs.nasa.gov/search.jsp?R=19890062959&hterms=atmospheric+pressure&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D60%26Ntt%3Datmospheric%2Bpressure','NASA-TRS'); return false;" href="https://ntrs.nasa.gov/search.jsp?R=19890062959&hterms=atmospheric+pressure&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D60%26Ntt%3Datmospheric%2Bpressure"><span>Airborne and ground based lidar measurements of the atmospheric <span class="hlt">pressure</span> <span class="hlt">profile</span></span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Korb, C. Laurence; Schwemmer, Geary K.; Dombrowski, Mark; Weng, Chi Y.</p> <p>1989-01-01</p> <p>The first high accuracy remote measurements of the atmospheric <span class="hlt">pressure</span> <span class="hlt">profile</span> have been made. The measurements were made with a differential absorption lidar system that utilizes tunable alexandrite lasers. The absorption in the trough between two lines in the oxygen A-band near 760 nm was used for probing the atmosphere. Measurements of the two-dimensional structure of the <span class="hlt">pressure</span> field were made in the troposphere from an aircraft looking down. Also, measurements of the one-dimensional structure were made from the ground looking up. Typical <span class="hlt">pressure</span> accuracies for the aircraft measurements were 1.5-2 mbar with a 30-m vertical resolution and a 100-shot average (20 s), which corresponds to a 2-km horizontal resolution. Typical accuracies for the upward viewing ground based measurements were 2.0 mbar for a 30-m resolution and a 100-shot average.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/10835248','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/10835248"><span>Modeling conductive heat transfer during high-<span class="hlt">pressure</span> thawing processes: determination of latent heat as a function of <span class="hlt">pressure</span>.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Denys, S; Van Loey, A M; Hendrickx, M E</p> <p>2000-01-01</p> <p>A numerical heat transfer model for predicting product temperature <span class="hlt">profiles</span> during high-<span class="hlt">pressure</span> thawing processes was recently proposed by the authors. In the present work, the predictive capacity of the model was considerably improved by taking into account the <span class="hlt">pressure</span> dependence of the latent heat of the product that was used (Tylose). The effect of <span class="hlt">pressure</span> on the latent heat of Tylose was experimentally determined by a series of freezing experiments conducted at different <span class="hlt">pressure</span> levels. By combining a numerical heat transfer model for freezing processes with a least sum of squares optimization procedure, the corresponding latent heat at each <span class="hlt">pressure</span> level was estimated, and the obtained <span class="hlt">pressure</span> relation was incorporated in the original high-<span class="hlt">pressure</span> thawing model. Excellent agreement with the experimental temperature <span class="hlt">profiles</span> for both high-<span class="hlt">pressure</span> freezing and thawing was <span class="hlt">observed</span>.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/19930092109','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/19930092109"><span>Airfoil <span class="hlt">profiles</span> for minimum <span class="hlt">pressure</span> drag at supersonic velocities -- general analysis with application to linearized supersonic flow</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Chapman, Dean R</p> <p>1952-01-01</p> <p>A theoretical investigation is made of the airfoil <span class="hlt">profile</span> for minimum <span class="hlt">pressure</span> drag at zero lift in supersonic flow. In the first part of the report a general method is developed for calculating the <span class="hlt">profile</span> having the least <span class="hlt">pressure</span> drag for a given auxiliary condition, such as a given structural requirement or a given thickness ratio. The various structural requirements considered include bending strength, bending stiffness, torsional strength, and torsional stiffness. No assumption is made regarding the trailing-edge thickness; the optimum value is determined in the calculations as a function of the base <span class="hlt">pressure</span>. To illustrate the general method, the optimum airfoil, defined as the airfoil having minimum <span class="hlt">pressure</span> drag for a given auxiliary condition, is calculated in a second part of the report using the equations of linearized supersonic flow.</p> </li> </ol> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_1");'>1</a></li> <li><a href="#" onclick='return showDiv("page_2");'>2</a></li> <li class="active"><span>3</span></li> <li><a href="#" onclick='return showDiv("page_4");'>4</a></li> <li><a href="#" onclick='return showDiv("page_5");'>5</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div><!-- col-sm-12 --> </div><!-- row --> </div><!-- page_3 --> <div id="page_4" class="hiddenDiv"> <div class="row"> <div class="col-sm-12"> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_2");'>2</a></li> <li><a href="#" onclick='return showDiv("page_3");'>3</a></li> <li class="active"><span>4</span></li> <li><a href="#" onclick='return showDiv("page_5");'>5</a></li> <li><a href="#" onclick='return showDiv("page_6");'>6</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div> </div> <div class="row"> <div class="col-sm-12"> <ol class="result-class" start="61"> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/28436177','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/28436177"><span>Limited evidence of abnormal intra-colonic <span class="hlt">pressure</span> <span class="hlt">profiles</span> in diverticular disease - a systematic review.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Jaung, R; Robertson, J; O'Grady, G; Milne, T; Rowbotham, D; Bissett, I P</p> <p>2017-06-01</p> <p>Abnormal colonic <span class="hlt">pressure</span> <span class="hlt">profiles</span> and high intraluminal <span class="hlt">pressures</span> are postulated to contribute to the formation of sigmoid colon diverticulosis and the pathophysiology of diverticular disease. This study aimed to review evidence for abnormal colonic <span class="hlt">pressure</span> <span class="hlt">profiles</span> in diverticulosis. All published studies investigating colonic <span class="hlt">pressure</span> in patients with diverticulosis were searched in three databases (Medline, Embase, Scopus). No language restrictions were applied. Any manometry studies in which patients with diverticulosis were compared with controls were included. The Newcastle-Ottawa Quality Assessment Scale (NOS) for case-control studies was used as a measure of risk of bias. A cut-off of five or more points on the NOS (fair quality in terms of risk of bias) was chosen for inclusion in the meta-analysis. Ten studies (published 1962-2005) met the inclusion criteria. The studies followed a wide variety of protocols and all used low-resolution manometry (sensor spacing range 7.5-15 cm). Six studies compared intra-sigmoid <span class="hlt">pressure</span>, with five of six showing higher <span class="hlt">pressure</span> in diverticulosis vs controls, but only two reached statistical significance. A meta-analysis was not performed as only two studies were above the cut-off and these did not have comparable outcomes. This systematic review of manometry data shows that evidence for abnormal <span class="hlt">pressure</span> in the sigmoid colon in patients with diverticulosis is weak. Existing studies utilized inconsistent methodology, showed heterogeneous results and are of limited quality. Higher quality studies using modern manometric techniques and standardized reporting methods are needed to clarify the role of colonic <span class="hlt">pressure</span> in diverticulosis. Colorectal Disease © 2017 The Association of Coloproctology of Great Britain and Ireland.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://rosap.ntl.bts.gov/view/dot/5197','DOTNTL'); return false;" href="https://rosap.ntl.bts.gov/view/dot/5197"><span>Tire <span class="hlt">pressure</span> special study : vehicle <span class="hlt">observation</span> data</span></a></p> <p><a target="_blank" href="http://ntlsearch.bts.gov/tris/index.do">DOT National Transportation Integrated Search</a></p> <p></p> <p>2001-08-01</p> <p>Twenty seven percent of passenger cars with : regular passenger car tires have at least one : tire that is underinflated by 8 psi or more. : Tire <span class="hlt">Pressure</span> Special Study: Vehicle : <span class="hlt">Observation</span> Data is the third in a series of : research notes co...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/1996JGR...10112555K','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/1996JGR...10112555K"><span>Interpretation of nitric oxide <span class="hlt">profile</span> <span class="hlt">observed</span> in January 1992 over Kiruna</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Kondo, Y.; Kawa, S. R.; Lary, D.; Sugita, T.; Douglass, Anne R.; Lutman, E.; Koike, M.; Deshler, T.</p> <p>1996-05-01</p> <p>NO mixing ratios measured from Kiruna (68°N, 20°E), Sweden, on January 22, 1992, revealed values much smaller than those <span class="hlt">observed</span> at midlatitude near equinox and had a sharper vertical gradient around 25 km. Location of the measurements was close to the terminator and near the edge of the polar vortex, which is highly distorted from concentric flow by strong planetary wave activities. These conditions necessitate accurate calculation, properly taking into account the transport and photochemical processes, in order to quantitatively explain the <span class="hlt">observed</span> NO <span class="hlt">profile</span>. A three-dimensional chemistry and transport model (CTM) and a trajectory model (TM) were used to interpret the <span class="hlt">profile</span> <span class="hlt">observations</span> within their larger spatial, temporal, and chemical context. The NOy <span class="hlt">profile</span> calculated by the CTM is in good agreement with that <span class="hlt">observed</span> on January 31, 1992. In addition, model NOy <span class="hlt">profiles</span> show small variabilities depending on latitudes, and they change little between January 22 and 31. The TM uses the <span class="hlt">observed</span> NOy values. The NO values calculated by the CTM and TM agree with <span class="hlt">observations</span> up to 27 km. Between 20 and 27 km the NO values calculated by the trajectory model including only gas phase chemistry are much larger than those including heterogeneous chemistry, indicating that NO mixing ratios were reduced significantly by heterogeneous chemistry on sulfuric acid aerosols. Very little sunlight to generate NOx from HNO3 was available, also causing the very low NO values. The good agreement between the <span class="hlt">observed</span> and modeled NO <span class="hlt">profiles</span> indicates that models can reproduce the photochemical and transport processes in the region where NO values have a sharp horizontal gradient. Moreover, CTM and TM model results show that even when the NOy gradients are weak, the model NO depends upon accurate calculation of the transport and insolation for several days.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2010CosRe..48..211K','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2010CosRe..48..211K"><span>Radial <span class="hlt">profile</span> of <span class="hlt">pressure</span> in a storm ring current as a function of D st</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Kovtyukh, A. S.</p> <p>2010-06-01</p> <p>Using satellite data obtained near the equatorial plane during 12 magnetic storms with amplitudes from -61 down to -422 nT, the dependences of maximum in L-<span class="hlt">profile</span> of <span class="hlt">pressure</span> ( L m) of the ring current (RC) on the current value of D st are constructed, and their analytical approximations are derived. It is established that function L m( D st ) is steeper on the phase of recovery than during the storm’s main phase. The form of the outer edge of experimental radial <span class="hlt">profiles</span> of RC <span class="hlt">pressure</span> is studied, and it is demonstrated to correspond to exponential growth of the total energy of RC particles on a given L shell with decreasing L. It is shown that during the storms’ main phase the ratio of plasma and magnetic field <span class="hlt">pressures</span> at the RC maximum does not practically depend on the storm strength and L m value. This fact reflects resistance of the Earth’s magnetic field to RC expansion, and testifies that during storms the possibilities of injection to small L are limited for RC particles. During the storms’ recovery phase this ratio quickly increases with increasing L m, which reflects an increased fraction of plasma in the total <span class="hlt">pressure</span> balance. It is demonstrated that function L m( D st ) is derived for the main phase of storms from the equations of drift motion of RC ions in electrical and magnetic fields, reflecting the dipole character of magnetic field and scale invariance of the pattern of particle convection near the RC maximum. For the recovery phase it is obtained from the Dessler-Parker-Sckopke relationship. The obtained regularities allow one to judge about the radial <span class="hlt">profile</span> of RC <span class="hlt">pressure</span> from ground-based magnetic measurements (data on the D st variation).</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=4433261','PMC'); return false;" href="https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=4433261"><span>Biochemical Association of Metabolic <span class="hlt">Profile</span> and Microbiome in Chronic <span class="hlt">Pressure</span> Ulcer Wounds</span></a></p> <p><a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pmc">PubMed Central</a></p> <p>Ammons, Mary Cloud B.; Morrissey, Kathryn; Tripet, Brian P.; Van Leuven, James T.; Han, Anne; Lazarus, Gerald S.; Zenilman, Jonathan M.; Stewart, Philip S.; James, Garth A.; Copié, Valérie</p> <p>2015-01-01</p> <p>Chronic, non-healing wounds contribute significantly to the suffering of patients with co-morbidities in the clinical population with mild to severely compromised immune systems. Normal wound healing proceeds through a well-described process. However, in chronic wounds this process seems to become dysregulated at the transition between resolution of inflammation and re-epithelialization. Bioburden in the form of colonizing bacteria is a major contributor to the delayed headlining in chronic wounds such as <span class="hlt">pressure</span> ulcers. However how the microbiome influences the wound metabolic landscape is unknown. Here, we have used a Systems Biology approach to determine the biochemical associations between the taxonomic and metabolomic <span class="hlt">profiles</span> of wounds colonized by bacteria. <span class="hlt">Pressure</span> ulcer biopsies were harvested from primary chronic wounds and bisected into top and bottom sections prior to analysis of microbiome by pyrosequencing and analysis of metabolome using 1H nuclear magnetic resonance (NMR) spectroscopy. Bacterial taxonomy revealed that wounds were colonized predominantly by three main phyla, but differed significantly at the genus level. While taxonomic <span class="hlt">profiles</span> demonstrated significant variability between wounds, metabolic <span class="hlt">profiles</span> shared significant similarity based on the depth of the wound biopsy. Biochemical association between taxonomy and metabolic landscape indicated significant wound-to-wound similarity in metabolite enrichment sets and metabolic pathway impacts, especially with regard to amino acid metabolism. To our knowledge, this is the first demonstration of a statistically robust correlation between bacterial colonization and metabolic landscape within the chronic wound environment. PMID:25978400</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/22356881','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/22356881"><span>The effects of stereotypes and <span class="hlt">observer</span> <span class="hlt">pressure</span> on athletic performance.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Krendl, Anne; Gainsburg, Izzy; Ambady, Nalini</p> <p>2012-02-01</p> <p>Although the effects of negative stereotypes and <span class="hlt">observer</span> <span class="hlt">pressure</span> on athletic performance have been well researched, the effects of positive stereotypes on performance, particularly in the presence of <span class="hlt">observers</span>, is not known. In the current study, White males watched a video either depicting Whites basketball players as the best free throwers in the NBA (positive stereotype), Black basketball players as the best free throwers in the NBA (negative stereotype), or a neutral sports video (control). Participants then shot a set of free throws, during which half the participants were also videotaped (<span class="hlt">observer</span> condition), whereas the other half were not (no <span class="hlt">observer</span> condition). Results demonstrated that positive stereotypes improved free throw performance, but only in the no <span class="hlt">observer</span> condition. Interestingly, <span class="hlt">observer</span> <span class="hlt">pressure</span> interacted with the positive stereotype to lead to performance decrements. In the negative stereotype condition, performance decrements were <span class="hlt">observed</span> both in the <span class="hlt">observer</span> and no <span class="hlt">observer</span> conditions.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.osti.gov/servlets/purl/984358','SCIGOV-STC'); return false;" href="https://www.osti.gov/servlets/purl/984358"><span>Calibration of the Total Carbon Column <span class="hlt">Observing</span> Network using Aircraft <span class="hlt">Profile</span> Data</span></a></p> <p><a target="_blank" href="http://www.osti.gov/search">DOE Office of Scientific and Technical Information (OSTI.GOV)</a></p> <p>Wunch, Debra; Toon, Geoffrey C.; Wennberg, Paul O.</p> <p>2010-03-26</p> <p>The Total Carbon Column <span class="hlt">Observing</span> Network (TCCON) produces precise measurements of the column average dry-air mole fractions of CO{sub 2}, CO, CH{sub 4}, N{sub 2}O and H{sub 2}O at a variety of sites worldwide. These <span class="hlt">observations</span> rely on spectroscopic parameters that are not known with sufficient accuracy to compute total columns that can be used in combination with in situ measure ments. The TCCON must therefore be calibrated to World Meteorological Organization (WMO) in situ trace gas measurement scales. We present a calibration of TCCON data using WMO-scale instrumentation aboard aircraft that measured <span class="hlt">profiles</span> over four TCCON stations during 2008more » and 2009. The aircraft campaigns are the Stratosphere-Troposphere Analyses of Regional Transport 2008 (START-08), which included a <span class="hlt">profile</span> over the Park Falls site, the HIAPER Pole-to-Pole <span class="hlt">Observations</span> (HIPPO-1) campaign, which included <span class="hlt">profiles</span> over the Lamont and Lauder sites, a series of Learjet <span class="hlt">profiles</span> over the Lamont site, and a Beechcraft King Air <span class="hlt">profile</span> over the Tsukuba site. These calibrations are compared with similar <span class="hlt">observations</span> made during the INTEX-NA (2004), COBRA-ME (2004) and TWP-ICE (2006) campaigns. A single, global calibration factor for each gas accurately captures the TCCON total column data within error.« less</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2013APS..DFDH12004G','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2013APS..DFDH12004G"><span>Investigation of the Unsteady Total <span class="hlt">Pressure</span> <span class="hlt">Profile</span> Corresponding to Counter-Rotating Vortices in an Internal Flow Application</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Gordon, Kathryn; Morris, Scott; Jemcov, Aleksandar; Cameron, Joshua</p> <p>2013-11-01</p> <p>The interaction of components in a compressible, internal flow often results in unsteady interactions between the wakes and moving blades. A prime example in which this flow feature is of interest is the interaction between the downstream rotor blades in a transonic axial compressor with the wake vortices shed from the upstream inlet guide vane (IGV). Previous work shows that a double row of counter-rotating vortices convects downstream into the rotor passage as a result of the rotor blade bow shock impinging on the IGV. The rotor-relative time-mean total <span class="hlt">pressure</span> distribution has a region of high total <span class="hlt">pressure</span> corresponding to the pathline of the vortices. The present work focuses on the relationship between the magnitude of the time-mean rotor-relative total <span class="hlt">pressure</span> <span class="hlt">profile</span> and the axial spacing between the IGV and the rotor. A survey of different axial gap sizes is performed in a two-dimensional computational study to obtain the sensitivity of the <span class="hlt">pressure</span> <span class="hlt">profile</span> amplitude to IGV-rotor axial spacing.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/20140000733','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/20140000733"><span>Background <span class="hlt">Pressure</span> <span class="hlt">Profiles</span> for Sonic Boom Vehicle Testing in the NASA Glenn 8- by 6-Foot Supersonic Wind Tunnel</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Castner, Raymond; Shaw, Stephen; Adamson, Eric; Simerly, Stephanie</p> <p>2013-01-01</p> <p>In an effort to identify test facilities that offer sonic boom measurement capabilities, an exploratory test program was initiated using wind tunnels at NASA research centers. The subject of this report is the sonic boom <span class="hlt">pressure</span> rail data collected in the Glenn Research Center 8- by 6-Foot Supersonic Wind Tunnel. The purpose is to summarize the lessons learned based on the test activity, specifically relating to collecting sonic boom data which has a large amount of spatial <span class="hlt">pressure</span> variation. The wind tunnel background <span class="hlt">pressure</span> <span class="hlt">profiles</span> are presented as well as data which demonstrated how both wind tunnel Mach number and model support-strut position affected the wind tunnel background <span class="hlt">pressure</span> <span class="hlt">profile</span>. Techniques were developed to mitigate these effects and are presented.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2018A%26A...612A..39R','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2018A%26A...612A..39R"><span>A multi-instrument non-parametric reconstruction of the electron <span class="hlt">pressure</span> <span class="hlt">profile</span> in the galaxy cluster CLJ1226.9+3332</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Romero, C.; McWilliam, M.; Macías-Pérez, J.-F.; Adam, R.; Ade, P.; André, P.; Aussel, H.; Beelen, A.; Benoît, A.; Bideaud, A.; Billot, N.; Bourrion, O.; Calvo, M.; Catalano, A.; Coiffard, G.; Comis, B.; de Petris, M.; Désert, F.-X.; Doyle, S.; Goupy, J.; Kramer, C.; Lagache, G.; Leclercq, S.; Lestrade, J.-F.; Mauskopf, P.; Mayet, F.; Monfardini, A.; Pascale, E.; Perotto, L.; Pisano, G.; Ponthieu, N.; Revéret, V.; Ritacco, A.; Roussel, H.; Ruppin, F.; Schuster, K.; Sievers, A.; Triqueneaux, S.; Tucker, C.; Zylka, R.</p> <p>2018-04-01</p> <p>Context. In the past decade, sensitive, resolved Sunyaev-Zel'dovich (SZ) studies of galaxy clusters have become common. Whereas many previous SZ studies have parameterized the <span class="hlt">pressure</span> <span class="hlt">profiles</span> of galaxy clusters, non-parametric reconstructions will provide insights into the thermodynamic state of the intracluster medium. Aim. We seek to recover the non-parametric <span class="hlt">pressure</span> <span class="hlt">profiles</span> of the high redshift (z = 0.89) galaxy cluster CLJ 1226.9+3332 as inferred from SZ data from the MUSTANG, NIKA, Bolocam, and Planck instruments, which all probe different angular scales. Methods: Our non-parametric algorithm makes use of logarithmic interpolation, which under the assumption of ellipsoidal symmetry is analytically integrable. For MUSTANG, NIKA, and Bolocam we derive a non-parametric <span class="hlt">pressure</span> <span class="hlt">profile</span> independently and find good agreement among the instruments. In particular, we find that the non-parametric <span class="hlt">profiles</span> are consistent with a fitted generalized Navaro-Frenk-White (gNFW) <span class="hlt">profile</span>. Given the ability of Planck to constrain the total signal, we include a prior on the integrated Compton Y parameter as determined by Planck. Results: For a given instrument, constraints on the <span class="hlt">pressure</span> <span class="hlt">profile</span> diminish rapidly beyond the field of view. The overlap in spatial scales probed by these four datasets is therefore critical in checking for consistency between instruments. By using multiple instruments, our analysis of CLJ 1226.9+3332 covers a large radial range, from the central regions to the cluster outskirts: 0.05 R500 < r < 1.1 R500. This is a wider range of spatial scales than is typically recovered by SZ instruments. Similar analyses will be possible with the new generation of SZ instruments such as NIKA2 and MUSTANG2.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2014JCAP...08..049N','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2014JCAP...08..049N"><span>How does <span class="hlt">pressure</span> gravitate? Cosmological constant problem confronts <span class="hlt">observational</span> cosmology</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Narimani, Ali; Afshordi, Niayesh; Scott, Douglas</p> <p>2014-08-01</p> <p>An important and long-standing puzzle in the history of modern physics is the gross inconsistency between theoretical expectations and cosmological <span class="hlt">observations</span> of the vacuum energy density, by at least 60 orders of magnitude, otherwise known as the cosmological constant problem. A characteristic feature of vacuum energy is that it has a <span class="hlt">pressure</span> with the same amplitude, but opposite sign to its energy density, while all the precision tests of General Relativity are either in vacuum, or for media with negligible <span class="hlt">pressure</span>. Therefore, one may wonder whether an anomalous coupling to <span class="hlt">pressure</span> might be responsible for decoupling vacuum from gravity. We test this possibility in the context of the Gravitational Aether proposal, using current cosmological <span class="hlt">observations</span>, which probe the gravity of relativistic <span class="hlt">pressure</span> in the radiation era. Interestingly, we find that the best fit for anomalous <span class="hlt">pressure</span> coupling is about half-way between General Relativity (GR), and Gravitational Aether (GA), if we include Planck together with WMAP and BICEP2 polarization cosmic microwave background (CMB) <span class="hlt">observations</span>. Taken at face value, this data combination excludes both GR and GA at around the 3 σ level. However, including higher resolution CMB <span class="hlt">observations</span> (``highL'') or baryonic acoustic oscillations (BAO) pushes the best fit closer to GR, excluding the Gravitational Aether solution to the cosmological constant problem at the 4- 5 σ level. This constraint effectively places a limit on the anomalous coupling to <span class="hlt">pressure</span> in the parametrized post-Newtonian (PPN) expansion, ζ4 = 0.105 ± 0.049 (+highL CMB), or ζ4 = 0.066 ± 0.039 (+BAO). These represent the most precise measurement of this parameter to date, indicating a mild tension with GR (for ΛCDM including tensors, with 0ζ4=), and also among different data sets.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017EGUGA..1916328K','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017EGUGA..1916328K"><span>A new retrieval algorithm for tropospheric temperature, humidity and <span class="hlt">pressure</span> <span class="hlt">profiling</span> based on GNSS radio occultation data</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Kirchengast, Gottfried; Li, Ying; Scherllin-Pirscher, Barbara; Schwärz, Marc; Schwarz, Jakob; Nielsen, Johannes K.</p> <p>2017-04-01</p> <p>The GNSS radio occultation (RO) technique is an important remote sensing technique for obtaining thermodynamic <span class="hlt">profiles</span> of temperature, humidity, and <span class="hlt">pressure</span> in the Earth's troposphere. However, due to refraction effects of both dry ambient air and water vapor in the troposphere, retrieval of accurate thermodynamic <span class="hlt">profiles</span> at these lower altitudes is challenging and requires suitable background information in addition to the RO refractivity information. Here we introduce a new moist air retrieval algorithm aiming to improve the quality and robustness of retrieving temperature, humidity and <span class="hlt">pressure</span> <span class="hlt">profiles</span> in moist air tropospheric conditions. The new algorithm consists of four steps: (1) use of prescribed specific humidity and its uncertainty to retrieve temperature and its associated uncertainty; (2) use of prescribed temperature and its uncertainty to retrieve specific humidity and its associated uncertainty; (3) use of the previous results to estimate final temperature and specific humidity <span class="hlt">profiles</span> through optimal estimation; (4) determination of air <span class="hlt">pressure</span> and density <span class="hlt">profiles</span> from the results obtained before. The new algorithm does not require elaborated matrix inversions which are otherwise widely used in 1D-Var retrieval algorithms, and it allows a transparent uncertainty propagation, whereby the uncertainties of prescribed variables are dynamically estimated accounting for their spatial and temporal variations. Estimated random uncertainties are calculated by constructing error covariance matrices from co-located ECMWF short-range forecast and corresponding analysis <span class="hlt">profiles</span>. Systematic uncertainties are estimated by empirical modeling. The influence of regarding or disregarding vertical error correlations is quantified. The new scheme is implemented with static input uncertainty <span class="hlt">profiles</span> in WEGC's current OPSv5.6 processing system and with full scope in WEGC's next-generation system, the Reference Occultation Processing System (rOPS). Results from</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://pubs.er.usgs.gov/publication/70155511','USGSPUBS'); return false;" href="https://pubs.er.usgs.gov/publication/70155511"><span>Pore-<span class="hlt">pressure</span> sensitivities to dynamic strains: <span class="hlt">observations</span> in active tectonic regions</span></a></p> <p><a target="_blank" href="http://pubs.er.usgs.gov/pubs/index.jsp?view=adv">USGS Publications Warehouse</a></p> <p>Barbour, Andrew J.</p> <p>2015-01-01</p> <p>Triggered seismicity arising from dynamic stresses is often explained by the Mohr-Coulomb failure criterion, where elevated pore <span class="hlt">pressures</span> reduce the effective strength of faults in fluid-saturated rock. The seismic response of a fluid-rock system naturally depends on its hydro-mechanical properties, but accurately assessing how pore-fluid <span class="hlt">pressure</span> responds to applied stress over large scales in situ remains a challenging task; hence, spatial variations in response are not well understood, especially around active faults. Here I analyze previously unutilized records of dynamic strain and pore-<span class="hlt">pressure</span> from regional and teleseismic earthquakes at Plate Boundary Observatory (PBO) stations from 2006 through 2012 to investigate variations in response along the Pacific/North American tectonic plate boundary. I find robust scaling-response coefficients between excess pore <span class="hlt">pressure</span> and dynamic strain at each station that are spatially correlated: around the San Andreas and San Jacinto fault systems, the response is lowest in regions of the crust undergoing the highest rates of secular shear strain. PBO stations in the Parkfield instrument cluster are at comparable distances to the San Andreas fault (SAF), and spatial variations there follow patterns in dextral creep rates along the fault, with the highest response in the actively creeping section, which is consistent with a narrowing zone of strain accumulation seen in geodetic velocity <span class="hlt">profiles</span>. At stations in the San Juan Bautista (SJB) and Anza instrument clusters, the response depends non-linearly on the inverse fault-perpendicular distance, with the response decreasing towards the fault; the SJB cluster is at the northern transition from creeping-to-locked behavior along the SAF, where creep rates are at moderate to low levels, and the Anza cluster is around the San Jacinto fault, where to date there have been no statistically significant creep rates <span class="hlt">observed</span> at the surface. These results suggest that the strength</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2016A%26A...585L...6P','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2016A%26A...585L...6P"><span>Damping <span class="hlt">profile</span> of standing kink oscillations <span class="hlt">observed</span> by SDO/AIA</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Pascoe, D. J.; Goddard, C. R.; Nisticò, G.; Anfinogentov, S.; Nakariakov, V. M.</p> <p>2016-01-01</p> <p>Aims: Strongly damped standing and propagating kink oscillations are <span class="hlt">observed</span> in the solar corona. This can be understood in terms of mode coupling, which causes the wave energy to be converted from the bulk transverse oscillation to localised, unresolved azimuthal motions. The damping rate can provide information about the loop structure, and theory predicts two possible damping <span class="hlt">profiles</span>. Methods: We used the recently compiled catalogue of decaying standing kink oscillations of coronal loops to search for examples with high spatial and temporal resolution and sufficient signal quality to allow the damping <span class="hlt">profile</span> to be examined. The location of the loop axis was tracked, detrended, and fitted with sinusoidal oscillations with Gaussian and exponential damping <span class="hlt">profiles</span>. Results: Using the highest quality data currently available, we find that for the majority of our cases a Gaussian <span class="hlt">profile</span> describes the damping behaviour at least as well as an exponential <span class="hlt">profile</span>, which is consistent with the recently developed theory for the damping <span class="hlt">profile</span> due to mode coupling.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/9763093','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/9763093"><span>Stimulated <span class="hlt">pressure</span> <span class="hlt">profile</span> at rest: a noninvasive method for assessing urethral sphincter function.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Meyer, S; Kuntzer, T; De Grandi, P; Bachelard, O; Schreyer, A</p> <p>1998-10-01</p> <p>To validate a method for assessing urethral sphincter muscle function by recording rises in intraurethral <span class="hlt">pressure</span> during repetitive pudendal nerve stimulations. A supine urethral <span class="hlt">pressure</span> <span class="hlt">profile</span> at rest was performed on 12 stress-continent and 28 stress-incontinent patients during repetitive pudendal nerve stimulations applied near the ischial spine, and the intraurethral <span class="hlt">pressure</span> increases were calculated for each third of the urethral functional length. No significant difference in intraurethral <span class="hlt">pressure</span> increases was seen between continent and stress-incontinent women. On the various regression curves, the intraurethral <span class="hlt">pressure</span> increases showed a significant correlation with maximal urethral closure <span class="hlt">pressure</span> values at rest and at stress (r = 0.36 to 0.54) and with the patient's age (r = 0.46), but not with pudendal nerve conduction times to the urethral sphincter on either side (r = 0.14 and 0.19). This method (1) measures intraurethral <span class="hlt">pressure</span> increases that correlate well with the anatomic location of the urethral sphincter muscle, (2) shows there is no significant difference between them in continent and stress-incontinent patients, except in patients with a low-<span class="hlt">pressure</span> urethra, and (3) demonstrates that they correlate well with the maximal urethral closure <span class="hlt">pressure</span> and the patient's age, but not with pudendal motor latencies to the urethral sphincter. This method gives us a mapping of the urethral sphincter activity, explaining why some patients with a low-<span class="hlt">pressure</span> urethra have less urinary loss than others with the same urethral closure <span class="hlt">pressure</span>.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.osti.gov/biblio/22661004-observations-simulations-nai-sub-line-profiles-class-solar-flare','SCIGOV-STC'); return false;" href="https://www.osti.gov/biblio/22661004-observations-simulations-nai-sub-line-profiles-class-solar-flare"><span><span class="hlt">OBSERVATIONS</span> AND SIMULATIONS OF THE Na i D{sub 1} LINE <span class="hlt">PROFILES</span> IN AN M-CLASS SOLAR FLARE</span></a></p> <p><a target="_blank" href="http://www.osti.gov/search">DOE Office of Scientific and Technical Information (OSTI.GOV)</a></p> <p>Kuridze, D.; Mathioudakis, M.; Jess, D. B.</p> <p>2016-12-01</p> <p>We study the temporal evolution of the Na i D{sub 1} line <span class="hlt">profiles</span> in the M3.9 flare SOL2014-06-11T21:03 UT, using <span class="hlt">observations</span> at high spectral resolution obtained with the Interferometric Bidimensional Spectrometer instrument on the Dunn Solar Telescope combined with radiative hydrodynamic simulations. Our results show a significant increase in the intensities of the line core and wings during the flare. The analysis of the line <span class="hlt">profiles</span> from the flare ribbons reveals that the Na i D{sub 1} line has a central reversal with excess emission in the blue wing (blue asymmetry). We combine RADYN and RH simulations to synthesize Na imore » D{sub 1} line <span class="hlt">profiles</span> of the flaring atmosphere and find good agreement with the <span class="hlt">observations</span>. Heating with a beam of electrons modifies the radiation field in the flaring atmosphere and excites electrons from the ground state 3s {sup 2}S to the first excited state 3p {sup 2}P, which in turn modifies the relative population of the two states. The change in temperature and the population density of the energy states make the sodium line <span class="hlt">profile</span> revert from absorption into emission. Furthermore, the rapid changes in temperature break the <span class="hlt">pressure</span> balance between the different layers of the lower atmosphere, generating upflow/downflow patterns. Analysis of the simulated spectra reveals that the asymmetries of the Na i D{sub 1} flare <span class="hlt">profile</span> are produced by the velocity gradients in the lower solar atmosphere.« less</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/25255389','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/25255389"><span>Movement of the lacrimal canalicular wall under intracanalicular <span class="hlt">pressure</span> changes <span class="hlt">observed</span> with dacryoendoscopy.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Kakizaki, Hirohiko; Takahashi, Yasuhiro; Mito, Hidenori; Nakamura, Yasuhisa</p> <p>2015-01-01</p> <p>Movement of the lacrimal canalicular wall has been speculated to occur during blinking. Movement of the common internal ostium has been <span class="hlt">observed</span> under nasal endoscopy, and <span class="hlt">pressure</span> changes in the lacrimal canalicular cavity have been <span class="hlt">observed</span> with a <span class="hlt">pressure</span> sensor; however, lacrimal canalicular wall movement under <span class="hlt">pressure</span> changes has not been <span class="hlt">observed</span>. To examine movement of the lacrimal canalicular wall under intracanalicular <span class="hlt">pressure</span> changes using dacryoendoscopy. The authors examined 20 obstruction-free lacrimal canaliculi in 10 patients. A dacryoendoscope was inserted, and water was poured into the intracanalicular cavity via the dacryoendoscope's water channel. The water was then poured or suctioned to cause positive or negative <span class="hlt">pressure</span> changes in the intracanalicular cavity, and movement of the lacrimal canalicular wall was examined. The lacrimal canalicular wall moved flexibly with <span class="hlt">pressure</span> changes. Under positive <span class="hlt">pressure</span>, the intracanalicular cavity was dilated; however, it narrowed under negative <span class="hlt">pressure</span>. The extent of movement was more dramatic in the common canalicular portion than the proximal canalicular portion. Intracanalicular <span class="hlt">pressure</span> changes cause movement of the lacrimal canalicular wall. There was a consistent relationship between intracanalicular cavity changes and <span class="hlt">pressure</span> changes, possibly contributing to lacrimal drainage of the canaliculus.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/20000091542','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/20000091542"><span>An Analysis of Water Line <span class="hlt">Profiles</span> in Star Formation Regions <span class="hlt">Observed</span> by SWAS</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Ashby, Matthew L. N.; Bergin, Edwin A.; Plume, Rene; Carpenter, John M.; Neufeld, David A.; Chin, Gordon; Erickson, Neal R.; Goldsmith, Paul F.; Harwit, Martin; Howe, J. E.</p> <p>2000-01-01</p> <p>We present spectral line <span class="hlt">profiles</span> for the 557 GHz 1(sub 1,0) yields 1(sub 0,1) ground-state rotational transition of ortho-H2(16)O for 18 galactic star formation regions <span class="hlt">observed</span> by SWAS. 2 Water is unambiguously detected in every source. The line <span class="hlt">profiles</span> exhibit a wide variety of shapes, including single-peaked spectra and self-reversed <span class="hlt">profiles</span>. We interpret these <span class="hlt">profiles</span> using a Monte Carlo code to model the radiative transport. The <span class="hlt">observed</span> variations in the line <span class="hlt">profiles</span> can be explained by variations in the relative strengths of the bulk flow and small-scale turbulent motions within the clouds. Bulk flow (infall, outflow) must be present in some cloud cores, and in certain cases this bulk flow dominates the turbulent motions.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/19800024549','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/19800024549"><span>Weather and climate needs for Lidar <span class="hlt">observations</span> from space and concepts for their realization. [wind, temperature, moisture, and <span class="hlt">pressure</span> data needs</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Atlas, D.; Korb, C. L.</p> <p>1980-01-01</p> <p>The spectrum of weather and climate needs for Lidar <span class="hlt">observations</span> from space is discussed with emphasis on the requirements for wind, temperature, moisture, and <span class="hlt">pressure</span> data. It is shown that winds are required to realistically depict all atmospheric scales in the tropics and the smaller scales at higher latitudes, where both temperature and wind <span class="hlt">profiles</span> are necessary. The need for means to estimate air-sea exchanges of sensible and latent heat also is noted. A concept for achieving this through a combination of Lidar cloud top heights and IR cloud top temperatures of cloud streets formed during cold air outbreaks over the warmer ocean is outlined. Recent theoretical feasibility studies concerning the <span class="hlt">profiling</span> of temperatures, <span class="hlt">pressure</span>, and humidity by differential absorption Lidar (DIAL) from space and expected accuracies are reviewed. An alternative approach to Doppler Lidar wind measurements also is presented. The concept involves the measurement of the displacement of the aerosol backscatter pattern, at constant heights, between two successive scans of the same area, one ahead of the spacecraft and the other behind it a few minutes later. Finally, an integrated space Lidar system capable of measuring temperature, <span class="hlt">pressure</span>, humidity, and winds which combines the DIAL methods with the aerosol pattern displacement concept is described.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2001ShWav..11...77H','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2001ShWav..11...77H"><span><span class="hlt">Pressure</span> <span class="hlt">profiles</span> in detonation cells with rectangular and diagonal structures</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Hanana, M.; Lefebvre, M. H.</p> <p></p> <p>Experimental results presented in this work enable us to classify the three-dimensional structure of the detonation into two fundamental types: a rectangular structure and a diagonal structure. The rectangular structure is well documented in the literature and consists of orthogonal waves travelling independently from each another. The soot record in this case shows the classical diamond detonation cell exhibiting `slapping waves'. The experiments indicate that the diagonal structure is a structure with the triple point intersections moving along the diagonal line of the tube cross section. The axes of the transverse waves are canted at 45 degrees to the wall, accounting for the lack of slapping waves. It is possible to reproduce these diagonal structures by appropriately controlling the experimental ignition procedure. The characteristics of the diagonal structure show some similarities with detonation structure in round tube. <span class="hlt">Pressure</span> measurements recorded along the central axis of the cellular structure show a series of <span class="hlt">pressure</span> peaks, depending on the type of structure and the position inside the detonation cell. <span class="hlt">Pressure</span> <span class="hlt">profiles</span> measured for the whole length of the two types of detonation cells show that the intensity of the shock front is higher and the length of the detonation cell is shorter for the diagonal structures.</p> </li> </ol> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_2");'>2</a></li> <li><a href="#" onclick='return showDiv("page_3");'>3</a></li> <li class="active"><span>4</span></li> <li><a href="#" onclick='return showDiv("page_5");'>5</a></li> <li><a href="#" onclick='return showDiv("page_6");'>6</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div><!-- col-sm-12 --> </div><!-- row --> </div><!-- page_4 --> <div id="page_5" class="hiddenDiv"> <div class="row"> <div class="col-sm-12"> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_3");'>3</a></li> <li><a href="#" onclick='return showDiv("page_4");'>4</a></li> <li class="active"><span>5</span></li> <li><a href="#" onclick='return showDiv("page_6");'>6</a></li> <li><a href="#" onclick='return showDiv("page_7");'>7</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div> </div> <div class="row"> <div class="col-sm-12"> <ol class="result-class" start="81"> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.osti.gov/biblio/22475489-real-time-measurements-temperature-pressure-moisture-profiles-high-performance-concrete-exposed-high-temperatures-during-neutron-radiography-imaging','SCIGOV-STC'); return false;" href="https://www.osti.gov/biblio/22475489-real-time-measurements-temperature-pressure-moisture-profiles-high-performance-concrete-exposed-high-temperatures-during-neutron-radiography-imaging"><span>Real-time measurements of temperature, <span class="hlt">pressure</span> and moisture <span class="hlt">profiles</span> in High-Performance Concrete exposed to high temperatures during neutron radiography imaging</span></a></p> <p><a target="_blank" href="http://www.osti.gov/search">DOE Office of Scientific and Technical Information (OSTI.GOV)</a></p> <p>Toropovs, N., E-mail: nikolajs.toropovs@rtu.lv; Riga Technical University, Institute of Materials and Structures, Riga; Lo Monte, F.</p> <p>2015-02-15</p> <p>High-Performance Concrete (HPC) is particularly prone to explosive spalling when exposed to high temperature. Although the exact causes that lead to spalling are still being debated, moisture transport during heating plays an important role in all proposed mechanisms. In this study, slabs made of high-performance, low water-to-binder ratio mortars with addition of superabsorbent polymers (SAP) and polypropylene fibers (PP) were heated from one side on a temperature-controlled plate up to 550 °C. A combination of measurements was performed simultaneously on the same sample: moisture <span class="hlt">profiles</span> via neutron radiography, temperature <span class="hlt">profiles</span> with embedded thermocouples and pore <span class="hlt">pressure</span> evolution with embedded pressuremore » sensors. Spalling occurred in the sample with SAP, where sharp <span class="hlt">profiles</span> of moisture and temperature were <span class="hlt">observed</span>. No spalling occurred when PP-fibers were introduced in addition to SAP. The experimental procedure described here is essential for developing and verifying numerical models and studying measures against fire spalling risk in HPC.« less</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017IJBm...61..181H','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017IJBm...61..181H"><span>The major influence of the atmosphere on intracranial <span class="hlt">pressure</span>: an <span class="hlt">observational</span> study</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Herbowski, Leszek</p> <p>2017-01-01</p> <p>The impact of the atmosphere on human physiology has been studied widely within the last years. In practice, intracranial <span class="hlt">pressure</span> is a <span class="hlt">pressure</span> difference between intracranial compartments and the surrounding atmosphere. This means that gauge intracranial <span class="hlt">pressure</span> uses atmospheric <span class="hlt">pressure</span> as its zero point, and therefore, this method of <span class="hlt">pressure</span> measurement excludes the effects of barometric <span class="hlt">pressure</span>'s fluctuation. The comparison of these two physical quantities can only take place through their absolute value relationship. The aim of this study is to investigate the direct effect of barometric <span class="hlt">pressure</span> on the absolute intracranial <span class="hlt">pressure</span> homeostasis. A prospective <span class="hlt">observational</span> cross-sectional open study was conducted in Szczecin, Poland. In 28 neurosurgical patients with suspected normal-<span class="hlt">pressure</span> hydrocephalus, intracranial intraventricular <span class="hlt">pressure</span> was monitored in a sitting position. A total of 168 intracranial <span class="hlt">pressure</span> and atmospheric <span class="hlt">pressure</span> measurements were performed. Absolute atmospheric <span class="hlt">pressure</span> was recorded directly. All values of intracranial gauge <span class="hlt">pressure</span> were converted to absolute <span class="hlt">pressure</span> (the sum of gauge intracranial <span class="hlt">pressure</span> and local absolute atmospheric <span class="hlt">pressure</span>). The average absolute mean intracranial <span class="hlt">pressure</span> in the patients is 1006.6 hPa (95 % CI 1004.5 to 1008.8 hPa, SEM 1.1), and the mean absolute atmospheric <span class="hlt">pressure</span> is 1007.9 hPa (95 % CI 1006.3 to 1009.6 hPa, SEM 0.8). The <span class="hlt">observed</span> association between atmospheric and intracranial <span class="hlt">pressure</span> is strongly significant (Spearman correlation r = 0.87, p < 0.05) and all the measurements are perfectly reliable (Bland-Altman coefficient is 4.8 %). It appears from this study that changes in absolute intracranial <span class="hlt">pressure</span> are related to seasonal variation. Absolute intracranial <span class="hlt">pressure</span> is shown to be impacted positively by atmospheric <span class="hlt">pressure</span>.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2016AGUOSOD21A..03E','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2016AGUOSOD21A..03E"><span>Spatiotemporal Variability in Particulate Organic Carbon Export <span class="hlt">Observed</span> Using Bio-Optical <span class="hlt">Profiling</span> Floats</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Estapa, M. L.</p> <p>2016-02-01</p> <p>Autonomous, bio-optical <span class="hlt">profiling</span> floats are poised to broaden the number and spatiotemporal resolution of <span class="hlt">observations</span> of the ocean's biological pump. Here, we used multiple optical sensors aboard two bio-optical <span class="hlt">profiling</span> floats (Navis BGCi, Sea-Bird) deployed in the Sargasso Sea to derive in situ proxies for particulate carbon (PC) flux, sub-mixed layer net community production (NCP) and to drive a model of net primary production (NPP). <span class="hlt">Profiles</span> were collected at approximately 2-day resolution, and drift-phase PC flux <span class="hlt">observations</span> were collected at subdaily resolution at a rotating cycle of <span class="hlt">observation</span> depths between 150 and 1000 m. The magnitudes of NPP, PC flux, and their annually-averaged ratio were generally consistent with <span class="hlt">observations</span> at the nearby Bermuda Atlantic Timeseries Study (BATS) site. PC flux and the export ratio were enhanced in the autumn as well as in the spring, and varied over short timescales possibly due to the influence of mesoscale eddies. The relatively shallow park depths and short <span class="hlt">profile</span> cycle lengths allow us to identify ephemeral, subsurface bio-optical features and compare them to measured fluxes and satellite-<span class="hlt">observed</span> surface properties.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2014EGUGA..1615548T','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2014EGUGA..1615548T"><span><span class="hlt">Pressure</span> Variations in Metamorphic Rocks: Implications for the Interpretation of Petrographic <span class="hlt">Observations</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Tajčmanová, Lucie</p> <p>2014-05-01</p> <p>Metamorphic petrologists and structural geologists, using direct measurements, bring the only direct <span class="hlt">observational</span> constrains for validating geodynamic models. Therefore, petrological and structural geological <span class="hlt">observations</span> are essential for the quality and reproducibility of geodynamic reconstructions and models. One of the important assumptions for geodynamic reconstructions arises from the <span class="hlt">pressure</span> and temperature estimates in the petrology analysis. <span class="hlt">Pressure</span> is commonly converted to depth through the equation for lithostatic <span class="hlt">pressure</span> and so the original position of the rock sample within the Earth's interior can be constrained. The current assumption that the studied sample corresponds to uniform <span class="hlt">pressure</span> may not be correct, and if so, it has serious implications. Increasing evidence from analytical data shows that <span class="hlt">pressure</span> is not constant even on a grain scale, posing new challenges because, if ignored, it leads to an incorrect use of petrology data in constraining geodynamic models. Well known examples of the preservation of coesite and diamond in a host mineral like garnet show that high <span class="hlt">pressure</span> inclusions are preserved during decompression. Tajčmanová et al. (2014) has shown that grain-scale <span class="hlt">pressure</span> variations can develop and that these <span class="hlt">pressure</span> variations allow compositional zoning in minerals preserved over geological time scales. A new unconventional barometric method based on equilibrium under <span class="hlt">pressure</span> variations has been developed . Such <span class="hlt">pressure</span> variations are also connected with differences in fluid <span class="hlt">pressure</span> in open systems and can be thus <span class="hlt">observed</span> at all scales. Tajčmanová L., Podladchikov Y., Powell R., Moulas E., Vrijmoed J. and Connolly J. (2014). Grain scale <span class="hlt">pressure</span> variations and chemical equilibrium in high-grade metamorphic rocks.Journal of Metamorphic Geology, doi:10.1111/jmg.12066 This work was supported by ERC starting grant 335577 to Lucie Tajcmanova</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017xru..conf..335T','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017xru..conf..335T"><span>Radial <span class="hlt">Profiles</span> of PKS 0745-191 Galaxy Cluster with XMM-Newton X-Ray <span class="hlt">Observations</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Tumer, A.; Ezer, C.; Ercan, E.</p> <p>2017-10-01</p> <p>Since clusters of galaxies are the largest comprehensive samples of the universe, they provide essential information on from the most basic to the most complex physical mechanisms such as nucleosynthesis and supernovae events. Some of these information are provided by the X-ray emission data from Intra Cluster Medium (ICM) which contains hot dilute gas. Recent archieved <span class="hlt">observation</span> of the X-Ray spectrum of the cool core galaxy cluster PKS 0745-191 provided by XMM-Newton is subjected to data analysis using ESAS package. Followed by spectra analysis utilizing Xspec spectral fitting software, we present the radial <span class="hlt">profiles</span> of temperature and abundance from the core to 0.5R_500 of brightest distant cluster (z ˜ 0.102) PKS 0745-191. Using the deprojected spectra, the radial distribution of <span class="hlt">pressure</span> and entropy in the aforementioned region are also presented.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/19960012278','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/19960012278"><span>Differential absorption lidars for remote sensing of atmospheric <span class="hlt">pressure</span> and temperature <span class="hlt">profiles</span></span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Korb, C. Laurence; Schwemmer, Geary K.; Famiglietti, Joseph; Walden, Harvey; Prasad, Coorg</p> <p>1995-01-01</p> <p>A near infrared differential absorption lidar technique is developed using atmospheric oxygen as a tracer for high resolution vertical <span class="hlt">profiles</span> of <span class="hlt">pressure</span> and temperature with high accuracy. Solid-state tunable lasers and high-resolution spectrum analyzers are developed to carry out ground-based and airborne measurement demonstrations and results of the measurements presented. Numerical error analysis of high-altitude airborne and spaceborne experiments is carried out, and system concepts developed for their implementation.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2005AGUFM.P21B0151M','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2005AGUFM.P21B0151M"><span>Atmospheric soundings by SPICAM occultation <span class="hlt">observations</span>: aerosol and ozone vertical <span class="hlt">profiles</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Montmessin, F.</p> <p>2005-12-01</p> <p>The SPICAM instrument is a highly versatile, dual spectrometer probing both the UV and the NIR spectral region and is currently flying around Mars onboard Mars Express. Since the beginning of MEx operations, SPICAM has collected about thousand atmospheric <span class="hlt">profiles</span> while <span class="hlt">observing</span> in a solar or a stellar occultation mode. UV spectra bear the signatures of several species; i.e carbon dioxide, ozone and aerosols, while infrared spectra potentially bring information on atmospheric condensates and on water vapor. This presentation will focus on the measured aerosol, ozone and water vapor <span class="hlt">profiles</span>. For the aerosol, we will emphasize the numerous <span class="hlt">observations</span> made in the polar night and will also discuss some high altitude clouds discovered in the southern hemisphere. Ozone and water vapor <span class="hlt">profiles</span> will be presented along with some General Circulation Model comparisons. This work has been supported by CNES.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2006MNRAS.370..753B','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2006MNRAS.370..753B"><span>K-band <span class="hlt">observations</span> of boxy bulges - I. Morphology and surface brightness <span class="hlt">profiles</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Bureau, M.; Aronica, G.; Athanassoula, E.; Dettmar, R.-J.; Bosma, A.; Freeman, K. C.</p> <p>2006-08-01</p> <p>In this first paper of a series on the structure of boxy and peanut-shaped (B/PS) bulges, Kn-band <span class="hlt">observations</span> of a sample of 30 edge-on spiral galaxies are described and discussed. Kn-band <span class="hlt">observations</span> best trace the dominant luminous galactic mass and are minimally affected by dust. Images, unsharp-masked images, as well as major-axis and vertically summed surface brightness <span class="hlt">profiles</span> are presented and discussed. Galaxies with a B/PS bulge tend to have a more complex morphology than galaxies with other bulge types, more often showing centred or off-centred X structures, secondary maxima along the major-axis and spiral-like structures. While probably not uniquely related to bars, those features are <span class="hlt">observed</span> in three-dimensional N-body simulations of barred discs and may trace the main bar orbit families. The surface brightness <span class="hlt">profiles</span> of galaxies with a B/PS bulge are also more complex, typically containing three or more clearly separated regions, including a shallow or flat intermediate region (Freeman Type II <span class="hlt">profiles</span>). The breaks in the <span class="hlt">profiles</span> offer evidence for bar-driven transfer of angular momentum and radial redistribution of material. The <span class="hlt">profiles</span> further suggest a rapid variation of the scaleheight of the disc material, contrary to conventional wisdom but again as expected from the vertical resonances and instabilities present in barred discs. Interestingly, the steep inner region of the surface brightness <span class="hlt">profiles</span> is often shorter than the isophotally thick part of the galaxies, itself always shorter than the flat intermediate region of the <span class="hlt">profiles</span>. The steep inner region is also much more prominent along the major-axis than in the vertically summed <span class="hlt">profiles</span>. Similarly to other recent work but contrary to the standard `bulge + disc' model (where the bulge is both thick and steep), we thus propose that galaxies with a B/PS bulge are composed of a thin concentrated disc (a disc-like bulge) contained within a partially thick bar (the B/PS bulge), itself</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/27333899','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/27333899"><span>The major influence of the atmosphere on intracranial <span class="hlt">pressure</span>: an <span class="hlt">observational</span> study.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Herbowski, Leszek</p> <p>2017-01-01</p> <p>The impact of the atmosphere on human physiology has been studied widely within the last years. In practice, intracranial <span class="hlt">pressure</span> is a <span class="hlt">pressure</span> difference between intracranial compartments and the surrounding atmosphere. This means that gauge intracranial <span class="hlt">pressure</span> uses atmospheric <span class="hlt">pressure</span> as its zero point, and therefore, this method of <span class="hlt">pressure</span> measurement excludes the effects of barometric <span class="hlt">pressure</span>'s fluctuation. The comparison of these two physical quantities can only take place through their absolute value relationship. The aim of this study is to investigate the direct effect of barometric <span class="hlt">pressure</span> on the absolute intracranial <span class="hlt">pressure</span> homeostasis. A prospective <span class="hlt">observational</span> cross-sectional open study was conducted in Szczecin, Poland. In 28 neurosurgical patients with suspected normal-<span class="hlt">pressure</span> hydrocephalus, intracranial intraventricular <span class="hlt">pressure</span> was monitored in a sitting position. A total of 168 intracranial <span class="hlt">pressure</span> and atmospheric <span class="hlt">pressure</span> measurements were performed. Absolute atmospheric <span class="hlt">pressure</span> was recorded directly. All values of intracranial gauge <span class="hlt">pressure</span> were converted to absolute <span class="hlt">pressure</span> (the sum of gauge intracranial <span class="hlt">pressure</span> and local absolute atmospheric <span class="hlt">pressure</span>). The average absolute mean intracranial <span class="hlt">pressure</span> in the patients is 1006.6 hPa (95 % CI 1004.5 to 1008.8 hPa, SEM 1.1), and the mean absolute atmospheric <span class="hlt">pressure</span> is 1007.9 hPa (95 % CI 1006.3 to 1009.6 hPa, SEM 0.8). The <span class="hlt">observed</span> association between atmospheric and intracranial <span class="hlt">pressure</span> is strongly significant (Spearman correlation r = 0.87, p < 0.05) and all the measurements are perfectly reliable (Bland-Altman coefficient is 4.8 %). It appears from this study that changes in absolute intracranial <span class="hlt">pressure</span> are related to seasonal variation. Absolute intracranial <span class="hlt">pressure</span> is shown to be impacted positively by atmospheric <span class="hlt">pressure</span>.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2010HPR....30..118K','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2010HPR....30..118K"><span><span class="hlt">Observations</span> of a high-<span class="hlt">pressure</span> phase creation in oleic acid</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Kościesza, R.; Kulisiewicz, L.; Delgado, A.</p> <p>2010-03-01</p> <p>Oleic acid is one of the unsaturated fatty acids which frequently appears in food products such as edible fats and oils. A molecule of oleic acid possesses a double carbon bond, C=C, which is responsible for a transition to a new phase when <span class="hlt">pressure</span> is applied. This work presents the results of optical <span class="hlt">observations</span> of such a transition. The <span class="hlt">observations</span> were made in two cases, the first being static p-T conditions under 60 MPa at 20°C and the other the dynamic application of the <span class="hlt">pressure</span> up to 350 MPa. The obtained visualization reveals differences in the creation of the phase and in its further appearance. Some crystal forms may be recognized. These results tend to be of interest for food engineers due to increasing interest in high-<span class="hlt">pressure</span> food preservation among nutritionists and medical scientists concerned with fatty acids.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2016IAUS..320...89G','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2016IAUS..320...89G"><span>Model of flare lightcurve <span class="hlt">profile</span> <span class="hlt">observed</span> in soft X-rays</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Gryciuk, Magdalena; Siarkowski, Marek; Gburek, Szymon; Podgorski, Piotr; Sylwester, Janusz; Kepa, Anna; Mrozek, Tomasz</p> <p></p> <p>We propose a new model for description of solar flare lightcurve <span class="hlt">profile</span> <span class="hlt">observed</span> in soft X-rays. The method assumes that single-peaked `regular' flares seen in lightcurves can be fitted with the elementary time <span class="hlt">profile</span> being a convolution of Gaussian and exponential functions. More complex, multi-peaked flares can be decomposed as a sum of elementary <span class="hlt">profiles</span>. During flare lightcurve fitting process a linear background is determined as well. In our study we allow the background shape over the event to change linearly with time. Presented approach originally was dedicated to the soft X-ray small flares recorded by Polish spectrophotometer SphinX during the phase of very deep solar minimum of activity, between 23 rd and 24 th Solar Cycles. However, the method can and will be used to interpret the lightcurves as obtained by the other soft X-ray broad-band spectrometers at the time of both low and higher solar activity level. In the paper we introduce the model and present examples of fits to SphinX and GOES 1-8 Å channel <span class="hlt">observations</span> as well.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/17654092','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/17654092"><span>Effects of aromatherapy massage on blood <span class="hlt">pressure</span> and lipid <span class="hlt">profile</span> in korean climacteric women.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Hur, Myung-Haeng; Oh, Heeyoung; Lee, Myeong Soo; Kim, Chan; Choi, Ae-Na; Shin, Gil-Ran</p> <p>2007-09-01</p> <p>This study investigated the effects of aromatherapy massage on the lipid <span class="hlt">profile</span> and blood <span class="hlt">pressure</span> in Korean climacteric women. A wait-listed control group, pretest-posttest design was used. The subjects comprised 58 climacteric women: 30 in the experimental group and 28 in the control group. Aromatherapy massage using lavender, rose geranium, rose, and jasmine was given to the experimental group only. Each massage session lasted 30 minutes, and was performed once weekly for two 8-week periods with self abdominal daily massage at home. The intervention produced significant differences in the systolic blood <span class="hlt">pressure</span> compare to pretreatment and significant differences in systolic and diastolic blood <span class="hlt">pressures</span> at posttreatment between the two groups. These results suggest that aromatherapy massage may exert positive effects on blood <span class="hlt">pressure</span>. However, more objective, clinical measures should be applied in a future study with a randomized placebo-controlled design.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2015AMT.....8..369R','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2015AMT.....8..369R"><span>Adaptive neuro-fuzzy inference system for temperature and humidity <span class="hlt">profile</span> retrieval from microwave radiometer <span class="hlt">observations</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Ramesh, K.; Kesarkar, A. P.; Bhate, J.; Venkat Ratnam, M.; Jayaraman, A.</p> <p>2015-01-01</p> <p>The retrieval of accurate <span class="hlt">profiles</span> of temperature and water vapour is important for the study of atmospheric convection. Recent development in computational techniques motivated us to use adaptive techniques in the retrieval algorithms. In this work, we have used an adaptive neuro-fuzzy inference system (ANFIS) to retrieve <span class="hlt">profiles</span> of temperature and humidity up to 10 km over the tropical station Gadanki (13.5° N, 79.2° E), India. ANFIS is trained by using <span class="hlt">observations</span> of temperature and humidity measurements by co-located Meisei GPS radiosonde (henceforth referred to as radiosonde) and microwave brightness temperatures <span class="hlt">observed</span> by radiometrics multichannel microwave radiometer MP3000 (MWR). ANFIS is trained by considering these <span class="hlt">observations</span> during rainy and non-rainy days (ANFIS(RD + NRD)) and during non-rainy days only (ANFIS(NRD)). The comparison of ANFIS(RD + NRD) and ANFIS(NRD) <span class="hlt">profiles</span> with independent radiosonde <span class="hlt">observations</span> and <span class="hlt">profiles</span> retrieved using multivariate linear regression (MVLR: RD + NRD and NRD) and artificial neural network (ANN) indicated that the errors in the ANFIS(RD + NRD) are less compared to other retrieval methods. The Pearson product movement correlation coefficient (r) between retrieved and <span class="hlt">observed</span> <span class="hlt">profiles</span> is more than 92% for temperature <span class="hlt">profiles</span> for all techniques and more than 99% for the ANFIS(RD + NRD) technique Therefore this new techniques is relatively better for the retrieval of temperature <span class="hlt">profiles</span>. The comparison of bias, mean absolute error (MAE), RMSE and symmetric mean absolute percentage error (SMAPE) of retrieved temperature and relative humidity (RH) <span class="hlt">profiles</span> using ANN and ANFIS also indicated that <span class="hlt">profiles</span> retrieved using ANFIS(RD + NRD) are significantly better compared to the ANN technique. The analysis of <span class="hlt">profiles</span> concludes that retrieved <span class="hlt">profiles</span> using ANFIS techniques have improved the temperature retrievals substantially; however, the retrieval of RH by all techniques considered in this paper (ANN, MVLR and</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017PhRvE..95c2414M','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017PhRvE..95c2414M"><span>Earliest effects of sudden occlusions on <span class="hlt">pressure</span> <span class="hlt">profiles</span> in selected locations of the human systemic arterial system</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Majka, Marcin; Gadda, Giacomo; Taibi, Angelo; Gałązka, Mirosław; Zieliński, Piotr</p> <p>2017-03-01</p> <p>We have developed a numerical simulation method for predicting the time dependence (wave form) of <span class="hlt">pressure</span> at any location in the systemic arterial system in humans. The method uses the matlab-Simulink environment. The input data include explicitly the geometry of the arterial tree, treated up to an arbitrary bifurcation level, and the elastic properties of arteries as well as rheological parameters of blood. Thus, the impact of anatomic details of an individual subject can be studied. The method is applied here to reveal the earliest stages of mechanical reaction of the <span class="hlt">pressure</span> <span class="hlt">profiles</span> to sudden local blockages (thromboses or embolisms) of selected arteries. The results obtained with a purely passive model provide reference data indispensable for studies of longer-term effects due to neural and humoral mechanisms. The reliability of the results has been checked by comparison of two available sets of anatomic, elastic, and rheological data involving (i) 55 and (ii) 138 arterial segments. The remaining arteries have been replaced with the appropriate resistive elements. Both models are efficient in predicting an overall shift of <span class="hlt">pressure</span>, whereas the accuracy of the 55-segment model in reproducing the detailed wave forms and stabilization times turns out dependent on the location of the blockage and the <span class="hlt">observation</span> point.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2018AMT....11.2135A','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2018AMT....11.2135A"><span>Retrieval of ozone <span class="hlt">profiles</span> from OMPS limb scattering <span class="hlt">observations</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Arosio, Carlo; Rozanov, Alexei; Malinina, Elizaveta; Eichmann, Kai-Uwe; von Clarmann, Thomas; Burrows, John P.</p> <p>2018-04-01</p> <p>This study describes a retrieval algorithm developed at the University of Bremen to obtain vertical <span class="hlt">profiles</span> of ozone from limb <span class="hlt">observations</span> performed by the Ozone Mapper and <span class="hlt">Profiler</span> Suite (OMPS). This algorithm is based on the technique originally developed for use with data from the SCanning Imaging Absorption spectroMeter for Atmospheric CHartographY (SCIAMACHY) instrument. As both instruments make limb measurements of the scattered solar radiation in the ultraviolet (UV) and visible (Vis) spectral ranges, an underlying objective of the study is to obtain consolidated and consistent ozone <span class="hlt">profiles</span> from the two satellites and to produce a combined data set. The retrieval algorithm uses radiances in the UV and Vis wavelength ranges normalized to the radiance at an upper tangent height to obtain ozone concentrations in the altitude range of 12-60 km. Measurements at altitudes contaminated by clouds in the instrument field of view are identified and filtered out. An independent aerosol retrieval is performed beforehand and its results are used to account for the stratospheric aerosol load in the ozone inversion. The typical vertical resolution of the retrieved <span class="hlt">profiles</span> varies from ˜ 2.5 km at lower altitudes ( < 30 km) to ˜ 1.5 km (about 45 km) and becomes coarser at upper altitudes. The retrieval errors resulting from the measurement noise are estimated to be 1-4 % above 25 km, increasing to 10-30 % in the upper troposphere. OMPS data are processed for the whole of 2016. The results are compared with the NASA product and validated against <span class="hlt">profiles</span> derived from passive satellite <span class="hlt">observations</span> or measured in situ by balloon-borne sondes. Between 20 and 60 km, OMPS ozone <span class="hlt">profiles</span> typically agree with data from the Microwave Limb Sounder (MLS) v4.2 within 5-10 %, whereas in the lower altitude range the bias becomes larger, especially in the tropics. The comparison of OMPS <span class="hlt">profiles</span> with ozonesonde measurements shows differences within ±5 % between 13 and 30 km at</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017AGUFMSM11B2312S','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017AGUFMSM11B2312S"><span>Vortex, ULF wave and Aurora <span class="hlt">Observation</span> after Solar Wind Dynamic <span class="hlt">Pressure</span> Change</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Shi, Q.</p> <p>2017-12-01</p> <p>Here we will summarize our recent study and show some new results on the Magnetosphere and Ionosphere Response to Dynamic <span class="hlt">Pressure</span> Change/disturbances in the Solar Wind and foreshock regions. We study the step function type solar wind dynamic <span class="hlt">pressure</span> change (increase/decrease) interaction with the magnetosphere using THEMIS satellites at both dayside and nightside in different geocentric distances. Vortices generated by the dynamic <span class="hlt">pressure</span> change passing along the magnetopause are found and compared with model predictions. ULF waves and vortices are excited in the dayside and nightside plasma sheet when dynamic <span class="hlt">pressure</span> change hit the magnetotail. The related ionospheric responses, such as aurora and TCVs, are also investigated. We compare Global MHD simulations with the <span class="hlt">observations</span>. We will also show some new results that dayside magnetospheric FLRs might be caused by foreshock structures.Shi, Q. Q. et al. (2013), THEMIS <span class="hlt">observations</span> of ULF wave excitation in the nightside plasma sheet during sudden impulse events, J. Geophys. Res. Space Physics, 118, doi:10.1029/2012JA017984. Shi, Q. Q. et al. (2014), Solar wind <span class="hlt">pressure</span> pulse-driven magnetospheric vortices and their global consequences, J. Geophys. Res. Space Physics, 119, doi:10.1002/2013JA019551. Tian, A.M. et al.(2016), Dayside magnetospheric and ionospheric responses to solar wind <span class="hlt">pressure</span> increase: Multispacecraft and ground <span class="hlt">observations</span>, J. Geophys. Res., 121, doi:10.1002/2016JA022459. Shen, X.C. et al.(2015), Magnetospheric ULF waves with increasing amplitude related to solar wind dynamic <span class="hlt">pressure</span> changes: THEMIS <span class="hlt">observations</span>, J. Geophys. Res., 120, doi:10.1002/2014JA020913Zhao, H. Y. et al. (2016), Magnetospheric vortices and their global effect after a solar wind dynamic <span class="hlt">pressure</span> decrease, J. Geophys. Res. Space Physics, 121, doi:10.1002/2015JA021646. Shen, X. C., et al. (2017), Dayside magnetospheric ULF wave frequency modulated by a solar wind dynamic <span class="hlt">pressure</span> negative impulse, J. Geophys. Res</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2015AGUFM.A41I0165K','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2015AGUFM.A41I0165K"><span>GOSAT TIR radiometric validation toward simultaneous GHG column and <span class="hlt">profile</span> <span class="hlt">observation</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Kataoka, F.; Knuteson, R. O.; Kuze, A.; Shiomi, K.; Suto, H.; Saitoh, N.</p> <p>2015-12-01</p> <p>The Greenhouse gases <span class="hlt">Observing</span> SATellite (GOSAT) was launched on January 2009 and continues its operation for more than six years. The thermal and near infrared sensor for carbon <span class="hlt">observation</span> Fourier-Transform Spectrometer (TANSO-FTS) onboard GOSAT measures greenhouse gases (GHG), such as CO2 and CH4, with wide and high resolution spectra from shortwave infrared (SWIR) to thermal infrared (TIR). This instrument has the advantage of being able to measure simultaneously the same field of view in different spectral ranges. The combination of column-GHG form SWIR band and vertical <span class="hlt">profile</span>-GHG from TIR band provide better understanding and distribution of GHG, especially in troposphere. This work describes the radiometric validation and sensitivity analysis of TANSO-FTS TIR spectra, especially CO2, atmospheric window and CH4 channels with forward calculation. In this evaluation, we used accurate in-situ dataset of the HIPPO (HIAPER Pole-to-Pole <span class="hlt">Observation</span>) airplane <span class="hlt">observation</span> data and GOSAT vicarious calibration and validation campaign data in Railroad Valley, NV. The HIPPO aircraft campaign had taken accurate atmospheric vertical <span class="hlt">profile</span> dataset (T, RH, O3, CO2, CH4, N2O, CO) approximately pole-to-pole from the surface to the tropopause over the ocean. We implemented these dataset for forward calculation and made the spectral correction model with respect to wavenumber and internal calibration blackbody temperature The GOSAT vicarious calibration campaign have conducted every year since 2009 near summer solstice in Railroad Valley, where high-temperature desert site. In this campaign, we have measured temperature and humidity by a radiosonde and CO2, CH4 and O3 <span class="hlt">profile</span> by the AJAX airplane at the time of the GOSAT overpass. Sometimes, the GHG <span class="hlt">profiles</span> over the Railroad Valley show the air mass advection in mid-troposphere depending on upper wind. These advections bring the different concentration of GHG in lower and upper troposphere. Using these cases, we made</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2015AGUFMSM23A2530W','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2015AGUFMSM23A2530W"><span>Field Aligned Currents Derived from <span class="hlt">Pressure</span> <span class="hlt">Profiles</span> Obtained from TWINS ENA Images</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Wood, K.; Perez, J. D.; McComas, D. J.; Goldstein, J.; Valek, P. W.</p> <p>2015-12-01</p> <p>Field aligned currents (FACs) that flow from the Earth's magnetosphere into the ionosphere are an important coupling mechanism in the interaction of the solar wind with the Earth's magnetosphere. Assuming <span class="hlt">pressure</span> balance along with charge conservation yields an expression for the FACs in terms of plasma <span class="hlt">pressure</span> gradients and <span class="hlt">pressure</span> anisotropy. The Two Wide-Angle Imaging Neutral Atom Spectrometers (TWINS) mission, the first stereoscopic ENA magnetospheric imager, provides global images of the inner magnetosphere from which ion <span class="hlt">pressure</span> distributions and <span class="hlt">pressure</span> anisotropies can be obtained. Following the formulations in Heineman [1990] and using results from TWINS <span class="hlt">observations</span>, we calculate the distribution of field aligned currents for the 17-18 March 2015 geomagnetic storm in which extended ionospheric precipitation was <span class="hlt">observed</span>. Initial results for the field aligned currents will be generated assuming an isotropic pitch angle distribution. Global maps of field aligned currents during the main and recovery phase of the storm will be presented. Heinemann, H. (1990), Representations of Currents and Magnetic Fields in Anisotropic Magnetohydrostatic Plasma, J. Geophys. Res., 95, 7789.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://eric.ed.gov/?q=PROFILE+AND+OF+AND+THE+AND+HIGHER+AND+EDUCATION+AND+TEACHER&pg=2&id=EJ978326','ERIC'); return false;" href="https://eric.ed.gov/?q=PROFILE+AND+OF+AND+THE+AND+HIGHER+AND+EDUCATION+AND+TEACHER&pg=2&id=EJ978326"><span><span class="hlt">Observed</span> Classroom Quality <span class="hlt">Profiles</span> of Kindergarten Classrooms in Finland</span></a></p> <p><a target="_blank" href="http://www.eric.ed.gov/ERICWebPortal/search/extended.jsp?_pageLabel=advanced">ERIC Educational Resources Information Center</a></p> <p>Salminen, Jenni; Lerkkanen, Marja-Kristiina; Poikkeus, Anna-Maija; Pakarinen, Eija; Siekkinen, Martti; Hannikainen, Maritta; Poikonen, Pirjo-Liisa; Rasku-Puttonen, Helena</p> <p>2012-01-01</p> <p>Research Findings: The aim of the present study was to examine classroom quality <span class="hlt">profiles</span> of kindergarten classrooms using a person-centered approach and to analyze these patterns in regard to teacher and classroom characteristics. <span class="hlt">Observations</span> of the domains of Emotional Support, Classroom Organization, and Instructional Support were conducted in…</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2015APS..DPPJP2099K','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2015APS..DPPJP2099K"><span>Current/<span class="hlt">Pressure</span> <span class="hlt">Profile</span> Effects on Tearing Mode Stability in DIII-D Hybrid Discharges</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Kim, K.; Park, J. M.; Murakami, M.; La Haye, R. J.; Na, Yong-Su</p> <p>2015-11-01</p> <p>It is important to understand the onset threshold and the evolution of tearing modes (TMs) for developing a high-performance steady state fusion reactor. As initial and basic comparisons to determine TM onset, the measured plasma <span class="hlt">profiles</span> (such as temperature, density, rotation) were compared with the calculated current <span class="hlt">profiles</span> between a pair of discharges with/without n=1 mode based on the database for DIII-D hybrid plasmas. The <span class="hlt">profiles</span> were not much different, but the details were analyzed to determine their characteristics, especially near the rational surface. The tearing stability index calculated from PEST3, Δ' tends to increase rapidly just before the n=1 mode onset for these cases. The modeled equilibrium with varying <span class="hlt">pressure</span> or current <span class="hlt">profiles</span> parametrically based on the reference discharge is reconstructed for checking the onset dependency on Δ' or neoclassical effects such as bootstrap current. Simulations of TMs with the modeled equilibrium using resistive MHD codes will also be presented and compared with experiments to determine the sensibility for predicting TM onset. Work supported by US DOE under DE-FC02-04ER54698 and DE-AC52-07NA27344.</p> </li> </ol> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_3");'>3</a></li> <li><a href="#" onclick='return showDiv("page_4");'>4</a></li> <li class="active"><span>5</span></li> <li><a href="#" onclick='return showDiv("page_6");'>6</a></li> <li><a href="#" onclick='return showDiv("page_7");'>7</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div><!-- col-sm-12 --> </div><!-- row --> </div><!-- page_5 --> <div id="page_6" class="hiddenDiv"> <div class="row"> <div class="col-sm-12"> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_4");'>4</a></li> <li><a href="#" onclick='return showDiv("page_5");'>5</a></li> <li class="active"><span>6</span></li> <li><a href="#" onclick='return showDiv("page_7");'>7</a></li> <li><a href="#" onclick='return showDiv("page_8");'>8</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div> </div> <div class="row"> <div class="col-sm-12"> <ol class="result-class" start="101"> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2016AGUFM.A51A0005T','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2016AGUFM.A51A0005T"><span>An Object-Oriented Approach for Analyzing CALIPSO's <span class="hlt">Profile</span> <span class="hlt">Observations</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Trepte, C. R.</p> <p>2016-12-01</p> <p>The CALIPSO satellite mission is a pioneering international partnership between NASA and the French Space Agency, CNES. Since launch on 28 April 2006, CALIPSO has been acquiring near-continuous lidar <span class="hlt">profile</span> <span class="hlt">observations</span> of clouds and aerosols in the Earth's atmosphere. Many studies have profitably used these <span class="hlt">observations</span> to advance our understanding of climate, weather and air quality. For the most part, however, these studies have considered CALIPSO <span class="hlt">profile</span> measurements independent from one another and have not related each to neighboring or family <span class="hlt">observations</span> within a cloud element or aerosol feature. In this presentation we describe an alternative approach that groups measurements into objects visually identified from CALIPSO browse images. The approach makes use of the Visualization of CALIPSO (VOCAL) software tool that enables a user to outline a region of interest and save coordinates into a database. The selected features or objects can then be analyzed to explore spatial correlations over the feature's domain and construct bulk statistical properties for each structure. This presentation will show examples that examine cirrus and dust layers and will describe how this object-oriented approach can provide added insight into physical processes beyond conventional statistical treatments. It will further show results with combined measurements from other A-Train sensors to highlight advantages of viewing features in this manner.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=3569425','PMC'); return false;" href="https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=3569425"><span>Super, Red Palm and Palm Oleins Improve the Blood <span class="hlt">Pressure</span>, Heart Size, Aortic Media Thickness and Lipid <span class="hlt">Profile</span> in Spontaneously Hypertensive Rats</span></a></p> <p><a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pmc">PubMed Central</a></p> <p>Boon, Chee-Meng; Ng, Mei-Han; Choo, Yuen-May; Mok, Shiueh-Lian</p> <p>2013-01-01</p> <p>Background Oleic acid has been shown to lower high blood <span class="hlt">pressure</span> and provide cardiovascular protection. Curiosity arises as to whether super olein (SO), red palm olein (RPO) and palm olein (PO), which have high oleic acid content, are able to prevent the development of hypertension. Methodology/Principal Findings Four-week-old male spontaneously hypertensive rats (SHR) and Wistar-Kyoto (WKY) rats were fed 15% SO, RPO or PO supplemented diet for 15 weeks. After 15 weeks of treatment, the systolic blood <span class="hlt">pressure</span> (SBP) of SHR treated with SO, RPO and PO were 158.4±5.0 mmHg (p<0.001), 178.9±2.7 mmHg (p<0.001) and 167.7±2.1 mmHg (p<0.001), respectively, compared with SHR controls (220.9±1.5 mmHg). Bradycardia was <span class="hlt">observed</span> with SO and PO. In contrast, the SBP and heart rate of treated WKY rats were not different from those of WKY controls. The SO and PO significantly reduced the increased heart size and thoracic aortic media thickness <span class="hlt">observed</span> in untreated SHR but RPO reduced only the latter. No such differences, however, were <span class="hlt">observed</span> between the treated and untreated WKY rats. Oil Red O enface staining of thoracic-abdominal aorta did not show any lipid deposition in all treated rats. The SO and RPO significantly raised serum alkaline phosphatase levels in the SHR while body weight and renal biochemical indices were unaltered in both strains. Serum lipid <span class="hlt">profiles</span> of treated SHR and WKY rats were unchanged, with the exception of a significant reduction in LDL-C level and total cholesterol/HDL ratio (atherogenic index) in SO and RPO treated SHR compared with untreated SHR. Conclusion The SO, RPO and PO attenuate the rise in blood <span class="hlt">pressure</span> in SHR, accompanied by bradycardia and heart size reduction with SO and PO, and aortic media thickness reduction with SO, RPO and PO. The SO and RPO are antiatherogenic in nature by improving blood lipid <span class="hlt">profiles</span> in SHR. PMID:23409085</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017AGUFMSH41A2741P','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017AGUFMSH41A2741P"><span><span class="hlt">Observation</span> and modelling of the Fe XXI line <span class="hlt">profile</span> <span class="hlt">observed</span> by IRIS during the impulsive phase of flares</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Polito, V.; Testa, P.; De Pontieu, B.; Allred, J. C.</p> <p>2017-12-01</p> <p>The <span class="hlt">observation</span> of the high temperature (above 10 MK) Fe XXI 1354.1 A line with the Interface Region Imaging Spectrograph (IRIS) has provided significant insights into the chromospheric evaporation process in flares. In particular, the line is often <span class="hlt">observed</span> to be completely blueshifted, in contrast to previous <span class="hlt">observations</span> at lower spatial and spectral resolution, and in agreement with predictions from theoretical models. Interestingly, the line is also <span class="hlt">observed</span> to be mostly symmetric and with a large excess above the thermal width. One popular interpretation for the excess broadening is given by assuming a superposition of flows from different loop strands. In this work, we perform a statistical analysis of Fe XXI line <span class="hlt">profiles</span> <span class="hlt">observed</span> by IRIS during the impulsive phase of flares and compare our results with hydrodynamic simulations of multi-thread flare loops performed with the 1D RADYN code. Our results indicate that the multi-thread models cannot easily reproduce the symmetry of the line and that some other physical process might need to be invoked in order to explain the <span class="hlt">observed</span> <span class="hlt">profiles</span>.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/20070023321','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/20070023321"><span>Estimating the Soil Temperature <span class="hlt">Profile</span> from a Single Depth <span class="hlt">Observation</span>: A Simple Empirical Heatflow Solution</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Holmes, Thomas; Owe, Manfred; deJeu, Richard</p> <p>2007-01-01</p> <p>Two data sets of experimental field <span class="hlt">observations</span> with a range of meteorological conditions are used to investigate the possibility of modeling near-surface soil temperature <span class="hlt">profiles</span> in a bare soil. It is shown that commonly used heat flow methods that assume a constant ground heat flux can not be used to model the extreme variations in temperature that occur near the surface. This paper proposes a simple approach for modeling the surface soil temperature <span class="hlt">profiles</span> from a single depth <span class="hlt">observation</span>. This approach consists of two parts: 1) modeling an instantaneous ground flux <span class="hlt">profile</span> based on net radiation and the ground heat flux at 5cm depth; 2) using this ground heat flux <span class="hlt">profile</span> to extrapolate a single temperature <span class="hlt">observation</span> to a continuous near surface temperature <span class="hlt">profile</span>. The new model is validated with an independent data set from a different soil and under a range of meteorological conditions.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.osti.gov/servlets/purl/6117','SCIGOV-STC'); return false;" href="https://www.osti.gov/servlets/purl/6117"><span>Tritiated Water on Molecular Sieve: Water Dynamics and <span class="hlt">Pressure</span> <span class="hlt">Observations</span></span></a></p> <p><a target="_blank" href="http://www.osti.gov/search">DOE Office of Scientific and Technical Information (OSTI.GOV)</a></p> <p>Walters, R.T.</p> <p>1999-04-23</p> <p>The production of fusion energy in a Tokamak using deuterium and tritium requires the safe handling and processing of exhaust gases that contain various amounts of tritium. Initial operation of the Tokamak Fusion Test Reactor (TFTR), Princeton Plasma Physics Laboratory, oxidized exhaust gases for tritium recovery or long-term storage. One of the most efficient and safest ways to contain tritiated water is to sorb it onto a pelletized 4A molecular sieve. A Disposable Molecular Sieve Bed (DMSB) was designed as a <span class="hlt">pressure</span> vessel because of the possibility of <span class="hlt">pressure</span> generation from the radiolysis of tritiated water on molecular sieve. Hydrogenmore » production contributes to the complexity of the containers used to transport and store tritiated water, and increases the fabrication costs. Two months after removing a DMSB from the process at TFTR, a <span class="hlt">pressure</span> in excess of that predicted from self-radiolysis was <span class="hlt">observed</span>. Interestingly, <span class="hlt">pressure</span> measurements at longer times (up to 2.5 years) showed less <span class="hlt">pressure</span> than expected. <span class="hlt">Pressure</span> was not being generated in the DMSBs at the predicted rate. This was unexpected and prompted an investigation into the mechanism responsible for the anomalous <span class="hlt">pressure</span> measurements.« less</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/24361920','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/24361920"><span>Does the accuracy of blood <span class="hlt">pressure</span> measurement correlate with hearing loss of the <span class="hlt">observer</span>?</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Song, Soohwa; Lee, Jongshill; Chee, Youngjoon; Jang, Dong Pyo; Kim, In Young</p> <p>2014-02-01</p> <p>The auscultatory method is influenced by the hearing level of the <span class="hlt">observers</span>. If the <span class="hlt">observer</span> has hearing loss, it is possible to measure blood <span class="hlt">pressure</span> inaccurately by misreading the Korotkoff sounds at systolic blood <span class="hlt">pressure</span> (SBP) and diastolic blood <span class="hlt">pressure</span> (DBP). Because of the potential clinical problems this discrepancy may cause, we used a hearing loss simulator to determine how hearing level affects the accuracy of blood <span class="hlt">pressure</span> measurements. Two data sets (data set A, 32 Korotkoff sound video clips recorded by the British Hypertension Society; data set B, 28 Korotkoff sound data acquired from the Korotkoff sound recording system developed by Hanyang University) were used and all the data were attenuated to simulate a hearing loss of 5, 10, 15, 20, and 25 dB using the hearing loss simulator. Five <span class="hlt">observers</span> with normal hearing assessed the blood <span class="hlt">pressures</span> from these data sets and the differences between the values measured from the original recordings (no attenuation) and the attenuated versions were analyzed. Greater attenuation of the Korotkoff sounds, or greater hearing loss, resulted in larger blood <span class="hlt">pressure</span> measurement differences when compared with the original data. When measuring blood <span class="hlt">pressure</span> with hearing loss, the SBP tended to be underestimated and the DBP was overestimated. The mean differences between the original data and the 25 dB hearing loss data for the two data sets combined were 1.55±2.71 and -4.32±4.21 mmHg for SBP and DBP, respectively. This experiment showed that the accuracy of blood <span class="hlt">pressure</span> measurements using the auscultatory method is affected by <span class="hlt">observer</span> hearing level. Therefore, to reduce possible error using the auscultatory method, <span class="hlt">observers</span>' hearing should be tested.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/25579390','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/25579390"><span>Impact of boiling conditions on the molecular and sensory <span class="hlt">profile</span> of a vegetable broth.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Mougin, Alice; Mauroux, Olivier; Matthey-Doret, Walter; Barcos, Eugenia Maria; Beaud, Fernand; Bousbaine, Ahmed; Viton, Florian; Smarrito-Menozzi, Candice</p> <p>2015-02-11</p> <p>Low-<span class="hlt">pressure</span> cooking has recently been identified as an alternative to ambient and high-<span class="hlt">pressure</span> cooking to provide food with enhanced organoleptic properties. This work investigates the impact of the cooking process at different <span class="hlt">pressures</span> on the molecular and sensory <span class="hlt">profile</span> of a vegetable broth. Experimental results showed similar sensory and chemical <span class="hlt">profiles</span> of vegetable broths when boiling at 0.93 and 1.5 bar, while an enhancement of sulfur volatile compounds correlated with a greater leek content and savory aroma was <span class="hlt">observed</span> when boiling at low <span class="hlt">pressure</span> (80 °C/0.48 bar). Thus, low-<span class="hlt">pressure</span> cooking would allow preserving the most labile volatiles likely due to the lower water boiling temperature and the reduced level of oxygen. This study evidenced chemical and sensory impact of <span class="hlt">pressure</span> during cooking and demonstrated that the flavor <span class="hlt">profile</span> of culinary preparations can be enhanced by applying low-<span class="hlt">pressure</span> conditions.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.osti.gov/biblio/22521951-energetic-particle-pressure-interplanetary-shocks-stereo-observations','SCIGOV-STC'); return false;" href="https://www.osti.gov/biblio/22521951-energetic-particle-pressure-interplanetary-shocks-stereo-observations"><span>ENERGETIC PARTICLE <span class="hlt">PRESSURE</span> AT INTERPLANETARY SHOCKS: STEREO-A <span class="hlt">OBSERVATIONS</span></span></a></p> <p><a target="_blank" href="http://www.osti.gov/search">DOE Office of Scientific and Technical Information (OSTI.GOV)</a></p> <p>Lario, D.; Decker, R. B.; Roelof, E. C.</p> <p>2015-11-10</p> <p>We study periods of elevated energetic particle intensities <span class="hlt">observed</span> by STEREO-A when the partial <span class="hlt">pressure</span> exerted by energetic (≥83 keV) protons (P{sub EP}) is larger than the <span class="hlt">pressure</span> exerted by the interplanetary magnetic field (P{sub B}). In the majority of cases, these periods are associated with the passage of interplanetary shocks. Periods when P{sub EP} exceeds P{sub B} by more than one order of magnitude are <span class="hlt">observed</span> in the upstream region of fast interplanetary shocks where depressed magnetic field regions coincide with increases of energetic particle intensities. When solar wind parameters are available, P{sub EP} also exceeds the <span class="hlt">pressure</span> exertedmore » by the solar wind thermal population (P{sub TH}). Prolonged periods (>12 hr) with both P{sub EP} > P{sub B} and P{sub EP} > P{sub TH} may also occur when energetic particles accelerated by an approaching shock encounter a region well upstream of the shock characterized by low magnetic field magnitude and tenuous solar wind density. Quasi-exponential increases of the sum P{sub SUM} = P{sub B} + P{sub TH} + P{sub EP} are <span class="hlt">observed</span> in the immediate upstream region of the shocks regardless of individual changes in P{sub EP}, P{sub B}, and P{sub TH}, indicating a coupling between P{sub EP} and the <span class="hlt">pressure</span> of the background medium characterized by P{sub B} and P{sub TH}. The quasi-exponential increase of P{sub SUM} implies a radial gradient ∂P{sub SUM}/∂r > 0 that is quasi-stationary in the shock frame and results in an outward force applied to the plasma upstream of the shock. This force can be maintained by the mobile energetic particles streaming upstream of the shocks that, in the most intense events, drive electric currents able to generate diamagnetic cavities and depressed solar wind density regions.« less</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/12454392','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/12454392"><span>Gene expression <span class="hlt">profiles</span> in chondrosarcoma cells subjected to cyclic stretching and hydrostatic <span class="hlt">pressure</span>. A cDNA array study.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Karjalainen, Hannu M; Sironen, Reijo K; Elo, Mika A; Kaarniranta, Kai; Takigawa, Masaharu; Helminen, Heikki J; Lammi, Mikko J</p> <p>2003-01-01</p> <p>Mechanical forces have a profound effect on cartilage tissue and chondrocyte metabolism. Strenuous loading inhibits the cellular metabolism, while optimal level of loading at correct frequency raises an anabolic response in chondrocytes. In this study, we used Atlas Human Cancer cDNA array to investigate mRNA expression <span class="hlt">profiles</span> in human chondrosarcoma cells stretched 8% for 6 hours at a frequency of 0.5 Hz. In addition, cultures were exposed to continuous and cyclic (0.5 Hz) 5 MPa hydrostatic <span class="hlt">pressure</span>. Cyclic stretch had a more profound effect on the gene expression <span class="hlt">profiles</span> than 5 MPa hydrostatic <span class="hlt">pressure</span>. Several genes involved with the regulation of cell cycle were increased in stretched cells, as well as mRNAs for PDGF-B, glucose-1-phosphate uridylyltransferase, Tiam1, cdc37 homolog, Gem, integrin alpha6, and matrix metalloproteinase-3. Among down-regulated genes were plakoglobin, TGF-alpha, retinoic acid receptor-alpha and Wnt8b. A smaller number of changes was detected after <span class="hlt">pressure</span> treatments. Plakoglobin was increased under cyclic and continuous 5 MPa hydrostatic <span class="hlt">pressure</span>, while mitogen-activated protein kinase-9, proliferating cell nuclear antigen, Rad6, CD9 antigen, integrins alphaE and beta8, and vimentin were decreased. Cyclic and continuous <span class="hlt">pressurization</span> induces a number of specific changes. In conclusion, a different set of genes were affected by three different types of mechanical stimuli applied on chondrosarcoma cells.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017AtmRe.194...17B','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017AtmRe.194...17B"><span>Potential of collocated radiometer and wind <span class="hlt">profiler</span> <span class="hlt">observations</span> for monsoon studies</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Balaji, B.; Prabha, Thara V.; Jaya Rao, Y.; Kiran, T.; Dinesh, G.; Chakravarty, Kaustav; Sonbawne, S. M.; Rajeevan, M.</p> <p>2017-09-01</p> <p>Collocated <span class="hlt">observations</span> from microwave radiometer and wind <span class="hlt">profiler</span> are used in a pilot study during the monsoon period to derive information on the thermodynamics and winds and association with rainfall characteristics. These instruments were operated throughout the monsoon season of 2015. Continuous vertical <span class="hlt">profiles</span> of winds, temperature and humidity show significant promise for understanding the low-level jet, its periodicity and its association with moisture transport, clouds and precipitation embedded within the monsoon large-scale convection. <span class="hlt">Observations</span> showed mutually beneficial in explaining variability that are part of the low frequency oscillations and the diurnal variability during monsoon. These <span class="hlt">observations</span> highlight the importance of locally driven convective systems, in the presence of weak moisture transport over the area. The episodic moisture convergence showed a periodicity of 9 days which matches with the subsequent convection and precipitation and thermodynamic regimes. Inferences from the diurnal cycle of moisture transport and the convective activity, relationship with the low-level jet characteristics and thermodynamics are also illustrated.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/24683321','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/24683321"><span>Adaptive super-twisting <span class="hlt">observer</span> for estimation of random road excitation <span class="hlt">profile</span> in automotive suspension systems.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Rath, J J; Veluvolu, K C; Defoort, M</p> <p>2014-01-01</p> <p>The estimation of road excitation <span class="hlt">profile</span> is important for evaluation of vehicle stability and vehicle suspension performance for autonomous vehicle control systems. In this work, the nonlinear dynamics of the active automotive system that is excited by the unknown road excitation <span class="hlt">profile</span> are considered for modeling. To address the issue of estimation of road <span class="hlt">profile</span>, we develop an adaptive supertwisting <span class="hlt">observer</span> for state and unknown road <span class="hlt">profile</span> estimation. Under Lipschitz conditions for the nonlinear functions, the convergence of the estimation error is proven. Simulation results with Ford Fiesta MK2 demonstrate the effectiveness of the proposed <span class="hlt">observer</span> for state and unknown input estimation for nonlinear active suspension system.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=3934084','PMC'); return false;" href="https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=3934084"><span>Adaptive Super-Twisting <span class="hlt">Observer</span> for Estimation of Random Road Excitation <span class="hlt">Profile</span> in Automotive Suspension Systems</span></a></p> <p><a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pmc">PubMed Central</a></p> <p>Rath, J. J.; Veluvolu, K. C.; Defoort, M.</p> <p>2014-01-01</p> <p>The estimation of road excitation <span class="hlt">profile</span> is important for evaluation of vehicle stability and vehicle suspension performance for autonomous vehicle control systems. In this work, the nonlinear dynamics of the active automotive system that is excited by the unknown road excitation <span class="hlt">profile</span> are considered for modeling. To address the issue of estimation of road <span class="hlt">profile</span>, we develop an adaptive supertwisting <span class="hlt">observer</span> for state and unknown road <span class="hlt">profile</span> estimation. Under Lipschitz conditions for the nonlinear functions, the convergence of the estimation error is proven. Simulation results with Ford Fiesta MK2 demonstrate the effectiveness of the proposed <span class="hlt">observer</span> for state and unknown input estimation for nonlinear active suspension system. PMID:24683321</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2006AGUSMSA31B..09M','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2006AGUSMSA31B..09M"><span>Geocoronal Balmer α line <span class="hlt">profile</span> <span class="hlt">observations</span> and forward-model analysis</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Mierkiewicz, E. J.; Bishop, J.; Roesler, F. L.; Nossal, S. M.</p> <p>2006-05-01</p> <p>High spectral resolution geocoronal Balmer α line <span class="hlt">profile</span> <span class="hlt">observations</span> from Pine Bluff Observatory (PBO) are presented in the context of forward-model analysis. Because Balmer series column emissions depend significantly on multiple scattering, retrieval of hydrogen parameters of general aeronomic interest from these <span class="hlt">observations</span> (e.g., the hydrogen column abundance) currently requires a forward modeling approach. This capability is provided by the resonance radiative transfer code LYAO_RT. We have recently developed a parametric data-model comparison search procedure employing an extensive grid of radiative transport model input parameters (defining a 6-dimensional parameter space) to map-out bounds for feasible forward model retrieved atomic hydrogen density distributions. We applied this technique to same-night (March, 2000) ground-based Balmer α data from PBO and geocoronal Lyman β measurements from the Espectrógrafo Ultravioleta extremo para la Radiación Difusa (EURD) instrument on the Spanish satellite MINISAT-1 (provided by J.F. Gómez and C. Morales of the Laboratorio de Astrofisica Espacial y Física Fundamental, INTA, Madrid, Spain) in order to investigate the modeling constraints imposed by two sets of independent geocoronal intensity measurements, both of which rely on astronomical calibration methods. In this poster we explore extending this analysis to the line <span class="hlt">profile</span> information also contained in the March 2000 PBO Balmer α data set. In general, a decrease in the Doppler width of the Balmer α emission with shadow altitude is a persistent feature in every night of PBO <span class="hlt">observations</span> in which a wide range of shadow altitudes are <span class="hlt">observed</span>. Preliminary applications of the LYAO_RT code, which includes the ability to output Doppler line <span class="hlt">profiles</span> for both the singly and multiply scattered contributions to the Balmer α emission line, displays good qualitative agreement with regard to geocoronal Doppler width trends <span class="hlt">observed</span> from PBO. Model-data Balmer</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/26378750','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/26378750"><span>[Sulphureous mud-bath therapy and changes in blood <span class="hlt">pressure</span>: <span class="hlt">observational</span> investigation].</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Costantino, M; Marongiu, M B; Russomanno, G; Conti, V; Manzo, V; Filippelli, A</p> <p>2015-01-01</p> <p>The chronic arthropathies currently appear to be a major cause of disability with a negative impact on quality of life and health care spending. The mud-bath therapy is a spa treatment that induces benefic effects in chronic rheumatic diseases. It has long been debated on the assumption that the mud-bath spa therapy could have adverse cardiovascular effects which often induce caution and even a contraindication to the use of this treatment in chronic arthropathies associated with cardiovascular alterations such as hypertension. The aim of this <span class="hlt">observational</span> study was to investigate, in arthrorheumatic subjects, the effects of sulphureous mud-bath cycle on blood <span class="hlt">pressure</span> and the possible appearance of adverse drug reaction. 169 patients, with age range 42-86 years, suffering by chronic arthropathies were treated with sulphureous mud-bath therapy for 2 weeks. According to the arterial <span class="hlt">pressure</span> values, measured before the spa treatment, the patients considered were divided in three groups: with normal blood <span class="hlt">pressure</span> (NOR group); with high blood <span class="hlt">pressure</span>, after, the latter group was divided in IPET (patients in treatment with antihypertensive drugs) and IPENT (patients not in antihypertensive therapy). The arterial <span class="hlt">pressure</span> values, maximum and minimum, expressed in mmHg, were detected in the first (T1) - sixth (T6) and twelfth (T12) day of spa treatment. The media arterial <span class="hlt">pressure</span> values collected before and after T1, before and after T6, before and after T12 , before T1 and after T12 were compared. The data, presented as mean±SD, were compared with the paired Student t test. A p value ≤0.05 was considered significant. The comparison between the mean values detected in pre and post T1, pre and post T6, pre and post T12 have showed that sulphureous mud-bath therapy induced a significant (p<0.05) reduction of arterial blood <span class="hlt">pressure</span> values in patients suffering of chronic arthropathies with high blood <span class="hlt">pressure</span> in antihypertensive therapy or not (IPET and IPENT groups</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://ntrs.nasa.gov/search.jsp?R=19820034893&hterms=Hydrodynamic+Cavitation+Oil&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D30%26Ntt%3DHydrodynamic%2BCavitation%2BOil','NASA-TRS'); return false;" href="https://ntrs.nasa.gov/search.jsp?R=19820034893&hterms=Hydrodynamic+Cavitation+Oil&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D30%26Ntt%3DHydrodynamic%2BCavitation%2BOil"><span><span class="hlt">Observation</span> of <span class="hlt">pressure</span> variation in the cavitation region of submerged journal bearings</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Etsion, I.; Ludwig, L. P.</p> <p>1981-01-01</p> <p>Visual <span class="hlt">observations</span> and <span class="hlt">pressure</span> measurements in the cavitation zone of a submerged journal bearing are described. Tests are run at speeds of 1840 and 3000 rpm, and at each speed, four different levels of the ambient supply <span class="hlt">pressure</span> are applied, ranging from 13.6 KPa to 54.4 KPa. A strong reverse flow is detected inside the cavitation area adjacent to its downstream end, and significant <span class="hlt">pressure</span> variations on the order of 50 KPa are found inside the cavitation region at the downstream portion of its circumferential extent. Results indicate that the assumption of a constant cavitation <span class="hlt">pressure</span> is incorrect in the case of enclosed cavitations, and it is postulated that oil which is saturated with air under atmospheric <span class="hlt">pressure</span> becomes oversaturated in the subcavity <span class="hlt">pressure</span> loop.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017Tectp.721..448S','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017Tectp.721..448S"><span>Microstructure of calcite deformed by high-<span class="hlt">pressure</span> torsion: An X-ray line <span class="hlt">profile</span> study</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Schuster, Roman; Schafler, Erhard; Schell, Norbert; Kunz, Martin; Abart, Rainer</p> <p>2017-11-01</p> <p>Calcite aggregates were deformed to high strain using high-<span class="hlt">pressure</span> torsion and applying confining <span class="hlt">pressures</span> of 1-6 GPa and temperatures between room temperature and 450 °C. The run products were characterized by X-ray diffraction, and key microstructural parameters were extracted employing X-ray line <span class="hlt">profile</span> analysis. The dominant slip system was determined as r { 10 1 bar 4 } ⟨ 2 bar 021 ⟩ with edge dislocation character. The resulting dislocation density and the size of the coherently scattering domains (CSD) exhibit a systematic dependence on the P-T conditions of deformation. While high <span class="hlt">pressure</span> generally impedes recovery through reducing point defect mobility, the picture is complicated by <span class="hlt">pressure</span>-induced phase transformations in the CaCO3 system. Transition from the calcite stability field to those of the high-<span class="hlt">pressure</span> polymorphs CaCO3-II, CaCO3-III and CaCO3-IIIb leads to a change of the microstructural evolution with deformation. At 450 °C and <span class="hlt">pressures</span> within the calcite stability field, dislocation densities and CSD sizes saturate at shear strains exceeding 10 in agreement with earlier studies at lower <span class="hlt">pressures</span>. In the stability field of CaCO3-II, the dislocation density exhibits a more complex behavior. Furthermore, at a given strain and strain rate, the dislocation density increases and the CSD size decreases with increasing <span class="hlt">pressure</span> within the stability fields of either calcite or of the high-<span class="hlt">pressure</span> polymorphs. There is, however, a jump from high dislocation densities and small CSDs in the upper <span class="hlt">pressure</span> region of the calcite stability field to lower dislocation densities and larger CSDs in the low-<span class="hlt">pressure</span> region of the CaCO3-II stability field. This jump is more pronounced at higher temperatures and less so at room temperature. The <span class="hlt">pressure</span> influence on the deformation-induced evolution of dislocation densities implies that <span class="hlt">pressure</span> variations may change the rheology of carbonate rocks. In particular, a weakening is expected to occur at</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2015JPhCS.659a2024H','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2015JPhCS.659a2024H"><span>Exponential Boundary <span class="hlt">Observers</span> for <span class="hlt">Pressurized</span> Water Pipe</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Hermine Som, Idellette Judith; Cocquempot, Vincent; Aitouche, Abdel</p> <p>2015-11-01</p> <p>This paper deals with state estimation on a <span class="hlt">pressurized</span> water pipe modeled by nonlinear coupled distributed hyperbolic equations for non-conservative laws with three known boundary measures. Our objective is to estimate the fourth boundary variable, which will be useful for leakage detection. Two approaches are studied. Firstly, the distributed hyperbolic equations are discretized through a finite-difference scheme. By using the Lipschitz property of the nonlinear term and a Lyapunov function, the exponential stability of the estimation error is proven by solving Linear Matrix Inequalities (LMIs). Secondly, the distributed hyperbolic system is preserved for state estimation. After state transformations, a Luenberger-like PDE boundary <span class="hlt">observer</span> based on backstepping mathematical tools is proposed. An exponential Lyapunov function is used to prove the stability of the resulted estimation error. The performance of the two <span class="hlt">observers</span> are shown on a water pipe prototype simulated example.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.osti.gov/pages/biblio/1229942-characterization-ultrafast-laser-ablation-plasma-plumes-various-ar-ambient-pressures','SCIGOV-DOEP'); return false;" href="https://www.osti.gov/pages/biblio/1229942-characterization-ultrafast-laser-ablation-plasma-plumes-various-ar-ambient-pressures"><span>Characterization of ultrafast laser-ablation plasma plumes at various Ar ambient <span class="hlt">pressures</span></span></a></p> <p><a target="_blank" href="http://www.osti.gov/pages">DOE PAGES</a></p> <p>Diwakar, P. K.; Harilal, S. S.; Phillips, M. C.; ...</p> <p>2015-07-30</p> <p>Expansion dynamics and internal plume structures of fs laser ablated brass plasma in Ar at various <span class="hlt">pressure</span> levels ranging from vacuum to atmospheric were studied using multitude of diagnostic tools including time resolved and time integrated 2-dimensional imaging, optical time of flight measurements and visible emission spectroscopy. Temporal evolution of excited Cu and Zn species in the plume were imaged using band pass interference filters and compared its hydrodynamic expansion features with spectrally integrated images of the plume. 2D imaging coupled with monochromatic line selection showed several interesting features at various <span class="hlt">pressure</span> levels which include velocity differences among the plumemore » species, emission intensity distribution, plasma temperature, electron density etc. Plume confinement, enhanced signal intensity, and dual peak structures in time-of-flight <span class="hlt">profiles</span> were <span class="hlt">observed</span> at intermediate <span class="hlt">pressure</span> range of ~10 Torr. Optimum signal to background ratio was also <span class="hlt">observed</span> in this <span class="hlt">pressure</span> range. As a result, possible mechanisms for <span class="hlt">observed</span> changes in plume shape, optical emission intensity and dual peak structures in time-of-flight <span class="hlt">profiles</span> were discussed.« less</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.osti.gov/servlets/purl/1334282','SCIGOV-STC'); return false;" href="https://www.osti.gov/servlets/purl/1334282"><span>Raw <span class="hlt">Pressure</span> Data from <span class="hlt">Observation</span> Wells at Brady's Hot Springs</span></a></p> <p><a target="_blank" href="http://www.osti.gov/search">DOE Office of Scientific and Technical Information (OSTI.GOV)</a></p> <p>David Lim</p> <p></p> <p>This .csv files contain the raw water <span class="hlt">pressure</span> data from three <span class="hlt">observation</span> wells during pumping tests performed in the Spring of 2016. Included is a "read me" file explaining the details of where and how the data were collected.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/20059898','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/20059898"><span>Casein micelle dissociation in skim milk during high-<span class="hlt">pressure</span> treatment: effects of <span class="hlt">pressure</span>, pH, and temperature.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Orlien, V; Boserup, L; Olsen, K</p> <p>2010-01-01</p> <p>The effect of pH (from 5.5 to 7.5) and temperature (from 5 to 40 degrees C) on the turbidity of reconstituted skim milk powder was investigated at ambient <span class="hlt">pressure</span> and in situ under <span class="hlt">pressure</span> (up to 500MPa) by measurement of light scattering. High-<span class="hlt">pressure</span> treatment reduced the turbidity of milk for all combinations of pH and temperature due to micelle dissociation. The turbidity <span class="hlt">profiles</span> had a characteristic sigmoidal shape in which almost no effect on turbidity was <span class="hlt">observed</span> at low <span class="hlt">pressures</span> (100MPa), followed by a stronger <span class="hlt">pressure</span> dependency over a <span class="hlt">pressure</span> range of 150MPa during which turbidity decreased extremely. From the turbidity <span class="hlt">profiles</span>, the threshold <span class="hlt">pressure</span> for disruption of micelle integrity was determined and ranged from 150MPa at low pH to 350-400MPa at high pH. The threshold <span class="hlt">pressure</span> diagram clearly showed a relationship between the barostability of casein micelles and pH, whereas almost no effect of temperature was shown. This remarkable pH effect was a consequence of <span class="hlt">pressure</span>-induced changes in the electrostatic interactions between colloidal calcium phosphate and the caseins responsible for maintaining micellar structure and was explained by a shift in the calcium phosphate balance in the micelle-serum system. Accordingly, a mechanism for high <span class="hlt">pressure</span>-induced disruption of micelle integrity is suggested in which the state of calcium plays a crucial role in the micelle dissociation process. Copyright 2010 American Dairy Science Association. Published by Elsevier Inc. All rights reserved.</p> </li> </ol> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_4");'>4</a></li> <li><a href="#" onclick='return showDiv("page_5");'>5</a></li> <li class="active"><span>6</span></li> <li><a href="#" onclick='return showDiv("page_7");'>7</a></li> <li><a href="#" onclick='return showDiv("page_8");'>8</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div><!-- col-sm-12 --> </div><!-- row --> </div><!-- page_6 --> <div id="page_7" class="hiddenDiv"> <div class="row"> <div class="col-sm-12"> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_5");'>5</a></li> <li><a href="#" onclick='return showDiv("page_6");'>6</a></li> <li class="active"><span>7</span></li> <li><a href="#" onclick='return showDiv("page_8");'>8</a></li> <li><a href="#" onclick='return showDiv("page_9");'>9</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div> </div> <div class="row"> <div class="col-sm-12"> <ol class="result-class" start="121"> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2001PhDT.......183K','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2001PhDT.......183K"><span>Validation of ionospheric electron density <span class="hlt">profiles</span> inferred from GPS occultation <span class="hlt">observations</span> of the GPS/MET experiment</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Kawakami, Todd Mori</p> <p></p> <p>In April of 1995, the launch of the GPS Meteorology Experiment (GPS/MET) onboard the Orbview-1 satellite, formerly known as Microlab-1, provided the first technology demonstration of active limb sounding of the Earth's atmosphere with a low Earth orbiting spacecraft utilizing the signals transmitted by the satellites of the Global Positioning System (GPS). Though the experiment's primary mission was to probe the troposphere and stratosphere, GPS/MET was also capable of making radio occultation <span class="hlt">observations</span> of the ionosphere. The application of the GPS occultation technique to the upper atmosphere created a unique opportunity to conduct ionospheric research with an unprecedented global distribution of <span class="hlt">observations</span>. For operational support requirements, the Abel transform could be employed to invert the horizontal TEC <span class="hlt">profiles</span> computed from the L1 and L2 phase measurements <span class="hlt">observed</span> by GPS/MET into electron density <span class="hlt">profiles</span> versus altitude in near real time. The usefulness of the method depends on how effectively the TEC limb <span class="hlt">profiles</span> can be transformed into vertical electron density <span class="hlt">profiles</span>. An assessment of GPS/MET's ability to determine electron density <span class="hlt">profiles</span> needs to be examined to validate the significance of the GPS occultation method as a new and complementary ionospheric research tool to enhance the <span class="hlt">observational</span> databases and improve space weather modeling and forecasting. To that end, simulations of the occultation <span class="hlt">observations</span> and their inversions have been conducted to test the Abel transform algorithm and to provide qualitative information about the type and range of errors that might be experienced during the processing of real data. Comparisons of the electron density <span class="hlt">profiles</span> inferred from real GPS/MET <span class="hlt">observations</span> are then compared with coincident in situ measurements from the satellites of Defense Meteorological Satellite Program (DMSP) and ground-based remote sensing from digisonde and incoherent scatter radar facilities. The principal focus of</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2005DPS....37.4520M','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2005DPS....37.4520M"><span>PPI/HASI <span class="hlt">Pressure</span> Measurements in the Atmosphere of Titan</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>M'akinen, J. T. T.; Harri, A.-M.; Siili, T.; Lehto, A.; Kahanp'a'a, H.; Genzer, M.; Leppelmeier, G. W.; Leinonen, J.</p> <p>2005-08-01</p> <p>The Huygens probe descended through the atmosphere of Titan on January 14, 2005, providing an excellent set of <span class="hlt">observations</span>. As a part of the Huygens Atmospheric Structure Instrument (HASI) measuring several variables, including acceleration, <span class="hlt">pressure</span>, temperature and atmospheric electricity, the <span class="hlt">Pressure</span> <span class="hlt">Profile</span> Instrument (PPI) provided by FMI commenced operations after the deployment of the main parachute and jettisoning of the heat shield at an altitude of about 160 km. Based on aerodynamic considerations, PPI measured the total <span class="hlt">pressure</span> with a Kiel probe at the end of a boom, connected to the sensor electronics inside the probe through an inlet tube. The instrument performed flawlessly during the 2.5 hour descent and the 0.5 hour surface phase before the termination of radio link between Huygens and the Cassini orbiter. We present an analysis of the <span class="hlt">pressure</span> data including recreation of the <span class="hlt">pressure</span>, temperature, altitude, velocity and acceleration <span class="hlt">profiles</span> as well as an estimate for the level of atmospheric activity on the surface of Titan.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/26133928','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/26133928"><span>Comparing effects of perfusion and hydrostatic <span class="hlt">pressure</span> on gene <span class="hlt">profiles</span> of human chondrocyte.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Zhu, Ge; Mayer-Wagner, Susanne; Schröder, Christian; Woiczinski, Matthias; Blum, Helmut; Lavagi, Ilaria; Krebs, Stefan; Redeker, Julia I; Hölzer, Andreas; Jansson, Volkmar; Betz, Oliver; Müller, Peter E</p> <p>2015-09-20</p> <p>Hydrostatic <span class="hlt">pressure</span> and perfusion have been shown to regulate the chondrogenic potential of articular chondrocytes. In order to compare the effects of hydrostatic <span class="hlt">pressure</span> plus perfusion (HPP) and perfusion (P) we investigated the complete gene expression <span class="hlt">profiles</span> of human chondrocytes under HPP and P. A simplified bioreactor was constructed to apply loading (0.1 MPa for 2 h) and perfusion (2 ml) through the same piping by <span class="hlt">pressurizing</span> the medium directly. High-density monolayer cultures of human chondrocytes were exposed to HPP or P for 4 days. Controls (C) were maintained in static cultures. Gene expression was evaluated by sequencing (RNAseq) and quantitative real-time PCR analysis. Both treatments changed gene expression levels of human chondrocytes significantly. Specifically, HPP and P increased COL2A1 expression and decreased COL1A1 and MMP-13 expression. Despite of these similarities, RNAseq revealed a list of cartilage genes including ACAN, ITGA10 and TNC, which were differentially expressed by HPP and P. Of these candidates, adhesion related molecules were found to be upregulated in HPP. Both HPP and P treatment had beneficial effects on chondrocyte differentiation and decreased catabolic enzyme expression. The study provides new insight into how hydrostatic <span class="hlt">pressure</span> and perfusion enhance cartilage differentiation and inhibit catabolic effects. Copyright © 2015 Elsevier B.V. All rights reserved.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=3922657','PMC'); return false;" href="https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=3922657"><span>Baseline <span class="hlt">pressure</span> errors (BPEs) extensively influence intracranial <span class="hlt">pressure</span> scores: results of a prospective <span class="hlt">observational</span> study</span></a></p> <p><a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pmc">PubMed Central</a></p> <p></p> <p>2014-01-01</p> <p>Background Monitoring of intracranial <span class="hlt">pressure</span> (ICP) is a cornerstone in the surveillance of neurosurgical patients. The ICP is measured against a baseline <span class="hlt">pressure</span> (i.e. zero - or reference <span class="hlt">pressure</span>). We have previously reported that baseline <span class="hlt">pressure</span> errors (BPEs), manifested as spontaneous shift or drifts in baseline <span class="hlt">pressure</span>, cause erroneous readings of mean ICP in individual patients. The objective of this study was to monitor the frequency and severity of BPEs. To this end, we performed a prospective, <span class="hlt">observational</span> study monitoring the ICP from two separate ICP sensors (Sensors 1 and 2) placed in close proximity in the brain. We characterized BPEs as differences in mean ICP despite near to identical ICP waveform in Sensors 1 and 2. Methods The study enrolled patients with aneurysmal subarachnoid hemorrhage in need of continuous ICP monitoring as part of their intensive care management. The two sensors were placed close to each other in the brain parenchyma via the same burr hole. The monitoring was performed as long as needed from a clinical perspective and the ICP recordings were stored digitally for analysis. For every patient the mean ICP as well as the various ICP wave parameters of the two sensors were compared. Results Sixteen patients were monitored median 164 hours (ranges 70 – 364 hours). Major BPEs, as defined by marked differences in mean ICP despite similar ICP waveform, were seen in 9 of them (56%). The BPEs were of magnitudes that had the potential to alter patient management. Conclusions Baseline <span class="hlt">Pressure</span> Errors (BPEs) occur in a significant number of patients undergoing continuous ICP monitoring and they may alter patient management. The current practice of measuring ICP against a baseline <span class="hlt">pressure</span> does not comply with the concept of State of the Art. Monitoring of the ICP waves ought to become the new State of the Art as they are not influenced by BPEs. PMID:24472296</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://www.dtic.mil/docs/citations/AD1004526','DTIC-ST'); return false;" href="http://www.dtic.mil/docs/citations/AD1004526"><span>A Method for Evaluation of Model-Generated Vertical <span class="hlt">Profiles</span> of Meteorological Variables</span></a></p> <p><a target="_blank" href="http://www.dtic.mil/">DTIC Science & Technology</a></p> <p></p> <p>2016-03-01</p> <p>3 2.1 RAOB Soundings and WRF Output for <span class="hlt">Profile</span> Generation 3 2.2 Height-Based <span class="hlt">Profiles</span> 5 2.3 <span class="hlt">Pressure</span>-Based <span class="hlt">Profiles</span> 5 3. Comparisons 8 4...downward arrow. The blue lines represent sublayers with sublayer means indicated by red triangles. Circles indicate the <span class="hlt">observations</span> or WRF output...9 Table 3 Sample of differences in listed variables derived from WRF and RAOB data</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/1994CmpSt..28..255S','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/1994CmpSt..28..255S"><span><span class="hlt">Observations</span> of a <span class="hlt">pressurized</span> hydraulic hose under lateral liquid impacts</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Stewart, C. D.; Gorman, D. G.</p> <p></p> <p>The effects of 'pin-hole' failure of one <span class="hlt">pressurized</span> hydraulic hose on its neighbour are investigated. A <span class="hlt">pressurized</span> test hose was inserted into a custom testing apparatus and subjected to a series of ten short duration liquid impacts simulating the pin-hole failure of an initial hose. Subsequent displacements of the hose were filmed and plotted with respect to time. Three distinct pattern groups emerged which were used to explain the resultant damage to the hose. It was <span class="hlt">observed</span> that the middle pattern, corresponding to impacts 6 and 7, appears to be the point where the very damaging hydraulic penetration mechanism became dominant and the outer layer of the hose failed. On completion of the ten impact series it was <span class="hlt">observed</span> that a small hole on the outer surface of the hose gave way to a relatively large damaged area in the strength bearing inner braid material.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=5808170','PMC'); return false;" href="https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=5808170"><span>On the Accurate Determination of Shock Wave Time-<span class="hlt">Pressure</span> <span class="hlt">Profile</span> in the Experimental Models of Blast-Induced Neurotrauma</span></a></p> <p><a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pmc">PubMed Central</a></p> <p>Skotak, Maciej; Alay, Eren; Chandra, Namas</p> <p>2018-01-01</p> <p>Measurement issues leading to the acquisition of artifact-free shock wave <span class="hlt">pressure</span>-time <span class="hlt">profiles</span> are discussed. We address the importance of in-house sensor calibration and data acquisition sampling rate. Sensor calibration takes into account possible differences between calibration methodology in a manufacturing facility, and those used in the specific laboratory. We found in-house calibration factors of brand new sensors differ by less than 10% from their manufacturer supplied data. Larger differences were noticeable for sensors that have been used for hundreds of experiments and were as high as 30% for sensors close to the end of their useful lifetime. These <span class="hlt">observations</span> were despite the fact that typical overpressures in our experiments do not exceed 50 psi for sensors that are rated at 1,000 psi maximum <span class="hlt">pressure</span>. We demonstrate that sampling rate of 1,000 kHz is necessary to capture the correct rise time values, but there were no statistically significant differences between peak overpressure and impulse values for low-intensity shock waves (Mach number <2) at lower rates. We discuss two sources of experimental errors originating from mechanical vibration and electromagnetic interference on the quality of a waveform recorded using state-of-the-art high-frequency <span class="hlt">pressure</span> sensors. The implementation of preventive measures, <span class="hlt">pressure</span> acquisition artifacts, and data interpretation with examples, are provided in this paper that will help the community at large to avoid these mistakes. In order to facilitate inter-laboratory data comparison, common reporting standards should be developed by the blast TBI research community. We noticed the majority of published literature on the subject limits reporting to peak overpressure; with much less attention directed toward other important parameters, i.e., duration, impulse, and dynamic <span class="hlt">pressure</span>. These parameters should be included as a mandatory requirement in publications so the results can be properly compared with</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/21770413','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/21770413"><span>Influence of high-<span class="hlt">pressure</span> processing on the <span class="hlt">profile</span> of polyglutamyl 5-methyltetrahydrofolate in selected vegetables.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Wang, Chao; Riedl, Ken M; Somerville, Jeremy; Balasubramaniam, V M; Schwartz, Steven J</p> <p>2011-08-24</p> <p>In plants, folate occurs predominantly as 5-methyltetrahydrofolate (5MTHF) polyglutamyl forms. Differences in stability and bioavailability of food folate compared to synthetic folic acid have been attributed to the presence of the polyglutamyl chain. High-<span class="hlt">pressure</span> processing (HPP) was tested for whether it might shorten polyglutamyl chains of 5MTHF species in fresh vegetables by enabling action of native γ-glutamylhydrolase (GGH). A validated ultrahigh-performance reversed-phase liquid chromatography-tandem mass spectrometry method using stable isotope as internal standard was applied for characterizing 5MTHF polyglutamyl <span class="hlt">profiles</span>. HPP conditions included 300, 450, and 600 MPa at 30 °C for 0 or 5 min, and vegetables were vacuum-packed before treatment. Investigated vegetables included cauliflower (Brassica oleracea), baby carrots (Daucus carota), and carrot greens (D. carota). HPP treatment caused conversion of polyglutamyl 5MTHF species to short-chain and monoglutamyl forms. Maximal conversion of polyglutamyl folate to monoglutamyl folate occurred at the highest <span class="hlt">pressure</span>/time combination investigated, 600 MPa/30 °C/5 min. Under this condition, cauliflower monoglutamyl folate increased nearly 4-fold, diglutamyl folate 32-fold, and triglutamyl folate 8-fold; carrot monoglutamyl increased 23-fold and diglutamyl 32-fold; and carrot greens monoglutamyl increased 2.5-fold and the diglutamyl form 19-fold. Although some folate degradation was <span class="hlt">observed</span> at certain intermediate HPP conditions, total 5MTHF folate was largely preserved at 600 MPa/5 min. Thus, HPP of raw vegetables is a feasible strategy for enhancing vegetable monoglutamate 5MTHF.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://ntrs.nasa.gov/search.jsp?R=19930036960&hterms=vertical+height&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D70%26Ntt%3Dvertical%2Bheight','NASA-TRS'); return false;" href="https://ntrs.nasa.gov/search.jsp?R=19930036960&hterms=vertical+height&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D70%26Ntt%3Dvertical%2Bheight"><span><span class="hlt">Observations</span> of height-dependent <span class="hlt">pressure</span>-perturbation structure of a strong mesoscale gravity wave</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Starr, David O'C.; Korb, C. L.; Schwemmer, Geary K.; Weng, Chi Y.</p> <p>1992-01-01</p> <p>Airborne <span class="hlt">observations</span> using a downward-looking, dual-frequency, near-infrared, differential absorption lidar system provide the first measurements of the height-dependent <span class="hlt">pressure</span>-perturbation field associated with a strong mesoscale gravity wave. A <span class="hlt">pressure</span>-perturbation amplitude of 3.5 mb was measured within the lowest 1.6 km of the atmosphere over a 52-km flight line. Corresponding vertical displacements of 250-500 m were inferred from lidar-<span class="hlt">observed</span> displacement of aerosol layers. Accounting for probable wave orientation, a horizontal wavelength of about 40 km was estimated. Satellite <span class="hlt">observations</span> reveal wave structure of a comparable scale in concurrent cirrus cloud fields over an extended area. Smaller-scale waves were also <span class="hlt">observed</span>. Local meteorological soundings are analyzed to confirm the existence of a suitable wave duct. Potential wave-generation mechanisms are examined and discussed. The large <span class="hlt">pressure</span>-perturbation wave is attributed to rapid amplification or possible wave breaking of a gravity wave as it propagated offshore and interacted with a very stable marine boundary layer capped by a strong shear layer.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/19930010629','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/19930010629"><span>Mars <span class="hlt">observer</span> radio science (MORS) <span class="hlt">observations</span> in polar regions</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Simpson, Richard A.</p> <p>1992-01-01</p> <p>MORS <span class="hlt">observations</span> will focus on two major areas of study: (1) the gravity field of Mars and its interpretation in terms of internal structure and history and (2) the structure of the atmosphere, with emphasis on both temperature-<span class="hlt">pressure</span> <span class="hlt">profiles</span> of the background atmosphere and small scale inhomogeneities resulting from turbulence. Scattering of cm wavelength radio signals from Mars' surface at highly oblique angles will also be studied during the primary mission; nongrazing scattering experiments may be possible during an extended mission. During the MORS primary mission, measurements of the spacecraft distance and velocity with respect to Earth based tracking stations will be used to develop models of the global gravity field. The improvement in knowledge of the gravity field will be especially evident in polar regions. The spatial and temporal coverage of atmospheric radio occultation measurements are determined by the geometry of the spacecraft orbit and the direction to the Earth. <span class="hlt">Profiles</span> of atmospheric temperature and <span class="hlt">pressure</span> will extend from the surface to altitudes of 50 to 70 km.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/27566166','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/27566166"><span><span class="hlt">Observability</span> of Plant Metabolic Networks Is Reflected in the Correlation of Metabolic <span class="hlt">Profiles</span>.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Schwahn, Kevin; Küken, Anika; Kliebenstein, Daniel J; Fernie, Alisdair R; Nikoloski, Zoran</p> <p>2016-10-01</p> <p>Understanding whether the functionality of a biological system can be characterized by measuring few selected components is key to targeted phenotyping techniques in systems biology. Methods from <span class="hlt">observability</span> theory have proven useful in identifying sensor components that have to be measured to obtain information about the entire system. Yet, the extent to which the data <span class="hlt">profiles</span> reflect the role of components in the <span class="hlt">observability</span> of the system remains unexplored. Here we first identify the sensor metabolites in the model plant Arabidopsis (Arabidopsis thaliana) by employing state-of-the-art genome-scale metabolic networks. By using metabolic data <span class="hlt">profiles</span> from a set of seven environmental perturbations as well as from natural variability, we demonstrate that the data <span class="hlt">profiles</span> of sensor metabolites are more correlated than those of nonsensor metabolites. This pattern was confirmed with in silico generated metabolic <span class="hlt">profiles</span> from a medium-size kinetic model of plant central carbon metabolism. Altogether, due to the small number of identified sensors, our study implies that targeted metabolite analyses may provide the vast majority of relevant information about plant metabolic systems. © 2016 American Society of Plant Biologists. All Rights Reserved.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017APS..DPPKI2003P','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017APS..DPPKI2003P"><span><span class="hlt">Observation</span> of a New High-<span class="hlt">Pressure</span> Solid Phase in Dynamically Compressed Aluminum</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Polsin, D. N.</p> <p>2017-10-01</p> <p>Aluminum is ideal for testing theoretical first-principles calculations because of the relative simplicity of its atomic structure. Density functional theory (DFT) calculations predict that Al transforms from an ambient-<span class="hlt">pressure</span>, face-centered-cubic (fcc) crystal to the hexagonal close-packed (hcp) and body-centered-cubic (bcc) structures as it is compressed. Laser-driven experiments performed at the University of Rochester's Laboratory for Laser Energetics and the National Ignition Facility (NIF) ramp compressed Al samples to <span class="hlt">pressures</span> up to 540 GPa without melting. Nanosecond in-situ x-ray diffraction was used to directly measure the crystal structure at <span class="hlt">pressures</span> where the solid-solid phase transformations of Al are predicted to occur. Laser velocimetry provided the <span class="hlt">pressure</span> in the Al. Our results show clear evidence of the fcc-hcp and hpc-bcc transformations at 216 +/- 9 GPa and 321 +/- 12 GPa, respectively. This is the first experimental in-situ <span class="hlt">observation</span> of the bcc phase in compressed Al and a confirmation of the fcc-hcp transition previously <span class="hlt">observed</span> under static compression at 217 GPa. The <span class="hlt">observations</span> indicate these solid-solid phase transitions occur on the order of tens of nanoseconds time scales. In the fcc-hcp transition we find the original texture of the sample is preserved; however, the hcp-bcc transition diminishes that texture producing a structure that is more polycrystalline. The importance of this dynamic is discussed. The NIF results are the first demonstration of x-ray diffraction measurements at two different <span class="hlt">pressures</span> in a single laser shot. This material is based upon work supported by the Department of Energy National Nuclear Security Administration under Award Number DE-NA0001944.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2005AdAtS..22..936Z','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2005AdAtS..22..936Z"><span>Estimating the soil moisture <span class="hlt">profile</span> by assimilating near-surface <span class="hlt">observations</span> with the ensemble Kalman filter (EnKF)</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Zhang, Shuwen; Li, Haorui; Zhang, Weidong; Qiu, Chongjian; Li, Xin</p> <p>2005-11-01</p> <p>The paper investigates the ability to retrieve the true soil moisture <span class="hlt">profile</span> by assimilating near-surface soil moisture into a soil moisture model with an ensemble Kaiman filter (EnKF) assimilation scheme, including the effect of ensemble size, update interval and nonlinearities in the <span class="hlt">profile</span> retrieval, the required time for full retrieval of the soil moisture <span class="hlt">profiles</span>, and the possible influence of the depth of the soil moisture <span class="hlt">observation</span>. These questions are addressed by a desktop study using synthetic data. The “true” soil moisture <span class="hlt">profiles</span> are generated from the soil moisture model under the boundary condition of 0.5 cm d-1 evaporation. To test the assimilation schemes, the model is initialized with a poor initial guess of the soil moisture <span class="hlt">profile</span>, and different ensemble sizes are tested showing that an ensemble of 40 members is enough to represent the covariance of the model forecasts. Also compared are the results with those from the direct insertion assimilation scheme, showing that the EnKF is superior to the direct insertion assimilation scheme, for hourly <span class="hlt">observations</span>, with retrieval of the soil moisture <span class="hlt">profile</span> being achieved in 16 h as compared to 12 days or more. For daily <span class="hlt">observations</span>, the true soil moisture <span class="hlt">profile</span> is achieved in about 15 days with the EnKF, but it is impossible to approximate the true moisture within 18 days by using direct insertion. It is also found that <span class="hlt">observation</span> depth does not have a significant effect on <span class="hlt">profile</span> retrieval time for the EnKF. The nonlinearities have some negative influence on the optimal estimates of soil moisture <span class="hlt">profile</span> but not very seriously.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/14694451','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/14694451"><span><span class="hlt">Observations</span> on the function of the female urethra: II: Relation between maximum urethral closure <span class="hlt">pressure</span> at rest and the degree of urethral incompetence.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Schick, Erik; Bertrand, Pierre E; Jolivet-Tremblay, Martine; Dupont, Charles; Tessier, Jocelyne</p> <p>2004-01-01</p> <p>To study the relation between maximum urethral closure <span class="hlt">pressure</span> (MUCP) at rest and the degree of urethral incompetence in the female. Two hundred fifty five patients aged 20 years or older, with stable bladders on multichannel urodynamics, without known neurological pathology, and with no previous history of pelvic or anti-incontinence surgery were included in the study. Resting urethral <span class="hlt">pressure</span> <span class="hlt">profile</span> (UPP) and the grade of urethral incompetence was registered. Mean age of the group was 45.6+/-12.7 years; mean MUCP was 62.7+/-28.5 cm of water. There was a statistically significant difference in the MUCP when the different grades of urethral incompetence were compared to each other, the higher grades being associated with a lower maximal closure <span class="hlt">pressure</span>. This study demonstrates that there is a highly significant relationship between MUCP and between all grades of urethral incompetence. This supports previous <span class="hlt">observations</span> that MUCP decreases when abdominal leak point <span class="hlt">pressure</span> (ALPP) is low and that this might be secondary to some mechanical failure in the <span class="hlt">pressure</span> transmission from the abdominal cavity to the urethra. Studies should never compare continent to incontinent cohorts without considering their ALPP because in doing so they are comparing groups that are functionally heterogeneous. Copyright 2003 Wiley-Liss, Inc.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2016AGUOSIS54A2373C','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2016AGUOSIS54A2373C"><span>Surface layer and bloom dynamics <span class="hlt">observed</span> with the Prince William Sound Autonomous <span class="hlt">Profiler</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Campbell, R. W.</p> <p>2016-02-01</p> <p>As part of a recent long term monitoring effort, deployments of a WETLabs Autonomous Moored <span class="hlt">Profiler</span> (AMP) began Prince William Sound (PWS) in 2013. The PWS AMP consists of a positively buoyant instrument frame, with a winch and associated electronics that <span class="hlt">profiles</span> the frame from a park depth (usually 55 m) to the surface by releasing and retrieving a thin UHMWPE tether; it generally conducts a daily cast and measures temperature, salinity, chlorophyll-a fluorescence, turbidity, and oxygen and nitrate concentrations. Upward and downward looking ADCPs are mounted on a float below the <span class="hlt">profiler</span>, and an in situ plankton imager is in development and will be installed in 2016. Autonomous <span class="hlt">profilers</span> are a relatively new technology, and early deployments experienced a number of failures from which valuable lessons may be learned. Nevertheless, an unprecedented time series of the seasonal biogeochemical procession in the surface waters coastal Gulf of Alaska was collected in 2014 and 2015. The northern Gulf of Alaska has experienced a widespread warm anomaly since early 2014, and surface layer temperature anomalies in PWS were strongly positive during winter 2014. The spring bloom <span class="hlt">observed</span> by the <span class="hlt">profiler</span> began 2-3 weeks earlier than average, with surface nitrate depleted by late April. Although surface temperatures were still above average in 2015, bloom timing was much later, with a short vigorous bloom in late April and a subsurface bloom in late May that coincided with significant nitrate drawdown. As well as the vernal blooms, wind-driven upwelling events lead to several small productivity pulses that were evident in changes in nitrate and oxygen concentrations, and chlorophyll-a fluorescence. As well as providing a mechanistic understanding of surface layer biogeochemistry, high frequency <span class="hlt">observations</span> such as these put historical <span class="hlt">observations</span> in context, and provide new insights into the scales of variability in the annual cycles of the surface ocean in the North</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2011AGUFM.S41E..01A','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2011AGUFM.S41E..01A"><span>Discriminating different type waves from <span class="hlt">pressure</span> and ground motion <span class="hlt">observation</span> in the seafloor by DONET cabled <span class="hlt">observation</span> network.</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Araki, E.; Kawaguchi, K.; Kaneda, Y.</p> <p>2011-12-01</p> <p>We developed and deployed seafloor cabled observatory called "Dense Ocean-floor Network for Earthquake and Tsunamis (DONET)" in the Nankai Trough, south of Japan. The main purpose of the DONET network is to <span class="hlt">observe</span> large earthquake such as Tonankai earthquake in the deployed seafloor and associate Tsunamis in real-time to help disaster mitigation, and as well to monitor inter-seismic crustal activities such as micro earthquakes, very low frequency earthquakes, and slower crustal deformation. In each DONET seafloor observatory, high-sensitive broadband set of instruments for seismic and seafloor <span class="hlt">pressure</span> monitoring, consisted from Guralp CMG3T broadband seismometer, Metrozet TSA100S accelerometer, Paroscientific 8B7000-2 <span class="hlt">pressure</span> gauge, a deep-sea differential <span class="hlt">pressure</span> gauge, a hydrophone, and a seawater thermometer, are installed. The density of seafloor observatories are 20 observatories distributed in 15-30 km interval which is optimized for monitoring of events in the plate boundary beneath the network. DONET may be regarded as a large-scale, high sensitive high density seismic array for monitoring teleseismic events in the Philippine Sea and the Pacific Ocean. The DONET seafloor observatories are situated in wide range of seafloor depth between 1800m and 4500m, from the seafloor basin about 50 km off Japanese Island through the slope of accerecionary prism to the deep trench axis 150 km off the coast, that may also regarded as a vertical array in the 4.5km thick ocean. This variation of depths helps identify T-phases from the array record. In data analysis, it is necessary to identify propagation mode of each <span class="hlt">observed</span> wave which may often be mixed together. In our design of DONET <span class="hlt">observation</span> system, we took care to help identification of seismic phase by obtaining both ground motion and seafloor <span class="hlt">pressure</span> in the same location. This is simply achieved by combining seafloor <span class="hlt">pressure</span> gauges and seismometer in a single observatory package, but care was taken to</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/29353355','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/29353355"><span>Cerebrospinal fluid biomarkers <span class="hlt">profile</span> of idiopathic normal <span class="hlt">pressure</span> hydrocephalus.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Schirinzi, Tommaso; Sancesario, Giulia Maria; Di Lazzaro, Giulia; D'Elia, Alessio; Imbriani, Paola; Scalise, Simona; Pisani, Antonio</p> <p>2018-04-01</p> <p>Idiopathic normal <span class="hlt">pressure</span> hydrocephalus (iNPH) is a disabling neurological disorder whose potential treatability is significantly limited by diagnostic uncertainty. In fact, typical clinical presentation occurs at late phases of disease, when CSF shunting could be ineffective. In recent years, measurement of different CSF proteins, whose concentration directly reflects neuropathological changes of CNS, has significantly improved both diagnostic timing and accuracy of neurodegenerative disease. Unfortunately iNPH lacks neuropathological hallmarks allowing the identification of specific disease biomarkers. However, neuropathology of iNPH is so rich and heterogeneous that many processes can be tracked in CSF, including Alzheimer's disease core pathology, subcortical degeneration, neuroinflammation and vascular dysfunction. Indeed, a huge number of CSF biomarkers have been analyzed in iNPH patients, but a unifying <span class="hlt">profile</span> has not been provided yet. In this brief survey, we thus attempted to summarize the main findings in the field of iNPH CSF biomarkers, aimed at outlining a synthetic model. Although defined cut-off values for biomarkers are not available, a better knowledge of CSF characteristics may definitely assist in diagnosing the disease.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2018MSSP..106..249Z','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2018MSSP..106..249Z"><span>Clutch <span class="hlt">pressure</span> estimation for a power-split hybrid transmission using nonlinear robust <span class="hlt">observer</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Zhou, Bin; Zhang, Jianwu; Gao, Ji; Yu, Haisheng; Liu, Dong</p> <p>2018-06-01</p> <p>For a power-split hybrid transmission, using the brake clutch to realize the transition from electric drive mode to hybrid drive mode is an available strategy. Since the <span class="hlt">pressure</span> information of the brake clutch is essential for the mode transition control, this research designs a nonlinear robust reduced-order <span class="hlt">observer</span> to estimate the brake clutch <span class="hlt">pressure</span>. Model uncertainties or disturbances are considered as additional inputs, thus the <span class="hlt">observer</span> is designed in order that the error dynamics is input-to-state stable. The nonlinear characteristics of the system are expressed as the lookup tables in the <span class="hlt">observer</span>. Moreover, the gain matrix of the <span class="hlt">observer</span> is solved by two optimization procedures under the constraints of the linear matrix inequalities. The proposed <span class="hlt">observer</span> is validated by offline simulation and online test, the results have shown that the <span class="hlt">observer</span> achieves significant performance during the mode transition, as the estimation error is within a reasonable range, more importantly, it is asymptotically stable.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017AGUFM.S51E..08B','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017AGUFM.S51E..08B"><span>New Laboratory <span class="hlt">Observations</span> of Thermal <span class="hlt">Pressurization</span> Weakening</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Badt, N.; Tullis, T. E.; Hirth, G.</p> <p>2017-12-01</p> <p>Dynamic frictional weakening due to pore fluid thermal <span class="hlt">pressurization</span> has been studied under elevated confining <span class="hlt">pressure</span> in the laboratory, using a rotary-shear apparatus having a sample with independent pore <span class="hlt">pressure</span> and confining <span class="hlt">pressure</span> systems. Thermal <span class="hlt">pressurization</span> is directly controlled by the permeability of the rocks, not only for the initiation of high-speed frictional weakening but also for a subsequent sequence of high-speed sliding events. First, the permeability is evaluated at different effective <span class="hlt">pressures</span> using a method where the pore <span class="hlt">pressure</span> drop and the flow-through rate are compared using Darcy's Law as well as a pore fluid oscillation method, the latter method also permitting measurement of the storage capacity. Then, the samples undergo a series of high-speed frictional sliding segments at a velocity of 2.5 mm/s, under an applied confining <span class="hlt">pressure</span> and normal stress of 45 MPa and 50 MPa, respectively, and an initial pore <span class="hlt">pressure</span> of 25 MPa. Finally the rock permeability and storage capacity are measured again to assess the evolution of the rock's pore fluid properties. For samples with a permeability of 10-20 m2 thermal <span class="hlt">pressurization</span> promotes a 40% decrease in strength. However, after a sequence of three high-speed sliding events, the magnitude of weakening diminishes progressively from 40% to 15%. The weakening events coincide with dilation of the sliding interface. Moreover, the decrease in the weakening degree with progressive fast-slip events suggest that the hydraulic diffusivity may increase locally near the sliding interface during thermal <span class="hlt">pressurization</span>-enhanced slip. This could result from stress- or thermally-induced damage to the host rock, which would perhaps increase both permeability and storage capacity, and so possibly decrease the susceptibility of dynamic weakening due to thermal <span class="hlt">pressurization</span> in subsequent high-speed sliding events.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017ApJ...849L...6T','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017ApJ...849L...6T"><span>Halo <span class="hlt">Pressure</span> <span class="hlt">Profile</span> through the Skew Cross-power Spectrum of the Sunyaev-Zel’dovich Effect and CMB Lensing in Planck</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Timmons, Nicholas; Cooray, Asantha; Feng, Chang; Keating, Brian</p> <p>2017-11-01</p> <p>We measure the cosmic microwave background (CMB) skewness power spectrum in Planck, using frequency maps of the HFI instrument and the Sunyaev-Zel’dovich (SZ) component map. The two-to-one skewness power spectrum measures the cross-correlation between CMB lensing and the thermal SZ effect. We also directly measure the same cross-correlation using the Planck CMB lensing map and the SZ map and compare it to the cross-correlation derived from the skewness power spectrum. We model fit the SZ power spectrum and CMB lensing-SZ cross-power spectrum via the skewness power spectrum to constrain the gas <span class="hlt">pressure</span> <span class="hlt">profile</span> of dark matter halos. The gas <span class="hlt">pressure</span> <span class="hlt">profile</span> is compared to existing measurements in the literature including a direct estimate based on the stacking of SZ clusters in Planck.</p> </li> </ol> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_5");'>5</a></li> <li><a href="#" onclick='return showDiv("page_6");'>6</a></li> <li class="active"><span>7</span></li> <li><a href="#" onclick='return showDiv("page_8");'>8</a></li> <li><a href="#" onclick='return showDiv("page_9");'>9</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div><!-- col-sm-12 --> </div><!-- row --> </div><!-- page_7 --> <div id="page_8" class="hiddenDiv"> <div class="row"> <div class="col-sm-12"> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_6");'>6</a></li> <li><a href="#" onclick='return showDiv("page_7");'>7</a></li> <li class="active"><span>8</span></li> <li><a href="#" onclick='return showDiv("page_9");'>9</a></li> <li><a href="#" onclick='return showDiv("page_10");'>10</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div> </div> <div class="row"> <div class="col-sm-12"> <ol class="result-class" start="141"> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017EGUGA..19.6740C','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017EGUGA..19.6740C"><span>A New Quality Control Method base on IRMCD for Wind <span class="hlt">Profiler</span> <span class="hlt">Observation</span> towards Future Assimilation Application</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Chen, Min; Zhang, Yu</p> <p>2017-04-01</p> <p>A wind <span class="hlt">profiler</span> network with a total of 65 <span class="hlt">profiling</span> radars was operated by the MOC/CMA in China until July 2015. In this study, a quality control procedure is constructed to incorporate the <span class="hlt">profiler</span> data from the wind-<span class="hlt">profiling</span> network into the local data assimilation and forecasting system (BJRUC). The procedure applies a blacklisting check that removes stations with gross errors and an outlier check that rejects data with large deviations from the background. Instead of the bi-weighting method, which has been commonly implemented in outlier elimination for one-dimensional scalar <span class="hlt">observations</span>, an outlier elimination method is developed based on the iterated reweighted minimum covariance determinant (IRMCD) for multi-variate <span class="hlt">observations</span> such as wind <span class="hlt">profiler</span> data. A quality control experiment is separately performed for subsets containing <span class="hlt">profiler</span> data tagged in parallel with/without rain flags at every 00UTC/12UTC from 20 June to 30 Sep 2015. From the results, we find that with the quality control, the frequency distributions of the differences between the <span class="hlt">observations</span> and model background become more Gaussian-like and meet the requirements of a Gaussian distribution for data assimilation. Further intensive assessment for each quality control step reveals that the stations rejected by blacklisting contain poor data quality, and the IRMCD rejects outliers in a robust and physically reasonable manner.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://www.dtic.mil/docs/citations/ADA258842','DTIC-ST'); return false;" href="http://www.dtic.mil/docs/citations/ADA258842"><span>Application of the Program <span class="hlt">Profile</span> for the Design of Low-Speed, Low- <span class="hlt">Observable</span> Configuration Airfoils</span></a></p> <p><a target="_blank" href="http://www.dtic.mil/">DTIC Science & Technology</a></p> <p></p> <p>1992-12-01</p> <p>112 61 . Airfoil T503 - t/c = 3.79% .... ........... .. 113 62. Airfoil T503 Leading-Edge - t/c = 3.79% ..... ... 114 63. <span class="hlt">Pressure</span>...points on C unit circle, 6 slope of airfoil surface near trailing edge 61 boundary-layer displacement thickness 62 boundary-layer momentum thickness 63...equivalent thickness NACA 4-digit airfoils . 4 II. Theory Potential-Flow Design Method This section will overview the basic theory used in <span class="hlt">PROFILE</span>. Eppler</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/1998JPCRD..27.1217D','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/1998JPCRD..27.1217D"><span>The <span class="hlt">Observed</span> Properties of Liquid Helium at the Saturated Vapor <span class="hlt">Pressure</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Donnelly, Russell J.; Barenghi, Carlo F.</p> <p>1998-11-01</p> <p>The equilibrium and transport properties of liquid 4He are deduced from experimental <span class="hlt">observations</span> at the saturated vapor <span class="hlt">pressure</span>. In each case, the bibliography lists all known measurements. Quantities reported here include density, thermal expansion coefficient, dielectric constant, superfluid and normal fluid densities, first, second, third, and fourth sound velocities, specific heat, enthalpy, entropy, surface tension, ion mobilities, mutual friction, viscosity and kinematic viscosity, dispersion curve, structure factor, thermal conductivity, latent heat, saturated vapor <span class="hlt">pressure</span>, thermal diffusivity and Prandtl number of helium I, and displacement length and vortex core parameter in helium II.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017MNRAS.467.3827P','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017MNRAS.467.3827P"><span><span class="hlt">Pressure</span> of the hot gas in simulations of galaxy clusters</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Planelles, S.; Fabjan, D.; Borgani, S.; Murante, G.; Rasia, E.; Biffi, V.; Truong, N.; Ragone-Figueroa, C.; Granato, G. L.; Dolag, K.; Pierpaoli, E.; Beck, A. M.; Steinborn, Lisa K.; Gaspari, M.</p> <p>2017-06-01</p> <p>We analyse the radial <span class="hlt">pressure</span> <span class="hlt">profiles</span>, the intracluster medium (ICM) clumping factor and the Sunyaev-Zel'dovich (SZ) scaling relations of a sample of simulated galaxy clusters and groups identified in a set of hydrodynamical simulations based on an updated version of the treepm-SPH GADGET-3 code. Three different sets of simulations are performed: the first assumes non-radiative physics, the others include, among other processes, active galactic nucleus (AGN) and/or stellar feedback. Our results are analysed as a function of redshift, ICM physics, cluster mass and cluster cool-coreness or dynamical state. In general, the mean <span class="hlt">pressure</span> <span class="hlt">profiles</span> obtained for our sample of groups and clusters show a good agreement with X-ray and SZ <span class="hlt">observations</span>. Simulated cool-core (CC) and non-cool-core (NCC) clusters also show a good match with real data. We obtain in all cases a small (if any) redshift evolution of the <span class="hlt">pressure</span> <span class="hlt">profiles</span> of massive clusters, at least back to z = 1. We find that the clumpiness of gas density and <span class="hlt">pressure</span> increases with the distance from the cluster centre and with the dynamical activity. The inclusion of AGN feedback in our simulations generates values for the gas clumping (√{C}_{ρ }˜ 1.2 at R200) in good agreement with recent <span class="hlt">observational</span> estimates. The simulated YSZ-M scaling relations are in good accordance with several <span class="hlt">observed</span> samples, especially for massive clusters. As for the scatter of these relations, we obtain a clear dependence on the cluster dynamical state, whereas this distinction is not so evident when looking at the subsamples of CC and NCC clusters.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=3850051','PMC'); return false;" href="https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=3850051"><span>Influence of High-<span class="hlt">Pressure</span> Processing on the <span class="hlt">Profile</span> of Polyglutamyl 5-Methyltetrahydrofolate in Selected Vegetables</span></a></p> <p><a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pmc">PubMed Central</a></p> <p>Wang, Chao; Riedl, Ken M.; Somerville, Jeremy; Balasubramaniam, V. M.; Schwartz, Steven J.</p> <p>2013-01-01</p> <p>In plants, folate occurs predominantly as 5-methyltetrahydrofolate (5MTHF) polyglutamyl forms. Differences in stability and bioavailability of food folate compared to synthetic folic acid have been attributed to the presence of the polyglutamyl chain. High-<span class="hlt">pressure</span> processing (HPP) was tested for whether it might shorten polyglutamyl chains of 5MTHF species in fresh vegetables by enabling action of native γ-glutamylhydrolase (GGH). A validated ultrahigh-performance reversed-phase liquid chromatography–tandem mass spectrometry method using stable isotope as internal standard was applied for characterizing 5MTHF polyglutamyl <span class="hlt">profiles</span>. HPP conditions included 300, 450, and 600 MPa at 30 °C for 0 or 5 min, and vegetables were vacuum-packed before treatment. Investigated vegetables included cauliflower (Brassica oleracea), baby carrots (Daucus carota), and carrot greens (D. carota). HPP treatment caused conversion of polyglutamyl 5MTHF species to short-chain and monoglutamyl forms. Maximal conversion of polyglutamyl folate to monoglutamyl folate occurred at the highest <span class="hlt">pressure</span>/time combination investigated, 600 MPa/30 °C/5 min. Under this condition, cauliflower monoglutamyl folate increased nearly 4-fold, diglutamyl folate 32-fold, and triglutamyl folate 8-fold; carrot monoglutamyl increased 23-fold and diglutamyl 32-fold; and carrot greens monoglutamyl increased 2.5-fold and the diglutamyl form 19-fold. Although some folate degradation was <span class="hlt">observed</span> at certain intermediate HPP conditions, total 5MTHF folate was largely preserved at 600 MPa/5 min. Thus, HPP of raw vegetables is a feasible strategy for enhancing vegetable monoglutamate 5MTHF. PMID:21770413</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/20180001126','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/20180001126"><span>High Temporal Resolution Tropospheric Wind <span class="hlt">Profile</span> <span class="hlt">Observations</span> at NASA Kennedy Space Center During Hurricane Irma</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Decker, Ryan K.; Barbre, Robert E., Jr.; Huddleston, Lisa; Brauer, Thomas; Wilfong, Timothy</p> <p>2018-01-01</p> <p>The NASA Kennedy Space Center (KSC) operates a 48-MHz Tropospheric/Stratospheric Doppler Radar Wind <span class="hlt">Profiler</span> (TDRWP) on a continual basis generating wind <span class="hlt">profiles</span> between 2-19 km in the support of space launch vehicle operations. A benefit of the continual operability of the system is the ability to provide unique <span class="hlt">observations</span> of severe weather events such as hurricanes. Over the past two Atlantic Hurricane seasons the TDRWP has made high temporal resolution wind <span class="hlt">profile</span> <span class="hlt">observations</span> of Hurricane Irma in 2017 and Hurricane Matthew in 2016. Hurricane Irma was responsible for power outages to approximately 2/3 of Florida's population during its movement over the state(Stein,2017). An overview of the TDRWP system configuration, brief summary of Hurricanes Irma and Matthew storm track in proximity to KSC, characteristics of the tropospheric wind <span class="hlt">observations</span> from the TDRWP during both events, and discussion of the dissemination of TDRWP data during the event will be presented.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/26545653','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/26545653"><span>[LEVELS OF OBESITY, METABOLIC <span class="hlt">PROFILE</span>, CONSUMPTION OF TABACO AND BLOOD <span class="hlt">PRESSURE</span> IN SEDENTARY YOUTHS].</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Caamaño Navarrete, Felipe; Alarcón Hormazábal, Manuel; Delgado Floody, Pedro</p> <p>2015-11-01</p> <p>in Chile, the National Health Survey (ENS) conducted in 2009-2010 reported high prevalence of overweight, sedentary lifestyle, high cholesterol and metabolic syndrome in the population. to determine the prevalence in young sedentary obesity and consumption of tabaco and analyze their association with the metabolic <span class="hlt">profile</span>, body fat percentage and blood <span class="hlt">pressure</span>. 125 young sedentary, 26 men and 99 women, aged between 17 and 29 years old were evaluated. Body mass index (BMI), percent body fat (% fat), waist contour (CC), systolic and diastolic blood <span class="hlt">pressure</span>, total cholesterol, HDL cholesterol (HDL-C), LDL cholesterol (LDL-C), triglycerides: measurements were performed, glycemia and consumption of snuff. HDL-C (p = 0.000) and% MG (p = 0.043) were higher in women. 37.6% of young people turned smoker. 35, 2% of the sample showed excessive malnutrition. Obese subjects had higher levels: waist contour (p = 0.000) and% FM (p = 0.000). When analyzing obesity DC, this showed significant differences in BMI,% fat, systolic and diastolic blood <span class="hlt">pressure</span>. BMI presented positive association with CC,% fat, total cholesterol, triglycerides, LDL, systolic and diastolic blood <span class="hlt">pressure</span> (p < 0.05). The CC presented association with MG%, triglycerides, systolic blood <span class="hlt">pressure</span> and diastolic (p < 0.05). The MG% did not present association with other variables a high prevalence of malnutrition by excess consumption of tabaco in the study sample, while other variables are not high-risk categories, it is an opportune time to intervene and reverse these negative health trends now. Copyright AULA MEDICA EDICIONES 2014. Published by AULA MEDICA. All rights reserved.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=3303806','PMC'); return false;" href="https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=3303806"><span><span class="hlt">Observation</span> of Live Ticks (Haemaphysalis flava) by Scanning Electron Microscopy under High Vacuum <span class="hlt">Pressure</span></span></a></p> <p><a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pmc">PubMed Central</a></p> <p>Ishigaki, Yasuhito; Nakamura, Yuka; Oikawa, Yosaburo; Yano, Yasuhiro; Kuwabata, Susumu; Nakagawa, Hideaki; Tomosugi, Naohisa; Takegami, Tsutomu</p> <p>2012-01-01</p> <p>Scanning electron microscopes (SEM), which image sample surfaces by scanning with an electron beam, are widely used for steric <span class="hlt">observations</span> of resting samples in basic and applied biology. Various conventional methods exist for SEM sample preparation. However, conventional SEM is not a good tool to <span class="hlt">observe</span> living organisms because of the associated exposure to high vacuum <span class="hlt">pressure</span> and electron beam radiation. Here we attempted SEM <span class="hlt">observations</span> of live ticks. During 1.5×10−3 Pa vacuum <span class="hlt">pressure</span> and electron beam irradiation with accelerated voltages (2–5 kV), many ticks remained alive and moved their legs. After 30-min <span class="hlt">observation</span>, we removed the ticks from the SEM stage; they could walk actively under atmospheric <span class="hlt">pressure</span>. When we tested 20 ticks (8 female adults and 12 nymphs), they survived for two days after SEM <span class="hlt">observation</span>. These results indicate the resistance of ticks against SEM <span class="hlt">observation</span>. Our second survival test showed that the electron beam, not vacuum conditions, results in tick death. Moreover, we describe the reaction of their legs to electron beam exposure. These findings open the new possibility of SEM <span class="hlt">observation</span> of living organisms and showed the resistance of living ticks to vacuum condition in SEM. These data also indicate, for the first time, the usefulness of tick as a model system for biology under extreme condition. PMID:22431980</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.osti.gov/pages/biblio/1393192-improved-observations-turbulence-dissipation-rates-from-wind-profiling-radars','SCIGOV-DOEP'); return false;" href="https://www.osti.gov/pages/biblio/1393192-improved-observations-turbulence-dissipation-rates-from-wind-profiling-radars"><span>Improved <span class="hlt">observations</span> of turbulence dissipation rates from wind <span class="hlt">profiling</span> radars</span></a></p> <p><a target="_blank" href="http://www.osti.gov/pages">DOE PAGES</a></p> <p>McCaffrey, Katherine; Bianco, Laura; Wilczak, James M.</p> <p>2017-07-20</p> <p><span class="hlt">Observations</span> of turbulence dissipation rates in the planetary boundary layer are crucial for validation of parameterizations in numerical weather prediction models. However, because dissipation rates are difficult to obtain, they are infrequently measured through the depth of the boundary layer. For this reason, demonstrating the ability of commonly used wind <span class="hlt">profiling</span> radars (WPRs) to estimate this quantity would be greatly beneficial. During the XPIA field campaign at the Boulder Atmospheric Observatory, two WPRs operated in an optimized configuration, using high spectral resolution for increased accuracy of Doppler spectral width, specifically chosen to estimate turbulence from a vertically pointing beam. Multiplemore » post-processing techniques, including different numbers of spectral averages and peak processing algorithms for calculating spectral moments, were evaluated to determine the most accurate procedures for estimating turbulence dissipation rates using the information contained in the Doppler spectral width, using sonic anemometers mounted on a 300 m tower for validation. Furthermore, the optimal settings were determined, producing a low bias, which was later corrected. Resulting estimations of turbulence dissipation rates correlated well ( R 2 = 0.54 and 0.41) with the sonic anemometers, and <span class="hlt">profiles</span> up to 2 km from the 449 MHz WPR and 1 km from the 915 MHz WPR were <span class="hlt">observed</span>.« less</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.osti.gov/servlets/purl/1393192','SCIGOV-STC'); return false;" href="https://www.osti.gov/servlets/purl/1393192"><span>Improved <span class="hlt">observations</span> of turbulence dissipation rates from wind <span class="hlt">profiling</span> radars</span></a></p> <p><a target="_blank" href="http://www.osti.gov/search">DOE Office of Scientific and Technical Information (OSTI.GOV)</a></p> <p>McCaffrey, Katherine; Bianco, Laura; Wilczak, James M.</p> <p></p> <p><span class="hlt">Observations</span> of turbulence dissipation rates in the planetary boundary layer are crucial for validation of parameterizations in numerical weather prediction models. However, because dissipation rates are difficult to obtain, they are infrequently measured through the depth of the boundary layer. For this reason, demonstrating the ability of commonly used wind <span class="hlt">profiling</span> radars (WPRs) to estimate this quantity would be greatly beneficial. During the XPIA field campaign at the Boulder Atmospheric Observatory, two WPRs operated in an optimized configuration, using high spectral resolution for increased accuracy of Doppler spectral width, specifically chosen to estimate turbulence from a vertically pointing beam. Multiplemore » post-processing techniques, including different numbers of spectral averages and peak processing algorithms for calculating spectral moments, were evaluated to determine the most accurate procedures for estimating turbulence dissipation rates using the information contained in the Doppler spectral width, using sonic anemometers mounted on a 300 m tower for validation. Furthermore, the optimal settings were determined, producing a low bias, which was later corrected. Resulting estimations of turbulence dissipation rates correlated well ( R 2 = 0.54 and 0.41) with the sonic anemometers, and <span class="hlt">profiles</span> up to 2 km from the 449 MHz WPR and 1 km from the 915 MHz WPR were <span class="hlt">observed</span>.« less</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2016AtmEn.147..133F','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2016AtmEn.147..133F"><span>Variability of O3 and NO2 <span class="hlt">profile</span> shapes during DISCOVER-AQ: Implications for satellite <span class="hlt">observations</span> and comparisons to model-simulated <span class="hlt">profiles</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Flynn, Clare Marie; Pickering, Kenneth E.; Crawford, James H.; Weinheimer, Andrew J.; Diskin, Glenn; Thornhill, K. Lee; Loughner, Christopher; Lee, Pius; Strode, Sarah A.</p> <p>2016-12-01</p> <p>To investigate the variability of in situ <span class="hlt">profile</span> shapes under a variety of meteorological and pollution conditions, results are presented of an agglomerative hierarchical cluster analysis of the in situ O3 and NO2 <span class="hlt">profiles</span> for each of the four campaigns of the NASA DISCOVER-AQ mission. Understanding the <span class="hlt">observed</span> <span class="hlt">profile</span> variability for these trace gases is useful for understanding the accuracy of the assumed <span class="hlt">profile</span> shapes used in satellite retrieval algorithms as well as for understanding the correlation between satellite column <span class="hlt">observations</span> and surface concentrations. The four campaigns of the DISCOVER-AQ mission took place in Maryland during July 2011, the San Joaquin Valley of California during January-February 2013, the Houston, Texas, metropolitan region during September 2013, and the Denver-Front Range region of Colorado during July-August 2014. Several distinct <span class="hlt">profile</span> clusters emerged for the California, Texas, and Colorado campaigns for O3, indicating significant variability of O3 <span class="hlt">profile</span> shapes, while the Maryland campaign presented only one distinct O3 cluster. In contrast, very few distinct <span class="hlt">profile</span> clusters emerged for NO2 during any campaign for this particular clustering technique, indicating the NO2 <span class="hlt">profile</span> behavior was relatively uniform throughout each campaign. However, changes in NO2 <span class="hlt">profile</span> shape were evident as the boundary layer evolved through the day, but they were apparently not significant enough to yield more clusters. The degree of vertical mixing (as indicated by temperature lapse rate) associated with each cluster exerted an important influence on the shapes of the median cluster <span class="hlt">profiles</span> for O3, as well as impacted the correlations between the associated column and surface data for each cluster for O3. The correlation analyses suggest satellites may have the best chance to relate to surface O3 under the conditions encountered during the Maryland campaign Clusters 1 and 2, which include deep, convective boundary layers and few</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.osti.gov/biblio/22654360-halo-pressure-profile-through-skew-cross-power-spectrum-sunyaevzeldovich-effect-cmb-lensing-planck','SCIGOV-STC'); return false;" href="https://www.osti.gov/biblio/22654360-halo-pressure-profile-through-skew-cross-power-spectrum-sunyaevzeldovich-effect-cmb-lensing-planck"><span>Halo <span class="hlt">Pressure</span> <span class="hlt">Profile</span> through the Skew Cross-power Spectrum of the Sunyaev–Zel’dovich Effect and CMB Lensing in Planck</span></a></p> <p><a target="_blank" href="http://www.osti.gov/search">DOE Office of Scientific and Technical Information (OSTI.GOV)</a></p> <p>Timmons, Nicholas; Cooray, Asantha; Feng, Chang</p> <p>2017-11-01</p> <p>We measure the cosmic microwave background (CMB) skewness power spectrum in Planck , using frequency maps of the HFI instrument and the Sunyaev–Zel’dovich (SZ) component map. The two-to-one skewness power spectrum measures the cross-correlation between CMB lensing and the thermal SZ effect. We also directly measure the same cross-correlation using the Planck CMB lensing map and the SZ map and compare it to the cross-correlation derived from the skewness power spectrum. We model fit the SZ power spectrum and CMB lensing–SZ cross-power spectrum via the skewness power spectrum to constrain the gas <span class="hlt">pressure</span> <span class="hlt">profile</span> of dark matter halos. The gasmore » <span class="hlt">pressure</span> <span class="hlt">profile</span> is compared to existing measurements in the literature including a direct estimate based on the stacking of SZ clusters in Planck .« less</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/25796840','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/25796840"><span>[Changes of twenty-four-hour <span class="hlt">profile</span> blood <span class="hlt">pressure</span> and its correction of patients with arterial hypertension on the background of combined antihypertensive therapy application].</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Solomennchuk, T M; Slaba, N A; Prots'ko, V V; Bedzaĭ, A O</p> <p>2014-01-01</p> <p>The aim of this research was the study of efficiency and endurance antihypertensive therapy on the basis of fixed combination of enalapril and hydrochlorothiazide (HCTZ) and enalapril and HCTZ in combination with amlodipine according to the twenty-four-hour (? day-and-night) monitoring of blood <span class="hlt">pressure</span> (? 24H BPM) of patients with arterial hypertension (AH) 2-3 severity. The study included 33 patients with 2-3 grade of hypertension (average age--54,40 ± 3.45 years). All patients performed ? 24H BPM before treatment and after 12 weeks of therapy. The combination of enalapril and HCTZ allowed to achieve target levels of blood <span class="hlt">pressure</span> in 79% of patients, amlodipine additional purpose--in 86% of patients. We found that this therapy has a corrective effect on daily blood <span class="hlt">pressure</span> <span class="hlt">profile</span>, significantly reducing the load <span class="hlt">pressure</span> and blood <span class="hlt">pressure</span> variability. During treatment with the combination of enalapril and HCTZ combination of enalapril, HCTZ with amlodipine optimal daily <span class="hlt">profile</span> of blood <span class="hlt">pressure</span> after 12 weeks of reaching respectively 63.1% and 71.4% of patients. The treatment with combination of enalapril and HCTZ and adding of amlodipine is characterized by good endurance and high adherence to treatment.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=4125597','PMC'); return false;" href="https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=4125597"><span>The effect of baseline <span class="hlt">pressure</span> errors on an intracranial <span class="hlt">pressure</span>-derived index: results of a prospective <span class="hlt">observational</span> study</span></a></p> <p><a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pmc">PubMed Central</a></p> <p></p> <p>2014-01-01</p> <p>Background In order to characterize the intracranial <span class="hlt">pressure</span>-volume reserve capacity, the correlation coefficient (R) between the ICP wave amplitude (A) and the mean ICP level (P), the RAP index, has been used to improve the diagnostic value of ICP monitoring. Baseline <span class="hlt">pressure</span> errors (BPEs), caused by spontaneous shifts or drifts in baseline <span class="hlt">pressure</span>, cause erroneous readings of mean ICP. Consequently, BPEs could also affect ICP indices such as the RAP where in the mean ICP is incorporated. Methods A prospective, <span class="hlt">observational</span> study was carried out on patients with aneurysmal subarachnoid hemorrhage (aSAH) undergoing ICP monitoring as part of their surveillance. Via the same burr hole in the scull, two separate ICP sensors were placed close to each other. For each consecutive 6-sec time window, the dynamic mean ICP wave amplitude (MWA; measure of the amplitude of the single <span class="hlt">pressure</span> waves) and the static mean ICP, were computed. The RAP index was computed as the Pearson correlation coefficient between the MWA and the mean ICP for 40 6-sec time windows, i.e. every subsequent 4-min period (method 1). We compared this approach with a method of calculating RAP using a 4-min moving window updated every 6 seconds (method 2). Results The study included 16 aSAH patients. We compared 43,653 4-min RAP <span class="hlt">observations</span> of signals 1 and 2 (method 1), and 1,727,000 6-sec RAP <span class="hlt">observations</span> (method 2). The two methods of calculating RAP produced similar results. Differences in RAP ≥0.4 in at least 7% of <span class="hlt">observations</span> were seen in 5/16 (31%) patients. Moreover, the combination of a RAP of ≥0.6 in one signal and <0.6 in the other was seen in ≥13% of RAP-<span class="hlt">observations</span> in 4/16 (25%) patients, and in ≥8% in another 4/16 (25%) patients. The frequency of differences in RAP >0.2 was significantly associated with the frequency of BPEs (5 mmHg ≤ BPE <10 mmHg). Conclusions Simultaneous monitoring from two separate, close-by ICP sensors reveals significant differences in RAP that</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/19830002757','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/19830002757"><span>Wind-tunnel measurements of the chordwise <span class="hlt">pressure</span> distribution and <span class="hlt">profile</span> drag of a research airplane model incorporating a 17-percent-thick supercritical wing</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Ferris, J. C.</p> <p>1973-01-01</p> <p>The Langley 8-foot transonic <span class="hlt">pressure</span> tunnel to determine the wing chordwise <span class="hlt">pressure</span> distribution for a 0.09-scale model of a research airplane incorporating a 17-percent-thick supercritical wing. Airfoil <span class="hlt">profile</span> drag was determined from wake <span class="hlt">pressure</span> measurements at the 42-percent-semispan wing station. The investigation was conducted at Mach numbers from 0.30 to 0.80 over an angle-of-attack range sufficient to include buffet onset. The Reynolds number based on the mean geometric chord varied from 2 x 10 to the 6th power at Mach number 0.30 to 3.33 x 10 to the 6th power at Mach number 0.65 and was maintained at a constant value of 3.86 x 10 to the 6th power at Mach numbers from 0.70 to 0.80. <span class="hlt">Pressure</span> coefficients for four wing semispan stations and wing-section normal-force and pitching-moment coefficients for two semispan stations are presented in tabular form over the Mach number range from 0.30 to 0.80. Plotted chordwise <span class="hlt">pressure</span> distributions and wake <span class="hlt">profiles</span> are given for a selected range of section normal-force coefficients over the same Mach number range.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2005nrdd.conf....3A','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2005nrdd.conf....3A"><span>The AU Mic debris ring: density <span class="hlt">profile</span> and dynamics of the dust</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Augereau, Jean-Charles; Beust, Herve</p> <p>2005-10-01</p> <p>AU Mic is an M-type star surrounded by a debris disk that is viewed almost perfectly edge-on. This disk shares many common <span class="hlt">observational</span> properties with the well-known disk orbiting Beta Pictoris but the properties of the AU Mic disk as well as the dynamics of the dust grains have not been studied in detail yet. Using a standard deprojection technique, we derive the surface density <span class="hlt">profile</span> of the AU Mic disk from near-IR scattered light <span class="hlt">observations</span>. We show that irrespective of the asymmetry parameter of the phase function, most of the dust emission arises from a ring-like region that extends from 30 to 45 AU. We estimate that the mean collision time-scale at these distances is of the order of a few 10000 years. Therefore, collisional evolution can happen. A striking common feature between AU Mic and Beta Pic is the surface brightness <span class="hlt">profile</span>. In both cases, the surface brightness falls off as r^{-5} further away than 120 AU in the case of Beta Pic and 35 AU in the case of AU Mic. In the case of Beta Pic, this <span class="hlt">profile</span> is well explained by the combined effect of collisions and radiation <span class="hlt">pressure</span> on the smallest dust particules (e.g. Augereau et al. 2001). But this model does not apply to AU Mic because of its low luminosity (thus generating a too low radiation <span class="hlt">pressure</span>). Conversely, we show that a standard, solar-like stellar wind generates a drag force onto dust particles that behaves much like a radiation <span class="hlt">pressure</span>. This wind <span class="hlt">pressure</span> appears stronger than the radiation <span class="hlt">pressure</span> itself and this effect is considerably enhanced by the recurrent stellar flares of AU Mic. This greatly contributes to populating the extended debris disk of AU Mic and explains the similarity between the Beta Pic and AU Mic brightness <span class="hlt">profiles</span>.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2018PhRvF...3f3602B','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2018PhRvF...3f3602B"><span><span class="hlt">Observation</span> of the <span class="hlt">pressure</span> effect in simulations of droplets splashing on a dry surface</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Boelens, A. M. P.; Latka, A.; de Pablo, J. J.</p> <p>2018-06-01</p> <p>At atmospheric <span class="hlt">pressure</span>, a drop of ethanol impacting on a solid surface produces a splash. Reducing the ambient <span class="hlt">pressure</span> below its atmospheric value suppresses this splash. The origin of this so-called <span class="hlt">pressure</span> effect is not well understood, and this study presents an in-depth comparison between various theoretical models that aim to predict splashing and simulations. In this paper, the <span class="hlt">pressure</span> effect is explored numerically by resolving the Navier-Stokes equations at a 3-nm resolution. In addition to reproducing numerous experimental <span class="hlt">observations</span>, it is found that different models all provide elements of what is <span class="hlt">observed</span> in the simulations. The skating droplet model correctly predicts the existence and scaling of a gas film under the droplet, the lamella formation theory is able to correctly predict the scaling of the lamella ejection velocity as a function of the impact velocity for liquids with different viscosity, and lastly, the dewetting theory's hypothesis of a lift force acting on the liquid sheet after ejection is consistent with our results.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2009SASS...28...19D','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2009SASS...28...19D"><span>High Resolution Asteroid <span class="hlt">Profile</span> by Multi Chord Occultation <span class="hlt">Observations</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Degenhardt, Scott</p> <p>2009-05-01</p> <p>For millennia man has <span class="hlt">observed</span> celestial objects occulting other bodies and distant stars. We have used these celestial synchronicities to measure the properties of objects. On January 1, 1801 Italian astronomer Giusappe Piazzi discovered the first asteroid that would soon be named Ceres. To date 190,000 of these objects have been catalogued, but only a fraction of these have accurate measurements of their true size and shape. The International Occultation Timing Association (IOTA) currently facilitates the prediction and reduction of asteroidal occultations. By measuring the shadow cast on the earth by an asteroid during a stellar occultation one can directly measure the physical size, shape, and position in space of this body to accuracies orders of magnitudes better than the best ground based adaptive optics telescope and can provide verification to 3D inverted reflective lightcurve prediction models. Recent novel methods developed by IOTA involving an individual making multiple <span class="hlt">observations</span> through unattended remote <span class="hlt">observing</span> stations have made way for numerous chords of occultation measurement through a single body yielding high resolution <span class="hlt">profiles</span> of asteroid bodies. Methodology of how <span class="hlt">observing</span> stations are deployed will be demonstrated, results of some of these <span class="hlt">observations</span> are presented as comparisons to their inverted lightcurve are shown.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/19750007150','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/19750007150"><span>Uncertainties in derived temperature-height <span class="hlt">profiles</span></span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Minzner, R. A.</p> <p>1974-01-01</p> <p>Nomographs were developed for relating uncertainty in temperature T to uncertainty in the <span class="hlt">observed</span> height <span class="hlt">profiles</span> of both <span class="hlt">pressure</span> p and density rho. The relative uncertainty delta T/T is seen to depend not only upon the relative uncertainties delta P/P or delta rho/rho, and to a small extent upon the value of T or H, but primarily upon the sampling-height increment Delta h, the height increment between successive <span class="hlt">observations</span> of p or delta. For a fixed value of delta p/p, the value of delta T/T varies inversely with Delta h. No limit exists in the fineness of usable height resolution of T which may be derived from densities, while a fine height resolution in <span class="hlt">pressure</span>-height data leads to temperatures with unacceptably large uncertainties.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2013SPIE.8599E..1ZW','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2013SPIE.8599E..1ZW"><span><span class="hlt">Observation</span> of laser beam <span class="hlt">profile</span> progression inside an extended laser cavity</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Wu, Frank F.; Farrell, Thomas C.</p> <p>2013-03-01</p> <p>This report presents the result of the laser beam <span class="hlt">profile</span> progression in target-in-the-loop (TIL) system. This simulation experiment is to verify whether it is possible to form a tight hot spot similar to a single transversal mode in an extended laser cavity. Therefore, it is very important to <span class="hlt">observe</span> the progression of the laser <span class="hlt">profile</span> at a laser cavity mirror when a seeded high energy laser pulse is injected into the TIL system. The extended laser cavity is formed with a high reflectivity mirror on one end and an optical phase conjugated mirror as the second mirror, with potential disturbance media inside. The laser oscillation occurs only when it is triggered with a single frequency high energy laser pulse to overcome the threshold condition. With a laser cavity length of around 11 meters and a seeded laser pulse of 10 ns, we have been able to acquire and distinguish the laser beam <span class="hlt">profiles</span> of each round-trip. Inserting a scattering media and other distortion elements can simulate atmospheric effects.</p> </li> </ol> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_6");'>6</a></li> <li><a href="#" onclick='return showDiv("page_7");'>7</a></li> <li class="active"><span>8</span></li> <li><a href="#" onclick='return showDiv("page_9");'>9</a></li> <li><a href="#" onclick='return showDiv("page_10");'>10</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div><!-- col-sm-12 --> </div><!-- row --> </div><!-- page_8 --> <div id="page_9" class="hiddenDiv"> <div class="row"> <div class="col-sm-12"> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_7");'>7</a></li> <li><a href="#" onclick='return showDiv("page_8");'>8</a></li> <li class="active"><span>9</span></li> <li><a href="#" onclick='return showDiv("page_10");'>10</a></li> <li><a href="#" onclick='return showDiv("page_11");'>11</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div> </div> <div class="row"> <div class="col-sm-12"> <ol class="result-class" start="161"> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/26037903','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/26037903"><span>Tea, but not coffee consumption, is associated with components of arterial <span class="hlt">pressure</span>. The <span class="hlt">Observation</span> of Cardiovascular Risk Factors study in Luxembourg.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Alkerwi, Ala'a; Sauvageot, Nicolas; Crichton, Georgina E; Elias, Merrill F</p> <p>2015-07-01</p> <p>There is uncertainty regarding the impact of tea and coffee consumption on arterial blood <span class="hlt">pressure</span>. The present study aimed to examine the association between blood <span class="hlt">pressure</span> (BP) components, namely, systolic BP (SBP), diastolic BP, mean arterial <span class="hlt">pressure</span>, and pulse <span class="hlt">pressure</span> (PP), and tea or coffee consumption, taking into account simultaneous consumption. The study population was derived from a national cross-sectional stratified sample of 1352 individuals aged 18 to 69 years, recruited between November 2007 and January 2009 to participate in the <span class="hlt">Observation</span> of Cardiovascular Risk Factors in Luxembourg study. We hypothesized that greater tea consumption would be independently associated with lower BP. Tea and coffee consumptions in deciliters per day were obtained from a semiquantitative food frequency questionnaire. Participants were classified into 3 groups: nonconsumers, ≤3-dL/d consumers, and >3-dL/d consumers of each beverage separately. After exclusion of subjects taking antihypertensive medications, several general linear models were performed to investigate the independent relationship between tea/coffee consumption and BP components. Tea consumers (36.3%) were more likely to be younger women, nonsmokers, with better cardiometabolic <span class="hlt">profiles</span>, and less frequent chronic pathologies, whereas the reverse was true for coffee consumers (88%). Greater tea consumption was associated with lower SBP and PP values, after adjustment for age, sex, education, lifestyle, and dietary confounding factors, including coffee drinking. No association between BP components and coffee consumption was <span class="hlt">observed</span>. Daily consumption of 1 dL of tea was associated with a significant reduction of SBP by 0.6 mm Hg and PP by 0.5 mm Hg. Given the widespread consumption of tea and coffee throughout the world, together with the major cardiovascular disease risk, our findings have important implications for human health. Copyright © 2015 Elsevier Inc. All rights reserved.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://ntrs.nasa.gov/search.jsp?R=20050000547&hterms=power+healthy&qs=N%3D0%26Ntk%3DAll%26Ntx%3Dmode%2Bmatchall%26Ntt%3Dpower%2Bhealthy','NASA-TRS'); return false;" href="https://ntrs.nasa.gov/search.jsp?R=20050000547&hterms=power+healthy&qs=N%3D0%26Ntk%3DAll%26Ntx%3Dmode%2Bmatchall%26Ntt%3Dpower%2Bhealthy"><span>Hemodynamic and hormonal responses to lower body negative <span class="hlt">pressure</span> in men with varying <span class="hlt">profiles</span> of strength and aerobic power</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Convertino, V. A.; Mathes, K. L.; Lasley, M. L.; Tomaselli, C. M.; Frey, M. A.; Hoffler, G. W.</p> <p>1993-01-01</p> <p>Hemodynamic, cardiac, and hormonal responses to lower-body negative <span class="hlt">pressure</span> (LBNP) were examined in 24 healthy men to test the hypothesis that responsiveness of reflex control of blood <span class="hlt">pressure</span> during orthostatic challenge is associated with interactions between strength and aerobic power. Subjects underwent treadmill tests to determine peak oxygen uptake (VO2max) and isokinetic dynamometer tests to determine knee extensor strength. Based on predetermined criteria, subjects were classified into one of four fitness <span class="hlt">profiles</span> of six subjects each, matched for age, height, and body mass: (a) low strength/average aerobic fitness, (b) low strength/high aerobic fitness, (c) high strength/average aerobic fitness, and (d) high strength/high aerobic fitness. Following 90 min of 0.11 rad (6 degrees) head-down tilt (HDT), each subject underwent graded LBNP to -6.7 kPa or presyncope, with maximal duration 15 min, while hemodynamic, cardiac, and hormonal responses were measured. All groups exhibited typical hemodynamic, hormonal, and fluid shift responses during LBNP, with no intergroup differences between high and low strength characteristics. Subjects with high aerobic power exhibited greater (P < 0.05) stroke volume and lower (P < 0.05) heart rate, vascular peripheral resistance, and mean arterial <span class="hlt">pressure</span> during rest, HDT, and LBNP. Seven subjects, distributed among the four fitness <span class="hlt">profiles</span>, became presyncopal. These subjects showed greatest reduction in mean arterial <span class="hlt">pressure</span> during LBNP, had greater elevations in vasopressin, and lesser increases in heart rate and peripheral resistance. Neither VO2max nor leg strength were associated with fall in arterial <span class="hlt">pressure</span> or with syncopal episodes. We conclude that interactions between aerobic and strength fitness characteristics do not influence responses to LBNP challenge.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/20020091934','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/20020091934"><span>Retrieval of Precipitation <span class="hlt">Profiles</span> from Multiresolution, Multifrequency, Active and Passive Microwave <span class="hlt">Observations</span></span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Grecu, Mircea; Anagnostou, Emmanouil N.; Olson, William S.; Starr, David OC. (Technical Monitor)</p> <p>2002-01-01</p> <p>In this study, a technique for estimating vertical <span class="hlt">profiles</span> of precipitation from multifrequency, multiresolution active and passive microwave <span class="hlt">observations</span> is investigated using both simulated and airborne data. The technique is applicable to the Tropical Rainfall Measuring Mission (TRMM) satellite multi-frequency active and passive <span class="hlt">observations</span>. These <span class="hlt">observations</span> are characterized by various spatial and sampling resolutions. This makes the retrieval problem mathematically more difficult and ill-determined because the quality of information decreases with decreasing resolution. A model that, given reflectivity <span class="hlt">profiles</span> and a small set of parameters (including the cloud water content, the intercept drop size distribution, and a variable describing the frozen hydrometeor properties), simulates high-resolution brightness temperatures is used. The high-resolution simulated brightness temperatures are convolved at the real sensor resolution. An optimal estimation procedure is used to minimize the differences between simulated and <span class="hlt">observed</span> brightness temperatures. The retrieval technique is investigated using cloud model synthetic and airborne data from the Fourth Convection And Moisture Experiment. Simulated high-resolution brightness temperatures and reflectivities and airborne <span class="hlt">observation</span> strong are convolved at the resolution of the TRMM instruments and retrievals are performed and analyzed relative to the reference data used in <span class="hlt">observations</span> synthesis. An illustration of the possible use of the technique in satellite rainfall estimation is presented through an application to TRMM data. The study suggests improvements in combined active and passive retrievals even when the instruments resolutions are significantly different. Future work needs to better quantify the retrievals performance, especially in connection with satellite applications, and the uncertainty of the models used in retrieval.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2018MNRAS.475.1340F','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2018MNRAS.475.1340F"><span>Non-thermal <span class="hlt">pressure</span> in the outskirts of Abell 2142</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Fusco-Femiano, Roberto; Lapi, Andrea</p> <p>2018-03-01</p> <p>Clumping and turbulence are expected to affect the matter accreted on to the outskirts of galaxy clusters. To determine their impact on the thermodynamic properties of Abell 2142, we perform an analysis of the X-ray temperature data from XMM-Newton via our SuperModel, a state-of-the-art tool for investigating the astrophysics of the intracluster medium already tested on many individual clusters (since Cavaliere, Lapi & Fusco-Femiano 2009). Using the gas density <span class="hlt">profile</span> corrected for clumpiness derived by Tchernin et al. (2016), we find evidence for the presence of a non-thermal <span class="hlt">pressure</span> component required to sustain gravity in the cluster outskirts of Abell 2142, that amounts to about 30 per cent of the total <span class="hlt">pressure</span> at the virial radius. The presence of the non-thermal component implies the gas fraction to be consistent with the universal value at the virial radius and the electron thermal <span class="hlt">pressure</span> <span class="hlt">profile</span> to be in good agreement with that inferred from the SZ data. Our results indicate that the presence of gas clumping and of a non-thermal <span class="hlt">pressure</span> component are both necessary to recover the <span class="hlt">observed</span> physical properties in the cluster outskirts. Moreover, we stress that an alternative method often exploited in the literature (included Abell 2142) to determine the temperature <span class="hlt">profile</span> kBT = Pe/ne basing on a combination of the Sunyaev-Zel'dovich (SZ) <span class="hlt">pressure</span> Pe and of the X-ray electron density ne does not allow us to highlight the presence of non-thermal <span class="hlt">pressure</span> support in the cluster outskirts.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/29853430','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/29853430"><span>The association of the dietary approach to stop hypertension (DASH) diet with blood <span class="hlt">pressure</span>, glucose and lipid <span class="hlt">profiles</span> in Malaysian and Philippines populations.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Tiong, X T; Nursara Shahirah, A; Pun, V C; Wong, K Y; Fong, A Y Y; Sy, R G; Castillo-Carandang, N T; Nang, E E K; Woodward, M; van Dam, R M; Tai, E S; Venkataraman, K</p> <p>2018-05-07</p> <p>Despite a growing body of evidence from Western populations on the health benefits of Dietary Approaches to Stop Hypertension (DASH) diets, their applicability in South East Asian settings is not clear. We examined cross-sectional associations between DASH diet and cardio-metabolic risk factors among 1837 Malaysian and 2898 Philippines participants in a multi-national cohort. Blood <span class="hlt">pressures</span>, fasting lipid <span class="hlt">profile</span> and fasting glucose were measured, and DASH score was computed based on a 22-item food frequency questionnaire. Older individuals, women, those not consuming alcohol and those undertaking regular physical activity were more likely to have higher DASH scores. In the Malaysian cohort, while total DASH score was not significantly associated with cardio-metabolic risk factors after adjusting for confounders, significant associations were <span class="hlt">observed</span> for intake of green vegetable [0.011, standard error (SE): 0.004], and red and processed meat (-0.009, SE: 0.004) with total cholesterol. In the Philippines cohort, a 5-unit increase in total DASH score was significantly and inversely associated with systolic blood <span class="hlt">pressure</span> (-1.41, SE: 0.40), diastolic blood <span class="hlt">pressure</span> (-1.09, SE: 0.28), total cholesterol (-0.015, SE: 0.005), low-density lipoprotein cholesterol (-0.025, SE: 0.008), and triglyceride (-0.034, SE: 0.012) after adjusting for socio-demographic and lifestyle groups. Intake of milk and dairy products, red and processed meat, and sugared drinks were found to significantly associated with most risk factors. Differential associations of DASH diet and dietary components with cardio-metabolic risk factors by country suggest the need for country-specific tailoring of dietary interventions to improve cardio-metabolic risk <span class="hlt">profiles</span>. Copyright © 2018 The Italian Society of Diabetology, the Italian Society for the Study of Atherosclerosis, the Italian Society of Human Nutrition, and the Department of Clinical Medicine and Surgery, Federico II University. Published by</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=4431309','PMC'); return false;" href="https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=4431309"><span>Embedding Piezoresistive <span class="hlt">Pressure</span> Sensors to Obtain Online <span class="hlt">Pressure</span> <span class="hlt">Profiles</span> Inside Fiber Composite Laminates</span></a></p> <p><a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pmc">PubMed Central</a></p> <p>Kahali Moghaddam, Maryam; Breede, Arne; Brauner, Christian; Lang, Walter</p> <p>2015-01-01</p> <p>The production of large and complex parts using fiber composite materials is costly due to the frequent formation of voids, porosity and waste products. By embedding different types of sensors and monitoring the process in real time, the amount of wastage can be significantly reduced. This work focuses on developing a knowledge-based method to improve and ensure complete impregnation of the fibers before initiation of the resin cure. Piezoresistive and capacitive <span class="hlt">pressure</span> sensors were embedded in fiber composite laminates to measure the real-time the <span class="hlt">pressure</span> values inside the laminate. A change of <span class="hlt">pressure</span> indicates resin infusion. The sensors were placed in the laminate and the resin was infused by vacuum. The embedded piezoresistive <span class="hlt">pressure</span> sensors were able to track the vacuum <span class="hlt">pressure</span> in the fiber composite laminate setup, as well as the arrival of the resin at the sensor. The <span class="hlt">pressure</span> increase due to closing the resin inlet was also measured. In contrast, the capacitive type of sensor was found to be inappropriate for measuring these quantities. The following study demonstrates real-time monitoring of <span class="hlt">pressure</span> changes inside the fiber composite laminate, which validate the use of Darcy’s law in porous media to control the resin flow during infusion. PMID:25825973</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/25825973','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/25825973"><span>Embedding piezoresistive <span class="hlt">pressure</span> sensors to obtain online <span class="hlt">pressure</span> <span class="hlt">profiles</span> inside fiber composite laminates.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Moghaddam, Maryam Kahali; Breede, Arne; Brauner, Christian; Lang, Walter</p> <p>2015-03-27</p> <p>The production of large and complex parts using fiber composite materials is costly due to the frequent formation of voids, porosity and waste products. By embedding different types of sensors and monitoring the process in real time, the amount of wastage can be significantly reduced. This work focuses on developing a knowledge-based method to improve and ensure complete impregnation of the fibers before initiation of the resin cure. Piezoresistive and capacitive <span class="hlt">pressure</span> sensors were embedded in fiber composite laminates to measure the real-time the <span class="hlt">pressure</span> values inside the laminate. A change of <span class="hlt">pressure</span> indicates resin infusion. The sensors were placed in the laminate and the resin was infused by vacuum. The embedded piezoresistive <span class="hlt">pressure</span> sensors were able to track the vacuum <span class="hlt">pressure</span> in the fiber composite laminate setup, as well as the arrival of the resin at the sensor. The <span class="hlt">pressure</span> increase due to closing the resin inlet was also measured. In contrast, the capacitive type of sensor was found to be inappropriate for measuring these quantities. The following study demonstrates real-time monitoring of <span class="hlt">pressure</span> changes inside the fiber composite laminate, which validate the use of Darcy's law in porous media to control the resin flow during infusion.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/28516029','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/28516029"><span>The power of vertical geolocation of atmospheric <span class="hlt">profiles</span> from GNSS radio occultation.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Scherllin-Pirscher, Barbara; Steiner, Andrea K; Kirchengast, Gottfried; Schwärz, Marc; Leroy, Stephen S</p> <p>2017-02-16</p> <p>High-resolution measurements from Global Navigation Satellite System (GNSS) radio occultation (RO) provide atmospheric <span class="hlt">profiles</span> with independent information on altitude and <span class="hlt">pressure</span>. This unique property is of crucial advantage when analyzing atmospheric characteristics that require joint knowledge of altitude and <span class="hlt">pressure</span> or other thermodynamic atmospheric variables. Here we introduce and demonstrate the utility of this independent information from RO and discuss the computation, uncertainty, and use of RO atmospheric <span class="hlt">profiles</span> on isohypsic coordinates-mean sea level altitude and geopotential height-as well as on thermodynamic coordinates (<span class="hlt">pressure</span> and potential temperature). Using geopotential height as vertical grid, we give information on errors of RO-derived temperature, <span class="hlt">pressure</span>, and potential temperature <span class="hlt">profiles</span> and provide an empirical error model which accounts for seasonal and latitudinal variations. The <span class="hlt">observational</span> uncertainty of individual temperature/<span class="hlt">pressure</span>/potential temperature <span class="hlt">profiles</span> is about 0.7 K/0.15%/1.4 K in the tropopause region. It gradually increases into the stratosphere and decreases toward the lower troposphere. This decrease is due to the increasing influence of background information. The total climatological error of mean atmospheric fields is, in general, dominated by the systematic error component. We use sampling error-corrected climatological fields to demonstrate the power of having different and accurate vertical coordinates available. As examples we analyze characteristics of the location of the tropopause for geopotential height, <span class="hlt">pressure</span>, and potential temperature coordinates as well as seasonal variations of the midlatitude jet stream core. This highlights the broad applicability of RO and the utility of its versatile vertical geolocation for investigating the vertical structure of the troposphere and stratosphere.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://pubs.er.usgs.gov/publication/70020775','USGSPUBS'); return false;" href="https://pubs.er.usgs.gov/publication/70020775"><span>In situ <span class="hlt">observations</span> of a high-<span class="hlt">pressure</span> phase of H2O ice</span></a></p> <p><a target="_blank" href="http://pubs.er.usgs.gov/pubs/index.jsp?view=adv">USGS Publications Warehouse</a></p> <p>Chou, I.-Ming; Blank, J.G.; Goncharov, A.F.; Mao, Ho-kwang; Hemley, R.J.</p> <p>1998-01-01</p> <p>A previously unknown solid phase of H2O has been identified by its peculiar growth patterns, distinct <span class="hlt">pressure</span>-temperature melting relations, and vibrational Raman spectra. Morphologies of ice crystals and their <span class="hlt">pressure</span>-temperature melting relations were directly <span class="hlt">observed</span> in a hydrothermal diamond-anvil cell for H2O bulk densities between 1203 and 1257 kilograms per cubic meter at temperatures between -10??and 50??C. Under these conditions, four different ice forms were <span class="hlt">observed</span> to melt: two stable phases, ice V and ice VI, and two metastable phases, ice IV and the new ice phase. The Raman spectra and crystal morphology are consistent with a disordered anisotropic structure with some similarities to ice VI.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/27438965','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/27438965"><span>Reliability of transpulmonary <span class="hlt">pressure</span>-time curve <span class="hlt">profile</span> to identify tidal recruitment/hyperinflation in experimental unilateral pleural effusion.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Formenti, P; Umbrello, M; Graf, J; Adams, A B; Dries, D J; Marini, J J</p> <p>2017-08-01</p> <p>The stress index (SI) is a parameter that characterizes the shape of the airway <span class="hlt">pressure</span>-time <span class="hlt">profile</span> (P/t). It indicates the slope progression of the curve, reflecting both lung and chest wall properties. The presence of pleural effusion alters the mechanical properties of the respiratory system decreasing transpulmonary <span class="hlt">pressure</span> (Ptp). We investigated whether the SI computed using Ptp tracing would provide reliable insight into tidal recruitment/overdistention during the tidal cycle in the presence of unilateral effusion. Unilateral pleural effusion was simulated in anesthetized, mechanically ventilated pigs. Respiratory system mechanics and thoracic computed tomography (CT) were studied to assess P/t curve shape and changes in global lung aeration. SI derived from airway <span class="hlt">pressure</span> (Paw) was compared with that calculated by Ptp under the same conditions. These results were themselves compared with quantitative CT analysis as a gold standard for tidal recruitment/hyperinflation. Despite marked changes in tidal recruitment, mean values of SI computed either from Paw or Ptp were remarkably insensitive to variations of PEEP or condition. After the instillation of effusion, SI indicates a preponderant over-distension effect, not detected by CT. After the increment in PEEP level, the extent of CT-determined tidal recruitment suggest a huge recruitment effect of PEEP as reflected by lung compliance. Both SI in this case were unaffected. We showed that the ability of SI to predict tidal recruitment and overdistension was significantly reduced in a model of altered chest wall-lung relationship, even if the parameter was computed from the Ptp curve <span class="hlt">profile</span>.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://ntrs.nasa.gov/search.jsp?R=19950044670&hterms=atmospheric+pressure&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D50%26Ntt%3Datmospheric%2Bpressure','NASA-TRS'); return false;" href="https://ntrs.nasa.gov/search.jsp?R=19950044670&hterms=atmospheric+pressure&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D50%26Ntt%3Datmospheric%2Bpressure"><span>Stratospheric and mesospheric <span class="hlt">pressure</span>-temperature <span class="hlt">profiles</span> from rotational analysis of CO2 lines in atmospheric trace molecule spectroscopy/ATLAS 1 infrared solar occultation spectra</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Stiller, G. P.; Gunson, M. R.; Lowes, L. L.; Abrams, M. C.; Raper, O. F.; Farmer, C. B.; Zander, R.; Rinsland, C. P.</p> <p>1995-01-01</p> <p>A simple, classical, and expedient method for the retrieval of atmospheric <span class="hlt">pressure</span>-temperature <span class="hlt">profiles</span> has been applied to the high-resolution infrared solar absorption spectra obtained with the atmospheric trace molecule spectroscopy (ATMOS) instrument. The basis for this method is a rotational analysis of retrieved apparent abundances from CO2 rovibrational absorption lines, employing existing constituent concentration retrieval software used in the analysis of data returned by ATMOS. <span class="hlt">Pressure</span>-temperature <span class="hlt">profiles</span> derived from spectra acquired during the ATLAS 1 space shuttle mission of March-April 1992 are quantitatively evaluated and compared with climatological and meteorological data as a means of assessing the validity of this approach.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/24445083','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/24445083"><span>Reliability of laser Doppler flowmetry curve reading for measurement of toe and ankle <span class="hlt">pressures</span>: intra- and inter-<span class="hlt">observer</span> variation.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Høyer, C; Paludan, J P D; Pavar, S; Biurrun Manresa, J A; Petersen, L J</p> <p>2014-03-01</p> <p>To assess the intra- and inter-<span class="hlt">observer</span> variation in laser Doppler flowmetry curve reading for measurement of toe and ankle <span class="hlt">pressures</span>. A prospective single blinded diagnostic accuracy study was conducted on 200 patients with known or suspected peripheral arterial disease (PAD), with a total of 760 curve sets produced. The first curve reading for this study was performed by laboratory technologists blinded to clinical clues and previous readings at least 3 months after the primary data sampling. The <span class="hlt">pressure</span> curves were later reassessed following another period of at least 3 months. <span class="hlt">Observer</span> agreement in diagnostic classification according to TASC-II criteria was quantified using Cohen's kappa. Reliability was quantified using intra-class correlation coefficients, coefficients of variance, and Bland-Altman analysis. The overall agreement in diagnostic classification (PAD/not PAD) was 173/200 (87%) for intra-<span class="hlt">observer</span> (κ = .858) and 175/200 (88%) for inter-<span class="hlt">observer</span> data (κ = .787). Reliability analysis confirmed excellent correlation for both intra- and inter-<span class="hlt">observer</span> data (ICC all ≥.931). The coefficients of variance ranged from 2.27% to 6.44% for intra-<span class="hlt">observer</span> and 2.39% to 8.42% for inter-<span class="hlt">observer</span> data. Subgroup analysis showed lower <span class="hlt">observer</span>-variation for reading of toe <span class="hlt">pressures</span> in patients with diabetes and/or chronic kidney disease than patients not diagnosed with these conditions. Bland-Altman plots showed higher variation in toe <span class="hlt">pressure</span> readings than ankle <span class="hlt">pressure</span> readings. This study shows substantial intra- and inter-<span class="hlt">observer</span> agreement in diagnostic classification and reading of absolute <span class="hlt">pressures</span> when using laboratory technologists as <span class="hlt">observers</span>. The study emphasises that <span class="hlt">observer</span> variation for curve reading is an important factor concerning the overall reproducibility of the method. Our data suggest diabetes and chronic kidney disease have an influence on toe <span class="hlt">pressure</span> reproducibility. Copyright © 2013 European Society for Vascular Surgery. Published</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.osti.gov/biblio/5471333-copernicus-observations-pressures-carbon-abundances-diffuse-interstellar-clouds','SCIGOV-STC'); return false;" href="https://www.osti.gov/biblio/5471333-copernicus-observations-pressures-carbon-abundances-diffuse-interstellar-clouds"><span>Copernicus <span class="hlt">observations</span> of C I: <span class="hlt">pressures</span> and carbon abundances in diffuse interstellar clouds</span></a></p> <p><a target="_blank" href="http://www.osti.gov/search">DOE Office of Scientific and Technical Information (OSTI.GOV)</a></p> <p>Jenkins, E.B.; Jura, M.; Loewenstein, M.</p> <p>1983-07-01</p> <p>Using the Copernicus satellite, we <span class="hlt">observed</span> ultraviolet absorption lines of interstellar neutral carbon atoms toward 27 stars. In addition to deriving column densities of C I (both in its ground state and the two excited fine-structure levels), we used our equivalent widths to revise the f-values of some of the C I transitions measured by other investigators. We also <span class="hlt">observed</span> H/sub 2/ from the J = 4 level so that we could compare the rotational excitation of H/sub 2/ with the fine-structure excitation of C I. From the amount of fine-structure excitation of C I in each case, we havemore » derived information on the thermal gas <span class="hlt">pressures</span> within the diffuse clouds. Most clouds have p/k between 10/sup 3/ cm/sup -3/ K and 10/sup 4/ cm/sup -3/ K, but we found that at least 6% of the C I-bearing material is at p/k>10/sup 4/ cm/sup -3/ K, and one-third of the gas has upper limits for <span class="hlt">pressure</span> below 10/sup 3/ cm/sup -3/ K, assuming temperatures are not appreciably below 20 K. An analysis of radial velocities for the absorption lines showed no distinctive trends for the kinematics of high- or low-<span class="hlt">pressure</span> gas components. From the apparent lack of acceleration of high-<span class="hlt">pressure</span> clouds, we conclude that it is unlikely that streaming intercloud material is causing significant ram <span class="hlt">pressurization</span>. We have compared our results with the predictions for <span class="hlt">pressure</span> fluctuations caused by supernova explosions in the theory of McKee and Ostriker.« less</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2014EGUGA..1612784G','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2014EGUGA..1612784G"><span>Stratospheric NO2 vertical <span class="hlt">profile</span> retrieved from ground-based Zenith-Sky DOAS <span class="hlt">observations</span> at Kiruna, Sweden</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Gu, Myojeong; Enell, Carl-Fredrik; Hendrick, François; Pukite, Janis; Van Roozendael, Michel; Platt, Ulrich; Raffalski, Uwe; Wagner, Thomas</p> <p>2014-05-01</p> <p>Stratospheric NO2 destroys ozone and acts as a buffer against halogen-catalyzed ozone loss through the formation of reservoir species (ClONO2, BrONO2). Since the importance of both mechanisms depends on the altitude, the investigation of stratospheric NO2 vertical distribution can provide more insight into the role of nitrogen compounds in the destruction of ozone. Here we present stratospheric NO2 vertical <span class="hlt">profiles</span> retrieved from twilight ground-based zenith-sky DOAS <span class="hlt">observations</span> at Kiruna, Sweden (68.84°N, 20.41°E) covering 1997 - 2013 periods. This instrument <span class="hlt">observes</span> zenith scattered sunlight. The sensitivity for stratospheric trace gases is highest during twilight due to the maximum altitude of the scattering <span class="hlt">profile</span> and the light path through the stratosphere, which vary with the solar zenith angle. The <span class="hlt">profiling</span> algorithm, based on the Optimal Estimation Method, has been developed by IASB-BIRA and successfully applied at other stations (Hendrick et al., 2004). The basic principle behind this <span class="hlt">profiling</span> approach is that during twilight, the mean Rayleigh scattering altitude scans the stratosphere rapidly, providing height-resolved information on the absorption by stratospheric NO2. In this study, the long-term evolution of the stratospheric NO2 <span class="hlt">profile</span> at polar latitude will be investigated. Hendrick, F., B. Barret, M. Van Roozendael, H. Boesch, A. Butz, M. De Mazière, F. Goutail, C. Hermans, J.-C. Lambert, K. Pfeilsticker, and J.-P. Pommereau, Retrieval of nitrogen dioxide stratospheric <span class="hlt">profiles</span> from ground-based zenith-sky UV-visible <span class="hlt">observations</span>: Validation of the technique through correlative comparisons, Atmospheric Chemistry and Physics, 4, 2091-2106, 2004</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/26192133','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/26192133"><span>Beyond the average marital communication: Latent <span class="hlt">profiles</span> of the <span class="hlt">observed</span> interactions among Chinese newlywed couples.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Cao, Hongjian; Fang, Xiaoyi; Fine, Mark A; Ju, Xiaoyan; Lan, Jing; Liu, Xuanwen</p> <p>2015-12-01</p> <p>Employing a multicontext <span class="hlt">observational</span> design, using a person-centered approach, and treating the marital dyad as the unit of analysis, this study examined the within-couple communication patterning of 144 Chinese newlywed couples and its association with relationship satisfaction. Latent <span class="hlt">profile</span> analysis consistently revealed 3 <span class="hlt">profiles</span> of spouses' interactive behaviors across contexts differing in both topic nature (i.e., problem-solving vs. social support) and initiator (i.e., husbands vs. wives): (a) traditionally undemonstrative <span class="hlt">profile</span>, (b) emotionally quarrelling <span class="hlt">profile</span>, and (c) warmly supportive <span class="hlt">profile</span>. The prevalence of communication <span class="hlt">profiles</span> changed markedly with the nature of the discussion topic and the topic initiator. Further, using latent class analysis, we classified couples into subgroups based on their identified <span class="hlt">profile</span> memberships across contexts (i.e., consistency of interaction mode across contexts). Three classes were identified: (a) consistently quarrelling class, (b) consistently supportive class, and (c) modestly traditional class. Both the consistently supportive class and the modestly traditional class reported significantly higher levels of marital satisfaction than did the consistently quarrelling class. (c) 2015 APA, all rights reserved).</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/17823731','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/17823731"><span>[Assessment of patients with <span class="hlt">pressure</span> sores admitted in a tertiary care center].</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Moro, Adriana; Maurici, Alice; do Valle, Juliana Barros; Zaclikevis, Viviane Renata; Kleinubing, Harry</p> <p>2007-01-01</p> <p>To determine the prevalence and analyze the <span class="hlt">profile</span> of patients with <span class="hlt">pressure</span> sores, focusing on risk factors, the patients' clinical characteristics at a tertiary care center, as well as stage and location of the lesions on the body. This was a cross sectional not controlled <span class="hlt">observational</span> study, all patients admitted from April to June of 2005 were <span class="hlt">observed</span> daily to identify all cases of <span class="hlt">pressure</span> sores. The affected patients were evaluated by a standard questionnaire and the Scale of Braden was applied to define the risk of developing ulcers. Of the 690 patients admitted during the referred period, a prevalence of 5.9% of patients with lesions was <span class="hlt">observed</span>, equivalent to 41 patients 63.9% of which were elderly and the average length of stay was 18 days. In the sample studied 41.5% of patients were found in the internal medicine section and the intensive care unit, ICU. The most common location for sores was the sacral area, corresponding to 73.1% of the patients, and stage II was the most frequent, <span class="hlt">observed</span> in 58.5% of those patients. According to the Braden scale, most patients, 80.4%, had a high risk of developing <span class="hlt">pressure</span> ulcers, compared to 9.7% of patients with moderate risk and 7.4% with low risk. The affected patients were at high risk of developing <span class="hlt">pressure</span> sores. Prevalence of these lesions and the clinical and demographic <span class="hlt">profile</span> of the affected patients are in accordance with the data in literature.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2016EGUGA..18.7648K','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2016EGUGA..18.7648K"><span>Comparison of MADE3-simulated and <span class="hlt">observed</span> aerosol distributions with a focus on aerosol vertical <span class="hlt">profiles</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Kaiser, Christopher; Hendricks, Johannes; Righi, Mattia; Jöckel, Patrick</p> <p>2016-04-01</p> <p>The reliability of aerosol radiative forcing estimates from climate models depends on the accuracy of simulated global aerosol distribution and composition, as well as on the models' representation of the aerosol-cloud and aerosol-radiation interactions. To help improve on previous modeling studies, we recently developed the new aerosol microphysics submodel MADE3 that explicitly tracks particle mixing state in the Aitken, accumulation, and coarse mode size ranges. We implemented MADE3 into the global atmospheric chemistry general circulation model EMAC and evaluated it by comparison of simulated aerosol properties to <span class="hlt">observations</span>. Compared properties include continental near-surface aerosol component concentrations and size distributions, continental and marine aerosol vertical <span class="hlt">profiles</span>, and nearly global aerosol optical depth. Recent studies have shown the specific importance of aerosol vertical <span class="hlt">profiles</span> for determination of the aerosol radiative forcing. Therefore, our focus here is on the evaluation of simulated vertical <span class="hlt">profiles</span>. The <span class="hlt">observational</span> data is taken from campaigns between 1990 and 2011 over the Pacific Ocean, over North and South America, and over Europe. The datasets include black carbon and total aerosol mass mixing ratios, as well as aerosol particle number concentrations. Compared to other models, EMAC with MADE3 yields good agreement with the <span class="hlt">observations</span> - despite a general high bias of the simulated mass mixing ratio <span class="hlt">profiles</span>. However, BC concentrations are generally overestimated by many models in the upper troposphere. With MADE3 in EMAC, we find better agreement of the simulated BC <span class="hlt">profiles</span> with HIPPO data than the multi-model average of the models that took part in the AeroCom project. There is an interesting difference between the <span class="hlt">profiles</span> from individual campaigns and more "climatological" datasets. For instance, compared to spatially and temporally localized campaigns, the model simulates a more continuous decline in both total</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/28817574','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/28817574"><span>Diffusion tensor imaging <span class="hlt">profiles</span> reveal specific neural tract distortion in normal <span class="hlt">pressure</span> hydrocephalus.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Keong, Nicole C; Pena, Alonso; Price, Stephen J; Czosnyka, Marek; Czosnyka, Zofia; DeVito, Elise E; Housden, Charlotte R; Sahakian, Barbara J; Pickard, John D</p> <p>2017-01-01</p> <p>The pathogenesis of normal <span class="hlt">pressure</span> hydrocephalus (NPH) remains unclear which limits both early diagnosis and prognostication. The responsiveness to intervention of differing, complex and concurrent injury patterns on imaging have not been well-characterized. We used diffusion tensor imaging (DTI) to explore the topography and reversibility of white matter injury in NPH pre- and early after shunting. Twenty-five participants (sixteen NPH patients and nine healthy controls) underwent DTI, pre-operatively and at two weeks post-intervention in patients. We interrogated 40 datasets to generate a full panel of DTI measures and corroborated findings with plots of isotropy (p) vs. anisotropy (q). Concurrent examination of DTI measures revealed distinct <span class="hlt">profiles</span> for NPH patients vs. controls. PQ plots demonstrated that patterns of injury occupied discrete white matter districts. DTI <span class="hlt">profiles</span> for different white matter tracts showed changes consistent with i) predominant transependymal diffusion with stretch/ compression, ii) oedema with or without stretch/ compression and iii) predominant stretch/ compression. Findings were specific to individual tracts and dependent upon their proximity to the ventricles. At two weeks post-intervention, there was a 6·7% drop in axial diffusivity (p = 0·022) in the posterior limb of the internal capsule, compatible with improvement in stretch/ compression, that preceded any discernible changes in clinical outcome. On PQ plots, the trajectories of the posterior limb of the internal capsule and inferior longitudinal fasciculus suggested attempted 'round trips'. i.e. return to normality. DTI <span class="hlt">profiling</span> with p:q correlation may offer a non-invasive biomarker of the characteristics of potentially reversible white matter injury.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/29354177','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/29354177"><span>The influence of adding tomato extract and acetylsalicylic acid to hypotensive therapy on the daily blood <span class="hlt">pressure</span> <span class="hlt">profiles</span> of patients with arterial hypertension and high cardiovascular risk.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Osińska, Angelika N; Begier-Krasińska, Beata; Rzymski, Piotr; Krasińska, Aleksandra; Tykarski, Andrzej; Krasiński, Zbigniew</p> <p>2017-12-01</p> <p>Arterial hypertension (HT) is one of the most common diseases around the world and constitutes a significant medical, social, and economic problem. Lifestyle changes, including adequate fruit and vegetable consumption, play an important role in controlling blood <span class="hlt">pressure</span> (BP) and other cardiovascular risk factors. To compare the influence of adding acetylsalicylic acid (ASA) or standardized tomato extract (STE) to standard hypotensive therapy on the values of arterial <span class="hlt">pressure</span> and the daily blood <span class="hlt">pressure</span> <span class="hlt">profiles</span> of patients with hypertension and high cardiovascular risk. The study included 65 patients with arterial hypertension and high cardiovascular risk. High-risk patients with primary hypertension were randomly allocated in a blinded fashion to one of two groups (ASA or STE). In each case, two visits were made: the first - before the treatment, and the second - after 4 weeks of treatment. During each visit, the patients underwent a clinical measurement of arterial <span class="hlt">pressure</span> and an ambulatory blood <span class="hlt">pressure</span> measurement (ABPM). Blood platelet aggregation was assessed using the VerifyNow analyzer. After 4 weeks of treatment, the blood <span class="hlt">pressure</span> values during the day (p < 0.001), during the night ( p < 0.05), and in 24-h BP <span class="hlt">profiles</span> ( p < 0.01) obtained with ABPM were significantly lower in the STE group in comparison to the ASA group. The addition of STE to standard hypotensive treatment resulted in a favorable increase in the nocturnal fall of diastolic blood <span class="hlt">pressure</span> (DBP) (by 6.5%) and mean arterial <span class="hlt">pressure</span> (MAP) (by 3.3%). The use of STE is significant in HT patients with high total cardiovascular risk; it is associated with better BP control and improvements in the daily BP <span class="hlt">profile</span>.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/25786405','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/25786405"><span>Dynamic airway <span class="hlt">pressure</span>-time curve <span class="hlt">profile</span> (Stress Index): a systematic review.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Terragni, Pierpaolo; Bussone, Guido; Mascia, Luciana</p> <p>2016-01-01</p> <p>The assessment of respiratory mechanics at the bedside is necessary in order to identify the most protective ventilatory strategy. Indeed in the last 20 years, adverse effects of positive ventilation to the lung structures have led to a reappraisal of the objectives of mechanical ventilation. The ventilator setting requires repeated readjustment over the period of mechanical ventilation dependency and careful respiratory monitoring to minimize the risks, preventing further injury and permitting the lung and airways healing. Among the different methods that have been proposed and validated, the analysis of dynamic P-t curve (named Stress Index, SI) represents an adequate tool available at the bedside, repeatable and, therefore, able to identify the amount of overdistension occurring in the daily clinical practice, when modifying positive end-expiratory <span class="hlt">pressure</span>. In this review we will analyze the evidence that supports respiratory mechanics assessment at the bedside and the application of the dynamic P/t curve <span class="hlt">profile</span> (SI) to optimize protective ventilation in patients with acute respiratory failure.</p> </li> </ol> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_7");'>7</a></li> <li><a href="#" onclick='return showDiv("page_8");'>8</a></li> <li class="active"><span>9</span></li> <li><a href="#" onclick='return showDiv("page_10");'>10</a></li> <li><a href="#" onclick='return showDiv("page_11");'>11</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div><!-- col-sm-12 --> </div><!-- row --> </div><!-- page_9 --> <div id="page_10" class="hiddenDiv"> <div class="row"> <div class="col-sm-12"> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_8");'>8</a></li> <li><a href="#" onclick='return showDiv("page_9");'>9</a></li> <li class="active"><span>10</span></li> <li><a href="#" onclick='return showDiv("page_11");'>11</a></li> <li><a href="#" onclick='return showDiv("page_12");'>12</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div> </div> <div class="row"> <div class="col-sm-12"> <ol class="result-class" start="181"> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017AAS...22934743Z','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017AAS...22934743Z"><span>Ram <span class="hlt">Pressure</span> Stripping of Galaxy JO201</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Zhong, Greta; Tonnesen, Stephanie; Jaffé, Yara; Bellhouse, Callum; Bianca Poggianti</p> <p>2017-01-01</p> <p>Despite the discovery of the morphology-density relation more than 30 years ago, the process driving the evolution of spiral galaxies into S0s in clusters is still widely debated. Ram <span class="hlt">pressure</span> stripping--the removal of a galaxy's interstellar medium by the <span class="hlt">pressure</span> of the intracluster medium through which it orbits--may help explain galactic evolution and quenching in clusters. MUSE (Multi Unit Spectroscopic Explorer) <span class="hlt">observational</span> data of galaxy JO201 in cluster Abell 85 reveal it to be a jellyfish galaxy--one with an H-alpha emitting gas tail on only one side. We model the possible orbits for this galaxy, constrained by the cluster mass <span class="hlt">profile</span>, line of sight velocity, and projected distance from the cluster center. Using Enzo, an adaptive mesh refinement hydrodynamics code, we simulate effects of ram <span class="hlt">pressure</span> on this galaxy for a range of possible orbits. We present comparisons of both the morphology and velocity structure of our simulated galaxy to the <span class="hlt">observations</span> of H-alpha emission.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/19810020989','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/19810020989"><span>Evaluation of distributed gas cooling of <span class="hlt">pressurized</span> PAFC for utility power generation</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Farooque, M.; Maru, H.; Skok, A.</p> <p>1981-01-01</p> <p>Two short stacks were <span class="hlt">pressure</span> tested at 446 kPa (4.4 atm.) and the <span class="hlt">pressure</span> gains were more than the theoretically predicted gains. Temperature <span class="hlt">profiles</span> were <span class="hlt">observed</span> to be independent of operating <span class="hlt">pressure</span>. The <span class="hlt">pressure</span> drop was found to be inversely proportional to operating <span class="hlt">pressure</span> as expected. Continuous <span class="hlt">pressurized</span> operation of a stack for 1000 hours verified the compatability of the fuel cell component design. A simple <span class="hlt">pressurization</span> procedure was also developed. Six separate designs, covering two gas cooling schemes (DIGAS and separated) and two cooling channel geometries (straight through and treed), were analysed on the net voltage output basis. Separated cooling with 5 cells per cooler was recognized to be the best among the designs considered.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/29157582','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/29157582"><span>Serum lipid <span class="hlt">profile</span>, sleep-disordered breathing and blood <span class="hlt">pressure</span> in the elderly: a 10-year follow-up of the PROOF-SYNAPSE cohort.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Monneret, Denis; Barthélémy, Jean-Claude; Hupin, David; Maudoux, Delphine; Celle, Sébastien; Sforza, Emilia; Roche, Frédéric</p> <p>2017-11-01</p> <p>Dyslipidemia, sleep-disordered breathing (SDB) and hypertension are comorbid factors evidenced in adults, but poorly studied in old people. This study aimed to examine the long-term evolution of the serum lipid <span class="hlt">profile</span>, and its relationships with SDB and blood <span class="hlt">pressure</span> (BP) in the elderly. A ten-year follow-up of the prospective Prognostic Indicator of Cardiovascular and Cerebrovascular Events (PROOF) and the Autonomic Nervous System Activity, Aging and Sleep Apnea/Hypopnea (SYNAPSE) cohort, which initially included 1011 elderly subjects from the general population, and who were untreated by continuous positive airway <span class="hlt">pressure</span> (CPAP). Serum lipid <span class="hlt">profile</span>, respiratory polygraphy for SDB and ambulatory blood <span class="hlt">pressure</span> monitoring were performed. A total of 266 subjects (male/female 150/116; age 66.2 ± 0.8 years) were reassessed after 9.6 ± 0.7 years (age 75.8 ± 1.2 years). The prevalence of high-risk dyslipidemia decreased from 61.3 to 44.4%, and hypertension from 57.9 to 27.4%. The nocturnal oxygen desaturation index increased (mean + 2.3 ± 6.7 events/hour; p < 0.001), while the mean SaO 2 and minimal SaO 2 decreased. These variations (Δ) of oxygen desaturation worsened whether or not elderly subjects took anti-hypertensive and lipid-lowering treatments, and were not associated with serum lipid variations. The decrease in diurnal diastolic BP was independently associated with aging, and with the lowering of the waist/hip ratio (ΔW/H) and low-density lipoprotein cholesterol (LDL-C)/high-density lipoprotein cholesterol (HDL-C) ratio, while the decrease in diurnal systolic BP only depended on aging and ΔW/H. The results suggested that the <span class="hlt">observed</span> worsening of nocturnal oxygen desaturation after 10 years in the elderly was independent of the change in circulating lipids, and not influenced by lipid-lowering treatments. However, the variation in blood <span class="hlt">pressure</span> remained associated with aging, waist/hip and LDL-C/HDL-C ratios. NCT00759304 and NCT00766584</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/28946326','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/28946326"><span>Effect of high <span class="hlt">pressure</span> treatment on metabolite <span class="hlt">profile</span> of marinated meat in soy sauce.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Yang, Yang; Ye, Yangfang; Wang, Ying; Sun, Yangying; Pan, Daodong; Cao, Jinxuan</p> <p>2018-02-01</p> <p>Marinated meat in soy sauce was produced using hind leg by washing, rubbing salt, marinating with soy sauce and spices, and air dry-ripening for 15d. The effect of high <span class="hlt">pressure</span> (HP) (150 and 300MPa for 15min) on the metabolite <span class="hlt">profiles</span> of products was characterized using 1 H NMR and multivariate data analysis. The results showed that the metabonome was dominated by 26 metabolites, including amino acids, sugars, organic acids, nucleic aides and their derivatives. PC1 and PC2 explained a total of 75.4 and 11.9% of variables, respectively. HP treatments increased most of the metabolites, especially PC1, glutamate, sugars, nucleotides, anserine, lactate and creatine compared to the control. The increase of metabolites under HP was not dependent on <span class="hlt">pressure</span> level except for alanine, lactate, acetate, formate, fumarate, glucose and 5'-IMP. These findings demonstrated that HP treatment at 150MPa was economical to improve the taste of marinated meat in soy sauce. Copyright © 2017 Elsevier Ltd. All rights reserved.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/27413016','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/27413016"><span>Effects of high hydrostatic <span class="hlt">pressure</span> and thermal processing on bioactive compounds, antioxidant activity, and volatile <span class="hlt">profile</span> of mulberry juice.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Wang, Fan; Du, Bao-Lei; Cui, Zheng-Wei; Xu, Li-Ping; Li, Chun-Yang</p> <p>2017-03-01</p> <p>The aim of this study was to investigate the effects of high hydrostatic <span class="hlt">pressure</span> and thermal processing on microbiological quality, bioactive compounds, antioxidant activity, and volatile <span class="hlt">profile</span> of mulberry juice. High hydrostatic <span class="hlt">pressure</span> processing at 500 MPa for 10 min reduced the total viable count from 4.38 log cfu/ml to nondetectable level and completely inactivated yeasts and molds in raw mulberry juice, ensuring the microbiological safety as thermal processing at 85 ℃ for 15 min. High hydrostatic <span class="hlt">pressure</span> processing maintained significantly (p < 0.05) higher contents of total phenolic, total flavonoid and resveratrol, and antioxidant activity of mulberry juice than thermal processing. The main volatile compounds of mulberry juice were aldehydes, alcohols, and ketones. High hydrostatic <span class="hlt">pressure</span> processing enhanced the volatile compound concentrations of mulberry juice while thermal processing reduced them in comparison with the control. These results suggested that high hydrostatic <span class="hlt">pressure</span> processing could be an alternative to conventional thermal processing for production of high-quality mulberry juice.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.osti.gov/pages/biblio/1281695-observed-large-scale-structures-diabatic-heating-drying-profiles-during-twp-ice','SCIGOV-DOEP'); return false;" href="https://www.osti.gov/pages/biblio/1281695-observed-large-scale-structures-diabatic-heating-drying-profiles-during-twp-ice"><span><span class="hlt">Observed</span> large-scale structures and diabatic heating and drying <span class="hlt">profiles</span> during TWP-ICE</span></a></p> <p><a target="_blank" href="http://www.osti.gov/pages">DOE PAGES</a></p> <p>Xie, Shaocheng; Hume, Timothy; Jakob, Christian; ...</p> <p>2010-01-01</p> <p>This study documents the characteristics of the large-scale structures and diabatic heating and drying <span class="hlt">profiles</span> <span class="hlt">observed</span> during the Tropical Warm Pool–International Cloud Experiment (TWP-ICE), which was conducted in January–February 2006 in Darwin during the northern Australian monsoon season. The examined <span class="hlt">profiles</span> exhibit significant variations between four distinct synoptic regimes that were <span class="hlt">observed</span> during the experiment. The active monsoon period is characterized by strong upward motion and large advective cooling and moistening throughout the entire troposphere, while the suppressed and clear periods are dominated by moderate midlevel subsidence and significant low- to midlevel drying through horizontal advection. The midlevel subsidence andmore » horizontal dry advection are largely responsible for the dry midtroposphere <span class="hlt">observed</span> during the suppressed period and limit the growth of clouds to low levels. During the break period, upward motion and advective cooling and moistening located primarily at midlevels dominate together with weak advective warming and drying (mainly from horizontal advection) at low levels. The variations of the diabatic heating and drying <span class="hlt">profiles</span> with the different regimes are closely associated with differences in the large-scale structures, cloud types, and rainfall rates between the regimes. Strong diabatic heating and drying are seen throughout the troposphere during the active monsoon period while they are moderate and only occur above 700 hPa during the break period. The diabatic heating and drying tend to have their maxima at low levels during the suppressed periods. Furthermore, the diurnal variations of these structures between monsoon systems, continental/coastal, and tropical inland-initiated convective systems are also examined.« less</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://ntrs.nasa.gov/search.jsp?R=19910039610&hterms=midi&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D40%26Ntt%3Dmidi','NASA-TRS'); return false;" href="https://ntrs.nasa.gov/search.jsp?R=19910039610&hterms=midi&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D40%26Ntt%3Dmidi"><span>UV <span class="hlt">observations</span> of the cool DBQA5 white dwarf LDS 678A - Limits on the atmospheric composition, <span class="hlt">pressure</span> shift, and gravitational redshift derived from C I 2479</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Oswalt, Terry D.; Sion, Edward M.; Hammond, Gordon; Vauclair, Gerard; Liebert, James W.</p> <p>1991-01-01</p> <p>A high-resolution ultraviolet spectrum of the helium-rich degenerate LDS 678A, obtained with the International Ultraviolet Explorer (IUE) satellite, is presented. LDS 678A is the coolest metallic line degenerate (DQ or DZ) yet <span class="hlt">observed</span> with the IUE echelle. These <span class="hlt">observations</span> provide a detailed line <span class="hlt">profile</span> of the strong C I 2479 absorption line and equivalent width W2479 = 2.35 + or - 0.06 A from which theoretical <span class="hlt">profile</span> fits yield a carbon abundance of log C/He = (-6.7 + or- 0.2). The presence of carbon in a He-rich atmosphere lends credence to the notion that LDS 678A is a transitional case between the DB white dwarfs with nearly pure helium atmospheres and the helium-rich DQ white dwarfs which exhibit carbon bands. Corrected for an inferred <span class="hlt">pressure</span> shift Vp = + 38 + or - 4 km/s for the C I 2479 line, a gravitational redshift of Vrs = + 26 + or - 13 km/s is deduced from which a most probable mass of 0.55 solar mass is derived.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/27212015','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/27212015"><span>Blood <span class="hlt">pressure</span> and antihypertensive medication <span class="hlt">profile</span> in a multiethnic Asian population of stable chronic kidney disease patients.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Teo, Boon Wee; Chua, Horng Ruey; Wong, Weng Kin; Haroon, Sabrina; Subramanian, Srinivas; Loh, Ping Tyug; Sethi, Sunil; Lau, Titus</p> <p>2016-05-01</p> <p>Clinical practice guidelines recommend different blood <span class="hlt">pressure</span> (BP) goals for chronic kidney disease (CKD) patients. Usage of antihypertensive medication and attainment of BP targets in Asian CKD patients remain unclear. This study describes the <span class="hlt">profile</span> of antihypertensive agents used and BP components in a multiethnic Asian population with stable CKD. Stable CKD outpatients with variability of serum creatinine levels < 20%, taken > 3 months apart, were recruited. Mean systolic blood <span class="hlt">pressure</span> (SBP) and diastolic blood <span class="hlt">pressure</span> (DBP) were measured using automated manometers, according to practice guidelines. Serum creatinine was assayed and the estimated glomerular filtration rate (GFR) calculated using the CKD Epidemiology Collaboration equation. BP and antihypertensive medication <span class="hlt">profile</span> was examined using univariate analyses. 613 patients (55.1% male; 74.7% Chinese, 6.4% Indian, 11.4% Malay; 35.7% diabetes mellitus) with a mean age of 57.8 ± 14.5 years were recruited. Mean SBP was 139 ± 20 mmHg, DBP was 74 ± 11 mmHg, serum creatinine was 166 ± 115 µmol/L and GFR was 53 ± 32 mL/min/1.73 m(2). At a lower GFR, SBP increased (p < 0.001), whereas DBP decreased (p = 0.0052). Mean SBP increased in tandem with the number of antihypertensive agents used (p < 0.001), while mean DBP decreased when ≥ 3 antihypertensive agents were used (p = 0.0020). Different targets are recommended for each BP component in CKD patients. A majority of patients cannot attain SBP targets and/or exceed DBP targets. Research into monitoring and treatment methods is required to better define BP targets in CKD patients. Copyright: © Singapore Medical Association.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/20180001135','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/20180001135"><span>High Temporal Resolution Tropospheric Wind <span class="hlt">Profile</span> <span class="hlt">Observations</span> at NASA Kennedy Space Center During Hurricane Irma</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Decker, Ryan; Barbre, Robert; Huddleston, Lisa; Wilfong, Tim; Brauer, Tom</p> <p>2018-01-01</p> <p>The NASA Kennedy Space Center (KSC) operates a 48-MHz Tropospheric/Stratospheric Doppler Radar Wind <span class="hlt">Profiler</span> (TDRWP) on a continual basis generating wind <span class="hlt">profiles</span> between 2-19 km in the support of space launch vehicle operations. A benefit of the continual operability of the system is the ability to provide unique <span class="hlt">observations</span> of severe weather events such as hurricanes. On the evening of 10 September 2017, Hurricane Irma passed within 100 miles to the west of KSC through the middle of the Florida peninsula. The hurricane was responsible for power outages to approximately 2/3 of Florida's population. This paper will describe the characteristics of the tropospheric wind <span class="hlt">observations</span> from the TDRWP during Irma, provide a comparison to previous TDRWP <span class="hlt">observations</span> from Hurricane Matthew in 2016, and discuss lessons learned regarding dissemination of TDRWP data during the event.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/27537378','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/27537378"><span>Abnormal Circadian Blood <span class="hlt">Pressure</span> <span class="hlt">Profile</span> as a Prognostic Marker in Patients with Nonischemic Dilated Cardiomyopathy.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Sawamura, Akinori; Okumura, Takahiro; Takeshita, Kyosuke; Watanabe, Naoki; Kano, Naoaki; Mori, Hiroaki; Fukaya, Kenji; Morimoto, Ryota; Hirashiki, Akihiro; Bando, Yasuko Kureishi; Murohara, Toyoaki</p> <p></p> <p>An abnormal circadian blood <span class="hlt">pressure</span> (BP) <span class="hlt">profile</span> is considered a risk factor for cardiovascular disease. However, its significance in heart failure patients with nonischemic etiology is unknown. Herein, we investigated the prognostic value of a circadian BP <span class="hlt">profile</span> in patients with nonischemic dilated cardiomyopathy (NIDCM). We enrolled 114 NIDCM patients (76 males, mean age 53.1 years). The percent nighttime BP fall (%NBPF) was defined using ambulatory BP monitoring as a percent decrease in mean systolic BP in nighttime from daytime. All patients were divided into three groups: dipper (%NBPF ≥10), non-dipper (0 ≤ %NBPF < 10), and riser (%NBPF <0). Riser patients had the highest serum creatinine levels (dipper, 0.78 ± 0.20 mg/dl; non-dipper, 0.85 ± 0.21 mg/dl; riser, 0.99 ± 0.23 mg/dl; p = 0.006). In survival analysis, riser patients had the highest cumulative cardiac-related deaths (log-rank, p = 0.001), which was an independent predictor of cardiac-related deaths (hazard ratio, 12.6; 95% confidence interval, 1.76-253; p = 0.01). Multivariate analysis revealed that the norepinephrine level at 24-hour collected urine (24 h U-NE) and the serum creatinine level were independent determinants of %NBPF (adjusted R2 = 0.20; 24 h U-NE, p = 0.0001; serum creatinine, p = 0.04). The riser <span class="hlt">profile</span> was associated with poor prognosis of NIDCM, which may reflect impaired sympathetic nervous system activity. Evaluating the circadian BP <span class="hlt">profile</span> may be useful for risk stratification in NIDCM patients. © 2016 S. Karger AG, Basel.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/29739583','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/29739583"><span>The impact of high <span class="hlt">pressure</span> processing on the phenolic <span class="hlt">profile</span>, hydrophilic antioxidant and reducing capacity of purée obtained from commercial tomato varieties.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Jeż, Maja; Wiczkowski, Wiesław; Zielińska, Danuta; Białobrzewski, Ireneusz; Błaszczak, Wioletta</p> <p>2018-09-30</p> <p>The effect of high hydrostatic <span class="hlt">pressure</span> (HHP) (450-550-650 MPa/5-10-15 min) on polyphenols <span class="hlt">profile</span> of purée obtained from commercial tomato varieties (Maliniak, Cerise, Black Prince and Lima) was investigated. Individual polyphenols, total phenolic index (TPI) were quantified using a mass spectrometer (HPLC-MS/MS). Photochemiluminescence (PCLACW), cyclic voltammetry (CV) and ferric reducing antioxidant power (FRAP) assays were used to determine the antioxidant capacity of the hydrophilic extract. The results demonstrated that at certain processing conditions, HHP may enhance or decrease the nutritional quality of tomato purée. However, the tomato variety was a key factor influencing the polyphenols <span class="hlt">profile</span> and the antioxidant capacity. A significant positive correlation was found among TPI, FRAP or CV parameters and the concentration of caffeic, ferulic, sinapic and p-coumaric acids, and epicatechin. On the other hand, significant positive correlation was <span class="hlt">observed</span> among antioxidant capacity (PCLACW), TPC, rutin and naringenin concentration as well as chlorogenic and isochlorogenic acids. Copyright © 2018 Elsevier Ltd. All rights reserved.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/20040110843','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/20040110843"><span><span class="hlt">Observation</span> of Quartz Cathode-Luminescence in a Low <span class="hlt">Pressure</span> Plasma Discharge</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Foster, John E.</p> <p>2004-01-01</p> <p>Intense, steady-state cathode-luminescence has been <span class="hlt">observed</span> from exposure of quartz powder to a low <span class="hlt">pressure</span> rf-excited argon plasma discharge. The emission spectra (400 to 850 nm) associated with the powder luminescence were documented as a function of bias voltage using a spectrometer. The emission was broad-band, essentially washing out the line spectra features of the argon plasma discharge.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=2106054','PMC'); return false;" href="https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=2106054"><span>ELECTRON MICROSCOPIC <span class="hlt">OBSERVATION</span> OF SPECIMENS UNDER CONTROLLED GAS <span class="hlt">PRESSURE</span></span></a></p> <p><a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pmc">PubMed Central</a></p> <p>Heide, Hans Gunther</p> <p>1962-01-01</p> <p>A technique for encasing specimens in a thin gas layer during their <span class="hlt">observation</span> in the Siemens Elmiskop I is described. All gases can be employed at <span class="hlt">pressures</span> up to one atmosphere. Destruction of specimens can occur in the beam; all organic specimens are particularly liable to decompose. The conditions under which this can be avoided are given. A useful application of the technique allows one to prevent specimens from drying out, as they normally do in vacuum. A further application uses the controlled removal of carbon for thinning organic layers and for selective etching of organic materials. PMID:13905967</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2014HESS...18.2503C','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2014HESS...18.2503C"><span>Kalman filters for assimilating near-surface <span class="hlt">observations</span> into the Richards equation - Part 1: Retrieving state <span class="hlt">profiles</span> with linear and nonlinear numerical schemes</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Chirico, G. B.; Medina, H.; Romano, N.</p> <p>2014-07-01</p> <p>This paper examines the potential of different algorithms, based on the Kalman filtering approach, for assimilating near-surface <span class="hlt">observations</span> into a one-dimensional Richards equation governing soil water flow in soil. Our specific objectives are: (i) to compare the efficiency of different Kalman filter algorithms in retrieving matric <span class="hlt">pressure</span> head <span class="hlt">profiles</span> when they are implemented with different numerical schemes of the Richards equation; (ii) to evaluate the performance of these algorithms when nonlinearities arise from the nonlinearity of the <span class="hlt">observation</span> equation, i.e. when surface soil water content <span class="hlt">observations</span> are assimilated to retrieve matric <span class="hlt">pressure</span> head values. The study is based on a synthetic simulation of an evaporation process from a homogeneous soil column. Our first objective is achieved by implementing a Standard Kalman Filter (SKF) algorithm with both an explicit finite difference scheme (EX) and a Crank-Nicolson (CN) linear finite difference scheme of the Richards equation. The Unscented (UKF) and Ensemble Kalman Filters (EnKF) are applied to handle the nonlinearity of a backward Euler finite difference scheme. To accomplish the second objective, an analogous framework is applied, with the exception of replacing SKF with the Extended Kalman Filter (EKF) in combination with a CN numerical scheme, so as to handle the nonlinearity of the <span class="hlt">observation</span> equation. While the EX scheme is computationally too inefficient to be implemented in an operational assimilation scheme, the retrieval algorithm implemented with a CN scheme is found to be computationally more feasible and accurate than those implemented with the backward Euler scheme, at least for the examined one-dimensional problem. The UKF appears to be as feasible as the EnKF when one has to handle nonlinear numerical schemes or additional nonlinearities arising from the <span class="hlt">observation</span> equation, at least for systems of small dimensionality as the one examined in this study.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/1994JGR....9921511B','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/1994JGR....9921511B"><span>Pickup protons and <span class="hlt">pressure</span>-balanced structures: Voyager 2 <span class="hlt">observations</span> in merged interaction regions near 35 AU</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Burlaga, L. F.; Ness, N. F.; Belcher, J. W.; Szabo, A.; Isenberg, P. A.; Lee, M. A.</p> <p>1994-11-01</p> <p>Five <span class="hlt">pressure</span>-balanced structures, each with a scale of the order of a few hundredths of an astonomical unit (AU), were identified in two merged interaction regions (MIRs) near 35 AU in the Voyager 2 plasma and magnetic field data. They include a tangential discontinuity, simple and complex magnetic holes, slow correlated variations among the plasma and magnetic field parameters, and complex uncorrelated variations among the parameters. The changes in the magnetic <span class="hlt">pressure</span> in these events are balanced by changes in the <span class="hlt">pressure</span> of interstellar pickup protons. Thus the pickup protons probably play a major role in the dynamics of the MIRs. The solar wind proton and electron <span class="hlt">pressures</span> are relatively unimportant in the MIRs at 35 AU and beyond. The region near 35 AU is transition region: the Sun is the source of the magnetic field, but the interstellar medium in source of pickups protons. Relative to the solar wind proton guyroadius, the thicknesses of the discontinuities and simple magnetic holes <span class="hlt">observed</span> near 35 AU are at least an order of magnitude greater than those <span class="hlt">observed</span> at 1 AU. However, the thicknesses of the tangential discontinuity and simple magnetic holes <span class="hlt">observed</span> near 35 AU (in units of the pickup proton Larmor radius) are comparable to those <span class="hlt">observed</span> at 1 AU (in units of the solar wind proton gyroradius). Thus the gyroradius of interstellar pickup protons controls the thickness of current sheets near 35 AU. We determine the interstellar pickup proton <span class="hlt">pressure</span> in the PBSs. Using a model for the pickup proton temperature, we estimate that the average interstellar pickup proton <span class="hlt">pressure</span>, temperature, and density in the MIRs at 35 AU are (0.53 +/- 0.14) x 10-12 erg/cu cm, (5.8 +/- 0.4) x 106 K and (7 +/- 2) x 10-4/cu cm.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=5560677','PMC'); return false;" href="https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=5560677"><span>Diffusion tensor imaging <span class="hlt">profiles</span> reveal specific neural tract distortion in normal <span class="hlt">pressure</span> hydrocephalus</span></a></p> <p><a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pmc">PubMed Central</a></p> <p>Pena, Alonso; Price, Stephen J.; Czosnyka, Marek; Czosnyka, Zofia; DeVito, Elise E.; Housden, Charlotte R.; Sahakian, Barbara J.; Pickard, John D.</p> <p>2017-01-01</p> <p>Background The pathogenesis of normal <span class="hlt">pressure</span> hydrocephalus (NPH) remains unclear which limits both early diagnosis and prognostication. The responsiveness to intervention of differing, complex and concurrent injury patterns on imaging have not been well-characterized. We used diffusion tensor imaging (DTI) to explore the topography and reversibility of white matter injury in NPH pre- and early after shunting. Methods Twenty-five participants (sixteen NPH patients and nine healthy controls) underwent DTI, pre-operatively and at two weeks post-intervention in patients. We interrogated 40 datasets to generate a full panel of DTI measures and corroborated findings with plots of isotropy (p) vs. anisotropy (q). Results Concurrent examination of DTI measures revealed distinct <span class="hlt">profiles</span> for NPH patients vs. controls. PQ plots demonstrated that patterns of injury occupied discrete white matter districts. DTI <span class="hlt">profiles</span> for different white matter tracts showed changes consistent with i) predominant transependymal diffusion with stretch/ compression, ii) oedema with or without stretch/ compression and iii) predominant stretch/ compression. Findings were specific to individual tracts and dependent upon their proximity to the ventricles. At two weeks post-intervention, there was a 6·7% drop in axial diffusivity (p = 0·022) in the posterior limb of the internal capsule, compatible with improvement in stretch/ compression, that preceded any discernible changes in clinical outcome. On PQ plots, the trajectories of the posterior limb of the internal capsule and inferior longitudinal fasciculus suggested attempted ‘round trips’. i.e. return to normality. Conclusion DTI <span class="hlt">profiling</span> with p:q correlation may offer a non-invasive biomarker of the characteristics of potentially reversible white matter injury. PMID:28817574</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://ntrs.nasa.gov/search.jsp?R=19780029799&hterms=copernicus&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D50%26Ntt%3Dcopernicus','NASA-TRS'); return false;" href="https://ntrs.nasa.gov/search.jsp?R=19780029799&hterms=copernicus&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D50%26Ntt%3Dcopernicus"><span>Long-term changes in ultraviolet P Cygni <span class="hlt">profiles</span> <span class="hlt">observed</span> with Copernicus</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Snow, T. P., Jr.</p> <p>1977-01-01</p> <p>The incidence and nature of variability occurring on time scales of years in the ultraviolet P Cygni <span class="hlt">profiles</span> of 15 O and B stars are investigated using spectrophotometric data obtained with the Copernicus satellite. It is found that some change in at least a few details of the P Cygni <span class="hlt">profiles</span> is evident in almost every case, that the changes in a few stars appear to represent substantial variations in the column densities of the particular ions <span class="hlt">observed</span>, and that the changes in other stars are minor in nature and do not result from significant alterations in the quantity of material in the stellar winds. Most of the narrow absorption features are shown to be invariant in velocity, although their strengths have apparently changed in certain cases. The nature of the changes <span class="hlt">observed</span> in each of the program stars is briefly described, the time scale for variability in the stellar winds is considered, and two stars (Zeta Pup and Delta Ori A) are identified for which some alteration in the total amount of material in the stellar wind has taken place. It is suggested that the narrow absorption features probably represent temperature gradients or plateaus in the stellar-wind velocity fields or may be caused by flat regions in the height dependence of the wind velocity.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=1718232','PMC'); return false;" href="https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=1718232"><span>Infant feeding and adult glucose tolerance, lipid <span class="hlt">profile</span>, blood <span class="hlt">pressure</span>, and obesity</span></a></p> <p><a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pmc">PubMed Central</a></p> <p>Ravelli, A; van der Meulen, J H P; Osmond, C; Barker, D; Bleker, O</p> <p>2000-01-01</p> <p>BACKGROUND—It is generally accepted that breast feeding has a beneficial effect on the health of infants and young children. Recently, a few studies have shown that the method of infant feeding is also associated with cardiovascular disease and its risk factors in adult life.
AIMS—To examine the association between the method of infant feeding in the first weeks after birth and glucose tolerance, plasma lipid <span class="hlt">profile</span>, blood <span class="hlt">pressure</span>, and body mass in adults aged 48-53 years.
METHODS—Subjects born at term between 1 November 1943 and 28 February 1947 in the Wilhelmina Gasthuis in Amsterdam around the time of a severe period of famine (late November 1944 to early May 1945). For 625 subjects, information was available about infant feeding at the time of discharge from hospital (on average 10.4days after birth), and at least one blood sample after an overnight fast.
RESULTS—Subjects who were bottle fed had a higher mean 120 minute plasma glucose concentration after a standard oral glucose tolerance test than those who were exclusively breast fed. They also had a higher plasma low density lipoprotein (LDL) cholesterol concentration, a lower high density lipoprotein (HDL) cholesterol concentration, and a higher LDL/HDL ratio. Systolic blood <span class="hlt">pressure</span> and body mass index were not affected by the method of infant feeding.
CONCLUSIONS—Exclusive breast feeding seems to have a protective effect against some risk factors for cardiovascular disease in later life.

 PMID:10685933</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2014APS..MARA26008G','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2014APS..MARA26008G"><span><span class="hlt">Observation</span> of antiferromagnetic order collapse in the <span class="hlt">pressurized</span> insulator LaMnPO</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Guo, Jing; Simonson, Jack; Sun, Liling; Wu, Qi; Guo, Peiwen; Zhang, Chao; Gu, Dachun; Kotliar, Gabriel; Aronson, Meigan; Zhao, Zhongxian</p> <p>2014-03-01</p> <p>The emergence of superconductivity in the iron pnictide or cuprate high temperature superconductors usually accompanies the suppression of a long-ranged antiferromagnetic (AFM) order state in a corresponding parent compound by doping or <span class="hlt">pressurizing</span>. A great deal of effort by doping has been made to find superconductivity in Mn-based compounds, which are thought to bridge the gap between the two families of high temperature superconductors, but the AFM order was not successfully suppressed. Here we report the first <span class="hlt">observations</span> of the <span class="hlt">pressure</span>-induced elimination of long-ranged AFM order at ~ 34 GPa and a crossover from an AFM insulating to an AFM metallic state at ~ 20 GPa in LaMnPO single crystals that are iso-structural to the LaFeAsO superconductor by in-situ high <span class="hlt">pressure</span> resistance and ac susceptibility measurements. These findings are of importance to explore potential superconductivity in Mn-based compounds and to shed new light on the underlying mechanism of high temperature superconductivity.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2013NatSR...3E2555G','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2013NatSR...3E2555G"><span><span class="hlt">Observation</span> of antiferromagnetic order collapse in the <span class="hlt">pressurized</span> insulator LaMnPO</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Guo, Jing; Simonson, J. W.; Sun, Liling; Wu, Qi; Gao, Peiwen; Zhang, Chao; Gu, Dachun; Kotliar, Gabriel; Aronson, Meigan; Zhao, Zhongxian</p> <p>2013-08-01</p> <p>The emergence of superconductivity in the iron pnictide or cuprate high temperature superconductors usually accompanies the suppression of a long-ranged antiferromagnetic (AFM) order state in a corresponding parent compound by doping or <span class="hlt">pressurizing</span>. A great deal of effort by doping has been made to find superconductivity in Mn-based compounds, which are thought to bridge the gap between the two families of high temperature superconductors, but the AFM order was not successfully suppressed. Here we report the first <span class="hlt">observations</span> of the <span class="hlt">pressure</span>-induced elimination of long-ranged AFM order at ~ 34 GPa and a crossover from an AFM insulating to an AFM metallic state at ~ 20 GPa in LaMnPO single crystals that are iso-structural to the LaFeAsO superconductor by in-situ high <span class="hlt">pressure</span> resistance and ac susceptibility measurements. These findings are of importance to explore potential superconductivity in Mn-based compounds and to shed new light on the underlying mechanism of high temperature superconductivity.</p> </li> </ol> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_8");'>8</a></li> <li><a href="#" onclick='return showDiv("page_9");'>9</a></li> <li class="active"><span>10</span></li> <li><a href="#" onclick='return showDiv("page_11");'>11</a></li> <li><a href="#" onclick='return showDiv("page_12");'>12</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div><!-- col-sm-12 --> </div><!-- row --> </div><!-- page_10 --> <div id="page_11" class="hiddenDiv"> <div class="row"> <div class="col-sm-12"> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_9");'>9</a></li> <li><a href="#" onclick='return showDiv("page_10");'>10</a></li> <li class="active"><span>11</span></li> <li><a href="#" onclick='return showDiv("page_12");'>12</a></li> <li><a href="#" onclick='return showDiv("page_13");'>13</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div> </div> <div class="row"> <div class="col-sm-12"> <ol class="result-class" start="201"> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/23989921','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/23989921"><span><span class="hlt">Observation</span> of antiferromagnetic order collapse in the <span class="hlt">pressurized</span> insulator LaMnPO.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Guo, Jing; Simonson, J W; Sun, Liling; Wu, Qi; Gao, Peiwen; Zhang, Chao; Gu, Dachun; Kotliar, Gabriel; Aronson, Meigan; Zhao, Zhongxian</p> <p>2013-01-01</p> <p>The emergence of superconductivity in the iron pnictide or cuprate high temperature superconductors usually accompanies the suppression of a long-ranged antiferromagnetic (AFM) order state in a corresponding parent compound by doping or <span class="hlt">pressurizing</span>. A great deal of effort by doping has been made to find superconductivity in Mn-based compounds, which are thought to bridge the gap between the two families of high temperature superconductors, but the AFM order was not successfully suppressed. Here we report the first <span class="hlt">observations</span> of the <span class="hlt">pressure</span>-induced elimination of long-ranged AFM order at ~ 34 GPa and a crossover from an AFM insulating to an AFM metallic state at ~ 20 GPa in LaMnPO single crystals that are iso-structural to the LaFeAsO superconductor by in-situ high <span class="hlt">pressure</span> resistance and ac susceptibility measurements. These findings are of importance to explore potential superconductivity in Mn-based compounds and to shed new light on the underlying mechanism of high temperature superconductivity.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2015EGUGA..17.7930C','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2015EGUGA..17.7930C"><span>A study of the Ionospheric electron density <span class="hlt">profile</span> with FORMOSAT-3/COSMIC <span class="hlt">observation</span> data</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Chou, Min-Yang; Tsai, Ho-Fang; Lin, Chi-Yen; Lee, I.-Te; Lin, Charles; Liu, Jann-Yenq</p> <p>2015-04-01</p> <p>The GPS Occultation Experiment payload onboard FORMOSAT-3/COSMIC microsatellite constellation is capable of scanning the ionospheric structure by the radio occultation (RO) technique to retrieve precise electron density <span class="hlt">profiles</span> since 2006. Due to the success of FORMOSAT-3/COSMIC, the follow-on mission, FORMOSAT-7/COSMIC-2, is to launch 12 microsatellites in 2016 and 2018, respectively, with the Global Navigation Satellite Systems (GNSS) RO instrument onboard for tracking GPS, Galileo and/or GLONASS satellite signals and to provide more than 8,000 RO soundings per day globally. An overview of the validation of the FORMOSAT-3/COSMIC ionospheric <span class="hlt">profiling</span> is given by means of the traditional Abel transform through bending angle and total electron content (TEC), while the ionospheric data assimilation is also applied, based on the Gauss-Markov Kalman filter with the International Reference Ionosphere model (IRI-2007) and global ionosphere map (GIM) as background model, to assimilate TEC <span class="hlt">observations</span> from FORMOSAT-3/COSMIC. The results shows comparison of electron density <span class="hlt">profiles</span> from Abel inversion and data assimilation. Furthermore, an <span class="hlt">observing</span> system simulation experiment is also applied to determine the impact of FORMOSAT-7/COSMIC-2 on ionospheric weather monitoring, which reveals an opportunity on advanced study of small spatial and temporal variations in the ionosphere.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2016APS..DPPJ10105K','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2016APS..DPPJ10105K"><span>Dependency of Tearing Mode Stability on Current and <span class="hlt">Pressure</span> <span class="hlt">Profiles</span> in DIII-D Hybrid Discharges</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Kim, K.; Park, J. M.; Murakami, M.; La Haye, R. J.; Na, Y.-S.; SNU/ORAU; ORNL; Atomics, General; SNU; DIII-D Team</p> <p>2016-10-01</p> <p>Understanding the physics of the onset and evolution of tearing modes (TMs) in tokamak plasmas is important for high- β steady-state operation. Based on DIII-D steady-state hybrid experiments with accurate equilibrium reconstruction and well-measured plasma <span class="hlt">profiles</span>, the 2/1 tearing mode can be more stable with increasing local current and <span class="hlt">pressure</span> gradient at rational surface and with lower <span class="hlt">pressure</span> peaking and plasma inductance. The tearing stability index Δ', estimated by the Rutherford equation with experimental mode growth rate was validated against Δ' calculated by linear eigenvalue solver (PEST3); preliminary comprehensive MHD modeling by NIMROD reproduced the TM onset reasonably well. We present a novel integrated modeling for the purpose of predicting TM onset in experiment by combining a model equilibrium reconstruction using IPS/FASTRAN, linear stability Δ' calculation using PEST3, and fitting formula for critical Δ' from NIMROD. Work supported in part by the US DoE under DE-AC05-06OR23100, DE-AC05-00OR22725, and DEFC02-04ER54698.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/20180001112','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/20180001112"><span>High Temporal Resolution Tropospheric Wind <span class="hlt">Profile</span> <span class="hlt">Observations</span> at NASA Kennedy Space Center during Hurricane Irma</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Decker, Ryan K.; Barbre, Robert E., Jr.; Huddleston, Lisa; Brauer, Thomas; Wilfong, Timothy</p> <p>2018-01-01</p> <p>The National Aeronautics and Space Administration's (NASA) Kennedy Space Center (KSC) operates a 48-MHz Tropospheric/Stratospheric Doppler Radar Wind <span class="hlt">Profiler</span> (TDRWP) on a continual basis generating wind <span class="hlt">profiles</span> between 2-19 km (approximately 6.6-62.3 kft) in the support of space launch vehicle operations. A benefit of the continual operability of the system is the ability to provide unique <span class="hlt">observations</span> of severe weather events such as hurricanes. On the evening of 10 September 2017, Hurricane Irma passed within 160 km (87 nmi) to the west of KSC through the middle of the Florida peninsula. The hurricane was responsible for power outages to approximately 2/3 of Florida's population (Stein, 2017). This paper will provide an overview of the TDRWP system, describe the characteristics of the wind <span class="hlt">observations</span> from the TDRWP during Irma passage, provide a comparison to previous TDRWP <span class="hlt">observations</span> from Hurricane Matthew in 2016, and provide the location where TDRWP data is available to the meteorological community.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/17210835','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/17210835"><span>Stress management at the worksite: reversal of symptoms <span class="hlt">profile</span> and cardiovascular dysregulation.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Lucini, Daniela; Riva, Silvano; Pizzinelli, Paolo; Pagani, Massimo</p> <p>2007-02-01</p> <p>Work stress may increase cardiovascular risk either indirectly, by inducing unhealthy life styles, or directly, by affecting the autonomic nervous system and arterial <span class="hlt">pressure</span>. We hypothesized that, before any apparent sign of disease, work-related stress is already accompanied by alterations of RR variability <span class="hlt">profile</span> and that a simple onsite stress management program based on cognitive restructuring and relaxation training could reduce the level of stress symptoms, revert stress-related autonomic nervous system dysregulation, and lower arterial <span class="hlt">pressure</span>. We compared 91 white-collar workers, enrolled at a time of work downsizing (hence, in a stress condition), with 79 healthy control subjects. Psychological <span class="hlt">profiles</span> were assessed by questionnaires and autonomic nervous system regulation by spectral analysis of RR variability. We also tested a simple onsite stress management program (cognitive restructuring and relaxation training) in a subgroup of workers compared with a sham subgroup (sham program). Workers presented an elevated level of stress-related symptoms and an altered variability <span class="hlt">profile</span> as compared with control subjects (low-frequency component of RR variability was, respectively, 65.2+/-2 versus 55.3+/-2 normalized units; P<0.001; opposite changes were <span class="hlt">observed</span> for the high-frequency component). These alterations were largely reverted (low-frequency component of RR variability from 63.6+/-3.9 to 49.3+/-3 normalized units; P<0.001) by the stress management program, which also slightly lowered systolic arterial <span class="hlt">pressure</span>. No changes were <span class="hlt">observed</span> in the sham program group. This noninvasive study indicates that work stress is associated with unpleasant symptoms and with an altered autonomic <span class="hlt">profile</span> and suggests that a stress management program could be implemented at the worksite, with possible preventive advantages for hypertension.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2014Ap%26SS.351..289K','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2014Ap%26SS.351..289K"><span>A comparison between <span class="hlt">observed</span> and analytical velocity dispersion <span class="hlt">profiles</span> of 20 nearby galaxy clusters</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Khan, Mohammad S.; Abdullah, Mohamed H.; Ali, Gamal B.</p> <p>2014-05-01</p> <p>We derive analytical expression for the velocity dispersion of galaxy clusters, using the statistical mechanical approach. We compare the <span class="hlt">observed</span> velocity dispersion <span class="hlt">profiles</span> for 20 nearby ( z≤0.1) galaxy clusters with the analytical ones. It is interesting to find that the analytical results closely match with the <span class="hlt">observed</span> velocity dispersion <span class="hlt">profiles</span> only if the presence of the diffuse matter in clusters is taken into consideration. This takes us to introduce a new approach to detect the ratio of diffuse mass, M diff , within a galaxy cluster. For the present sample, the ratio f= M diff / M, where M the cluster's total mass is found to has an average value of 45±12 %. This leads us to the result that nearly 45 % of the cluster mass is impeded outside the galaxies, while around 55 % of the cluster mass is settled in the galaxies.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2018MNRAS.473..317H','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2018MNRAS.473..317H"><span>Radiation-<span class="hlt">pressure</span>-driven sub-Keplerian rotation of the disc around the AGB star L2 Pup</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Haworth, Thomas J.; Booth, Richard A.; Homan, Ward; Decin, Leen; Clarke, Cathie J.; Mohanty, Subhanjoy</p> <p>2018-01-01</p> <p>We study the sub-Keplerian rotation and dust content of the circumstellar material around the asymptotic giant branch (AGB) star L2 Puppis. We find that the thermal <span class="hlt">pressure</span> gradient alone cannot explain the <span class="hlt">observed</span> rotation <span class="hlt">profile</span>. We find that there is a family of possible dust populations for which radiation <span class="hlt">pressure</span> can drive the <span class="hlt">observed</span> sub-Keplerian rotation. This set of solutions is further constrained by the spectral energy distribution (SED) of the system, and we find that a dust-to-gas mass ratio of ∼10-3 and a maximum grain size that decreases radially outwards can satisfy both the rotation curve and SED. These dust populations are dynamically tightly coupled to the gas azimuthally. However, grains larger than ∼ 0.5 μm are driven outwards radially by radiation <span class="hlt">pressure</span> at velocities ∼5 km s-1, which implies a dust replenishment rate of ∼3 × 10-9 M⊙ yr-1. This replenishment rate is consistent with <span class="hlt">observational</span> estimates to within uncertainties. Coupling between the radial motion of the dust and gas is weak and hence the gas does not share in this rapid outward motion. Overall, we conclude that radiation <span class="hlt">pressure</span> is a capable and necessary mechanism to explain the <span class="hlt">observed</span> rotation <span class="hlt">profile</span> of L2 Pup, and offers other additional constraints on the dust properties.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2012AGUFM.C31B0612B','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2012AGUFM.C31B0612B"><span><span class="hlt">Observations</span> of Fabric Development in Polycrystalline Ice at Basal <span class="hlt">Pressures</span>: Methods and Initial Results</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Breton, D. J.; Baker, I.; Cole, D. M.</p> <p>2012-12-01</p> <p>Understanding and predicting the flow of polycrystalline ice is crucial to ice sheet modeling and paleoclimate reconstruction from ice cores. Ice flow rates depend strongly on the fabric (i.e. the distribution of grain sizes and crystallographic orientations) which evolves over time and enhances the flow rate in the direction of applied stress. The mechanisms for fabric evolution in ice have been extensively studied at atmospheric <span class="hlt">pressures</span>, but little work has been done to <span class="hlt">observe</span> these processes at the high <span class="hlt">pressures</span> experienced deep within ice sheets where long-term changes in ice rheology are expected to have significance. We conducted compressive creep tests on a 917 kg m-3 polycrystalline ice specimen at 20 MPa hydrostatic <span class="hlt">pressure</span>, thus simulating ~2,000 m depth. Initial specimen grain orientations were random, typical grain diameters were 1.2 mm, and the applied creep stress was 0.3 MPa. Subsequent microstructural analyses on the deformed specimen and a similarly prepared, undeformed specimen allowed characterization of crystal fabric evolution under <span class="hlt">pressure</span>. Our microstructural analysis technique simultaneously collected grain shape and size data from Scanning Electron Microscope (SEM) micrographs and obtained crystallographic orientation data via Electron BackScatter Diffraction (EBSD). Combining these measurements allows rapid analysis of the ice fabric over large numbers of grains, yielding statistically useful numbers of grain size and full c- and a-axis grain orientation data. The combined creep and microstructural data demonstrate <span class="hlt">pressure</span>-dependent effects on the mechanical and microstructural evolution of polycrystalline ice. We discuss possible mechanisms for the <span class="hlt">observed</span> phenomena, and future directions for hydrostatic creep testing.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017EGUGA..1916285M','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017EGUGA..1916285M"><span>Influence of wind-induced air <span class="hlt">pressure</span> fluctuations on topsoil gas concentrations within a Scots pine forest</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Mohr, Manuel; Laemmel, Thomas; Maier, Martin; Schindler, Dirk</p> <p>2017-04-01</p> <p>Commonly it is assumed that soil gas transport is dominated by molecular diffusion. Few recent studies indicate that the atmosphere above the soil triggers non-diffusive gas transport processes in the soil, which can enhance soil gas transport and therefore soil gas efflux significantly. During high wind speed conditions, the so called <span class="hlt">pressure</span> pumping effect has been <span class="hlt">observed</span>: the enhancement of soil gas transport through dynamic changes in the air <span class="hlt">pressure</span> field above the soil. However, the amplitudes and frequencies of the air <span class="hlt">pressure</span> fluctuations responsible for <span class="hlt">pressure</span> pumping are still uncertain. Moreover, an in situ <span class="hlt">observation</span> of the <span class="hlt">pressure</span> pumping effect is still missing. To investigate the <span class="hlt">pressure</span> pumping effect, airflow measurements above and below the canopy of a Scots pine forest and high-precision relative air <span class="hlt">pressure</span> measurements were conducted in the below-canopy space and in the soil over a measurement period of 16 weeks. To monitor the soil gas transport, a newly developed gas measurement system was used. The gas measurement system continuously injects helium as a tracer gas into the soil until a diffusive steady state is reached. With the steady state concentration <span class="hlt">profile</span> of the tracer gas, it is possible to inversely model the gas diffusion coefficient <span class="hlt">profile</span> of the soil. If the gas diffusion coefficient <span class="hlt">profile</span> differed from steady state, we deduced that the soil gas transport is not only diffusive, but also influenced by non-diffusive processes. Results show that the occurrence of small air <span class="hlt">pressure</span> fluctuations is strongly dependent on the mean above-canopy wind speed. The wind-induced air <span class="hlt">pressure</span> fluctuations have mean amplitudes up to 10 Pa and lie in the frequency range 0.01-0.1 Hz. To describe the pumping motion of the air <span class="hlt">pressure</span> field, the <span class="hlt">pressure</span> pumping coefficient (PPC) was defined as the mean change in <span class="hlt">pressure</span> per second. The PPC shows a clear quadratic dependence on mean above-canopy wind speed. Empirical modelling of</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2013ApJ...776...73A','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2013ApJ...776...73A"><span>Distribution of CO2 in Saturn's Atmosphere from Cassini/cirs Infrared <span class="hlt">Observations</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Abbas, M. M.; LeClair, A.; Woodard, E.; Young, M.; Stanbro, M.; Flasar, F. M.; Kunde, V. G.; Achterberg, R. K.; Bjoraker, G.; Brasunas, J.; Jennings, D. E.; the Cassini/CIRS Team</p> <p>2013-10-01</p> <p>This paper focuses on the CO2 distribution in Saturn's atmosphere based on analysis of infrared spectral <span class="hlt">observations</span> of Saturn made by the Composite Infrared Spectrometer aboard the Cassini spacecraft. The Cassini spacecraft was launched in 1997 October, inserted in Saturn's orbit in 2004 July, and has been successfully making infrared <span class="hlt">observations</span> of Saturn, its rings, Titan, and other icy satellites during well-planned orbital tours. The infrared <span class="hlt">observations</span>, made with a dual Fourier transform spectrometer in both nadir- and limb-viewing modes, cover spectral regions of 10-1400 cm-1, with the option of variable apodized spectral resolutions from 0.53 to 15 cm-1. An analysis of the <span class="hlt">observed</span> spectra with well-developed radiative transfer models and spectral inversion techniques has the potential to provide knowledge of Saturn's thermal structure and composition with global distributions of a series of gases. In this paper, we present an analysis of a large <span class="hlt">observational</span> data set for retrieval of Saturn's CO2 distribution utilizing spectral features of CO2 in the Q-branch of the ν2 band, and discuss its possible relationship to the influx of interstellar dust grains. With limited spectral regions available for analysis, due to low densities of CO2 and interference from other gases, the retrieved CO2 <span class="hlt">profile</span> is obtained as a function of a model photochemical <span class="hlt">profile</span>, with the retrieved values at atmospheric <span class="hlt">pressures</span> in the region of ~1-10 mbar levels. The retrieved CO2 <span class="hlt">profile</span> is found to be in good agreement with the model <span class="hlt">profile</span> based on Infrared Space Observatory measurements with mixing ratios of ~4.9 × 10-10 at atmospheric <span class="hlt">pressures</span> of ~1 mbar.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2008AGUFMOS31A1232J','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2008AGUFMOS31A1232J"><span>Long-Term <span class="hlt">Observations</span> of Ocean Biogeochemistry with Nitrate and Oxygen Sensors in Apex <span class="hlt">Profiling</span> Floats</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Johnson, K. S.; Coletti, L.; Jannasch, H.; Martz, T.; Swift, D.; Riser, S.</p> <p>2008-12-01</p> <p>Long-term, autonomous <span class="hlt">observations</span> of ocean biogeochemical cycles are now feasible with chemical sensors in <span class="hlt">profiling</span> floats. These sensors will enable decadal-scale <span class="hlt">observations</span> of trends in global ocean biogeochemical cycles. Here, we focus on measurements on nitrate and dissolved oxygen. The ISUS (In Situ Ultraviolet Spectrophotometer) optical nitrate sensor has been adapted to operate in a Webb Research, Apex <span class="hlt">profiling</span> float. The Apex float is of the type used in the Argo array and is designed for multi-year, expendable deployments in the ocean. Floats park at 1000 m depth and make 60 nitrate and oxygen measurements at depth intervals ranging from 50 m below 400 m to 5 m in the upper 100 m as they <span class="hlt">profile</span> to the surface. All data are transmitted to shore using the Iridium telemetry system and they are available on the Internet in near-real time. Floats equipped with ISUS and an Aanderaa oxygen sensor are capable of making 280 vertical <span class="hlt">profiles</span> from 1000 m. At a 5 day cycle time, the floats should have nearly a four year endurance. Three floats have now been deployed at the Hawaii Ocean Time series station (HOT), Ocean Station Papa (OSP) in the Gulf of Alaska and at 50 South, 30 East in the Southern Ocean. Two additional floats are designated for deployment at the Bermuda Atlantic Time Series station (BATS) and in the Drake Passage. The HOT float has made 56 <span class="hlt">profiles</span> over 260 days and should continue operating for 3 more years. Nitrate concentrations are in excellent agreement with the long-term mean <span class="hlt">observed</span> at HOT. No significant long-term drift in sensor response has occurred. A variety of features have been <span class="hlt">observed</span> in the HOT nitrate data that are linked to contemporaneous changes in oxygen production and mesoscale dynamics. The impacts of these features will be briefly described. The Southern Ocean float has operated for 200 days and is now <span class="hlt">observing</span> reinjection of nitrate into surface waters as winter mixing occurs(surface nitrate > 24 micromolar). We</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://ntrs.nasa.gov/search.jsp?R=20080036248&hterms=Wrf&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D50%26Ntt%3DWrf','NASA-TRS'); return false;" href="https://ntrs.nasa.gov/search.jsp?R=20080036248&hterms=Wrf&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D50%26Ntt%3DWrf"><span>Assimilation of Atmospheric InfraRed Sounder (AIRS) <span class="hlt">Profiles</span> using WRF-Var</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Zavodsky, Brad; Jedlovec, Gary J.; Lapenta, William</p> <p>2008-01-01</p> <p>The Weather Research and Forecasting (WRF) model contains a three-dimensional variational (3DVAR) assimilation system (WRF-Var), which allows a user to join data from multiple sources into one coherent analysis. WRF-Var combines <span class="hlt">observations</span> with a background field traditionally generated using a previous model forecast through minimization of a cost function. In data sparse regions, remotely-sensed <span class="hlt">observations</span> may be able to improve analyses and produce improved forecasts. One such source comes from the Atmospheric Infrared Sounder (AIRS), which together with the Advanced Microwave Sounding Unit (AMSU), represents one of the most advanced space-based atmospheric sounding systems. The combined AIRS/AMSU system provides radiance measurements used as input to a sophisticated retrieval scheme which has been shown to produce temperature <span class="hlt">profiles</span> with an accuracy of 1 K over 1 km layers and humidity <span class="hlt">profiles</span> with accuracy of 15% in 2 km layers in both clear and partly cloudy conditions. The retrieval algorithm also provides estimates of the accuracy of the retrieved values at each <span class="hlt">pressure</span> level, allowing the user to select <span class="hlt">profiles</span> based on the required error tolerances of the application. The purpose of this paper is to describe a procedure to optimally assimilate high-resolution AIRS <span class="hlt">profile</span> data into a regional configuration of the Advanced Research WRF (ARW) version 2.2 using WRF-Var. The paper focuses on development of background error covariances for the regional domain and background field type using gen_be and an optimal methodology for ingesting AIRS temperature and moisture <span class="hlt">profiles</span> as separate overland and overwater retrievals with different error characteristics in the WRF-Var. The AIRS thermodynamic <span class="hlt">profiles</span> are obtained from the version 5.0 Earth <span class="hlt">Observing</span> System (EOS) science team retrieval algorithm and contain information about the quality of each temperature layer. The quality indicators are used to select the highest quality temperature and moisture</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2015IJAEO..37..124N','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2015IJAEO..37..124N"><span>Satellite Earth <span class="hlt">observation</span> data to identify anthropogenic <span class="hlt">pressures</span> in selected protected areas</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Nagendra, Harini; Mairota, Paola; Marangi, Carmela; Lucas, Richard; Dimopoulos, Panayotis; Honrado, João Pradinho; Niphadkar, Madhura; Mücher, Caspar A.; Tomaselli, Valeria; Panitsa, Maria; Tarantino, Cristina; Manakos, Ioannis; Blonda, Palma</p> <p>2015-05-01</p> <p>Protected areas are experiencing increased levels of human <span class="hlt">pressure</span>. To enable appropriate conservation action, it is critical to map and monitor changes in the type and extent of land cover/use and habitat classes, which can be related to human <span class="hlt">pressures</span> over time. Satellite Earth <span class="hlt">observation</span> (EO) data and techniques offer the opportunity to detect such changes. Yet association with field information and expert interpretation by ecologists is required to interpret, qualify and link these changes to human <span class="hlt">pressure</span>. There is thus an urgent need to harmonize the technical background of experts in the field of EO data analysis with the terminology of ecologists, protected area management authorities and policy makers in order to provide meaningful, context-specific value-added EO products. This paper builds on the DPSIR framework, providing a terminology to relate the concepts of state, <span class="hlt">pressures</span>, and drivers with the application of EO analysis. The type of <span class="hlt">pressure</span> can be inferred through the detection of changes in state (i.e. changes in land cover and/or habitat type and/or condition). Four broad categories of changes in state are identified, i.e. land cover/habitat conversion, land cover/habitat modification, habitat fragmentation and changes in landscape connectivity, and changes in plant community structure. These categories of change in state can be mapped through EO analyses, with the goal of using expert judgement to relate changes in state to causal direct anthropogenic <span class="hlt">pressures</span>. Drawing on expert knowledge, a set of protected areas located in diverse socio-ecological contexts and subject to a variety of <span class="hlt">pressures</span> are analysed to (a) link the four categories of changes in state of land cover/habitats to the drivers (anthropogenic <span class="hlt">pressure</span>), as relevant to specific target land cover and habitat classes; (b) identify (for <span class="hlt">pressure</span> mapping) the most appropriate spatial and temporal EO data sources as well as interpretations from ecologists and field data</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2018PlST...20c5402Y','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2018PlST...20c5402Y"><span>Self-organized pattern on the surface of a metal anode in low-<span class="hlt">pressure</span> DC discharge</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Yaqi, YANG; Weiguo, LI</p> <p>2018-03-01</p> <p>Self-organization phenomena on the surface of a metal electrode in low-<span class="hlt">pressure</span> DC discharge is studied. In this paper, we carry out laboratory investigations of self-organization in a low-<span class="hlt">pressure</span> test platform for 100-200 mm rod-plane gaps with a needle tip, conical tip and hemispherical tip within 1-10 kPa. The factors influencing the pattern <span class="hlt">profile</span> are the <span class="hlt">pressure</span> value, gap length and shape of the electrode, and a variety of pattern structures are <span class="hlt">observed</span> by changing these factors. With increasing <span class="hlt">pressure</span>, first the pattern diameter increases and then decreases. With the needle tip, layer structure, single-ring structure and double-ring structure are displayed successively with increasing <span class="hlt">pressure</span>. With the conical tip, the ring-like structure gradually forms separate spots with increasing <span class="hlt">pressure</span>. With the hemispherical tip, there are anode spots inside the ring structure. With the increase of gap length, the diameter of the self-organized pattern increases and the <span class="hlt">profile</span> of the pattern changes. The development process of the pattern contains three key stages: pattern enlargement, pattern stabilization and pattern shrink.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2006AGUFM.V41B1722B','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2006AGUFM.V41B1722B"><span>Significance of Dynamic Pore <span class="hlt">Pressure</span> Variations - Comparison of <span class="hlt">Observations</span> on Mud Volcanoes on the Costa Rica Margin and in the Gulf of Cadiz</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Brueckmann, W.; Linke, P.; Pieper, M.; Hensen, C.; Tuerk, M.</p> <p>2006-12-01</p> <p>Research in the cooperative research center (SFB) 574 "Volatiles and Fluids in Subduction Zones" at the University Kiel focuses on volatile and fluid exchange processes at subduction zones. These have a significant impact on the long-term geochemical evolution of the hydrosphere and atmosphere. In the SFB 574 working area off Central America more than 120 mud volcanoes, mud diapirs and cold seeps have been identified and sampled. To better understand the internal dynamics of these structures and the temporal variability of fluid expulsion an in-situ tool for monitoring shallow pore <span class="hlt">pressure</span> variations was devised. The tool (PWPL) monitors pore <span class="hlt">pressure</span> variations along a 2m <span class="hlt">profile</span> in the shallow subsurface using a stinger with 4 <span class="hlt">pressure</span> ports. Positioned with a video-guided lander the stinger is gently pushed into the seafloor where it remains for several weeks or months in autonomous mode before being retrieved. While particular emphasis was placed on the convergent margin of Central America, mud volcanoes in other tectonic settings suitable for long-term <span class="hlt">observations</span> of fluid flux are used for comparison. Here we will present data and interpretations from two mud volcanoes off Costa Rica and in the Gulf of Cadiz where we have conducted successful tests. Pore <span class="hlt">pressure</span> data from short-term tests on Mound 11 on the continental slope off Costa Rica are compared with new results from a long-term (3-month) campaign on the Captain Arutjunov deep water mud volcano in the Gulf of Cadiz. Rates of fluid flow at both structures have been thoroughly characterized and quantified with geochemical methods providing a frame of reference for judging the significance of dynamic pore <span class="hlt">pressure</span> variations.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/22128539','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/22128539"><span>Characteristics of ozone vertical <span class="hlt">profile</span> <span class="hlt">observed</span> in the boundary layer around Beijing in autumn.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Ma, Zhiqiang; Zhang, Xiaoling; Xu, Jing; Zhao, Xiujuan; Meng, Wei</p> <p>2011-01-01</p> <p>In the autumn of 2008, the vertical <span class="hlt">profiles</span> of ozone and meteorological parameters in the low troposphere (0-1000 m) were <span class="hlt">observed</span> at two sites around Beijing, specifically urban Nanjiao and rural Shangdianzi. At night and early morning, the lower troposphere divided into two stratified layers due to temperature inversion. Ozone in the lower layer showed a large gradient due to the titration of NO. Air flow from the southwest brought ozone-rich air to Beijing, and the ozone <span class="hlt">profiles</span> were marked by a continuous increase in the residual layer at night. The accumulated ozone in the upper layer played an important role in the next day's surface peak ozone concentration, and caused a rapid increase in surface ozone in the morning. Wind direction shear and wind speed shear exhibited different influences on ozone <span class="hlt">profiles</span> and resulted in different surface ozone concentrations in Beijing.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/1987JGR....9212389B','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/1987JGR....9212389B"><span>Geocoronal structure. 3. Optically thin, Doppler-broadened line <span class="hlt">profiles</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Bishop, James; Chamberlain, Joseph W.</p> <p>1987-11-01</p> <p>Theoretical line <span class="hlt">profiles</span>, applicable to the analysis of geocoronal Hα prifile measurements, are presented for illustrative cases. While retaining a number of simplifications (classical exobase and diffusive equilibrium plasmasphere conditions), distinctive spectral signatures of mechanisms governing the geocorona are isolated. Examining the consequences of solar radiation <span class="hlt">pressure</span> dynamics is the main point here. In the prototype evaporative case, radiation <span class="hlt">pressure</span> acts to form narrow <span class="hlt">profiles</span> via the creation of an extensive quasi-satellite component. Comparison with a simple extension of the earlier analytic theory discloses the influence of an exopause in this regard. The main modifications to evaporative spectral shapes in the geocoronal application, for shadow heights greater than 2 RE, are predicted to be (1) a blueward ``shift'' or bias near line center, for look directions parallel to the antisolar axis, generated by loss mechanisms acting over the time of flight of exospheric constituents (for example, solar ionization) and (2) an enhanced redward wing at spectral displacements exceeding that defined by the shadow height escape speed, produced by plasmaspheric charge exchange collisions. Implications of these results for recent <span class="hlt">observations</span> of geocoronal Hα line <span class="hlt">profiles</span> are briefly discussed.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/23736112','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/23736112"><span>Effects of antihypertensive drugs on central blood <span class="hlt">pressure</span> in humans: a preliminary <span class="hlt">observation</span>.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Agnoletti, Davide; Zhang, Yi; Borghi, Claudio; Blacher, Jacques; Safar, Michel E</p> <p>2013-08-01</p> <p>Central blood <span class="hlt">pressure</span> (BP) is considered a better predictor of cardiovascular events than brachial BP. Modifications of central, beyond brachial BP, can be assessed by <span class="hlt">pressure</span> amplification, a potential new cardiovascular risk factor. Comparison between drugs' effect on central hemodynamics has been poorly studied. Our aim was to assess the hemodynamic effect of a 12-week treatment with amlodipine 5mg, or candesartan 8mg, or indapamide sustained-release 1.5mg, in comparison with placebo. We analyzed 145 out-patients with essential hypertension in primary prevention enrolled in the Natrilix SR Versus Candesartan and Amlodipine in the Reduction of Systolic Blood <span class="hlt">Pressure</span> in Hypertensive Patients (X-CELLENT) study, a multicenter, randomized, double-blinded, placebo-controlled trial. Arterial stiffness, central BP, <span class="hlt">pressure</span> amplification, and wave reflection were measured by applanation tonometry. Baseline characteristics of patients were homogeneous between groups. After treatment, we found that active drugs produced similar reduction of both central and peripheral BPs, with no significant interdrug differences (all P < 0.05; excluded peripheral pulse <span class="hlt">pressure</span>, compared with placebo). Second, amlodipine (1.9% ± 15.3%), candesartan (3.0% ± 14.6%) and indapamide (4.1% ± 14.4%) all increased pulse <span class="hlt">pressure</span> amplification, but only indapamide was statistically different from placebo (P = 0.02). Finally, no significant changes were <span class="hlt">observed</span> on pulse wave velocity, heart rate, and augmentation index. The 3 antihypertensive drugs similarly reduced peripheral and central BP, as compared with placebo, but a significant increase in pulse <span class="hlt">pressure</span> amplification was obtained only with indapamide, independently of arterial stiffness modifications. 3283161 by BIOPHARMA.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://ntrs.nasa.gov/search.jsp?R=20090007695&hterms=taylor&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAuthor-Name%26N%3D0%26No%3D30%26Ntt%3Dtaylor%2Bt%2Bb','NASA-TRS'); return false;" href="https://ntrs.nasa.gov/search.jsp?R=20090007695&hterms=taylor&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAuthor-Name%26N%3D0%26No%3D30%26Ntt%3Dtaylor%2Bt%2Bb"><span>Assessment of the Quality of the Version 1.07 Temperature-Versus-<span class="hlt">Pressure</span> <span class="hlt">Profiles</span> of the Middle Atmosphere from TIMED/SABER</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Remsberg, E. E.; Marshall, B. T.; Garcia-Comas, M.; Krueger, D.; Lingenfelser, G. S.; Martin-Torres, J.; Mlynczak, M. G.; Russell, J. M., III; Smith, A. K.; Zhao, Y.; <a style="text-decoration: none; " href="javascript:void(0); " onClick="displayelement('author_20090007695'); toggleEditAbsImage('author_20090007695_show'); toggleEditAbsImage('author_20090007695_hide'); "> <img style="display:inline; width:12px; height:12px; " src="images/arrow-up.gif" width="12" height="12" border="0" alt="hide" id="author_20090007695_show"> <img style="width:12px; height:12px; display:none; " src="images/arrow-down.gif" width="12" height="12" border="0" alt="hide" id="author_20090007695_hide"></p> <p>2008-01-01</p> <p>The quality of the retrieved temperature-versus-<span class="hlt">pressure</span> (or T(p)) <span class="hlt">profiles</span> is described for the middle atmosphere for the publicly available Sounding of the Atmosphere using Broadband Emission Radiometry (SABER) Version 1.07 (V1.07) data set. The primary sources of systematic error for the SABER results below about 70 km are (1) errors in the measured radiances, (2) biases in the forward model, and (3) uncertainties in the corrections for ozone and in the determination of the reference <span class="hlt">pressure</span> for the retrieved <span class="hlt">profiles</span>. Comparisons with other correlative data sets indicate that SABER T(p) is too high by 1-3 K in the lower stratosphere but then too low by 1 K near the stratopause and by 2 K in the middle mesosphere. There is little difference between the local thermodynamic equilibrium (LTE) algorithm results below about 70 km from V1.07 and V1.06, but there are substantial improvements/differences for the non-LTE results of V1.07 for the upper mesosphere and lower thermosphere (UMLT) region. In particular, the V1.07 algorithm uses monthly, diurnally averaged CO2 <span class="hlt">profiles</span> versus latitude from the Whole Atmosphere Community Climate Model. This change has improved the consistency of the character of the tides in its kinetic temperature (T(sub k)). The T(sub k) <span class="hlt">profiles</span> agree with UMLT values obtained from ground-based measurements of column-averaged OH and O2 emissions and of the Na lidar returns, at least within their mutual uncertainties. SABER T(sub k) values obtained near the mesopause with its daytime algorithm also agree well with the falling sphere climatology at high northern latitudes in summer. It is concluded that the SABER data set can be the basis for improved, diurnal-to-interannual-scale temperatures for the middle atmosphere and especially for its UMLT region.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://ntrs.nasa.gov/search.jsp?R=19820048714&hterms=oso&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D20%26Ntt%3Doso','NASA-TRS'); return false;" href="https://ntrs.nasa.gov/search.jsp?R=19820048714&hterms=oso&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D20%26Ntt%3Doso"><span>Evidence of redshifts in the average solar line <span class="hlt">profiles</span> of C IV and Si IV from OSO-8 <span class="hlt">observations</span></span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Roussel-Dupre, D.; Shine, R. A.</p> <p>1982-01-01</p> <p>Line <span class="hlt">profiles</span> of C IV and Si V obtained by the Colorado spectrometer on OSO-8 are presented. It is shown that the mean <span class="hlt">profiles</span> are redshifted with a magnitude varying from 6-20 km/s, and with a mean of 12 km/s. An apparent average downflow of material in the 50,000-100,000 K temperature range is measured. The redshifts are <span class="hlt">observed</span> in the line center positions of spatially and temporally averaged <span class="hlt">profiles</span> and are measured either relative to chromospheric Si I lines or from a comparison of sun center and limb <span class="hlt">profiles</span>. The <span class="hlt">observations</span> of 6-20 km/s redshifts place constraints on the mechanisms that dominate EUV line emission since it requires a strong weighting of the emission in regions of downward moving material, and since there is little evidence for corresponding upward moving materials in these lines.</p> </li> </ol> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_9");'>9</a></li> <li><a href="#" onclick='return showDiv("page_10");'>10</a></li> <li class="active"><span>11</span></li> <li><a href="#" onclick='return showDiv("page_12");'>12</a></li> <li><a href="#" onclick='return showDiv("page_13");'>13</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div><!-- col-sm-12 --> </div><!-- row --> </div><!-- page_11 --> <div id="page_12" class="hiddenDiv"> <div class="row"> <div class="col-sm-12"> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_10");'>10</a></li> <li><a href="#" onclick='return showDiv("page_11");'>11</a></li> <li class="active"><span>12</span></li> <li><a href="#" onclick='return showDiv("page_13");'>13</a></li> <li><a href="#" onclick='return showDiv("page_14");'>14</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div> </div> <div class="row"> <div class="col-sm-12"> <ol class="result-class" start="221"> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/21207038','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/21207038"><span><span class="hlt">Pressure</span> <span class="hlt">profile</span> and morphology of the arteries along the giraffe limb.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Østergaard, Kristine Hovkjaer; Bertelsen, Mads F; Brøndum, Emil T; Aalkjaer, Christian; Hasenkam, J Michael; Smerup, Morten; Wang, Tobias; Nyengaard, Jens Randel; Baandrup, Ulrik</p> <p>2011-07-01</p> <p>Giraffes are the tallest animals on earth and the effects of gravity on their cardiovascular system have puzzled physiologists for centuries. The authors measured arterial and venous <span class="hlt">pressure</span> in the foreleg of anesthetized giraffes, suspended in upright standing position, and determined the ratio between tunica media and lumen areas along the length of the femoral/tibial arteries in the hindleg. Volume fraction of elastin, density of vasa vasorum and innervations was estimated by stereology. Immunohistological staining with S100 was used to examine the innervation. The <span class="hlt">pressure</span> increase in the artery and vein along the foreleg was not significantly different from what was expected on basis of gravity. The area of the arterial lumen in the hindleg decreased towards the hoof from 11.2 ± 4.2 to 0.6 ± 0.5 mm(2) (n = 10, P = 0.001), but most of this narrowing occurred within 2-4 cm immediately below the knee. This abrupt narrowing was associated with a marked increase in media to lumen area ratio (from 1.2 ± 0.5 to 7.8 ± 2.5; P = 0.001), and a decrease in mean volume fraction of elastin from 38 ± 6% proximal to the narrowing to 5.8 ± 1.1% distally (P = 0.001). The narrowing had a six-fold higher innervation density than the immediate distal and proximal regions. The sudden narrowing was also <span class="hlt">observed</span> in the hind legs of neonates, indicating that it does not develop as an adaptation to the high transmural <span class="hlt">pressure</span> in the standing giraffe. More likely it represents a preadaptation to the high <span class="hlt">pressures</span> experienced by adult giraffes.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/23116535','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/23116535"><span>Effects of supervised exercise on lipid <span class="hlt">profiles</span> and blood <span class="hlt">pressure</span> control in people with type 2 diabetes mellitus: a meta-analysis of randomized controlled trials.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Hayashino, Yasuaki; Jackson, Jeffrey L; Fukumori, Norio; Nakamura, Fumiaki; Fukuhara, Shunichi</p> <p>2012-12-01</p> <p>Our study's purpose was to perform a systematic review to assess the effect of supervised exercise interventions on lipid <span class="hlt">profiles</span> and blood <span class="hlt">pressure</span> control. We searched electronic databases and selected studies that evaluated the effect of supervised exercise intervention on cardiovascular risk factors in adult people with type 2 diabetes. We used random effect models to derive weighted mean differences of exercise on lipid <span class="hlt">profiles</span> and blood <span class="hlt">pressure</span> control. Forty-two RCTs (2808 subjects) met inclusion criteria and are included in our meta-analysis. Structured exercise was associated with a change in systolic blood <span class="hlt">pressure</span> (SBP) of -2.42 mmHg (95% CI, -4.39 to -0.45 mmHg), diastolic blood <span class="hlt">pressure</span> (DBP) of -2.23 mmHg (95% CI, -3.21 to -1.25 mmHg), high-density lipoprotein cholesterol (HDL-C) of 0.04 mmol/L (95% CI, 0.02-0.07 mmol/L), and low-density lipoprotein cholesterol (LDL-C) of -0.16 mmol/L (95% CI, -0.30 to -0.01 mmol/L). Heterogeneity was partially explained by age, dietary co-intervention and the duration and intensity of the exercise. Supervised exercise is effective in improving blood <span class="hlt">pressure</span> control, lowering LDL-C, and elevating HDL-C levels in people with diabetes. Physicians should recommend exercise for their adult patients with diabetes who can safely do so. Copyright © 2012 Elsevier Ireland Ltd. All rights reserved.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2014hitr.confE..22L','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2014hitr.confE..22L"><span>Spectral Line-Shape Model to Replace the Voigt <span class="hlt">Profile</span> in Spectroscopic Databases</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Lisak, Daniel; Ngo, Ngoc Hoa; Tran, Ha; Hartmann, Jean-Michel</p> <p>2014-06-01</p> <p>The standard description of molecular line shapes in spectral databases and radiative transfer codes is based on the Voigt <span class="hlt">profile</span>. It is well known that its simplified assumptions of absorber free motion and independence of collisional parameters from absorber velocity lead to systematic errors in analysis of experimental spectra, and retrieval of gas concentration. We demonstrate1,2 that the partially correlated quadratic speed-dependent hardcollision <span class="hlt">profile</span>3. (pCqSDHCP) is a good candidate to replace the Voigt <span class="hlt">profile</span> in the next generations of spectroscopic databases. This <span class="hlt">profile</span> takes into account the following physical effects: the Doppler broadening, the <span class="hlt">pressure</span> broadening and shifting of the line, the velocity-changing collisions, the speed-dependence of <span class="hlt">pressure</span> broadening and shifting, and correlations between velocity- and phase/state-changing collisions. The speed-dependence of <span class="hlt">pressure</span> broadening and shifting is incorporated into the pCqSDNGP in the so-called quadratic approximation. The velocity-changing collisions lead to the Dicke narrowing effect; however in many cases correlations between velocityand phase/state-changing collisions may lead to effective reduction of <span class="hlt">observed</span> Dicke narrowing. The hard-collision model of velocity-changing collisions is also known as the Nelkin-Ghatak model or Rautian model. Applicability of the pCqSDHCP for different molecular systems was tested on calculated and experimental spectra of such molecules as H2, O2, CO2, H2O in a wide span of <span class="hlt">pressures</span>. For all considered systems, pCqSDHCP is able to describe molecular spectra at least an order of magnitude better than the Voigt <span class="hlt">profile</span> with all fitted parameters being linear with <span class="hlt">pressure</span>. In the most cases pCqSDHCP can reproduce the reference spectra down to 0.2% or better, which fulfills the requirements of the most demanding remote-sensing applications. An important advantage of pCqSDHCP is that a fast algorithm for its computation was developedab4,5 and allows</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/20329371','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/20329371"><span>Sympathovagal imbalance in thyroid dysfunctions in females: correlation with thyroid <span class="hlt">profile</span>, heart rate and blood <span class="hlt">pressure</span>.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Karthik, S; Pal, G K; Nanda, Nivedita; Hamide, Abdoul; Bobby, Zachariah; Amudharaj, D; Pal, Pravati</p> <p>2009-01-01</p> <p>The aim of the study was to investigate the role of spectral analysis of heart rate variability (HRV) for assessing the type and degree of sympathovagal imbalance (SVI) and their link to cardiovascular morbidities in thyroid dysfunctions. Forty-five female subjects (15 control subjects and freshly diagnosed untreated 15 hypothyroid and 15 hyperthyroid patients) were recruited for the study. Thyroid <span class="hlt">profile</span>, body mass index (BMI), basal heart rate (BHR), blood <span class="hlt">pressure</span> (BP) and spectral indices of HRV (TP, LFnu, HFnu and LF-HF ratio, mean RR, SDNN and RMSSD) were assessed in all the three groups. LF-HF ratio was correlated with thyroid <span class="hlt">profile</span>, BMI, BHR and BP. SVI was more prominent in hyperthyroid (P < 0.001) compared to hypothyroid (P < 0.05) subjects. LF-HF ratio was correlated with thyroid <span class="hlt">profile</span> in both hypo and hyperthyroid subjects; but correlation with BHR and BP was significant only in hyperthyroidism. Though the SVI was found to be due to both vagal withdrawal and sympathetic activation, especially in hyperthyroidism, contribution by vagal inhibition was prominent. Vagal inhibition contributes significantly to SVI in thyroid dysfunctions, especially in hyperthyroidism. As the present study indicates poor cardiovascular health due to vagal inhibition in patients suffering from thyroid dysfunctions, attempt should be made to improve vagal tone especially in hyperthyroid subjects to attain a stable sympathovagal and cardiovascular homeostasis.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2018Icar..307..161K','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2018Icar..307..161K"><span>Atmospheric structure and helium abundance on Saturn from Cassini/UVIS and CIRS <span class="hlt">observations</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Koskinen, T. T.; Guerlet, S.</p> <p>2018-06-01</p> <p>We combine measurements from stellar occultations <span class="hlt">observed</span> by the Cassini Ultraviolet Imaging Spectrograph (UVIS) and limb scans <span class="hlt">observed</span> by the Composite Infrared Spectrometer (CIRS) to create empirical atmospheric structure models for Saturn corresponding to the locations probed by the occultations. The results cover multiple locations at low to mid-latitudes between the spring of 2005 and the fall of 2015. We connect the temperature-<span class="hlt">pressure</span> (T-P) <span class="hlt">profiles</span> retrieved from the CIRS limb scans in the stratosphere to the T-P <span class="hlt">profiles</span> in the thermosphere retrieved from the UVIS occultations. We calculate the altitudes corresponding to the <span class="hlt">pressure</span> levels in each case based on our best fit composition model that includes H2, He, CH4 and upper limits on H. We match the altitude structure to the density <span class="hlt">profile</span> in the thermosphere that is retrieved from the occultations. Our models depend on the abundance of helium and we derive a volume mixing ratio of 11 ± 2% for helium in the lower atmosphere based on a statistical analysis of the values derived for 32 different occultation locations. We also derive the mean temperature and methane <span class="hlt">profiles</span> in the upper atmosphere and constrain their variability. Our results are consistent with enhanced heating at the polar auroral region and a dynamically active upper atmosphere.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2016MMTA...47.5569M','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2016MMTA...47.5569M"><span>Modeling the Capillary <span class="hlt">Pressure</span> for the Migration of the Liquid Phase in Granular Solid-Liquid-Vapor Systems: Application to the Control of the Composition <span class="hlt">Profile</span> in W-Cu FGM Materials</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Missiaen, Jean-Michel; Raharijaona, Jean-Joël; Delannay, Francis</p> <p>2016-11-01</p> <p>A model is developed to compute the capillary <span class="hlt">pressure</span> for the migration of the liquid phase out or into a uniform solid-liquid-vapor system. The capillary <span class="hlt">pressure</span> is defined as the reduction of the overall interface energy per volume increment of the transferred fluid phase. The model takes into account the particle size of the solid particle aggregate, the packing configuration (coordination number, porosity), the volume fractions of the different phases, and the values of the interface energies in the system. The model is used for analyzing the stability of the composition <span class="hlt">profile</span> during processing of W-Cu functionally graded materials combining a composition gradient with a particle size gradient. The migration <span class="hlt">pressure</span> is computed with the model in two stages: (1) just after the melting of copper, i.e., when sintering and shape accommodation of the W particle aggregate can still be neglected and (2) at high temperature, when the system is close to full density with equilibrium particle shape. The model predicts well the different stages of liquid-phase migration <span class="hlt">observed</span> experimentally.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/28870547','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/28870547"><span>Association of Ambulatory Blood <span class="hlt">Pressure</span> Monitoring parameters with the Framingham Stroke Risk <span class="hlt">Profile</span>.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Tsivgoulis, Georgios; Pikilidou, Maria; Katsanos, Aristeidis H; Stamatelopoulos, Kimon; Michas, Fotios; Lykka, Aikaterini; Zompola, Christina; Filippatou, Angeliki; Boviatsis, Efstathios; Voumvourakis, Konstantinos; Zakopoulos, Nikolaos; Manios, Efstathios</p> <p>2017-09-15</p> <p>The Framingham Stroke Risk <span class="hlt">Profile</span> (FSRP) is a novel and reliable tool for estimating the 10-year probability for incident stroke in stroke-free individuals, while the predictive value of ambulatory blood <span class="hlt">pressure</span> monitoring (ABPM) for first-ever and recurrent stroke has been well established. We sought to evaluate cross-sectionally the association of ABPM parameters with FSRP score in a large sample of 2343 consecutive stroke-free individuals (mean age: 56.0±12.9, 49.1% male) who underwent 24-hour ABPM. True hypertensives showed significantly higher FSRP (11.2±5.0) compared to the normotensives (8.2±5.0, p<0.001), while subjects with white coat hypertension also had higher FSRP (10.2±4.7) than normotensives (8.2±5.0, p<0.001). Compared to dippers that exhibited the lowest FSRP, non-dippers and reverse-dippers exhibited significantly higher FSRP (9.8±4.8 for dippers vs 10.6±5.2 and 11.5±5.0 for non-dippers and reverse-dippers respectively, p≤0.001 for comparisons). In univariate analyses, the ABPM parameters that had the strongest correlation with FSRP were 24-hour (r=0.440, p<0.001), daytime (r=0.435, p<0.001) and night-time (r=0.423; p<0.001) pulse <span class="hlt">pressure</span> (PP). The best fitting model for predicting FSRP (R 2 =24.6%) on multiple linear regression analyses after adjustment for vascular risk factors not included in FSRP comprised the following parameters in descending order: 24-hour PP (β=0.349, p<0.001), daytime SBP variability (β=0.124, p<0.001), 24-hour HR variability (β=-0.091, p<0.001), mean 24-hour HR (β=-0.107, p<0.001), BMI (β=0.081, p<0.001) and dipping percentage (β=-0.063, p=0.001). 24-hour PP and daytime SBP variability are the two ABPM parameters that were more strongly associated with FSRP-score. Reverse dippers had the highest FSRP among all dipping status <span class="hlt">profiles</span>. Copyright © 2017 Elsevier B.V. All rights reserved.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017EGUGA..1915734M','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017EGUGA..1915734M"><span>Investigation of the spatial variability and possible origins of wind-induced air <span class="hlt">pressure</span> fluctuations responsible for <span class="hlt">pressure</span> pumping</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Mohr, Manuel; Laemmel, Thomas; Maier, Martin; Zeeman, Matthias; Longdoz, Bernard; Schindler, Dirk</p> <p>2017-04-01</p> <p>The exchange of greenhouse gases between the soil and the atmosphere is highly relevant for the climate of the Earth. Recent research suggests that wind-induced air <span class="hlt">pressure</span> fluctuations can alter the soil gas transport and therefore soil gas efflux significantly. Using a newly developed method, we measured soil gas transport in situ in a well aerated forest soil. Results from these measurements showed that the commonly used soil gas diffusion coefficient is enhanced up to 30% during periods of strong wind-induced air <span class="hlt">pressure</span> fluctuations. The air <span class="hlt">pressure</span> fluctuations above the forest floor are only induced at high above-canopy wind speeds (> 5 m s-1) and lie in the frequency range 0.01-0.1 Hz. Moreover, the amplitudes of air <span class="hlt">pressure</span> fluctuations in this frequency range show a clear quadratic dependence on mean above-canopy wind speed. However, the origin of these wind-induced <span class="hlt">pressure</span> fluctuations is still unclear. Airflow measurements and high-precision air <span class="hlt">pressure</span> measurements were conducted at three different vegetation-covered sites (conifer forest, deciduous forest, grassland) to investigate the spatial variability of dominant air <span class="hlt">pressure</span> fluctuations, their origin and vegetation-dependent characteristics. At the conifer forest site, a vertical <span class="hlt">profile</span> of air <span class="hlt">pressure</span> fluctuations was measured and an array consisting of five <span class="hlt">pressure</span> sensors were installed at the forest floor. At the grassland site, the air <span class="hlt">pressure</span> measurements were compared with wind <span class="hlt">observations</span> made by ground-based LIDAR and spatial temperature <span class="hlt">observations</span> from a fibre-optic sensing network (ScaleX Campaign 2016). Preliminary results show that at all sites the amplitudes of relevant air <span class="hlt">pressure</span> fluctuations increase with increasing wind speed. Data from the array measurements reveal that there are no time lags between the air <span class="hlt">pressure</span> signals of different heights, but a time lag existed between the air <span class="hlt">pressure</span> signals of the sensors distributed laterally on the forest floor</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://ntrs.nasa.gov/search.jsp?R=19780061652&hterms=1082&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D60%26Ntt%3D%2526%25231082','NASA-TRS'); return false;" href="https://ntrs.nasa.gov/search.jsp?R=19780061652&hterms=1082&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D60%26Ntt%3D%2526%25231082"><span>Sodium D-line emission from Io - Comparison of <span class="hlt">observed</span> and theoretical line <span class="hlt">profiles</span></span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Carlson, R. W.; Matson, D. L.; Johnson, T. V.; Bergstralh, J. T.</p> <p>1978-01-01</p> <p>High-resolution spectra of the D-line <span class="hlt">profiles</span> have been obtained for Io's sodium emission cloud. These lines, which are produced through resonance scattering of sunlight, are broad and asymmetric and can be used to infer source and dynamical properties of the sodium cloud. In this paper we compare line <span class="hlt">profile</span> data with theoretical line shapes computed for several assumed initial velocity distributions corresponding to various source mechanisms. We also examine the consequences of source distributions which are nonuniform over the surface of Io. It is found that the experimental data are compatible with escape of sodium atoms from the leading hemisphere of Io and with velocity distributions characteristic of sputtering processes. Thermal escape and simple models of plasma sweeping are found to be incompatible with the <span class="hlt">observations</span>.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://ntrs.nasa.gov/search.jsp?R=19920059644&hterms=taylor&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAuthor-Name%26N%3D0%26No%3D90%26Ntt%3Dtaylor%2Bt%2Bb','NASA-TRS'); return false;" href="https://ntrs.nasa.gov/search.jsp?R=19920059644&hterms=taylor&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAuthor-Name%26N%3D0%26No%3D90%26Ntt%3Dtaylor%2Bt%2Bb"><span>Atmosphere and climate studies of Mars using the Mars <span class="hlt">Observer</span> <span class="hlt">pressure</span> modulator infrared radiometer</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Mccleese, D. J.; Haskins, R. D.; Schofield, J. T.; Zurek, R. W.; Leovy, C. B.; Paige, D. A.; Taylor, F. W.</p> <p>1992-01-01</p> <p>Studies of the climate and atmosphere of Mars are limited at present by a lack of meteorological data having systematic global coverage with good horizontal and vertical resolution. The Mars <span class="hlt">Observer</span> spacecraft in a low, nearly circular, polar orbit will provide an excellent platform for acquiring the data needed to advance significantly our understanding of the Martian atmosphere and its remarkable variability. The Mars <span class="hlt">Observer</span> <span class="hlt">pressure</span> modulator infrared radiometer (PMIRR) is a nine-channel limb and nadir scanning atmospheric sounder which will <span class="hlt">observe</span> the atmosphere of Mars globally from 0 to 80 km for a full Martian year. PMIRR employs narrow-band radiometric channels and two <span class="hlt">pressure</span> modulation cells to measure atmospheric and surface emission in the thermal infrared. PMIRR infrared and visible measurements will be combined to determine the radiative balance of the polar regions, where a sizeable fraction of the global atmospheric mass annually condenses onto and sublimes from the surface. Derived meteorological fields, including diabatic heating and cooling and the vertical variation of horizontal winds, are computed from the globally mapped fields retrieved from PMIRR data.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2015JGRD..12011536D','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2015JGRD..12011536D"><span>Mesoscale kinematics derived from X-band Doppler radar <span class="hlt">observations</span> of convective versus stratiform precipitation and comparison with GPS radiosonde <span class="hlt">profiles</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Deshpande, Sachin M.; Dhangar, N.; Das, S. K.; Kalapureddy, M. C. R.; Chakravarty, K.; Sonbawne, S.; Konwar, M.</p> <p>2015-11-01</p> <p>Single Doppler analysis techniques known as velocity azimuth display (VAD) and volume velocity processing (VVP) are used to analyze kinematics of mesoscale flow such as horizontal wind and divergence using X-band Doppler weather radar <span class="hlt">observations</span>, for selected cases of convective, stratiform, and shallow cloud systems near tropical Indian sites Pune (18.58°N, 73.92°E, above sea level (asl) 560 m) and Mandhardev (18.51°N, 73.85°E, asl 1297 m). The vertical <span class="hlt">profiles</span> of horizontal wind estimated from radar VVP/VAD methods agree well with GPS radiosonde <span class="hlt">profiles</span>, with the low-level jet at about 1.5 km during monsoon season well depicted in both. The vertical structure and temporal variability of divergence and reflectivity <span class="hlt">profiles</span> are indicative of the dynamical and microphysical characteristics of shallow convective, deep convective, and stratiform cloud systems. In shallow convective systems, vertical development of reflectivity <span class="hlt">profiles</span> is limited below 5 km. In deep convective systems, reflectivity values as large as 55 dBZ were <span class="hlt">observed</span> above freezing level. The stratiform system shows the presence of a reflectivity bright band (~35 dBZ) near the melting level. The diagnosed vertical <span class="hlt">profiles</span> of divergence in convective and stratiform systems are distinct. In shallow convective conditions, convergence was seen below 4 km with divergence above. Low-level convergence and upper level divergence are <span class="hlt">observed</span> in deep convective <span class="hlt">profiles</span>, while stratiform precipitation has midlevel convergence present between lower level and upper level divergence. The divergence <span class="hlt">profiles</span> in stratiform precipitation exhibit intense shallow layers of "melting convergence" at 0°C level, near 4.5 km altitude, with a steep gradient on the both sides of the peak. The level of nondivergence in stratiform situations is lower than that in convective situations. These <span class="hlt">observed</span> vertical structures of divergence are largely indicative of latent heating <span class="hlt">profiles</span> in the atmosphere, an</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/28134672','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/28134672"><span>Effects of room environment and nursing experience on clinical blood <span class="hlt">pressure</span> measurement: an <span class="hlt">observational</span> study.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Zhang, Meng; Zhang, Xuemei; Chen, Fei; Dong, Birong; Chen, Aiqing; Zheng, Dingchang</p> <p>2017-04-01</p> <p>This study aimed to examine the effects of measurement room environment and nursing experience on the accuracy of manual auscultatory blood <span class="hlt">pressure</span> (BP) measurement. A training database with 32 Korotkoff sounds recordings from the British Hypertension Society was played randomly to 20 <span class="hlt">observers</span> who were divided into four groups according to the years of their nursing experience (i.e. ≥10 years, 1-9 years, nursing students with frequent training, and those without any medical background; five <span class="hlt">observers</span> in each group). All the <span class="hlt">observers</span> were asked to determine manual auscultatory systolic blood <span class="hlt">pressure</span> (SBP) and diastolic blood <span class="hlt">pressure</span> (DBP) both in a quiet clinical assessment room and in a noisy nurse station area. This procedure was repeated on another day, yielding a total of four measurements from each <span class="hlt">observer</span> (i.e. two room environments and two repeated determinations on 2 separate days) for each Korotkoff sound. The measurement error was then calculated against the reference answer, with the effects of room environment and nursing experience of the <span class="hlt">observer</span> investigated. Our results showed that there was no statistically significant difference for BPs measured under both quiet and noisy environments (P>0.80 for both SBP and DBP). However, there was a significant effect on the measurement accuracy between the <span class="hlt">observer</span> groups (P<0.001 for both SBP and DBP). The nursing students performed best with overall SBP and DBP errors of -0.8±2.4 and 0.1±1.8 mmHg, respectively. The SBP measurement error from the nursing students was significantly smaller than that for each of the other three groups (all P<0.001). Our results indicate that frequent nursing trainings are important for nurses to achieve accurate manual auscultatory BP measurement.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2011SPIE.8321E..28C','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2011SPIE.8321E..28C"><span>Analysis of microfluidic flow driven by electrokinetic and <span class="hlt">pressure</span> forces</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Chen, Chien-Hsin</p> <p>2011-12-01</p> <p>This work presents an analysis of microfluidic flow introduced by mixed electrokinetic force and <span class="hlt">pressure</span> gradient. Analytical solutions are presented for the case of constant surface heat flux, taking the Joule heating effect into account. The present problem is governed by two scale ratios and the dimensionless source term. The two important ratios are the length scale ratio e (the ratio of Debye length to the tube radius R) and the velocity scale ratio Γ (the ratio of the pressuredriven velocity scale for Poiseuille flow to Helmholtz-Smoluchowski velocity for electroosmotic flow). For mixed electroosmotic and <span class="hlt">pressure</span>-driven flow, the resulting velocity <span class="hlt">profile</span> is the superimposed effect of both electroosmotic and Poiseuille flow phenomena. It is found that the velocity <span class="hlt">profile</span> decreases as e increases and the normalized temperature <span class="hlt">profiles</span> across the tube increases monotonously form the core to the wall. The maximum dimensionless temperature is <span class="hlt">observed</span> at the wall and the wall temperature increases with increasing Joule heating. Also, the temperature is increased with increasing the value of ɛ . The fully developed Nusselt number takes the maximum value at the limiting case of ɛ --> 0 , and then decreases with increasing ɛ . Moreover, the Nusselt number decreases with Γ and then goes asymptotically to the limit of Poiseuille flow as Γ --> ∞ , where the flow is dominated by the <span class="hlt">pressure</span> force.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017APS..DPPN11005V','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017APS..DPPN11005V"><span>Catastrophic global-avalanche of a hollow <span class="hlt">pressure</span> filament</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>van Compernolle, B.; Poulos, M. J.; Morales, G. J.</p> <p>2017-10-01</p> <p>New results are presented of a basic heat transport experiment performed in the Large Plasma Device at UCLA. A ring-shaped electron beam source injects low energy electrons along a strong magnetic field into a preexisting, large and cold plasma. The injected electrons are thermalized by Coulomb collisions within a short distance and provide an off-axis heat source that results in a long, hollow, cylindrical region of elevated plasma <span class="hlt">pressure</span>. The off-axis source is active for a period long compared to the density decay time, i.e., as time progresses the power per particle increases. Two distinct regimes are <span class="hlt">observed</span> to take place, an early regime dominated by multiple avalanches, identified as a sudden intermittent rearrangement of the <span class="hlt">pressure</span> <span class="hlt">profile</span> that repeats under sustained heating, and a second regime dominated by broadband drift-Alfvén fluctuations. The transition between the two regimes is sudden and global, both radially and axially. The initial regime is characterized by peaked density and temperature <span class="hlt">profiles</span>, while only the peaked temperature <span class="hlt">profile</span> survives in the second regime. Recent measurements at multiple axial locations provide new insight into the axial dynamics of the global avalanche. Sponsored by NSF Grant 1619505 and by DOE/NSF at BaPSF.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/19990046771','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/19990046771"><span>Design and Test of Low-<span class="hlt">Profile</span> Composite Aerospace Tank Dome</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Ahmed, R.</p> <p>1999-01-01</p> <p>This report summarizes the design, analysis, manufacture, and test of a subscale, low-<span class="hlt">profile</span> composite aerospace dome under internal <span class="hlt">pressure</span>. A low-<span class="hlt">profile</span> dome has a radius-to-height ratio greater than the square root of two. This effort demonstrated that a low-<span class="hlt">profile</span> composite dome with a radius-to-height ratio of three was a feasible design and could adequately withstand the varying stress states resulting from internal <span class="hlt">pressurization</span>. Test data for strain and displacement versus <span class="hlt">pressure</span> are provided to validate the design.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.osti.gov/biblio/1054842-improving-glycan-coverage-using-hplc-ms-electrospray-ionization-subambient-pressure','SCIGOV-STC'); return false;" href="https://www.osti.gov/biblio/1054842-improving-glycan-coverage-using-hplc-ms-electrospray-ionization-subambient-pressure"><span>Improving N-Glycan Coverage using HPLC-MS with Electrospray Ionization at Subambient <span class="hlt">Pressure</span></span></a></p> <p><a target="_blank" href="http://www.osti.gov/search">DOE Office of Scientific and Technical Information (OSTI.GOV)</a></p> <p>Marginean, Ioan; Kronewitter, Scott R.; Moore, Ronald J.</p> <p></p> <p>Human serum glycan <span class="hlt">profiling</span> with mass spectrometry (MS) has been employed to study several disease conditions and is demonstrating promise for e.g. clinical biomarker discovery. However, the poor glycan ionization efficiency and the large dynamic range of glycan concentrations in human sera hinder comprehensive <span class="hlt">profiling</span>. In particular, large glycans are problematic because they are present at low concentrations and prone to fragmentation. Here we show that the sub-ambient <span class="hlt">pressure</span> ionization with nanoelectrospray (SPIN)-MS can expand the serum glycome <span class="hlt">profile</span> when compared with the conventional atmospheric <span class="hlt">pressure</span> electrospray ionization (ESI)-MS with a heated capillary inlet. Notably, the ions generated by themore » SPIN interface were <span class="hlt">observed</span> at higher charge states for 50% of the annotated glycans. Out of a total of 130 detected glycans, 34 were only detected with the SPIN-MS, resulting in improved coverage of glycan families as well as of glycans with larger numbers of labile monosaccharides.« less</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/11927200','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/11927200"><span>Accuracy of blood <span class="hlt">pressure</span> measurement and anthropometry among volunteer <span class="hlt">observers</span> in a large community survey.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Adams, Claire; Burke, Valerie; Beilin, Lawrie J</p> <p>2002-04-01</p> <p>The Busselton Survey is a population survey that is held about every three years. In 1994-1995 a re-survey was held of all past participants and 8,502 attended. Financial constraints precluded employing staff for data collection for blood <span class="hlt">pressure</span> and anthropometry, these therefore were collected by unpaid lay volunteers. Quality control by a health professional was critical to the assessment and maintenance of accuracy in these measurements. For blood <span class="hlt">pressure</span> three readings were taken simultaneously by a quality control person and the volunteer using a dual stethoscope. Duplicate anthropometric measurements were taken by a criterion anthropometrist and the volunteer. Inter and intra-<span class="hlt">observer</span> technical errors of measurement (TEM) were calculated. Sixty-two volunteers were trained to take BP measurements; of these, 38 collected data, and 63 were trained in anthropometry; of these, 30 were suitable as measurers. Training was conducted on a group and individual basis by the quality assurance person for the study both in the Perth metropolitan area and rural Busselton. The TEM for SBP was 1.6 mm Hg (SD 1.0 mm Hg) and 1.5 mm Hg (SD 0.8) for DBP. For skin-folds intra-<span class="hlt">observer</span> TEM ranged from 0.6 mm to 1.0 mm. Between-<span class="hlt">observer</span> TEM ranged from 2.1 mm to 5.4 mm. For limb and waist circumferences, intra-<span class="hlt">observer</span> TEM ranged from 0.3 cm to 1.6 cm. Between-<span class="hlt">observer</span> TEM for circumferences ranged from 0.5 cm to 1.9 cm. Unpaid volunteer measurers can, if carefully trained and supervised, provide acceptable blood <span class="hlt">pressure</span> data and anthropometry in large population surveys.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/20150011463','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/20150011463"><span><span class="hlt">Pressure</span> <span class="hlt">Profiles</span> in a Loop Heat Pipe Under Gravity Influence</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Ku, Jentung</p> <p>2015-01-01</p> <p>During the operation of a loop heat pipe (LHP), the viscous flow induces <span class="hlt">pressure</span> drops in various elements of the loop. The total <span class="hlt">pressure</span> drop is equal to the sum of <span class="hlt">pressure</span> drops in vapor grooves, vapor line, condenser, liquid line and primary wick, and is sustained by menisci at liquid and vapor interfaces on the outer surface of the primary wick in the evaporator. The menisci will curve naturally so that the resulting capillary <span class="hlt">pressure</span> matches the total <span class="hlt">pressure</span> drop. In ground testing, an additional gravitational <span class="hlt">pressure</span> head may be present and must be included in the total <span class="hlt">pressure</span> drop when LHP components are placed in a non-planar configuration. Under gravity-neutral and anti-gravity conditions, the fluid circulation in the LHP is driven solely by the capillary force. With gravity assist, however, the flow circulation can be driven by the combination of capillary and gravitational forces, or by the gravitational force alone. For a gravity-assist LHP at a given elevation between the horizontal condenser and evaporator, there exists a threshold heat load below which the LHP operation is gravity driven and above which the LHP operation is capillary force and gravity co-driven. The gravitational <span class="hlt">pressure</span> head can have profound effects on the LHP operation, and such effects depend on the elevation, evaporator heat load, and condenser sink temperature. This paper presents a theoretical study on LHP operations under gravity neutral, anti-gravity, and gravity-assist modes using <span class="hlt">pressure</span> diagrams to help understand the underlying physical processes. Effects of the condenser configuration on the gravitational <span class="hlt">pressure</span> head and LHP operation are also discussed.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/20150018317','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/20150018317"><span><span class="hlt">Pressure</span> <span class="hlt">Profiles</span> in a Loop Heat Pipe under Gravity Influence</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Ku, Jentung</p> <p>2015-01-01</p> <p>During the operation of a loop heat pipe (LHP), the viscous flow induces <span class="hlt">pressure</span> drops in various elements of the loop. The total <span class="hlt">pressure</span> drop is equal to the sum of <span class="hlt">pressure</span> drops in vapor grooves, vapor line, condenser, liquid line and primary wick, and is sustained by menisci at liquid and vapor interfaces on the outer surface of the primary wick in the evaporator. The menisci will curve naturally so that the resulting capillary <span class="hlt">pressure</span> matches the total <span class="hlt">pressure</span> drop. In ground testing, an additional gravitational <span class="hlt">pressure</span> head may be present and must be included in the total <span class="hlt">pressure</span> drop when LHP components are placed in a non-planar configuration. Under gravity-neutral and anti-gravity conditions, the fluid circulation in the LHP is driven solely by the capillary force. With gravity assist, however, the flow circulation can be driven by the combination of capillary and gravitational forces, or by the gravitational force alone. For a gravity-assist LHP at a given elevation between the horizontal condenser and evaporator, there exists a threshold heat load below which the LHP operation is gravity driven and above which the LHP operation is capillary force and gravity co-driven. The gravitational <span class="hlt">pressure</span> head can have profound effects on the LHP operation, and such effects depend on the elevation, evaporator heat load, and condenser sink temperature. This paper presents a theoretical study on LHP operations under gravity-neutral, anti-gravity, and gravity-assist modes using <span class="hlt">pressure</span> diagrams to help understand the underlying physical processes. Effects of the condenser configuration on the gravitational <span class="hlt">pressure</span> head and LHP operation are also discussed.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/20090009345','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/20090009345"><span>Combining Satellite Microwave Radiometer and Radar <span class="hlt">Observations</span> to Estimate Atmospheric Latent Heating <span class="hlt">Profiles</span></span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Grecu, Mircea; Olson, William S.; Shie, Chung-Lin; L'Ecuyer, Tristan S.; Tao, Wei-Kuo</p> <p>2009-01-01</p> <p>In this study, satellite passive microwave sensor <span class="hlt">observations</span> from the TRMM Microwave Imager (TMI) are utilized to make estimates of latent + eddy sensible heating rates (Q1-QR) in regions of precipitation. The TMI heating algorithm (TRAIN) is calibrated, or "trained" using relatively accurate estimates of heating based upon spaceborne Precipitation Radar (PR) <span class="hlt">observations</span> collocated with the TMI <span class="hlt">observations</span> over a one-month period. The heating estimation technique is based upon a previously described Bayesian methodology, but with improvements in supporting cloud-resolving model simulations, an adjustment of precipitation echo tops to compensate for model biases, and a separate scaling of convective and stratiform heating components that leads to an approximate balance between estimated vertically-integrated condensation and surface precipitation. Estimates of Q1-QR from TMI compare favorably with the PR training estimates and show only modest sensitivity to the cloud-resolving model simulations of heating used to construct the training data. Moreover, the net condensation in the corresponding annual mean satellite latent heating <span class="hlt">profile</span> is within a few percent of the annual mean surface precipitation rate over the tropical and subtropical oceans where the algorithm is applied. Comparisons of Q1 produced by combining TMI Q1-QR with independently derived estimates of QR show reasonable agreement with rawinsonde-based analyses of Q1 from two field campaigns, although the satellite estimates exhibit heating <span class="hlt">profile</span> structure with sharper and more intense heating peaks than the rawinsonde estimates. 2</p> </li> </ol> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_10");'>10</a></li> <li><a href="#" onclick='return showDiv("page_11");'>11</a></li> <li class="active"><span>12</span></li> <li><a href="#" onclick='return showDiv("page_13");'>13</a></li> <li><a href="#" onclick='return showDiv("page_14");'>14</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div><!-- col-sm-12 --> </div><!-- row --> </div><!-- page_12 --> <div id="page_13" class="hiddenDiv"> <div class="row"> <div class="col-sm-12"> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_11");'>11</a></li> <li><a href="#" onclick='return showDiv("page_12");'>12</a></li> <li class="active"><span>13</span></li> <li><a href="#" onclick='return showDiv("page_14");'>14</a></li> <li><a href="#" onclick='return showDiv("page_15");'>15</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div> </div> <div class="row"> <div class="col-sm-12"> <ol class="result-class" start="241"> <li> <p><a target="_blank" onclick="trackOutboundLink('https://ntrs.nasa.gov/search.jsp?R=20040115250&hterms=sada&qs=N%3D0%26Ntk%3DAll%26Ntx%3Dmode%2Bmatchall%26Ntt%3Dsada','NASA-TRS'); return false;" href="https://ntrs.nasa.gov/search.jsp?R=20040115250&hterms=sada&qs=N%3D0%26Ntk%3DAll%26Ntx%3Dmode%2Bmatchall%26Ntt%3Dsada"><span><span class="hlt">Observations</span> of CH4, C2H6, and C2H2 in the stratosphere of Jupiter</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Sada, P. V.; Bjoraker, G. L.; Jennings, D. E.; McCabe, G. H.; Romani, P. N.</p> <p>1998-01-01</p> <p>We have performed high-resolution spectral <span class="hlt">observations</span> at mid-infrared wavelengths of CH4 (8.14 micrometers), C2H6 (12.16 micrometers), and C2H2 (13.45 micrometers) on Jupiter. These emission features probe the stratosphere of the planet and provide information on the carbon-based photochemical processes taking place in that region of the atmosphere. The <span class="hlt">observations</span> were performed using our cryogenic echelle spectrometer CELESTE, in conjunction with the McMath-Pierce 1.5-m solar telescope between November 1994 and February 1995. We used the methane <span class="hlt">observations</span> to derive the temperature <span class="hlt">profile</span> of the jovian atmosphere in the 1-10 mbar region of the stratosphere. This <span class="hlt">profile</span> was then used in conjunction with height-dependent mixing ratios of each hydrocarbon to determine global abundances for ethane and acetylene. The resulting mixing ratios are 3.9(+1.9)(-1.3) x 10(-6) for C2H6 (5 mbar <span class="hlt">pressure</span> level), and 2.3 +/- 0.5 x 10(-8) for C2H2 (8 mbar <span class="hlt">pressure</span> level), where the quoted uncertainties are derived from model variations in the temperature <span class="hlt">profile</span> which match the methane <span class="hlt">observation</span> uncertainties. c1998 Academic Press.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=4888538','PMC'); return false;" href="https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=4888538"><span>Distinct neurohumoral biomarker <span class="hlt">profiles</span> in children with hemodynamically defined orthostatic intolerance may predict treatment options</span></a></p> <p><a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pmc">PubMed Central</a></p> <p>Wagoner, Ashley L.; Shaltout, Hossam A.; Fortunato, John E.</p> <p>2015-01-01</p> <p>Studies of adults with orthostatic intolerance (OI) have revealed altered neurohumoral responses to orthostasis, which provide mechanistic insights into the dysregulation of blood <span class="hlt">pressure</span> control. Similar studies in children with OI providing a thorough neurohumoral <span class="hlt">profile</span> are lacking. The objective of the present study was to determine the cardiovascular and neurohumoral <span class="hlt">profile</span> in adolescent subjects presenting with OI. Subjects at 10–18 yr of age were prospectively recruited if they exhibited two or more traditional OI symptoms and were referred for head-up tilt (HUT) testing. Circulating catecholamines, vasopressin, aldosterone, renin, and angiotensins were measured in the supine position and after 15 min of 70° tilt. Heart rate and blood <span class="hlt">pressure</span> were continuously measured. Of the 48 patients, 30 patients had an abnormal tilt. Subjects with an abnormal tilt had lower systolic, diastolic, and mean arterial blood <span class="hlt">pressures</span> during tilt, significantly higher levels of vasopressin during HUT, and relatively higher catecholamines and ANG II during HUT than subjects with a normal tilt. Distinct neurohumoral <span class="hlt">profiles</span> were <span class="hlt">observed</span> when OI subjects were placed into the following groups defined by the hemodynamic response: postural orthostatic tachycardia syndrome (POTS), orthostatic hypotension (OH), syncope, and POTS/syncope. Key characteristics included higher HUT-induced norepinephrine in POTS subjects, higher vasopressin in OH and syncope subjects, and higher supine and HUT aldosterone in OH subjects. In conclusion, children with OI and an abnormal response to tilt exhibit distinct neurohumoral <span class="hlt">profiles</span> associated with the type of the hemodynamic response during orthostatic challenge. Elevated arginine vasopressin levels in syncope and OH groups are likely an exaggerated response to decreased blood flow not compensated by higher norepinephrine levels, as <span class="hlt">observed</span> in POTS subjects. These different compensatory mechanisms support the role of measuring</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2008JPhCS.121b2021N','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2008JPhCS.121b2021N"><span>High-<span class="hlt">pressure</span> x-ray diffraction study on lithium borohydride using a synchrotron radiation</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Nakano, S.; Nakayama, A.; Kikegawa, T.</p> <p>2008-07-01</p> <p>Lithium borohydride (LiBH4) was compressed up to 10 GPa using a diamond-anvil-cell to investigate its high-<span class="hlt">pressure</span> structure. In-situ x-ray diffraction <span class="hlt">profiles</span> indicated a <span class="hlt">pressure</span>-induced transformation at 1.1 GPa, which was consistent with the previous experimental <span class="hlt">observation</span> such as Raman scattering spectroscopy. The high-<span class="hlt">pressure</span> phase was indexed on a tetragonal symmetry of P42/mmc, which was not corresponding some structural models proposed by previous calculation studies. An unknown substance (presumably another Li-B-H compound), which was contained in the starting material, also transformed into its high-<span class="hlt">pressure</span> phase at 0.6 GPa without any relation to the transformation of LiBH4.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/20160001778','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/20160001778"><span>Implications of Operational <span class="hlt">Pressure</span> on CSSE PGS Design</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Lee, Ryan</p> <p>2008-01-01</p> <p>The Constellation Spacesuit Element (CSSE) was required to support crew survival (CS); launch, entry, and abort (LEA) scenarios; zero gravity (0-g) extravehicular activity (EVA) (both unscheduled and contingency); and planetary EVA. Operation of the CSSE in all of these capacities required a <span class="hlt">pressure</span> garment subsystem (PGS) that would operate efficiently through various <span class="hlt">pressure</span> <span class="hlt">profiles</span>. The PGS team initiated a study to determine the appropriate operational <span class="hlt">pressure</span> <span class="hlt">profile</span> of the CSSE and how this selection would affect the design of the CSSE PGS. This study included an extensive review of historical PGS operational <span class="hlt">pressure</span> selection and the operational effects of those <span class="hlt">pressures</span>, the presentation of four possible <span class="hlt">pressure</span> paradigm options for use by the CSSE, the risks and design impacts of these options, and the down-selected <span class="hlt">pressure</span> option.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=4129134','PMC'); return false;" href="https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=4129134"><span>The Type of Fat Ingested at Breakfast Influences the Plasma Lipid <span class="hlt">Profile</span> of Postmenopausal Women</span></a></p> <p><a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pmc">PubMed Central</a></p> <p>Morillas-Ruiz, J. M.; Delgado-Alarcon, J. M.; Rubio-Perez, J. M.; Albaladejo Oton, M. D.</p> <p>2014-01-01</p> <p>To assess whether the type of fat ingested at breakfast can modify the plasma lipid <span class="hlt">profile</span> and other cardiovascular risk variables in postmenopausal women at risk of cardiovascular disease, a longitudinal, randomized, and crossover study was carried out with postmenopausal women at risk of CVD. They were randomly assigned to eat each type of breakfast during one month: 6 study periods (breakfast with the same composition plus butter/margarine/virgin olive oil) separated by two washout periods. On the first and last days of each study period, weight, arterial blood <span class="hlt">pressure</span>, heart rate, and body mass index were recorded in fasting conditions and a blood sample was collected to measure plasma lipid <span class="hlt">profile</span>. When comparing final values to baseline values, we only found out statistically significant differences on plasma lipid <span class="hlt">profiles</span>. Butter-based breakfast increased total cholesterol and HDL, while margarine-based breakfast decreased total cholesterol and LDL and increased HDL. After the olive oil-based breakfast intake, a tendency towards a decrease of total cholesterol and LDL levels and an increase of HDL levels was <span class="hlt">observed</span>. No statistically significant differences were <span class="hlt">observed</span> in triglycerides levels, BMI, and arterial <span class="hlt">pressure</span> in any breakfast type. The margarine-based breakfast was the only one which significantly increased the percentage of volunteers with optimal lipid <span class="hlt">profiles</span>. The polyunsaturated fat at breakfast has improved the plasma lipid <span class="hlt">profile</span> in the analyzed sample population, suggesting that PUFA-based breakfast can be advisable in women at risk of CVD. PMID:25136625</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/22515476','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/22515476"><span>Implementation of <span class="hlt">pressure</span> ulcer prevention best practice recommendations in acute care: an <span class="hlt">observational</span> study.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Barker, Anna Lucia; Kamar, Jeannette; Tyndall, Tamara Jane; White, Lyn; Hutchinson, Anastasia; Klopfer, Nicole; Weller, Carolina</p> <p>2013-06-01</p> <p><span class="hlt">Pressure</span> ulcers are a common but preventable problem in hospitals. Implementation of best practice guideline recommendations can prevent ulcers from occurring. This 9-year cohort study reports prevalence data from point prevalence surveys during the <span class="hlt">observation</span> period, and three practice metrics to assess implementation of best practice guideline recommendations: (i) nurse compliance with use of a validated <span class="hlt">pressure</span> ulcer risk assessment and intervention checklist; (ii) accuracy of risk assessment scoring in usual-care nurses and experienced injury prevention nurses; and (iii) use of <span class="hlt">pressure</span> ulcer prevention strategies. The prevalence of hospital-acquired <span class="hlt">pressure</span> ulcers decreased following implementation of an evidence-based prevention programme from 12·6% (2 years preprogramme implementation) to 2·6% (6 years postprogramme implementation) (P < 0·001). Audits between 2003 and 2011 of 4368 patient medical records identified compliance with <span class="hlt">pressure</span> ulcer prevention documentation according to best practice guidelines was high (>84%). A sample of 270 patients formed the sample for the study of risk assessment scoring accuracy and use of prevention strategies. It was found usual-care nurses under-estimated patients' risk of <span class="hlt">pressure</span> ulcer development and under-utilised prevention strategies compared with experienced injury prevention nurses. Despite a significant reduction in prevalence of hospital-acquired <span class="hlt">pressure</span> ulcers and high documentation compliance, use of prevention strategies could further be improved to achieve better patient outcomes. Barriers to the use of prevention strategies by nurses in the acute hospital setting require further examination. This study provides important insights into the knowledge translation of <span class="hlt">pressure</span> ulcer prevention best practice guideline recommendations at The Northern Hospital. © 2012 The Authors. International Wound Journal © 2012 John Wiley & Sons Ltd and Medicalhelplines.com Inc.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2008AGUFM.H31B0834B','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2008AGUFM.H31B0834B"><span>An Examination of Potential Causes of the Persistent Capillary Fringe Extension <span class="hlt">Observed</span> During a Pumping Test in an Unconfined Aquifer</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Bunn, M. I.; Jones, J.; Endres, A. L.</p> <p>2008-12-01</p> <p>Hydrogeologists quantify the properties of unconfined aquifers by analyzing the data from pumping tests. The most appropriate method of incorporating flow contributions from the vadose zone into these analyses has been the subject of debate for decades. Recently, a highly detailed data set was collected during a seven- day pumping test at CFB Borden, Ontario (Bevan et al., 2005) which has allowed a close examination of the vadose zone response to pumping. Water table drawdown was monitored using <span class="hlt">pressure</span> transducers in 11 monitoring wells, while moisture <span class="hlt">profiles</span> were collected 19 times during the 7-day test using neutron logging. The Borden aquifer system is quite homogeneous, and numerical simulations using the variably saturated model InHM resulted in excellent reproduction of the <span class="hlt">observed</span> hydraulic head drawdowns. Conversely, the simulated moisture <span class="hlt">profiles</span> correlated poorly with neutron-logging-derived <span class="hlt">observed</span> <span class="hlt">profiles</span>. Specifically, the field results show delayed drawdown in the vadose zone, resulting in a persistent and significant extension of the capillary fringe, with the shape of the moisture <span class="hlt">profile</span> remaining constant through the transition zone. Numerical simulations using various forms of the capillary <span class="hlt">pressure</span>-saturation relationship with reasonable parameter sets were unable produce the extension. Neutron moisture <span class="hlt">profiles</span> were selected from three locations (3, 5, and 15 m radial distance from the pumping well) at which an adjacent shallow deep piezometer pair could be used to accurately estimate water table location. Using this data in conjunction with the inverse modeling tool PEST, a set of van Genuchten capillary <span class="hlt">pressure</span>-saturation parameters was generated to match each <span class="hlt">observed</span> moisture <span class="hlt">profile</span>. Horizontal and vertical hydraulic gradients and flow rates at the water table were generated using model output and compared to the fitted parameters. The van Genuchten parameter n was found to have significant scatter in both <span class="hlt">profile</span> location and</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2007APS..DPPTO3006H','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2007APS..DPPTO3006H"><span>A stepped <span class="hlt">pressure</span> <span class="hlt">profile</span> model for internal transport barriers</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Hole, Matthew; Hudson, Stuart; Dewar, Robert</p> <p>2007-11-01</p> <p>B ∇x et al We develop a multiple interface variational model, comprising multiple Taylor-relaxed plasma regions separated by ideal MHD barriers. The magnetic field in each region is Beltrami, = μ, and the <span class="hlt">pressure</span> constant. Between these regions the <span class="hlt">pressure</span>, field strength, and rotational transform may have step changes at the ideal barrier. A principle motivation is the development of a mathematically rigorous ideal MHD model to describe intrinsically 3D equilibria, with nonzero internal <span class="hlt">pressure</span>, using robust KAM surfaces as the barriers. As each region is locally relaxed however, such a model may also yield reasons for existence of internal transport barriers (ITBs). Focusing on the latter, we build on Hole Nuc. Fus. 47, pp746-753, 2007, which recently studied the stability of a two-interface periodic-cylinder configuration. In this work, we perform a stability scan over <span class="hlt">pressure</span> and for a two-interface configuration with no jump in , and compare the characteristics of stable equilibria to those of ITB's.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.osti.gov/pages/biblio/1344234-convective-cloud-vertical-velocity-mass-flux-characteristics-from-radar-wind-profiler-observations-during-goamazon2014-vertical-velocity-goamazon2014','SCIGOV-DOEP'); return false;" href="https://www.osti.gov/pages/biblio/1344234-convective-cloud-vertical-velocity-mass-flux-characteristics-from-radar-wind-profiler-observations-during-goamazon2014-vertical-velocity-goamazon2014"><span>Convective cloud vertical velocity and mass-flux characteristics from radar wind <span class="hlt">profiler</span> <span class="hlt">observations</span> during GoAmazon2014/5: VERTICAL VELOCITY GOAMAZON2014/5</span></a></p> <p><a target="_blank" href="http://www.osti.gov/pages">DOE PAGES</a></p> <p>Giangrande, Scott E.; Toto, Tami; Jensen, Michael P.; ...</p> <p>2016-11-15</p> <p>A radar wind <span class="hlt">profiler</span> data set collected during the 2 year Department of Energy Atmospheric Radiation Measurement <span class="hlt">Observations</span> and Modeling of the Green Ocean Amazon (GoAmazon2014/5) campaign is used to estimate convective cloud vertical velocity, area fraction, and mass flux <span class="hlt">profiles</span>. Vertical velocity <span class="hlt">observations</span> are presented using cumulative frequency histograms and weighted mean <span class="hlt">profiles</span> to provide insights in a manner suitable for global climate model scale comparisons (spatial domains from 20 km to 60 km). Convective <span class="hlt">profile</span> sensitivity to changes in environmental conditions and seasonal regime controls is also considered. Aggregate and ensemble average vertical velocity, convective area fraction, andmore » mass flux <span class="hlt">profiles</span>, as well as magnitudes and relative <span class="hlt">profile</span> behaviors, are found consistent with previous studies. Updrafts and downdrafts increase in magnitude with height to midlevels (6 to 10 km), with updraft area also increasing with height. Updraft mass flux <span class="hlt">profiles</span> similarly increase with height, showing a peak in magnitude near 8 km. Downdrafts are <span class="hlt">observed</span> to be most frequent below the freezing level, with downdraft area monotonically decreasing with height. Updraft and downdraft <span class="hlt">profile</span> behaviors are further stratified according to environmental controls. These results indicate stronger vertical velocity <span class="hlt">profile</span> behaviors under higher convective available potential energy and lower low-level moisture conditions. Sharp contrasts in convective area fraction and mass flux <span class="hlt">profiles</span> are most pronounced when retrievals are segregated according to Amazonian wet and dry season conditions. During this deployment, wet season regimes favored higher domain mass flux <span class="hlt">profiles</span>, attributed to more frequent convection that offsets weaker average convective cell vertical velocities.« less</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2010JSV...329.2276D','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2010JSV...329.2276D"><span>Prediction of the acoustic <span class="hlt">pressure</span> above periodically uneven facings in industrial workplaces</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Ducourneau, J.; Bos, L.; Planeau, V.; Faiz, Adil; Skali Lami, Salah; Nejade, A.</p> <p>2010-05-01</p> <p>The aim of this work is to predict sound <span class="hlt">pressure</span> in front of wall facings based on periodic sound scattering surface <span class="hlt">profiles</span>. The method involves investigating plane wave reflections randomly incident upon an uneven surface. The waveguide approach is well suited to the geometries usually encountered in industrial workplaces. This method simplifies the <span class="hlt">profile</span> geometry by using elementary rectangular volumes. The acoustic field in the <span class="hlt">profile</span> interstices can then be expressed as the superposition of waveguide modes. In past work, walls considered are of infinite dimensions and are subjected to a periodic surface <span class="hlt">profile</span> in only one direction. We therefore generalise this approach by extending its applicability to "double-periodic" wall facings. Free-field measurements have been taken and the <span class="hlt">observed</span> agreement between numerical and experimental results supports the validity of the waveguide method.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2015AGUFM.A21H0252P','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2015AGUFM.A21H0252P"><span>Vertical <span class="hlt">Profiles</span> as <span class="hlt">Observational</span> Constraints on Nitrous Oxide (N2O) Emissions in an Agricultural Region</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Pusede, S.; Diskin, G. S.</p> <p>2015-12-01</p> <p>We use diurnal variability in near-surface N2O vertical <span class="hlt">profiles</span> to derive N2O emission rates. Our emissions estimates are ~3 times greater than are accounted for by inventories, a discrepancy in line with results from previous studies using different approaches. We quantify the surface N2O concentration's memory of local surface emissions on previous days to be 50-90%. We compare measured <span class="hlt">profiles</span> both over and away from a dense N2O source region in the San Joaquin Valley, finding that <span class="hlt">profile</span> shapes, diurnal variability, and changes in integrated near-surface column abundances are distinct according to proximity to source areas. To do this work, we use aircraft <span class="hlt">observations</span> from the wintertime DISCOVER-AQ project in California's San Joaquin Valley, a region of intense agricultural activity.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://ntrs.nasa.gov/search.jsp?R=20080046997&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D40%26Ntt%3DH%2526M','NASA-TRS'); return false;" href="https://ntrs.nasa.gov/search.jsp?R=20080046997&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D40%26Ntt%3DH%2526M"><span><span class="hlt">Observed</span> and Modeled HOCl <span class="hlt">Profiles</span> in the Midlatitude Stratosphere: Implication for Ozone Loss</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Kovalenko, L. J.; Jucks, K. W.; Salawitch, R. J.; Toon, G. C.; Blavier, J. F.; Johnson, D. G.; Kleinbohl, A.; Livesey, N. J .; Margitan, J. J.; Pickett, H. M.; <a style="text-decoration: none; " href="javascript:void(0); " onClick="displayelement('author_20080046997'); toggleEditAbsImage('author_20080046997_show'); toggleEditAbsImage('author_20080046997_hide'); "> <img style="display:inline; width:12px; height:12px; " src="images/arrow-up.gif" width="12" height="12" border="0" alt="hide" id="author_20080046997_show"> <img style="width:12px; height:12px; display:none; " src="images/arrow-down.gif" width="12" height="12" border="0" alt="hide" id="author_20080046997_hide"></p> <p>2007-01-01</p> <p>Vertical <span class="hlt">profiles</span> of stratospheric HOCl calculated with a diurnal steady-state photochemical model that uses currently recommended reaction rates and photolysis cross sections underestimate <span class="hlt">observed</span> <span class="hlt">profiles</span> of HOCl obtained by two balloon-borne instruments, FIRS-2 (a far-infrared emission spectrometer) and MkIV (a mid-infrared, solar absorption spectrometer). Considerable uncertainty (a factor of two) persists in laboratory measurements of the rate constant (k(sub 1)) for the reaction ClO + HO2 yields HOCl + O2. Agreement between modeled and measured HOCl can be attained using a value of k(sub 1) from Stimpfle et al. (1979) that is about a factor-of-two faster than the currently recommended rate constant. Comparison of modeled and measured HOCl suggests that models using the currently recommended value for k(sub 1) may underestimate the role of the HOCl catalytic cycle for ozone depletion, important in the midlatitude lower stratosphere.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/20120014384','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/20120014384"><span>Prevention of Over-<span class="hlt">Pressurization</span> During Combustion in a Sealed Chamber</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Gokoglu, Suleyman A.; Niehaus, Justin E.; Olson, Sandra L.; Dietrich, Daniel L.; Ruff, Gary A.; Johnston, Michael C.</p> <p>2012-01-01</p> <p>The combustion of flammable material in a sealed chamber invariably leads to an initial <span class="hlt">pressure</span> rise in the volume. The <span class="hlt">pressure</span> rise is due to the increase in the total number of gaseous moles (condensed fuel plus chamber oxygen combining to form gaseous carbon dioxide and water vapor) and, most importantly, the temperature rise of the gas in the chamber. Though the rise in temperature and <span class="hlt">pressure</span> would reduce with time after flame extinguishment due to the absorption of heat by the walls and contents of the sealed spacecraft, the initial <span class="hlt">pressure</span> rise from a fire, if large enough, could lead to a vehicle over-<span class="hlt">pressure</span> and the release of gas through the <span class="hlt">pressure</span> relief valve. This paper presents a simple lumped-parameter model of the <span class="hlt">pressure</span> rise in a sealed chamber resulting from the heat release during combustion. The transient model considers the increase in gaseous moles due to combustion, and heat transfer to the chamber walls by convection and radiation and to the fuel-sample holder by conduction, as a function of the burning rate of the material. The results of the model are compared to the <span class="hlt">pressure</span> rise in an experimental chamber during flame spread tests as well as to the <span class="hlt">pressure</span> falloff after flame extinguishment. The experiments involve flame spread over thin solid fuel samples. Estimates of the heat release rate <span class="hlt">profiles</span> for input to the model come from the assumed stoichiometric burning of the fuel along with the <span class="hlt">observed</span> flame spread behavior. The sensitivity of the model to predict maximum chamber <span class="hlt">pressure</span> is determined with respect to the uncertainties in input parameters. Model predictions are also presented for the <span class="hlt">pressure</span> <span class="hlt">profile</span> anticipated in the Fire Safety-1 experiment, a material flammability and fire safety experiment proposed for the European Space Agency (ESA) Automated Transfer Vehicle (ATV). Computations are done for a range of scenarios including various initial <span class="hlt">pressures</span> and sample sizes. Based on these results, various</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2005MeScT..16.1751P','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2005MeScT..16.1751P"><span>Dynamic calibration of fast-response probes in low-<span class="hlt">pressure</span> shock tubes</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Persico, G.; Gaetani, P.; Guardone, A.</p> <p>2005-09-01</p> <p>Shock tube flows resulting from the incomplete burst of the diaphragm are investigated in connection with the dynamic calibration of fast-response <span class="hlt">pressure</span> probes. As a result of the partial opening of the diaphragm, <span class="hlt">pressure</span> disturbances are <span class="hlt">observed</span> past the shock wave and the measured total <span class="hlt">pressure</span> <span class="hlt">profile</span> deviates from the envisaged step signal required by the calibration process. <span class="hlt">Pressure</span> oscillations are generated as the initially normal shock wave diffracts from the diaphragm's orifice and reflects on the shock tube walls, with the lowest local frequency roughly equal to the ratio of the sound speed in the perturbed region to the shock tube diameter. The energy integral of the perturbations decreases with increasing distance from the diaphragm, as the diffracted leading shock and downwind reflections coalesce into a single normal shock. A procedure is proposed to calibrate fast-response <span class="hlt">pressure</span> probes downwind of a partially opened shock tube diaphragm.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/26655791','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/26655791"><span>Liquid chromatography coupled to different atmospheric <span class="hlt">pressure</span> ionization sources-quadrupole-time-of-flight mass spectrometry and post-column addition of metal salt solutions as a powerful tool for the metabolic <span class="hlt">profiling</span> of Fusarium oxysporum.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Cirigliano, Adriana M; Rodriguez, M Alejandra; Gagliano, M Laura; Bertinetti, Brenda V; Godeas, Alicia M; Cabrera, Gabriela M</p> <p>2016-03-25</p> <p>Fusarium oxysporum L11 is a non-pathogenic soil-borne fungal strain that yielded an extract that showed antifungal activity against phytopathogens. In this study, reversed-phase high-performance liquid chromatography (RP-HPLC) coupled to different atmospheric <span class="hlt">pressure</span> ionization sources-quadrupole-time-of-flight mass spectrometry (API-QTOF-MS) was applied for the comprehensive <span class="hlt">profiling</span> of the metabolites from the extract. The employed sources were electrospray (ESI), atmospheric <span class="hlt">pressure</span> chemical ionization (APCI) and atmospheric <span class="hlt">pressure</span> photoionization (APPI). Post-column addition of metal solutions of Ca, Cu and Zn(II) was also tested using ESI. A total of 137 compounds were identified or tentatively identified by matching their accurate mass signals, suggested molecular formulae and MS/MS analysis with previously reported data. Some compounds were isolated and identified by NMR. The extract was rich in cyclic peptides like cyclosporins, diketopiperazines and sansalvamides, most of which were new, and are reported here for the first time. The use of post-column addition of metals resulted in a useful strategy for the discrimination of compound classes since specific adducts were <span class="hlt">observed</span> for the different compound families. This technique also allowed the screening for compounds with metal binding properties. Thus, the applied methodology is a useful choice for the metabolic <span class="hlt">profiling</span> of extracts and also for the selection of metabolites with potential biological activities related to interactions with metal ions. Copyright © 2015 Elsevier B.V. All rights reserved.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/23782628','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/23782628"><span>Tongue <span class="hlt">pressure</span> <span class="hlt">profile</span> training for dysphagia post stroke (TPPT): study protocol for an exploratory randomized controlled trial.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Steele, Catriona M; Bayley, Mark A; Péladeau-Pigeon, Melanie; Stokely, Shauna L</p> <p>2013-05-07</p> <p>It is estimated that approximately 50% of stroke survivors will experience swallowing difficulty, or dysphagia. The associated sequelae of dysphagia include dehydration, malnutrition, and aspiration pneumonia, all of which have can have serious medical consequences. To improve swallowing safety and efficiency, alternative nutritional intake methods (for example, a feeding tube) or a modified diet texture (such as pureed foods or thickened liquids) may be recommended but these modifications may negatively affect quality of life. An alternative approach to treating dysphagia has emerged over the past few years, targeting stronger lingual muscles through maximal isometric <span class="hlt">pressure</span> tasks. Although these studies have shown promising results, thin-liquid bolus control continues to be challenging for patients with dysphagia. Previous work investigating lingual <span class="hlt">pressures</span> when healthy participants swallow has suggested that greater task specificity in lingual exercises may yield improved results with thin liquids. This is a small, exploratory randomized clinical trial being conducted with post-stroke patients 4 to 20 weeks after onset of dysphagia secondary to impaired lingual control. At enrollment, participants are randomly assigned to one of two treatment protocols, either tongue <span class="hlt">pressure</span> <span class="hlt">profile</span> training (TPPT) or the control treatment, tongue <span class="hlt">pressure</span> strength-and-accuracy training (TPSAT). Each treatment protocol consists of 24 sessions of treatment over 8 to 12 weeks with monitoring of tongue <span class="hlt">pressure</span> as well as a baseline and outcome videofluoroscopic swallowing study. Tongue <span class="hlt">pressure</span> measures, videofluoroscopic measures, and functional outcome measures will be obtained following training of 60 participants (30 in each condition), to determine whether TPPT yields better outcomes. This study will continue to explore options beyond tube feeding and modified diets for people with neurogenic dysphagia following stroke. Should the novel protocol, TPPT, prove to be more</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2018AMT....11.1653S','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2018AMT....11.1653S"><span>Vertical <span class="hlt">profile</span> of tropospheric ozone derived from synergetic retrieval using three different wavelength ranges, UV, IR, and microwave: sensitivity study for satellite <span class="hlt">observation</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Sato, Tomohiro O.; Sato, Takao M.; Sagawa, Hideo; Noguchi, Katsuyuki; Saitoh, Naoko; Irie, Hitoshi; Kita, Kazuyuki; Mahani, Mona E.; Zettsu, Koji; Imasu, Ryoichi; Hayashida, Sachiko; Kasai, Yasuko</p> <p>2018-03-01</p> <p>We performed a feasibility study of constraining the vertical <span class="hlt">profile</span> of the tropospheric ozone by using a synergetic retrieval method on multiple spectra, i.e., ultraviolet (UV), thermal infrared (TIR), and microwave (MW) ranges, measured from space. This work provides, for the first time, a quantitative evaluation of the retrieval sensitivity of the tropospheric ozone by adding the MW measurement to the UV and TIR measurements. Two <span class="hlt">observation</span> points in East Asia (one in an urban area and one in an ocean area) and two <span class="hlt">observation</span> times (one during summer and one during winter) were assumed. Geometry of line of sight was nadir down-looking for the UV and TIR measurements, and limb sounding for the MW measurement. The retrieval sensitivities of the ozone <span class="hlt">profiles</span> in the upper troposphere (UT), middle troposphere (MT), and lowermost troposphere (LMT) were estimated using the degree of freedom for signal (DFS), the <span class="hlt">pressure</span> of maximum sensitivity, reduction rate of error from the a priori error, and the averaging kernel matrix, derived based on the optimal estimation method. The measurement noise levels were assumed to be the same as those for currently available instruments. The weighting functions for the UV, TIR, and MW ranges were calculated using the SCIATRAN radiative transfer model, the Line-By-Line Radiative Transfer Model (LBLRTM), and the Advanced Model for Atmospheric Terahertz Radiation Analysis and Simulation (AMATERASU), respectively. The DFS value was increased by approximately 96, 23, and 30 % by adding the MW measurements to the combination of UV and TIR measurements in the UT, MT, and LMT regions, respectively. The MW measurement increased the DFS value of the LMT ozone; nevertheless, the MW measurement alone has no sensitivity to the LMT ozone. The <span class="hlt">pressure</span> of maximum sensitivity value for the LMT ozone was also increased by adding the MW measurement. These findings indicate that better information on LMT ozone can be obtained by adding constraints</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2013BoLMe.149..103R','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2013BoLMe.149..103R"><span>The Effect of Wind-Turbine Wakes on Summertime US Midwest Atmospheric Wind <span class="hlt">Profiles</span> as <span class="hlt">Observed</span> with Ground-Based Doppler Lidar</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Rhodes, Michael E.; Lundquist, Julie K.</p> <p>2013-07-01</p> <p>We examine the influence of a modern multi-megawatt wind turbine on wind and turbulence <span class="hlt">profiles</span> three rotor diameters (D) downwind of the turbine. Light detection and ranging (lidar) wind-<span class="hlt">profile</span> <span class="hlt">observations</span> were collected during summer 2011 in an operating wind farm in central Iowa at 20-m vertical intervals from 40 to 220 m above the surface. After a calibration period during which two lidars were operated next to each other, one lidar was located approximately 2D directly south of a wind turbine; the other lidar was moved approximately 3D north of the same wind turbine. Data from the two lidars during southerly flow conditions enabled the simultaneous capture of inflow and wake conditions. The inflow wind and turbulence <span class="hlt">profiles</span> exhibit strong variability with atmospheric stability: daytime <span class="hlt">profiles</span> are well-mixed with little shear and strong turbulence, while nighttime <span class="hlt">profiles</span> exhibit minimal turbulence and considerable shear across the rotor disk region and above. Consistent with the <span class="hlt">observations</span> available from other studies and with wind-tunnel and large-eddy simulation studies, measurable reductions in wake wind-speeds occur at heights spanning the wind turbine rotor (43-117 m), and turbulent quantities increase in the wake. In generalizing these results as a function of inflow wind speed, we find the wind-speed deficit in the wake is largest at hub height or just above, and the maximum deficit occurs when wind speeds are below the rated speed for the turbine. Similarly, the maximum enhancement of turbulence kinetic energy and turbulence intensity occurs at hub height, although <span class="hlt">observations</span> at the top of the rotor disk do not allow assessment of turbulence in that region. The wind shear below turbine hub height (quantified here with the power-law coefficient) is found to be a useful parameter to identify whether a downwind lidar <span class="hlt">observes</span> turbine wake or free-flow conditions. These field <span class="hlt">observations</span> provide data for validating turbine-wake models and wind</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2013AGUFMDI31B..01G','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2013AGUFMDI31B..01G"><span>Petrologically-based Electrical <span class="hlt">Profiles</span> vs. Geophysical <span class="hlt">Observations</span> through the Upper Mantle (Invited)</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Gaillard, F.; Massuyeau, M.; Sifre, D.; Tarits, P.</p> <p>2013-12-01</p> <p>Mineralogical transformations in the up-welling mantle play a critical role on the dynamics of mass and heat transfers at mid-ocean-ridgeS. The melting event producing ridge basalts occur at 60 km depth below the ridge axis, but because of small amounts of H2O and CO2 in the source region of MOR-basalts, incipient melting can initiate at much greater depth. Such incipient melts concentrate incompatible elements, and are particularly rich in volatile species. These juices evolve from carbonatites, carbonated basalts, to CO2-H2O-rich basalts as recently exposed by petrological surveys; the passage from carbonate to silicate melts is a complex pathway that is strongly non-linear. This picture has recently been complicated further by studies showing that oxygen increasingly partitions into garnet as <span class="hlt">pressure</span> increases; this implies that incipient melting may be prevented at depth exceeding 200 km because not enough oxygen is available in the system to stabilize carbonate melts. The aim of this work is twofold: - We modelled the complex pathway of mantle melting in presence of C-O-H volatiles by adjusting the thermodynamic properties of mixing in the multi-component C-O-H-melt system. This allows us to calculate the change in melt composition vs. depth following any sortS of adiabat. - We modelled the continuous change in electrical properties from carbonatites, carbonated basalts, to CO2-H2O-rich basalts. We then successfully converted this petrological evolution along a ridge adiabat into electrical conductivity vs. depth signal. The discussion that follows is about comparison of this petrologically-based conductivity <span class="hlt">profile</span> with the recent <span class="hlt">profiles</span> obtained by inversion of the long-period electromagnetic signals from the East-Pacific-Rise. These geophysically-based <span class="hlt">profiles</span> reveal the electrical conductivity structure down to 400 km depth and they show some intriguing highly conductive sections. We will discuss heterogeneity in electrical conductivity of the upper</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/19780009587','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/19780009587"><span>Recovery of refractivity <span class="hlt">profiles</span> and <span class="hlt">pressure</span> and temperature distributions in the lower atmosphere from satellite-to-satellite radio occultation data</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Murray, C. W., Jr.</p> <p>1977-01-01</p> <p>The feasibility of recovering parameters from one-way range rate between two earth orbiting spacecraft during occultation of the tracking signal by the earth's lower atmosphere. The tracking data is inverted by an integral transformation (Abel transform) to obtain a vertical refractivity <span class="hlt">profile</span> above the point of closest approach of the ray connecting the satellites. <span class="hlt">Pressure</span> and temperature distributions can be obtained from values of dry refractivity using the hydrostatic equation and perfect gas law. Two methods are investigated for recovering <span class="hlt">pressure</span> and temperature parameters. Results show that recovery is much more sensitive to satellite velocity errors than to satellite position errors. An error analysis is performed. An example is given demonstrating recovery of parameters from radio occultation data obtained during satellite-to-satellite tracking of Nimbus 6 by the ATS 6 satellite.</p> </li> </ol> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_11");'>11</a></li> <li><a href="#" onclick='return showDiv("page_12");'>12</a></li> <li class="active"><span>13</span></li> <li><a href="#" onclick='return showDiv("page_14");'>14</a></li> <li><a href="#" onclick='return showDiv("page_15");'>15</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div><!-- col-sm-12 --> </div><!-- row --> </div><!-- page_13 --> <div id="page_14" class="hiddenDiv"> <div class="row"> <div class="col-sm-12"> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_12");'>12</a></li> <li><a href="#" onclick='return showDiv("page_13");'>13</a></li> <li class="active"><span>14</span></li> <li><a href="#" onclick='return showDiv("page_15");'>15</a></li> <li><a href="#" onclick='return showDiv("page_16");'>16</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div> </div> <div class="row"> <div class="col-sm-12"> <ol class="result-class" start="261"> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/27618407','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/27618407"><span>Better together? Examining <span class="hlt">profiles</span> of employee recovery experiences.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Bennett, Andrew A; Gabriel, Allison S; Calderwood, Charles; Dahling, Jason J; Trougakos, John P</p> <p>2016-12-01</p> <p>Employees are exposed to a wide variety of job demands that deplete personal resources and necessitate recovery. In light of this need, research on work recovery has focused on how distinct recovery experiences during postwork time relate to employee well-being. However, investigators have largely tested the effects of these experiences in isolation, neglecting the possibility that <span class="hlt">profiles</span> of recovery experiences may exist and influence the recovery process. The current set of studies adopted a person-centered approach using latent <span class="hlt">profile</span> analysis to understand whether unique constellations of recovery experiences-psychological detachment, relaxation, mastery, control, and problem-solving pondering-emerged for 2 samples of full-time employees. In Study 1, which involved a single-time-point assessment, we identified 4 unique <span class="hlt">profiles</span> of recovery experiences, tested whether job demands (i.e., time <span class="hlt">pressure</span>, role ambiguity) and job resources (i.e., job control) differentiated <span class="hlt">profile</span> membership, and evaluated whether each <span class="hlt">profile</span> uniquely related to employee well-being outcomes (i.e., emotional exhaustion, engagement, somatic complaints). In Study 2, which involved 2 time points, we replicated 3 of the 4 <span class="hlt">profiles</span> <span class="hlt">observed</span> in Study 1, and tested 2 additional antecedents rated by employees' supervisors: leader-member exchange and supervisor support for recovery. Across both studies, unique differences emerged in regard to antecedents and outcomes tied to recovery experience <span class="hlt">profile</span> membership. (PsycINFO Database Record (c) 2016 APA, all rights reserved).</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/24059637','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/24059637"><span>Ramadan fasting ameliorates arterial pulse <span class="hlt">pressure</span> and lipid <span class="hlt">profile</span>, and alleviates oxidative stress in hypertensive patients.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Al-Shafei, Ahmad I M</p> <p>2014-06-01</p> <p>Effects of Ramadan fasting on health are important. Its effects on arterial pulse <span class="hlt">pressure</span> (PP), lipid <span class="hlt">profile</span> and oxidative stress were characterized in hypertensives. PP, indices of lipid <span class="hlt">profile</span> and oxidative stress were measured pre-, during and post-fasting in equal (40 each), sex- and age-matched groups (age 55 ± 5 years) of hypertensives (HT) and controls (C). Fasting reduced PP significantly by 17.2% and insignificantly by 9.3% in the HT and C groups, respectively. Total cholesterol (TC) was lowered insignificantly by 11.7% and 4.7% in the HT and C patients, respectively. Triglycerides (TG) and malondialdehyde (MDA) were significantly lowered by: TG: 24.5% and 22.8%; MDA: 45.6% and 54.3%; while glutathione (GSH) elevated by 56.8% and 52.6% in the HT and C groups, respectively. High-density lipoproteins (HDL) were raised significantly by 33.3% and insignificantly by 6.7%, whereas low-density lipoproteins (LDL) decreased significantly by 17.7% and insignificantly by 4.0% in the HT and C groups, respectively. At 6 weeks post-fasting, MDA remained significantly lower than the pre-fasting level by 24.3% and 25.7%, and GSH higher by 30.2% and 26.3% in the HT and C groups, respectively, while PP and TC returned to pre-fasting values in both groups. The post-fasting, HDL was significantly higher by 20.3% and LDL lower by 12.0% than the fasting levels in the HT patients. Fasting improves PP and lipids <span class="hlt">profile</span> and ameliorates oxidative stress in hypertensives.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2015ACPD...15.6745S','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2015ACPD...15.6745S"><span>Simulating CO2 <span class="hlt">profiles</span> using NIES TM and comparison with HIAPER Pole-to-Pole <span class="hlt">Observations</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Song, C.; Maksyutov, S.; Belikov, D.; Takagi, H.; Shu, J.</p> <p>2015-03-01</p> <p>We present a study on validation of the National Institute for Environmental Studies Transport Model (NIES TM) by comparing to <span class="hlt">observed</span> vertical <span class="hlt">profiles</span> of atmospheric CO2. The model uses a hybrid sigma-isentropic (σ-θ) vertical coordinate that employs both terrain-following and isentropic parts switched smoothly in the stratosphere. The model transport is driven by reanalyzed meteorological fields and designed to simulate seasonal and diurnal cycles, synoptic variations, and spatial distributions of atmospheric chemical constituents in the troposphere. The model simulations were run for biosphere, fossil fuel, air-ocean exchange, biomass burning and inverse correction fluxes of carbon dioxide (CO2) by GOSAT Level 4 product. We compared the NIES TM simulated fluxes with data from the HIAPER Pole-to-Pole <span class="hlt">Observations</span> (HIPPO) Merged 10 s Meteorology, Atmospheric Chemistry, and Aerosol Data, including HIPPO-1, HIPPO-2 and HIPPO-3 from 128.0° E to -84.0° W, and 87.0° N to -67.2° S. The simulation results were compared with CO2 <span class="hlt">observations</span> made in January and November 2009, and March and April 2010. The analysis attests that the model is good enough to simulate vertical <span class="hlt">profiles</span> with errors generally within 1-2 ppmv, except for the lower stratosphere in the Northern Hemisphere high latitudes.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.fs.usda.gov/treesearch/pubs/48398','TREESEARCH'); return false;" href="https://www.fs.usda.gov/treesearch/pubs/48398"><span>CO2 flux through a Wyoming seasonal snowpack: Diffusional and <span class="hlt">pressure</span> pumping effects</span></a></p> <p><a target="_blank" href="http://www.fs.usda.gov/treesearch/">Treesearch</a></p> <p>William Massman; Richard Sommerfeld; Karl Zeller; Ted Hehn; Laura Hudnell; Shannon Rochelle</p> <p>1995-01-01</p> <p>The movement of trace gases through porous media results from a combination of molecular diffusion and natural convection forced by turbulent atmospheric <span class="hlt">pressure</span> pumping. This study presents <span class="hlt">observational</span> and modeling results of an experiment to estimate the C02 flux through a seasonal snowpack in the Rocky Mountains of southern Wyoming, USA. <span class="hlt">Profiles</span> of C02 mole...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/1997APS..GEC.CM106K','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/1997APS..GEC.CM106K"><span>Kinetic description of large-scale low <span class="hlt">pressure</span> glow discharges</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Kortshagen, Uwe; Heil, Brian</p> <p>1997-10-01</p> <p>In recent years the so called ``nonlocal approximation'' to the solution of the electron Boltzmann equation has attracted considerable attention as an extremely efficient method for the kinetic modeling of low <span class="hlt">pressure</span> discharges. However, it appears that modern discharges, which are optimized to provide large-scale plasma uniformity, are explicitly designed to work in a regime, in which the nonlocal approximation is no longer strictly valid. In the presentation we discuss results of a hybrid model, which is based on the natural division of the electron distribution function into a nonlocal body, which is determined by elastic collisions only, and a high energy part which requires a more complete treatment due to the action of inelastic collisions and wall losses of electrons. The method is applied to an inductively coupled low <span class="hlt">pressure</span> discharge. We discuss the transition from plasma density <span class="hlt">profiles</span> maximal on the discharge axis to plasma density <span class="hlt">profiles</span> with off-center maxima, which has been <span class="hlt">observed</span> in experiments. A positive feedback mechanism involved in this transition is pointed out.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/19950004619','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/19950004619"><span><span class="hlt">Observed</span> changes in the vertical <span class="hlt">profile</span> of stratopheric nitrous oxide at Thule, Greenland, February - March 1992</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Emmons, Louisa K.; Reeves, John M.; Shindell, Drew T.; Dezafra, Robert L.</p> <p>1994-01-01</p> <p>Using a ground-based mm-wave spectrometer, we have <span class="hlt">observed</span> stratospheric N2O over Thule, Greenland (76.3 N, 68.4 W) during late February and March, 1992. Vertical <span class="hlt">profiles</span> of mixing ratio ranging from 16 to 50 km were recovered from molecular emission spectra. The <span class="hlt">profiles</span> of early March show an abrupt increase in the lower-stratosphere N2O mixing ratio similar to the spring-to-summer change associated with the break up of the Antarctic polar vortex. This increase is correlated with changes in potential vorticity, air temperature, and ozone mixing ratio.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2015AGUFM.A43E0329H','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2015AGUFM.A43E0329H"><span>Validation of 10 years of SAO OMI Ozone <span class="hlt">Profiles</span> with Ozonesonde and MLS <span class="hlt">Observations</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Huang, G.; Liu, X.; Chance, K.; Bhartia, P. K.</p> <p>2015-12-01</p> <p>To evaluate the accuracy and long-term stability of the SAO OMI ozone <span class="hlt">profile</span> product, we validate ~10 years of ozone <span class="hlt">profile</span> product (Oct. 2004-Dec. 2014) against collocated ozonesonde and MLS data. Ozone <span class="hlt">profiles</span> as well stratospheric, tropospheric, lower tropospheric ozone columns are compared with ozonesonde data for different latitude bands, and time periods (e.g., 2004-2008/2009-2014 for without/with row anomaly. The mean biases and their standard deviations are also assessed as a function of time to evaluate the long-term stability and bias trends. In the mid-latitude and tropical regions, OMI generally shows good agreement with ozonesonde <span class="hlt">observations</span>. The mean ozone <span class="hlt">profile</span> biases are generally within 6% with up to 30% standard deviations. The biases of stratospheric ozone columns (SOC) and tropospheric ozone columns (TOC) are -0.3%-2.2% and -0.2%-3%, while standard deviations are 3.9%-5.8% and 14.4%-16.0%, respectively. However, the retrievals during 2009-2014 show larger standard deviations and larger temporal variations; the standard deviations increase by ~5% in the troposphere and ~2% in the stratosphere. Retrieval biases at individual levels in the stratosphere and upper troposphere show statistically significant trends and different trends for 2004-2008 and 2009-2014 periods. The trends in integrated ozone partial columns are less significant due to cancellation from various layers, except for significant trend in tropical SOC. These results suggest the need to perform time dependent radiometric calibration to maintain the long-term stability of this product. Similarly, we are comparing the OMI stratospheric ozone <span class="hlt">profiles</span> and SOC with collocated MLS data, and the results will be reported.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2015AGUFM.A51T..07D','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2015AGUFM.A51T..07D"><span>Calculating clear-sky radiative heating rates using the Fu-Liou RTM with inputs from <span class="hlt">observed</span> and reanalyzed <span class="hlt">profiles</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Dolinar, E. K.; Dong, X.; Xi, B.</p> <p>2015-12-01</p> <p>One-dimensional radiative transfer models (RTM) are a common tool used for calculating atmospheric heating rates and radiative fluxes. In the forward sense, RTMs use known (or <span class="hlt">observed</span>) quantities of the atmospheric state and surface characteristics to determine the appropriate surface and top-of-atmosphere (TOA) radiative fluxes. The NASA CERES science team uses the modified Fu-Liou RTM to calculate atmospheric heating rates and surface and TOA fluxes using the CERES <span class="hlt">observed</span> TOA shortwave (SW) and longwave (LW) fluxes as constraints to derive global surface and TOA radiation budgets using a reanalyzed atmospheric state (e.g. temperature and various greenhouse gases) from the newly developed MERRA-2. However, closure studies have shown that using the reanalyzed state as input to the RTM introduces some disparity between the RTM calculated fluxes and surface <span class="hlt">observed</span> ones. The purpose of this study is to generate a database of <span class="hlt">observed</span> atmospheric state <span class="hlt">profiles</span>, from satellite and ground-based sources, at several permanent Atmospheric Radiation Measurement (ARM) Program sites, including the Southern Great Plains (SGP), Northern Slope of Alaska (NSA) and Tropical Western Pacific Nauru (TWP-C2), and Eastern North Atlantic (ENA) permanent facilities. Since clouds are a major modulator of radiative transfer within the Earth's atmosphere, we will focus on the clear-sky conditions in this study, which will set up the baseline for our cloudy studies in the future. Clear-sky flux <span class="hlt">profiles</span> are calculated using the Edition 4 NASA LaRC modified Fu-Liou RTM. The aforementioned atmospheric <span class="hlt">profiles</span> generated in-house are used as input into the RTM, as well as from reanalyses. The calculated surface and TOA fluxes are compared with ARM surface measured and CERES satellite <span class="hlt">observed</span> SW and LW fluxes, respectively. Clear-sky cases are identified by the ARM radar-lidar <span class="hlt">observations</span>, as well as satellite <span class="hlt">observations</span>, at the select ARM sites.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/28128198','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/28128198"><span>Cell-like <span class="hlt">pressure</span> sensors reveal increase of mechanical stress towards the core of multicellular spheroids under compression.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Dolega, M E; Delarue, M; Ingremeau, F; Prost, J; Delon, A; Cappello, G</p> <p>2017-01-27</p> <p>The surrounding microenvironment limits tumour expansion, imposing a compressive stress on the tumour, but little is known how <span class="hlt">pressure</span> propagates inside the tumour. Here we present non-destructive cell-like microsensors to locally quantify mechanical stress distribution in three-dimensional tissue. Our sensors are polyacrylamide microbeads of well-defined elasticity, size and surface coating to enable internalization within the cellular environment. By isotropically compressing multicellular spheroids (MCS), which are spherical aggregates of cells mimicking a tumour, we show that the <span class="hlt">pressure</span> is transmitted in a non-trivial manner inside the MCS, with a <span class="hlt">pressure</span> rise towards the core. This <span class="hlt">observed</span> <span class="hlt">pressure</span> <span class="hlt">profile</span> is explained by the anisotropic arrangement of cells and our results suggest that such anisotropy alone is sufficient to explain the <span class="hlt">pressure</span> rise inside MCS composed of a single cell type. Furthermore, such <span class="hlt">pressure</span> distribution suggests a direct link between increased mechanical stress and previously <span class="hlt">observed</span> lack of proliferation within the spheroids core.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=3751437','PMC'); return false;" href="https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=3751437"><span>Evaluation of eating and rumination behaviour in cows using a noseband <span class="hlt">pressure</span> sensor</span></a></p> <p><a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pmc">PubMed Central</a></p> <p></p> <p>2013-01-01</p> <p>Background An automated technique for recording eating and rumination behaviour was evaluated in ten lactating Brown Swiss cows by comparing data obtained from a <span class="hlt">pressure</span> sensor with data obtained via direct <span class="hlt">observation</span> over a 24-hour period. The recording device involved a <span class="hlt">pressure</span> sensor integrated in the noseband of a halter. The analysed variables included number and duration of individual rumination, eating and resting phases, total daily length of these phases and number of cuds chewed per day. Results Eating and rumination phases were readily differentiated based on characteristic <span class="hlt">pressure</span> <span class="hlt">profiles</span>. Chewing movements during rumination were regular and generated regular waveforms with uniform amplitudes, whereas eating generated irregular waveforms with variable amplitudes. There was complete or almost complete agreement and no significant differences between data obtained via direct <span class="hlt">observation</span> and <span class="hlt">pressure</span> sensor technique. Both methods yielded an average of 16 daily eating phases with a mean duration of 28.3 minutes. Total time spent eating was 445.0 minutes for direct <span class="hlt">observation</span> and 445.4 minutes for the <span class="hlt">pressure</span> sensor technique. Both techniques recorded an average of 13.3 rumination phases with a mean duration of 30.3 (direct <span class="hlt">observation</span>) and of 30.2 (<span class="hlt">pressure</span> sensor) minutes. Total time spent ruminating per day, number of cuds per day and chewing cycles per cud were 389.3 and 388.3 minutes, 410.1 and 410.0 and 60.0 and 60.3 for direct <span class="hlt">observation</span> and <span class="hlt">pressure</span> sensor technique, respectively. There was a significant difference between the two methods with respect to mean number of chewing cycles per day (24′669, direct <span class="hlt">observation</span> vs. 24′751, <span class="hlt">pressure</span> sensor, P < 0.05, paired t-test). There were strong correlations between the two recording methods with correlation coefficients ranging from 0.98 to 1.00. Conclusions The results confirmed that measurements of eating and rumination variables obtained via the <span class="hlt">pressure</span> sensor technique are in</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2006HyPr...20..241K','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2006HyPr...20..241K"><span>Infiltration pattern in a regolith-fractured bedrock <span class="hlt">profile</span>: field <span class="hlt">observation</span> of a dye stain pattern</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Kim, Jae Gon; Lee, Gyoo Ho; Lee, Jin-Soo; Chon, Chul-Min; Kim, Tack Hyun; Ha, Kyoochul</p> <p>2006-02-01</p> <p>We examined the infiltration pattern of water in a regolith-bedrock <span class="hlt">profile</span> consisting of two overburdens (OB1 and OB2), a buried rice paddy soil (PS), two texturally distinctive weathered materials (WM1 and WM2) and a fractured sedimentary rock (BR), using a Brilliant Blue FCF dye tracer. A black-coloured coating in conducting fractures in WM1, WM2 and BR was analysed by X-ray diffraction and scanning electron microscopy. The dye tracer penetrated to greater than 2 m depth in the <span class="hlt">profile</span>. The macropore flow and saturated interflow were the major infiltration patterns in the <span class="hlt">profile</span>. Macropore flow and saturated interflow were <span class="hlt">observed</span> along fractures in WM1, WM2 and BR and at the dipping interfaces of PS-WM1, PS-WM2 and PS-BR respectively. Heterogeneous matrix flow occurred in upper overburden (OB1) and PS. Compared with OB1, the coarser textured OB2 acted as a physical barrier for vertical flow of water. The PS with low bulk density and many fine roots was another major conducting route of water in the <span class="hlt">profile</span>. Manganese oxide and iron oxide were positively identified in the black coating material and had low crystallinity and high surface area, indicating their high reactivity with conducting contaminants.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://ntrs.nasa.gov/search.jsp?R=20120013537&hterms=High+Pressure&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D40%26Ntt%3DHigh%2BPressure','NASA-TRS'); return false;" href="https://ntrs.nasa.gov/search.jsp?R=20120013537&hterms=High+Pressure&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D40%26Ntt%3DHigh%2BPressure"><span>A Record-High Ocean Bottom <span class="hlt">Pressure</span> in the South Pacific <span class="hlt">Observed</span> by GRACE</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Boening, Carmen; Lee, Tong; Zlotnicki, Victor</p> <p>2011-01-01</p> <p>In late 2009 to early 2010, the Gravity Recovery and Climate Experiment (GRACE) satellite pair <span class="hlt">observed</span> a record increase in ocean bottom <span class="hlt">pressure</span> (OBP) over a large mid-latitude region of the South East Pacific. Its magnitude is substantially larger than other oceanic events in the Southern Hemisphere found in the entire GRACE data records (2003-2010) on multi-month time scales. The OBP data help to understand the nature of a similar signal in sea surface height (SSH) anomaly <span class="hlt">observed</span> by altimetry: the SSH increase is mainly due to mass convergence. Analysis of the barotropic vorticity equation using scatterometer data, atmospheric reanalysis product, and GRACE and altimeter an atmospheric reanalysis product <span class="hlt">observations</span> suggests that the <span class="hlt">observed</span> OBP/SSH signal was primarily caused by wind stress curl associated with a strong and persistent anticyclone in late 2009 in combination with effects of planetary vorticity gradient, bottom topography, and friction</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2008A%26A...489..795C','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2008A%26A...489..795C"><span>Vertical temperature <span class="hlt">profile</span> and mesospheric winds retrieval on Mars from CO ;millimeter <span class="hlt">observations</span>. Comparison with general circulation model predictions</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Cavalié, T.; Billebaud, F.; Encrenaz, T.; Dobrijevic, M.; Brillet, J.; Forget, F.; Lellouch, E.</p> <p>2008-10-01</p> <p>Aims: We have recorded high spectral resolution spectra and derived precise atmospheric temperature <span class="hlt">profiles</span> and wind velocities in the atmosphere of Mars. We have compared <span class="hlt">observations</span> of the planetary mean thermal <span class="hlt">profile</span> and mesospheric wind velocities on the disk, obtained with our millimetric <span class="hlt">observations</span> of CO rotational lines, to predictions from the Laboratoire de Météorologie Dynamique (LMD) Mars General Circulation Model, as provided through the Mars Climate Database (MCD) numerical tool. Methods: We <span class="hlt">observed</span> the atmosphere of Mars at CO(1-0) and CO(2-1) wavelengths with the IRAM 30-m antenna in June 2001 and November 2005. We retrieved the mean thermal <span class="hlt">profile</span> of the planet from high and low spectral resolution data with an inversion method detailed here. High spectral resolution spectra were used to derive mesospheric wind velocities on the planetary disk. We also report here the use of 13CO(2-1) line core shifts to measure wind velocities at 40 km. Results: Neither the Mars Year 24 (MY24) nor the Dust Storm scenario from the Mars Climate Database (MCD) provides satisfactory fits to the 2001 and 2005 data when retrieving the thermal <span class="hlt">profiles</span>. The Warm scenario only provides good fits for altitudes lower than 30 km. The atmosphere is warmer than predicted up to 60 km and then becomes colder. Dust loading could be the reason for this mismatch. The MCD MY24 scenario predicts a thermal inversion layer between 40 and 60 km, which is not retrieved from the high spectral resolution data. Our results are generally in agreement with other <span class="hlt">observations</span> from 10 to 40 km in altitude, but our results obtained from the high spectral resolution spectra differ in the 40-70 km layer, where the instruments are the most sensitive. The wind velocities we retrieve from our 12CO <span class="hlt">observations</span> confirm MCD predictions for 2001 and 2005. Velocities obtained from 13CO <span class="hlt">observations</span> are consistent with MCD predictions in 2001, but are lower than predicted in 2005.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/25230047','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/25230047"><span>Mechanical breath <span class="hlt">profile</span> of airway <span class="hlt">pressure</span> release ventilation: the effect on alveolar recruitment and microstrain in acute lung injury.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Kollisch-Singule, Michaela; Emr, Bryanna; Smith, Bradford; Roy, Shreyas; Jain, Sumeet; Satalin, Joshua; Snyder, Kathy; Andrews, Penny; Habashi, Nader; Bates, Jason; Marx, William; Nieman, Gary; Gatto, Louis A</p> <p>2014-11-01</p> <p>Improper mechanical ventilation settings can exacerbate acute lung injury by causing a secondary ventilator-induced lung injury. It is therefore important to establish the mechanism by which the ventilator induces lung injury to develop protective ventilation strategies. It has been postulated that the mechanism of ventilator-induced lung injury is the result of heterogeneous, elevated strain on the pulmonary parenchyma. Acute lung injury has been associated with increases in whole-lung macrostrain, which is correlated with increased pathology. However, the effect of mechanical ventilation on alveolar microstrain remains unknown. To examine whether the mechanical breath <span class="hlt">profile</span> of airway <span class="hlt">pressure</span> release ventilation (APRV), consisting of a prolonged <span class="hlt">pressure</span>-time <span class="hlt">profile</span> and brief expiratory release phase, reduces microstrain. In a randomized, nonblinded laboratory animal study, rats were randomized into a controlled mandatory ventilation group (n = 3) and an APRV group (n = 3). Lung injury was induced by polysorbate lavage. A thoracotomy was performed and an in vivo microscope was placed on the lungs to measure alveolar mechanics. In the controlled mandatory ventilation group, multiple levels of positive end-expiratory <span class="hlt">pressure</span> (PEEP; 5, 10, 16, 20, and 24 cm H2O) were tested. In the APRV group, decreasing durations of expiratory release (time at low <span class="hlt">pressure</span> [T(low)]) were tested. The T(low) was set to achieve ratios of termination of peak expiratory flow rate (T-PEFR) to peak expiratory flow rate (PEFR) of 10%, 25%, 50%, and 75% (the smaller this ratio is [ie, 10%], the more time the lung is exposed to low <span class="hlt">pressure</span> during the release phase, which decreases end-expiratory lung volume and potentiates derecruitment). Alveolar perimeters were measured at peak inspiration and end expiration using digital image analysis, and strain was calculated by normalizing the change in alveolar perimeter length to the original length. Macrostrain was measured by volume</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/25984597','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/25984597"><span>In Situ <span class="hlt">Observations</span> of Thermoreversible Gelation and Phase Separation of Agarose and Methylcellulose Solutions under High <span class="hlt">Pressure</span>.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Kometani, Noritsugu; Tanabe, Masahiro; Su, Lei; Yang, Kun; Nishinari, Katsuyoshi</p> <p>2015-06-04</p> <p>Thermoreversible sol-gel transitions of agarose and methylcellulose (MC) aqueous solutions on isobaric cooling or heating under high <span class="hlt">pressure</span> up to 400 MPa have been investigated by in situ <span class="hlt">observations</span> of optical transmittance and falling-ball experiments. For agarose, which undergoes the gelation on cooling, the application of <span class="hlt">pressure</span> caused a gradual rise in the cloud-point temperature over the whole <span class="hlt">pressure</span> range examined, which is almost consistent with the <span class="hlt">pressure</span> dependence of gelling temperature estimated by falling-ball experiments, suggesting that agarose gel is stabilized by compression and that the gelation occurs nearly in parallel with phase separation under ambient and high-<span class="hlt">pressure</span> conditions. For MC, which undergoes the gelation on heating, the cloud-point temperature showed a slight rise with an initial elevation of <span class="hlt">pressure</span> up to ∼150 MPa, whereas it showed a marked depression above 200 MPa. In contrast, the gelling temperature of MC, which is nearly identical to the cloud-point temperature at ambient <span class="hlt">pressure</span>, showed a monotonous rise with increasing <span class="hlt">pressure</span> up to 350 MPa, which means that MC undergoes phase separation prior to gelation on heating under high <span class="hlt">pressure</span> above 200 MPa. Similar results were obtained for the melting process of MC gel on cooling. The unique behavior of the sol-gel transition of MC under high <span class="hlt">pressure</span> has been interpreted in terms of the destruction of hydrophobic hydration by compression.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://pubs.er.usgs.gov/publication/70023277','USGSPUBS'); return false;" href="https://pubs.er.usgs.gov/publication/70023277"><span>Diamond-anvil cell <span class="hlt">observations</span> of a new methane hydrate phase in the 100-MPa <span class="hlt">pressure</span> range</span></a></p> <p><a target="_blank" href="http://pubs.er.usgs.gov/pubs/index.jsp?view=adv">USGS Publications Warehouse</a></p> <p>Chou, I.-Ming; Sharma, A.; Burruss, R.C.; Hemley, R.J.; Goncharov, A.F.; Stern, L.A.; Kirby, S.H.</p> <p>2001-01-01</p> <p>A new high-<span class="hlt">pressure</span> phase of methane hydrate has been identified based on its high optical relief, distinct <span class="hlt">pressure</span>-temperature phase relations, and Raman spectra. In-situ optical <span class="hlt">observations</span> were made in a hydrothermal diamond-anvil cell at temperatures between -40?? and 60 ??C and at <span class="hlt">pressures</span> up to 900 MPa. Two new invariant points were located at -8.7 ??C and 99 MPa for the assemblage consisting of the new phase, structure I methane hydrate, ice Ih, and water, and at 35.3 ??C and 137 MPa for the new phase-structure I methane hydrate-water-methane vapor. Existence of the new phase is critical for understanding the phase relations among the hydrates at low to moderate <span class="hlt">pressures</span>, and may also have important implications for understanding the hydrogen bonding in H2O and the behavior of water in the planetary bodies, such as Europa, of the outer solar system.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.osti.gov/pages/biblio/1408469-observing-electrochemical-oxidation-co-metal-solid-liquid-interface-using-ambient-pressure-ray-photoelectron-spectroscopy','SCIGOV-DOEP'); return false;" href="https://www.osti.gov/pages/biblio/1408469-observing-electrochemical-oxidation-co-metal-solid-liquid-interface-using-ambient-pressure-ray-photoelectron-spectroscopy"><span><span class="hlt">Observing</span> the Electrochemical Oxidation of Co Metal at the Solid/Liquid Interface Using Ambient <span class="hlt">Pressure</span> X-ray Photoelectron Spectroscopy</span></a></p> <p><a target="_blank" href="http://www.osti.gov/pages">DOE PAGES</a></p> <p>Han, Yong; Axnanda, Stephanus; Crumlin, Ethan J.; ...</p> <p>2017-08-28</p> <p>Some rcent advances of ambient <span class="hlt">pressure</span> X-ray photoelectron spectroscopy (AP-XPS) have enabled the chemical composition and the electrical potential <span class="hlt">profile</span> at a liquid/electrode interface under electrochemical reaction conditions to be directly probed. In this work, we apply this operando technique to study the surface chemical composition evolution on a Co metal electrode in 0.1 M KOH aqueous solution under various electrical biases. It is found that an ~12.2 nm-thick layer of Co(OH) 2 forms at a potential of about -0.4 V Ag/AgCl, and upon increasing the anodic potential to about +0.4 V Ag/AgCl, this layer is partially oxidized into cobaltmore » oxyhydroxide (CoOOH). A CoOOH/Co(OH) 2 mixture layer is formed on the top of the electrode surface. Finally, the oxidized surface layer can be reduced to Co0 at a cathodic potential of -1.35 VAg/Cl. Our <span class="hlt">observations</span> indicate that the ultrathin layer containing cobalt oxyhydroxide is the active phase for oxygen evolution reaction (OER) on a Co electrode in an alkaline electrolyte, consistent with previous studies.« less</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2006A%26A...455..987A','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2006A%26A...455..987A"><span>On the AU Microscopii debris disk. Density <span class="hlt">profiles</span>, grain properties, and dust dynamics</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Augereau, J.-C.; Beust, H.</p> <p>2006-09-01</p> <p>Context: . AU Mic is a young M-type star surrounded by an edge-on optically thin debris disk that shares many common <span class="hlt">observational</span> properties with the disk around β Pictoris. In particular, the scattered light surface brightness <span class="hlt">profile</span> falls off as ˜ r-5 outside 120 AU for β Pictoris and 35 AU for AU Mic. In both cases, the disk color rises as the distance increases beyond these reference radii. Aims: . In this paper, we present the first comprehensive analysis of the AU Mic disk properties since the system was resolved by Kalas et al. (2004, Science, 303, 1990). We explore whether the dynamical model, which successfully reproduces the β Pictoris brightness <span class="hlt">profile</span> (e.g., Augereau et al. 2001, A&A, 370, 447), could apply to AU Mic. Methods: . We calculate the surface density <span class="hlt">profile</span> of the AU Mic disk by performing the inversion of the near-IR and visible scattered light brightness <span class="hlt">profiles</span> measured by Liu (2004, Science, 305, 1442) and Krist et al. (2005, AJ, 129, 1008), respectively. We discuss the grain properties by analysing the blue color of the disk in the visible (Krist et al. 2005) and by fitting the disk spectral energy distribution. Finally, we evaluate the radiation and wind forces on the grains. The impact of the recurrent X-ray and UV-flares on the dust dynamics is also discussed. Results: . We show that irrespective of the mean scattering asymmetry factor of the grains, most of the emission arises from an asymmetric, collisionally-dominated region that peaks close to the surface brightness break around 35 AU. The elementary scatterers at visible wavelengths are found to be sub-micronic, but the inferred size distribution underestimates the number of large grains, resulting in sub-millimeter emissions that are too low compared to the <span class="hlt">observations</span>. From our inversion procedure, we find that the V- to H-band scattering cross sections ratio increases outside 40 AU, in line with the <span class="hlt">observed</span> color gradient of the disk. This behavior is expected if</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.osti.gov/biblio/22666073-extrasolar-storms-pressure-dependent-changes-light-curve-phase-brown-dwarfs-from-simultaneous-hst-spitzer-observations','SCIGOV-STC'); return false;" href="https://www.osti.gov/biblio/22666073-extrasolar-storms-pressure-dependent-changes-light-curve-phase-brown-dwarfs-from-simultaneous-hst-spitzer-observations"><span>EXTRASOLAR STORMS: <span class="hlt">PRESSURE</span>-DEPENDENT CHANGES IN LIGHT-CURVE PHASE IN BROWN DWARFS FROM SIMULTANEOUS HST AND SPITZER <span class="hlt">OBSERVATIONS</span></span></a></p> <p><a target="_blank" href="http://www.osti.gov/search">DOE Office of Scientific and Technical Information (OSTI.GOV)</a></p> <p>Yang, Hao; Apai, Dániel; Karalidi, Theodora</p> <p></p> <p>We present Spitzer /Infrared Array Camera Ch1 and Ch2 monitoring of six brown dwarfs during eight different epochs over the course of 20 months. For four brown dwarfs, we also obtained simulataneous Hubble Space Telescope ( HST )/WFC3 G141 grism spectra during two epochs and derived light curves in five narrowband filters. Probing different <span class="hlt">pressure</span> levels in the atmospheres, the multiwavelength light curves of our six targets all exhibit variations, and the shape of the light curves evolves over the timescale of a rotation period, ranging from 1.4 to 13 hr. We compare the shapes of the light curves andmore » estimate the phase shifts between the light curves <span class="hlt">observed</span> at different wavelengths by comparing the phase of the primary Fourier components. We use state-of-the-art atmosphere models to determine the flux contribution of different <span class="hlt">pressure</span> layers to the <span class="hlt">observed</span> flux in each filter. We find that the light curves that probe higher <span class="hlt">pressures</span> are similar and in phase, but are offset and often different from the light curves that probe lower <span class="hlt">pressures</span>. The phase differences between the two groups of light curves suggest that the modulations seen at lower and higher <span class="hlt">pressures</span> may be introduced by different cloud layers.« less</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/12110067','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/12110067"><span>Reproducibility of blood <span class="hlt">pressure</span> variation in older ambulatory and bedridden subjects.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Tsuchihashi, Takuya; Kawakami, Yasunobu; Imamura, Tsuyoshi; Abe, Isao</p> <p>2002-06-01</p> <p>We investigated the influence of ambulation on the reproducibility of circadian blood <span class="hlt">pressure</span> variation in older nursing home residents. Ambulatory blood <span class="hlt">pressure</span> monitoring was performed twice in 37 older nursing home residents. Nursing home in Japan. Subjects included 18 ambulatory nursing home residents who had no limitation on physical activity and 19 bedridden residents who did not participate in physical activity. Twenty-four-hour, daytime, and nighttime blood <span class="hlt">pressure</span> levels and their variability. The 24-hour and daytime variability of systolic blood <span class="hlt">pressure</span> (SBP) was significantly greater in ambulatory than in bedridden subjects, whereas nighttime variability was similar. Significant correlations in SBP averaged for the whole day, daytime, and nighttime were <span class="hlt">observed</span> between the two examinations in ambulatory (r =.80-.83) and bedridden (r =.83-.91) subjects, but the variabilities of SBP for the whole day and during the daytime of the first measurement were correlated with those of the second measurement in bedridden (r =.67 and r =.47, respectively) but not in ambulatory (r =.39 and r =.28, respectively) subjects. Significant correlations were found between the nocturnal SBP changes at two occasions in both ambulatory (r =.50) and bedridden (r =.51) subjects, but the dipper versus nondipper <span class="hlt">profiles</span>, defined as reduction in SBP of greater than 10% versus not, showed low reproducibility in ambulatory subjects; five ambulatory (28%) and one bedridden (5%) subjects showed divergent <span class="hlt">profiles</span> between the two examinations. The reproducibility of blood <span class="hlt">pressure</span> variation in nursing home residents is influenced by ambulation.</p> </li> </ol> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_12");'>12</a></li> <li><a href="#" onclick='return showDiv("page_13");'>13</a></li> <li class="active"><span>14</span></li> <li><a href="#" onclick='return showDiv("page_15");'>15</a></li> <li><a href="#" onclick='return showDiv("page_16");'>16</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div><!-- col-sm-12 --> </div><!-- row --> </div><!-- page_14 --> <div id="page_15" class="hiddenDiv"> <div class="row"> <div class="col-sm-12"> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_13");'>13</a></li> <li><a href="#" onclick='return showDiv("page_14");'>14</a></li> <li class="active"><span>15</span></li> <li><a href="#" onclick='return showDiv("page_16");'>16</a></li> <li><a href="#" onclick='return showDiv("page_17");'>17</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div> </div> <div class="row"> <div class="col-sm-12"> <ol class="result-class" start="281"> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017JGRC..122.6668J','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017JGRC..122.6668J"><span>Annual nitrate drawdown <span class="hlt">observed</span> by SOCCOM <span class="hlt">profiling</span> floats and the relationship to annual net community production</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Johnson, Kenneth S.; Plant, Joshua N.; Dunne, John P.; Talley, Lynne D.; Sarmiento, Jorge L.</p> <p>2017-08-01</p> <p>Annual nitrate cycles have been measured throughout the pelagic waters of the Southern Ocean, including regions with seasonal ice cover and southern hemisphere subtropical zones. Vertically resolved nitrate measurements were made using in situ ultraviolet spectrophotometer (ISUS) and submersible ultraviolet nitrate analyzer (SUNA) optical nitrate sensors deployed on <span class="hlt">profiling</span> floats. Thirty-one floats returned 40 complete annual cycles. The mean nitrate <span class="hlt">profile</span> from the month with the highest winter nitrate minus the mean <span class="hlt">profile</span> from the month with the lowest nitrate yields the annual nitrate drawdown. This quantity was integrated to 200 m depth and converted to carbon using the Redfield ratio to estimate annual net community production (ANCP) throughout the Southern Ocean south of 30°S. A well-defined, zonal mean distribution is found with highest values (3-4 mol C m-2 yr-1) from 40 to 50°S. Lowest values are found in the subtropics and in the seasonal ice zone. The area weighted mean was 2.9 mol C m-2 yr-1 for all regions south of 40°S. Cumulative ANCP south of 50°S is 1.3 Pg C yr-1. This represents about 13% of global ANCP in about 14% of the global ocean area.<abstract type="synopsis"><title type="main">Plain Language SummaryThis manuscript reports on 40 annual cycles of nitrate <span class="hlt">observed</span> by chemical sensors on SOCCOM <span class="hlt">profiling</span> floats. The annual drawdown in nitrate concentration by phytoplankton is used to assess the spatial variability of annual net community production in the Southern Ocean. This ANCP is a key component of the global carbon cycle and it exerts an important control on atmospheric carbon dioxide. We show that the results are consistent with our prior understanding of Southern Ocean ANCP, which has required decades of <span class="hlt">observations</span> to accumulate. The <span class="hlt">profiling</span> floats now enable annual resolution of this key process. The results also highlight spatial variability in ANCP in the Southern Ocean.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/27788267','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/27788267"><span>HBK-14 and HBK-15 Do Not Influence Blood <span class="hlt">Pressure</span>, Lipid <span class="hlt">Profile</span>, Glucose Level, or Liver Enzymes Activity after Chronic Treatment in Rats.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Pytka, Karolina; Głuch-Lutwin, Monika; Knutelska, Joanna; Jakubczyk, Magdalena; Waszkielewicz, Anna; Kotańska, Magdalena</p> <p>2016-01-01</p> <p>Older and even new antidepressants cause adverse effects, such as orthostatic hypotension, hyper- or hypoglycemia, liver injury or lipid disorders. In our previous experiments we showed significant antidepressant- and anxiolytic-like activities of dual 5-HT1A and 5-HT7 antagonists with α1-adrenolitic properties i.e. 1-[(2,6-dimethylphenoxy)ethoxyethyl]-4-(2-methoxyphenyl)piperazine hydrochloride (HBK-14) and 1-[(2-chloro-6-methylphenoxy)ethoxyethyl]-4-(2-methoxyphenyl)piperazine hydrochloride (HBK-15). Here, we evaluated the influence of chronic administration of HBK-14 and HBK-15 on blood <span class="hlt">pressure</span> (non-invasive blood <span class="hlt">pressure</span> measurement system for rodents), lipid <span class="hlt">profile</span> (total cholesterol, low density lipoproteins-LDL, high density lipoproteins-HDL, triglycerides), glucose level, and liver enzymes activity (aspartate aminotransferase, alanine aminotransferase, γ-glutamyl transferase). We determined potential antihistaminic (isolated guinea pig ileum) and antioxidant properties (ferric reducing ability of plasma-FRAP, non-protein thiols-NPSH, stable free radical diphenylpicrylhydrazyl-DPPH) cytotoxicity. Our experiments revealed that HBK-14 and HBK-15 did not influence blood <span class="hlt">pressure</span>, lipid <span class="hlt">profile</span>, glucose level or liver enzymes activity in rats after 2-week treatment. We also showed that none of the compounds possessed antioxidant or cytotoxic properties at antidepressant- and anxiolytic-like doses. HBK-14 and HBK-15 very weakly blocked H1 receptors in guinea pig ileum. Positive results of our preliminary experiments on the safety of HBK-14 and HBK-15 encourage further studies concerning their effectiveness in the treatment of depression and/or anxiety disorders.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/18637201','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/18637201"><span>Differences in evolutionary <span class="hlt">pressure</span> acting within highly conserved ortholog groups.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Przytycka, Teresa M; Jothi, Raja; Aravind, L; Lipman, David J</p> <p>2008-07-17</p> <p>In highly conserved widely distributed ortholog groups, the main evolutionary force is assumed to be purifying selection that enforces sequence conservation, with most divergence occurring by accumulation of neutral substitutions. Using a set of ortholog groups from prokaryotes, with a single representative in each studied organism, we asked the question if this evolutionary <span class="hlt">pressure</span> is acting similarly on different subgroups of orthologs defined as major lineages (e.g. Proteobacteria or Firmicutes). Using correlations in entropy measures as a proxy for evolutionary <span class="hlt">pressure</span>, we <span class="hlt">observed</span> two distinct behaviors within our ortholog collection. The first subset of ortholog groups, called here informational, consisted mostly of proteins associated with information processing (i.e. translation, transcription, DNA replication) and the second, the non-informational ortholog groups, mostly comprised of proteins involved in metabolic pathways. The evolutionary <span class="hlt">pressure</span> acting on non-informational proteins is more uniform relative to their informational counterparts. The non-informational proteins show higher level of correlation between entropy <span class="hlt">profiles</span> and more uniformity across subgroups. The low correlation of entropy <span class="hlt">profiles</span> in the informational ortholog groups suggest that the evolutionary <span class="hlt">pressure</span> acting on the informational ortholog groups is not uniform across different clades considered this study. This might suggest "fine-tuning" of informational proteins in each lineage leading to lineage-specific differences in selection. This, in turn, could make these proteins less exchangeable between lineages. In contrast, the uniformity of the selective <span class="hlt">pressure</span> acting on the non-informational groups might allow the exchange of the genetic material via lateral gene transfer.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/23939415','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/23939415"><span>Nonlinear mixed effects modeling of the diurnal blood <span class="hlt">pressure</span> <span class="hlt">profile</span> in a multiracial population.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>van Rijn-Bikker, Petra C; Snelder, Nelleke; Ackaert, Oliver; van Hest, Reinier M; Ploeger, Bart A; van Montfrans, Gert A; Koopmans, Richard P; Mathôt, Ron A</p> <p>2013-09-01</p> <p>Cardiac and cerebrovascular events in hypertensive patients are related to specific features of the 24-hour diurnal blood <span class="hlt">pressure</span> (BP) <span class="hlt">profile</span> (i.e., daytime and nighttime BP, nocturnal dip (ND), and morning surge (MS)). This investigation aimed to characterize 24-hour diurnal systolic BP (SBP) with parameters that correlate directly with daytime and nighttime SBP, ND, and MS using nonlinear mixed effects modeling. Ambulatory 24-hour SBP measurements (ABPM) of 196 nontreated subjects from three ethnic groups were available. A population model was parameterized in NONMEM to estimate and evaluate the parameters baseline SBP (BSL), nadir (minimum SBP during the night), and change (SBP difference between day and night). Associations were tested between these parameters and patient-related factors to explain interindividual variability. The diurnal SBP <span class="hlt">profile</span> was adequately described as the sum of 2 cosine functions. The following typical values (interindividual variability) were found: BSL = 139 mm Hg (11%); nadir = 122 mm Hg (14%); change = 25 mm Hg (52%), and residual error = 12 mm Hg. The model parameters correlate well with daytime and nighttime SBP, ND, and MS (R (2) = 0.50-0.92). During covariate analysis, ethnicity was found to be associated with change; change was 40% higher in white Dutch subjects and 26.8% higher in South Asians than in blacks. The developed population model allows simultaneous estimation of BSL, nadir, and change for all individuals in the investigated population, regardless of individual number of SBP measurements. Ethnicity was associated with change. The model provides a tool to evaluate and optimize the sampling frequency for 24-hour ABPM.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/29091112','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/29091112"><span>Speech <span class="hlt">profile</span> of patients undergoing primary palatoplasty.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Menegueti, Katia Ignacio; Mangilli, Laura Davison; Alonso, Nivaldo; Andrade, Claudia Regina Furquim de</p> <p>2017-10-26</p> <p>To characterize the <span class="hlt">profile</span> and speech characteristics of patients undergoing primary palatoplasty in a Brazilian university hospital, considering the time of intervention (early, before two years of age; late, after two years of age). Participants were 97 patients of both genders with cleft palate and/or cleft and lip palate, assigned to the Speech-language Pathology Department, who had been submitted to primary palatoplasty and presented no prior history of speech-language therapy. Patients were divided into two groups: early intervention group (EIG) - 43 patients undergoing primary palatoplasty before 2 years of age and late intervention group (LIG) - 54 patients undergoing primary palatoplasty after 2 years of age. All patients underwent speech-language pathology assessment. The following parameters were assessed: resonance classification, presence of nasal turbulence, presence of weak intraoral air <span class="hlt">pressure</span>, presence of audible nasal air emission, speech understandability, and compensatory articulation disorder (CAD). At statistical significance level of 5% (p≤0.05), no significant difference was <span class="hlt">observed</span> between the groups in the following parameters: resonance classification (p=0.067); level of hypernasality (p=0.113), presence of nasal turbulence (p=0.179); presence of weak intraoral air <span class="hlt">pressure</span> (p=0.152); presence of nasal air emission (p=0.369), and speech understandability (p=0.113). The groups differed with respect to presence of compensatory articulation disorders (p=0.020), with the LIG presenting higher occurrence of altered phonemes. It was possible to assess the general <span class="hlt">profile</span> and speech characteristics of the study participants. Patients submitted to early primary palatoplasty present better speech <span class="hlt">profile</span>.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/25624205','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/25624205"><span>Changes in the contents and <span class="hlt">profiles</span> of selected phenolics, soyasapogenols, tocopherols, and amino acids during soybean-rice mixture cooking: Electric rice cooker vs electric <span class="hlt">pressure</span> rice cooker.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Kim, Seung-Hyun; Yu, Bo-Ra; Chung, Ill-Min</p> <p>2015-06-01</p> <p>This study investigated the changes in the contents and <span class="hlt">profiles</span> of 35 phenolics (including 12 isoflavones), four tocopherols, two soyasapogenols and 20 amino acids when soybean and rice were cooked together (soybean-rice mixture) using either an electric rice cooker (ERC) or an electric <span class="hlt">pressure</span> rice cooker (EPRC). The contents of the 35 selected phenolics in soybean decreased by 12% and 8% upon cooking by ERC and EPRC, respectively, and their <span class="hlt">profiles</span> were different from that prior to cooking (P<0.05). Total tocopherol content of soybeans decreased by 7% after cooking in an ERC, but increased by 3% in soybeans cooked by EPRC. Total soyasapogenol content in soybeans cooked by ERC and EPRC decreased by 15% and 6%, respectively. Lastly, the total amino acid content of soybeans increased by 41% and 10% after cooking by ERC and EPRC, respectively. This study extends our knowledge about the effects of heat and <span class="hlt">pressure</span> on the contents and <span class="hlt">profiles</span> of bioactive compounds during soybean-rice mixture cooking. These results may be useful for improving the quality of bioactive compounds in soybean and rice depending on cooking conditions. Copyright © 2014 Elsevier Ltd. All rights reserved.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.osti.gov/biblio/22599868-effects-electron-pressure-anisotropy-current-sheet-configuration','SCIGOV-STC'); return false;" href="https://www.osti.gov/biblio/22599868-effects-electron-pressure-anisotropy-current-sheet-configuration"><span>Effects of electron <span class="hlt">pressure</span> anisotropy on current sheet configuration</span></a></p> <p><a target="_blank" href="http://www.osti.gov/search">DOE Office of Scientific and Technical Information (OSTI.GOV)</a></p> <p>Artemyev, A. V., E-mail: aartemyev@igpp.ucla.edu; Angelopoulos, V.; Runov, A.</p> <p>2016-09-15</p> <p>Recent spacecraft <span class="hlt">observations</span> in the Earth's magnetosphere have demonstrated that the magnetotail current sheet can be supported by currents of anisotropic electron population. Strong electron currents are responsible for the formation of very thin (intense) current sheets playing the crucial role in stability of the Earth's magnetotail. We explore the properties of such thin current sheets with hot isotropic ions and cold anisotropic electrons. Decoupling of the motions of ions and electrons results in the generation of a polarization electric field. The distribution of the corresponding scalar potential is derived from the electron <span class="hlt">pressure</span> balance and the quasi-neutrality condition. Wemore » find that electron <span class="hlt">pressure</span> anisotropy is partially balanced by a field-aligned component of this polarization electric field. We propose a 2D model that describes a thin current sheet supported by currents of anisotropic electrons embedded in an ion-dominated current sheet. Current density <span class="hlt">profiles</span> in our model agree well with THEMIS <span class="hlt">observations</span> in the Earth's magnetotail.« less</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=2576329','PMC'); return false;" href="https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=2576329"><span>Aerophagia and Gastroesophageal Reflux Disease in Patients using Continuous Positive Airway <span class="hlt">Pressure</span>: A Preliminary <span class="hlt">Observation</span></span></a></p> <p><a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pmc">PubMed Central</a></p> <p>Watson, Nathaniel F.; Mystkowski, Sue K.</p> <p>2008-01-01</p> <p>Study Objectives: Aerophagia is a complication of continuous positive airway <span class="hlt">pressure</span> (CPAP) therapy for sleep disordered breathing (SDB), whereupon air is forced into the stomach and bowel. Associated discomfort can result in CPAP discontinuation. We hypothesize that aerophagia is associated with gastroesophageal reflux disease (GERD) via mechanisms involving GERD related lower esophageal sphincter (LES) compromise. Methods: Twenty-two subjects with aerophagia and 22 controls, matched for age, gender, and body mass index, who were being treated with CPAP for SDB were compared in regard to clinical aspects of GERD, GERD associated habits, SDB severity as measured by polysomnography, and mean CPAP <span class="hlt">pressure</span>. Results: More subjects with aerophagia had symptoms of GERD (77.3% vs. 36.4%; p < 0.01) and were on GERD related medications (45.5% vs. 18.2%, p < 0.05) than controls. Regarding polysomnography, mean oxygen saturation percentages were lower in the aerophagia group than controls (95.0% vs. 96.5%, p < 0.05). No other differences were <span class="hlt">observed</span>, including mean CPAP <span class="hlt">pressures</span>. No one in the aerophagia group (vs. 27.3% of the control group) was a current tobacco user (p < 0.01). There was no difference in caffeine or alcohol use between the 2 groups. Conclusions: These results imply aerophagia is associated with GERD symptoms and GERD related medication use. This finding suggests a relationship between GERD related LES pathophysiology and the development of aerophagia in patients with SDB treated with CPAP. Citation: Watson NF; Mystkowski SK. Aerophagia and gastroesophageal reflux disease in patients using continuous positive airway <span class="hlt">pressure</span>: a preliminary <span class="hlt">observation</span>. J Clin Sleep Med 2008;4(5):434–438. PMID:18853700</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2018AIPA....8d5201F','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2018AIPA....8d5201F"><span>Instability of a shear layer between multicomponent fluids at supercritical <span class="hlt">pressure</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Fu, Qing-fei; Zhang, Yun-xiao; Mo, Chao-jie; Yang, Li-jun</p> <p>2018-04-01</p> <p>The temporal instability of a thin shear layer lying between streams of two components of fluids has been studied. The effects of density <span class="hlt">profile</span> of the layer on the instability behavior were mainly considered. The detailed density <span class="hlt">profile</span> was obtained through Linear Gradient Theory. The eigenvalue problem was calculated, and the temporal instability curves were obtained for the thermodynamic parameters, e.g. <span class="hlt">pressure</span> and temperature. The results show that, increase of <span class="hlt">pressure</span> leads to the increase of the maximum growth rate. However, increasing <span class="hlt">pressure</span> has opposite effects on the disturbances with small and large wave length. The increase of temperature causes the decrease of disturbance growth rate. The instability behavior of the shear layers was determined mainly by the interval between the inflections of the velocity and density <span class="hlt">profiles</span>, and the maximum density gradient. The total effects, determined by coupling density stratification, and interval between the inflections of the velocity and density <span class="hlt">profiles</span>, were quite distinct for different ranges of temperature and <span class="hlt">pressure</span>.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017AtmRe.194..258S','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017AtmRe.194..258S"><span>Raman lidar water vapor <span class="hlt">profiling</span> over Warsaw, Poland</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Stachlewska, Iwona S.; Costa-Surós, Montserrat; Althausen, Dietrich</p> <p>2017-09-01</p> <p>Water vapor mixing ratio and relative humidity <span class="hlt">profiles</span> were derived from the multi-wavelength Raman PollyXT lidar at the EARLINET site in Warsaw, using the Rayleigh molecular extinction calculation based on atmospheric temperature and <span class="hlt">pressure</span> from three different sources: i) the standard atmosphere US 62, ii) the Global Data Assimilation System (GDAS) model output, and iii) the WMO 12374 radiosoundings launched at Legionowo. With each method, 136 midnight relative humidity <span class="hlt">profiles</span> were obtained for lidar <span class="hlt">observations</span> from July 2013 to August 2015. Comparisons of these <span class="hlt">profiles</span> showed in favor of the latter method (iii), but it also indicated that the other two data sources could replace it, if necessary. Such use was demonstrated for an automated retrieval of water vapor mixing ratio from dusk until dawn on 19/20 March 2015; a case study related to an advection of biomass burning aerosol from forest fires over Ukraine. Additionally, an algorithm that applies thresholds to the radiosounding relative humidity <span class="hlt">profiles</span> to estimate macro-physical cloud vertical structure was used for the first time on the Raman lidar relative humidity <span class="hlt">profiles</span>. The results, based on a subset of 66 <span class="hlt">profiles</span>, indicate that below 6 km cloud bases/tops can be successfully obtained in 53% and 76% cases from lidar and radiosounding <span class="hlt">profiles</span>, respectively. Finally, a contribution of the lidar derived mean relative humidity to cloudy conditions within the range of 0.8 to 6.2 km, in comparison to clear-sky conditions, was estimated.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=3345817','PMC'); return false;" href="https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=3345817"><span><span class="hlt">Observing</span> and Studying Extreme Low <span class="hlt">Pressure</span> Events with Altimetry</span></a></p> <p><a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pmc">PubMed Central</a></p> <p>Carrère, Loren; Mertz, Françoise; Dorandeu, Joel; Quilfen, Yves; Patoux, Jerome</p> <p>2009-01-01</p> <p>The ability of altimetry to detect extreme low <span class="hlt">pressure</span> events and the relationship between sea level <span class="hlt">pressure</span> and sea level anomalies during extra-tropical depressions have been investigated. Specific altimeter treatments have been developed for tropical cyclones and applied to obtain a relevant along-track sea surface height (SSH) signal: the case of tropical cyclone Isabel is presented here. The S- and C-band measurements are used because they are less impacted by rain than the Ku-band, and new sea state bias (SSB) and wet troposphere corrections are proposed. More accurate strong altimeter wind speeds are computed thanks to the Young algorithm. Ocean signals not related to atmospheric <span class="hlt">pressure</span> can be removed with accuracy, even within a Near Real Time context, by removing the maps of sea level anomaly (SLA) provided by SSALTO/Duacs. In the case of Extra-Tropical Depressions, the classical altimeter processing can be used. Ocean signal not related to atmospheric <span class="hlt">pressure</span> is along-track filtered. The sea level <span class="hlt">pressure</span> (SLP)-SLA relationship is investigated for the North Atlantic, North Pacific and Indian oceans; three regression models are proposed allowing restoring an altimeter SLP with a mean error of 5 hPa if compared to ECMWF or buoys SLP. The analysis of barotropic simulation outputs points out the regional variability of the SLP/Model Sea Level relationship and the wind effects. PMID:22573955</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/1997ApJ...481..267D','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/1997ApJ...481..267D"><span>The Dynamics of M15: <span class="hlt">Observations</span> of the Velocity Dispersion <span class="hlt">Profile</span> and Fokker-Planck Models</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Dull, J. D.; Cohn, H. N.; Lugger, P. M.; Murphy, B. W.; Seitzer, P. O.; Callanan, P. J.; Rutten, R. G. M.; Charles, P. A.</p> <p>1997-05-01</p> <p>We report a new measurement of the velocity dispersion <span class="hlt">profile</span> within 1' (3 pc) of the center of the globular cluster M15 (NGC 7078), using long-slit spectra from the 4.2 m William Herschel Telescope at La Palma Observatory. We obtained spatially resolved spectra for a total of 23 slit positions during two <span class="hlt">observing</span> runs. During each run, a set of parallel slit positions was used to map out the central region of the cluster; the position angle used during the second run was orthogonal to that used for the first. The spectra are centered in wavelength near the Ca II infrared triplet at 8650 Å, with a spectral range of about 450 Å. We determined radial velocities by cross-correlation techniques for 131 cluster members. A total of 32 stars were <span class="hlt">observed</span> more than once. Internal and external comparisons indicate a velocity accuracy of about 4 km s-1. The velocity dispersion <span class="hlt">profile</span> rises from about σ = 7.2 +/- 1.4 km s-1 near 1' from the center of the cluster to σ = 13.9 +/- 1.8 km s-1 at 20". Inside of 20", the dispersion remains approximately constant at about 10.2 +/- 1.4 km s-1 with no evidence for a sharp rise near the center. This last result stands in contrast with that of Peterson, Seitzer, & Cudworth who found a central velocity dispersion of 25 +/- 7 km s-1, based on a line-broadening measurement. Our velocity dispersion <span class="hlt">profile</span> is in good agreement with those determined in the recent studies of Gebhardt et al. and Dubath & Meylan. We have developed a new set of Fokker-Planck models and have fitted these to the surface brightness and velocity dispersion <span class="hlt">profiles</span> of M15. We also use the two measured millisecond pulsar accelerations as constraints. The best-fitting model has a mass function slope of x = 0.9 (where 1.35 is the slope of the Salpeter mass function) and a total mass of 4.9 × 105 M⊙. This model contains approximately 104 neutron stars (3% of the total mass), the majority of which lie within 6" (0.2 pc) of the cluster center. Since the</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/27338333','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/27338333"><span>Ultrahigh <span class="hlt">Pressure</span> Processing Produces Alterations in the Metabolite <span class="hlt">Profiles</span> of Panax ginseng.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Lee, Mee Youn; Singh, Digar; Kim, Sung Han; Lee, Sang Jun; Lee, Choong Hwan</p> <p>2016-06-22</p> <p>Ultrahigh <span class="hlt">pressure</span> (UHP) treatments are non-thermal processing methods that have customarily been employed to enhance the quality and productivity of plant consumables. We aimed to evaluate the effects of UHP treatments on ginseng samples (white ginseng: WG; UHP-treated WG: UWG; red ginseng: RG; UHP-treated RG: URG; ginseng berries: GB; and UHP-treated GB: UGB) using metabolite <span class="hlt">profiling</span> based on ultrahigh performance liquid chromatography-linear trap quadrupole-ion trap-tandem mass spectrometry (UHPLC-LTQ-IT-MS/MS) and gas chromatography time-of-flight mass spectrometry (GC-TOF-MS). Multivariate data analyses revealed a clear demarcation among the GB and UGB samples, and the phenotypic evaluations correlated the highest antioxidant activities and the total phenolic and flavonoid compositions with the UGB samples. Overall, eight amino acids, seven organic acids, seven sugars and sugar derivatives, two fatty acids, three notoginsenosides, three malonylginsenosides, and three ginsenosides, were identified as significantly discriminant metabolites between the GB and UGB samples, with relatively higher proportions in the latter. Ideally, these metabolites can be used as quality biomarkers for the assessment of ginseng products and our results indicate that UHP treatment likely led to an elevation in the proportions of total extractable metabolites in ginseng samples.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/10516739','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/10516739"><span>Blood <span class="hlt">pressure</span> and social support <span class="hlt">observations</span> from Mamre, South Africa, during social and political transition.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Daniels, A; Hoffman, M; Lombard, C; Steyn, K; Levitt, N; Katzenellenbogen, J</p> <p>1999-10-01</p> <p>Social support, by moderating cardiovascular reactivity, has been demonstrated to attenuate the effects of stress on blood <span class="hlt">pressure</span> in American communities. This is the first report to examine the relationship between social support and blood <span class="hlt">pressure</span> in a South African context, during a period of infrastructure modernisation and political change. A total of 1240 residents (542 men, 698 women) of mixed ethnic origin, older than 14 years and stratified by age and sex, participated in a survey to determine risk factors for hypertension and cardiovascular diseases. Social support was assessed by a questionnaire developed in consultation with the community. It was defined by interactions that may threaten family harmony (score 1) and by networking between relatives, friends, colleagues and neighbours (score 2). Mean blood <span class="hlt">pressure</span> of the sample was 130/79 mm Hg (s.d. 25/14 mm Hg). Hypertension prevalence was 26.9%. Only 36% of women compared to 57.3% of men (P < 0.0001) were employed. More women (29%) than men (22%) reported threats to family harmony, but social support networks were similarly perceived by both sexes. Systolic and diastolic blood <span class="hlt">pressure</span> correlated weakly with score 1 (r = 0.096, P < 0.0007) but no association was <span class="hlt">observed</span> with score 2. Score 1 was not associated with blood <span class="hlt">pressure</span> by multiple regression analysis, that included confounding by age, sex, BMI, alcohol consumption and smoking status. Neither threats to family harmony nor networking between relatives, friends or neighbours, significantly influences blood <span class="hlt">pressure</span> in this community. Measures of social support thought to moderate blood <span class="hlt">pressure</span> may have limited cross-cultural application. Attitudinal changes during socio-political transition may impact on the generalisability of instruments for measurement.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://ntrs.nasa.gov/search.jsp?R=19950041429&hterms=coma&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D50%26Ntt%3Dcoma','NASA-TRS'); return false;" href="https://ntrs.nasa.gov/search.jsp?R=19950041429&hterms=coma&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D50%26Ntt%3Dcoma"><span><span class="hlt">Observations</span> and analysis of O(1D) and NH2 line <span class="hlt">profiles</span> for the coma of comet P/Halley</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Smyth, William H.; Combi, Michael R.; Roesler, Fred L.; Scherb, Frank</p> <p>1995-01-01</p> <p>A set of high-resolution Fabry-Perot measurements of the coma of comet P/Halley was acquired in the (O I) 6300 A and NH2 6298.62 A emission lines. These high-resolution measurements provide the first optical <span class="hlt">observations</span> capable of studying directly the photochemical kinetics and dynamic outflow of the coma. The <span class="hlt">observations</span> were analyzed by a Monte Carlo Particle Trajectory Model. The agreement of the model and <span class="hlt">observed</span> line <span class="hlt">profiles</span> was excellent and verified the underlying dynamics, exothermic photodissociative chemistry, and collisional thermalization in the coma. The somewhat wider intrinsic line <span class="hlt">profile</span> width for the O(1D) emission in 1986 January compared to 1986 May, is, for example, produced by the larger outflow speeds and gas temperatures nearer perihelion in January. The January O(1D) <span class="hlt">profile</span>, which is wider than the January NH2 <span class="hlt">profile</span>, is indicative of the photochemical kinetics in the dissociation of the parent molecules H2O and OH in the coma. The absolute calibration of the <span class="hlt">observations</span> in 1986 January allowed the production rates for H2O and the NH2-parent molecules to be determined. The average daily water production rates derived from the O(1D) emission data for January 16 and 17 are presented. These very large water production rates are consistent with the extrapolated (and 7.6 day time variable) water production rates determined from the analysis of lower spectral resolution <span class="hlt">observations</span> for O(1D) and H-alpha emissions that covered the time period up to January 13. The large production rates on January 16 and 17 establish that the maximum water production rate for comet Halley accurred pre-perihelion in January. Implications drawn from comparison with 18 cm radio emission data in January suggest that the peak water production rate was even larger. The average production rate for NH3 determined from the NH2 emission data for January 17 was (1.48 +/- 0.10) x 10(exp 28) molecules/s, yielding an NH3/H2O production rate ratio of 0.55%.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2015EGUGA..1710719G','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2015EGUGA..1710719G"><span>Comparison of stratospheric NO2 <span class="hlt">profiles</span> above Kiruna, Sweden retrieved from ground-based zenith sky DOAS measurements, SAOZ balloon measurements and SCIAMACHY limb <span class="hlt">observations</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Gu, Myojeong; Enell, Carl-Fredrik; Hendrick, François; Pukite, Janis; Van Roozendael, Michel; Platt, Ulrich; Raffalski, Uwe; Wagner, Thomas</p> <p>2015-04-01</p> <p>Stratospheric NO2 not only destroys ozone but acts as a buffer against halogen catalyzed ozone loss by converting halogen species into stable nitrates. These two roles of stratospheric NO2 depend on the altitude. Hence, the objective of this study is to investigate the vertical distribution of stratospheric NO2. We compare the NO2 <span class="hlt">profiles</span> derived from the zenith sky DOAS with those obtained from, SAOZ balloon measurements and satellite limb <span class="hlt">observations</span>. Vertical <span class="hlt">profiles</span> of stratospheric NO2 are retrieved from ground-based zenith sky DOAS <span class="hlt">observations</span> operated at Kiruna, Sweden (68.84°N, 20.41°E) since 1996. To determine the <span class="hlt">profile</span> of stratospheric NO2 measured from ground-based zenith sky DOAS, we apply the Optimal Estimation Method (OEM) to retrieval of vertical <span class="hlt">profiles</span> of stratospheric NO2 which has been developed by IASB-BIRA. The basic principle behind this <span class="hlt">profiling</span> approach is the dependence of the mean scattering height on solar zenith angle (SZA). We compare the retrieved <span class="hlt">profiles</span> to two additional datasets of stratospheric NO2 <span class="hlt">profile</span>. The first one is derived from satellite limb <span class="hlt">observations</span> by SCIAMACHY (Scanning Imaging Absorption spectrometer for Atmospheric CHartographY) on EnviSAT. The second is derived from the SAOZ balloon measurements (using a UV/Visible spectrometer) performed at Kiruna in Sweden.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/15811750','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/15811750"><span>Experimental <span class="hlt">observation</span> of intraocular <span class="hlt">pressure</span> changes during microkeratome suctioning in laser in situ keratomileusis.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Bissen-Miyajima, Hiroko; Suzuki, Shintaro; Ohashi, Yoshie; Minami, Keiichiro</p> <p>2005-03-01</p> <p>To <span class="hlt">observe</span> changes in intraocular <span class="hlt">pressure</span> (IOP), the manner in which the eye is suctioned, and the effect of the number of suction ports. Department of Ophthalmology, Tokyo Dental College, Suidobashi Hospital, Tokyo, Japan. Suction rings with single or dual ports were made of transparent acrylic acid resin to facilitate <span class="hlt">observation</span> with a digital video camera. The IOP and the duration of the IOP increase (time to reach 90% of the maximum IOP) were measured in 6 porcine eyes with an intra-vein <span class="hlt">pressure</span>-sensor catheter in the vitreous cavity. The IOP changes were recorded using a personal computer. Suctioning with single- and dual-port suction rings was similar. The IOP increases with single- and dual-port suction rings were similar (99.1 mm Hg +/- 6.1 [SD] and 99.0 +/- 6.5 mm Hg, respectively) (P=.987). The duration of the IOP increase was also similar (4.21 +/- 0.24 seconds and 4.12 +/- 0.33 seconds, respectively) (P=.190). The number of ports did not affect suctioning and changes in IOP. This technique is useful in developing the ideal shape and setting of the suction ring.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2016AGUFMDI41C2638K','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2016AGUFMDI41C2638K"><span>Melting temperatures of MgO under high <span class="hlt">pressure</span> determined by micro-texture <span class="hlt">observation</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Kimura, T.; Ohfuji, H.; Nishi, M.; Irifune, T.</p> <p>2016-12-01</p> <p>Periclase (MgO) is the second abundant mineral after bridgmanite in the Earth's lower mantle, and its melting temperature (Tm) under <span class="hlt">pressure</span> is important to constrain the chemical composition of ultra-deep magma formed near the mantle-core boundary. However, the melting behavior is highly controversial among previous studies: a laser-heated diamond anvil cell (LHDAC) study reported a melting curve with a dTm/dP of 30 K/GPa at zero <span class="hlt">pressure</span> [1], while several theoretical computations gave substantially higher dTm/dP of 90 100 K/GPa [2,3]. We performed a series of LHDAC experiments for measurements of Tm of MgO under high <span class="hlt">pressure</span>, using single crystal MgO as the starting material. The melting was detected by using micro-texture <span class="hlt">observations</span> of the quenched samples. We found that the laser-heated area of the sample quenched from the Tm in previous LHDAC experiments [1] showed randomly aggregated granular crystals, which was not caused by melting, but by plastic deformation of the sample. This suggests that the Tms of their study were substantially underestimated. On the other hand, the sample recovered from the temperature higher by 1500-1700 K than the Tms in previous LHDAC experiments showed a characteristic internal texture comparable to the solidification texture typically shown in metal casting. We determined the Tms based on the <span class="hlt">observation</span> of this texture up to 32 GPa. Fitting our Tms to the Simon equation yields dTm/dP of 82 K/GPa at zero <span class="hlt">pressure</span>, which is consistent with those of the theoretical predictions (90 100 K/GPa) [2,3]. Extrapolation of the present melting curve of MgO to the <span class="hlt">pressure</span> of the CMB (135 GPa) gives a melting temperature of 8900 K. The present steep melting slope offers the eutectic composition close to peridotite (in terms of Mg/Si ratio) throughout the lower mantle conditions. According to the model for sink/float relationship between the solid mantle and the magma [4], a considerable amount of iron (Fe/(Mg+Fe) > 0.24) is expected</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/17547656','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/17547656"><span>During measurements of root hydraulics with <span class="hlt">pressure</span> probes, the contribution of unstirred layers is minimized in the <span class="hlt">pressure</span> relaxation mode: comparison with <span class="hlt">pressure</span> clamp and high-<span class="hlt">pressure</span> flowmeter.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Knipfer, Thorsten; Das, Debasish; Steudle, Ernst</p> <p>2007-07-01</p> <p>The effects of unstirred layers (USLs) at the endodermis of roots of young maize plants (Zea mays L.) were quantified, when measuring the water permeability of roots using a root <span class="hlt">pressure</span> probe (RPP) in the <span class="hlt">pressure</span> relaxation (PR) and <span class="hlt">pressure</span> clamp (PC) modes. Different from PRs, PCs were performed by applying a constant <span class="hlt">pressure</span> for certain periods of time. Experimental data were compared with results from simulations based on a convection versus diffusion (C/D) model, with the endodermis being the main barrier for solutes and water. Solute <span class="hlt">profiles</span> in the stele were calculated as they occurred during rapid water flows across the root. The model quantitatively predicted the experimental finding of two distinct phases during PRs, in terms of a build-up of concentration <span class="hlt">profiles</span> in the stele between endodermis and xylem vessels. It also predicted that, following a PC, half-times (T1/2) of PRs increased as the time used for clamping (and the build-up of USLs) increased. Following PCs of durations of 15, 30 and 60 s, T1/2 increased by factors of between 2.5 and 7.0, and water permeability of roots (root hydraulic conductivity, Lpr) was reduced by the same factors. When root <span class="hlt">pressure</span> was immediately taken back to the original equilibrium root <span class="hlt">pressure</span> following a PC, there was a transient uptake of water into the root stele (transient increase of root <span class="hlt">pressure</span>), and the size of transients rose with time of clamping, as predicted by the model. The results indicated that the 'real' hydraulic conductivity of roots should be measured during initial water flows, such as during the rapid phase of PRs, when the effect of USLs was minimized. It was discussed that '<span class="hlt">pressure</span>-propagation effects' could not explain the finding of two phases during PRs. The results of USL effects threw some doubt on the use of PC and high-<span class="hlt">pressure</span> flowmeter (HPFM) techniques with roots, where rigorous estimates of USLs were still missing despite the fact that large quantities of water were forced</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2016EGUGA..1816412M','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2016EGUGA..1816412M"><span>ACTRIS aerosol vertical <span class="hlt">profile</span> data and <span class="hlt">observations</span>: potentiality and first examples of integrated studies with models</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Mona, Lucia; Benedetti, Angela; D'Amico, Giuseppe; Myhre, Cathrine Lund; Schulz, Michael; Wandinger, Ulla; Laj, Paolo; Pappalardo, Gelsomina</p> <p>2016-04-01</p> <p>The ACTRIS-2 project, funded by Horizon 2020, addresses the scope of integrating state-of-the-art European ground-based stations for long term <span class="hlt">observations</span> of aerosols, clouds and short lived gases, capitalizing on the work of FP7-ACTRIS. It aims at achieving the construction of a user-oriented RI, unique in the EU-RI landscape for providing 4-D integrated high-quality data from near-surface to high altitude (vertical <span class="hlt">profiles</span> and total-column) which are relevant to climate and air-quality research. ACTRIS-2 develops and implements, in a large network of stations in Europe and beyond, <span class="hlt">observational</span> protocols that permit the harmonization of collected data and their dissemination. ACTRIS secures provision and dissemination of a unique set of data and data-products that would not otherwise be available with the same level of quality and standardization. This results from a 10-year plus effort in constructing a research infrastructure capable of responding to community needs and requirements, and has been engaged since the start of the FP5 EU commission program. ACTRIS ensures compliance with reporting requirements (timing, format, traceability) defined by the major global <span class="hlt">observing</span> networks. EARLINET (European Aerosol research Lidar NETwork), the aerosol vertical <span class="hlt">profiling</span> component of ACTRIS, is providing since May 2000 vertical <span class="hlt">profiles</span> of aerosol extinction and backscatter over Europe. A new structure of the EARLINET database has been designed in a more user oriented approach reporting new data products which are more effective for specific uses of different communities. In particular, a new era is starting with the Copernicus program during which the aerosol vertical <span class="hlt">profiling</span> capability will be fundamental for assimilation and validation purposes. The new data products have been designed thanks to a strong link with EARLINET data users, first of all modeling and satellite communities, established since the beginning of EARLINET and re-enforced within ACTRIS2</p> </li> </ol> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_13");'>13</a></li> <li><a href="#" onclick='return showDiv("page_14");'>14</a></li> <li class="active"><span>15</span></li> <li><a href="#" onclick='return showDiv("page_16");'>16</a></li> <li><a href="#" onclick='return showDiv("page_17");'>17</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div><!-- col-sm-12 --> </div><!-- row --> </div><!-- page_15 --> <div id="page_16" class="hiddenDiv"> <div class="row"> <div class="col-sm-12"> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_14");'>14</a></li> <li><a href="#" onclick='return showDiv("page_15");'>15</a></li> <li class="active"><span>16</span></li> <li><a href="#" onclick='return showDiv("page_17");'>17</a></li> <li><a href="#" onclick='return showDiv("page_18");'>18</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div> </div> <div class="row"> <div class="col-sm-12"> <ol class="result-class" start="301"> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/27878400','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/27878400"><span>Multiphoton microscopy <span class="hlt">observations</span> of 3D elastin and collagen fiber microstructure changes during <span class="hlt">pressurization</span> in aortic media.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Sugita, Shukei; Matsumoto, Takeo</p> <p>2017-06-01</p> <p>Elastin and collagen fibers play important roles in the mechanical properties of aortic media. Because knowledge of local fiber structures is required for detailed analysis of blood vessel wall mechanics, we investigated 3D microstructures of elastin and collagen fibers in thoracic aortas and monitored changes during <span class="hlt">pressurization</span>. Using multiphoton microscopy, autofluorescence images from elastin and second harmonic generation signals from collagen were acquired in media from rabbit thoracic aortas that were stretched biaxially to restore physiological dimensions. Both elastin and collagen fibers were <span class="hlt">observed</span> in all longitudinal-circumferential plane images, whereas alternate bright and dark layers were <span class="hlt">observed</span> along the radial direction and were recognized as elastic laminas (ELs) and smooth muscle-rich layers (SMLs), respectively. Elastin and collagen fibers are mainly oriented in the circumferential direction, and waviness of collagen fibers was significantly higher than that of elastin fibers. Collagen fibers were more undulated in longitudinal than in radial direction, whereas undulation of elastin fibers was equibiaxial. Changes in waviness of collagen fibers during <span class="hlt">pressurization</span> were then evaluated using 2-dimensional fast Fourier transform in mouse aortas, and indices of waviness of collagen fibers decreased with increases in intraluminal <span class="hlt">pressure</span>. These indices also showed that collagen fibers in SMLs became straight at lower intraluminal <span class="hlt">pressures</span> than those in EL, indicating that SMLs stretched more than ELs. These results indicate that deformation of the aorta due to <span class="hlt">pressurization</span> is complicated because of the heterogeneity of tissue layers and differences in elastic properties of ELs, SMLs, and surrounding collagen and elastin.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2013SPIE.8692E..3CW','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2013SPIE.8692E..3CW"><span>Road <span class="hlt">profile</span> estimation of city roads using DTPS</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Wang, Qi; McDaniel, J. Gregory; Sun, Nian X.; Wang, Ming L.</p> <p>2013-04-01</p> <p>This work presents a non-destructive and non-contact acoustic sensing approach for measuring road <span class="hlt">profile</span> of road and bridge deck with vehicles running at normal speed without stopping traffic. This approach uses an instantaneous and real-time dynamic tire <span class="hlt">pressure</span> sensor (DTPS) that can measure dynamic response of the tire-road interaction and increases the efficiency of currently used road <span class="hlt">profile</span> measuring systems with vehicle body-mounted <span class="hlt">profilers</span> and axle-mounted accelerometers. In this work, a prototype of real-time DTPS system has been developed and demonstrated on a testing van at speeds from 5 to 80 miles per hour (mph). A data analysis algorithm has been developed to remove axle dynamic motions from the measured DTPS data and to find the transfer function between dynamic tire <span class="hlt">pressure</span> change and the road <span class="hlt">profile</span>. Field test has been performed to estimate road <span class="hlt">profiles</span>. The road <span class="hlt">profile</span> resolution is approximately 5 to 10 cm in width and sensitivity is 0. 3 cm for the height road surface features at driving speeds of 5 to 80 mph.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://eric.ed.gov/?q=reactive+AND+program&pg=4&id=EJ927509','ERIC'); return false;" href="https://eric.ed.gov/?q=reactive+AND+program&pg=4&id=EJ927509"><span><span class="hlt">Profiles</span> of Anger Control in Second-Grade Children: Examination of Self-Report, <span class="hlt">Observational</span>, and Physiological Components</span></a></p> <p><a target="_blank" href="http://www.eric.ed.gov/ERICWebPortal/search/extended.jsp?_pageLabel=advanced">ERIC Educational Resources Information Center</a></p> <p>Smith, Marissa; Hubbard, Julie A.; Laurenceau, Jean-Philippe</p> <p>2011-01-01</p> <p>The current study used latent <span class="hlt">profile</span> analysis (LPA) to examine anger control in 257 second-grade children (approximately 8 years of age). Anger was induced through losing a game and prize to a confederate who cheated. Three components of anger control were assessed: self-report of awareness of anger, <span class="hlt">observed</span> intensity of angry facial…</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2015AGUFM.T13H..03K','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2015AGUFM.T13H..03K"><span>Simultaneous <span class="hlt">observations</span> of reaction kinetics, creep behavior, and AE activities during syndeformational antigorite dehydration at high <span class="hlt">pressures</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Kubo, T.; Iwasato, T.; Higo, Y.; Kato, T.; Kaneshima, S.; Uehara, S.; Koizumi, S.; Imamura, M.; Tange, Y.</p> <p>2015-12-01</p> <p>Intermediate-depth earthquakes are seismic activities in Wadati-Benioff zone at depths from 60 km to 300 km, where subducting plates deform plastically rather than brittle failure. Although it has been reported that unstable faulting occurred during antigorite dehydration even at higher <span class="hlt">pressures</span> than ~2 GPa (e.g., Jung et al., 2009), the recent study by Chernak and Hirth (2011) revealed that the syndefromational antigorite dehydration does not produces stick-slip instabilities but stable fault slip. In the present study, we newly developed an AE monitoring system for high-<span class="hlt">pressure</span> reaction-deformation processes combined with D-DIA and synchrotron monochromatic X-ray to <span class="hlt">observe</span> reaction kinetics, creep behaviors, and AE activities simultaneously. We applied this technique to investigate shear instability during syndeformational antigorite dehydration. High-<span class="hlt">pressure</span> deformation experiments were conducted up to ~8 GPa, ~1050 K, and strain rates of 3.4-9.2 x 10-5 s-1 in compression using a D-DIA type apparatus installed at BL-04B1, SPring-8. 50 keV mono X-ray were used to measure reaction kinetics and stress-strain data. To monitor shear instabilities by detecting AEs, six piezoelectric devices were positioned between first and second stage anvils of MA 6-6 type system. We used three kinds of starting materials of polycrystalline antigorite, fine-grained forsterite polycrystal, and two-phase mixtures of antigorite and San Carlos olivine (10%, 30%, and 50%atg). Clear contrasts were <span class="hlt">observed</span> in AE activities between forsterite and antigorite samples. AE activities detected within the forsterite polycrystal suggested (semi) brittle behaviors at low <span class="hlt">pressures</span> during the cold compression stage.
Almost no AEs were detected within the antigorite samples during any stages of cold compression, ramping, deformation, and syndeformational dehydration although localized deformation textures were <span class="hlt">observed</span> in recovered samples. Instead, we detected some AEs outside the sample</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2008ApPhL..93w1503L','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2008ApPhL..93w1503L"><span><span class="hlt">Observation</span> of collisionless heating of low energy electrons in low <span class="hlt">pressure</span> inductively coupled argon plasmas</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Lee, Min-Hyong; Lee, Hyo-Chang; Chung, Chin-Wook</p> <p>2008-12-01</p> <p>Collisionless heating of low energy electrons was <span class="hlt">observed</span> in low <span class="hlt">pressure</span> argon rf-biased inductively coupled plasmas (ICPs) by measurement of the electron energy distribution function (EEDF). When only capacitive power (bias) was supplied, the EEDF in the discharge was a bi-Maxwellian distribution with two electron groups. It was found that the low energy electrons were heated up significantly even with a little inductive power (<20 W) even when the discharge was in E mode. Due to the low gas <span class="hlt">pressure</span> and low temperature of low energy electrons (close to the energy of the Ramsauer minimum), the collisional heating of low energy electrons appears to be negligible. Therefore, this effective heating of the low energy electrons showed a direct experimental evidence of the collisionless heating by inductive field. The significant heating of low energy electrons in E mode indicates that collisionless heating in the skin layer is an important electron heating mechanism of low <span class="hlt">pressure</span> ICP even when the discharge is in E mode.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/19930091965','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/19930091965"><span>Knocking Combustion <span class="hlt">Observed</span> in a Spark-Ignition Engine with Simultaneous Direct and Schlieren High-Speed Motion Pictures and <span class="hlt">Pressure</span> Records</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Osterstrom, Gordon E</p> <p>1948-01-01</p> <p>Simultaneous direct and Schlieren photographs at 40,000 frames per second and correlated <span class="hlt">pressure</span> records were taken of knocking combustion in a special spark-ignition engine to ascertain the intensity of certain end-zone reactions previously noted from Schlieren photography alone. A violent propagated homogeneous autoignition, or a similar phenomenon, previously <span class="hlt">observed</span>, was again <span class="hlt">observed</span>. The <span class="hlt">pressure</span> records show autoignition of varying violence before the passage of a probable detonation wave. Extensive autoignition without occurrence of gas vibrations was seen in one explosion.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/20160014504','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/20160014504"><span>Jupiter's Deep Cloud Structure Revealed Using Keck <span class="hlt">Observations</span> of Spectrally Resolved Line Shapes</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Bjoraker, G. L.; Wong, M.H.; de Pater, I.; Adamkovics, M.</p> <p>2015-01-01</p> <p>Technique: We present a method to determine the <span class="hlt">pressure</span> at which significant cloud opacity is present between 2 and 6 bars on Jupiter. We use: a) the strength of a Fraunhofer absorption line in a zone to determine the ratio of reflected sunlight to thermal emission, and b) <span class="hlt">pressure</span>- broadened line <span class="hlt">profiles</span> of deuterated methane (CH3D) at 4.66 meters to determine the location of clouds. We use radiative transfer models to constrain the altitude region of both the solar and thermal components of Jupiter's 5-meter spectrum. Results: For nearly all latitudes on Jupiter the thermal component is large enough to constrain the deep cloud structure even when upper clouds are present. We find that Hot Spots, belts, and high latitudes have broader line <span class="hlt">profiles</span> than do zones. Radiative transfer models show that Hot Spots in the North and South Equatorial Belts (NEB, SEB) typically do not have opaque clouds at <span class="hlt">pressures</span> greater than 2 bars. The South Tropical Zone (STZ) at 32 degrees South has an opaque cloud top between 4 and 5 bars. From thermochemical models this must be a water cloud. We measured the variation of the equivalent width of CH3D with latitude for comparison with Jupiter's belt-zone structure. We also constrained the vertical <span class="hlt">profile</span> of H2O in an SEB Hot Spot and in the STZ. The Hot Spot is very dry for a probability less than 4.5 bars and then follows the H2O <span class="hlt">profile</span> <span class="hlt">observed</span> by the Galileo Probe. The STZ has a saturated H2O <span class="hlt">profile</span> above its cloud top between 4 and 5 bars.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2004MeScT..15.1185M','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2004MeScT..15.1185M"><span>Exhaust <span class="hlt">pressure</span> pulsation <span class="hlt">observation</span> from turbocharger instantaneous speed measurement</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Macián, V.; Luján, J. M.; Bermúdez, V.; Guardiola, C.</p> <p>2004-06-01</p> <p>In internal combustion engines, instantaneous exhaust <span class="hlt">pressure</span> measurements are difficult to perform in a production environment. The high temperature of the exhaust manifold and its pulsating character make its application to exhaust gas recirculation control algorithms impossible. In this paper an alternative method for estimating the exhaust <span class="hlt">pressure</span> pulsation is presented. A numerical model is built which enables the exhaust <span class="hlt">pressure</span> pulses to be predicted from instantaneous turbocharger speed measurements. Although the model is data based, a theoretical description of the process is also provided. This combined approach makes it possible to export the model for different engine operating points. Also, compressor contribution in the turbocharger speed pulsation is discussed extensively. The compressor contribution is initially neglected, and effects of this simplified approach are analysed.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=5301936','PMC'); return false;" href="https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=5301936"><span>Artificially decreased vapour <span class="hlt">pressure</span> deficit in field conditions modifies foliar metabolite <span class="hlt">profiles</span> in birch and aspen</span></a></p> <p><a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pmc">PubMed Central</a></p> <p>Lihavainen, Jenna; Keinänen, Markku; Keski-Saari, Sarita; Kontunen-Soppela, Sari; Sõber, Anu; Oksanen, Elina</p> <p>2016-01-01</p> <p>Relative air humidity (RH) is expected to increase in northern Europe due to climate change. Increasing RH reduces the difference of water vapour <span class="hlt">pressure</span> deficit (VPD) between the leaf and the atmosphere, and affects the gas exchange of plants. Little is known about the effects of decreased VPD on plant metabolism, especially under field conditions. This study was conducted to determine the effects of artificially decreased VPD on silver birch (Betula pendula Roth.) and hybrid aspen (Populus tremula L.×P. tremuloides Michx.) foliar metabolite and nutrient <span class="hlt">profiles</span> in a unique free air humidity manipulation (FAHM) field experiment during the fourth season of humidity manipulation, in 2011. Long-term exposure to decreased VPD modified nutrient homeostasis in tree leaves, as demonstrated by a lower N concentration and N:P ratio in aspen leaves, and higher Na concentration and lower K:Na ratio in the leaves of both species in decreased VPD than in ambient VPD. Decreased VPD caused a shift in foliar metabolite <span class="hlt">profiles</span> of both species, affecting primary and secondary metabolites. Metabolic adjustment to decreased VPD included elevated levels of starch and heptulose sugars, sorbitol, hemiterpenoid and phenolic glycosides, and α-tocopherol. High levels of carbon reserves, phenolic compounds, and antioxidants under decreased VPD may modify plant resistance to environmental stresses emerging under changing climate. PMID:27255929</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/19830007373','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/19830007373"><span>Circumferential <span class="hlt">pressure</span> distributions in a model labyrinth seal</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Leong, Y. M. M. S.; Brown, R. D.</p> <p>1982-01-01</p> <p>A research program to isolate and study leakage flow through labyrinth glands was initiated. Circumferential <span class="hlt">pressure</span> distributions were measured in the labyrinth glands with geometry appropriate to the high <span class="hlt">pressure</span> labyrinths in large steam turbines. Knowledge of this <span class="hlt">pressure</span> distribution is essential as it is this unequal <span class="hlt">pressure</span> field that results in the destabilizing force. Parameters that are likely to affect the <span class="hlt">pressure</span> distributions are incorporated into the test rig. Some preliminary <span class="hlt">pressure</span> <span class="hlt">profiles</span> are presented.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017AGUFM.A41O..06H','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017AGUFM.A41O..06H"><span>A new MesosphEO dataset of temperature <span class="hlt">profiles</span> from 35 to 85 km using Rayleigh scattering at limb from GOMOS/ENVISAT daytime <span class="hlt">observations</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Hauchecorne, A.; Blanot, L.; Wing, R., Jr.; Keckhut, P.; Khaykin, S. M.</p> <p>2017-12-01</p> <p>The scattering of sunlight by the Earth atmosphere above the top of the stratospheric layer, about 30-35 km altitude, is only due to Rayleigh scattering by atmospheric molecules. Its intensity is then directly proportional to the atmospheric density. It is then possible to retrieve a temperature <span class="hlt">profile</span> in absolute value using the hydrostatic equation and the perfect gas law, assuming that the temperature is known from a climatological model at the top of the density <span class="hlt">profile</span>. This technique is applied to Rayleigh lidar <span class="hlt">observations</span> since more than 35 years (Hauchecorne and Chanin, 1980). The GOMOS star occultation spectrometer <span class="hlt">observed</span> the sunlight scattering at limb during daytime to remove it from the star spectrum. In the frame of the ESA funded MesosphEO project, GOMOS Rayleigh scattering <span class="hlt">profiles</span> in the spectral range 400-460 nm have been used to retrieve temperature <span class="hlt">profiles</span> from 35 to 85 km with a 2-km vertical resolution. A dataset of more than 310 thousands <span class="hlt">profiles</span> from 2002 to 2012 is available for climatology and atmospheric dynamics studies. The validation of this dataset using NDACC Rayleigh lidars and MLS-AURA and SABER-TIMED will be presented. Preliminary results on the variability of the upper stratosphere and the mesosphere will be shown. We propose to apply this technique in the future to ALTIUS <span class="hlt">observations</span>. The Rayleigh scattering technique can be applied to any sounder <span class="hlt">observing</span> the day-time limb on the near-UV and visible spectrum.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://ntrs.nasa.gov/search.jsp?R=19870038666&hterms=water+filters&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D80%26Ntt%3Dwater%2Bfilters','NASA-TRS'); return false;" href="https://ntrs.nasa.gov/search.jsp?R=19870038666&hterms=water+filters&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D80%26Ntt%3Dwater%2Bfilters"><span>Remote sensing of the atmosphere of Mars using infrared <span class="hlt">pressure</span> modulation and filter radiometry</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Mccleese, D. J.; Schofield, J. T.; Zurek, R. W.; Martonchik, J. V.; Haskins, R. D.</p> <p>1986-01-01</p> <p>The study of the atmosphere and climate of Mars will soon be advanced considerably by the Mars <span class="hlt">Observer</span> mission. This paper describes the atmospheric sounder for this mission and how it will measure key Martian atmospheric parameters using IR gas correlation and filter radiometry. The instrument now under development will provide high-resolution vertical <span class="hlt">profiles</span> of atmospheric temperature, <span class="hlt">pressure</span>, water vapor, dust, and clouds using limb sounding techniques as well as nadir <span class="hlt">observations</span> of surface thermal properties and polar radiative balance.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/28226363','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/28226363"><span>Coagulation <span class="hlt">Profile</span> in Patients with Different Etiologies for Cushing Syndrome: A Prospective <span class="hlt">Observational</span> Study.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Tirosh, Amit; Lodish, Maya; Lyssikatos, Charalampos; Belyavskaya, Elena; Feelders, Richard A; Stratakis, Constantine A</p> <p>2017-05-01</p> <p>Previous studies reported a higher prevalence of venous-thromboembolic events among patients with Cushing disease (CD) compared to those with ACTH-independent Cushing syndrome (CS) from adrenal sources. The objective of the current study was to evaluate the coagulation <span class="hlt">profile</span> of patients with CS from different etiologies. A prospective <span class="hlt">observational</span> study was conducted at a clinical research center. The study included adult patients admitted for evaluation of suspected CS (n=85), that were divided into 3 groups: CD (n=22), ACTH-independent CS from an adrenal tumor/hyperplasia (adrenal CS, n=21), and a control group consisting of subjects with negative screening for CS (rule-out CS, n=42). Coagulation <span class="hlt">profiles</span> were drawn before and 8.5±4.3 months after surgery (trans-sphenoidal or adrenalectomy, n=18), and included fibrinogen, Factor VIII (FVIII), von Willebrand factor antigen (vWF:Ag), plasminogen activator inhibitor-1 (PAI-1), antithrombin III (ATIII), Protein C (PC), Protein S (PS), α2-antiplasmin (α2AP), and aPTT measurements. Patients with CD had higher baseline mean cortisol levels, ATIII activity and vWF:Ag levels compared with adrenal CS. Differences in ATIII activity and vWF:Ag levels remained even after controlling for BMI, and ATIII after also controlling for 24-h urinary free cortisol collections. Our study showed for the first time the differences in coagulation <span class="hlt">profiles</span> between various etiologies of CS. We assume that the higher cortisol burden among CD patients may explain the differences found in the coagulation <span class="hlt">profile</span> as well as the higher risk for VTE compared with primary adrenal CS patients. © Georg Thieme Verlag KG Stuttgart · New York.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://pubs.er.usgs.gov/publication/70022294','USGSPUBS'); return false;" href="https://pubs.er.usgs.gov/publication/70022294"><span>A crustal model of the ultrahigh-<span class="hlt">pressure</span> Dabie Shan orogenic belt, China, derived from deep seismic refraction <span class="hlt">profiling</span></span></a></p> <p><a target="_blank" href="http://pubs.er.usgs.gov/pubs/index.jsp?view=adv">USGS Publications Warehouse</a></p> <p>Wang, Chun-Yong; Zeng, Rong-Sheng; Mooney, W.D.; Hacker, B.R.</p> <p>2000-01-01</p> <p>We present a new crustal cross section through the east-west trending ultrahigh-<span class="hlt">pressure</span> (UHP) Dabie Shan orogenic belt, east central China, based on a 400-km-long seismic refraction <span class="hlt">profile</span>. Data from our <span class="hlt">profile</span> reveal that the cratonal blocks north and south of the orogen are composed of 35-km-thick crust consisting of three layers (upper, middle, and lower crust) with average seismic velocities of 6.0±0.2 km/s, 6.5±0.1 km/s, and 6.8±0.1 km/s. The crust reaches a maximum thickness of 41.5 km beneath the northern margin of the orogen, and thus the present-day root beneath the orogen is only 6.5 km thick. The upper mantle velocity is 8.0±0.1 km/s. Modeling of shear wave data indicate that Poisson's ratio increases from 0.24±0.02 in the upper crust to 0.27±0.03 in the lower crust. This result is consistent with a dominantly felsic upper crustal composition and a mafic lower crustal composition within the amphibolite or granulite metamorphic facies. Our seismic model indicates that eclogite, which is abundant in surface exposures within the orogen, is not a volumetrically significant component in the middle or lower crust. Much of the Triassic structure associated with the formation of the UHP rocks of the Dabie Shan has been obscured by post-Triassic igneous activity, extension and large-offset strike-slip faulting. Nevertheless, we can identify a high-velocity (6.3 km/s) zone in the upper (<5 km depth) crustal core of the orogen which we interpret as a zone of ultrahigh-<span class="hlt">pressure</span> rocks, a north dipping suture, and an apparent Moho offset that marks a likely active strike-slip fault.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/27703288','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/27703288"><span>Blood <span class="hlt">Pressure</span> Control in Hypertensive Patients, Cardiovascular Risk <span class="hlt">Profile</span> and the Prevalence of Masked Uncontrolled Hypertension (MUCH).</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Naser, Nabil; Dzubur, Alen; Durak, Azra; Kulic, Mehmed; Naser, Nura</p> <p>2016-07-27</p> <p>The term masked hypertension (MH) should be used for untreated individuals who have normal office blood <span class="hlt">pressure</span> but elevated ambulatory blood <span class="hlt">pressure</span>. For treated patients, this condition should be termed masked uncontrolled hypertension (MUCH). Masked uncontrolled hypertension (MUCH) has gone unrecognized because few studies have used 24-h ABPM to determine the prevalence of suboptimal BP control in seemingly well-treated patients, and there are few such studies in large cohorts of treated patients attending usual clinical practice. This is important because masked hypertension is associated with a high risk of cardiovascular events. This study was conducted to obtain more information about the association between hypertension and other CV risk factors, about office and ambulatory blood <span class="hlt">pressure</span> (BP) control as well as on cardiovascular (CV) risk <span class="hlt">profile</span> in treated hypertensive patients, also to define the prevalence and characteristics of masked uncontrolled hypertension (MUCH) among treated hypertensive patients in routine clinical practice. In this study 2514 male and female patients were included during a period of 5 years follow up. All patients have ambulatory blood <span class="hlt">pressure</span> monitoring (ABPM) for at least 24h. We identified patients with treated and controlled BP according to current international guidelines (clinic BP, 140/90mmHg). Cardiovascular risk assessment was based on personal history, clinic BP values, as well as target organ damage evaluation. Masked uncontrolled hypertension (MUCH) was diagnosed in these patients if despite controlled clinic BP, the mean 24-h ABPM average remained elevated (24-h systolic BP ≥130mmHg and/or 24-h diastolic BP ≥80mmHg). Patients had a mean age of 60.2+10 years, and the majority of them (94.6%) were followed by specialist physicians. Average clinic BP was 150.4+16/89.9+12 mmHg. About 70% of patients displayed a very high-risk <span class="hlt">profile</span>. Ambulatory blood <span class="hlt">pressure</span> monitoring (ABPM) was performed in all recruited</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://ntrs.nasa.gov/search.jsp?R=19880051860&hterms=vertical+height&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D90%26Ntt%3Dvertical%2Bheight','NASA-TRS'); return false;" href="https://ntrs.nasa.gov/search.jsp?R=19880051860&hterms=vertical+height&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D90%26Ntt%3Dvertical%2Bheight"><span>Satellite remote sensing and ozonesonde <span class="hlt">observation</span> of ozone vertical <span class="hlt">profile</span> and severe storm development</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Hung, R. J.; Liu, J. M.</p> <p>1988-01-01</p> <p>Two year ozonesonde data, January 1981 to December 1982, <span class="hlt">observed</span> at four Canadian stations, and two-and-a-half year backscattered ultraviolet experiment data on the Nimbus-4 satellite, April 1970 to August 1972, <span class="hlt">observed</span> over five U.S. stations, were used to study the relationship between the total ozone, vertical distribution of the ozone mixing ratio, height of half the total ozone, and the variation of local tropopause height. In view of the correlation between the variation of the tropopause height and the possible development of severe storms, a better understanding of the effect of the vertical distribution of the local ozone <span class="hlt">profile</span> on the variation of the tropopause height can give considerable insight into the development of severe storms.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2007AGUFM.V51E0830M','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2007AGUFM.V51E0830M"><span><span class="hlt">Pressure</span>-dependent boron isotopic fractionation <span class="hlt">observed</span> by column chromatography</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Musashi, M.; Oi, T.; Matsuo, M.; Nomura, M.</p> <p>2007-12-01</p> <p>Boron isotopic fractionation factor ( S ) between boron taken up in strongly basic anion exchange resin and boron in aqueous solution was determined by breakthrough column chromatography at 5 and 17 MPa at 25°C, using 0.1 mmol/L boric acid solution as feed solution. The S values obtained were 1.018 and 1.012, respectively, which were smaller than the value reported by using the same chromatographic method at atmospheric <span class="hlt">pressure</span> at 25°C with the boron concentration of 10 mmol/L, but were larger than the values at the same condition with much higher concentration of 100 and 501 mmol/L, indicating that borate-polymerization reducing the isotopic fractionation was negligible. However, calculations based on the theory of isotope distribution between two phases estimated that 21% (5MPa) and 47% (17MPa) of boron taken up in the resin phase was in the three-coordinated B(OH)3-form, instead of in the four-coordinated B(OH)4--form, at high <span class="hlt">pressures</span> even with the very diluted solution. We discussed this discrepancy by introducing (1) hydration or (2) a partial molar volume difference between isotopic molecules. It was inferred that borate ions were partially dehydrated upon transfer from the solution phase to the resin phase at high <span class="hlt">pressures</span>, which resulted in smaller S values compared with those at the atmospheric <span class="hlt">pressure</span>. Alternatively, it was likely that the S value decreased with increasing <span class="hlt">pressure</span>, because the difference of the partial isotopic molar volumes between 10B(OH)3 and 11B(OH)3 was larger than that between 10B(OH)4- and 11B(OH)4-. If either will be the case, the influence of a <span class="hlt">pressure</span> upon the isotope effect may not be negligible for boron isotopic exchange equilibrium. This knowledge is crucial for the principle of the boron isotopic pH-metry reconstructing a chemical variation at the paleo-deep oceanic environment where the early life may have been evolved.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2009AGUFM.A31F0187S','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2009AGUFM.A31F0187S"><span><span class="hlt">Observing</span> the Great Plains Low-Level Jet Using the Aircraft Communications Addressing and Reporting System (ACARS): A Comparison with Boundary Layer <span class="hlt">Profiler</span> <span class="hlt">Observations</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Skinner, P. S.; Basu, S.</p> <p>2009-12-01</p> <p>Wind resources derived from the nocturnal low-level jet of the Great Plains of the United States are a driving factor in the proliferation of wind energy facilities across the region. Accurate diagnosis and forecasting of the low-level jet is important to not only assess the wind resource but to estimate the potential for shear-induced stress generation on turbine rotors. This study will examine the utility of Aircraft Communications Addressing and Reporting System (ACARS) <span class="hlt">observations</span> in diagnosing low-level jet events across the Texas Panhandle. ACARS <span class="hlt">observations</span> from Lubbock International Airport (KLBB) will be compared to <span class="hlt">observations</span> from a 915 MHZ Doppler radar vertical boundary-layer <span class="hlt">profiler</span> with 60m vertical resolution located at the field experiment site of Texas Tech University. The ability of ACARS data to adequately <span class="hlt">observe</span> low-level jet events during the spring and summer of 2009 will be assessed and presented.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2013AGUFM.P41C1937K','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2013AGUFM.P41C1937K"><span>Temperature and dust <span class="hlt">profiles</span> in Martian dust storm conditions retrieved from Mars Climate Sounder measurements</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Kleinboehl, A.; Kass, D. M.; Schofield, J. T.; McCleese, D. J.</p> <p>2013-12-01</p> <p>Mars Climate Sounder (MCS) is a mid- and far-infrared thermal emission radiometer on board the Mars Reconnaissance Orbiter. It measures radiances in limb and nadir/on-planet geometry from which vertical <span class="hlt">profiles</span> of atmospheric temperature, water vapor, dust and condensates can be retrieved in an altitude range from 0 to 80 km and with a vertical resolution of ~5 km. Due to the limb geometry used as the MCS primary <span class="hlt">observation</span> mode, retrievals in conditions with high aerosol loading are challenging. We have developed several modifications to the MCS retrieval algorithm that will facilitate <span class="hlt">profile</span> retrievals in high-dust conditions. Key modifications include a retrieval option that uses a surface <span class="hlt">pressure</span> climatology if a <span class="hlt">pressure</span> retrieval is not possible in high dust conditions, an extension of aerosol retrievals to higher altitudes, and a correction to the surface temperature climatology. In conditions of a global dust storm, surface temperatures tend to be lower compared to standard conditions. Taking this into account using an adaptive value based on atmospheric opacity leads to improved fits to the radiances measured by MCS and improves the retrieval success rate. We present first results of these improved retrievals during the global dust storm in 2007. Based on the limb opacities <span class="hlt">observed</span> during the storm, retrievals are typically possible above ~30 km altitude. Temperatures around 240 K are <span class="hlt">observed</span> in the middle atmosphere at mid- and high southern latitudes after the onset of the storm. Dust appears to be nearly homogeneously mixed at lower altitudes. Significant dust opacities are detected at least up to 70 km altitude. During much of the storm, in particular at higher altitudes, the retrieved dust <span class="hlt">profiles</span> closely resemble a Conrath-<span class="hlt">profile</span>.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.mayoclinic.org/diseases-conditions/high-blood-pressure/expert-answers/blood-pressure/FAQ-20058115?p=1','NIH-MEDLINEPLUS'); return false;" href="https://www.mayoclinic.org/diseases-conditions/high-blood-pressure/expert-answers/blood-pressure/FAQ-20058115?p=1"><span>Blood <span class="hlt">Pressure</span>: Does It Have a Daily Pattern?</span></a></p> <p><a target="_blank" href="http://medlineplus.gov/">MedlinePlus</a></p> <p></p> <p></p> <p>... better associated with the cardiovascular risk <span class="hlt">profile</span>? American Journal of Hypertension. 2014;27:680. Birkenhager AM, et al. Causes and consequences of a non-dipping blood <span class="hlt">pressure</span> <span class="hlt">profile</span>. Netherlands Journal of Medicine. 2007;65:127. Feb. 24, 2018 ...</p> </li> </ol> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_14");'>14</a></li> <li><a href="#" onclick='return showDiv("page_15");'>15</a></li> <li class="active"><span>16</span></li> <li><a href="#" onclick='return showDiv("page_17");'>17</a></li> <li><a href="#" onclick='return showDiv("page_18");'>18</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div><!-- col-sm-12 --> </div><!-- row --> </div><!-- page_16 --> <div id="page_17" class="hiddenDiv"> <div class="row"> <div class="col-sm-12"> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_15");'>15</a></li> <li><a href="#" onclick='return showDiv("page_16");'>16</a></li> <li class="active"><span>17</span></li> <li><a href="#" onclick='return showDiv("page_18");'>18</a></li> <li><a href="#" onclick='return showDiv("page_19");'>19</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div> </div> <div class="row"> <div class="col-sm-12"> <ol class="result-class" start="321"> <li> <p><a target="_blank" onclick="trackOutboundLink('https://ntrs.nasa.gov/search.jsp?R=20080047975&hterms=solute&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D60%26Ntt%3Dsolute','NASA-TRS'); return false;" href="https://ntrs.nasa.gov/search.jsp?R=20080047975&hterms=solute&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D60%26Ntt%3Dsolute"><span>Effect of Stepwise <span class="hlt">Pressure</span> Change on Porosity Evolution during Directional Solidification in Small Cylindrical Channels</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Grugel, R.N.; Lee, C.P.; Cox, M.C.; Blandford, B.T.; Anilkumar, A.V.</p> <p>2008-01-01</p> <p>Controlled directional solidification experiments were performed in capillary channels, using nitrogen-saturated succinonitrile, to examine the effect of an in-situ stepwise processing <span class="hlt">pressure</span> increase on an isolated pore evolution. Two experiments were performed using different processing <span class="hlt">pressure</span> input <span class="hlt">profiles</span>. The results indicate that a processing <span class="hlt">pressure</span> increase has a transient effect on pore growth geometry characterized by an initial phase of decreasing pore diameter, followed by a recovery phase of increasing pore diameter. The experimental results also show that processing <span class="hlt">pressure</span> can be used as a control parameter to either increase or terminate porosity formation. A theoretical model is introduced which indicates that the pore formation process is limited by the diffusion of solute-gas through the melt, and that the <span class="hlt">observed</span> response toa <span class="hlt">pressure</span> increase is attributed to the re-equilibration of solute concentration in the melt associated with the increased melt <span class="hlt">pressure</span>.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017AGUFMSM21A2557K','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017AGUFMSM21A2557K"><span>Energy and mass dependence of the contribution to storm-time plasma <span class="hlt">pressure</span> <span class="hlt">observed</span> by Arase/MEP-i</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Kasahara, S.; Keika, K.; Yokota, S.; Hoshino, M.; Seki, K.; Nose, M.; Amano, T.; Yoshizumi, M.; Shinohara, I.</p> <p>2017-12-01</p> <p>The ring current is mainly controlled by the ion <span class="hlt">pressure</span> and its spatial gradient. The ion <span class="hlt">pressure</span> is dominated by ions with energies of a few to a few 100s keV. Oxygen ions of ionospheric origin can be energized in the plasma sheet and/or the inner magnetosphere up to a few tens to a few hundreds of keV. The ionospheric oxygen ions make a significant contribution to the ion <span class="hlt">pressure</span> during geomagnetically active periods. This paper examines spatial variations and energy-spectral evolution of energetic ( 10 to 200 keV/q) ions during the main phase of a CIR-driven storm on 17 March 2017 (Storm 1) and a CME-driven storm on 27-28 May 2017 (Storm 2). We use ion data from the MEP-i instrument on board the Arase satellite. The instrument measured energetic ions with energies of 5-120 keV/q during Storm 1 and 9-180 keV/q during Storm 2; ion mass/charge was derived from energy and velocity measurements by an electrostatic analyzer and the time-of-flight system, respectively. Below is a brief summary of the MEP-i <span class="hlt">observations</span> during the two storms. During Storm 1, MEP-i saw high fluxes of >10 keV/q protons and oxygen ions (and possibly other minor ions) at Lm 3.5 around midnight. MEP-i continued to <span class="hlt">observe</span> high-flux ions until the end of the main phase. Both proton and oxygen ion <span class="hlt">pressures</span> increased; the O-to-H ratio increased by about an order of magnitude, from 0.02 to 0.2-0.3. The high-flux >10 keV/q ions consisted of clearly different two populations: one dominated by 5-20 keV/q ions, likely originating from pre-existing cold plasma sheet population; and the other with structured dispersion signatures at 30-90 keV/q, likely due to the penetration of ions accelerated in the near-Earth plasma sheet. We found that both populations contributed to the total <span class="hlt">pressure</span> almost equally. During Storm 2, MEP-i <span class="hlt">observed</span> proton and oxygen high fluxes in a wide energy range (10-120 keV/q). The <span class="hlt">pressure</span> increased for both protons and oxygen ions; the O-to-H ratio increased from 0</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://pubs.er.usgs.gov/publication/70024035','USGSPUBS'); return false;" href="https://pubs.er.usgs.gov/publication/70024035"><span>Experimental <span class="hlt">observations</span> of <span class="hlt">pressure</span> oscillations and flow regimes in an analogue volcanic system</span></a></p> <p><a target="_blank" href="http://pubs.er.usgs.gov/pubs/index.jsp?view=adv">USGS Publications Warehouse</a></p> <p>Lane, S.J.; Chouet, B.A.; Phillips, J.C.; Dawson, P.; Ryan, G.A.; Hurst, E.</p> <p>2001-01-01</p> <p>Gas-liquid flows, designed to be analogous to those in volcanic conduits, are generated in the laboratory using organic gas-gum rosin mixtures expanding in a vertically mounted tube. The expanding fluid shows a range of both flow and <span class="hlt">pressure</span> oscillation behaviors. Weakly supersaturated source liquids produce a low Reynolds number flow with foam expanding from the top surface of a liquid that exhibits zero fluid velocity at the tube wall; i.e., the conventional "no-slip" boundary condition. <span class="hlt">Pressure</span> oscillations, often with strong long-period characteristics and consistent with longitudinal and radial resonant oscillation modes, are detected in these fluids. Strongly supersaturated source liquids generate more energetic flows that display a number of flow regimes. These regimes include a static liquid source, viscous flow, detached flow (comprising gas-pockets-at-wall and foam-in-gas annular flow, therefore demonstrating strong radial heterogeneity), and a fully turbulent transonic fragmented or mist flow. Each of these flow regimes displays characteristic <span class="hlt">pressure</span> oscillations that can be related to resonance of flow features or wall impact phenomena. The <span class="hlt">pressure</span> oscillations are produced by the degassing processes without the need of elastic coupling to the confining medium or flow restrictors and valvelike features. The oscillatory behavior of the experimental flows is compared to seismoacoustic data from a range of volcanoes where resonant oscillation of the fluid within the conduit is also often invoked as controlling the <span class="hlt">observed</span> oscillation frequencies. On the basis of the experimental data we postulate on the nature of seismic signals that may be measured during large-scale explosive activity. Copyright 2001 by the American Geophysical Union.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://ntrs.nasa.gov/search.jsp?R=20090028685&hterms=Wrf&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D50%26Ntt%3DWrf','NASA-TRS'); return false;" href="https://ntrs.nasa.gov/search.jsp?R=20090028685&hterms=Wrf&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D50%26Ntt%3DWrf"><span>Improving Regional Forecast by Assimilating Atmospheric InfraRed Sounder (AIRS) <span class="hlt">Profiles</span> into WRF Model</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Chou, Shih-Hung; Zavodsky, Brad; Jedlovec, Gary J.</p> <p>2009-01-01</p> <p>In data sparse regions, remotely-sensed <span class="hlt">observations</span> can be used to improve analyses and produce improved forecasts. One such source comes from the Atmospheric InfraRed Sounder (AIRS), which together with the Advanced Microwave Sounding Unit (AMSU), represents one of the most advanced space-based atmospheric sounding systems. The purpose of this paper is to describe a procedure to optimally assimilate high resolution AIRS <span class="hlt">profile</span> data into a regional configuration of the Advanced Research WRF (ARW) version 2.2 using WRF-Var. The paper focuses on development of background error covariances for the regional domain and background type, and an optimal methodology for ingesting AIRS temperature and moisture <span class="hlt">profiles</span> as separate overland and overwater retrievals with different error characteristics. The AIRS thermodynamic <span class="hlt">profiles</span> are derived from the version 5.0 Earth <span class="hlt">Observing</span> System (EOS) science team retrieval algorithm and contain information about the quality of each temperature layer. The quality indicators were used to select the highest quality temperature and moisture data for each <span class="hlt">profile</span> location and <span class="hlt">pressure</span> level. The analyses were then used to conduct a month-long series of regional forecasts over the continental U.S. The long-term impacts of AIRS <span class="hlt">profiles</span> on forecast were assessed against verifying NAM analyses and stage IV precipitation data.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2015IAUGA..2258213C','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2015IAUGA..2258213C"><span>Jellyfish: <span class="hlt">Observational</span> Properties of Extreme Ram-<span class="hlt">Pressure</span> Stripping Events in Massive Galaxy Clusters</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Conor, McPartland; Ebeling, Harald; Roediger, Elke</p> <p>2015-08-01</p> <p>We investigate the physical origin and <span class="hlt">observational</span> signatures of extreme ram-<span class="hlt">pressure</span> stripping (RPS) in 63 massive galaxy clusters at z=0.3-0.7, based on data in the F606W passband obtained with the Advanced Camera for Surveys aboard the Hubble Space Telescope. Using a training set of a dozen ``jellyfish" galaxies identified earlier in the same imaging data, we define quantitative morphological criteria to select candidate galaxies which are similar to known cases of RPS. Considering a sample of 16 ``jellyfish" galaxies (10 of which we present for the first time), we visually derive estimates of the projected direction of motion based on dynamical features such as apparent compression shocks and debris trails. Our findings suggest that the <span class="hlt">observed</span> events occur primarily at large distances from the cluster core and involve infall trajectories featuring high impact parameters. Simple models of cluster growth show that such trajectories are consistent with two scenarios: 1) galaxy infall along filaments; and 2) infall at high velocities (≥1000 km/s) characteristic of cluster mergers. The <span class="hlt">observed</span> distribution of events is best described by timescales of ˜few Myr in agreement with recent numerical simulations of RPS. The broader areal coverage of the Hubble Frontier Fields should provide an even larger sample of RPS events to determine the relative contributions of infall and cluster mergers. Prompted by the discovery of several jellyfish galaxies whose brightness in the F606W passband rivals or exceeds that of the respective brightest cluster galaxy, we attempt to constrain the luminosity function of galaxies undergoing RPS. The <span class="hlt">observed</span> significant excess at the bright end compared to the luminosity functions of blue cluster members strongly suggests enhanced star formation, thus challenging theoretical and numerical studies according to which RPS merely displaces existing star-forming regions. In-depth studies of individual objects will help test our</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://ntrs.nasa.gov/search.jsp?R=19950058595&hterms=atmospheric+pressure&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D50%26Ntt%3Datmospheric%2Bpressure','NASA-TRS'); return false;" href="https://ntrs.nasa.gov/search.jsp?R=19950058595&hterms=atmospheric+pressure&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D50%26Ntt%3Datmospheric%2Bpressure"><span>Atmospheric <span class="hlt">pressure</span> loading parameters from very long baseline interferometry <span class="hlt">observations</span></span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Macmillan, D. S.; Gipson, John M.</p> <p>1994-01-01</p> <p>Atmospheric mass loading produces a primarily vertical displacement of the Earth's crust. This displacement is correlated with surface <span class="hlt">pressure</span> and is large enough to be detected by very long baseline interferometry (VLBI) measurements. Using the measured surface <span class="hlt">pressure</span> at VLBI stations, we have estimated the atmospheric loading term for each station location directly from VLBI data acquired from 1979 to 1992. Our estimates of the vertical sensitivity to change in <span class="hlt">pressure</span> range from 0 to -0.6 mm/mbar depending on the station. These estimates agree with inverted barometer model calculations (Manabe et al., 1991; vanDam and Herring, 1994) of the vertical displacement sensitivity computed by convolving actual <span class="hlt">pressure</span> distributions with loading Green's functions. The <span class="hlt">pressure</span> sensitivity tends to be smaller for stations near the coast, which is consistent with the inverted barometer hypothesis. Applying this estimated <span class="hlt">pressure</span> loading correction in standard VLBI geodetic analysis improves the repeatability of estimated lengths of 25 out of 37 baselines that were measured at least 50 times. In a root-sum-square (rss) sense, the improvement generally increases with baseline length at a rate of about 0.3 to 0.6 ppb depending on whether the baseline stations are close to the coast. For the 5998-km baseline from Westford, Massachusetts, to Wettzell, Germany, the rss improvement is about 3.6 mm out of 11.0 mm. The average rss reduction of the vertical scatter for inland stations ranges from 2.7 to 5.4 mm.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2009SPIE.7463E..09E','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2009SPIE.7463E..09E"><span>Preliminary VHF radar and high-data-rate optical turbulence <span class="hlt">profile</span> <span class="hlt">observations</span> using a balloon-ring platform</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Eaton, Frank D.; Nastrom, Gregory D.; Kyrazis, Demos T.; Black, Don G.; Black, Wiley T.; Black, R. Alastair</p> <p>2009-08-01</p> <p>A recent measurement campaign at Vandenberg Air Force Base, Calif. involved taking simultaneous <span class="hlt">observations</span> with a VHF radar and high-data-rate (1-micron diameter) platinum wires to sense optical turbulence (from temperature fluctuations). The radar <span class="hlt">observations</span> produce <span class="hlt">profiles</span> of the refractive index structure parameter (C2n ), the turbulent kinetic energy (σ2t ), the eddy dissipation rate (ɛ), the inner scale (lo ), the outer scale (Lo ) of turbulence, and wind speed and direction to an altitude of 20 km AGL. The fine wire measurements were taken from the surface with several sensors mounted on a balloon-ring platform sampling in excess of 3 kHz to balloon burst altitudes (typically above 25 km AGL). The main objectives of this effort are to compare the two measurement techniques and to obtain <span class="hlt">observations</span> that can address several fundamental turbulence issues of the real turbulent atmosphere related to laser beam propagation. To date, modeling and simulation of laser beam propagation through atmospheric turbulence have relied upon a traditional theoretical basis that assumes the existence of homogeneous, isotropic, stationary, and Kolmogorov turbulence. Results presented from the radar <span class="hlt">observations</span> include C2n, σ2t, ɛ, lo, and the standard deviation of vertical velocity (σw). A comparison of the <span class="hlt">profiles</span> of C2n obtained from the two measurement techniques is shown and discussed. A time series of temperature data obtained from a fine wire probe traversing one radar range gate is presented and discussed. Future measurement and analysis efforts are presented.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/23790639','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/23790639"><span><span class="hlt">Pressure</span> garment design tool to monitor exerted <span class="hlt">pressures</span>.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Macintyre, Lisa; Ferguson, Rhona</p> <p>2013-09-01</p> <p><span class="hlt">Pressure</span> garments are used in the treatment of hypertrophic scarring following serious burns. The use of <span class="hlt">pressure</span> garments is believed to hasten the maturation process, reduce pruritus associated with immature hypertrophic scars and prevent the formation of contractures over flexor joints. <span class="hlt">Pressure</span> garments are normally made to measure for individual patients from elastic fabrics and are worn continuously for up to 2 years or until scar maturation. There are 2 methods of constructing <span class="hlt">pressure</span> garments. The most common method, called the Reduction Factor method, involves reducing the patient's circumferential measurements by a certain percentage. The second method uses the Laplace Law to calculate the dimensions of <span class="hlt">pressure</span> garments based on the circumferential measurements of the patient and the tension <span class="hlt">profile</span> of the fabric. The Laplace Law method is complicated to utilise manually and no design tool is currently available to aid this process. This paper presents the development and suggested use of 2 new <span class="hlt">pressure</span> garment design tools that will aid <span class="hlt">pressure</span> garment design using the Reduction Factor and Laplace Law methods. Both tools calculate the <span class="hlt">pressure</span> garment dimensions and the mean <span class="hlt">pressure</span> that will be exerted around the body at each measurement point. Monitoring the <span class="hlt">pressures</span> exerted by <span class="hlt">pressure</span> garments and noting the clinical outcome would enable clinicians to build an understanding of the implications of particular <span class="hlt">pressures</span> on scar outcome, maturation times and patient compliance rates. Once the optimum <span class="hlt">pressure</span> for particular treatments is known, the Laplace Law method described in this paper can be used to deliver those average <span class="hlt">pressures</span> to all patients. This paper also presents the results of a small scale audit of measurements taken for the fabrication of <span class="hlt">pressure</span> garments in two UK hospitals. This audit highlights the wide range of <span class="hlt">pressures</span> that are exerted using the Reduction Factor method and that manual pattern 'smoothing' can dramatically</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/19990008518','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/19990008518"><span>Experimental Study of Boundary Layer Behavior in a Simulated Low <span class="hlt">Pressure</span> Turbine. Degree awarded by the University of Toledo, May 1998</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Shyne, Rickey J.</p> <p>1998-01-01</p> <p>A detailed investigation of the flow physics occurring on the suction side of a simulated Low <span class="hlt">Pressure</span> Turbine (LPT) blade was performed. A contoured upper wall was designed to simulate the <span class="hlt">pressure</span> distribution of an actual LPT blade onto a flat plate. The experiments were carried out at Reynolds numbers of 100,000 and 250,000 with three levels of freestream turbulence. Freestream turbulence levels ranging from 0.8% to 3% was used in this experiment. Smoke-wire flow visualization data was used to confirm that the boundary layer was separated and formed a bubble. Hot-wires (single and x-wire) and surface mounted hot-film gases and static <span class="hlt">pressure</span> taps were used to map the flowfield. The transition process over the separated flow region is <span class="hlt">observed</span> to be similar to a laminar free shear layer flow with the formation of a large coherent eddy structure. For each condition, the locations defining the separation bubble were determined by careful examination of <span class="hlt">pressure</span> and mean velocity <span class="hlt">profile</span> data. Transition onset location and length determined from intermittency <span class="hlt">profiles</span> decrease as freestream turbulence levels increase. Additionally, the length and height of the laminar separation bubbles were <span class="hlt">observed</span> to be inversely proportional to the levels of freestream turbulence.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=3985862','PMC'); return false;" href="https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=3985862"><span><span class="hlt">Observation</span> of Complete <span class="hlt">Pressure</span>-Jump Protein Refolding in Molecular Dynamics Simulation and Experiment</span></a></p> <p><a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pmc">PubMed Central</a></p> <p></p> <p>2015-01-01</p> <p>Density is an easily adjusted variable in molecular dynamics (MD) simulations. Thus, <span class="hlt">pressure</span>-jump (P-jump)-induced protein refolding, if it could be made fast enough, would be ideally suited for comparison with MD. Although <span class="hlt">pressure</span> denaturation perturbs secondary structure less than temperature denaturation, protein refolding after a fast P-jump is not necessarily faster than that after a temperature jump. Recent P-jump refolding experiments on the helix bundle λ-repressor have shown evidence of a <3 μs burst phase, but also of a ∼1.5 ms “slow” phase of refolding, attributed to non-native helical structure frustrating microsecond refolding. Here we show that a λ-repressor mutant is nonetheless capable of refolding in a single explicit solvent MD trajectory in about 19 μs, indicating that the burst phase <span class="hlt">observed</span> in experiments on the same mutant could produce native protein. The simulation reveals that after about 18.5 μs of conformational sampling, the productive structural rearrangement to the native state does not occur in a single swift step but is spread out over a brief series of helix and loop rearrangements that take about 0.9 μs. Our results support the molecular time scale inferred for λ-repressor from near-downhill folding experiments, where transition-state population can be seen experimentally, and also agrees with the transition-state transit time <span class="hlt">observed</span> in slower folding proteins by single-molecule spectroscopy. PMID:24437525</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/10159859','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/10159859"><span>Evaluation of an active seating system for <span class="hlt">pressure</span> relief.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Koo, T K; Mak, A F; Lee, Y L</p> <p>1995-01-01</p> <p>In the first part of this study, the inflation-<span class="hlt">pressure</span> and interface-<span class="hlt">pressure</span> <span class="hlt">profiles</span> of an active cushion system, the Talley active air bellows cushion, were examined continuously for one complete working cycle using the dynamic <span class="hlt">pressure</span> monitor. The relationship between the inflation <span class="hlt">pressure</span> and the interface <span class="hlt">pressure</span> was explored. A well-defined relationship was found in the areas directly over the air bellows. In the second part of this study, the <span class="hlt">pressure</span>-relieving characteristics of the active cushion were assessed quantitatively and compared to two types of passive cushions--the Roho high-<span class="hlt">profile</span> air floatation cushion and the polyurethane (PU) foam cushion. Eight non-disabled subjects were positioned on the active cushion at two inflation-<span class="hlt">pressure</span> levels--30 mmHg and 60 mmHg, or on the Roho or the PU foam cushions. Interface <span class="hlt">pressures</span> were recorded using the Oxford <span class="hlt">pressure</span> monitor. For the active cushion it was shown that the higher the inflation <span class="hlt">pressure</span> was, the better the <span class="hlt">pressure</span>-relieving characteristics seemed to be. In general, the <span class="hlt">pressure</span>-relieving characteristics of the active cushion were not as good as those of the passive cushions being tested. The active cushion could alter the <span class="hlt">pressures</span> over the ischial tuberosities cyclically but the amount of <span class="hlt">pressure</span> alternation depended on the relative position of the ischial tuberosities and the air bellows.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2001A%26A...369..889B','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2001A%26A...369..889B"><span>A study of polarized spectra of magnetic CP stars: Predicted š. <span class="hlt">observed</span> Stokes IQUV <span class="hlt">profiles</span> for beta CrB and 53 Cam</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Bagnulo, S.; Wade, G. A.; Donati, J.-F.; Landstreet, J. D.; Leone, F.; Monin, D. N.; Stift, M. J.</p> <p>2001-04-01</p> <p>We present a comparison of <span class="hlt">observed</span> and calculated Stokes IQUV spectra of two well-known magnetic chemically peculiar stars, beta Coronae Borealis and 53 Camelopardalis. The <span class="hlt">observed</span> Stokes spectra were recently described by Wade et al. (\\cite{wad00a}), and have been complemented with additional circularly polarized spectra obtained at the Special Astrophysical Observatory. The calculated spectra represent the predictions of new and previously published magnetic field models derived from the analysis of some surface averaged field estimates (e.g., longitudinal field, magnetic field modulus, etc.). We find that these magnetic models are not sufficient to account fully for the <span class="hlt">observed</span> Stokes <span class="hlt">profiles</span> - particularly remarkable is the disagreement between the predicted and <span class="hlt">observed</span> Stokes Q and U <span class="hlt">profiles</span> of 53 Cam. We suggest that this should be interpreted in terms of magnetic morphologies which are significantly more complex than the second-order multipolar expansions assumed in the models. However, it is clear that some of our inability to reproduce the detailed shapes of the Stokes IQUV <span class="hlt">profiles</span> is unrelated to the magnetic models. For many metallic ions, for both stars, we found it impossible to account for the strengths and shapes of the <span class="hlt">observed</span> spectral line <span class="hlt">profiles</span> when we adopted a unique value for the individual ion abundance. We suggest that this results from strongly non-uniform distributions of these ions as a function of optical depth (i.e., chemical stratification), a hypothesis that is supported by comparison with simple chemically stratified models. Based on <span class="hlt">observations</span> obtained with the 2 m Bernard Lyot telescope of the Pic-du-Midi Observatory, the 1 m telescope of the Special Astrophysical Observatory, and the 0.9 m telescope of the Osservatorio Astrofisico di Catania.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/20130008703','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/20130008703"><span>Integrating Wind <span class="hlt">Profiling</span> Radars and Radiosonde <span class="hlt">Observations</span> with Model Point Data to Develop a Decision Support Tool to Assess Upper-Level Winds for Space Launch</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Bauman, William H., III; Flinn, Clay</p> <p>2013-01-01</p> <p>On the day of launch, the 45th Weather Squadron (45 WS) Launch Weather Officers (LWOs) monitor the upper-level winds for their launch customers. During launch operations, the payload/launch team sometimes asks the LWOs if they expect the upper-level winds to change during the countdown. The LWOs used numerical weather prediction model point forecasts to provide the information, but did not have the capability to quickly retrieve or adequately display the upper-level <span class="hlt">observations</span> and compare them directly in the same display to the model point forecasts to help them determine which model performed the best. The LWOs requested the Applied Meteorology Unit (AMU) develop a graphical user interface (GUI) that will plot upper-level wind speed and direction <span class="hlt">observations</span> from the Cape Canaveral Air Force Station (CCAFS) Automated Meteorological <span class="hlt">Profiling</span> System (AMPS) rawinsondes with point forecast wind <span class="hlt">profiles</span> from the National Centers for Environmental Prediction (NCEP) North American Mesoscale (NAM), Rapid Refresh (RAP) and Global Forecast System (GFS) models to assess the performance of these models. The AMU suggested adding <span class="hlt">observations</span> from the NASA 50 MHz wind <span class="hlt">profiler</span> and one of the US Air Force 915 MHz wind <span class="hlt">profilers</span>, both located near the Kennedy Space Center (KSC) Shuttle Landing Facility, to supplement the AMPS <span class="hlt">observations</span> with more frequent upper-level <span class="hlt">profiles</span>. Figure 1 shows a map of KSC/CCAFS with the locations of the <span class="hlt">observation</span> sites and the model point forecasts.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://ntrs.nasa.gov/search.jsp?R=19820030941&hterms=climate+exchange&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D50%26Ntt%3Dclimate%2Bexchange','NASA-TRS'); return false;" href="https://ntrs.nasa.gov/search.jsp?R=19820030941&hterms=climate+exchange&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D50%26Ntt%3Dclimate%2Bexchange"><span>Weather and climate needs for lidar <span class="hlt">observations</span> from space and concepts for their realization</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Atlas, D.; Korb, C. L.</p> <p>1981-01-01</p> <p>The spectrum of weather and climate needs for lidar <span class="hlt">observations</span> from space is discussed. This paper focuses mainly on the requirements for winds, temperature, moisture, and <span class="hlt">pressure</span>. Special emphasis is given to the need for wind <span class="hlt">observations</span>, and it is shown that winds are required to depict realistically all atmospheric scales in the tropics and the smaller scales at higher latitudes, where both temperature and wind <span class="hlt">profiles</span> are necessary. The need for means to estimate air-sea exchanges of sensible and latent heat also is noted. Lidar can aid here by measurement of the slope of the boundary layer. Recent theoretical feasibility studies concerning the <span class="hlt">profiling</span> of temperature, <span class="hlt">pressure</span>, and humidity by differential absorption lidar (DIAL) from space and expected accuracies are reviewed. Initial ground-based trials provide support for these approaches and also indicate their direct applicability to path-average temperature measurements near the surface. An alternative approach to Doppler lidar wind measurements also is presented. The concept involves the measurement of the displacement of the aerosol backscatter pattern, at constant height, between two successive scans of the same area, one ahead of the spacecraft and the other behind it, a few minutes later. Finally, an integrated space lidar system capable of measuring temperature, <span class="hlt">pressure</span>, humidity, and winds which combines the DIAL methods with the aerosol pattern displacement concept is described briefly.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2011MNRAS.413.1991W','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2011MNRAS.413.1991W"><span><span class="hlt">Pressure</span> from dark matter annihilation and the rotation curve of spiral galaxies</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Wechakama, M.; Ascasibar, Y.</p> <p>2011-05-01</p> <p>The rotation curves of spiral galaxies are one of the basic predictions of the cold dark matter paradigm, and their shape in the innermost regions has been hotly debated over the last decades. The present work shows that dark matter annihilation into electron-positron pairs may affect the <span class="hlt">observed</span> rotation curve by a significant amount. We adopt a model-independent approach, where all the electrons and positrons are injected with the same initial energy E0˜mdmc2 in the range from 1 MeV to 1 TeV and the injection rate is constrained by INTEGRAL, Fermi and HESS data. The <span class="hlt">pressure</span> of the relativistic electron-positron gas is determined by solving the diffusion-loss equation, considering inverse Compton scattering, synchrotron radiation, Coulomb collisions, bremsstrahlung and ionization. For values of the gas density and magnetic field that are representative of the Milky Way, it is estimated that <span class="hlt">pressure</span> gradients are strong enough to balance gravity in the central parts if E0 < 1 GeV. The exact value depends somewhat on the astrophysical parameters, and it changes dramatically with the slope of the dark matter density <span class="hlt">profile</span>. For very steep slopes, as those expected from adiabatic contraction, the rotation curves of spiral galaxies would be affected on ˜kpc scales for most values of E0. By comparing the predicted rotation curves with <span class="hlt">observations</span> of dwarf and low surface brightness galaxies, we show that the <span class="hlt">pressure</span> from dark matter annihilation may improve the agreement between theory and <span class="hlt">observations</span> in some cases, but it also imposes severe constraints on the model parameters (most notably, the inner slope of halo density <span class="hlt">profile</span>, as well as the mass and the annihilation cross-section of dark matter particles into electron-positron pairs).</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=5724067','PMC'); return false;" href="https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=5724067"><span>Antibiotic susceptibility <span class="hlt">profiles</span> of ocular and nasal flora in patients undergoing cataract surgery in Taiwan: an <span class="hlt">observational</span> and cross-sectional study</span></a></p> <p><a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pmc">PubMed Central</a></p> <p>Lin, Yun-Hsuan; Kang, Yu-Chuan; Hou, Chiun-Ho; Huang, Yhu-Chering; Chen, Chih-Jung; Shu, Jwu-Ching; Hsieh, Pang-Hsin; Hsiao, Ching-Hsi</p> <p>2017-01-01</p> <p>Objective To investigate the conjunctival and nasal flora and the antibiotic susceptibility <span class="hlt">profiles</span> of isolates from patients undergoing cataract surgery. Design <span class="hlt">Observational</span> and cross-sectional study. Setting A single-centre study in Taiwan. Participants 128 consecutive patients precataract surgery. Primary and secondary outcome measures methods Conjunctival and nasal cultures were prospectively obtained from 128 patients on the day of cataract surgery before instillation of ophthalmic solutions in our hospital. Isolates and antibiotic susceptibility <span class="hlt">profiles</span> were identified through standard microbiological techniques. Participants were asked to complete a questionnaire on healthcare-associated factors. Results The positive culture rate from conjunctiva was 26.6%, yielding 84 isolates. Coagulase-negative Staphylococci were the most commonly isolated organisms (45.2%), and 35% of staphylococcal isolates were methicillin-resistant. Among staphylococcal isolates, all were susceptible to vancomycin, and 75%–82.5% were susceptible to fluoroquinolones. Methicillin-resistant isolates were significantly less susceptible than their methicillin-sensitive counterparts to tobramycin, the most commonly used prophylactic antibiotic in our hospital (28.6% vs 69.2%; p=0.005). The positive culture rate from nares for Staphylococcus aureus was 21.9%, and six isolates were methicillin-resistant. No subjects had S. aureus colonisation on conjunctiva and nares simultaneously. There were no associated risk factors for colonisation of methicillin-resistant Staphylococci. Conclusion The most common conjunctival bacterial isolate of patients undergoing cataract surgery was coagulase-negative Staphylococci in Taiwan. Because of predominant antibiotic preferences and selective antibiotic <span class="hlt">pressures</span>, Staphylococci were more susceptible to fluoroquinolones but less to tobramycin than in other reports. Additionally, methicillin-resistant Staphylococci exhibited co-resistance to tobramycin</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/28904452','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/28904452"><span>Long-term Response of Cerebrospinal Fluid <span class="hlt">Pressure</span> in Patients with Idiopathic Intracranial Hypertension - A Prospective <span class="hlt">Observational</span> Study.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Gafoor, V Abdul; Smita, B; Jose, James</p> <p>2017-01-01</p> <p>Idiopathic intracranial hypertension (IIH) is increased intracranial <span class="hlt">pressure</span> (ICP) with normal cerebrospinal fluid (CSF) contents, in the absence of an intracranial mass, hydrocephalus, or other identifiable causes. The current knowledge of the treatment outcome of IIH is limited, and the data on the natural history of this entity are scant. The objective of the study is to study the treatment response of IIH by serially measuring the CSF opening <span class="hlt">pressure</span> and to delineate the factors influencing the same. A prospective <span class="hlt">observational</span> study in a cohort of fifty patients with IIH in whom CSF opening <span class="hlt">pressure</span> was serially measured at pre-specified intervals. The mean CSF opening <span class="hlt">pressure</span> at baseline was 302.4 ± 51.69 mm of H 2 O (range: 220-410). Even though a higher body mass index (BMI) showed a trend toward a higher CSF opening <span class="hlt">pressure</span>, the association was not significant ( P = 0.168). However, the age of the patient had a significant negative correlation with the CSF <span class="hlt">pressure</span> ( P = 0.006). The maximum reduction in CSF <span class="hlt">pressure</span> occurred in the first 3 months of treatment, and thereafter it plateaued. Remission was attained in 12 (24%) patients. BMI had the strongest association with remission ( P = 0.001). In patients with IIH, treatment response is strongly related to BMI. However, patients with normal BMI are also shown to relapse and hence should have continuous, long-term follow-up. The reduction in CSF <span class="hlt">pressure</span> attained in the first 3 months could reflect the long-term response to treatment.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/19910004271','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/19910004271"><span>Pioneer-Venus radio occultation (ORO) data reduction: <span class="hlt">Profiles</span> of 13 cm absorptivity</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Steffes, Paul G.</p> <p>1990-01-01</p> <p>In order to characterize possible variations in the abundance and distribution of subcloud sulfuric acid vapor, 13 cm radio occultation signals from 23 orbits that occurred in late 1986 and 1987 (Season 10) and 7 orbits that occurred in 1979 (Season 1) were processed. The data were inverted via inverse Abel transform to produce 13 cm absorptivity <span class="hlt">profiles</span>. <span class="hlt">Pressure</span> and temperature <span class="hlt">profiles</span> obtained with the Pioneer-Venus night probe and the northern probe were used along with the absorptivity <span class="hlt">profiles</span> to infer upper limits for vertical <span class="hlt">profiles</span> of the abundance of gaseous H2SO4. In addition to inverting the data, error bars were placed on the absorptivity <span class="hlt">profiles</span> and H2SO4 abundance <span class="hlt">profiles</span> using the standard propagation of errors. These error bars were developed by considering the effects of statistical errors only. The <span class="hlt">profiles</span> show a distinct pattern with regard to latitude which is consistent with latitude variations <span class="hlt">observed</span> in data obtained during the occultation seasons nos. 1 and 2. However, when compared with the earlier data, the recent occultation studies suggest that the amount of sulfuric acid vapor occurring at and below the main cloud layer may have decreased between early 1979 and late 1986.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/11642089','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/11642089"><span>[24-Hour blood <span class="hlt">pressure</span> <span class="hlt">profile</span> in patients with mild and moderate arterial hypertension and sleep apnea/hypopnea].</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Zelveian, P A; Oshchepkova, E V; Buniatian, M S; Badikov, D N; Rogoza, A N</p> <p>2001-01-01</p> <p>To evaluate 24-hour blood <span class="hlt">pressure</span> (BP) <span class="hlt">profile</span> in arterial hypertension (AH) patients (pts) with desaturation signs of sleep apnea/hypopnea syndrome (SAHS). We investigated 61 pts (44 males and 17 females) aged between 23-70 (52 +/- 2) years with mild to moderate AH. BP monitoring was performed with multisensor system TM-2425 (A&D, Japan). We assessed the following parameters: mean 24-h, awake, sleep systolic (S), diastolic (D) and pulse (P) BPs, systolic and diastolic BP loads ("normalized area under the curve"--NAUC). A normal circadian rhythm of BP was defined when nocturnal fall of SBP was > 10% and < 20%. The morning rise of BP we assessed by speed of increase of mean BP from 4 a.m. to 12 a.m. The nocturnal monitoring of arterial oxygen saturation(SaO2) was performed with pulseoximeter "NONIN 8500M" (USA). The analysis of the results was performed with the original program ARM-SaO2". The presence of SAHS was confirmed when the number of 4% desaturations were greater than 15 per hour or in the presence of group episodes of 4% desaturation below 90%. In 19 pts we revealed desaturation signs of SAHS. The comparison group included pts without SAHS (n = 42). We compared the groups regarding 24-h BP <span class="hlt">profile</span> parameters. SAHS group had the following parameters significantly higher: mean 24-h (151.7 +/- 4.5 vs 142.9 +/- 2.4 mm Hg, p < 0.07) and sleep SBPs (142.8 +/- 5.1 vs 132.7 +/- 2.6 mm Hg, p < 0.05); mean 24-h (65.2 +/- 2.6 vs 55.9 +/- 1.9 mm Hg, p < 0.008), daytime (65.6 +/- 2.7 vs 56.6 +/- 2.0 mm Hg, p < 0.01) and sleep PBPs (64.1 +/- 2.7 vs 53.1 +/- 1.9 mm Hg, p < 0.002); 24-h (20.1 +/- 3.8 vs 12.6 +/- 1.8 mm Hg, p < 0.05) and sleep NAUC of SBP (24.6 +/- 4.4 vs 15.3 +/- 2.2 mm Hg, p < 0.03). In the group with SAHS were significantly higher the frequency of abnormal circadian rhythm of SBP (84 vs 57%, p < 0.05) and the speed of morning rise of mean BP (23.3 +/- 5.9 vs 8.5 +/- 2.8 mm Hg/h, p < 0.01). Our results suggest that pts with desaturation signs of SAHS</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2014AGUFM.A31C3048Z','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2014AGUFM.A31C3048Z"><span>Vertical <span class="hlt">Profiles</span> of Light-Absorbing Aerosol: A Combination of In-situ and AERONET <span class="hlt">Observations</span> during NASA DISCOVER-AQ</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Ziemba, L. D.; Beyersdorf, A. J.; Chen, G.; Corr, C.; Crumeyrolle, S.; Giles, D. M.; Holben, B. N.; Hudgins, C.; Martin, R.; Moore, R.; Shook, M.; Thornhill, K. L., II; Winstead, E.; Anderson, B. E.</p> <p>2014-12-01</p> <p>Understanding the vertical <span class="hlt">profile</span> of atmospheric aerosols plays a vital role in utilizing spaceborne, column-integrated satellite <span class="hlt">observations</span>. The properties and distribution of light-absorbing aerosol are particularly uncertain despite significant air quality and climate ramifications. Advanced retrieval algorithms are able to derive complex aerosol properties (e.g., wavelength-dependent absorption coefficient and single scattering albedo) from remote-sensing measurements, but quantitative relationships to surface conditions remain a challenge. Highly systematic atmospheric <span class="hlt">profiling</span> during four unique deployments for the NASA DISCOVER-AQ project (Baltimore, MD, 2011; San Joaquin Valley, CA, 2013; Houston, TX, 2013; Denver, CO, 2014) allow statistical assessment of spatial, temporal, and source-related variability for light-absorbing aerosol properties in these distinct regions. In-situ sampling in conjunction with a dense network of AERONET sensors also allows evaluation of the sensitivity, limitations, and advantages of remote-sensing data products over a wide range of conditions. In-situ aerosol and gas-phase <span class="hlt">observations</span> were made during DISCOVER-AQ aboard the NASA P-3B aircraft. Aerosol absorption coefficients were measured by a Particle Soot Absorption Photometer (PSAP). Approximately 200 <span class="hlt">profiles</span> for each of the four deployments were obtained, from the surface (25-300m altitude) to 5 km, and are used to calculate absorption aerosol optical depths (AAODs). These are quantitatively compared to AAOD derived from AERONET Level 1.5 retrievals to 1) explore discrepancies between measurements, 2) quantify the fraction of AAOD that exists directly at the surface and is often missed by airborne sampling, and 3) evaluate the potential for deriving ground-level black carbon (BC) concentrations for air quality prediction. Aerosol size distributions are used to assess absorption contributions from mineral dust, both at the surface and aloft. SP2 (Single Particle Soot</p> </li> </ol> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_15");'>15</a></li> <li><a href="#" onclick='return showDiv("page_16");'>16</a></li> <li class="active"><span>17</span></li> <li><a href="#" onclick='return showDiv("page_18");'>18</a></li> <li><a href="#" onclick='return showDiv("page_19");'>19</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div><!-- col-sm-12 --> </div><!-- row --> </div><!-- page_17 --> <div id="page_18" class="hiddenDiv"> <div class="row"> <div class="col-sm-12"> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_16");'>16</a></li> <li><a href="#" onclick='return showDiv("page_17");'>17</a></li> <li class="active"><span>18</span></li> <li><a href="#" onclick='return showDiv("page_19");'>19</a></li> <li><a href="#" onclick='return showDiv("page_20");'>20</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div> </div> <div class="row"> <div class="col-sm-12"> <ol class="result-class" start="341"> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.osti.gov/biblio/21443013-observability-radiation-pressure-shot-noise-optomechanical-systems','SCIGOV-STC'); return false;" href="https://www.osti.gov/biblio/21443013-observability-radiation-pressure-shot-noise-optomechanical-systems"><span><span class="hlt">Observability</span> of radiation-<span class="hlt">pressure</span> shot noise in optomechanical systems</span></a></p> <p><a target="_blank" href="http://www.osti.gov/search">DOE Office of Scientific and Technical Information (OSTI.GOV)</a></p> <p>Boerkje, K.; Nunnenkamp, A.; Zwickl, B. M.</p> <p>2010-07-15</p> <p>We present a theoretical study of an experiment designed to detect radiation-<span class="hlt">pressure</span> shot noise in an optomechanical system. Our model consists of a coherently driven optical cavity mode that is coupled to a mechanical oscillator. We examine the cross-correlation between two quadratures of the output field from the cavity. We determine under which circumstances radiation-<span class="hlt">pressure</span> shot noise can be detected by a measurement of this cross-correlation. This is done in the general case of nonzero detuning between the frequency of the drive and the cavity resonance frequency. We study the qualitative features of the different contributions to the cross-correlator andmore » provide quantitative figures of merit for the relative importance of the radiation-<span class="hlt">pressure</span> shot noise contribution to other contributions. We also propose a modified setup of this experiment relevant to the 'membrane-in-the-middle' geometry, which potentially can avoid the problems of static bistability and classical noise in the drive.« less</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/24492424','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/24492424"><span>Home blood <span class="hlt">pressure</span> monitoring in heart transplant recipients: comparison with ambulatory blood <span class="hlt">pressure</span> monitoring.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Ambrosi, Pierre; Kreitmann, Bernard; Habib, Gilbert</p> <p>2014-02-15</p> <p>How reliable is home blood <span class="hlt">pressure</span> monitoring (HBPM) in heart transplant recipients is not known. Possibly, it may underestimate hypertensive burden, because blood <span class="hlt">pressure</span> (BP) nondipper <span class="hlt">profile</span> is frequent among these patients. This prospective study has been designed to determine whether HBPM adequately identifies hypertension in heart transplant recipients. We compared HBPM with ambulatory blood <span class="hlt">pressure</span> monitoring (ABPM) for the diagnosis of uncontrolled hypertension in 74 patients 13.5±6.7 years after heart transplantation. HBPM was measured with a validated semiautomatic device twice every morning and twice every evening on 7 consecutive days, within 15 days of ABPM. We also measured the relationship between HBPM, ABPM, and organ damage as measured by albuminuria and left ventricular mass. A nondipper <span class="hlt">profile</span> was found in 53 (72%) patients. HBPM and ABPM were close according to Pearson bivariate correlations. There was no significant correlation between left ventricular mass and BP either at HBPM or ABPM. Proteinuria significantly correlated with systolic BP either at HBPM (R=0.42; P=0.0002) or ABPM (R=0.25; P=0.03). HBPM adequately classified 61 of 74 (82%) patients as hypertensives or as nonhypertensives or controlled hypertensives. Despite a high prevalence of nondipper <span class="hlt">profile</span>, HBPM gives a reliable estimate of BP burden in most heart transplant recipients. Thus, our results strongly suggest that HBPM is useful for the long-term follow-up of heart transplant recipients.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=4172515','PMC'); return false;" href="https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=4172515"><span><span class="hlt">Profiles</span> of <span class="hlt">observed</span> infant anger predict preschool behavior problems: Moderation by life stress</span></a></p> <p><a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pmc">PubMed Central</a></p> <p>Brooker, Rebecca J.; Buss, Kristin A.; Lemery-Chalfant, Kathryn; Aksan, Nazan; Davidson, Richard J.; Goldsmith, H. Hill</p> <p>2014-01-01</p> <p>Using both traditional composites and novel <span class="hlt">profiles</span> of anger, we examined associations between infant anger and preschool behavior problems in a large, longitudinal data set (N = 966). We also tested the role of life stress as a moderator of the link between early anger and the development of behavior problems. Although traditional measures of anger were largely unrelated to later behavior problems, <span class="hlt">profiles</span> of anger that dissociated typical from atypical development predicted behavior problems during preschool. Moreover, the relation between infant anger <span class="hlt">profiles</span> and preschool behavior problems was moderated such that, when early life stress was low, infants with atypical <span class="hlt">profiles</span> of early anger showed more preschool behavior problems than did infants with normative anger <span class="hlt">profiles</span>. However, when early life stress was high, infants with atypical and normative <span class="hlt">profiles</span> of infant anger did not differ in preschool behavior problems. We conclude that a discrete emotions approach including latent <span class="hlt">profile</span> analysis is useful for elucidating biological and environmental developmental pathways to early problem behaviors. PMID:25151247</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2012EGUGA..1410770V','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2012EGUGA..1410770V"><span>Integration of Infrasound, Atmospheric <span class="hlt">Pressure</span>, and Seismic <span class="hlt">Observations</span> with the NSF EarthScope USArray Transportable Array</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Vernon, F.; Tytell, J.; Hedlin, M. A. H.; Walker, K.; Busby, R.; Woodward, R.</p> <p>2012-04-01</p> <p>Earthscope's USArray Transportable Array (TA) network serves as a real-time monitoring and recording platform for both seismic and weather phenomena. To date, most of the approximately 500 TA stations have been retrofitted with VTI SCP1000 MEMS barometric <span class="hlt">pressure</span> gauges capable of recording data at 1 sample per second (sps). Additionally, over 300 of the TA stations have also been retrofitted with Setra 278 barometric gauges and NCPA infrasound sensors capable of recording data at 1 and 40 sps. While individual seismic events have been successfully researched via the TA network, <span class="hlt">observations</span> of powerful weather events by the TA network have yet to be embraced by the scientific community. This presentation will focus on case studies involving severe weather passage across portions of the TA network throughout 2011 in order to highlight its viability as a platform for real-time weather monitoring and research. It will also highlight the coupling of atmospheric signals into the seismic <span class="hlt">observations</span>. Examples of gust front passages and <span class="hlt">pressure</span> couplets from severe thunderstorms will be presented, as will <span class="hlt">observations</span> of multiple tornados occurred in the Spring of 2011. These data will demonstrate the overall viability of the TA network for monitoring severe weather events in real-time.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://ntrs.nasa.gov/search.jsp?R=19800054734&hterms=1089&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D20%26Ntt%3D%2526%25231089','NASA-TRS'); return false;" href="https://ntrs.nasa.gov/search.jsp?R=19800054734&hterms=1089&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D20%26Ntt%3D%2526%25231089"><span>An experimental investigation of endwall <span class="hlt">profiling</span> in a turbine vane cascade</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Kopper, F. C.; Milano, R.; Vanco, M.</p> <p>1980-01-01</p> <p>Measurements of surface static <span class="hlt">pressures</span>, flow total <span class="hlt">pressure</span> loss, and exit air angle were obtained for two linear cascades to establish the effects of endwall <span class="hlt">profiling</span>. Testing was conducted at an isentropic exit Mach number of 0.85. One cascade was fabricated with planar endwalls while the other had one planar and one <span class="hlt">profiled</span> endwall. Both cascades utilized the same high <span class="hlt">pressure</span> turbine inlet guide vane section. It was found that in terms of full passage loss the <span class="hlt">profiled</span> endwall cascade has the superior performance. The secondary loss results obtained are reasonably well predicted by correlations developed from incompressible flow testing of similar configurations. Inviscid flow and boundary layer calculations are compared with the test data, and overall, the agreement is found to be good. Use of the results for design purposes is briefly discussed.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2015ChPhB..24e8901L','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2015ChPhB..24e8901L"><span>Transportation-cyber-physical-systems-oriented engine cylinder <span class="hlt">pressure</span> estimation using high gain <span class="hlt">observer</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Li, Yong-Fu; Xiao-Pei, Kou; Zheng, Tai-Xiong; Li, Yin-Guo</p> <p>2015-05-01</p> <p>In transportation cyber-physical-systems (T-CPS), vehicle-to-vehicle (V2V) communications play an important role in the coordination between individual vehicles as well as between vehicles and the roadside infrastructures, and engine cylinder <span class="hlt">pressure</span> is significant for engine diagnosis on-line and torque control within the information exchange process under V2V communications. However, the parametric uncertainties caused from measurement noise in T-CPS lead to the dynamic performance deterioration of the engine cylinder <span class="hlt">pressure</span> estimation. Considering the high accuracy requirement under V2V communications, a high gain <span class="hlt">observer</span> based on the engine dynamic model is designed to improve the accuracy of <span class="hlt">pressure</span> estimation. Then, the analyses about convergence, converge speed and stability of the corresponding error model are conducted using the Laplace and Lyapunov method. Finally, results from combination of Simulink with GT-Power based numerical experiments and comparisons demonstrate the effectiveness of the proposed approach with respect to robustness and accuracy. Project supported by the National Natural Science Foundation of China (Grant No. 61304197), the Scientific and Technological Talents of Chongqing, China (Grant No. cstc2014kjrc-qnrc30002), the Key Project of Application and Development of Chongqing, China (Grant No. cstc2014yykfB40001), the Natural Science Funds of Chongqing, China (Grant No. cstc2014jcyjA60003), and the Doctoral Start-up Funds of Chongqing University of Posts and Telecommunications, China (Grant No. A2012-26).</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017AGUFM.A33B2363K','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017AGUFM.A33B2363K"><span>Effects of Temperature and Air Density <span class="hlt">Profiles</span> on Ozone Lidar Retrievals</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Kirgis, G.; Langford, A. O.; Senff, C. J.; Alvarez, R. J. _II, II</p> <p>2017-12-01</p> <p>The recent reduction in the primary U.S. National Ambient Air Quality Standard (NAAQS) for ozone (O3) from 75 to 70 parts-per-billion by volume (ppbv) adds urgency to the need for better understanding of the processes that control ground-level concentrations in the United States. While ground-based in situ sensors are capable of measuring ozone levels, they don't give any insight into upper air transport and mixing. Differential absorption lidars such as the NOAA/ESRL Tunable Optical <span class="hlt">Profiler</span> for Aerosol and oZone (TOPAZ) measure continuous vertical ozone <span class="hlt">profiles</span> with high spatial and temporal resolution. However, the retrieved ozone mixing ratios depend on the temperature and air density <span class="hlt">profiles</span> used in the analysis. This study analyzes the ozone concentrations for seven field campaigns from 2013 to 2016 to evaluate the impact of the assumed <span class="hlt">pressure</span> and temperature <span class="hlt">profiles</span> on the ozone mixing ratio retrieval. <span class="hlt">Pressure</span> and temperature <span class="hlt">profiles</span> from various spatial and temporal resolution models (Modern Era Retrospective-Analysis for Research and Applications, NCEP/NCAR Reanalysis, NCEP North American Regional Reanalysis, Rapid Refresh, and High-Resolution Rapid Refresh) are compared to reference ozone <span class="hlt">profiles</span> created with <span class="hlt">pressure</span> and temperature <span class="hlt">profiles</span> from ozonesondes launched close to the TOPAZ measurement site. The results show significant biases with respect to time of day and season, altitude, and location of the model-extracted <span class="hlt">profiles</span>. Limitations and advantages of all datasets used will also be discussed.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2016AGUFM.A23N..04S','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2016AGUFM.A23N..04S"><span>Simultaneous Measurements of CO2 Concentration and Temperature <span class="hlt">profiles</span> using 1.6 μm DIAL in the Lower-Atmosphere</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Shibata, Y.; Nagasawa, C.; Abo, M.</p> <p>2016-12-01</p> <p>High-accurate vertical carbon dioxide (CO2) <span class="hlt">profiles</span> are highly desirable in the inverse method to improve quantification and understanding of the global sink and source of CO2, and also global climate change. We have developed a ground based 1.6μm differential absorption lidar (DIAL) to achieve measurements of vertical CO2 <span class="hlt">profiles</span> in the atmosphere. As the spectra of absorption lines of any molecules are influenced basically by the temperature and <span class="hlt">pressure</span> in the atmosphere, it is important to measure them simultaneously so that the better accuracy of the DIAL measurement is realized. The barometric formula can derive atmospheric <span class="hlt">pressure</span> of each altitude using atmospheric <span class="hlt">pressure</span> of ground level at the lidar site. Comparison of atmospheric <span class="hlt">pressure</span> prlofiles calculated from this equation and those obtained from radiosonde <span class="hlt">observations</span> at Tateno, Japan are consisted within 0.2 % below 3 km altitude. So, we have developed a 1.6 μm CO2 DIAL system for simultaneous measurements of the CO2 concentration and temperature <span class="hlt">profiles</span> in the lower-atmosphere. Laser beams of three wavelengths around a CO2 absorption spectrum is transmitted alternately to the atmosphere. Moreover, the value of the retrieved CO2 concentration will be improved remarkably by processing the iteration assignment of CO2 concentration and temperature, which measured by these DIAL techniques. We have acheived vertical CO2 concentration and temperature <span class="hlt">profile</span> from 0.5 to 2.0 km altitude by this DIAL system. In the next step, we will use this high accuracy CO2 concentration <span class="hlt">profile</span> and back-trajectory analysis for the behavior analysis of the CO2 mass. This work was financially supported by the System Development Program for Advanced Measurement and Analysis of the Japan Science and Technology Agency.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017JPCS..109...26B','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017JPCS..109...26B"><span>Noise-modulated self-polarization effect of impurity doped quantum dots under simultaneous presence of hydrostatic <span class="hlt">pressure</span> and temperature</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Bera, Aindrila; Ghosh, Manas</p> <p>2017-10-01</p> <p>We explore the <span class="hlt">profiles</span> of self-polarization effect (SPE) of doped GaAs QD under simultaneous presence of hydrostatic <span class="hlt">pressure</span> (HP), temperature and in presence of noise. Noise term carries Gaussian white character and it has been administered to the system via two different pathways; additive and multiplicative. <span class="hlt">Profiles</span> of SPE have been monitored as a function of HP, temperature and noise strength. Under a given condition of HP and temperature, noise marks its prominent signature on the SPE <span class="hlt">profile</span>. However, the extent to which noise affects the SPE <span class="hlt">profile</span> visibly depends on the noise strength and the pathway through which noise is introduced. As interesting <span class="hlt">observations</span> we have found that SPE exhibits minimization at a <span class="hlt">pressure</span> of ∼ 170 kbar in absence of noise and at ∼ 150 kbar when noise is present. Furthermore, in presence of multiplicative noise SPE exhibits a very faint decrease with increase in T up to T ∼ 420 K. However, beyond T ∼ 420 K, further increase in temperature causes abrupt fall of SPE in a highly sharp way. The findings highlight viable ways of tuning SPE of doped QD system through subtle interplay between HP, temperature and noise.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.osti.gov/biblio/22663529-non-maxwellian-analysis-transition-region-line-profiles-observed-interface-region-imaging-spectrograph','SCIGOV-STC'); return false;" href="https://www.osti.gov/biblio/22663529-non-maxwellian-analysis-transition-region-line-profiles-observed-interface-region-imaging-spectrograph"><span>Non-Maxwellian Analysis of the Transition-region Line <span class="hlt">Profiles</span> <span class="hlt">Observed</span> by the Interface Region Imaging Spectrograph</span></a></p> <p><a target="_blank" href="http://www.osti.gov/search">DOE Office of Scientific and Technical Information (OSTI.GOV)</a></p> <p>Dudík, Jaroslav; Dzifčáková, Elena; Polito, Vanessa</p> <p>2017-06-10</p> <p>We investigate the nature of the spectral line <span class="hlt">profiles</span> for transition-region (TR) ions <span class="hlt">observed</span> with the Interface Region Imaging Spectrograph (IRIS) . In this context, we analyzed an active-region <span class="hlt">observation</span> performed by IRIS in its 1400 Å spectral window. The TR lines are found to exhibit significant wings in their spectral <span class="hlt">profiles</span>, which can be well fitted with a non-Maxwellian κ distribution. The fit with a κ distribution can perform better than a double-Gaussian fit, especially for the strongest line, Si iv 1402.8 Å. Typical values of κ found are about 2, occurring in a majority of spatial pixels wheremore » the TR lines are symmetric, i.e., the fit can be performed. Furthermore, all five spectral lines studied (from Si iv, O iv, and S iv) appear to have the same full-width at half-maximum irrespective of whether the line is an allowed or an intercombination transition. A similar value of κ is obtained for the electron distribution by the fitting of the line intensities relative to Si iv 1402.8 Å, if photospheric abundances are assumed. The κ distributions, however, do not remove the presence of non-thermal broadening. Instead, they actually increase the non-thermal width. This is because, for κ distributions, TR ions are formed at lower temperatures. The large <span class="hlt">observed</span> non-thermal width lowers the opacity of the Si iv line sufficiently enough for this line to become optically thin.« less</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/18523125','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/18523125"><span>Effect of continuous positive airway <span class="hlt">pressure</span> therapy on hypothalamic-pituitary-adrenal axis function and 24-h blood <span class="hlt">pressure</span> <span class="hlt">profile</span> in obese men with obstructive sleep apnea syndrome.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Carneiro, Gláucia; Togeiro, Sônia Maria; Hayashi, Lílian F; Ribeiro-Filho, Fernando Flexa; Ribeiro, Artur Beltrame; Tufik, Sérgio; Zanella, Maria Teresa</p> <p>2008-08-01</p> <p>Obstructive sleep apnea syndrome (OSAS) increases the risk of cardiovascular events. Sympathetic nervous system and hypothalamic-pituitary-adrenal (HPA) axis activation may be the mechanism of this relationship. The aim of this study was to evaluate HPA axis and ambulatory blood <span class="hlt">pressure</span> monitoring in obese men with and without OSAS and to determine whether nasal continuous positive airway <span class="hlt">pressure</span> therapy (nCPAP) influenced responses. Twenty-four-hour ambulatory blood <span class="hlt">pressure</span> monitoring and overnight cortisol suppression test with 0.25 mg of dexamethasone were performed in 16 obese men with OSAS and 13 obese men controls. Nine men with severe apnea were reevaluated 3 mo after nCPAP therapy. Body mass index and blood <span class="hlt">pressure</span> of OSAS patients and obese controls were similar. In OSAS patients, the percentage of fall in systolic blood <span class="hlt">pressure</span> at night (P = 0.027) and salivary cortisol suppression postdexamethasone (P = 0.038) were lower, whereas heart rate (P = 0.022) was higher compared with obese controls. After nCPAP therapy, patients showed a reduction in heart rate (P = 0.036) and a greater cortisol suppression after dexamethasone (P = 0.001). No difference in arterial blood <span class="hlt">pressure</span> (P = 0.183) was <span class="hlt">observed</span> after 3 mo of nCPAP therapy. Improvement in cortisol suppression was positively correlated with an improvement in apnea-hypopnea index during nCPAP therapy (r = 0.799, P = 0.010). In conclusion, men with OSAS present increased postdexamethasone cortisol levels and heart rate, which were recovered by nCPAP.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://www.ars.usda.gov/research/publications/publication/?seqNo115=269984','TEKTRAN'); return false;" href="http://www.ars.usda.gov/research/publications/publication/?seqNo115=269984"><span>Effects of secoisolariciresinol diglucoside lignan-enriched flaxseed powder on body weight, visceral fat, lipid <span class="hlt">profile</span>, adipokines, and blood <span class="hlt">pressure</span> in rats fed a high-fructose and high-fat diet</span></a></p> <p><a target="_blank" href="https://www.ars.usda.gov/research/publications/find-a-publication/">USDA-ARS?s Scientific Manuscript database</a></p> <p></p> <p></p> <p>The potential effects of secoisolariciresinol diglucoside (SDG) lignan-enriched flaxseed powder LEFP) on body weight, visceral fat, lipid <span class="hlt">profile</span>, adipokines, and blood <span class="hlt">pressure</span> were investigated using Sprague-Dawley rats. The animals were divided into three groups (n=8) that were fed either a norm...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://ntrs.nasa.gov/search.jsp?R=20150018623&hterms=report&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D40%26Ntt%3Dreport','NASA-TRS'); return false;" href="https://ntrs.nasa.gov/search.jsp?R=20150018623&hterms=report&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D40%26Ntt%3Dreport"><span>Externally <span class="hlt">Pressurized</span> Journal Gas Bearings</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Laub, John H.</p> <p>1959-01-01</p> <p>Externally <span class="hlt">pressurized</span> gas-lubricated bearings with multiple orifice feed are investigated. An analytical treatment is developed for a semi-cylindrical bearing with 9 orifices and for a cylindrical journal bearing with 192 radial and 24 axial orifices. Experiments are described on models of the two bearing configurations with specially designed fixtures which incorporate pneumatic loading and means for determining <span class="hlt">pressure</span> <span class="hlt">profiles</span>, gas flow and gap height. The correlation between theory and experiment is satisfactory.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2015APS..DFDA24003O','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2015APS..DFDA24003O"><span>Fluid dynamic modelling of renal pelvic <span class="hlt">pressure</span> during endoscopic stone removal</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Oratis, Alexandros; Subasic, John; Bird, James; Eisner, Brian</p> <p>2015-11-01</p> <p>Endoscopic kidney stone removal procedures are known to increase internal <span class="hlt">pressure</span> in the renal pelvis, the kidney's urinary collecting system. High renal pelvic <span class="hlt">pressure</span> incites systemic absorption of irrigation fluid, which can increase the risk of postoperative fever and sepsis or the unwanted absorption of electrolytes. Urologists choose the appropriate surgical procedure based on patient history and kidney stone size. However, no study has been conducted to compare the <span class="hlt">pressure</span> <span class="hlt">profiles</span> of each procedure, nor is there a precise sense of how the renal pelvic <span class="hlt">pressure</span> scales with various operational parameters. Here we develop physical models for the flow rates and renal pelvic <span class="hlt">pressure</span> for various procedures. We show that the results of our models are consistent with existing urological data on each procedure and that the models can predict <span class="hlt">pressure</span> <span class="hlt">profiles</span> where data is unavailable.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017JAESc.145..130X','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017JAESc.145..130X"><span>Different origins of garnet in high <span class="hlt">pressure</span> to ultrahigh <span class="hlt">pressure</span> metamorphic rocks</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Xia, Qiong-Xia; Zhou, Li-Gang</p> <p>2017-09-01</p> <p>Garnet in high-<span class="hlt">pressure</span> (HP) to ultrahigh-<span class="hlt">pressure</span> (UHP) metamorphic rocks in subduction zone commonly shows considerable zonation in major and trace elements as well as mineral inclusions, which bears information on its growth mechanism via metamorphic or peritectic reactions in coexistence with relic minerals and metamorphic fluids or anatectic melts at subduction-zone conditions. It provides an important target to retrieve physicochemical changes in subduction-zone processes, including those not only in <span class="hlt">pressure</span> and temperature but also in the durations of metamorphism and anatexis. Garnet from different compositions of HP to UHP metamorphic rocks may show different types of major and trace element zonation, as well as mineral inclusions. Discrimination between the different origins of garnet provides important constraints on <span class="hlt">pressure</span> and temperature and the evolution history for the HP to UHP metamorphic rocks. Magmatic garnet may occur as relics in granitic gneisses despite metamorphic modification at subduction-zone conditions, with spessartine-increasing or flat major element <span class="hlt">profiles</span> from inner to outer core and exceptionally higher contents of trace elements than metamorphic mantle and rim. Metamorphic garnet can grow at different metamorphic stages during prograde subduction and retrograde exhumation, with spessartine-decreasing from core to rim if the intracrystalline diffusion is not too fast. The compositional <span class="hlt">profiles</span> of metamorphic garnet in the abundances of grossular, almandine and pyrope are variable depending on the composition of host rocks and co-existing minerals. Peritectic garnet grows through peritectic reactions during partial melting of HP to UHP rocks, with the composition of major elements to be controlled by anatectic P-T conditions and the compositions of parental rocks and anatectic melts. Trace element <span class="hlt">profiles</span> in garnet with different origins are also variable depending on the coexisting mineral assemblages, the garnet</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/1980WRR....16..365C','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/1980WRR....16..365C"><span>Numerical Analysis of Infiltration Into a Sand <span class="hlt">Profile</span> Bounded by a Capillary Fringe</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Curtis, Alan A.; Watson, Keith K.</p> <p>1980-04-01</p> <p>The rapid response sometimes <span class="hlt">observed</span> in a tile drain system following surface ponding of water is discussed in terms of the air compressibility effect. An earlier numerical study describing water movement into a bounded <span class="hlt">profile</span> with a lower boundary impermeable to the passage of both air and water is reviewed with particular reference to the validity of the time-dependent boundary condition transformation used in simulating the inhibiting effects of the air <span class="hlt">pressure</span> increase on infiltration. The extension of the transformation approach to a <span class="hlt">profile</span> bounded by a capillary fringe is then considered in detail, and the results of numerical analyses are presented for infiltration into two columns of a fine sand initially in hydraulic equilibrium from a prior gravity drainage regime. The shorter column develops a steady state flow condition at short times which is consistent with earlier experimental findings. In contrast, the <span class="hlt">pressure</span> of the entrapped air in the longer column gradually increases as infiltration proceeds until the analysis is terminated when air escape through the lower boundary is imminent.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2015EGUGA..17.2296M','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2015EGUGA..17.2296M"><span>Systematic <span class="hlt">observations</span> of long-range transport events and climatological backscatter <span class="hlt">profiles</span> with the DWD ceilometer network</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Mattis, Ina; Müller, Gerhard; Wagner, Frank; Hervo, Maxime</p> <p>2015-04-01</p> <p>The German Meteorological Service (DWD) operates a network of about 60 CHM15K-Nimbus ceilometers for cloud base height <span class="hlt">observations</span>. Those very powerful ceilometers allow for the detection and characterization of aerosol layers. Raw data of all network ceilometers are transferred online to DWD's data analysis center at the Hohenpeißenberg Meteorological Observatory. There, the occurrence of aerosol layers from long-range transport events in the free troposphere is systematically monitored on daily basis for each single station. If possible, the origin of the aerosol layers is determined manually from the analysis of the meteorological situation and model output. We use backward trajectories as well as the output of the MACC and DREAM models for the decision, whether the <span class="hlt">observed</span> layer originated in the Sahara region, from forest fires in North America or from another, unknown source. Further, the magnitude of the <span class="hlt">observed</span> layers is qualitatively estimated taking into account the geometrical layer depth, signal intensity, model output and nearby sun photometer or lidar <span class="hlt">observations</span> (where available). All <span class="hlt">observed</span> layers are attributed to one of the categories 'faint', 'weak', 'medium', 'strong', or 'extreme'. We started this kind of analysis in August 2013 and plan to continue this systematic documentation of long-range transport events of aerosol layers to Germany on long-term base in the framework of our GAW activities. Most of the <span class="hlt">observed</span> aerosol layers have been advected from the Sahara region to Germany. In the 15 months between August 2013 and November 2014 we <span class="hlt">observed</span> on average 46 days with Sahara dust layers per station, but only 16 days with aerosol layers from forest fires. The occurrence of Sahara dust layers vary with latitude. We <span class="hlt">observed</span> only 28 dusty days in the north, close to the coasts of North Sea and Baltic Sea. In contrast, in southern Germany, in Bavarian Pre-Alps and in the Black Forest mountains, we <span class="hlt">observed</span> up to 59 days with dust. At</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2010ACP....10.6749D','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2010ACP....10.6749D"><span>Probabilistic description of ice-supersaturated layers in low resolution <span class="hlt">profiles</span> of relative humidity</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Dickson, N. C.; Gierens, K. M.; Rogers, H. L.; Jones, R. L.</p> <p>2010-07-01</p> <p>The global <span class="hlt">observation</span>, assimilation and prediction in numerical models of ice super-saturated (ISS) regions (ISSR) are crucial if the climate impact of aircraft condensation trails (contrails) is to be fully understood, and if, for example, contrail formation is to be avoided through aircraft operational measures. Given their small scales compared to typical atmospheric model grid sizes, statistical representations of the spatial scales of ISSR are required, in both horizontal and vertical dimensions, if global occurrence of ISSR is to be adequately represented in climate models. This paper uses radiosonde launches made by the UK Meteorological Office, from the British Isles, Gibraltar, St. Helena and the Falkland Islands between January 2002 and December 2006, to investigate the probabilistic occurrence of ISSR. Each radiosonde <span class="hlt">profile</span> is divided into 50- and 100-hPa <span class="hlt">pressure</span> layers, to emulate the coarse vertical resolution of some atmospheric models. Then the high resolution <span class="hlt">observations</span> contained within each thick <span class="hlt">pressure</span> layer are used to calculate an average relative humidity and an ISS fraction for each individual thick <span class="hlt">pressure</span> layer. These relative humidity <span class="hlt">pressure</span> layer descriptions are then linked through a probability function to produce an s-shaped curve which empirically describes the ISS fraction in any average relative humidity <span class="hlt">pressure</span> layer. Using this empirical understanding of the s-shaped relationship a mathematical model was developed to represent the ISS fraction within any arbitrary thick <span class="hlt">pressure</span> layer. Two models were developed to represent both 50- and 100-hPa <span class="hlt">pressure</span> layers with each reconstructing their respective s-shapes within 8-10% of the empirical curves. These new models can be used, to represent the small scale structures of ISS events, in modelled data where only low vertical resolution is available. This will be useful in understanding, and improving the global distribution, both <span class="hlt">observed</span> and forecasted, of ice super-saturation.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/FR-2011-01-10/pdf/2011-208.pdf','FEDREG'); return false;" href="https://www.gpo.gov/fdsys/pkg/FR-2011-01-10/pdf/2011-208.pdf"><span>76 FR 1504 - Pipeline Safety: Establishing Maximum Allowable Operating <span class="hlt">Pressure</span> or Maximum Operating <span class="hlt">Pressure</span>...</span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collection.action?collectionCode=FR">Federal Register 2010, 2011, 2012, 2013, 2014</a></p> <p></p> <p>2011-01-10</p> <p>... <span class="hlt">profile</span> that is dependent upon the pipelines attributes, its geographical location, design, operating... type of threats posed by the pipeline segment, including consideration of the age, design, pipe... calculation. There are several methods available for establishing MAOP or MOP. A hydrostatic <span class="hlt">pressure</span> test...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2016AGUFMSM51D2516W','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2016AGUFMSM51D2516W"><span>Field Aligned Currents Derived From <span class="hlt">Pressure</span> <span class="hlt">Profiles</span> Obtained From TWINS ENA Images for Geomagnetic Storms That Occurred On 01 June 2013 and 17 March 2015.</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Wood, K.; Perez, J. D.; Goldstein, J.; McComas, D. J.; Valek, P. W.</p> <p>2016-12-01</p> <p>Field aligned currents (FACs) that flow from the Earth's magnetosphere into the ionosphere are an important coupling mechanism in the interaction of the solar wind with the Earth's magnetosphere and ionosphere. Assuming <span class="hlt">pressure</span> balance and charge conservation yields an expression for the FACs in terms of plasma <span class="hlt">pressure</span> gradients and <span class="hlt">pressure</span> anisotropy. The Two Wide-angle Imaging Neutral Atom Spectrometers (TWINS) mission, the first stereoscopic ENA magnetospheric imager, provides global images of the inner magnetosphere from which ion <span class="hlt">pressure</span> distributions and <span class="hlt">pressure</span> anisotropies are obtained. Following the formulations in Vasyliunas (1970), Vasyliunas (1984), and Heinemann (1990), and using results from TWINS <span class="hlt">observations</span>, we calculate the distributions of field aligned currents for geomagnetic storms on 1 June 2013 and 17 March 2015, in which extended ionospheric precipitation was <span class="hlt">observed</span>. As previous work has assumed isotropic <span class="hlt">pressure</span> distributions, we perform calculations both assuming <span class="hlt">pressure</span> isotropy, and using the <span class="hlt">pressure</span> anisotropy <span class="hlt">observed</span> by TWINS, and compare the results from the two storms. References: 1. Vasyliunas, V. M. (1970). Mathematical Models of Magnetospheric Convection and its Coupling to the Ionosphere. Particles and Fields in the Magnetosphere Astrophysics and Space Science Library, 60-71. doi:10.1007/978-94-010-3284-1_6 2. Vasyliunas, V. M. (1984). Fundamentals of current description. Magnetospheric Currents Geophysical Monograph Series, 63-66. doi:10.1029/gm028p0063 3. Heinemann, M. (1990). Representations of currents and magnetic fields in anisotropic magnetohydrostatic plasma. J. Geophys. Res. Journal of Geophysical Research, 95(A6), 7789. doi:10.1029/ja095ia06p07789</p> </li> </ol> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_16");'>16</a></li> <li><a href="#" onclick='return showDiv("page_17");'>17</a></li> <li class="active"><span>18</span></li> <li><a href="#" onclick='return showDiv("page_19");'>19</a></li> <li><a href="#" onclick='return showDiv("page_20");'>20</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div><!-- col-sm-12 --> </div><!-- row --> </div><!-- page_18 --> <div id="page_19" class="hiddenDiv"> <div class="row"> <div class="col-sm-12"> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_17");'>17</a></li> <li><a href="#" onclick='return showDiv("page_18");'>18</a></li> <li class="active"><span>19</span></li> <li><a href="#" onclick='return showDiv("page_20");'>20</a></li> <li><a href="#" onclick='return showDiv("page_21");'>21</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div> </div> <div class="row"> <div class="col-sm-12"> <ol class="result-class" start="361"> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/25671068','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/25671068"><span>The effect of glutathione S-transferase M1 and T1 polymorphisms on blood <span class="hlt">pressure</span>, blood glucose, and lipid <span class="hlt">profiles</span> following the supplementation of kale (Brassica oleracea acephala) juice in South Korean subclinical hypertensive patients.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Han, Jeong-Hwa; Lee, Hye-Jin; Kim, Tae-Seok; Kang, Myung-Hee</p> <p>2015-02-01</p> <p>Glutathione S-transferase (GST) forms a multigene family of phase II detoxification enzymes which are involved in the detoxification of reactive oxygen species. This study examines whether daily supplementation of kale juice can modulate blood <span class="hlt">pressure</span> (BP), levels of lipid <span class="hlt">profiles</span>, and blood glucose, and whether this modulation could be affected by the GSTM1 and GSTT1 polymorphisms. 84 subclinical hypertensive patients showing systolic BP over 130 mmHg or diastolic BP over 85 mmHg received 300 ml/day of kale juice for 6 weeks, and blood samples were collected on 0-week and 6-week in order to evaluate plasma lipid <span class="hlt">profiles</span> (total cholesterol, triglyceride, HDL-cholesterol, and LDL-cholesterol) and blood glucose. Systolic and diastolic blood <span class="hlt">pressure</span> was significantly decreased in all patients regardless of their GSTM1 or GSTT1 polymorphisms after kale juice supplementation. Blood glucose level was decreased only in the GSTM1-present genotype, and plasma lipid <span class="hlt">profiles</span> showed no difference in both the GSTM1-null and GSTM1-present genotypes. In the case of GSTT1, on the other hand, plasma HDL-C was increased and LDL-C was decreased only in the GSTT1-present type, while blood glucose was decreased only in the GSTT1-null genotype. These findings suggest that the supplementation of kale juice affected blood <span class="hlt">pressure</span>, lipid <span class="hlt">profiles</span>, and blood glucose in subclinical hypertensive patients depending on their GST genetic polymorphisms, and the improvement of lipid <span class="hlt">profiles</span> was mainly greater in the GSTT1-present genotype and the decrease of blood glucose was greater in the GSTM1-present or GSTT1-null genotypes.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=4317480','PMC'); return false;" href="https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=4317480"><span>The effect of glutathione S-transferase M1 and T1 polymorphisms on blood <span class="hlt">pressure</span>, blood glucose, and lipid <span class="hlt">profiles</span> following the supplementation of kale (Brassica oleracea acephala) juice in South Korean subclinical hypertensive patients</span></a></p> <p><a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pmc">PubMed Central</a></p> <p>Han, Jeong-Hwa; Lee, Hye-Jin; Kim, Tae-Seok</p> <p>2015-01-01</p> <p>BACKGROUND/OBJECTIVES Glutathione S-transferase (GST) forms a multigene family of phase II detoxification enzymes which are involved in the detoxification of reactive oxygen species. This study examines whether daily supplementation of kale juice can modulate blood <span class="hlt">pressure</span> (BP), levels of lipid <span class="hlt">profiles</span>, and blood glucose, and whether this modulation could be affected by the GSTM1 and GSTT1 polymorphisms. SUBJECTS/METHODS 84 subclinical hypertensive patients showing systolic BP over 130 mmHg or diastolic BP over 85 mmHg received 300 ml/day of kale juice for 6 weeks, and blood samples were collected on 0-week and 6-week in order to evaluate plasma lipid <span class="hlt">profiles</span> (total cholesterol, triglyceride, HDL-cholesterol, and LDL-cholesterol) and blood glucose. RESULTS Systolic and diastolic blood <span class="hlt">pressure</span> was significantly decreased in all patients regardless of their GSTM1 or GSTT1 polymorphisms after kale juice supplementation. Blood glucose level was decreased only in the GSTM1-present genotype, and plasma lipid <span class="hlt">profiles</span> showed no difference in both the GSTM1-null and GSTM1-present genotypes. In the case of GSTT1, on the other hand, plasma HDL-C was increased and LDL-C was decreased only in the GSTT1-present type, while blood glucose was decreased only in the GSTT1-null genotype. CONCLUSIONS These findings suggest that the supplementation of kale juice affected blood <span class="hlt">pressure</span>, lipid <span class="hlt">profiles</span>, and blood glucose in subclinical hypertensive patients depending on their GST genetic polymorphisms, and the improvement of lipid <span class="hlt">profiles</span> was mainly greater in the GSTT1-present genotype and the decrease of blood glucose was greater in the GSTM1-present or GSTT1-null genotypes. PMID:25671068</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/19740021601','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/19740021601"><span>An occultation satellite system for determining <span class="hlt">pressure</span> levels in the atmosphere</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Morrison, A. R.; Vngar, S. G.; Lusignan, B. B.</p> <p>1974-01-01</p> <p>A two-satellite microwave occultation system is described that will fix, as an absolute function of altitude, the <span class="hlt">pressure</span>-temperature <span class="hlt">profile</span> generated by a passive infrared sounder. The 300 mb <span class="hlt">pressure</span> level is determined to within 24 m rms, assuming the temperture errors produced by the infrared sensor are not greater than 2 K rms. Error caused by water vapor in the radio path is corrected by climatological adjustments. A ground test of the proposed system is described. A microwave signal propagating between two mountain tops was found to be subject to periods of intense fading. Computer analysis of the raypath between the transmitting and receiving stations indicates that multipath and defocusing were responsible for this fading. It is unlikely that an operational <span class="hlt">pressure</span>-reference-level system will be subject to the deep fades <span class="hlt">observed</span> in the ground test, because the phenomena are associated with lower altitudes than the closest approach altitude of an occultation-system raypath.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/27055965','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/27055965"><span>A blend of sesame oil and rice bran oil lowers blood <span class="hlt">pressure</span> and improves the lipid <span class="hlt">profile</span> in mild-to-moderate hypertensive patients.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Devarajan, Sankar; Singh, Ravinder; Chatterjee, Biprabuddha; Zhang, Bo; Ali, Amanat</p> <p>2016-01-01</p> <p>Sesame oil and rice bran oil are known for their unsaturated fatty acids and antioxidants contents and have been reported to reduce the cardiovascular risk. To determine the effect of a blend of 20% unrefined cold-pressed lignans-rich sesame oil and 80% physically refined γ-oryzanol-rich rice bran oil (Vivo) as cooking oil in mild-to-moderate hypertensive patients. In this prospective, open-label dietary approach, 300 hypertensive patients and 100 normotensives were divided into groups as: (1) normotensives treated with sesame oil blend, (2) hypertensives treated with sesame oil blend, (3) hypertensives treated with nifedipine, a calcium channel blocker (20 mg/d), and (4) hypertensives receiving the combination of sesame oil blend and nifedipine (20 mg/d). Sesame oil blend was supplied to respective groups, and they were instructed to use it as the only cooking oil for 60 days. Resting blood <span class="hlt">pressure</span> was measured at days 0, 15, 30, 45, and 60, whereas the fasting lipid <span class="hlt">profile</span> was measured at days 0 and 60. Significant reduction in blood <span class="hlt">pressure</span> (systolic, diastolic, and mean arterial) from days 0 to 15, 30, 45, and 60 were <span class="hlt">observed</span> in hypertensives treated with sesame oil blend alone (P < .001), nifedipine alone (P < .001), and combination of sesame oil blend and nifedipine (P < .001). Sesame oil blend with nifedipine-treated group showed greatest reduction in blood <span class="hlt">pressure</span>. Total cholesterol, low-density lipoprotein cholesterol, triglycerides, and non-high-density lipoprotein cholesterol levels reduced, whereas high-density lipoprotein cholesterol levels increased significantly only in hypertensives treated with sesame oil blend alone and the combination of sesame oil blend and nifedipine (P < .001). We demonstrate for the first time that using a blend of sesame oil and rice bran oil as cooking oil showed a significant antihypertensive and lipid-lowering action and had noteworthy additive effect with antihypertensive medication. Copyright © 2016 National</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017AGUFM.C51B0970C','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017AGUFM.C51B0970C"><span>Ocean Wave-to-Ice Energy Transfer Determined from Seafloor <span class="hlt">Pressure</span> and Ice Shelf Seismic <span class="hlt">Observations</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Chen, Z.; Bromirski, P. D.; Gerstoft, P.; Stephen, R. A.; Wiens, D.; Aster, R. C.; Nyblade, A.</p> <p>2017-12-01</p> <p>Ice shelves play an important role in buttressing land ice from reaching the sea, thus restraining the rate of sea level rise. Long-period gravity wave impacts excite vibrations in ice shelves that may trigger tabular iceberg calving and/or ice shelf collapse events. Three kinds of seismic plate waves were continuously <span class="hlt">observed</span> by broadband seismic arrays on the Ross Ice Shelf (RIS) and on the Pine Island Glacier (PIG) ice shelf: (1) flexural-gravity waves, (2) flexural waves, and (3) extensional Lamb waves, suggesting that all West Antarctic ice shelves are subjected to similar gravity wave excitation. Ocean gravity wave heights were estimated from <span class="hlt">pressure</span> perturbations recorded by an ocean bottom differential <span class="hlt">pressure</span> gauge at the RIS front, water depth 741 m, about 8 km north of an on-ice seismic station that is 2 km from the shelf front. Combining the plate wave spectrum, the frequency-dependent energy transmission and reflection at the ice-water interface were determined. In addition, Young's modulus and Poisson's ratio of the RIS are estimated from the plate wave motions, and compared with the widely used values. Quantifying these ice shelf parameters from <span class="hlt">observations</span> will improve modeling of ice shelf response to ocean forcing, and ice shelf evolution.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017AGUFMMR24A..04L','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017AGUFMMR24A..04L"><span>Elasticity of the Earth's Lower Mantle Minerals at High <span class="hlt">Pressures</span>: Implications to Understanding Seismic <span class="hlt">Observations</span> of the Deep Mantle</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Lin, J. F.; Yang, J.; Fu, S.</p> <p>2017-12-01</p> <p>Elasticity of the candidate lower-mantle minerals at relevant P-T conditions of the region provides critical information in understanding seismic <span class="hlt">profiles</span>, compositional and mineralogical models, and geodynamic processes of the Earth's interior. Here we will discuss recent major research advances in the investigation of the elasticity of major lower-mantle minerals in a high-<span class="hlt">pressure</span> diamond anvil cell coupled with Brillouin Light Scattering, Impulsive Stimulated Scattering (ISS), and X-ray diffraction. These have permitted direct and reliable measurements of both Vp and Vs to derive full elastic constants of single-crystal ferropericlase and (Fe, Al)-bearing bridgmanite as well as velocity <span class="hlt">profiles</span> of polycrystalline silicate post-perovskite at relevant lower-mantle <span class="hlt">pressures</span>. The effects of the spin transition on the single-crystal elasticity of ferropericlase are now well understood experimentally and theoretically1,2: the spin transition causes drastic softening in elastic constants involving the compressive stress component (C11 and C12) due to the additional Gibbs free energy term arising from the mixing of the high-spin and low-spin states, while the elastic constant(s) related to the shear stress component (C44) is not affected. This leads to significant reduction in VP/VS ratio within the spin transition of ferropericlase in the mid-lower mantle. The derived single-crystal Cij of bridgmanite at lower mantle <span class="hlt">pressures</span> display relatively small elastic Vp and Vs anisotropies as compared to the ferropericlase counterpart. Using thermoelastic modelling, we will discuss the application of the elasticity of ferropericlase, bridgmanite, and silicate post-perovskite at relevant conditions of the Earth's lower mantle to differentiate the role of the thermal vs. chemical perturbations as well as the spin transition and iron partitioning effects in the reported seismic lateral heterogeneity in lower mantle as well as the D″ zone region3,4. We will address how recent</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017APS..DFDQ28001L','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017APS..DFDQ28001L"><span>Universality of the logarithmic velocity <span class="hlt">profile</span> restored</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Luchini, Paolo</p> <p>2017-11-01</p> <p>The logarithmic velocity <span class="hlt">profile</span> of wall-bounded turbulent flow, despite its widespread adoption in research and in teaching, exhibits discrepancies with both experiments and numerical simulations that have been repeatedly <span class="hlt">observed</span> in the literature; serious doubts ensued about its precise form and universality, leading to the formulation of alternate theories and hindering ongoing experimental efforts to measure von Kármán's constant. By comparing different geometries of pipe, plane-channel and plane-Couette flow, here we show that such discrepancies can be physically interpreted, and analytically accounted for, through an equally universal higher-order correction caused by the <span class="hlt">pressure</span> gradient. Inclusion of this term produces a tenfold increase in the adherence of the predicted <span class="hlt">profile</span> to existing experiments and numerical simulations in all three geometries. Universality of the logarithmic law then emerges beyond doubt and a satisfactorily simple formulation is established. Among the consequences of this formulation is a strongly increased confidence that the Reynolds number of present-day direct numerical simulations is actually high enough to uncover asymptotic behaviour, but research efforts are still needed in order to increase their accuracy.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/19800010071','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/19800010071"><span>Resonant Doppler velocimeter. Ph.D. Thesis. Final Report, 1 Jul. 1974 - 31 Oct. 1979; [velocity, temperature, and <span class="hlt">pressure</span> measurement</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Zimmermann, M.</p> <p>1980-01-01</p> <p>A technique is presented for visualizing and quantitatively measuring velocity, temperature, and <span class="hlt">pressure</span> by shining a single frequency laser beam into a gaseous flow which is seeded with an atomic species. The laser is tuned through the absorption frequencies of the seeded species and the absorption <span class="hlt">profile</span> is detected by <span class="hlt">observing</span> fluorescence as the atoms relax back to the ground state. The flow velocity is determined by <span class="hlt">observing</span> the Doppler shift in the absorption frequency. Spectroscopic absorption line broadening mechanisms furnish information regarding the static temperature and <span class="hlt">pressure</span> of the moving gas. Results of experiments conducted in the free stream and in the bow shock of a conical model mounted in a hypersonic wind tunnel indicate that the experimental uncertainties in the measurement of average values for the velocity, temperature and <span class="hlt">pressure</span> of the flow are 0.1, 5 and 10 percent respectively.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.osti.gov/pages/biblio/1437155-mean-velocity-profile-smooth-channel-flow-explained-cospectral-budget-model-wall-blockage','SCIGOV-DOEP'); return false;" href="https://www.osti.gov/pages/biblio/1437155-mean-velocity-profile-smooth-channel-flow-explained-cospectral-budget-model-wall-blockage"><span>Mean-velocity <span class="hlt">profile</span> of smooth channel flow explained by a cospectral budget model with wall-blockage</span></a></p> <p><a target="_blank" href="http://www.osti.gov/pages">DOE PAGES</a></p> <p>McColl, Kaighin A.; Katul, Gabriel G.; Gentine, Pierre; ...</p> <p>2016-03-16</p> <p>A series of recent studies has shown that a model of the turbulent vertical velocity variance spectrum (F vv) combined with a simplified cospectral budget can reproduce many macroscopic flow properties of turbulent wall-bounded flows, including various features of the mean-velocity <span class="hlt">profile</span> (MVP), i.e., the "law of the wall". While the approach reasonably models the MVP's logarithmic layer, the buffer layer displays insufficient curvature compared to measurements. The assumptions are re-examined here using a direct numerical simulation (DNS) dataset at moderate Reynolds number that includes all the requisite spectral and co-spectral information. Starting with several hypotheses for the cause ofmore » the "missing" curvature in the buffer layer, it is shown that the curvature deficit is mainly due to mismatches between (i) the modelled and DNS-<span class="hlt">observed</span> <span class="hlt">pressure</span>-strain terms in the cospectral budget and (ii) the DNS-<span class="hlt">observed</span> F vv and the idealized form used in previous models. By replacing the current parameterization for the <span class="hlt">pressure</span>-strain term with an expansive version that directly accounts for wall-blocking effects, the modelled and DNS reported <span class="hlt">pressure</span>-strain <span class="hlt">profiles</span> match each other in the buffer and logarithmic layers. Forcing the new model with DNS-reported F vv rather than the idealized form previously used reproduces the missing buffer layer curvature to high fidelity thereby confirming the "spectral link" between F vv and the MVP across the full <span class="hlt">profile</span>. A broad implication of this work is that much of the macroscopic properties of the flow (such as the MVP) may be derived from the energy distribution in turbulent eddies (i.e., F vv) representing the microstate of the flow, provided the link between them accounts for wall-blocking.« less</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2015CliPa..11.1027B','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2015CliPa..11.1027B"><span>A collection of sub-daily <span class="hlt">pressure</span> and temperature <span class="hlt">observations</span> for the early instrumental period with a focus on the "year without a summer" 1816</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Brugnara, Y.; Auchmann, R.; Brönnimann, S.; Allan, R. J.; Auer, I.; Barriendos, M.; Bergström, H.; Bhend, J.; Brázdil, R.; Compo, G. P.; Cornes, R. C.; Dominguez-Castro, F.; van Engelen, A. F. V.; Filipiak, J.; Holopainen, J.; Jourdain, S.; Kunz, M.; Luterbacher, J.; Maugeri, M.; Mercalli, L.; Moberg, A.; Mock, C. J.; Pichard, G.; Řezníčková, L.; van der Schrier, G.; Slonosky, V.; Ustrnul, Z.; Valente, M. A.; Wypych, A.; Yin, X.</p> <p>2015-08-01</p> <p>The eruption of Mount Tambora (Indonesia) in April 1815 is the largest documented volcanic eruption in history. It is associated with a large global cooling during the following year, felt particularly in parts of Europe and North America, where the year 1816 became known as the "year without a summer". This paper describes an effort made to collect surface meteorological <span class="hlt">observations</span> from the early instrumental period, with a focus on the years of and immediately following the eruption (1815-1817). Although the collection aimed in particular at <span class="hlt">pressure</span> <span class="hlt">observations</span>, correspondent temperature <span class="hlt">observations</span> were also recovered. Some of the series had already been described in the literature, but a large part of the data, recently digitised from original weather diaries and contemporary magazines and newspapers, is presented here for the first time. The collection puts together more than 50 sub-daily series from land observatories in Europe and North America and from ships in the tropics. The <span class="hlt">pressure</span> <span class="hlt">observations</span> have been corrected for temperature and gravity and reduced to mean sea level. Moreover, an additional statistical correction was applied to take into account common error sources in mercury barometers. To assess the reliability of the corrected data set, the variance in the <span class="hlt">pressure</span> <span class="hlt">observations</span> is compared with modern climatologies, and single <span class="hlt">observations</span> are used for synoptic analyses of three case studies in Europe. All raw <span class="hlt">observations</span> will be made available to the scientific community in the International Surface <span class="hlt">Pressure</span> Databank.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/20120015537','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/20120015537"><span>Integrating Wind <span class="hlt">Profiling</span> Radars and Radiosonde <span class="hlt">Observations</span> with Model Point Data to Develop a Decision Support Tool to Assess Upper-Level Winds for Space Launch</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Bauman, William H., III; Flinn, Clay</p> <p>2013-01-01</p> <p>On the day-of-launch, the 45th Weather Squadron (45 WS) Launch Weather Officers (LWOs) monitor the upper-level winds for their launch customers to include NASA's Launch Services Program and NASA's Ground Systems Development and Operations Program. They currently do not have the capability to display and overlay <span class="hlt">profiles</span> of upper-level <span class="hlt">observations</span> and numerical weather prediction model forecasts. The LWOs requested the Applied Meteorology Unit (AMU) develop a tool in the form of a graphical user interface (GUI) that will allow them to plot upper-level wind speed and direction <span class="hlt">observations</span> from the Kennedy Space Center (KSC) 50 MHz tropospheric wind <span class="hlt">profiling</span> radar, KSC Shuttle Landing Facility 915 MHz boundary layer wind <span class="hlt">profiling</span> radar and Cape Canaveral Air Force Station (CCAFS) Automated Meteorological Processing System (AMPS) radiosondes, and then overlay forecast wind <span class="hlt">profiles</span> from the model point data including the North American Mesoscale (NAM) model, Rapid Refresh (RAP) model and Global Forecast System (GFS) model to assess the performance of these models. The AMU developed an Excel-based tool that provides an objective method for the LWOs to compare the model-forecast upper-level winds to the KSC wind <span class="hlt">profiling</span> radars and CCAFS AMPS <span class="hlt">observations</span> to assess the model potential to accurately forecast changes in the upperlevel <span class="hlt">profile</span> through the launch count. The AMU wrote Excel Visual Basic for Applications (VBA) scripts to automatically retrieve model point data for CCAFS (XMR) from the Iowa State University Archive Data Server (http://mtarchive.qeol.iastate.edu) and the 50 MHz, 915 MHz and AMPS <span class="hlt">observations</span> from the NASA/KSC Spaceport Weather Data Archive web site (http://trmm.ksc.nasa.gov). The AMU then developed code in Excel VBA to automatically ingest and format the <span class="hlt">observations</span> and model point data in Excel to ready the data for generating Excel charts for the LWO's. The resulting charts allow the LWOs to independently initialize the three models 0</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/29219620','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/29219620"><span>A common humoral background of intraocular and arterial blood <span class="hlt">pressure</span> dysregulation.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Skrzypecki, Janusz; Grabska-Liberek, Iwona; Przybek, Joanna; Ufnal, Marcin</p> <p>2018-03-01</p> <p>It has been postulated that intraocular <span class="hlt">pressure</span>, an important glaucoma risk factor, correlates positively with arterial blood <span class="hlt">pressure</span> (blood <span class="hlt">pressure</span>). However, results of experimental and clinical studies are often contradictory. It is hypothesized that, in some hypertensive patients, disturbances in intraocular <span class="hlt">pressure</span> regulation may depend on biological effects of blood borne hormones underlying a particular type of hypertension, rather than on blood <span class="hlt">pressure</span> level itself. This review compares the effects of hormones on blood <span class="hlt">pressure</span> and intraocular <span class="hlt">pressure</span>, in order to identify a hormonal <span class="hlt">profile</span> of hypertensive patients with an increased risk of intraocular <span class="hlt">pressure</span> surge. The PUBMED database was searched to identify pre-clinical and clinical studies investigating the role of angiotensin II, vasopressin, adrenaline, noradrenaline, prostaglandins, and gaseous transmitters in the regulation of blood <span class="hlt">pressure</span> and intraocular <span class="hlt">pressure</span>. Studies included in the review suggest that intraocular and blood <span class="hlt">pressures</span> often follow a different pattern of response to the same hormone. For example, vasopressin increases blood <span class="hlt">pressure</span>, but decreases intraocular <span class="hlt">pressure</span>. In contrast, high level of nitric oxide decreases blood <span class="hlt">pressure</span>, but increases intraocular <span class="hlt">pressure</span>. Arterial hypertension is associated with altered levels of blood borne hormones. Contradicting results of studies on the relationship between arterial hypertension and intraocular <span class="hlt">pressure</span> might be partially explained by diverse effects of hormones on arterial and intraocular <span class="hlt">pressures</span>. Further studies are needed to evaluate if hormonal <span class="hlt">profiling</span> may help to identify glaucoma-prone patients.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://ntrs.nasa.gov/search.jsp?R=19780058272&hterms=MOOS&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D80%26Ntt%3DMOOS','NASA-TRS'); return false;" href="https://ntrs.nasa.gov/search.jsp?R=19780058272&hterms=MOOS&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D80%26Ntt%3DMOOS"><span>Ultraviolet <span class="hlt">observations</span> of cool stars. VI - L alpha and Mg II emission line <span class="hlt">profiles</span> /and a search for flux variability/ in Arcturus</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Mcclintock, W.; Moos, H. W.; Henry, R. C.; Linsky, J. L.; Barker, E. S.</p> <p>1978-01-01</p> <p>High-precision, high-resolution <span class="hlt">profiles</span> of the L alpha and Mg II k chromospheric emission lines from Arcturus (alpha Boo) obtained with the Princeton Experimental Package aboard the Copernicus satellite are presented. Asymmetries seen in the <span class="hlt">profiles</span> of these lines are probably intrinsic to the star, rather than the result of interstellar absorption. In contrast to previous <span class="hlt">observations</span> of the Ca II K emission line, no evidence is found during a three-year period for variability in the <span class="hlt">profiles</span> or in the total fluxes from these lines on time scales ranging from hours to months. Also presented is a flux <span class="hlt">profile</span> of the O I 1302 line and flux upper limits for L beta, O VI 1032, Si III 1206, and O V 1218.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2014hitr.confE..38T','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2014hitr.confE..38T"><span>Recommended Isolated-Line <span class="hlt">Profile</span> for Representing High-Resolution Spectroscoscopic Transitions</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Tennyson, J.; Bernath, P. F.; Campargue, A.; Császár, A. G.; Daumont, L.; Gamache, R. R.; Hodges, J. T.; Lisak, D.; Naumenko, O. V.; Rothman, L. S.; Tran, H.; Hartmann, J.-M.; Zobov, N. F.; Buldyreva, J.; Boone, C. D.; De Vizia, M. Domenica; Gianfrani, L.; McPheat, R.; Weidmann, D.; Murray, J.; Ngo, N. H.; Polyansky, O. L.</p> <p>2014-06-01</p> <p>Recommendations of an IUPAC Task Group, formed in 2011 on "Intensities and line shapes in high-resolution spectra of water isotopologues from experiment and theory" (Project No. 2011-022-2-100), on line <span class="hlt">profiles</span> of isolated high-resolution rotational-vibrational transitions perturbed by neutral gas-phase molecules are presented. The well-documented inadequacies of the Voigt <span class="hlt">profile</span>, used almost universally by databases and radiative-transfer codes to represent <span class="hlt">pressure</span> effects and Doppler broadening in isolated vibrational-rotational and pure rotational transitions of the water molecule, have resulted in the development of a variety of alternative line <span class="hlt">profile</span> models. These models capture more of the physics of the influence of <span class="hlt">pressure</span> on line shapes but, in general, at the price of greater complexity. The Task Group recommends that the partially-Correlated quadratic-Speed-Dependent Hard-Collision <span class="hlt">profile</span> should be adopted as the appropriate model for high-resolution spectroscopy. For simplicity this should be called the Hartmann-Tran <span class="hlt">profile</span> (HTP). This <span class="hlt">profile</span> is sophisticated enough to capture the various collisional contributions to the isolated line shape, can be computed in a straightforward and rapid manner, and reduces to simpler <span class="hlt">profiles</span>, including the Voigt <span class="hlt">profile</span>, under certain simplifying assumptions. For further details see: J. Tennyson et al, Pure Appl. Chem., 2014, in press.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2007APS..DPPTP8112B','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2007APS..DPPTP8112B"><span>Initial Edge Stability <span class="hlt">Observations</span> in the PEGASUS Toroidal Experiment</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Bongard, M. W.; Battaglia, D. J.; Garstka, G. D.; Sontag, A. C.; Unterberg, E. A.</p> <p>2007-11-01</p> <p>Edge stability is an important consideration for design of fusion experiments, as transient heat loads generated by edge instabilities may damage the first wall. Such instabilities are now believed to include peeling (current driven) and ballooning (<span class="hlt">pressure</span> driven) components. Peeling instability may be expected for high values of edge j||/B and low edge <span class="hlt">pressure</span> gradient. This matches the operating space of Pegasus, with typical <j||/B> ˜100 kA/m^2, |B|˜ 0.01 T, and an L-mode edge. A new camera system has <span class="hlt">observed</span> filamentary structures in the edge of nearly all ohmically-heated discharges. Ideal stability analysis of these discharges with DCON indicates marginal stability to resistive interchange for ψN>= 0.95. Modification of triangularity during startup is <span class="hlt">observed</span> to delay instability onset. A plasma control system based on that used on DIII-D will allow study of the influence of plasma shaping on mode stability characteristics. An array of magnetic probes capable of insertion into the scrape-off layer and plasma edge is being developed to provide a local constraint on the edge current <span class="hlt">profile</span>.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/27324326','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/27324326"><span>Pneumoperitoneum deteriorates intratidal respiratory system mechanics: an <span class="hlt">observational</span> study in lung-healthy patients.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Wirth, Steffen; Biesemann, Andreas; Spaeth, Johannes; Schumann, Stefan</p> <p>2017-02-01</p> <p>Pneumoperitoneum during laparoscopic surgery leads to atelectasis and impairment of oxygenation. Positive end-expiratory <span class="hlt">pressure</span> (PEEP) is supposed to counteract atelectasis. We hypothesized that the derecruiting effects of pneumoperitoneum would deteriorate the intratidal compliance <span class="hlt">profile</span> in patients undergoing laparoscopic surgery. In 30 adult patients scheduled for surgery with pneumoperitoneum, respiratory variables were measured during mechanical ventilation. We calculated the dynamic compliance of the respiratory system (C RS ) and the intratidal volume-dependent C RS curve using the gliding-SLICE method. The C RS curve was then classified in terms of indicating intratidal recruitment/derecruitment (increasing <span class="hlt">profile</span>) and overdistension (decreasing <span class="hlt">profile</span>). During the surgical interventions, the PEEP level was maintained nearly constant at 7 cm H 2 O. Data are expressed as mean [confidence interval]. Baseline C RS was 60 [54-67] mL cm H 2 O -1 . Application of pneumoperitoneum decreased C RS to 40 [37-43] mL cm H 2 O -1 which partially recovered to 54 [50-59] mL cm H 2 O -1 (P < 0.001) after removal but remained below the value measured before pneumoperitoneum (P < 0.001). Baseline compliance <span class="hlt">profiles</span> indicated intratidal recruitment/derecruitment in 48 % patients. After induction of pneumoperitoneum, intratidal recruitment/derecruitment was indicated in 93 % patients (P < 0.01), and after removal intratidal recruitment/derecruitment was indicated in 59 % patients. Compliance <span class="hlt">profiles</span> showing overdistension were not <span class="hlt">observed</span>. Analyses of the intratidal compliance <span class="hlt">profiles</span> reveal that pneumoperitoneum during laparoscopic surgery causes intratidal recruitment/derecruitment which partly persists after its removal. The analysis of the intratidal volume-dependent C RS <span class="hlt">profiles</span> could be used to guide intraoperative PEEP adjustments during elevated intraabdominal <span class="hlt">pressure</span>.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017ApJ...844..156R','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017ApJ...844..156R"><span>From Neutron Star <span class="hlt">Observables</span> to the Equation of State. II. Bayesian Inference of Equation of State <span class="hlt">Pressures</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Raithel, Carolyn A.; Özel, Feryal; Psaltis, Dimitrios</p> <p>2017-08-01</p> <p>One of the key goals of <span class="hlt">observing</span> neutron stars is to infer the equation of state (EoS) of the cold, ultradense matter in their interiors. Here, we present a Bayesian statistical method of inferring the <span class="hlt">pressures</span> at five fixed densities, from a sample of mock neutron star masses and radii. We show that while five polytropic segments are needed for maximum flexibility in the absence of any prior knowledge of the EoS, regularizers are also necessary to ensure that simple underlying EoS are not over-parameterized. For ideal data with small measurement uncertainties, we show that the <span class="hlt">pressure</span> at roughly twice the nuclear saturation density, {ρ }{sat}, can be inferred to within 0.3 dex for many realizations of potential sources of uncertainties. The <span class="hlt">pressures</span> of more complicated EoS with significant phase transitions can also be inferred to within ˜30%. We also find that marginalizing the multi-dimensional parameter space of <span class="hlt">pressure</span> to infer a mass-radius relation can lead to biases of nearly 1 km in radius, toward larger radii. Using the full, five-dimensional posterior likelihoods avoids this bias.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2005AGUFMMR33B..02S','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2005AGUFMMR33B..02S"><span>High-<span class="hlt">pressure</span> phases transitions in SnO2 to 117 GPa: Implications for silica</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Shieh, S. R.; Kubo, A.; Duffy, T. S.; Prakapenka, V. B.; Shen, G.</p> <p>2005-12-01</p> <p>Cassiterite (SnO2) is regarded to be a good analog material for silica as both SnO2 and SiO2 are group IV-B metal dioxides. The high-<span class="hlt">pressure</span> behavior of SnO2 has been the subject of many previous investigations extending up to 49 GPa and in addition to the rutile structure, three high-<span class="hlt">pressure</span> phases, CaCl2-type, α-PbO2-type, and pyrite-type were <span class="hlt">observed</span>. Better knowledge of high-<span class="hlt">pressure</span> phases of SnO2 will be useful to understand the behavior of silica at deep mantle conditions. In addition, high-<span class="hlt">pressure</span> metal dioxide phases may qualify as superhard solids. Our study will also provide insights into interpretation of shock compression data. Pure natural cassiterite (SnO2) powder was compressed in a diamond anvil cell using an argon medium. <span class="hlt">Pressure</span> was determined from the equation of state of platinum. In situ monochromatic x-ray diffraction at high <span class="hlt">pressure</span> was carried out at the GSECARS, Advanced Photon Source. High temperatures were achieved using double-sided laser heating . Three heating cycles were conducted with total heating times up to 30 minutes. Our diffraction results on SnO2 demonstrate the existence of four phase transitions to 117 GPa. The <span class="hlt">observed</span> sequence of high-<span class="hlt">pressure</span> phases for SnO2 is rutile-type, CaCl2-type, pyrite-type, ZrO2 orthorhombic phase I (Pbca), cotunnite-type. Our <span class="hlt">observations</span> of the first three phases are generally in agreement with earlier studies. The orthorhombic phase I and cotunnite-type structures were <span class="hlt">observed</span> in SnO2 for the first time. The Pbca phase is found at 50-74 GPa during room-temperature compression. The cotunnite-type structure was synthesized when SnO2 was heated at 74 GPa and 1200 K. The cotunnite-type form was <span class="hlt">observed</span> during compression between 54-117 GPa. Fitting the <span class="hlt">pressure</span>-volume data for the high-<span class="hlt">pressure</span> phases to the second-order Birch-Murnaghan equation of state yields a bulk modulus of 259(26) GPa for the Pbca phase and 417(7) GPa for the cotunnite-type phase. Rietveld <span class="hlt">profile</span> refinements were</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2018AMT....11.1669S','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2018AMT....11.1669S"><span>High-resolution humidity <span class="hlt">profiles</span> retrieved from wind <span class="hlt">profiler</span> radar measurements</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Saïd, Frédérique; Campistron, Bernard; Di Girolamo, Paolo</p> <p>2018-03-01</p> <p>The retrieval of humidity <span class="hlt">profiles</span> from wind <span class="hlt">profiler</span> radars has already been documented in the past 30 years and is known to be neither as straightforward and nor as robust as the retrieval of the wind velocity. The main constraint to retrieve the humidity <span class="hlt">profile</span> is the necessity to combine measurements from the wind <span class="hlt">profiler</span> and additional measurements (such as <span class="hlt">observations</span> from radiosoundings at a coarser time resolution). Furthermore, the method relies on some assumptions and simplifications that restrict the scope of its application. The first objective of this paper is to identify the obstacles and limitations and solve them, or at least define the field of applicability. To improve the method, we propose using the radar capacity to detect transition levels, such as the top level of the boundary layer, marked by a maximum in the radar reflectivity. This forces the humidity <span class="hlt">profile</span> from the free troposphere and from the boundary layer to coincide at this level, after an optimization of the calibration coefficients, and reduces the error. The resulting mean bias affecting the specific humidity <span class="hlt">profile</span> never exceeds 0.25 g kg-1. The second objective is to explore the capability of the algorithm to retrieve the humidity vertical <span class="hlt">profiles</span> for an operational purpose by comparing the results with <span class="hlt">observations</span> from a Raman lidar.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/20150002878','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/20150002878"><span>Development of a Climatology of Vertically Complete Wind <span class="hlt">Profiles</span> from Doppler Radar Wind <span class="hlt">Profiler</span> Systems</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Barbre, Robert, Jr.</p> <p>2015-01-01</p> <p>Assessment of space vehicle loads and trajectories during design requires a large sample of wind <span class="hlt">profiles</span> at the altitudes where winds affect the vehicle. Traditionally, this altitude region extends from near 8-14 km to address maximum dynamic <span class="hlt">pressure</span> upon ascent into space, but some applications require knowledge of measured wind <span class="hlt">profiles</span> at lower altitudes. Such applications include crew capsule pad abort and plume damage analyses. Two Doppler Radar Wind <span class="hlt">Profiler</span> (DRWP) systems exist at the United States Air Force (USAF) Eastern Range and at the National Aeronautics and Space Administration's Kennedy Space Center. The 50-MHz DRWP provides wind <span class="hlt">profiles</span> every 3-5 minutes from roughly 2.5-18.5 km, and five 915-MHz DRWPs provide wind <span class="hlt">profiles</span> every 15 minutes from approximately 0.2-3.0 km. Archived wind <span class="hlt">profiles</span> from all systems underwent rigorous quality control (QC) processes, and concurrent measurements from the QC'ed 50- and 915-MHz DRWP archives were spliced into individual <span class="hlt">profiles</span> that extend from about 0.2-18.5 km. The archive contains combined <span class="hlt">profiles</span> from April 2000 to December 2009, and thousands of <span class="hlt">profiles</span> during each month are available for use by the launch vehicle community. This paper presents the details of the QC and splice methodology, as well as some attributes of the archive.</p> </li> </ol> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_17");'>17</a></li> <li><a href="#" onclick='return showDiv("page_18");'>18</a></li> <li class="active"><span>19</span></li> <li><a href="#" onclick='return showDiv("page_20");'>20</a></li> <li><a href="#" onclick='return showDiv("page_21");'>21</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div><!-- col-sm-12 --> </div><!-- row --> </div><!-- page_19 --> <div id="page_20" class="hiddenDiv"> <div class="row"> <div class="col-sm-12"> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_18");'>18</a></li> <li><a href="#" onclick='return showDiv("page_19");'>19</a></li> <li class="active"><span>20</span></li> <li><a href="#" onclick='return showDiv("page_21");'>21</a></li> <li><a href="#" onclick='return showDiv("page_22");'>22</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div> </div> <div class="row"> <div class="col-sm-12"> <ol class="result-class" start="381"> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2012AGUFMOS31F1780V','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2012AGUFMOS31F1780V"><span>A Self-Powered Fast-Sampling <span class="hlt">Profiling</span> Float in support of a Mesoscale Ocean <span class="hlt">Observing</span> System in the Western North Pacific</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Valdez, T.; Chao, Y.; Davis, R. E.; Jones, J.</p> <p>2012-12-01</p> <p>This talk will describe a new self-powered <span class="hlt">profiling</span> float that can perform fast sampling over the upper ocean for long durations in support of a mesoscale ocean <span class="hlt">observing</span> system in the Western North Pacific. The current state-of-the-art <span class="hlt">profiling</span> floats can provide several hundreds <span class="hlt">profiles</span> for the upper ocean every ten days. To quantify the role of the upper ocean in modulating the development of Typhoons requires at least an order of magnitude reduction for the sampling interval. With today's <span class="hlt">profiling</span> float and battery technology, a fast sampling of one day or even a few hours will reduce the typical lifetime of <span class="hlt">profiling</span> floats from years to months. Interactions between the ocean and typhoons often involves mesoscale eddies and fronts, which require a dense array of floats to reveal the 3-dimensional structure. To measure the mesoscale ocean over a large area like the Western North Pacific therefore requires a new technology that enables fast sampling and long duration at the same time. Harvesting the ocean renewable energy associated with the vertical temperature differentials has the potential to power <span class="hlt">profiling</span> floats with fast sampling over long durations. Results from the development and deployment of a prototype self-powered <span class="hlt">profiling</span> float (known as SOLO-TREC) will be presented. With eight hours sampling in the upper 500 meters, the upper ocean temperature and salinity reveal pronounced high frequency variations. Plans to use the SOLO-TREC technology in support of a dense array of fast sampling <span class="hlt">profiling</span> floats in the Western North Pacific will be discussed.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://ntrs.nasa.gov/search.jsp?R=19850040016&hterms=sensors+pressure&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D90%26Ntt%3Dsensors%2Bpressure','NASA-TRS'); return false;" href="https://ntrs.nasa.gov/search.jsp?R=19850040016&hterms=sensors+pressure&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D90%26Ntt%3Dsensors%2Bpressure"><span>Radiosonde <span class="hlt">pressure</span> sensor performance - Evaluation using tracking radars</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Parsons, C. L.; Norcross, G. A.; Brooks, R. L.</p> <p>1984-01-01</p> <p>The standard balloon-borne radiosonde employed for synoptic meteorology provides vertical <span class="hlt">profiles</span> of temperature, <span class="hlt">pressure</span>, and humidity as a function of elapsed time. These parameters are used in the hypsometric equation to calculate the geopotential altitude at each sampling point during the balloon's flight. It is important that the vertical location information be accurate. The present investigation was conducted with the objective to evaluate the altitude determination accuracy of the standard radiosonde throughout the entire balloon <span class="hlt">profile</span>. The tests included two other commercially available <span class="hlt">pressure</span> sensors to see if they could provide improved accuracy in the stratosphere. The <span class="hlt">pressure</span>-measuring performance of standard baroswitches, premium baroswitches, and hypsometers in balloon-borne sondes was correlated with tracking radars. It was found that the standard and premium baroswitches perform well up to about 25 km altitude, while hypsometers provide more reliable data above 25 km.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://ntrs.nasa.gov/search.jsp?R=20020022192&hterms=balance+sheet&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D60%26Ntt%3Dbalance%2Bsheet','NASA-TRS'); return false;" href="https://ntrs.nasa.gov/search.jsp?R=20020022192&hterms=balance+sheet&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D60%26Ntt%3Dbalance%2Bsheet"><span>Relation Between <span class="hlt">Pressure</span> Balance Structures and Polar Plumes from Ulysses High Latitude <span class="hlt">Observations</span></span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Yamauchi, Y.; Suess, Steven T.; Sakurai, T.; Whitaker, Ann F. (Technical Monitor)</p> <p>2001-01-01</p> <p>Ulysses <span class="hlt">observations</span> have shown that <span class="hlt">pressure</span> balance structures (PBSs) are a common feature in high-latitude, fast solar wind near solar minimum. Previous studies of Ulysses/SWOOPS plasma data suggest these PBSs may be remnants of coronal polar plumes. Here we find support for this suggestion in an analysis of PBS magnetic structure. We used Ulysses magnetometer data and applied a minimum variance analysis to discontinuities. We found that PBSs preferentially contain tangential discontinuities, as opposed to rotational discontinuities and to non-PBS regions in the solar wind. This suggests that PBSs contain structures like current sheets or plasmoids that may be associated with network activity at the base of plumes.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/27723794','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/27723794"><span>The Intracranial Volume <span class="hlt">Pressure</span> Response in Increased Intracranial <span class="hlt">Pressure</span> Patients: Clinical Significance of the Volume <span class="hlt">Pressure</span> Indicator.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Lai, Hung-Yi; Lee, Ching-Hsin; Lee, Ching-Yi</p> <p>2016-01-01</p> <p>For patients suffering from primary brain injury, monitoring intracranial <span class="hlt">pressure</span> alone is not enough to reflect the dynamic intracranial condition. In our previous study, a segment of the <span class="hlt">pressure</span>-volume curve can be expressed by the parabolic regression model with single indicator "a". The aim of this study is to evaluate if the indicator "a" can reflect intracranial conditions. Patients with traumatic brain injury, spontaneous intracranial hemorrhage, and/or hydrocephalus who had external ventricular drainage from January 2009 to February 2010 were included. The successive volume <span class="hlt">pressure</span> response values were obtained by successive drainage of cerebral spinal fluid from intracranial <span class="hlt">pressure</span> 20-25 mm Hg to 10 mm Hg. The relationship between withdrawn cerebral spinal fluid volume and intracranial <span class="hlt">pressure</span> was analyzed by the parabolic regression model with single parameter "a". The overall mean for indicator "a" was 0.422 ± 0.046. The mean of "a" in hydrocephalus was 0.173 ± 0.024 and in severe intracranial mass with slender ventricle, it was 0.663 ± 0.062. The two extreme intracranial conditions had a statistical significant difference (p<0.001). The indicator "a" of a <span class="hlt">pressure</span>-volume curve can reflect the dynamic intracranial condition and is comparable in different situations. A significantly larger indicator "a" with increased intracranial <span class="hlt">pressure</span> is always <span class="hlt">observed</span> in severe intracranial mass lesions with cerebral edema. A significantly smaller indicator "a" with increased intracranial <span class="hlt">pressure</span> is <span class="hlt">observed</span> in hydrocephalus. Brain computed tomography should be performed early if a rapid elevation of indicator "a" is detected, as it can reveal some ongoing intracranial pathology prior to clinical deterioration. Increased intracranial <span class="hlt">pressure</span> was frequently <span class="hlt">observed</span> in patients with intracranial pathology. The progression can be differentiated using the pattern of the volume <span class="hlt">pressure</span> indicator.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=5056694','PMC'); return false;" href="https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=5056694"><span>The Intracranial Volume <span class="hlt">Pressure</span> Response in Increased Intracranial <span class="hlt">Pressure</span> Patients: Clinical Significance of the Volume <span class="hlt">Pressure</span> Indicator</span></a></p> <p><a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pmc">PubMed Central</a></p> <p></p> <p>2016-01-01</p> <p>Background For patients suffering from primary brain injury, monitoring intracranial <span class="hlt">pressure</span> alone is not enough to reflect the dynamic intracranial condition. In our previous study, a segment of the <span class="hlt">pressure</span>-volume curve can be expressed by the parabolic regression model with single indicator “a”. The aim of this study is to evaluate if the indicator “a” can reflect intracranial conditions. Methods Patients with traumatic brain injury, spontaneous intracranial hemorrhage, and/or hydrocephalus who had external ventricular drainage from January 2009 to February 2010 were included. The successive volume <span class="hlt">pressure</span> response values were obtained by successive drainage of cerebral spinal fluid from intracranial <span class="hlt">pressure</span> 20–25 mm Hg to 10 mm Hg. The relationship between withdrawn cerebral spinal fluid volume and intracranial <span class="hlt">pressure</span> was analyzed by the parabolic regression model with single parameter “a”. Results The overall mean for indicator “a” was 0.422 ± 0.046. The mean of “a” in hydrocephalus was 0.173 ± 0.024 and in severe intracranial mass with slender ventricle, it was 0.663 ± 0.062. The two extreme intracranial conditions had a statistical significant difference (p<0.001). Conclusion The indicator “a” of a <span class="hlt">pressure</span>-volume curve can reflect the dynamic intracranial condition and is comparable in different situations. A significantly larger indicator “a” with increased intracranial <span class="hlt">pressure</span> is always <span class="hlt">observed</span> in severe intracranial mass lesions with cerebral edema. A significantly smaller indicator “a” with increased intracranial <span class="hlt">pressure</span> is <span class="hlt">observed</span> in hydrocephalus. Brain computed tomography should be performed early if a rapid elevation of indicator “a” is detected, as it can reveal some ongoing intracranial pathology prior to clinical deterioration. Increased intracranial <span class="hlt">pressure</span> was frequently <span class="hlt">observed</span> in patients with intracranial pathology. The progression can be differentiated using the pattern of the volume</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017ApJ...851..108R','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017ApJ...851..108R"><span><span class="hlt">Observations</span> of the Coronal Mass Ejection with a Complex Acceleration <span class="hlt">Profile</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Reva, A. A.; Kirichenko, A. S.; Ulyanov, A. S.; Kuzin, S. V.</p> <p>2017-12-01</p> <p>We study the coronal mass ejection (CME) with a complex acceleration <span class="hlt">profile</span>. The event occurred on 2009 April 23. It had an impulsive acceleration phase, an impulsive deceleration phase, and a second impulsive acceleration phase. During its evolution, the CME showed signatures of different acceleration mechanisms: kink instability, prominence drainage, flare reconnection, and a CME–CME collision. The special feature of the <span class="hlt">observations</span> is the usage of the TESIS EUV telescope. The instrument could image the solar corona in the Fe 171 Å line up to a distance of 2 {R}ȯ from the center of the Sun. This allows us to trace the CME up to the LASCO/C2 field of view without losing the CME from sight. The onset of the CME was caused by kink instability. The mass drainage occurred after the kink instability. The mass drainage played only an auxiliary role: it decreased the CME mass, which helped to accelerate the CME. The first impulsive acceleration phase was caused by the flare reconnection. We <span class="hlt">observed</span> the two-ribbon flare and an increase of the soft X-ray flux during the first impulsive acceleration phase. The impulsive deceleration and the second impulsive acceleration phases were caused by the CME–CME collision. The studied event shows that CMEs are complex phenomena that cannot be explained with only one acceleration mechanism. We should seek a combination of different mechanisms that accelerate CMEs at different stages of their evolution.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.osti.gov/biblio/5029483-observational-study-nightside-ionospheres-mars-venus-radio-occultation-methods','SCIGOV-STC'); return false;" href="https://www.osti.gov/biblio/5029483-observational-study-nightside-ionospheres-mars-venus-radio-occultation-methods"><span>An <span class="hlt">observational</span> study of the nightside ionospheres of Mars and Venus with radio occultation methods</span></a></p> <p><a target="_blank" href="http://www.osti.gov/search">DOE Office of Scientific and Technical Information (OSTI.GOV)</a></p> <p>Zhang, M.H.G.; Luhmann, J.G.; Kliore, A.J.</p> <p>1990-10-01</p> <p>An analysis of Mars and Venus nightside electron density <span class="hlt">profiles</span> obtained with radio occultation methods shows how the nightside ionospheres of both planets vary with solar zenith angle. From previous studies it is known that the dayside peak electron densities at Mars and Venus show a basic similarity in that they both exhibit Chapman layer-like behavior. In contrast, the peak altitudes at mars behave like an ideal Chapman layer on the dayside, whereas the altitude of the peak at Venus is fairly constant up to the terminator. The effect of major dust storms can also be seen in the peakmore » altitudes at Mars. All Venus nightside electron density <span class="hlt">profiles</span> show a distinct main peak for both solar minimum and maximum, whereas many <span class="hlt">profiles</span> from the nightside of Mars do not show any peak at all. This suggests that the electron density in the Mars nightside ionosphere is frequently too low to be detected by radio occultation. On the Pioneer Venus orbiter, disappearing ionospheres were <span class="hlt">observed</span> near solar maximum in the in-situ data when the solar wind dynamic <span class="hlt">pressure</span> was exceptionally high. This condition occurs because the high solar wind dynamic <span class="hlt">pressure</span> decreases the altitude of the ionopause near the terminator below {approximately}250 km, thus reducing the normal nightward transport of dayside ionospheric plasma. On the basis of the Venus <span class="hlt">observations</span>, one might predict that if a positive correlation of nightside peak density with dynamic <span class="hlt">pressure</span> was found, it could mean that transport from the dayside is the only significant source for the nightside ionosphere of Mars. The lack of a correlation would imply that the precipitation source at Mars is quite variable.« less</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/20040171164','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/20040171164"><span>Version 8 SBUV Ozone <span class="hlt">Profile</span> Trends Compared with Trends from a Zonally Averaged Chemical Model</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Rosenfield, Joan E.; Frith, Stacey; Stolarski, Richard</p> <p>2004-01-01</p> <p>Linear regression trends for the years 1979-2003 were computed using the new Version 8 merged Solar Backscatter Ultraviolet (SBUV) data set of ozone <span class="hlt">profiles</span>. These trends were compared to trends computed using ozone <span class="hlt">profiles</span> from the Goddard Space Flight Center (GSFC) zonally averaged coupled model. <span class="hlt">Observed</span> and modeled annual trends between 50 N and 50 S were a maximum in the higher latitudes of the upper stratosphere, with southern hemisphere (SH) trends greater than northern hemisphere (NH) trends. The <span class="hlt">observed</span> upper stratospheric maximum annual trend is -5.5 +/- 0.9 % per decade (1 sigma) at 47.5 S and -3.8 +/- 0.5 % per decade at 47.5 N, to be compared with the modeled trends of -4.5 +/- 0.3 % per decade in the SH and -4.0 +/- 0.2% per decade in the NH. Both <span class="hlt">observed</span> and modeled trends are most negative in winter and least negative in summer, although the modeled seasonal difference is less than <span class="hlt">observed</span>. Model trends are shown to be greatest in winter due to a repartitioning of chlorine species and the increasing abundance of chlorine with time. The model results show that trend differences can occur depending on whether ozone <span class="hlt">profiles</span> are in mixing ratio or number density coordinates, and on whether they are recorded on <span class="hlt">pressure</span> or altitude levels.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/28539251','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/28539251"><span>Anabolic hormone <span class="hlt">profiles</span> in elite military men: Robust associations with age, stress, and fatigue.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Taylor, Marcus K; Padilla, Genieleah A; Hernández, Lisa M</p> <p>2017-08-01</p> <p>We recently established stable daily <span class="hlt">profiles</span> of the anabolic hormones dehydroepiandrosterone (DHEA) and testosterone in 57 elite military men. In this follow-on study, we explored associations of salivary anabolic hormone <span class="hlt">profiles</span> with demographic (i.e., age, body mass index [BMI]) and biobehavioral health indices (i.e., blood <span class="hlt">pressure</span>, sleep, perceived stress, fatigue) via correlational models. Next, nuanced patterns were constructed using quartile splits followed by one-way analysis of variance and post hoc subgroup comparisons. Both DHEA (r range: -0.33 to -0.49) and testosterone (r range: -0.19 to -0.41) were inversely associated with age. Quartile comparisons revealed that age-related declines in DHEA were linear, curvilinear, or sigmoidal, depending on the summary parameter of interest. Anabolic hormone <span class="hlt">profiles</span> did not associate with BMI, blood <span class="hlt">pressure</span>, or sleep efficiency. Robust linear associations were <span class="hlt">observed</span> between testosterone and perceived stress (r range: -0.29 to -0.36); concentration-dependent patterns were less discernible. Lower DHEA (r range: -0.22 to -0.30) and testosterone (r range: -0.22 to -0.36) concentrations associated with higher fatigue. Subsequent quartile comparisons suggested a concentration-dependent threshold with respect to evening testosterone. Specifically, those individuals within the lowest quartile (≤68.4pg/mL) endorsed the highest fatigue of the four groups (p=0.01), while the remaining three groups did not differ from each other. This study not only showed that anabolic hormone <span class="hlt">profiles</span> have distinctive age trajectories, but are also valuable predictors of stress and fatigue in elite military men. This highlights the importance of routine monitoring of anabolic hormone <span class="hlt">profiles</span> to sustain and optimize health and readiness in chronically stressed populations. Published by Elsevier Inc.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/28675969','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/28675969"><span>The dietary fiber <span class="hlt">profile</span> of fruit peels and functionality modifications induced by high hydrostatic <span class="hlt">pressure</span> treatments.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Tejada-Ortigoza, Viridiana; García-Amezquita, Luis Eduardo; Serna-Saldívar, Sergio O; Welti-Chanes, Jorge</p> <p>2017-07-01</p> <p>The effect of high hydrostatic <span class="hlt">pressure</span> (HHP) and temperature on composition of non-conventional dietary fiber (DF) sources and functional properties were evaluated. Mango, orange, or prickly pear peels were processed at 600 MPa during 10 min at 22 ℃ and 55 ℃. Total (TDF), soluble (SDF), and insoluble (IDF) dietary fiber, water/oil holding, and retention capacity, solubility, swelling capacity, and bulk density were assayed. An increment in the SDF content was <span class="hlt">observed</span> due to the effect of <span class="hlt">pressure</span> with the greatest changes noticed in mango peel, increasing from 37.4% (control) to 45.7% (SDF/TDF) in the HHP-treated (55 ℃) sample. Constant values of TDF after the treatments suggest a conversion of IDF to SDF in mango (38.9%-40.5% dw) and orange (49.0%-50.8% dw) peels. The highest fiber solubility values were <span class="hlt">observed</span> for mango peel ranging between 80.3% and 83.9%, but the highest increase, from 55.1% to 62.3%, due to treatment was displayed in orange peel processed at 22 ℃. A relationship between DF modifications induced by HHP treatment and changes in the functional properties of the materials was established. Application of HHP opens up the opportunity to modify non-conventional sources of DF and to obtain novel functional properties for different food applications.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/24118408','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/24118408"><span>Physical activity levels and torso orientations of hospitalized patients at risk of developing a <span class="hlt">pressure</span> injury: an <span class="hlt">observational</span> study.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Chaboyer, Wendy; Mills, Peter M; Roberts, Shelley; Latimer, Sharon</p> <p>2015-02-01</p> <p><span class="hlt">Pressure</span> injury guidelines recommend regular repositioning yet patients' mobility and repositioning patterns are unknown. An <span class="hlt">observational</span> study using activity monitors was undertaken to describe the 24 h activity patterns of 84 hospitalized patients at risk of developing a <span class="hlt">pressure</span> injury. The vast majority of participants' time was spent in the sedentary activity range (94% ± 3%) followed by the light range (5% ± 4 %). Patients changed their posture a median of 94 (interquartile range 48) time in the 24-h period (range 11-154), or ≈ 3.8 times per hour. Although a main focus for <span class="hlt">pressure</span> injury prevention has been on repositioning, this study shows that patients with restricted mobility are actually moving quite often. Therefore, it might be appropriate to focus more attention on other <span class="hlt">pressure</span> injury prevention strategies such as adequate nutrition, appropriate support surfaces and good skin care. © 2013 Wiley Publishing Asia Pty Ltd.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/20140012692','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/20140012692"><span>Propagation of Radiosonde <span class="hlt">Pressure</span> Sensor Errors to Ozonesonde Measurements</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Stauffer, R. M.; Morris, G.A.; Thompson, A. M.; Joseph, E.; Coetzee, G. J. R.; Nalli, N. R.</p> <p>2014-01-01</p> <p>Several previous studies highlight <span class="hlt">pressure</span> (or equivalently, <span class="hlt">pressure</span> altitude) discrepancies between the radiosonde <span class="hlt">pressure</span> sensor and that derived from a GPS flown with the radiosonde. The offsets vary during the ascent both in absolute and percent <span class="hlt">pressure</span> differences. To investigate this problem further, a total of 731 radiosonde-ozonesonde launches from the Southern Hemisphere subtropics to Northern mid-latitudes are considered, with launches between 2005 - 2013 from both longer-term and campaign-based intensive stations. Five series of radiosondes from two manufacturers (International Met Systems: iMet, iMet-P, iMet-S, and Vaisala: RS80-15N and RS92-SGP) are analyzed to determine the magnitude of the <span class="hlt">pressure</span> offset. Additionally, electrochemical concentration cell (ECC) ozonesondes from three manufacturers (Science Pump Corporation; SPC and ENSCI-Droplet Measurement Technologies; DMT) are analyzed to quantify the effects these offsets have on the calculation of ECC ozone (O3) mixing ratio <span class="hlt">profiles</span> (O3MR) from the ozonesonde-measured partial <span class="hlt">pressure</span>. Approximately half of all offsets are 0.6 hPa in the free troposphere, with nearly a third 1.0 hPa at 26 km, where the 1.0 hPa error represents 5 persent of the total atmospheric <span class="hlt">pressure</span>. <span class="hlt">Pressure</span> offsets have negligible effects on O3MR below 20 km (96 percent of launches lie within 5 percent O3MR error at 20 km). Ozone mixing ratio errors above 10 hPa (30 km), can approach greater than 10 percent ( 25 percent of launches that reach 30 km exceed this threshold). These errors cause disagreement between the integrated ozonesonde-only column O3 from the GPS and radiosonde <span class="hlt">pressure</span> <span class="hlt">profile</span> by an average of +6.5 DU. Comparisons of total column O3 between the GPS and radiosonde <span class="hlt">pressure</span> <span class="hlt">profiles</span> yield average differences of +1.1 DU when the O3 is integrated to burst with addition of the McPeters and Labow (2012) above-burst O3 column climatology. Total column differences are reduced to an average of -0.5 DU when</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017AGUFMSA41B2620J','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017AGUFMSA41B2620J"><span>Characteristics of ionospheric electron density <span class="hlt">profiles</span> in the auroral and polar cap regions from long-term incoherent scatter radar <span class="hlt">observations</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Jee, G.; Kim, E.; Kwak, Y. S.; Kim, Y.; Kil, H.</p> <p>2017-12-01</p> <p>We investigate the climatological characteristics of the ionospheric electron density <span class="hlt">profiles</span> in the auroral and polar cap regions in comparison with the mid-latitude ionosphere using incoherent scatter radars (ISR) <span class="hlt">observations</span> from Svalbard (78.15N, 16.05E), Tromso (69.59N, 19.23E), and Millstone Hill (42.6N, 288.5E) during a period of 1995 - 2015. Diurnal variations of electron density <span class="hlt">profiles</span> from 100 to 500 km are compared among the three radar <span class="hlt">observations</span> during equinox, summer and winter solstice for different solar and geomagnetic activities. Also investigated are the physical characteristics of E-region and F-region peak parameters of electron density <span class="hlt">profiles</span> in the auroral and polar cap regions, which are significantly different from the mid-latitude ionosphere. In the polar ionosphere, the diurnal variations of density <span class="hlt">profiles</span> are extremely small in summer hemisphere. Semiannual anomaly hardly appears for all latitudes, but winter anomaly occurs at mid-latitude and auroral ionospheres for high solar activity. Nighttime density becomes larger than daytime density in the winter polar cap ionosphere for high solar activity. The E-region peak is very distinctive in the nighttime auroral region and the peak height is nearly constant at about 110 km for all conditions. Compared with the F-region peak density, the E-region peak density does not change much with solar activity. Furthermore, the E-region peak density can be even larger than F-region density for low solar activity in the auroral region, particularly during disturbed condition.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2018JGRA..123.3170Z','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2018JGRA..123.3170Z"><span>The Detached Auroras Induced by the Solar Wind <span class="hlt">Pressure</span> Enhancement in Both Hemispheres From Imaging and In Situ Particle <span class="hlt">Observations</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Zhou, Su; Luan, Xiaoli; Søraas, Finn; Østgaard, Nikolai; Raita, Tero</p> <p>2018-04-01</p> <p>This paper presents simultaneous detached proton auroras that appeared in both hemispheres at 11:06 UT, 08 March 2012, just 2 min after a sudden solar wind <span class="hlt">pressure</span> enhancement ( 11:04 UT) hit the Earth. They were <span class="hlt">observed</span> under northward interplanetary magnetic field Bz condition and during the recovery phase of a moderate geomagnetic storm. In the Northern Hemisphere, Defense Meteorological Satellite Program/Special Sensor Ultraviolet Spectrographic Imager <span class="hlt">observed</span> that the detached arc occurred within 60°-65° magnetic latitude and covered a few magnetic local time (MLT) hours ranging from 0530 to 0830 MLT with a possible extension toward noon. At the same time (11:06 UT), Polar Orbiting Environment Satellites 19 detected a detached proton aurora around 1300 MLT in the Southern Hemisphere, centering 62° magnetic latitude, which was at the same latitudes as the northern detached arc. This southern aurora was most probably a part of a dayside detached arc that was conjugate to the northern one. In situ particle <span class="hlt">observations</span> indicated that the detached auroras were dominated by protons/ions with energies ranging from around 20 keV to several hundreds of keV, without obvious electron precipitations. These detached arcs persisted for less than 6 min, consistent with the impact from <span class="hlt">pressure</span> enhancement and the <span class="hlt">observed</span> electromagnetic ion cyclotron (EMIC) waves. It is suggested that the increasing solar wind <span class="hlt">pressure</span> pushed the hot ions in the ring current closer to Earth where the steep gradient of cold plasma favored EMIC wave growth. By losing energy to EMIC waves the energetic protons (>20 keV) were scattered into the loss cone and produced the <span class="hlt">observed</span> detached proton auroras.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2014AGUFM.G23A0462P','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2014AGUFM.G23A0462P"><span>Bridging a possible gap of GRACE <span class="hlt">observations</span> in the Arctic Ocean using existing GRACE data and in situ bottom <span class="hlt">pressure</span> sensors</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Peralta Ferriz, C.; Morison, J.</p> <p>2014-12-01</p> <p>Since 2003, the Gravity Recovery and Climate Experiment (GRACE) satellite system has provided the means of investigating month-to-month to inter-annual variability of, among many other things, Arctic Ocean circulation over the entire Arctic Basin. Such a comprehensive picture could not have been achieved with the limited in situ <span class="hlt">pressure</span> <span class="hlt">observations</span> available. Results from the first 10 years of ocean bottom <span class="hlt">pressure</span> measurements from GRACE in the Arctic Ocean reveal distinct patterns of ocean variability that are strongly associated with changes in large-scale atmospheric circulation (Peralta-Ferriz et al., 2014): the leading mode of variability being a wintertime basin-coherent mass change driven by winds in the Nordic Seas; the second mode of variability corresponding to a mass signal coherent along the Siberian shelves, and driven by the Arctic Oscillation; and the third mode being a see-saw between western and eastern Arctic shelves, also driven by the large-scale wind patterns. In order to understand Arctic Ocean changes, it is fundamental to continue to track ocean bottom <span class="hlt">pressure</span>. Our concern is what to do if the present GRACE system, which is already well beyond its design lifetime, should fail before its follow-on is launched, currently estimated to be in 2017. In this work, we regress time series of <span class="hlt">pressure</span> from the existing and potential Arctic Ocean bottom <span class="hlt">pressure</span> recorder locations against the fundamental modes of bottom <span class="hlt">pressure</span> variation. Our aim is to determine the optimum combination of in situ measurements to represent the broader scale variability now <span class="hlt">observed</span> by GRACE. With this understanding, we can be better prepared to use in situ <span class="hlt">observations</span> to at least partially cover a possible gap in GRACE coverage. Reference:Peralta-Ferriz, Cecilia, James H. Morison, John M. Wallace, Jennifer A. Bonin, Jinlun Zhang, 2014: Arctic Ocean Circulation Patterns Revealed by GRACE. J. Climate, 27, 1445-1468. doi: http://dx.doi.org/10.1175/JCLI-D-13-00013.1</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2003ApJS..148...39P','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2003ApJS..148...39P"><span>First-Year Wilkinson Microwave Anisotropy Probe (WMAP) <span class="hlt">Observations</span>: Beam <span class="hlt">Profiles</span> and Window Functions</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Page, L.; Barnes, C.; Hinshaw, G.; Spergel, D. N.; Weiland, J. L.; Wollack, E.; Bennett, C. L.; Halpern, M.; Jarosik, N.; Kogut, A.; Limon, M.; Meyer, S. S.; Tucker, G. S.; Wright, E. L.</p> <p>2003-09-01</p> <p>Knowledge of the beam <span class="hlt">profiles</span> is of critical importance for interpreting data from cosmic microwave background experiments. In this paper, we present the characterization of the in-flight optical response of the WMAP satellite. The main-beam intensities have been mapped to <=-30 dB of their peak values by <span class="hlt">observing</span> Jupiter with the satellite in the same <span class="hlt">observing</span> mode as for CMB <span class="hlt">observations</span>. The beam patterns closely follow the prelaunch expectations. The full width at half-maximum is a function of frequency and ranges from 0.82d at 23 GHz to 0.21d at 94 GHz; however, the beams are not Gaussian. We present (a) the beam patterns for all 10 differential radiometers, showing that the patterns are substantially independent of polarization in all but the 23 GHz channel; (b) the effective symmetrized beam patterns that result from WMAP's compound spin <span class="hlt">observing</span> pattern; (c) the effective window functions for all radiometers and the formalism for propagating the window function uncertainty; and (d) the conversion factor from point-source flux to antenna temperature. A summary of the systematic uncertainties, which currently dominate our knowledge of the beams, is also presented. The constancy of Jupiter's temperature within a frequency band is an essential check of the optical system. The tests enable us to report a calibration of Jupiter to 1%-3% accuracy relative to the CMB dipole. WMAP is the result of a partnership between Princeton University and the NASA Goddard Space Flight Center. Scientific guidance is provided by the WMAP Science Team.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/28629940','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/28629940"><span>Highly informative multiclass <span class="hlt">profiling</span> of lipids by ultra-high performance liquid chromatography - Low resolution (quadrupole) mass spectrometry by using electrospray ionization and atmospheric <span class="hlt">pressure</span> chemical ionization interfaces.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Beccaria, Marco; Inferrera, Veronica; Rigano, Francesca; Gorynski, Krzysztof; Purcaro, Giorgia; Pawliszyn, Janusz; Dugo, Paola; Mondello, Luigi</p> <p>2017-08-04</p> <p>A simple, fast, and versatile method, using an ultra-high performance liquid chromatography system coupled with a low resolution (single quadrupole) mass spectrometer was optimized to perform multiclass lipid <span class="hlt">profiling</span> of human plasma. Particular attention was made to develop a method suitable for both electrospray ionization and atmospheric <span class="hlt">pressure</span> chemical ionization interfaces (sequentially in positive- and negative-ion mode), without any modification of the chromatographic conditions (mobile phase, flow-rate, gradient, etc.). Emphasis was given to the extrapolation of the structural information based on the fragmentation pattern obtained using atmospheric <span class="hlt">pressure</span> chemical ionization interface, under each different ionization condition, highlighting the complementary information obtained using the electrospray ionization interface, of support for related molecule ions identification. Furthermore, mass spectra of phosphatidylserine and phosphatidylinositol obtained using the atmospheric <span class="hlt">pressure</span> chemical ionization interface are reported and discussed for the first time. Copyright © 2017 Elsevier B.V. All rights reserved.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://ntrs.nasa.gov/search.jsp?R=20040172696&hterms=Sex&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D70%26Ntt%3DSex','NASA-TRS'); return false;" href="https://ntrs.nasa.gov/search.jsp?R=20040172696&hterms=Sex&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D70%26Ntt%3DSex"><span>Distribution and <span class="hlt">observed</span> associations of orthostatic blood <span class="hlt">pressure</span> changes in elderly general medicine outpatients</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Robertson, D.; DesJardin, J. A.; Lichtenstein, M. J.</p> <p>1998-01-01</p> <p>Factors associated with orthostatic blood <span class="hlt">pressure</span> change in elderly outpatients were determined by surveying 398 medical clinical outpatients aged 65 years and older. Blood <span class="hlt">pressure</span> was measured with random-zero sphygmomanometers after patients were 5 minutes in a supine and 5 minutes in a standing position. Orthostatic blood <span class="hlt">pressure</span> changes were at normally distributed levels with systolic and diastolic <span class="hlt">pressures</span> dropping an average of 4 mm Hg (standard deviation [SD]=15 mm Hg) and 2 mm Hg (SD=11 mm Hg), respectively. Orthostatic blood <span class="hlt">pressure</span> changes were unassociated with age, race, sex, body mass, time since eating, symptoms, or other factors. According to multiple linear regression analysis, supine systolic <span class="hlt">pressure</span>, chronic obstructive pulmonary disease (COPD), and diabetes mellitus were associated with a decrease in systolic <span class="hlt">pressure</span> on standing. Hypertension, antiarthritic drugs, and abnormal heartbeat were associated with an increase in systolic <span class="hlt">pressure</span> on standing. For orthostatic diastolic <span class="hlt">pressure</span> changes, supine diastolic <span class="hlt">pressure</span> and COPD were associated with a decrease in diastolic <span class="hlt">pressure</span> on standing. Congestive heart failure was associated with an increase in standing diastolic <span class="hlt">pressure</span>. Using logistic regression analysis, only supine systolic <span class="hlt">pressure</span> was associated with a greater than 20-mm Hg drop in systolic <span class="hlt">pressure</span> (n=53, prevalence=13%). Supine diastolic <span class="hlt">pressure</span> and COPD were the only variables associated with a greater than 20-mm Hg drop in diastolic <span class="hlt">pressure</span> (n=16, prevalence=4%). These factors may help physicians in identifying older persons at risk for having orthostatic hypotension.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2016JChPh.144u4904G','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2016JChPh.144u4904G"><span>Highly efficient and selective <span class="hlt">pressure</span>-assisted photon-induced polymerization of styrene</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Guan, Jiwen; Song, Yang</p> <p>2016-06-01</p> <p>The polymerization process of condensed styrene to produce polystyrene as an industrially important polymeric material was investigated using a novel approach by combining external compression with ultraviolet radiation. The reaction evolution was monitored as a function of time and the reaction products were characterized by in situ Fourier transform infrared spectroscopy. By optimizing the loading <span class="hlt">pressures</span>, we <span class="hlt">observed</span> highly efficient and selective production of polystyrene of different tacticities. Specifically, at relatively low loading <span class="hlt">pressures</span>, infrared spectra suggest that styrene monomers transform to amorphous atactic polystyrene (APS) with minor crystalline isotactic polystyrene. In contrast, APS was found to be the sole product when polymerization occurs at relatively higher loading <span class="hlt">pressures</span>. The time-dependent reaction <span class="hlt">profiles</span> allow the examination of the polymerization kinetics by analyzing the rate constant and activation volume as a function of <span class="hlt">pressure</span>. As a result, an optimized <span class="hlt">pressure</span> condition, which allows a barrierless reaction to proceed, was identified and attributed to the very desirable reaction yield and kinetics. Finally, the photoinitiated reaction mechanism and the growth geometry of the polymer chains were investigated from the energy diagram of styrene and by the topology analysis of the crystal styrene. This study shows strong promise to produce functional polymeric materials in a highly efficient and controlled manner.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://ntrs.nasa.gov/search.jsp?R=20030053447&hterms=balance+sheet&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D50%26Ntt%3Dbalance%2Bsheet','NASA-TRS'); return false;" href="https://ntrs.nasa.gov/search.jsp?R=20030053447&hterms=balance+sheet&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D50%26Ntt%3Dbalance%2Bsheet"><span>Relation between <span class="hlt">Pressure</span> Balance Structures and Polar Plumes from Ulysses High Latitude <span class="hlt">Observations</span></span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Yamauchi, Yohei; Suess, Steven T.; Sakurai, Takashi</p> <p>2002-01-01</p> <p>Ulysses <span class="hlt">observations</span> have shown that <span class="hlt">pressure</span> balance structures (PBSs) are a common feature in high-latitude, fast solar wind near solar minimum. Previous studies of Ulysses/SWOOPS plasma data suggest these PBSs may be remnants of coronal polar plumes. Here we find support for this suggestion in an analysis of PBS magnetic structure. We used Ulysses magnetometer data and applied a minimum variance analysis to magnetic discontinuities in PBSs. We found that PBSs preferentially contain tangential discontinuities, as opposed to rotational discontinuities and to non-PBS regions in the solar wind. This suggests that PBSs contain structures like current sheets or plasmoids that may be associated with network activity at the base of plumes.</p> </li> </ol> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_18");'>18</a></li> <li><a href="#" onclick='return showDiv("page_19");'>19</a></li> <li class="active"><span>20</span></li> <li><a href="#" onclick='return showDiv("page_21");'>21</a></li> <li><a href="#" onclick='return showDiv("page_22");'>22</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div><!-- col-sm-12 --> </div><!-- row --> </div><!-- page_20 --> <div id="page_21" class="hiddenDiv"> <div class="row"> <div class="col-sm-12"> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_19");'>19</a></li> <li><a href="#" onclick='return showDiv("page_20");'>20</a></li> <li class="active"><span>21</span></li> <li><a href="#" onclick='return showDiv("page_22");'>22</a></li> <li><a href="#" onclick='return showDiv("page_23");'>23</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div> </div> <div class="row"> <div class="col-sm-12"> <ol class="result-class" start="401"> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/15324518','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/15324518"><span>Deleterious effects of increased body weight associated with intensive insulin therapy for type 1 diabetes: increased blood <span class="hlt">pressure</span> and worsened lipid <span class="hlt">profile</span> partially negate improvements in life expectancy.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Palmer, Andrew J; Roze, Stéphane; Valentine, William J; Minshall, Michael E; Lammert, Morten; Nicklasson, Lars; Spinas, Giatgen A</p> <p>2004-08-01</p> <p>Weight gain is an unwanted side effect of improved glycaemic control in type 1 diabetes, associated with increased blood <span class="hlt">pressure</span> (BP) and worsening lipid <span class="hlt">profiles</span>. While improved glycaemic control per se should improve long-term patient outcomes, increases in BP and worsening lipid <span class="hlt">profiles</span> may counteract these benefits. The aim of this modelling study was to assess whether the increased body weight and associated worsening of lipid <span class="hlt">profile</span> and blood <span class="hlt">pressure</span> would negate the improvements in glycaemic control seen with intensive therapy in patients with type 1 diabetes. A validated diabetes model projected life expectancy (LE), quality-adjusted LE (QALE) and total lifetime costs of complications in type 1 diabetes cohorts with the characteristics of patients from the Diabetes Control and Complications Trial (DCCT). The following four cohorts (A-D) were created based on increased body weight under either conventional or intensive therapy: A) conventional glycaemic control in the subgroup with lowest weight-gain quartile after 6.5 years (HbA1c increased by 11% from baseline); B) conventional control in the highest weight-gain quartile (no change in HbA1c from baseline); C) intensive control in the lowest quartile of weight gain (with 16.1% decrease in HbA1c, but no increase in weight or associated BP, and improved lipid <span class="hlt">profile</span>); D) intensive control in the highest quartile of weight gain (with 21% decrease in HbA1c, increased systolic BP of 6 mmHg, and worsened lipid <span class="hlt">profile</span>). Data were derived from DCCT and other published sources. Intensive control, even with weight gain, led to major improvements in LE and QALE, and reduction in costs of complications versus conventional therapy. Intensive therapy with no weight increase led to a higher LE (increased by 0.57 years) and higher QALE (increased by 0.28 years) and lower costs of complications (reduced by 523 dollars/patient), compared to intensive therapy with the highest quartile of weight gain. Concerns about</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2014Icar..243...91H','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2014Icar..243...91H"><span>Initial results from radio occultation measurements with the Mars Reconnaissance Orbiter: A nocturnal mixed layer in the tropics and comparisons with polar <span class="hlt">profiles</span> from the Mars Climate Sounder</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Hinson, David P.; Asmar, Sami W.; Kahan, Daniel S.; Akopian, Varoujan; Haberle, Robert M.; Spiga, Aymeric; Schofield, John T.; Kleinböhl, Armin; Abdou, Wedad A.; Lewis, Stephen R.; Paik, Meegyeong; Maalouf, Sami G.</p> <p>2014-11-01</p> <p>The Mars Reconnaissance Orbiter (MRO) performs radio occultation (RO) measurements on selected orbits, generally once per day. We have retrieved atmospheric <span class="hlt">profiles</span> from two subsets of data, yielding a variety of new results that illustrate the scientific value of the <span class="hlt">observations</span>. One set of measurements sounded the tropics in northern summer at a local time ∼1 h before sunrise. Some of these <span class="hlt">profiles</span> contain an unexpected layer of neutral stability with a depth of ∼4 km and a <span class="hlt">pressure</span> at its upper boundary of ∼160 Pa. The mixed layer is bounded above by a temperature inversion and below by another strong inversion adjacent to the surface. This type of structure is <span class="hlt">observed</span> near Gale Crater, in the Tharsis region, and at a few other locations, whereas <span class="hlt">profiles</span> in Amazonis Planitia and Elysium Planitia show no sign of a detached mixed layer with an overlying inversion. We supplemented the measurements with numerical simulations by the NASA Ames Mars General Circulation Model, which demonstrate that water ice clouds can generate this distinctive type of temperature structure through their influence on radiative transfer at infrared wavelengths. In particular, the simulations predict the presence of a nocturnal cloud layer in the Tharsis region at a <span class="hlt">pressure</span> of ∼150 Pa (∼10 km above the surface), and the nighttime radiative cooling at cloud level is sufficient to produce a temperature inversion above the cloud as well as convective instability below the cloud, consistent with the <span class="hlt">observations</span>. The second set of measurements sounded mid-to-high northern latitudes in spring, when carefully coordinated <span class="hlt">observations</span> by the MRO Mars Climate Sounder (MCS) are also available. The differences between the RO and MCS temperature <span class="hlt">profiles</span> are generally consistent with the expected performance of the two instruments. Within this set of 21 comparisons the average temperature difference is less than 1 K where the aerosol opacities are smaller than 10-3km-1 , at</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2018JAP...123v3304H','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2018JAP...123v3304H"><span><span class="hlt">Observation</span> of the standing wave effect in large-area, very-high-frequency capacitively coupled plasmas by using a fiber Bragg grating sensor</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Han, Dao-Man; Liu, Yong-Xin; Gao, Fei; Wang, Xiang-Yu; Li, Ang; Xu, Jun; Jing, Zhen-Guo; Wang, You-Nian</p> <p>2018-06-01</p> <p>The large-area capacitive discharges driven at very high frequencies have been attracting much attention due to their wide applications in material etching and thin film deposition. However, in the regime, the standing wave effect (SWE) becomes a major limitation for plasma material processing uniformity. In this work, a fiber Bragg grating sensor was utilized for the <span class="hlt">observation</span> of the SWE in a large-area capacitive discharge reactor by measuring the radial distribution of the neutral gas temperature T g. The influences of the RF power and the working <span class="hlt">pressure</span> on the radial <span class="hlt">profiles</span> of T g were studied. At a higher frequency (100 MHz) and a lower <span class="hlt">pressure</span> (5 Pa), T g presents a center-peaked radial distribution, indicating a significant SWE. As the RF power increases, the central peak of T g becomes more evident due to the enhanced SWE. By contrast, at 100 MHz and a higher <span class="hlt">pressure</span> (40 Pa), the radial distribution of T g shows an evident peak at the electrode edge and T g decays dramatically towards the discharge center because the electromagnetic waves are strongly damped as they are propagating from the edge to the center. At a lower frequency (27 MHz), only edge-high <span class="hlt">profiles</span> of T g are <span class="hlt">observed</span> for various <span class="hlt">pressures</span>. For the sake of a comparison, a hairpin resonance probe was used to measure the radial distributions of the plasma density n p under the same condition. The radial <span class="hlt">profiles</span> of T g are found to generally resemble those of n p under various conditions. Based on the experimental results, the neutral gas heating mechanism was analyzed.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/16550667','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/16550667"><span>Measuring sub-bandage <span class="hlt">pressure</span>: comparing the use of <span class="hlt">pressure</span> monitors and pulse oximeters.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Satpathy, A; Hayes, S; Dodds, S R</p> <p>2006-03-01</p> <p>To test the use of low-cost sub-bandage <span class="hlt">pressure</span> monitors and pulse oximeters as part of a quality-control measure for graduated compression bandaging in leg ulcer clinics. Twenty-five healthy volunteers (mean age 40 years) providing 50 limbs were bandaged with a four-layer compression bandaging system. The ankle systolic <span class="hlt">pressure</span> (ASP) was measured using a pulse oximeter (Nellcor NBP-40) before applying the graduated compression bandages. Interface <span class="hlt">pressure</span> was measured by placing <span class="hlt">pressure</span> sensors on the skin at three points (2cm above the medial malleolus; the widest part of the calf; and a point midway between them) in the supine and standing positions. The ASP was measured again with the pulse oximeter after the bandage had been applied, and the effect of the bandage on the ASP was recorded. The actual <span class="hlt">pressure</span> created by the bandage was compared with the required <span class="hlt">pressure</span> <span class="hlt">profile</span>. Interface <span class="hlt">pressures</span> varied with change of position and movement. With the operator blinded to the <span class="hlt">pressure</span> monitors while applying the bandages, the target <span class="hlt">pressure</span> of 35-40mmHg at the ankle was achieved in only 36% of limbs ([mean +/- 95% confidence interval]; 32.3 +/- 1.6mmHg [supine]; 38.4 +/- 2.4mmHg [standing position]). With the help of the <span class="hlt">pressure</span> monitors, the target <span class="hlt">pressure</span> was achieved in 78% of the limbs. There was no correlation between the <span class="hlt">pressure</span> monitors and pulse oximeter <span class="hlt">pressures</span>, demonstrating that the pulse oximeter is not a useful tool for measuring sub-bandage <span class="hlt">pressures</span>. The results suggest a tool (interface <span class="hlt">pressure</span> monitors) that is easy to operate should be available as part of quality assurance for treatment, training of care providers and education.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2014BGD....1117413G','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2014BGD....1117413G"><span>Autonomous <span class="hlt">profiling</span> float <span class="hlt">observations</span> of the high biomass plume downstream of the Kerguelen plateau in the Southern Ocean</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Grenier, M.; Della Penna, A.; Trull, T. W.</p> <p>2014-12-01</p> <p>Natural iron fertilisation from Southern Ocean islands results in high primary production and phytoplankton biomass accumulations readily visible in satellite ocean colour <span class="hlt">observations</span>. These images reveal great spatial complexity with highly varying concentrations of chlorophyll, presumably reflecting both variations in iron supply and conditions favouring phytoplankton accumulation. To examine the second aspect, in particular the influences of variations in temperature and stratification, we deployed four autonomous <span class="hlt">profiling</span> floats in the Antarctic Circumpolar Current near the Kerguelen plateau in the Indian sector of the Southern Ocean. Each "bio-<span class="hlt">profiler</span>" measured more than 250 <span class="hlt">profiles</span> of temperature (T), salinity (S), dissolved oxygen, chlorophyll fluorescence (Chl a), and particle backscatter in the top 300 m of the water column, sampling up to 5 <span class="hlt">profiles</span> per day along meandering trajectories extending up to 1000 km. Comparison of surface Chl a estimates (top 50 m depth; analogous to values from satellite images) with total water column inventories revealed largely linear relationships, suggesting that dilution of chlorophyll by mixed layer depth variations plays only a minor role in the spatial distributions <span class="hlt">observed</span> by satellite, and correspondingly that these images provide credible information on total and not just surface biomass accumulations. Regions of very high Chl a accumulation (1.5-10 μg L-1) were associated predominantly with a narrow T-S class of surface waters, which appears to derive from the northern Kerguelen plateau. In contrast, waters with only moderate Chl a enrichments (0.5-1.5 μg L-1) displayed no clear correlation with water properties, including no dependence on mixed layer depth, suggesting a diversity of sources of iron and/or its efficient dispersion across filaments of the plume. The lack of dependence on mixed layer depth also indicates a limited influence on production by light limitation. One float became trapped in a</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.osti.gov/biblio/22270829-suzaku-observations-ray-brightest-fossil-group-eso','SCIGOV-STC'); return false;" href="https://www.osti.gov/biblio/22270829-suzaku-observations-ray-brightest-fossil-group-eso"><span>SUZAKU <span class="hlt">OBSERVATIONS</span> OF THE X-RAY BRIGHTEST FOSSIL GROUP ESO 3060170</span></a></p> <p><a target="_blank" href="http://www.osti.gov/search">DOE Office of Scientific and Technical Information (OSTI.GOV)</a></p> <p>Su, Yuanyuan; White, Raymond E. III; Miller, Eric D., E-mail: ysu@crimson.ua.edu</p> <p>2013-10-01</p> <p>'Fossil' galaxy groups, each dominated by a relatively isolated giant elliptical galaxy, have many properties intermediate between groups and clusters of galaxies. We used the Suzaku X-ray observatory to <span class="hlt">observe</span> the X-ray brightest fossil group, ESO 3060170, out to R{sub 200}, in order to better elucidate the relation between fossil groups, normal groups, and clusters. We determined the intragroup gas temperature, density, and metal abundance distributions and derived the entropy, <span class="hlt">pressure</span>, and mass <span class="hlt">profiles</span> for this group. The entropy and <span class="hlt">pressure</span> <span class="hlt">profiles</span> in the outer regions are flatter than in simulated clusters, similar to what is seen in <span class="hlt">observations</span> ofmore » massive clusters. This may indicate that the gas is clumpy and/or the gas has been redistributed. Assuming hydrostatic equilibrium, the total mass is estimated to be ∼1.7 × 10{sup 14} M{sub ☉} within a radius R{sub 200} of ∼1.15 Mpc, with an enclosed baryon mass fraction of 0.13. The integrated iron mass-to-light ratio of this fossil group is larger than in most groups and comparable to those of clusters, indicating that this fossil group has retained the bulk of its metals. A galaxy luminosity density map on a scale of 25 Mpc shows that this fossil group resides in a relatively isolated environment, unlike the filamentary structures in which typical groups and clusters are embedded.« less</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=5932198','PMC'); return false;" href="https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=5932198"><span>The Effect of Hydrostatic <span class="hlt">Pressure</span> on Enrichments of Hydrocarbon Degrading Microbes From the Gulf of Mexico Following the Deepwater Horizon Oil Spill</span></a></p> <p><a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pmc">PubMed Central</a></p> <p>Marietou, Angeliki; Chastain, Roger; Beulig, Felix; Scoma, Alberto; Hazen, Terry C.; Bartlett, Douglas H.</p> <p>2018-01-01</p> <p>The Deepwater Horizon oil spill was one of the largest and deepest oil spills recorded. The wellhead was located at approximately 1500 m below the sea where low temperature and high <span class="hlt">pressure</span> are key environmental characteristics. Using cells collected 4 months following the Deepwater Horizon oil spill at the Gulf of Mexico, we set up Macondo crude oil enrichments at wellhead temperature and different <span class="hlt">pressures</span> to determine the effect of increasing depth/<span class="hlt">pressure</span> to the in situ microbial community and their ability to degrade oil. We <span class="hlt">observed</span> oil degradation under all <span class="hlt">pressure</span> conditions tested [0.1, 15, and 30 megapascals (MPa)], although oil degradation <span class="hlt">profiles</span>, cell numbers, and hydrocarbon degradation gene abundances indicated greatest activity at atmospheric <span class="hlt">pressure</span>. Under all incubations the growth of psychrophilic bacteria was promoted. Bacteria closely related to Oleispira antarctica RB-8 dominated the communities at all <span class="hlt">pressures</span>. At 30 MPa we <span class="hlt">observed</span> a shift toward Photobacterium, a genus that includes piezophiles. Alphaproteobacterial members of the Sulfitobacter, previously associated with oil-degradation, were also highly abundant at 0.1 MPa. Our results suggest that <span class="hlt">pressure</span> acts synergistically with low temperature to slow microbial growth and thus oil degradation in deep-sea environments. PMID:29755436</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/29755436','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/29755436"><span>The Effect of Hydrostatic <span class="hlt">Pressure</span> on Enrichments of Hydrocarbon Degrading Microbes From the Gulf of Mexico Following the Deepwater Horizon Oil Spill.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Marietou, Angeliki; Chastain, Roger; Beulig, Felix; Scoma, Alberto; Hazen, Terry C; Bartlett, Douglas H</p> <p>2018-01-01</p> <p>The Deepwater Horizon oil spill was one of the largest and deepest oil spills recorded. The wellhead was located at approximately 1500 m below the sea where low temperature and high <span class="hlt">pressure</span> are key environmental characteristics. Using cells collected 4 months following the Deepwater Horizon oil spill at the Gulf of Mexico, we set up Macondo crude oil enrichments at wellhead temperature and different <span class="hlt">pressures</span> to determine the effect of increasing depth/<span class="hlt">pressure</span> to the in situ microbial community and their ability to degrade oil. We <span class="hlt">observed</span> oil degradation under all <span class="hlt">pressure</span> conditions tested [0.1, 15, and 30 megapascals (MPa)], although oil degradation <span class="hlt">profiles</span>, cell numbers, and hydrocarbon degradation gene abundances indicated greatest activity at atmospheric <span class="hlt">pressure</span>. Under all incubations the growth of psychrophilic bacteria was promoted. Bacteria closely related to Oleispira antarctica RB-8 dominated the communities at all <span class="hlt">pressures</span>. At 30 MPa we <span class="hlt">observed</span> a shift toward Photobacterium , a genus that includes piezophiles. Alphaproteobacterial members of the Sulfitobacter , previously associated with oil-degradation, were also highly abundant at 0.1 MPa. Our results suggest that <span class="hlt">pressure</span> acts synergistically with low temperature to slow microbial growth and thus oil degradation in deep-sea environments.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2016AGUFM.C21C0710W','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2016AGUFM.C21C0710W"><span><span class="hlt">Observations</span> of upper ocean stability and heat fluxes in the Antarctic from under-ice Argo float <span class="hlt">profile</span> data.</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Wilson, E. A.; Riser, S.</p> <p>2016-12-01</p> <p>Sea ice growth around Antarctica is intimately linked to the stability and thermohaline structure of the underlying ocean. As sea ice grows, the resulting brine triggers convective instabilities that deepen the mixed layer and entrain warm water from the weakly stratified pycnocline. The heat released from this process acts as a strong negative feedback to ice growth which, under the right scenarios, can exceed the initial atmospheric heat loss. Much of our current understanding of this ice-ocean interaction comes from a handful of relatively short field campaigns in the Weddell Sea. Here, we supplement those <span class="hlt">observations</span> with an analysis of over 9000 under-ice Argo float <span class="hlt">profiles</span>, collected between 2006-2015. These <span class="hlt">profiles</span> provide an unprecedented view of the temporal and spatial variability of the upper ocean structure throughout the Antarctic region. With these <span class="hlt">observations</span> and a theoretical understanding of the coupled ice-ocean system, we assess the ocean's potential to limit thermodynamic ice growth as well as its susceptibility to deep convection in different regions. Using these results, we infer how recent climatic changes may influence Antarctic sea ice growth and deep ocean ventilation in the near future.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/19357147','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/19357147"><span>Sibutramine versus continuous positive airway <span class="hlt">pressure</span> in obese obstructive sleep apnoea patients.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Ferland, A; Poirier, P; Sériès, F</p> <p>2009-09-01</p> <p>The aim of the present study was to compare the efficacy of 1 yr of sibutramine-induced weight loss versus continuous positive airway <span class="hlt">pressure</span> (CPAP) treatment on sleep-disordered breathing, cardiac autonomic function and systemic blood <span class="hlt">pressure</span> in obese patients with obstructive sleep apnoea. Subjects with a body mass index of > or =30 kg.m(-2) without previous treatment for obstructive sleep apnoea underwent either sibutramine (n = 22) or CPAP (n = 18) treatment for 1 yr. Sibutramine induced a 5.4+/-1.4 kg decrease in body weight compared to the CPAP group, in which no changes in anthropometric variables were <span class="hlt">observed</span>. The CPAP treatment improved all sleep and respiratory variables, whereas sibutramine-induced weight loss improved only nocturnal arterial oxygen saturation <span class="hlt">profile</span>. Only CPAP treatment improved night-time systolic and diastolic blood <span class="hlt">pressure</span> and 24-h and daytime ambulatory diastolic blood <span class="hlt">pressure</span>. Sibutramine-induced weight loss had no impact on indices of heart rate variability, whereas CPAP treatment increased daytime time domain indices. CPAP treatment for 1 yr had beneficial impacts on nocturnal breathing disturbances, and improved nocturnal oxygenation, night-time systolic and diastolic blood <span class="hlt">pressure</span>, and daytime cardiac parasympathetic modulation. Sibutramine did not improve sleep-disordered breathing, systemic blood <span class="hlt">pressure</span> or heart rate variability. There were no adverse effects, such as increment in blood <span class="hlt">pressure</span> or arrhythmias, associated with this treatment regimen.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.osti.gov/servlets/purl/1038128','SCIGOV-STC'); return false;" href="https://www.osti.gov/servlets/purl/1038128"><span>Deflagration Wave <span class="hlt">Profiles</span></span></a></p> <p><a target="_blank" href="http://www.osti.gov/search">DOE Office of Scientific and Technical Information (OSTI.GOV)</a></p> <p>Menikoff, Ralph</p> <p>2012-04-03</p> <p>Shock initiation in a plastic-bonded explosives (PBX) is due to hot spots. Current reactive burn models are based, at least heuristically, on the ignition and growth concept. The ignition phase occurs when a small localized region of high temperature (or hot spot) burns on a fast time scale. This is followed by a growth phase in which a reactive front spreads out from the hot spot. Propagating reactive fronts are deflagration waves. A key question is the deflagration speed in a PBX compressed and heated by a shock wave that generated the hot spot. Here, the ODEs for a steadymore » deflagration wave <span class="hlt">profile</span> in a compressible fluid are derived, along with the needed thermodynamic quantities of realistic equations of state corresponding to the reactants and products of a PBX. The properties of the wave <span class="hlt">profile</span> equations are analyzed and an algorithm is derived for computing the deflagration speed. As an illustrative example, the algorithm is applied to compute the deflagration speed in shock compressed PBX 9501 as a function of shock <span class="hlt">pressure</span>. The calculated deflagration speed, even at the CJ <span class="hlt">pressure</span>, is low compared to the detonation speed. The implication of this are briefly discussed.« less</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017EGUGA..1919099T','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017EGUGA..1919099T"><span>Tsunami simulation method initiated from waveforms <span class="hlt">observed</span> by ocean bottom <span class="hlt">pressure</span> sensors for real-time tsunami forecast; Applied for 2011 Tohoku Tsunami</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Tanioka, Yuichiro</p> <p>2017-04-01</p> <p>After tsunami disaster due to the 2011 Tohoku-oki great earthquake, improvement of the tsunami forecast has been an urgent issue in Japan. National Institute of Disaster Prevention is installing a cable network system of earthquake and tsunami <span class="hlt">observation</span> (S-NET) at the ocean bottom along the Japan and Kurile trench. This cable system includes 125 <span class="hlt">pressure</span> sensors (tsunami meters) which are separated by 30 km. Along the Nankai trough, JAMSTEC already installed and operated the cable network system of seismometers and <span class="hlt">pressure</span> sensors (DONET and DONET2). Those systems are the most dense <span class="hlt">observation</span> network systems on top of source areas of great underthrust earthquakes in the world. Real-time tsunami forecast has depended on estimation of earthquake parameters, such as epicenter, depth, and magnitude of earthquakes. Recently, tsunami forecast method has been developed using the estimation of tsunami source from tsunami waveforms <span class="hlt">observed</span> at the ocean bottom <span class="hlt">pressure</span> sensors. However, when we have many <span class="hlt">pressure</span> sensors separated by 30km on top of the source area, we do not need to estimate the tsunami source or earthquake source to compute tsunami. Instead, we can initiate a tsunami simulation from those dense tsunami <span class="hlt">observed</span> data. <span class="hlt">Observed</span> tsunami height differences with a time interval at the ocean bottom <span class="hlt">pressure</span> sensors separated by 30 km were used to estimate tsunami height distribution at a particular time. In our new method, tsunami numerical simulation was initiated from those estimated tsunami height distribution. In this paper, the above method is improved and applied for the tsunami generated by the 2011 Tohoku-oki great earthquake. Tsunami source model of the 2011 Tohoku-oki great earthquake estimated using <span class="hlt">observed</span> tsunami waveforms, coseimic deformation <span class="hlt">observed</span> by GPS and ocean bottom sensors by Gusman et al. (2012) is used in this study. The ocean surface deformation is computed from the source model and used as an initial condition of tsunami</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2016isms.confEWK14I','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2016isms.confEWK14I"><span><span class="hlt">Observation</span> of Ortho-Para Dependence of <span class="hlt">Pressure</span> Broadening Coefficient in Acetylene νb{1}+νb{3} Vibration Band Using Dual-Comb Spectroscopy</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Iwakuni, Kana; Okubo, Sho; Inaba, Hajime; Onae, Atsushi; Hong, Feng-Lei; Sasada, Hiroyuki; Yamada, Koichi MT</p> <p>2016-06-01</p> <p>We <span class="hlt">observe</span> that the <span class="hlt">pressure</span>-broadening coefficients depend on the ortho-para levels. The spectrum is taken with a dual-comb spectrometer which has the resolution of 48 MHz and the frequency accuracy of 8 digit when the signal-to-noise ratio is more than 20. In this study, about 4.4-Tz wide spectra of the P(31) to R(31) transitions in the νb{1}+νb{3} vibration band of 12C_2H_2 are <span class="hlt">observed</span> at the <span class="hlt">pressure</span> of 25, 60, 396, 1047, 1962 and 2654 Pa. Each rotation-vibration absorption line is fitted to Voight function and we determined <span class="hlt">pressure</span>-broadening coefficients for each rotation-vibration transition. The Figure shows <span class="hlt">pressure</span> broadening coefficient as a function of m. Here m is J"+1 for R and -J" for P-branch. The graph shows obvious dependence on ortho and para. We fit it to Pade function considering the population ratio of three-to-one for the ortho and para levels. This would lead to detailed understanding of the <span class="hlt">pressure</span> boarding mechanism. S. Okubo et al., Applied Physics Express 8, 082402 (2015)</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017APS..DPPJ11027G','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017APS..DPPJ11027G"><span>Study of high field side/low field side asymmetry in the electron temperature <span class="hlt">profile</span> with electron cyclotron emission</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Gugliada, V. R.; Austin, M. E.; Brookman, M. W.</p> <p>2017-10-01</p> <p>Electron cyclotron emission (ECE) provides high resolution measurements of electron temperature <span class="hlt">profiles</span> (Te(R , t)) in tokamaks. Calibration accuracy of this data can be improved using a sawtooth averaging technique. This improved calibration will then be utilized to determine the symmetry of Te <span class="hlt">profiles</span> by comparing low field side (LFS) and high field side (HFS) measurements. Although Te is considered constant on flux surfaces, cases have been <span class="hlt">observed</span> in which there are pronounced asymmetries about the magnetic axis, particularly with increased <span class="hlt">pressure</span>. Trends in LFS/HFS overlap are examined as functions of plasma <span class="hlt">pressure</span>, MHD mode presence, heating techniques, and other discharge conditions. This research will provide information on the accuracy of the current two-dimensional mapping of flux surfaces in the tokamak. Findings can be used to generate higher quality EFITs and inform ECE calibration. Work supported in part by US DoE under the Science Undergraduate Laboratory Internship (SULI) program and under DE-FC02-04ER549698.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2010AGUFM.T12B..01A','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2010AGUFM.T12B..01A"><span>Broadband Seismic Array <span class="hlt">Observation</span> along a ~2000-km-long Linear <span class="hlt">Profile</span> in South China</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Ai, Y.; Zhao, L.; Chen, L.; Zheng, T.; He, Y.; Jiang, M.</p> <p>2010-12-01</p> <p>In order to study the interior structure and geodynamic evolution of South China, we have started implementation of a linear seismic array <span class="hlt">observation</span> in this region since December 2009. The linear array extends for ~2000 km from the northwestern continental interior all the way to the southeastern coastal area, across major tectonic units of South China including the Songpan-Ganze Orogenic Belt (SGOB) in the northwest, the Yangtze Craton (YzC) in the middle, and the Huanan Orogenic Belt (HOB) in the southeast. We plan to deploy a total of 200 broadband stations in the time period from December 2009 to June 2012. All the stations will be equipped with Guralp CMG-3ESP sensors and Ref-tek 130-1 or Ref-tek 72-A digitizers. The entire array <span class="hlt">observation</span> includes three stages. In the time period from December 2009 to March 2011, 64 stations were deployed with a spatial interval of ~25 km from Chengdu city in Sichuan province in the west to Quanzhou city in Fujian province in the southeast of China. In the second stage, about 70 stations with a spatial interval of ~10 km will be deployed from Gonghe city in Qinghai province in the northwest to Chengdu city in the southeast in the time period from October 2010 to November 2011. In the last stage from April 2011 to June 2012, 66 stations with a spatial interval of ~25 km will be deployed to densify the station coverage along the Chengdu - Quanzhou segment of the <span class="hlt">profile</span>. We have already analyzed the seismic data collected at the 64 stations using receiver function methods. Our preliminary results show an obvious W-E variation in the crustal thickness of the region. In particular, from inland to offshore of the Fujian Province the crustal thickness decreases, whereas the Poisson's ratio increases. These may indicate decreasing SiO2 and increasing calc-alkaline contents in the crust. The receiver function data also reveal a coherent structure of the 410-km and 660-km discontinuities along the <span class="hlt">observation</span> <span class="hlt">profile</span></p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/19940012048','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/19940012048"><span>Temperature and <span class="hlt">pressure</span> effects on capacitance probe cryogenic liquid level measurement accuracy</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Edwards, Lawrence G.; Haberbusch, Mark</p> <p>1993-01-01</p> <p>The inaccuracies of liquid nitrogen and liquid hydrogen level measurements by use of a coaxial capacitance probe were investigated as a function of fluid temperatures and <span class="hlt">pressures</span>. Significant liquid level measurement errors were found to occur due to the changes in the fluids dielectric constants which develop over the operating temperature and <span class="hlt">pressure</span> ranges of the cryogenic storage tanks. The level measurement inaccuracies can be reduced by using fluid dielectric correction factors based on measured fluid temperatures and <span class="hlt">pressures</span>. The errors in the corrected liquid level measurements were estimated based on the reported calibration errors of the temperature and <span class="hlt">pressure</span> measurement systems. Experimental liquid nitrogen (LN2) and liquid hydrogen (LH2) level measurements were obtained using the calibrated capacitance probe equations and also by the dielectric constant correction factor method. The liquid levels obtained by the capacitance probe for the two methods were compared with the liquid level estimated from the fluid temperature <span class="hlt">profiles</span>. Results show that the dielectric constant corrected liquid levels agreed within 0.5 percent of the temperature <span class="hlt">profile</span> estimated liquid level. The uncorrected dielectric constant capacitance liquid level measurements deviated from the temperature <span class="hlt">profile</span> level by more than 5 percent. This paper identifies the magnitude of liquid level measurement error that can occur for LN2 and LH2 fluids due to temperature and <span class="hlt">pressure</span> effects on the dielectric constants over the tank storage conditions from 5 to 40 psia. A method of reducing the level measurement errors by using dielectric constant correction factors based on fluid temperature and <span class="hlt">pressure</span> measurements is derived. The improved accuracy by use of the correction factors is experimentally verified by comparing liquid levels derived from fluid temperature <span class="hlt">profiles</span>.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/12848294','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/12848294"><span>Increased blood <span class="hlt">pressure</span> later in life may be associated with perinatal n-3 fatty acid deficiency.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Armitage, James A; Pearce, Adrian D; Sinclair, Andrew J; Vingrys, Algis J; Weisinger, Richard S; Weisinger, Harrison S</p> <p>2003-04-01</p> <p>Hypertension is a major risk factor for cardiovascular and cerebrovascular disease. Previous work in both animals and humans with high blood <span class="hlt">pressure</span> has demonstrated the antihypertensive effects of n-3 polyunsaturated fatty acids (PUFA), although it is not known whether these nutrients are effective in preventing hypertension. The predominant n-3 PUFA in the mammalian nervous system, docosahexaenoic acid (DHA), is deposited into synaptic membranes at a high rate during the perinatal period, and recent <span class="hlt">observations</span> indicate that the perinatal environment is important for the normal development of blood <span class="hlt">pressure</span> control. This study investigated the importance of perinatal n-3 PUFA supply in the control of blood <span class="hlt">pressure</span> in adult Sprague-Dawley rats. Pregnant rat dams were fed semisynthetic diets that were either deficient in (DEF) or supplemented with (CON) n-3 PUFA. Offspring were fed the same diets as their mothers until 9 wk; then, half of the rats from each group were crossed over to the opposite diet creating four groups, i.e., CON-CON; CON-DEF; DEF-DEF, DEF-CON. Mean arterial blood <span class="hlt">pressures</span> (MAP) were measured directly, at 33 wk of age, by cannulation of the femoral artery. The phospholipid fatty acid <span class="hlt">profile</span> of the hypothalamic region was determined by capillary gas-liquid chromatography. The tissue phospholipid fatty acid <span class="hlt">profile</span> reflected the diet that the rats were consuming at the time of testing. Both groups receiving DEF after 9 wk of age (i.e., DEF-DEF and CON-DEF) had similar <span class="hlt">profiles</span> with a reduction in DHA levels of 30%, compared with rats receiving CON (i.e., CON-CON and DEF-CON). DEF-DEF rats had significantly raised MAP compared with all other groups, with differences as great as 17 mm Hg. DEF-CON rats had raised MAP compared with CON-CON rats, and DEF-DEF rats had higher MAP than CON-DEF rats, despite the fact that their respective fatty acid <span class="hlt">profiles</span> were not different. These findings indicate that inadequate levels of DHA in the perinatal</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://www.dtic.mil/docs/citations/ADA538038','DTIC-ST'); return false;" href="http://www.dtic.mil/docs/citations/ADA538038"><span><span class="hlt">Observation</span> of an Ultrahard Phase of Graphite Quenched from High-<span class="hlt">pressure</span></span></a></p> <p><a target="_blank" href="http://www.dtic.mil/">DTIC Science & Technology</a></p> <p></p> <p>2011-02-01</p> <p>Polycrystalline NaCl at High <span class="hlt">Pressures</span> and 300 °K. J. Geophys. Res. 1978, 83, 1257–1268. 23. Selvi , E.; Ma, Y.; Askoy, R.; Ertas, A.; White, A. High...<span class="hlt">Pressure</span> X-ray Diffraction Study of Tungsten Disulfide. J. Phys. Chem. Solids 2006, 67, 2183–2186. 24. Askoy, R.; Ma, Y.; Selvi , E.; Chyu, M. C</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/25414062','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/25414062"><span>Antimicrobial Resistance <span class="hlt">Profiles</span> and Diversity in Salmonella from Humans and Cattle, 2004-2011.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Afema, J A; Mather, A E; Sischo, W M</p> <p>2015-11-01</p> <p>Analysis of long-term anti-microbial resistance (AMR) data is useful to understand source and transmission dynamics of AMR. We analysed 5124 human clinical isolates from Washington State Department of Health, 391 cattle clinical isolates from the Washington Animal Disease Diagnostic Laboratory and 1864 non-clinical isolates from foodborne disease research on dairies in the Pacific Northwest. Isolates were assigned <span class="hlt">profiles</span> based on phenotypic resistance to 11 anti-microbials belonging to eight classes. Salmonella Typhimurium (ST), Salmonella Newport (SN) and Salmonella Montevideo (SM) were the most common serovars in both humans and cattle. Multinomial logistic regression showed ST and SN from cattle had greater probability of resistance to multiple classes of anti-microbials than ST and SN from humans (P < 0.0001). While these findings could be consistent with the belief that cattle are a source of resistant ST and SN for people, occurrence of <span class="hlt">profiles</span> unique to cattle and not <span class="hlt">observed</span> in temporally related human isolates indicates these <span class="hlt">profiles</span> are circulating in cattle only. We used various measures to assess AMR diversity, conditional on the weighting of rare versus abundant <span class="hlt">profiles</span>. AMR <span class="hlt">profile</span> richness was greater in the common serovars from humans, although both source data sets were dominated by relatively few <span class="hlt">profiles</span>. The greater <span class="hlt">profile</span> richness in human Salmonella may be due to greater diversity of sources entering the human population compared to cattle or due to continuous evolution in the human environment. Also, AMR diversity was greater in clinical compared to non-clinical cattle Salmonella, and this could be due to anti-microbial selection <span class="hlt">pressure</span> in diseased cattle that received treatment. The use of bootstrapping techniques showed that although there were shared <span class="hlt">profiles</span> between humans and cattle, the expected and <span class="hlt">observed</span> number of <span class="hlt">profiles</span> was different, suggesting Salmonella and associated resistance from humans and cattle may not be</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/28198751','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/28198751"><span>The Role of Agonistic Striving in the Association Between Cortisol and High Blood <span class="hlt">Pressure</span>.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Ewart, Craig K; Elder, Gavin J; Jorgensen, Randall S; Fitzgerald, Sheila T</p> <p>2017-05-01</p> <p>A social action theory of chronic stress proposes that agonistic striving (seeking to influence or control others) impairs cardiovascular health by magnifying the impact of high adversity-induced cortisol levels on blood <span class="hlt">pressure</span>. We tested three predictions of social action theory: (1) the social action theory taxonomy of regulatory strivings characterizes young adults from high-adversity neighborhoods; (2) high cortisol levels predict high blood <span class="hlt">pressure</span> more reliably in the subgroup with the agonistic striving <span class="hlt">profile</span> than in subgroups with other <span class="hlt">profiles</span>; (3) the association of higher cortisol and higher blood <span class="hlt">pressure</span> with agonistic striving is not explained by negative affect (depressive symptoms/dysphoria, anger, hostility). Participants were young adults (N = 198, mean [SD] age = 32 [3.4] years); 71% female; 65% black) from disadvantaged urban neighborhoods. Motive <span class="hlt">profiles</span> (including agonistic strivings) were assessed using the Social Competence Interview. Cortisol levels were derived from saliva samples; blood <span class="hlt">pressure</span> level was obtained during two days of ambulatory monitoring. Psychological measures of negative affect were assessed using questionnaires. The predicted taxonomy of regulatory strivings was replicated in this sample; the interaction between cortisol and motive <span class="hlt">profile</span> was significant (F(2, 91) = 6.72, p = .002); analyses of simple effects disclosed that higher cortisol levels predicted higher ambulatory blood <span class="hlt">pressure</span> only in individuals who exhibited agonistic striving. Depressive symptoms/dysphoria, trait anger, and hostility were not correlated with agonistic striving, cortisol, or blood <span class="hlt">pressure</span>. Agonistic striving may represent a distinctive (and novel) social-cognitive mechanism of toxic stress and cardiovascular risk.</p> </li> </ol> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_19");'>19</a></li> <li><a href="#" onclick='return showDiv("page_20");'>20</a></li> <li class="active"><span>21</span></li> <li><a href="#" onclick='return showDiv("page_22");'>22</a></li> <li><a href="#" onclick='return showDiv("page_23");'>23</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div><!-- col-sm-12 --> </div><!-- row --> </div><!-- page_21 --> <div id="page_22" class="hiddenDiv"> <div class="row"> <div class="col-sm-12"> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_20");'>20</a></li> <li><a href="#" onclick='return showDiv("page_21");'>21</a></li> <li class="active"><span>22</span></li> <li><a href="#" onclick='return showDiv("page_23");'>23</a></li> <li><a href="#" onclick='return showDiv("page_24");'>24</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div> </div> <div class="row"> <div class="col-sm-12"> <ol class="result-class" start="421"> <li> <p><a target="_blank" onclick="trackOutboundLink('http://www.dtic.mil/docs/citations/ADA157108','DTIC-ST'); return false;" href="http://www.dtic.mil/docs/citations/ADA157108"><span>Compressor Research Facility F100 High <span class="hlt">Pressure</span> Compressor Inlet Total <span class="hlt">Pressure</span> and Swirl <span class="hlt">Profile</span> Simulation.</span></a></p> <p><a target="_blank" href="http://www.dtic.mil/">DTIC Science & Technology</a></p> <p></p> <p>1984-10-01</p> <p>SECTION I INTRODUCTION 1. GENERAL -.The F100 gas turbine engine currently powers the Air Force F-15 and F-16 aircraft . The compression section of this... Aircraft in designing these vanes and screens to provide the measured engine <span class="hlt">profiles</span>. lata acquisition system was defined and transported to Pratt and...WILLIAM W. COEHVRWALKER H. MITCHELL Compressor Test Group Chief, Technology Branch Technology Branch Turbine Engine Division Turbine Engine Division</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2014EGUGA..1614952D','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2014EGUGA..1614952D"><span>CO2 <span class="hlt">profile</span> retrievals from TCCON spectra</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Dohe, Susanne; Hase, Frank; Sepúlveda, Eliezer; García, Omaira; Wunch, Debra; Wennberg, Paul; Gómez-Peláez, Angel; Abshire, James B.; Wofsy, Steven C.; Schneider, Matthias; Blumenstock, Thomas</p> <p>2014-05-01</p> <p>The Total Carbon Column <span class="hlt">Observing</span> Network (TCCON) is a global network of ground-based Fourier Transform Spectrometers recording direct solar spectra in the near-infrared spectral region. With stringent requirements on the instrumentation, data processing and calibration, accurate and precise column-averaged abundances of CO2, CH4, N2O, HF, CO, H2O, and HDO are retrieved being an essential contribution for the validation of satellite data (e.g. GOSAT, OCO-2) and carbon cycle research (Olsen and Randerson, 2004). However, the determined column-averaged dry air mole fraction (DMF) contains no information about the vertical CO2 <span class="hlt">profile</span>, due to the use of a simple scaling retrieval within the common TCCON analysis, where the fitting algorithm GFIT (e.g. Yang et al., 2005) is used. In this presentation we will apply a different procedure for calculating trace gas abundances from the measured spectra, the fitting algorithm PROFFIT (Hase et. al., 2004) which has been shown to be in very good accordance with GFIT. PROFFIT additionally offers the ability to perform <span class="hlt">profile</span> retrievals in which the <span class="hlt">pressure</span> broadening effect of absorption lines is used to retrieve vertical gas <span class="hlt">profiles</span>, being of great interest especially for the CO2 modelling community. A new analyzing procedure will be shown and retrieved vertical CO2 <span class="hlt">profiles</span> of the TCCON sites Izaña (Tenerife, Canary Islands, Spain) and Lamont (Oklahoma, USA) will be presented and compared with simultaneously performed surface in-situ measurements and CO2 <span class="hlt">profiles</span> from different aircraft campaigns. References: - Hase, F. et al., J.Q.S.R.T. 87, 25-52, 2004. - Olsen, S.C. and Randerson, J.T., J.G.Res., 109, D023012, 2004. - Yang, Z. et al., J.Q.S.R.T., 90, 309-321, 2005.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/29433455','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/29433455"><span>Elevated blood <span class="hlt">pressure</span> among primary school children in Dar es salaam, Tanzania: prevalence and risk factors.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Muhihi, Alfa J; Njelekela, Marina A; Mpembeni, Rose N M; Muhihi, Bikolimana G; Anaeli, Amani; Chillo, Omary; Kubhoja, Sulende; Lujani, Benjamin; Maghembe, Mwanamkuu; Ngarashi, Davis</p> <p>2018-02-13</p> <p>Whilst the burden of non-communicable diseases is increasing in developing countries, little data is available on blood <span class="hlt">pressure</span> among Tanzanian children. This study aimed at determining the blood <span class="hlt">pressure</span> <span class="hlt">profiles</span> and risk factors associated with elevated blood <span class="hlt">pressure</span> among primary school children in Dar es Salaam, Tanzania. We conducted a cross sectional survey among 446 children aged 6-17 years from 9 randomly selected primary schools in Dar es Salaam. We measured blood <span class="hlt">pressure</span> using a standardized digital blood <span class="hlt">pressure</span> measuring machine (Omron Digital HEM-907, Tokyo, Japan). We used an average of the three blood <span class="hlt">pressure</span> readings for analysis. Elevated blood <span class="hlt">pressure</span> was defined as average systolic or diastolic blood pressure ≥ 90th percentile for age, gender and height. The proportion of children with elevated blood <span class="hlt">pressure</span> was 15.2% (pre-hypertension 4.4% and hypertension 10.8%). No significant gender differences were <span class="hlt">observed</span> in the prevalence of elevated BP. Increasing age and overweight/obese children were significantly associated with elevated BP (p = 0.0029 and p < 0.0001) respectively. Similar associations were <span class="hlt">observed</span> for age and overweight/obesity with hypertension. (p = 0.0506 and p < 0.0001) respectively. In multivariate analysis, age above 10 years (adjusted RR = 3.63, 95% CI = 1.03-7.82) was significantly and independently associated with elevated BP in this population of school age children. We <span class="hlt">observed</span> a higher proportion of elevated BP in this population of school age children. Older age and overweight/obesity were associated with elevated BP. Assessment of BP and BMI should be incorporated in school health program in Tanzania to identify those at risk so that appropriate interventions can be instituted before development of associated complications.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2016AGUOSPO34A3026S','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2016AGUOSPO34A3026S"><span>Variation of subsurface chlorophyll maximum layer from the vertical <span class="hlt">profiler</span> and in-situ <span class="hlt">observation</span> in the eastern coastal region of Korea (the East/Japan Sea)</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Son, Y. T.; Chang, K. I.; Nam, S.; Kang, D. J.</p> <p>2016-02-01</p> <p>Coastal monitoring buoy (called it as ESROB) has been continually operated to monitor meteorological (wind, air temperature, air <span class="hlt">pressure</span>, PAR) and oceanic properties (temperature, salinity, current, chlorophyll fluorescence, DO, turbidity) using equipment such as CTD, fluorometer and WQM (Water Quality Monitor) in the eastern coastal region of Korea (the East/Japan Sea) since April 2011. The ESROB produced temporal evolution of physical and biogeochemical parameters of the water column with high resolution of 10 min interval. In order to understand horizontal influence of physical and biogeochemical parameters on variation of subsurface chlorophyll maximum layer (SCM), interdisciplinary in-situ surveys with small R/V in the study area for about week were conducted in June/October 2014 and in May 2015. A wirewalker, a wave-driven vertically <span class="hlt">profiling</span> platform (Rainville and Pinkel 2001), was also deployed at two points (about 30 m and 80 m water depth) along cross-shore direction with the ESROB for about one or two weeks with in-situ survey durations. The wirewalker was equipped with CTD, turbidity and chlorophyll a fluorometer <span class="hlt">profiler</span>, which was completed approximately every 3 10 minute depending on sea surface state. The SCM was <span class="hlt">observed</span> in almost every deployment nearest coast, except for June in 2014, with variation of semi- and diurnal time periods. Temporal evolution of the wirewalker showed that disappearance and reoccurrence of the SCM within the water column in October 2014, which was associated with vertical mixing induced by strong wind stress. Low salinity plume in the surface layer and shoaling of bottom cold water were concurrently <span class="hlt">observed</span> after homogeneous water column, affecting another condition to the vertical distribution of chlorophyll a in this coastal region. Moreover in-situ <span class="hlt">observation</span> with densely points and temporal interval for 1 day revealed that distribution with high concentration of chlorophyll a on isopycnal was association with</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/7954916','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/7954916"><span>Release <span class="hlt">profiles</span> of phenytoin from new oral dosage form for the elderly.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Watanabe, A; Hanawa, T; Sugihara, M; Yamamoto, K</p> <p>1994-08-01</p> <p>Utilization of the solid mass containing phenytoin, sodium caseinate and microcrystalline cellulose (MCC) as a new dosage form for the elderly was studied. The solid mass was prepared by treatment of the powder mixture with high <span class="hlt">pressure</span> steam at 115 degrees C for 10 min. The stability of phenytoin in the solid mass was confirmed by infrared spectroscopy and high performance liquid chromatography. The extent of swelling of the solid mass containing phenytoin was investigated by water absorption test and gel strength test, and the swelling property was almost independent of the presence of phenytoin. The release <span class="hlt">profile</span> of phenytoin from the solid mass was determined under various conditions, and was found to be influenced by the extent of swelling and the swollen state. It was <span class="hlt">observed</span> that the protein adsorption to the phenytoin crystal surface and the addition of digestive enzyme also affected the release <span class="hlt">profile</span>. In water, the solid mass prepared from a ground mixture of phenytoin and MCC showed remarkable improvement of release <span class="hlt">profile</span> of phenytoin.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/20844075','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/20844075"><span>Effects of Concord grape juice on ambulatory blood <span class="hlt">pressure</span> in prehypertension and stage 1 hypertension.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Dohadwala, Mustali M; Hamburg, Naomi M; Holbrook, Monika; Kim, Brian H; Duess, Mai-Ann; Levit, Aaron; Titas, Megan; Chung, William B; Vincent, Felix B; Caiano, Tara L; Frame, Alissa A; Keaney, John F; Vita, Joseph A</p> <p>2010-11-01</p> <p>Consumption of flavonoid-containing foods may be useful for the management of hypertension. We investigated whether 100% Concord grape juice lowers blood <span class="hlt">pressure</span> in patients with prehypertension and stage 1 hypertension. We conducted a double-blind crossover study to compare the effects of grape juice (7 mL · kg⁻¹ · d⁻¹) and matched placebo beverage on 24-h ambulatory blood <span class="hlt">pressure</span>, stress-induced changes in blood <span class="hlt">pressure</span>, and biochemical <span class="hlt">profile</span>. Participants consumed each beverage for 8 wk with a 4-wk rest period between beverages. They ceased consumption of grapes and other flavonoid-containing beverages throughout the study. We enrolled 64 otherwise healthy patients taking no antihypertensive medications (31% women, 42% black, age 43 ± 12 y). Baseline mean (± SD) cuff blood <span class="hlt">pressure</span> was 138 ± 7 (systolic)/82 ± 7 (diastolic) mm Hg. No effects on the primary endpoint of 24-h mean systolic blood <span class="hlt">pressure</span>, diastolic blood <span class="hlt">pressure</span>, or stress-induced changes in blood <span class="hlt">pressure</span> were <span class="hlt">observed</span>. A secondary endpoint was nocturnal dip in systolic <span class="hlt">pressure</span>. At baseline, nocturnal <span class="hlt">pressure</span> was 8.3 ± 7.1% lower at night than during daytime. The mean nocturnal dip increased 1.4 percentage points after grape juice and decreased 2.3 percentage points after placebo (P = 0.005). Fasting blood glucose was 91 ± 10 mg/dL at baseline for the entire cohort. Glucose decreased 2 mg/dL after consumption of grape juice and increased 1 mg/dL after consuming the placebo (P = 0.03). We <span class="hlt">observed</span> no effect of grape juice on ambulatory blood <span class="hlt">pressure</span> in this cohort of relatively healthy individuals with modestly elevated blood <span class="hlt">pressure</span>. Secondary analyses suggested favorable effects on nocturnal dip and glucose homeostasis that may merit further investigation. This trial was registered at clinicaltrials.gov as NCT00302809.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/26113719','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/26113719"><span>HIGH-<span class="hlt">PRESSURE</span> PHYSICS. Direct <span class="hlt">observation</span> of an abrupt insulator-to-metal transition in dense liquid deuterium.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Knudson, M D; Desjarlais, M P; Becker, A; Lemke, R W; Cochrane, K R; Savage, M E; Bliss, D E; Mattsson, T R; Redmer, R</p> <p>2015-06-26</p> <p>Eighty years ago, it was proposed that solid hydrogen would become metallic at sufficiently high density. Despite numerous investigations, this transition has not yet been experimentally <span class="hlt">observed</span>. More recently, there has been much interest in the analog of this predicted metallic transition in the dense liquid, due to its relevance to planetary science. Here, we show direct <span class="hlt">observation</span> of an abrupt insulator-to-metal transition in dense liquid deuterium. Experimental determination of the location of this transition provides a much-needed benchmark for theory and may constrain the region of hydrogen-helium immiscibility and the boundary-layer <span class="hlt">pressure</span> in standard models of the internal structure of gas-giant planets. Copyright © 2015, American Association for the Advancement of Science.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=2583190','PMC'); return false;" href="https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=2583190"><span>Altered disc <span class="hlt">pressure</span> <span class="hlt">profile</span> after an osteoporotic vertebral fracture is a risk factor for adjacent vertebral body fracture</span></a></p> <p><a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pmc">PubMed Central</a></p> <p>Tzermiadianos, Michael N.; Renner, Susan M.; Phillips, Frank M.; Hadjipavlou, Alexander G.; Zindrick, Michael R.; Havey, Robert M.; Voronov, Michael</p> <p>2008-01-01</p> <p>This study investigated the effect of endplate deformity after an osteoporotic vertebral fracture in increasing the risk for adjacent vertebral fractures. Eight human lower thoracic or thoracolumbar specimens, each consisting of five vertebrae were used. To selectively fracture one of the endplates of the middle VB of each specimen a void was created under the target endplate and the specimen was flexed and compressed until failure. The fractured vertebra was subjected to spinal extension under 150 N preload that restored the anterior wall height and vertebral kyphosis, while the fractured endplate remained significantly depressed. The VB was filled with cement to stabilize the fracture, after complete evacuation of its trabecular content to ensure similar cement distribution under both the endplates. Specimens were tested in flexion-extension under 400 N preload while <span class="hlt">pressure</span> in the discs and strain at the anterior wall of the adjacent vertebrae were recorded. Disc <span class="hlt">pressure</span> in the intact specimens increased during flexion by 26 ± 14%. After cementation, disc <span class="hlt">pressure</span> increased during flexion by 15 ± 11% in the discs with un-fractured endplates, while decreased by 19 ± 26.7% in the discs with the fractured endplates. During flexion, the compressive strain at the anterior wall of the vertebra next to the fractured endplate increased by 94 ± 23% compared to intact status (p < 0.05), while it did not significantly change at the vertebra next to the un-fractured endplate (18.2 ± 7.1%, p > 0.05). Subsequent flexion with compression to failure resulted in adjacent fracture close to the fractured endplate in six specimens and in a non-adjacent fracture in one specimen, while one specimen had no adjacent fractures. Depression of the fractured endplate alters the <span class="hlt">pressure</span> <span class="hlt">profile</span> of the damaged disc resulting in increased compressive loading of the anterior wall of adjacent vertebra that predisposes it to wedge fracture. This data suggests that</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://ntrs.nasa.gov/search.jsp?R=20040110334&hterms=idea&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D30%26Ntt%3Didea','NASA-TRS'); return false;" href="https://ntrs.nasa.gov/search.jsp?R=20040110334&hterms=idea&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D30%26Ntt%3Didea"><span>Cloud Forcing and the Earth's Radiation Budget: New Ideas and New <span class="hlt">Observations</span></span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Barkstrom, Bruce R.</p> <p>1997-01-01</p> <p>1. NEW PERSPECTIVES ON CLOUD-RADIATIVE FORCING. When the Earth Radiation Budget Experiment (ERBE) produced the first measurements of cloud-radiative forcing, the climate community interpreted the results from a context in which the atmosphere was a single column, strongly coupled to the Earth's surface. 2. NEW PERSPECTIVES ON CLOUD-RADIATION <span class="hlt">OBSERVATIONS</span>. The climate community is also on the verge of adding a new dimension to its <span class="hlt">observational</span> capability. In classic thinking about atmospheric circulation and climate, surface <span class="hlt">pressure</span> was a readily available quantity. As meteorology developed, it was possible to develop quantitative predictions of future weather by bringing together a network of surface <span class="hlt">pressure</span> <span class="hlt">observations</span> and then of <span class="hlt">profiles</span> of temperature and humidity obtained from balloons. 3. ON COMBINING <span class="hlt">OBSERVATIONS</span> AND THE - ORY. With this new capability, it is natural to seek recognizable features in the <span class="hlt">observations</span> we make of the Earth. There are techniques we can use to group the remotely sensed data in the individual footprints into objects that we can track. We will present one such image-processing application to radiation budget data, showing how we can interpret the radiation budget data in terms of cloud systems that are organized into systematic patterns of behavior - an ecosystem-like view of cloud behavior.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/25546675','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/25546675"><span>Does the position or contact <span class="hlt">pressure</span> of the stethoscope make any difference to clinical blood <span class="hlt">pressure</span> measurements: an <span class="hlt">observational</span> study.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Pan, Fan; Zheng, Dingchang; He, Peiyu; Murray, Alan</p> <p>2014-12-01</p> <p>This study aimed to investigate the effect of stethoscope position and contact <span class="hlt">pressure</span> on auscultatory blood <span class="hlt">pressure</span> (BP) measurement. Thirty healthy subjects were studied. Two identical stethoscopes (one under the cuff, the other outside the cuff) were used to simultaneously and digitally record 2 channels of Korotkoff sounds during linear cuff <span class="hlt">pressure</span> deflation. For each subject, 3 measurements with different contact <span class="hlt">pressures</span> (0, 50, and 100 mm Hg) on the stethoscope outside the cuff were each recorded at 3 repeat sessions. The Korotkoff sounds were replayed twice on separate days to each of 2 experienced listeners to determine systolic and diastolic BPs (SBP and DBP). Variance analysis was performed to study the measurement repeatability and the effect of stethoscope position and contact <span class="hlt">pressure</span> on BPs. There was no significant BP difference between the 3 repeat sessions, between the 2 determinations from each listener, between the 2 listeners and between the 3 stethoscope contact <span class="hlt">pressures</span> (all P > 0.06). There was no significant SBP difference between the 2 stethoscope positions at the 2 lower stethoscope <span class="hlt">pressures</span> (P = 0.23 and 0.45), but there was a small (0.4 mm Hg, clinically unimportant) significant difference (P = 0.005) at the highest stethoscope <span class="hlt">pressure</span>. The key result was that, DBP from the stethoscope under the cuff was significantly lower than that from outside the cuff by 2.8 mm Hg (P < 0.001, 95% confidence interval -3.5 to -2.1 mm Hg). Since it is known that the traditional Korotkoff sound method, with the stethoscope outside the cuff, tends to give a higher DBP than the true intra-arterial <span class="hlt">pressure</span>, this study could suggest that the stethoscope position under the cuff, and closer to the arterial occlusion, might yield measurements closer to the actual invasive DBP.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://ntrs.nasa.gov/search.jsp?R=19720029617&hterms=NAD&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D50%26Ntt%3DNAD','NASA-TRS'); return false;" href="https://ntrs.nasa.gov/search.jsp?R=19720029617&hterms=NAD&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D50%26Ntt%3DNAD"><span>A <span class="hlt">pressure</span> scanning Fabry-Perot magnetometer.</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Fay, T. D.; Wyller, A. A.</p> <p>1971-01-01</p> <p>Description of an oscillating magnetic analyzer (KDP crystal plus Glan-Thompson prism) coupled to an echelle-interferometer spectrograph, and of single-slit magnetometer which by <span class="hlt">pressure</span> variations can be made to scan the entire <span class="hlt">profiles</span> of the circularly and linearly polarized Zeeman components. Freon gas is used as the scanner gas with wavelength displacements of 0.02 A per 0.1 in. Hg <span class="hlt">pressure</span> change at the NaD lines. The available scan range is 15 A in the visual spectral region.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/22112807','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/22112807"><span>Improved cortisol exposure-time <span class="hlt">profile</span> and outcome in patients with adrenal insufficiency: a prospective randomized trial of a novel hydrocortisone dual-release formulation.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Johannsson, G; Nilsson, A G; Bergthorsdottir, R; Burman, P; Dahlqvist, P; Ekman, B; Engström, B E; Olsson, T; Ragnarsson, O; Ryberg, M; Wahlberg, J; Biller, B M K; Monson, J P; Stewart, P M; Lennernäs, H; Skrtic, S</p> <p>2012-02-01</p> <p>Patients with treated adrenal insufficiency (AI) have increased morbidity and mortality rate. Our goal was to improve outcome by developing a once-daily (OD) oral hydrocortisone dual-release tablet with a more physiological exposure-time cortisol <span class="hlt">profile</span>. The aim was to compare pharmacokinetics and metabolic outcome between OD and the same daily dose of thrice-daily (TID) dose of conventional hydrocortisone tablets. We conducted an open, randomized, two-period, 12-wk crossover multicenter trial with a 24-wk extension at five university hospital centers. The trial enrolled 64 adults with primary AI; 11 had concomitant diabetes mellitus (DM). The same daily dose of hydrocortisone was administered as OD dual-release or TID. We evaluated cortisol pharmacokinetics. Compared with conventional TID, OD provided a sustained serum cortisol <span class="hlt">profile</span> 0-4 h after the morning intake and reduced the late afternoon and the 24-h cortisol exposure. The mean weight (difference = -0.7 kg, P = 0.005), systolic blood <span class="hlt">pressure</span> (difference = -5.5 mm Hg, P = 0.0001) and diastolic blood <span class="hlt">pressure</span> (difference: -2.3 mm Hg; P = 0.03), and glycated hemoglobin (absolute difference = -0.1%, P = 0.0006) were all reduced after OD compared with TID at 12 wk. Compared with TID, a reduction in glycated hemoglobin by 0.6% was <span class="hlt">observed</span> in patients with concomitant DM during OD (P = 0.004). The OD dual-release tablet provided a more circadian-based serum cortisol <span class="hlt">profile</span>. Reduced body weight, reduced blood <span class="hlt">pressure</span>, and improved glucose metabolism were <span class="hlt">observed</span> during OD treatment. In particular, glucose metabolism improved in patients with concomitant DM.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://ntrs.nasa.gov/search.jsp?R=20090026399&hterms=rain&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D80%26Ntt%3Drain','NASA-TRS'); return false;" href="https://ntrs.nasa.gov/search.jsp?R=20090026399&hterms=rain&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D80%26Ntt%3Drain"><span>Improved Atmospheric Boundary Layer <span class="hlt">Observations</span> of Tropical Cyclones with the Imaging Wind and Rain Airborne <span class="hlt">Profiler</span></span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Fernandez, D. Esteban; Chang, P.; Carswel, J.; Contreras, R.; Chu, T.; Asuzu, P.; Black, P.; Marks, F.</p> <p>2006-01-01</p> <p>The Imaging Wind and Rain Arborne <span class="hlt">Profilers</span> (IWRAP) is a dual-frequency, conically-scanning Doppler radar that measures high-resolution, dual-polarized, multi-beam C- and Ku-band reflectivity and Doppler velocity <span class="hlt">profiles</span> of the atmospheric boundary layer (ABL) within the inner core of hurricanes.From the datasets acquired during the 2002 through 20O5 hurricane seasons as part of the ONR Coupled Boundary Layer Air-Sea Transfer (CBLAST) program and the NOAA/NESDIS Ocean Winds and Rain experiments, very high resolution radar <span class="hlt">observations</span> of hurricanes have been acquired and made available to the CBLAST community. Of particular interest am the ABL wind fields and 3-D structures found within the inner core of hurricanes. As a result of these analysis, a limitation in the ability to retrieve the ABL wind field at very low altitudes was identified. This paper shows how this limitation has been removed and presents initial results demonstrating its new capabilities to derive the ABL wind field within the inner are of hurricanes to much lower altitudes than the ones the original system was capable of.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2016AGUFMSM33C2527M','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2016AGUFMSM33C2527M"><span>The O+ contribution and role on the ring current <span class="hlt">pressure</span> development for CMEs and CIRs using Van Allen Probes <span class="hlt">observations</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Mouikis, C.; Bingham, S.; Kistler, L. M.; Farrugia, C. J.; Spence, H. E.; Gkioulidou, M.</p> <p>2016-12-01</p> <p>The ring current responds differently to the different solar and interplanetary storm drivers such as coronal mass injections, (CME's), co-rotating interaction regions (CIR's), high-speed streamers and other structures. The resulting changes in the ring current particle <span class="hlt">pressure</span> change the global magnetic field, which affects the transport of the radiation belts. In order to determine the field changes during a storm, it is necessary to understand the transport, sources and losses of the particles that contribute to the ring current. The source population of the storm time ring current is the night side plasma sheet. We use Van Allen Probes <span class="hlt">observations</span> to determine the ring current <span class="hlt">pressure</span> contribution of the convecting plasma sheet H+ and O+ particles in the storm time development of the ring current. We compare storms that are related to different interplanetary drivers, CMEs and CIRs, as <span class="hlt">observed</span> at different local times. We find that during the storm main phase most of the ring current <span class="hlt">pressure</span> in the pre-midnight inner magnetosphere is contributed by particles on open drift paths that cause the development of a strong partial ring current that causes most of the main phase Dst drop. These particles can reach as deep as L 2 and their <span class="hlt">pressure</span> compares to the local magnetic field <span class="hlt">pressure</span> as deep as L 3. During the recovery phase, if these particles are not lost at the magnetopause, will become trapped and will contribute to the symmetric ring current. However, the largest difference between the CME and CIR ring current responses during the storm main and early recovery phases is caused by how the 15 - 60 keV O+ responds to these drivers.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://www.dtic.mil/docs/citations/ADA527193','DTIC-ST'); return false;" href="http://www.dtic.mil/docs/citations/ADA527193"><span>High Resolution Near-Bed <span class="hlt">Observations</span> in Winter Near Cape Hatteras, North Carolina</span></a></p> <p><a target="_blank" href="http://www.dtic.mil/">DTIC Science & Technology</a></p> <p></p> <p>2010-06-01</p> <p>Druck <span class="hlt">pressure</span> sensors, Campbell optical backscatter, and Seatech or Wetlabs CSTAR transmission sensors. All the transmissometers were 25 cm path...14.0 m Depth Flobee Tripods Sontek hydra Acoustic Doppler velocimeter (ADV), thermistor 3D flow velocity, temperature 8 Hz for 17.5 min hourly Pulse...coherent acoustic Doppler <span class="hlt">profiler</span> (PCADP), thermistor <span class="hlt">Profiles</span> of 3D flow velocity, temperature 1 Hz for 17.5 min hourly, 6.3 cm bins <span class="hlt">Pressure</span></p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2016AGUFM.A54F..01N','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2016AGUFM.A54F..01N"><span>Further Studies of <span class="hlt">Observational</span> Undersampling of the Surface Wind and <span class="hlt">Pressure</span> Fields in the Hurricane Inner-Core</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Nolan, D. S.; Klotz, B.</p> <p>2016-12-01</p> <p>Obtaining the best estimate of tropical cyclone (TC) intensity is vital for operational forecasting centers to produce accurate forecasts and to issue appropriate warnings. Aircraft data traditionally provide the most reliable information about the TC inner core and surrounding environment, but sampling strategies and <span class="hlt">observing</span> platforms associated with reconnaissance aircraft have inherent deficiencies that contribute to the uncertainty of the intensity estimate. One such instrument, the stepped frequency microwave radiometer (SFMR) on the NOAA WP-3D aircraft, provides surface wind speeds along the aircraft flight track. However, the standard "figure-4" flight pattern substantially limits the azimuthal coverage of the eyewall, such that the chance of <span class="hlt">observing</span> the true peak wind speeds is actually quite small. By simulating flights through a high-resolution simulation of Hurricane Isabel (2003), a previous study found that the 1-minute mean (maximum) SFMR winds underestimate a 6-hour running mean maximum wind (i.e. best track) by 7.5-10%. This project applies the same methodology to a suite of hurricane simulations with even higher resolution and more sophisticated physical parameterizations. These include the hurricane nature run of Nolan et al. (2013), the second hurricane nature run, a simulation of Hurricane Bill (2009), and additional idealized simulations. For the nature run cases, we find that the mean underestimate of the best-track estimate is 12-15%, considerably higher than determined from the Isabel simulation, while the other cases are similar to the previous result. Comparisons of the various cases indicates that the primary factors that lead to greater undersampling rates are storm size and storm asymmetry. Minimum surface <span class="hlt">pressure</span> is also frequently estimated from <span class="hlt">pressures</span> reported by dropsondes released into the eye, with a standard correction of 1 hPa per 10 knots of wind at the time of "splash." Statistics from thousands of simulated splash</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2016JaJAP..55fHA02C','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2016JaJAP..55fHA02C"><span>Mechanism of VHF H2 plasma production at high <span class="hlt">pressures</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Chen, Kuan-Chen; Chiu, Kuo-Feng; Chen, Chia-Fu; Lien, Cheng-Yang; Tsai, Yu-Jer; Lien, Ting-Kuei; Ogiwara, Kohei; Uchino, Kiichiro; Kawai, Yoshinobu</p> <p>2016-06-01</p> <p>A VHF H2 plasma was produced by a narrow-gap discharge at high <span class="hlt">pressures</span>, and the plasma parameters were examined with the Langmuir probe. A bi-Maxwellian electron distribution was <span class="hlt">observed</span> near the discharge electrode at a discharge gap of 10 mm, while a Maxwellian distribution was seen near the center. When the discharge gap was 15 mm, electrons had a Maxwellian distribution independent of the position. It was found that there must be a threshold in the discharge gap for stochastic heating to occur. The plasma potential near the discharge electrode was higher than that near the center of the interelectrode gap, suggesting the existence of negative ions. The simulation using the plasma hybrid code was carried out. The spatial <span class="hlt">profiles</span> of the density and temperature of electrons were similar to the experimental results. The plasma potential had a hill-like <span class="hlt">profile</span> that was quite different from the measured one. The negative ion density was negligible.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=4339756','PMC'); return false;" href="https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=4339756"><span>Cohort <span class="hlt">Profile</span>: HAART <span class="hlt">Observational</span> Medical Evaluation and Research (HOMER) Cohort</span></a></p> <p><a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pmc">PubMed Central</a></p> <p>Patterson, Sophie; Cescon, Angela; Samji, Hasina; Cui, Zishan; Yip, Benita; Lepik, Katherine J; Moore, David; Lima, Viviane D; Nosyk, Bohdan; Harrigan, P Richard; Montaner, Julio SG; Shannon, Kate; Wood, Evan; Hogg, Robert S</p> <p>2015-01-01</p> <p>Since 1986, antiretroviral therapy (ART) has been available free of charge to individuals living with HIV in British Columbia (BC), Canada, through the BC Centre of Excellence in HIV/AIDS (BC-CfE) Drug Treatment Program (DTP). The Highly Active Antiretroviral Therapy (HAART) <span class="hlt">Observational</span> Medical Evaluation and Research (HOMER) cohort was established in 1996 to maintain a prospective record of clinical measurements and medication <span class="hlt">profiles</span> of a subset of DTP participants initiating HAART in BC. This unique cohort provides a comprehensive data source to investigate mortality, prognostic factors and treatment response among people living with HIV in BC from the inception of HAART. Currently over 5000 individuals are enrolled in the HOMER cohort. Data captured include socio-demographic characteristics (e.g. sex, age, ethnicity, health authority), clinical variables (e.g. CD4 cell count, plasma HIV viral load, AIDS-defining illness, hepatitis C co-infection, mortality) and treatment variables (e.g. HAART regimens, date of treatment initiation, treatment interruptions, adherence data, resistance testing). Research findings from the HOMER cohort have featured in numerous high-impact peer-reviewed journals. The HOMER cohort collaborates with other HIV cohorts on both national and international scales to answer complex HIV-specific research questions, and welcomes input from external investigators regarding potential research proposals or future collaborations. For further information please contact the principal investigator, Dr Robert Hogg (robert_hogg@sfu.ca). PMID:24639444</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://ntrs.nasa.gov/search.jsp?R=19730002874&hterms=levels+maths&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D90%26Ntt%3Dlevels%2Bmaths','NASA-TRS'); return false;" href="https://ntrs.nasa.gov/search.jsp?R=19730002874&hterms=levels+maths&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D90%26Ntt%3Dlevels%2Bmaths"><span>An occultation satellite system for determining <span class="hlt">pressure</span> levels in the atmosphere</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Ungar, S. G.; Lusignan, B. B.</p> <p>1972-01-01</p> <p>An operational two-satellite microwave occultation system will establish a <span class="hlt">pressure</span> reference level to be used in fixing the temperature-<span class="hlt">pressure</span> <span class="hlt">profile</span> generated by the SIRS infrared sensor as a function of altitude. In the final error analysis, simulated data for the SIRS sensor were used to test the performance of the occultation system. The results of this analysis indicate that the occultation system is capable of measuring the altitude of the 300-mb level to within 24 mrms, given a maximum error of 2 K in the input temperature <span class="hlt">profile</span>. The effects of water vapor can be corrected by suitable climatological <span class="hlt">profiles</span>, and improvements in the accuracy of the SIRS instrument should yield additional improvements in the performance of the occultation system.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2018JPhCS1013a2031S','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2018JPhCS1013a2031S"><span>Argumentation skill <span class="hlt">profile</span> using “Toulmin Argumentation Pattern” analysis of high school student at Subang on topic hydrostatic <span class="hlt">pressure</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Syerliana, L.; Muslim; Setiawan, W.</p> <p>2018-05-01</p> <p>This study aims to know <span class="hlt">profile</span> of argumentation skill high school student at Kabupaten Subang. To achieve this goal, researcher conducted a descriptive study to analysis student test results of argumentation skill of 35 students XII SMAN. Data collection using argumentation test which has validation by expert and then it is analyzed using TAP (Toulmin Argumentation Pattern) which consist of some components such a data, claim, warrant, backing, and rebuttal on the topic of hydrostatic <span class="hlt">pressure</span>. The method used in this research is descriptive method. The result of this research show the student’s scientific argumentation skill is still low, this is proven by 54% average claim score, 38% data, 29% warrant, 35% backing and 35% rebuttal. These findings will serve as a basis for further research on innovative learning models that can improve students’ argumentation skill.</p> </li> </ol> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_20");'>20</a></li> <li><a href="#" onclick='return showDiv("page_21");'>21</a></li> <li class="active"><span>22</span></li> <li><a href="#" onclick='return showDiv("page_23");'>23</a></li> <li><a href="#" onclick='return showDiv("page_24");'>24</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div><!-- col-sm-12 --> </div><!-- row --> </div><!-- page_22 --> <div id="page_23" class="hiddenDiv"> <div class="row"> <div class="col-sm-12"> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_21");'>21</a></li> <li><a href="#" onclick='return showDiv("page_22");'>22</a></li> <li class="active"><span>23</span></li> <li><a href="#" onclick='return showDiv("page_24");'>24</a></li> <li><a href="#" onclick='return showDiv("page_25");'>25</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div> </div> <div class="row"> <div class="col-sm-12"> <ol class="result-class" start="441"> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/26513072','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/26513072"><span>Gonococcal infections in Austria: a long-term <span class="hlt">observation</span> of prevalence and resistance <span class="hlt">profiles</span> from 1999 to 2014.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Stary, Angelika; Heller-Vitouch, Claudia; Binder, Michael; Geusau, Alexandra; Stary, Georg; Rappersberger, Klemens; Komericki, Peter; Hoepfl, Reinhard; Haller, Maria</p> <p>2015-11-01</p> <p>The increase in minimum inhibitory concentrations (MICs) of cephalosporins for Neisseria gonorrhoeae has given rise to concerns regarding potentially untreatable gonococcal infections. The goal was to ascertain the prevalence of gonorrhea in a Viennese patient group and determine resistance patterns. Another objective was to evaluate resistance <span class="hlt">profiles</span> and MIC values of gonococcal isolates in an Austria-wide surveillance project. From 1999 to 2014, 350,000 individuals were tested for gonococci at the Viennese Outpatient Clinic. In addition, from 2010 to 2014, the MICs of recommended antibiotics was determined in 3,584 gonococcal isolates, initially by agar dilution and breakpoint determination, and, from 2012 onwards, by Etest®. During the <span class="hlt">observation</span> period, the prevalence of gonorrhea increased eightfold, with a significantly greater number of quinolone, penicillin, and tetracycline- resistant strains. In gonococcal strains isolated from across Austria, there was an increase in cefixime and ceftriaxone MICs toward breakpoints. Twenty-one isolates showed cefixime resistance, and while there was an increase in azithromycin resistance from 0.9 % (2013) to 3.2 % (2014), no resistance to ceftriaxone was <span class="hlt">observed</span>. Currently, there is no imminent risk of untreatable gonorrhea in Austria. However, continuing the use of gonococcal cultures as a diagnostic tool for establishing resistance <span class="hlt">profiles</span> is essential in order to monitor trends in the development of Neisseria (N.) gonorrhoeae resistance. © 2015 Deutsche Dermatologische Gesellschaft (DDG). Published by John Wiley & Sons Ltd.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://eric.ed.gov/?q=atmospheric+AND+pressure&pg=4&id=EJ512571','ERIC'); return false;" href="https://eric.ed.gov/?q=atmospheric+AND+pressure&pg=4&id=EJ512571"><span>Atmospheric <span class="hlt">Pressure</span> Indicator.</span></a></p> <p><a target="_blank" href="http://www.eric.ed.gov/ERICWebPortal/search/extended.jsp?_pageLabel=advanced">ERIC Educational Resources Information Center</a></p> <p>Salzsieder, John C.</p> <p>1995-01-01</p> <p>Discusses <span class="hlt">observable</span> phenomena related to air <span class="hlt">pressure</span>. Describes a simple, unobtrusive, semiquantitative device to monitor the changes in air <span class="hlt">pressure</span> that are associated with altitude, using a soft-drink bottle and a balloon. (JRH)</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/29307310','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/29307310"><span>Effects of green coffee extract supplementation on anthropometric indices, glycaemic control, blood <span class="hlt">pressure</span>, lipid <span class="hlt">profile</span>, insulin resistance and appetite in patients with the metabolic syndrome: a randomised clinical trial.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Roshan, Hanieh; Nikpayam, Omid; Sedaghat, Meghdad; Sohrab, Golbon</p> <p>2018-02-01</p> <p>This study was conducted to elucidate the effects of decaffeinated green coffee bean extract (GCE) on anthropometric indices, glycaemic control, blood <span class="hlt">pressure</span>, lipid <span class="hlt">profile</span>, insulin resistance and appetite in patients with the metabolic syndrome (Mets). Subjects were randomly allocated to consume 400 mg GCE or placebo capsules twice per d for 8 weeks. Both groups were advised to follow an energy balanced diet. After GCE supplementation, systolic blood <span class="hlt">pressure</span> (SBP) significantly reduced compared with the placebo group (-13·76 (sd 8·48) v. -6·56 (sd 9·58) mmHg, P=0·01). Also, GCE treatment significantly reduced fasting blood glucose (FBS) (-5·15 (sd 60·22) v. 29·42 (sd 40·01) mg/dl (-0·28 (SD 3·34) v. 1·63 (SD 2·22) mmol/l); P=0·03) and homoeostatic model of assessment of insulin resistance in comparison to placebo (-1·41 (sd 3·33) v. 1·23 (sd 3·84), P=0·02). In addition, waist circumference (-2·40 (sd 2·54) v. -0·66 (sd 1·17) cm, P=0·009) and appetite score (-1·44 (sd 1·72) v. -0·2 (sd 1·32), P=0·01) of the individuals supplemented with GCE indicated a significant decline. Besides, weight and BMI reduction in the intervention group was almost twice as much as the placebo group; however, this discrepancy was marginally significant (weight: -2·08 (sd 2·11) v. -0·92 (sd 1·30) kg, P=0·05). No difference was <span class="hlt">observed</span> in terms of glycated Hb (HbA1c) percentage and lipid <span class="hlt">profile</span> parameters between the two groups. To sum up, GCE administration had an ameliorating effect on some of the Mets components such as high SBP, high FBS and Mets main aetiological factors including insulin resistance and abdominal obesity. Furthermore, GCE supplementation could reduce appetite level.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=5566648','PMC'); return false;" href="https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=5566648"><span>Changes in body composition and metabolic <span class="hlt">profile</span> during interleukin 6 inhibition in rheumatoid arthritis</span></a></p> <p><a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pmc">PubMed Central</a></p> <p>Pereira, Bruno; Dutheil, Fréderic; Giraud, Charlotte; Courteix, Daniel; Sapin, Vincent; Frayssac, Thomas; Mathieu, Sylvain; Malochet‐Guinamand, Sandrine; Soubrier, Martin</p> <p>2017-01-01</p> <p>Abstract Background Rheumatoid arthritis (RA) is a chronic inflammatory disease characterized by increased mortality associated with cardiometabolic disorders including dyslipidaemia, insulin resistance, and cachectic obesity. Tumour necrosis factor inhibitors and interleukin 6 receptor blocker licensed for the treatment of RA decrease inflammation and could thus improve cardiovascular risk, but their effects on body composition and metabolic <span class="hlt">profile</span> need to be clarified. We investigated the effects of tocilizumab (TCZ), a humanized anti‐interleukin 6 receptor antibody, on body composition and metabolic <span class="hlt">profile</span> in patients treated for RA. Methods Twenty‐one active RA patients treated with TCZ were included in a 1 year open follow‐up study. Waist circumference, body mass index, blood <span class="hlt">pressure</span>, lipid <span class="hlt">profile</span>, fasting glucose, insulin, serum levels of adipokines and pancreatic/gastrointestinal hormones, and body composition (dual‐energy X‐ray absorptiometry) were measured at baseline and 6 and 12 months of treatment. At baseline, RA patients were compared with 21 non‐RA controls matched for age, sex, body mass index, and metabolic syndrome. Results Compared with controls, body composition was altered in RA with a decrease in total and appendicular lean mass, whereas fat composition was not modified. Among RA patients, 28.6% had a skeletal muscle mass index below the cut‐off point for sarcopaenia (4.8% of controls). After 1 year of treatment with TCZ, there was a significant weight gain without changes for fat mass. In contrast, an increase in lean mass was <span class="hlt">observed</span> with a significant gain in appendicular lean mass and skeletal muscle mass index between 6 and 12 months. Distribution of the fat was modified with a decrease in trunk/peripheral fat ratio and an increase in subcutaneous adipose tissue. No changes for waist circumference, blood <span class="hlt">pressure</span>, fasting glucose, and atherogenic index were <span class="hlt">observed</span>. Conclusions Despite weight gain during treatment</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/26476174','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/26476174"><span>Intragastric pH and <span class="hlt">pressure</span> <span class="hlt">profiles</span> after intake of the high-caloric, high-fat meal as used for food effect studies.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Koziolek, M; Schneider, F; Grimm, M; Modeβ, Chr; Seekamp, A; Roustom, T; Siegmund, W; Weitschies, W</p> <p>2015-12-28</p> <p>The intraluminal conditions of the fed stomach are critical for drug release from solid oral dosage forms and thus, often associated with the occurrence of food effects on oral bioavailability. In this study, intragastric pH and <span class="hlt">pressure</span> <span class="hlt">profiles</span> present after the ingestion of the high-caloric, high-fat (964 kcal) FDA standard breakfast were investigated in 19 healthy human subjects by using the telemetric SmartPill® capsule system (26 × 13 mm). Since the gastric emptying of such large non-digestible objects is typically accomplished by the migrating motor complex phase III activity, the time required for recurrence of fasted state motility determined the gastric emptying time (GET). Following the diet recommendations of the FDA guidance on food effect studies, the mean GET of the telemetric motility capsule was 15.3 ± 4.7 h. Thus, the high caloric value of the standard breakfast impeded gastric emptying before lunch in 18 out of 19 subjects. During its gastric transit, the capsule was exposed to highly dynamic conditions in terms of pH and <span class="hlt">pressure</span>, which were mainly dependent on further meal and liquid intake, as well as the intragastric capsule deposition behavior. Maximum pH values in the stomach were measured immediately after capsule intake. The median pH value of the 5 min period after capsule ingestion ranged between pH 3.3 and 5.3. Subsequently, the pH decreased relatively constantly and reached minimum values of pH 0-1 after approximately 4 h. The maximum <span class="hlt">pressure</span> within the stomach amounted to 293 ± 109 mbar and was clearly higher than the maximum <span class="hlt">pressure</span> measured at the ileocaecal junction (60 ± 35 mbar). The physiological data on the intraluminal conditions within the fed stomach generated in this study will hopefully contribute to a better understanding of food effects on oral drug product performance.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.fs.usda.gov/treesearch/pubs/24780','TREESEARCH'); return false;" href="https://www.fs.usda.gov/treesearch/pubs/24780"><span>Advective transport of CO2 in permeable media induced by atmospheric <span class="hlt">pressure</span> fluctuations: 2. <span class="hlt">Observational</span> evidence under snowpacks</span></a></p> <p><a target="_blank" href="http://www.fs.usda.gov/treesearch/">Treesearch</a></p> <p>W. J. Massman; J. M. Frank</p> <p>2006-01-01</p> <p>Meadow and forest CO2 amounts sampled beneath an approximately meter deep (steady state) snowpack at a subalpine site in southern Rocky Mountains of Wyoming are <span class="hlt">observed</span> to vary by nearly 200 ppm over periods ranging from 4 to 15 days. This work employs the model of periodic, <span class="hlt">pressure</span>-induced, advective transport in permeable media developed in...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2018AMT....11.2601S','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2018AMT....11.2601S"><span>Integrating uncertainty propagation in GNSS radio occultation retrieval: from excess phase to atmospheric bending angle <span class="hlt">profiles</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Schwarz, Jakob; Kirchengast, Gottfried; Schwaerz, Marc</p> <p>2018-05-01</p> <p>Global Navigation Satellite System (GNSS) radio occultation (RO) <span class="hlt">observations</span> are highly accurate, long-term stable data sets and are globally available as a continuous record from 2001. Essential climate variables for the thermodynamic state of the free atmosphere - such as <span class="hlt">pressure</span>, temperature, and tropospheric water vapor <span class="hlt">profiles</span> (involving background information) - can be derived from these records, which therefore have the potential to serve as climate benchmark data. However, to exploit this potential, atmospheric <span class="hlt">profile</span> retrievals need to be very accurate and the remaining uncertainties quantified and traced throughout the retrieval chain from raw <span class="hlt">observations</span> to essential climate variables. The new Reference Occultation Processing System (rOPS) at the Wegener Center aims to deliver such an accurate RO retrieval chain with integrated uncertainty propagation. Here we introduce and demonstrate the algorithms implemented in the rOPS for uncertainty propagation from excess phase to atmospheric bending angle <span class="hlt">profiles</span>, for estimated systematic and random uncertainties, including vertical error correlations and resolution estimates. We estimated systematic uncertainty <span class="hlt">profiles</span> with the same operators as used for the basic state <span class="hlt">profiles</span> retrieval. The random uncertainty is traced through covariance propagation and validated using Monte Carlo ensemble methods. The algorithm performance is demonstrated using test day ensembles of simulated data as well as real RO event data from the satellite missions CHAllenging Minisatellite Payload (CHAMP); Constellation <span class="hlt">Observing</span> System for Meteorology, Ionosphere, and Climate (COSMIC); and Meteorological Operational Satellite A (MetOp). The results of the Monte Carlo validation show that our covariance propagation delivers correct uncertainty quantification from excess phase to bending angle <span class="hlt">profiles</span>. The results from the real RO event ensembles demonstrate that the new uncertainty estimation chain performs robustly. Together</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/18853700','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/18853700"><span>Aerophagia and gastroesophageal reflux disease in patients using continuous positive airway <span class="hlt">pressure</span>: a preliminary <span class="hlt">observation</span>.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Watson, Nathaniel F; Mystkowski, Sue K</p> <p>2008-10-15</p> <p>Aerophagia is a complication of continuous positive airway <span class="hlt">pressure</span> (CPAP) therapy for sleep disordered breathing (SDB), whereupon air is forced into the stomach and bowel. Associated discomfort can result in CPAP discontinuation. We hypothesize that aerophagia is associated with gastroesophageal reflux disease (GERD) via mechanisms involving GERD related lower esophageal sphincter (LES) compromise. Twenty-two subjects with aerophagia and 22 controls, matched for age, gender, and body mass index, who were being treated with CPAP for SDB were compared in regard to clinical aspects of GERD, GERD associated habits, SDB severity as measured by polysomnography, and mean CPAP <span class="hlt">pressure</span>. More subjects with aerophagia had symptoms of GERD (77.3% vs. 36.4%; p < 0.01) and were on GERD related medications (45.5% vs. 18.2%, p < 0.05) than controls. Regarding polysomnography, mean oxygen saturation percentages were lower in the aerophagia group than controls (95.0% vs. 96.5%, p < 0.05). No other differences were <span class="hlt">observed</span>, including mean CPAP <span class="hlt">pressures</span>. No one in the aerophagia group (vs. 27.3% of the control group) was a current tobacco user (p < 0.01). There was no difference in caffeine or alcohol use between the 2 groups. These results imply aerophagia is associated with GERD symptoms and GERD related medication use. This finding suggests a relationship between GERD related LES pathophysiology and the development of aerophagia in patients with SDB treated with CPAP.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/23908391','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/23908391"><span>Application of high <span class="hlt">pressure</span> processing for shelf life extension of litchi fruits (Litchi chinensis cv. Bombai) during refrigerated storage.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Kaushik, Neelima; Kaur, Barjinder P; Rao, P Srinivasa</p> <p>2014-10-01</p> <p>This study attempts to report the effect of high <span class="hlt">pressure</span> processing (100, 200 and 300 MPa for 5, 10 and 15 min at 27 ± 2 ℃) on quality and shelf life extension of 'Bombai' variety peeled litchi fruits during refrigerated storage (5 ℃). High <span class="hlt">pressure</span> processing significantly increased total colour difference, browning index, drip loss and total soluble solids, whereas pH decreased after processing. Also, ascorbic acid content significantly decreased after high <span class="hlt">pressure</span> processing and retention of 83.5% was <span class="hlt">observed</span>. Texture <span class="hlt">profile</span> analysis showed that <span class="hlt">pressurization</span> significantly affected firmness and increased cohesiveness, gumminess, springiness and chewiness of litchi fruits. <span class="hlt">Pressure</span>-induced firming effect was <span class="hlt">observed</span> at 100 and 200 MPa <span class="hlt">pressure</span>. A maximum of 3.29, 3.24 and 3.77 log10 cycles reduction in aerobic mesophiles, yeast & mold and psychrotrophs count, respectively, was achieved after <span class="hlt">pressurization</span> of 300 MPa for 10 and 15 min treatments. During storage, samples treated at 300 MPa for 10 and 15 min showed relatively minimal changes in physico-chemical attributes, textural parameters and maintained lower viable microbial counts. Treatments at 300 MPa for 10 min and 15 min were found to enhance the shelf life of litchi fruits up to 32 days as compared to 12 days of untreated during refrigerated storage (5 ℃). © The Author(s) 2013 Reprints and permissions: sagepub.co.uk/journalsPermissions.nav.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2016AGUOSMG54B2033D','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2016AGUOSMG54B2033D"><span>Suspended Sediment Character in the Tidal Mekong River: <span class="hlt">Observations</span> from LISST <span class="hlt">Profiling</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Di Leonardo, D. R.; Allison, M. A.</p> <p>2016-02-01</p> <p>In two recent cooperative field campaigns, teams of researchers from the US and Vietnam collected hydrological and sedimentological data during a low flow season and a high flow season on the lower 100 km of the Song Hau distributary of the Mekong River. The objective of this study is to describe the forcing controls (e.g., tidal and riverine flow, water column stratification, resuspension) on suspended sediment grain size (e.g. mass, volume, granulometry, degree of flocculation) as measured by a Sequoia Scientific LISST 100X mounted on a <span class="hlt">profiling</span> CTD. LISST (Type C, 2.5-500 µm size range) casts were collected at five transects in the Song Hau distributary. Four transects were located in the Dinh An and the Tran De channels immediately above the ocean interface with one additional transect located above the channel bifurcation, 40 km from the river mouth. Casts were collected at multiple stations across each channel transect for 12 hour and 24 hour continuous periods. Stationary ADCP data was collected during each 5-15 minute cast period and used to characterize shear stress. Preliminary results from the LISST suggest that the majority of suspended sediment is in the silt and very fine sand range. Increasing concentrations of all size fractions towards the bed suggests a local sediment source. Bimodal grain size distributions, with the coarser peak in the 150 µm to 250 µm range, are <span class="hlt">observed</span> frequently, especially in the low discharge study. Grain size frequencies from the high discharge study tend to be more often unimodal. While there was effectively no salinity <span class="hlt">observed</span> during the October 2014 high flow season, a maximum of 25.8 PSU was <span class="hlt">observed</span> in the March 2015 low flow season. These results suggest that flocculation is an important process in the Mekong River, particularly during periods of higher salinity.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2018JPhCS1042a2004L','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2018JPhCS1042a2004L"><span>Numerical investigation on performance and sediment erosion of Francis runner with different guide vane <span class="hlt">profiles</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Lama, R.; Dahal, D. R.; Gautam, S.; Acharya, N.; Neopane, H.; Thapa, B. S.</p> <p>2018-06-01</p> <p>Francis turbine are ideal turbines for Himalayan and Andes region where both low and high-altitude mountains are located. Turbines operating in such regions face operational and maintenance problems due to the sediment erosion. In order to reduce the erosion effects on these components the design of components for higher sediment handling is essence. This paper presents performance analysis of Francis runner and prediction of sediment erosion on the runner blades for different operating conditions with different guide vane <span class="hlt">profiles</span>. The simulations were carried out for 11 guide vane opening angles using Tabakoff erosion model. At full load and best efficiency point the erosion was localized at <span class="hlt">pressure</span> side of runner blades outlet due to higher relative velocity. On the other hand, at part load condition, erosion was <span class="hlt">observed</span> at suction side of the blades. Application of asymmetric guide vane <span class="hlt">profile</span> NACA 4412 showed higher efficiency for all operating conditions with minimum erosion on runner blades in compare to symmetric guide vane <span class="hlt">profile</span> NACA 0012.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2016AGUFM.G24A..10Z','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2016AGUFM.G24A..10Z"><span>Merging altimeter data with Argo <span class="hlt">profiles</span> to improve <span class="hlt">observation</span> of tropical Pacific thermocline circulation and ENSO</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Zhang, D.; Lee, T.; Wang, F.; McPhaden, M. J.; Kessler, W. S.</p> <p>2016-12-01</p> <p>Meridional thermocline currents play an important role in the recharge and discharge of tropical Pacific warm water during the development and transition of ENSO cycles. Previous analyses have shown large variations of the equatorward meridional thermocline convergence/divergence on ENSO and decadal time scales in the interior ocean. The total convergence/divergence is however unknown due to the lack of long term <span class="hlt">observation</span> in the western boundary currents. Numerical modelling studies suggested a tendency of compensation between the interior and western boundary currents, but the exact compensation is model dependent. While Argo floats provide reasonable data coverage in the interior ocean, few floats are in the western boundary currents. Recent multi-mission satellite altimeter data and advanced processing techniques have resulted in higher resolution sea surface height anomaly (SSHA) products with better accuracy closer to the coasts. This study utilizes the statistical relationship between Argo dynamic height <span class="hlt">profiles</span> and altimeter SSHA to calculate geostrophic thermocline currents in both the interior ocean and the western boundary of the tropical Pacific. The derived thermocline currents in the western boundary are validated by a 3.5-year moored Acoustic Doppler Current <span class="hlt">Profiler</span> (ADCP) measurement in the Mindanao Current and by a series of glider surveys (Davis et al. 2012) in the Solomon Sea. The meridional transport timeseries of the interior and western boundary currents in the thermocline show different lead-lag relationships to the Nino 3.4 index. Results will be discussed in the context of recent 2014-2015 El Nino development and the potential contribution to the Tropical Pacific <span class="hlt">Observing</span> System (TPOS).</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=2954442','PMC'); return false;" href="https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=2954442"><span>Effects of Concord grape juice on ambulatory blood <span class="hlt">pressure</span> in prehypertension and stage 1 hypertension123</span></a></p> <p><a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pmc">PubMed Central</a></p> <p>Dohadwala, Mustali M; Hamburg, Naomi M; Holbrook, Monika; Kim, Brian H; Duess, Mai-Ann; Levit, Aaron; Titas, Megan; Chung, William B; Vincent, Felix B; Caiano, Tara L; Frame, Alissa A; Keaney, John F</p> <p>2010-01-01</p> <p>Background: Consumption of flavonoid-containing foods may be useful for the management of hypertension. Objective: We investigated whether 100% Concord grape juice lowers blood <span class="hlt">pressure</span> in patients with prehypertension and stage 1 hypertension. Design: We conducted a double-blind crossover study to compare the effects of grape juice (7 mL · kg−1 · d−1) and matched placebo beverage on 24-h ambulatory blood <span class="hlt">pressure</span>, stress-induced changes in blood <span class="hlt">pressure</span>, and biochemical <span class="hlt">profile</span>. Participants consumed each beverage for 8 wk with a 4-wk rest period between beverages. They ceased consumption of grapes and other flavonoid-containing beverages throughout the study. Results: We enrolled 64 otherwise healthy patients taking no antihypertensive medications (31% women, 42% black, age 43 ± 12 y). Baseline mean (±SD) cuff blood <span class="hlt">pressure</span> was 138 ± 7 (systolic)/82 ± 7 (diastolic) mm Hg. No effects on the primary endpoint of 24-h mean systolic blood <span class="hlt">pressure</span>, diastolic blood <span class="hlt">pressure</span>, or stress-induced changes in blood <span class="hlt">pressure</span> were <span class="hlt">observed</span>. A secondary endpoint was nocturnal dip in systolic <span class="hlt">pressure</span>. At baseline, nocturnal <span class="hlt">pressure</span> was 8.3 ± 7.1% lower at night than during daytime. The mean nocturnal dip increased 1.4 percentage points after grape juice and decreased 2.3 percentage points after placebo (P = 0.005). Fasting blood glucose was 91 ± 10 mg/dL at baseline for the entire cohort. Glucose decreased 2 mg/dL after consumption of grape juice and increased 1 mg/dL after consuming the placebo (P = 0.03). Conclusions: We <span class="hlt">observed</span> no effect of grape juice on ambulatory blood <span class="hlt">pressure</span> in this cohort of relatively healthy individuals with modestly elevated blood <span class="hlt">pressure</span>. Secondary analyses suggested favorable effects on nocturnal dip and glucose homeostasis that may merit further investigation. This trial was registered at clinicaltrials.gov as NCT00302809. PMID:20844075</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.osti.gov/servlets/purl/1175490','DOE-PATENT-XML'); return false;" href="https://www.osti.gov/servlets/purl/1175490"><span>High <span class="hlt">pressure</span> and high temperature apparatus</span></a></p> <p><a target="_blank" href="http://www.osti.gov/doepatents">DOEpatents</a></p> <p>Voronov, Oleg A.</p> <p>2005-09-13</p> <p>A design for high <span class="hlt">pressure</span>/high temperature apparatus and reaction cell to achieve .about.30 GPa <span class="hlt">pressure</span> in .about.1 cm volume and .about.100 GPa <span class="hlt">pressure</span> in .about.1 mm volumes and 20-5000.degree. C. temperatures in a static regime. The device includes <span class="hlt">profiled</span> anvils (28) action on a reaction cell (14, 16) containing the material (26) to be processed. The reaction cell includes a heater (18) surrounded by insulating layers and screens. Surrounding the anvils are cylindrical inserts and supporting rings (30-48) whose hardness increases towards the reaction cell. These volumes may be increased considerably if applications require it, making use of presses that have larger loading force capability, larger frames and using larger anvils.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2010ACPD...10.2357D','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2010ACPD...10.2357D"><span>Probabilistic description of ice-supersaturated layers in low resolution <span class="hlt">profiles</span> of relative humidity</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Dickson, N. C.; Gierens, K. M.; Rogers, H. L.; Jones, R. L.</p> <p>2010-02-01</p> <p>The global <span class="hlt">observation</span>, assimilation and prediction in numerical models of ice super-saturated (ISS) regions (ISSR) are crucial if the climate impact of aircraft condensations trails (contrails) is to be fully understood, and if, for example, contrail formation is to be avoided through aircraft operational measures. A robust assessment of the global distribution of ISSR will further this debate, and ISS event occurrence, frequency and spatial scales have recently attracted significant attention. The mean horizontal path length through ISSR as <span class="hlt">observed</span> by MOZAIC aircraft is 150 km (±250 km). The average vertical thickness of ISS layers is 600-800 m (±575 m) but layers ranging from 25 m to 3000 m have been <span class="hlt">observed</span>, with up to one third of ISS layers thought to be less than 100 m deep. Given their small scales compared to typical atmospheric model grid sizes, statistical representations of the spatial scales of ISSR are required, in both horizontal and vertical dimensions, if global occurrence of ISSR is to be adequately represented in climate models. This paper uses radiosonde launches made by the UK Meteorological Office, from the British Isles, Gibraltar, St. Helena and the Falkland Islands between January 2002 and December 2006, to investigate the probabilistic occurrence of ISSR. Specifically each radiosonde <span class="hlt">profile</span> is divided into 50- and 100-hPa <span class="hlt">pressure</span> layers, to emulate the coarse vertical resolution of some atmospheric models. Then the high resolution <span class="hlt">observations</span> contained within each thick <span class="hlt">pressure</span> layer are used to calculate an average relative humidity and an ISS fraction for each individual thick <span class="hlt">pressure</span> layer. These relative humidity <span class="hlt">pressure</span> layer descriptions are then linked through a probability function to produce an s-shaped curve describing the ISS fraction in any average relative humidity <span class="hlt">pressure</span> layer. An empirical investigation has shown that this one curve is statistically valid for mid-latitude locations, irrespective of season and</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/29351658','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/29351658"><span>Intensive versus conventional blood <span class="hlt">pressure</span> monitoring in a general practice population. The Blood <span class="hlt">Pressure</span> Reduction in Danish General Practice trial: a randomized controlled parallel group trial.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Klarskov, Pia; Bang, Lia E; Schultz-Larsen, Peter; Gregers Petersen, Hans; Benee Olsen, David; Berg, Ronan M G; Abrahamsen, Henrik; Wiinberg, Niels</p> <p>2018-01-17</p> <p>To compare the effect of a conventional to an intensive blood <span class="hlt">pressure</span> monitoring regimen on blood <span class="hlt">pressure</span> in hypertensive patients in the general practice setting. Randomized controlled parallel group trial with 12-month follow-up. One hundred and ten general practices in all regions of Denmark. One thousand forty-eight patients with essential hypertension. Conventional blood <span class="hlt">pressure</span> monitoring ('usual group') continued usual ad hoc blood <span class="hlt">pressure</span> monitoring by office blood <span class="hlt">pressure</span> measurements, while intensive blood <span class="hlt">pressure</span> monitoring ('intensive group') supplemented this with frequent home blood <span class="hlt">pressure</span> monitoring and 24-hour ambulatory blood <span class="hlt">pressure</span> monitoring. Mean day- and night-time systolic and diastolic 24-hour ambulatory blood <span class="hlt">pressure</span>. Change in systolic and diastolic office blood <span class="hlt">pressure</span> and change in cardiovascular risk <span class="hlt">profile</span>. Of the patients, 515 (49%) were allocated to the usual group, and 533 (51%) to the intensive group. The reductions in day- and night-time 24-hour ambulatory blood <span class="hlt">pressure</span> were similar (usual group: 4.6 ± 13.5/2.8 ± 82 mmHg; intensive group: 5.6 ± 13.0/3.5 ± 8.2 mmHg; P = 0.27/P = 0.20). Cardiovascular risk scores were reduced in both groups at follow-up, but more so in the intensive than in the usual group (P = 0.02). An intensive blood <span class="hlt">pressure</span> monitoring strategy led to a similar blood <span class="hlt">pressure</span> reduction to conventional monitoring. However, the intensive strategy appeared to improve patients' cardiovascular risk <span class="hlt">profile</span> through other effects than a reduction of blood <span class="hlt">pressure</span>. Clinical Trials NCT00244660. © The Author 2018. Published by Oxford University Press. All rights reserved. For permissions, please e-mail: journals.permissions@oup.com.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.osti.gov/servlets/purl/1093272','DOE-PATENT-XML'); return false;" href="https://www.osti.gov/servlets/purl/1093272"><span>High <span class="hlt">pressure</span> storage vessel</span></a></p> <p><a target="_blank" href="http://www.osti.gov/doepatents">DOEpatents</a></p> <p>Liu, Qiang</p> <p>2013-08-27</p> <p>Disclosed herein is a composite <span class="hlt">pressure</span> vessel with a liner having a polar boss and a blind boss a shell is formed around the liner via one or more filament wrappings continuously disposed around at least a substantial portion of the liner assembly combined the liner and filament wrapping have a support <span class="hlt">profile</span>. To reduce susceptible to rupture a locally disposed filament fiber is added.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2014AtmRe.140...28M','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2014AtmRe.140...28M"><span>Seasonal variability of aerosol vertical <span class="hlt">profiles</span> over east US and west Europe: GEOS-Chem/APM simulation and comparison with CALIPSO <span class="hlt">observations</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Ma, Xiaoyan; Yu, Fangqun</p> <p>2014-04-01</p> <p>In this study, we employed 5 years (2007-2011) of the CALIPSO level-3 monthly aerosol extinction product to compare with the GEOS-Chem/APM simulations for the same time period over two major industrial regions (east US and west Europe). The objective is to understand which aerosol types or species significantly determine the vertical <span class="hlt">profiles</span> by comparing the seasonal variability between the simulations and <span class="hlt">observations</span>. Our study shows that the model successfully produces the magnitude of aerosol extinction, <span class="hlt">profile</span> shape, and their seasonal variability <span class="hlt">observed</span> by CALIPSO over both east US (EUS) and west Europe (WEU). The extinctions below 1 km make up 44-79% to the total, from either the model simulations or satellite retrievals, with larger percentages in winter seasons (62-79%) and smaller percentages in summer seasons (44-57%) associated with the strength of vertical transport. The shape of the vertical <span class="hlt">profiles</span> has, therefore, a distinct seasonal variability, with a more like quasi-exponential shape in DJF (December, January, and February) and SON (September, October, and November) than in MAM (March, April, and May) and JJA (June, July, and August), which have been discerned from both measurements and simulations. Analysis of modeled aerosol species indicates that secondary particles (SP), containing sulfate, ammonia, nitrate, and secondary organic aerosols (SOAs), predominantly determine the total aerosol vertical <span class="hlt">profiles</span> while black carbon (BC), primary organic carbon (OC), and sea salt (SS), only account for a small fraction and are also limited near the surface. Mineral dust (DS) contributes more to the total extinction over WEU than over EUS, particularly in MAM, a result of being adjacent to the North Africa desert. Secondary inorganic aerosol (SIA, i.e. sulfate, ammonia, and nitrate) contributes most of the total SP mass in DJF and SON while SOA is particularly important in MAM and JJA when the emissions from leafed plants are active. Our study also</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2012APS..DPPTI2002S','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2012APS..DPPTI2002S"><span><span class="hlt">Observation</span> of improved and degraded confinement with driven flow on the LAPD</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Schaffner, David</p> <p>2012-10-01</p> <p>External continuous control over azimuthal flow and flow shear has been achieved in a linear plasma device for the first time allowing for a careful study of the effect of flow shear on <span class="hlt">pressure</span>-gradient-driven turbulence and transport in the edge of the Large Plasma Device (LAPD). The flow is controlled using biasable iris-like limiters situated axially between the cathode source and main plasma chamber. LAPD rotates spontaneously in the ion diamagnetic direction (IDD); positive limiter bias first reduces, then minimizes (producing a near-zero shear state), and finally reverses the flow into the electron diamagnetic direction (EDD). Degradation of particle confinement is <span class="hlt">observed</span> in the minimum shearing state and reduction in turbulent particle flux is <span class="hlt">observed</span> with increasing shearing in both flow directions. Near-complete suppression of turbulent particle flux is <span class="hlt">observed</span> for shearing rates comparable to the turbulent autocorrelation rate measured in the minimum shear state. Turbulent flux suppression is dominated by amplitude reduction in low-frequency (>10kHz) density fluctuations and a reduction in the radial correlation length. An increase in fluctuations for the highest shearing states is <span class="hlt">observed</span> with the emergence of a coherent mode which does not lead to net particle transport. Magnetic field is varied in order to explore whether and how field effects transport modification. Calculations of transport equations are used to predict density <span class="hlt">profiles</span> given source and temperature <span class="hlt">profiles</span> and can show the level of transport predicted to be necessary in order to produce the experimental density <span class="hlt">profiles</span> <span class="hlt">observed</span>. Finally, the variations of density fluctuations and radial correlation length are fit well with power-laws and compare favorably to simple models of shear suppression of transport.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/20298558','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/20298558"><span>Central blood <span class="hlt">pressure</span> and pulse wave velocity: relationship to target organ damage and cardiovascular morbidity-mortality in diabetic patients or metabolic syndrome. An <span class="hlt">observational</span> prospective study. LOD-DIABETES study protocol.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Gómez-Marcos, Manuel A; Recio-Rodríguez, José I; Rodríguez-Sánchez, Emiliano; Castaño-Sánchez, Yolanda; de Cabo-Laso, Angela; Sánchez-Salgado, Benigna; Rodríguez-Martín, Carmela; Castaño-Sánchez, Carmen; Gómez-Sánchez, Leticia; García-Ortiz, Luis</p> <p>2010-03-18</p> <p>Diabetic patients show an increased prevalence of non-dipping arterial <span class="hlt">pressure</span> pattern, target organ damage and elevated arterial stiffness. These alterations are associated with increased cardiovascular risk.The objectives of this study are the following: to evaluate the prognostic value of central arterial <span class="hlt">pressure</span> and pulse wave velocity in relation to the incidence and outcome of target organ damage and the appearance of cardiovascular episodes (cardiovascular mortality, myocardial infarction, chest pain and stroke) in patients with type 2 diabetes mellitus or metabolic syndrome. This is an <span class="hlt">observational</span> prospective study with 5 years duration, of which the first year corresponds to patient inclusion and initial evaluation, and the remaining four years to follow-up. The study will be carried out in the urban primary care setting. Consecutive sampling will be used to include patients diagnosed with type 2 diabetes between 20-80 years of age. A total of 110 patients meeting all the inclusion criteria and none of the exclusion criteria will be included. Patient age and sex, family and personal history of cardiovascular disease, and cardiovascular risk factors. Height, weight, heart rate and abdominal circumference. Laboratory tests: hemoglobin, lipid <span class="hlt">profile</span>, creatinine, microalbuminuria, glomerular filtration rate, blood glucose, glycosylated hemoglobin, blood insulin, fibrinogen and high sensitivity C-reactive protein. Clinical and 24-hour ambulatory (home) blood <span class="hlt">pressure</span> monitoring and self-measured blood <span class="hlt">pressure</span>. Common carotid artery ultrasound for the determination of mean carotid intima-media thickness. Electrocardiogram for assessing left ventricular hypertrophy. Ankle-brachial index. Retinal vascular study based on funduscopy with non-mydriatic retinography and evaluation of pulse wave morphology and pulse wave velocity using the SphygmoCor system. The medication used for diabetes, arterial hypertension and hyperlipidemia will be registered, together</p> </li> </ol> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_21");'>21</a></li> <li><a href="#" onclick='return showDiv("page_22");'>22</a></li> <li class="active"><span>23</span></li> <li><a href="#" onclick='return showDiv("page_24");'>24</a></li> <li><a href="#" onclick='return showDiv("page_25");'>25</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div><!-- col-sm-12 --> </div><!-- row --> </div><!-- page_23 --> <div id="page_24" class="hiddenDiv"> <div class="row"> <div class="col-sm-12"> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_21");'>21</a></li> <li><a href="#" onclick='return showDiv("page_22");'>22</a></li> <li><a href="#" onclick='return showDiv("page_23");'>23</a></li> <li class="active"><span>24</span></li> <li><a href="#" onclick='return showDiv("page_25");'>25</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div> </div> <div class="row"> <div class="col-sm-12"> <ol class="result-class" start="461"> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/25373956','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/25373956"><span>A transmission-line model of back-cavity dynamics for in-plane <span class="hlt">pressure</span>-differential microphones.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Kim, Donghwan; Kuntzman, Michael L; Hall, Neal A</p> <p>2014-11-01</p> <p><span class="hlt">Pressure</span>-differential microphones inspired by the hearing mechanism of a special parasitoid fly have been described previously. The designs employ a beam structure that rotates about two pivots over an enclosed back volume. The back volume is only partially enclosed due to open slits around the perimeter of the beam. The open slits enable incoming sound waves to affect the <span class="hlt">pressure</span> <span class="hlt">profile</span> in the microphone's back volume. The goal of this work is to study the net moment applied to <span class="hlt">pressure</span>-differential microphones by an incoming sound wave, which in-turn requires modeling the acoustic <span class="hlt">pressure</span> distribution within the back volume. A lumped-element distributed transmission-line model of the back volume is introduced for this purpose. It is discovered that the net applied moment follows a low-pass filter behavior such that, at frequencies below a corner frequency depending on geometrical parameters of the design, the applied moment is unaffected by the open slits. This is in contrast to the high-pass filter behavior introduced by barometric <span class="hlt">pressure</span> vents in conventional omnidirectional microphones. The model accurately predicts <span class="hlt">observed</span> curvature in the frequency response of a prototype <span class="hlt">pressure</span>-differential microphone 2 mm × 1 mm × 0.5 mm in size and employing piezoelectric readout.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.osti.gov/pages/biblio/1345846-ultrafast-laser-collision-induced-fluorescence-atmospheric-pressure-plasma','SCIGOV-DOEP'); return false;" href="https://www.osti.gov/pages/biblio/1345846-ultrafast-laser-collision-induced-fluorescence-atmospheric-pressure-plasma"><span>Ultrafast laser-collision-induced fluorescence in atmospheric <span class="hlt">pressure</span> plasma</span></a></p> <p><a target="_blank" href="http://www.osti.gov/pages">DOE PAGES</a></p> <p>Barnat, E. V.; Fierro, A.</p> <p>2017-03-07</p> <p>The implementation and demonstration of laser-collision-induced fluorescence (LCIF) generated in atmospheric <span class="hlt">pressure</span> helium environments is presented in this communication. As collision times are <span class="hlt">observed</span> to be fast (~10 ns), ultrashort pulse laser excitation (<100 fs) of the 2 3S to 3 3P (388.9 nm) is utilized to initiate the LCIF process. Both neutral-induced and electron-induced components of the LCIF are <span class="hlt">observed</span> in the helium afterglow plasma as the reduced electric field (E/N) is tuned from <0.1 Td to over 5 Td. Under the discharge conditions presented in this study (640 Torr He), the lower limit of electron density detection ismore » ~10 12 e cm -3. Lastly, the spatial <span class="hlt">profiles</span> of the 2 3S helium metastable and electrons are presented as functions of E/N to demonstrate the spatial resolving capabilities of the LCIF method.« less</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://ntrs.nasa.gov/search.jsp?R=19940020410&hterms=atmosphere+wind+profile&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D60%26Ntt%3Datmosphere%2Bwind%2Bprofile','NASA-TRS'); return false;" href="https://ntrs.nasa.gov/search.jsp?R=19940020410&hterms=atmosphere+wind+profile&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D60%26Ntt%3Datmosphere%2Bwind%2Bprofile"><span>Analyzing Martian winds and tracer concentrations using Mars <span class="hlt">Observer</span> data</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Houben, Howard C.</p> <p>1993-01-01</p> <p>During the courses of a day, the Mars <span class="hlt">Observer</span> spacecraft will acquire globally distributed <span class="hlt">profiles</span> of the martian atmosphere. It is highly desirable that this data be assembled into synoptic weather maps (complete specifications of the atmospheric <span class="hlt">pressure</span>, temperature, and winds at a given time), which can in turn be used as starting points in the study of many meteorological phenomena. Unfortunately, the special nature of the Mars <span class="hlt">Observer</span> data presents several challenges above and beyond the usual difficult problem of data initialization. Mars <span class="hlt">Observer</span> atmospheric data will consist almost exclusively of asynoptic vertical <span class="hlt">profiles</span> of temperatures (or radiances) and <span class="hlt">pressures</span>, whereas winds are generally in balance with horizontal gradients of these quantities (which will not be <span class="hlt">observed</span>). It will therefore be necessary to resort to dynamical models to analyze the wind fields. As a rule, data assimilation into atmospheric models can result in the generation of spurious gravity waves, so special steps must be taken to suppress these. In addition, the asynoptic nature of the data will require a four-dimensional (space and time) data assimilation scheme. The problem is to find a full set of meteorological fields (winds and temperatures) such that, when marched forward in time in the model, they achieve a best fit (in the weighted least-squares sense) to the data. The proposed solution is to develop a model especially for the Mars <span class="hlt">Observer</span> data assimilation problem. Gravity waves are filtered from the model by eliminating all divergence terms from the prognostic divergence equation. This leaves a diagnostic gradient wind relation between the rotational wind and the temperature field. The divergent wind is diagnosed as the wind required to maintain the gradient wind balance in the presence of the diabatic heating. The primitive equations of atmospheric dynamics (with three principal dependent variables) are thus reduced to a simpler system with a single prognostic</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2015ACP....15.3217F','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2015ACP....15.3217F"><span>Seasonal changes in the tropospheric carbon monoxide <span class="hlt">profile</span> over the remote Southern Hemisphere evaluated using multi-model simulations and aircraft <span class="hlt">observations</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Fisher, J. A.; Wilson, S. R.; Zeng, G.; Williams, J. E.; Emmons, L. K.; Langenfelds, R. L.; Krummel, P. B.; Steele, L. P.</p> <p>2015-03-01</p> <p>The combination of low anthropogenic emissions and large biogenic sources that characterizes the Southern Hemisphere (SH) leads to significant differences in atmospheric composition relative to the better studied Northern Hemisphere. This unique balance of sources poses significant challenges for global models. Carbon monoxide (CO) in particular is difficult to simulate in the SH due to the increased importance of secondary chemical production associated with the much more limited primary emissions. Here, we use aircraft <span class="hlt">observations</span> from the 1991-2000 Cape Grim Overflight Program (CGOP) and the 2009-2011 HIAPER (High-performance Instrumented Airborne Platform for Environmental Research) Pole-to-Pole <span class="hlt">Observations</span> (HIPPO), together with model output from the SH Model Intercomparison Project, to elucidate the drivers of CO vertical structure in the remote SH. <span class="hlt">Observed</span> CO vertical <span class="hlt">profiles</span> from Cape Grim are remarkably consistent with those <span class="hlt">observed</span> over the southern mid-latitudes Pacific 10-20 years later, despite major differences in time periods, flight locations, and sampling strategies between the two data sets. These similarities suggest the processes driving <span class="hlt">observed</span> vertical gradients are coherent across much of the remote SH and have not changed significantly over the past 2 decades. Model ability to simulate CO <span class="hlt">profiles</span> reflects the interplay between biogenic emission sources, the chemical mechanisms that drive CO production from these sources, and the transport that redistributes this CO throughout the SH. The four chemistry-climate and chemical transport models included in the intercomparison show large variability in their abilities to reproduce the <span class="hlt">observed</span> CO <span class="hlt">profiles</span>. In particular, two of the four models significantly underestimate vertical gradients in austral summer and autumn, which we find are driven by long-range transport of CO produced from oxidation of biogenic compounds. Comparisons between the models show that more complex chemical</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/26003622','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/26003622"><span>Method transfer from high-<span class="hlt">pressure</span> liquid chromatography to ultra-high-<span class="hlt">pressure</span> liquid chromatography. II. Temperature and <span class="hlt">pressure</span> effects.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Åsberg, Dennis; Samuelsson, Jörgen; Leśko, Marek; Cavazzini, Alberto; Kaczmarski, Krzysztof; Fornstedt, Torgny</p> <p>2015-07-03</p> <p>The importance of the generated temperature and <span class="hlt">pressure</span> gradients in ultra-high-<span class="hlt">pressure</span> liquid chromatography (UHPLC) are investigated and compared to high-<span class="hlt">pressure</span> liquid chromatography (HPLC). The drug Omeprazole, together with three other model compounds (with different chemical characteristics, namely uncharged, positively and negatively charged) were used. Calculations of the complete temperature <span class="hlt">profile</span> in the column at UHPLC conditions showed, in our experiments, a temperature difference between the inlet and outlet of 16 °C and a difference of 2 °C between the column center and the wall. Through van't Hoff plots, this information was used to single out the decrease in retention factor (k) solely due to the temperature gradient. The uncharged solute was least affected by temperature with a decrease in k of about 5% while for charged solutes the effect was more pronounced, with k decreases up to 14%. A <span class="hlt">pressure</span> increase of 500 bar gave roughly 5% increase in k for the uncharged solute, while omeprazole and the other two charged solutes gave about 25, 20 and 15% increases in k, respectively. The stochastic model of chromatography was applied to estimate the dependence of the average number of adsorption/desorption events (n) and the average time spent by a molecule in the stationary phase (τs) on temperature and <span class="hlt">pressure</span> on peak shape for the tailing, basic solute. Increasing the temperature yielded an increase in n and decrease in τs which resulted in less skew at high temperatures. With increasing <span class="hlt">pressure</span>, the stochastic modeling gave interesting results for the basic solute showing that the skew of the peak increased with <span class="hlt">pressure</span>. The conclusion is that <span class="hlt">pressure</span> effects are more pronounced for both retention and peak shape than the temperature effects for the polar or charged compounds in our study. Copyright © 2015 Elsevier B.V. All rights reserved.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017AGUFM.T51E0528C','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017AGUFM.T51E0528C"><span>Campaign-Style Measurements of Vertical Seafloor Deformation in the Cascadia Subduction Zone Using an Absolute Self-Calibrating <span class="hlt">Pressure</span> Recorder</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Cook, M. J.; Sasagawa, G. S.; Roland, E. C.; Schmidt, D. A.; Wilcock, W. S. D.; Zumberge, M. A.</p> <p>2017-12-01</p> <p>Seawater <span class="hlt">pressure</span> can be used to measure vertical seafloor deformation since small seafloor height changes produce measurable <span class="hlt">pressure</span> changes. However, resolving secular vertical deformation near subduction zones can be difficult due to <span class="hlt">pressure</span> gauge drift. A typical gauge drift rate of about 10 cm/year exceeds the expected secular rate of 1 cm/year or less in Cascadia. The absolute self-calibrating <span class="hlt">pressure</span> recorder (ASCPR) was developed to solve the issue of gauge drift by using a deadweight calibrator to make campaign-style measurements of the absolute seawater <span class="hlt">pressure</span>. <span class="hlt">Pressure</span> gauges alternate between <span class="hlt">observing</span> the ambient seawater <span class="hlt">pressure</span> and the deadweight calibrator <span class="hlt">pressure</span>, which is an accurately known reference value, every 10-20 minutes for several hours. The difference between the known reference <span class="hlt">pressure</span> and the <span class="hlt">observed</span> seafloor <span class="hlt">pressure</span> allows offsets and transients to be corrected to determine the true, absolute seafloor <span class="hlt">pressure</span>. Absolute seafloor <span class="hlt">pressure</span> measurements provide a great utility for geodetic deformation studies. The measurements provide instrument-independent, benchmark values that can be used far into the future as epoch points in long-term time series or as important calibration points for other continuous <span class="hlt">pressure</span> records. The ASCPR was first deployed in Cascadia in 2014 and 2015, when seven concrete seafloor benchmarks were placed along a trench-perpendicular <span class="hlt">profile</span> extending from 20 km to 105 km off the central Oregon coast. Two benchmarks have ASCPR measurements that span three years, one benchmark spans two years, and four benchmarks span one year. Measurement repeatability is currently 3 to 4 cm, but we anticipate accuracy on the order of 1 cm with improvements to the instrument metrology and processing tidal and non-tidal oceanographic signals.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/19664355','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/19664355"><span>[Topic efficacy of ialuronic acid associated with argentic sulphadiazine (Connettivina Plus) in the treatment of <span class="hlt">pressure</span> sores: a prospective <span class="hlt">observational</span> cohort study].</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Paghetti, Angela; Bellingeri, Andrea; Pomponio, Giovanni; Sansoni, Julita; Paladino, Dario</p> <p>2009-01-01</p> <p>The aim of this <span class="hlt">observational</span> study was to evaluate the efficacy, tolerability and methods of application of ialuronic acid associated with argentic sulphadiazine (Connettivina Plus) in routine clinical activity, on a target of "complex" patients with <span class="hlt">pressure</span> sores, for the most realistic assessment possible. The study comprised 127 patients hospitalized between January 2006 and December 2007, who received ialuronic acid associated with argentic sulphadiazine in addition to the standard treatment. Inclusion criteria were th presence of at least one stage 2 or 3 <span class="hlt">pressure</span> sore (NPUAP '89 classification), <span class="hlt">pressure</span> sore that the researcher had already decided to treat using ialuronic acid associated with argentic sulphadiazine , according to hospital protocol, area of the lesion less than 25cm2, patient age 18 years or more, informed patient consensus. Patients with these characteristics were , however, excluded if they did not provide written consent or if they had one of the following: presence of <span class="hlt">pressure</span> sores with escara, concomitant neoplastic disease, concomitant insulin-dependent diabetes or other pathologies that interfere with skin regeneration, allergic diasthesis (acclaimed or presumed) to ialuronic acid - argentic sulphadiazine, inability / refusal to undergo all the subsequent controls required by the study. Improvement or complete healing of the <span class="hlt">pressure</span> sores was <span class="hlt">observed</span> in 67% of patients at early follow-up (10 days), increasing to 76% and 87% at 20 and 35 day controls respectively. The Push tool further improved in patients who carried on treatment. Use of ialuronic acid associated with argentic sulphadiazine was effective for treating grade 2-3 <span class="hlt">pressure</span> sores in patients with chronic lesions and its efficacy was confirmed in association with both advanced and traditional types of medication.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2005AGUFM.A23C0957Z','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2005AGUFM.A23C0957Z"><span>Derivation of Cloud Heating Rate <span class="hlt">Profiles</span> using <span class="hlt">observations</span> of Mixed-Phase Arctic Clouds: Impacts of Solar Zenith Angle</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Zhang, G.; McFarquhar, G.; Poellot, M.; Verlinde, J.; Heymsfield, A.; Kok, G.</p> <p>2005-12-01</p> <p>Arctic stratus clouds play an important role in the energy balance of the Arctic region. Previous studies have suggested that Arctic stratus persist due to a balance among cloud top radiation cooling, latent heating, ice crystal fall out and large scale forcing. In this study, radiative heating <span class="hlt">profiles</span> through Arctic stratus are computed using cloud, surface and thermodynamic <span class="hlt">observations</span> obtained during the Mixed-Phase Arctic Cloud Experiment (M-PACE) as input to the radiative transfer model STREAMER. In particular, microphysical and macrophycial cloud properties such as phase, water content, effective particle size, particle shape, cloud height and cloud thickness were derived using data collected by in-situ sensors on the University of North Dakota (UND) Citation and ground-based remote sensors at Barrow and Oliktok Point. Temperature <span class="hlt">profiles</span> were derived from radiosonde launches and a fresh snow surface was assumed. One series of sensitivity studies explored the dependence of the heating <span class="hlt">profile</span> on the solar zenith angle. For smaller solar zenith angles, more incoming solar radiation is received at cloud top acting to counterbalance infrared cooling. As solar zenith angle in the Arctic is large compared to low latitudes, a large solar zenith angle may contribute to the longevity of these clouds.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/24639444','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/24639444"><span>Cohort <span class="hlt">Profile</span>: HAART <span class="hlt">Observational</span> Medical Evaluation and Research (HOMER) cohort.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Patterson, Sophie; Cescon, Angela; Samji, Hasina; Cui, Zishan; Yip, Benita; Lepik, Katherine J; Moore, David; Lima, Viviane D; Nosyk, Bohdan; Harrigan, P Richard; Montaner, Julio S G; Shannon, Kate; Wood, Evan; Hogg, Robert S</p> <p>2015-02-01</p> <p>Since 1986, antiretroviral therapy (ART) has been available free of charge to individuals living with HIV in British Columbia (BC), Canada, through the BC Centre of Excellence in HIV/AIDS (BC-CfE) Drug Treatment Program (DTP). The Highly Active Antiretroviral Therapy (HAART) <span class="hlt">Observational</span> Medical Evaluation and Research (HOMER) cohort was established in 1996 to maintain a prospective record of clinical measurements and medication <span class="hlt">profiles</span> of a subset of DTP participants initiating HAART in BC. This unique cohort provides a comprehensive data source to investigate mortality, prognostic factors and treatment response among people living with HIV in BC from the inception of HAART. Currently over 5000 individuals are enrolled in the HOMER cohort. Data captured include socio-demographic characteristics (e.g. sex, age, ethnicity, health authority), clinical variables (e.g. CD4 cell count, plasma HIV viral load, AIDS-defining illness, hepatitis C co-infection, mortality) and treatment variables (e.g. HAART regimens, date of treatment initiation, treatment interruptions, adherence data, resistance testing). Research findings from the HOMER cohort have featured in numerous high-impact peer-reviewed journals. The HOMER cohort collaborates with other HIV cohorts on both national and international scales to answer complex HIV-specific research questions, and welcomes input from external investigators regarding potential research proposals or future collaborations. For further information please contact the principal investigator, Dr Robert Hogg (robert_hogg@sfu.ca). © The Author 2014; all rights reserved. Published by Oxford University Press on behalf of the International Epidemiological Association.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2018PhRvB..97f4509W','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2018PhRvB..97f4509W"><span><span class="hlt">Pressure</span> dependence of coherence-incoherence crossover behavior in KFe2As2 <span class="hlt">observed</span> by resistivity and 75As-NMR/NQR</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Wiecki, P.; Taufour, V.; Chung, D. Y.; Kanatzidis, M. G.; Bud'ko, S. L.; Canfield, P. C.; Furukawa, Y.</p> <p>2018-02-01</p> <p>We present the results of 75As nuclear magnetic resonance (NMR), nuclear quadrupole resonance (NQR), and resistivity measurements in KFe2As2 under <span class="hlt">pressure</span> (p ). The temperature dependence of the NMR shift, nuclear spin-lattice relaxation time (T1), and resistivity show a crossover between a high-temperature incoherent, local-moment behavior and a low-temperature coherent behavior at a crossover temperature (T*). T* is found to increase monotonically with <span class="hlt">pressure</span>, consistent with increasing hybridization between localized 3 d orbital-derived bands with the itinerant electron bands. No anomaly in T* is seen at the critical <span class="hlt">pressure</span> pc=1.8 GPa where a change of slope of the superconducting (SC) transition temperature Tc(p ) has been <span class="hlt">observed</span>. In contrast, Tc(p ) seems to correlate with antiferromagnetic spin fluctuations in the normal state as measured by the NQR 1 /T1 data, although such a correlation cannot be seen in the replacement effects of A in the A Fe2As2 (A =K , Rb, Cs) family. In the superconducting state, two T1 components are <span class="hlt">observed</span> at low temperatures, suggesting the existence of two distinct local electronic environments. The temperature dependence of the short T1 s indicates a nearly gapless state below Tc. On the other hand, the temperature dependence of the long component 1 /T1 L implies a large reduction in the density of states at the Fermi level due to the SC gap formation. These results suggest a real-space modulation of the local SC gap structure in KFe2As2 under <span class="hlt">pressure</span>.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.osti.gov/biblio/1425286-pressure-dependence-coherence-incoherence-crossover-behavior-kfe2as2-observed-resistivity-nmr-nqr','SCIGOV-STC'); return false;" href="https://www.osti.gov/biblio/1425286-pressure-dependence-coherence-incoherence-crossover-behavior-kfe2as2-observed-resistivity-nmr-nqr"><span><span class="hlt">Pressure</span> Dependence of Coherence-Incoherence Crossover Behavior in KFe 2As 2 <span class="hlt">Observed</span> by Resistivity and 75As-NMR/NQR.</span></a></p> <p><a target="_blank" href="http://www.osti.gov/search">DOE Office of Scientific and Technical Information (OSTI.GOV)</a></p> <p>Wiecki, P.; Taufour, V.; Chung, D. Y.</p> <p></p> <p>We present the results of 75As nuclear magnetic resonance (NMR), nuclear quadrupole resonance (NQR), and resistivity measurements in KFe 2As 2 under <span class="hlt">pressure</span> (p). The temperature dependence of the NMR shift, nuclear spin-lattice relaxation time (T1), and resistivity show a crossover between a high-temperature incoherent, local-moment behavior and a low-temperature coherent behavior at a crossover temperature (T *). T * is found to increase monotonically with <span class="hlt">pressure</span>, consistent with increasing hybridization between localized 3d orbitalderived bands with the itinerant electron bands. No anomaly in T * is seen at the critical <span class="hlt">pressure</span> pc = 1.8 GPa where a change ofmore » slope of the superconducting (SC) transition temperature Tc(p) has been <span class="hlt">observed</span>. In contrast, Tc(p) seems to correlate with antiferromagnetic spin fluctuations in the normal state as measured by the NQR 1/T1 data, although such a correlation cannot be seen in the replacement effects of A in the KFe 2As 2 (A = K, Rb, Cs) family. In the superconducting state, two T1 components are <span class="hlt">observed</span> at low temperatures, suggesting the existence of two distinct local electronic environments. The temperature dependence of the short T1s indicates a nearly gapless state below Tc. On the other hand, the temperature dependence of the long component 1/T1L implies a large reduction in the density of states at the Fermi level due to the SC gap formation. These results suggest a real-space modulation of the local SC gap structure in KFe 2As 2 under <span class="hlt">pressure</span>.« less</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/24270899','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/24270899"><span>Strategies to prevent ventilation-associated pneumonia: the effect of cuff <span class="hlt">pressure</span> monitoring techniques and tracheal tube type on aspiration of subglottic secretions: an in-vitro study.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Carter, Eleanor L; Duguid, Alasdair; Ercole, Ari; Matta, Basil; Burnstein, Rowan M; Veenith, Tonny</p> <p>2014-03-01</p> <p>Ventilation-associated pneumonia (VAP) is the commonest nosocomial infection in intensive care. Implementation of a VAP prevention care bundle is a proven method to reduce its incidence. The UK care bundle recommends maintenance of the tracheal tube cuff <span class="hlt">pressure</span> at 20 to 30  cmH₂O with 4-hourly <span class="hlt">pressure</span> checks and use of tracheal tubes with subglottic aspiration ports in patients admitted for more than 72  h. To evaluate the effects of tracheal tube type and cuff <span class="hlt">pressure</span> monitoring technique on leakage of subglottic secretions past the tracheal tube cuff. Bench-top study. Laboratory. A model adult trachea with simulated subglottic secretions was intubated with a tracheal tube with the cuff inflated to 25  cmH₂O. Experiments were conducted using a Portex <span class="hlt">Profile</span> Soft Seal tracheal tube with three cuff <span class="hlt">pressure</span> monitoring strategies and using a Portex SACETT tracheal tube with intermittent cuff <span class="hlt">pressure</span> checks. Rate of simulated secretion leakage past the tracheal tube cuff. Mean ± SD leakage of fluid past the <span class="hlt">Profile</span> Soft Seal tracheal tube cuff was 2.25 ± 1.49  ml  min⁻¹ with no monitoring of cuff <span class="hlt">pressure</span>, 2.98 ± 1.63  ml  min⁻¹ with intermittent cuff <span class="hlt">pressure</span> monitoring and 3.83 ± 2.17  ml  min⁻¹ with continuous cuff <span class="hlt">pressure</span> monitoring (P <0.001). Using a SACETT tracheal tube with a subglottic aspiration port and aspirating the simulated secretions prior to intermittent cuff <span class="hlt">pressure</span> checks reduced the leakage rate to 0.50 ± 0.48  ml  min⁻¹ (P <0.001). Subglottic secretions leaked past the tracheal tube cuff with all tube types and cuff <span class="hlt">pressure</span> monitoring strategies in this model. Significantly higher rates were <span class="hlt">observed</span> with continuous cuff <span class="hlt">pressure</span> monitoring and significantly lower rates were <span class="hlt">observed</span> when using a tracheal tube with a subglottic aspiration port. Further evaluation of medical device performance is needed in order to design more effective VAP prevention strategies.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=3900925','PMC'); return false;" href="https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=3900925"><span>Characterization of a Setup to test the Impact of High-Amplitude <span class="hlt">Pressure</span> Waves on Living Cells</span></a></p> <p><a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pmc">PubMed Central</a></p> <p>Schmidt, Mischa; Kahlert, Ulf; Wessolleck, Johanna; Maciaczyk, Donata; Merkt, Benjamin; Maciaczyk, Jaroslaw; Osterholz, Jens; Nikkhah, Guido; Steinhauser, Martin O.</p> <p>2014-01-01</p> <p>The impact of <span class="hlt">pressure</span> waves on cells may provide several possible applications in biology and medicine including the direct killing of tumors, drug delivery or gene transfection. In this study we characterize the physical properties of mechanical <span class="hlt">pressure</span> waves generated by a nanosecond laser pulse in a setup with well-defined cell culture conditions. To systematically characterize the system on the relevant length and time scales (micrometers and nanoseconds) we use photon Doppler velocimetry (PDV) and obtain velocity <span class="hlt">profiles</span> of the cell culture vessel at the passage of the <span class="hlt">pressure</span> wave. These <span class="hlt">profiles</span> serve as input for numerical <span class="hlt">pressure</span> wave simulations that help to further quantify the <span class="hlt">pressure</span> conditions on the cellular length scale. On the biological level we demonstrate killing of glioblastoma cells and quantify experimentally the <span class="hlt">pressure</span> threshold for cell destruction. PMID:24458018</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/29205036','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/29205036"><span>Metabolic <span class="hlt">Profile</span> of Zearalenone in Liver Microsomes from Different Species and Its in Vivo Metabolism in Rats and Chickens Using Ultra High-<span class="hlt">Pressure</span> Liquid Chromatography-Quadrupole/Time-of-Flight Mass Spectrometry.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Yang, Shupeng; Zhang, Huiyan; Sun, Feifei; De Ruyck, Karl; Zhang, Jinzhen; Jin, Yue; Li, Yanshen; Wang, Zhanhui; Zhang, Suxia; De Saeger, Sarah; Zhou, Jinhui; Li, Yi; De Boevre, Marthe</p> <p>2017-12-27</p> <p>To explore differences of zearalenone (ZEN) metabolism between various species, phase I and II metabolism by liver microsomes of animals and human were investigated using ultra high-<span class="hlt">pressure</span> liquid chromatography-quadrupole/time-of-flight mass spectrometry (UHPLC-Q/TOF MS). A total of 24 metabolites were identified, among which 12 were reported for the first time. Reduction, hydroxylation, and glucuronidation were the major metabolic pathways of ZEN, and significant differences in various species were also <span class="hlt">observed</span>. Reduction was the main reaction in swine and human, whereas hydroxylation was predominant in rats, chickens, goats, and cows in in vitro systems. Furthemore, in vivo metabolism of ZEN in rats and chickens was investigated, and 23 and 6 metabolites were identified in each species, respectively. Reduction, hydroxylation, and glucuronidation were the major metabolic pathways in rats, while reduction and sulfation predominated in chickens. These results further enrich the biotransformation <span class="hlt">profile</span> of ZEN, providing a helpful reference for assessing the risks to animals and humans.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2012AGUFMOS13B1730B','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2012AGUFMOS13B1730B"><span>Long-term <span class="hlt">observations</span> of seafloor <span class="hlt">pressure</span> variations at Lucky Strike volcano, Mid-Atlantic Ridge</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Ballu, V.; de Viron, O.; Crawford, W. C.; Cannat, M.; Escartin, J.</p> <p>2012-12-01</p> <p>Lucky Strike volcano is a segment-center volcano on the Mid-Atlantic Ridge at 37°N. Extensive faulting reveals an important tectonic component in its formation, while a seismically imaged axial magma chamber reflector and active high-temperature hydrothermal vents reveal an important present-day magmatic component. Lucky Strike volcano has been the subject of long-term multidisciplinary seafloor <span class="hlt">observations</span> to understand relations between magmatism, tectonism, hydrothermal circulation, biology and chemistry as part of the MoMAR (Monitoring of the Mid-Atlantic Ridge) program. Absolute <span class="hlt">pressure</span> gauges have been recording on the volcano since 2007, to identify deformations associated with tectonism or magmatism. Deformation measurements are one of the principal means of determining volcanic activity, but the amount of deformation associated with volcanic events varies greatly between different volcanos. We installed two sites: one in the volcano's summit "lava lake" (1700 m depth) and another on the volcano's flank (2000 m depth). <span class="hlt">Pressure</span> is recorded every thirty seconds, giving a data set that constrains movements on the scale from minutes to years. No major deformation event has been detected by the instruments since their installation (nor has any significant tectonic event been detected by a seismic network in place since 2007), so we concentrate here on the detection limit of these instruments and on variations in the long-period ocean wave climate. Using the statistical characteristics of the <span class="hlt">pressure</span> signal, modeled by an auto-regressive process, we determine that a movement between the sites of 1 cm over less than 10 days is detectable; the detection threshold decreases to about 0.2 cm for the shortest time periods and increases for longer time periods due to instrumental drift. We compare the statistical characteristics and short- and long-term sensitivity of three different types of gauges used during the experiment: Paroscientific standard</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://www.dtic.mil/docs/citations/AD1013713','DTIC-ST'); return false;" href="http://www.dtic.mil/docs/citations/AD1013713"><span>Seasonal Ice Zone Reconnaissance Surveys Coordination and Ocean <span class="hlt">Profiles</span></span></a></p> <p><a target="_blank" href="http://www.dtic.mil/">DTIC Science & Technology</a></p> <p></p> <p>2015-09-30</p> <p>Morison), UpTempO buoy measurements of sea surface temperature (SST), sea level atmospheric <span class="hlt">pressure</span> ( SLP ), and velocity (Steele), and dropsonde...dropsondes, micro-aircraft), cloud top/base heights UpTempO buoys for understanding and prediction…. Steele UpTempO buoy drops for SLP , SST, SSS...Air Expendable Current <span class="hlt">Profiler</span>, SLP = Sea Level atmospheric <span class="hlt">Pressure</span>, SST= Seas Surface Temperature, A/C= aircraft, SIC=Sea Ice Concentration We</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/17552684','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/17552684"><span>Liquid jet response to internal modulated ultrasonic radiation <span class="hlt">pressure</span> and stimulated drop production.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Lonzaga, Joel B; Osterhoudt, Curtis F; Thiessen, David B; Marston, Philip L</p> <p>2007-06-01</p> <p>Experimental evidence shows that a liquid jet in air is an acoustic waveguide having a cutoff frequency inversely proportional to the jet diameter. Ultrasound applied to the jet supply liquid can propagate within the jet when the acoustic frequency is near to or above the cutoff frequency. Modulated radiation <span class="hlt">pressure</span> is used to stimulate large amplitude deformations and the breakup of the jet into drops. The jet response to the modulated internal ultrasonic radiation <span class="hlt">pressure</span> was monitored along the jet using (a) an optical extinction method and (b) images captured by a video camera. The jet <span class="hlt">profile</span> oscillates at the frequency of the radiation <span class="hlt">pressure</span> modulation and where the response is small, the amplitude was found to increase in proportion to the square of the acoustic <span class="hlt">pressure</span> amplitude as previously demonstrated for oscillating drops [P.L. Marston and R.E. Apfel, J. Acoust. Soc. Am. 67, 27-37 (1980)]. Small amplitude deformations initially grow approximately exponentially with axial distance along the jet. Though aspects of the perturbation growth can be approximated from Rayleigh's analysis of the capillary instability, some detailed features of the <span class="hlt">observed</span> jet response to modulated ultrasound are unexplained neglecting the effects of gravity.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://ntrs.nasa.gov/search.jsp?R=20020049815&hterms=level+processing+theory&qs=N%3D0%26Ntk%3DAll%26Ntx%3Dmode%2Bmatchall%26Ntt%3Dlevel%2Bprocessing%2Btheory','NASA-TRS'); return false;" href="https://ntrs.nasa.gov/search.jsp?R=20020049815&hterms=level+processing+theory&qs=N%3D0%26Ntk%3DAll%26Ntx%3Dmode%2Bmatchall%26Ntt%3Dlevel%2Bprocessing%2Btheory"><span>Etch <span class="hlt">Profile</span> Simulation Using Level Set Methods</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Hwang, Helen H.; Meyyappan, Meyya; Arnold, James O. (Technical Monitor)</p> <p>1997-01-01</p> <p>Etching and deposition of materials are critical steps in semiconductor processing for device manufacturing. Both etching and deposition may have isotropic and anisotropic components, due to directional sputtering and redeposition of materials, for example. Previous attempts at modeling <span class="hlt">profile</span> evolution have used so-called "string theory" to simulate the moving solid-gas interface between the semiconductor and the plasma. One complication of this method is that extensive de-looping schemes are required at the <span class="hlt">profile</span> corners. We will present a 2D <span class="hlt">profile</span> evolution simulation using level set theory to model the surface. (1) By embedding the location of the interface in a field variable, the need for de-looping schemes is eliminated and <span class="hlt">profile</span> corners are more accurately modeled. This level set <span class="hlt">profile</span> evolution model will calculate both isotropic and anisotropic etch and deposition rates of a substrate in low <span class="hlt">pressure</span> (10s mTorr) plasmas, considering the incident ion energy angular distribution functions and neutral fluxes. We will present etching <span class="hlt">profiles</span> of Si substrates in Ar/Cl2 discharges for various incident ion energies and trench geometries.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/9630133','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/9630133"><span><span class="hlt">Profiling</span> outcomes of ambulatory care: casemix affects perceived performance.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Berlowitz, D R; Ash, A S; Hickey, E C; Kader, B; Friedman, R; Moskowitz, M A</p> <p>1998-06-01</p> <p>The authors explored the role of casemix adjustment when <span class="hlt">profiling</span> outcomes of ambulatory care. The authors reviewed the medical records of 656 patients with hypertension, diabetes, or chronic obstructive pulmonary disease (COPD) receiving care at one of three Department of Veterans Affairs medical centers. Outcomes included measures of physiological control for hypertension and diabetes, and of exacerbations for COPD. Predictors of poor outcomes, including physical examination findings, symptoms, and comorbidities, were identified and entered into regression models. <span class="hlt">Observed</span> minus expected performance was described for each site, both before and after casemix adjustment. Risk-adjustment models were developed that were clinically plausible and had good performance properties. Differences existed among the three sites in the severity of the patients being cared for. For example, the percentage of patients expected to have poor blood <span class="hlt">pressure</span> control were 35% at site 1, 37% at site 2, and 44% at site 3 (P < 0.01). Casemix-adjusted measures of performance were different from unadjusted measures. Sites that were outliers (P < 0.05) with one approach had <span class="hlt">observed</span> performance no different from expected with another approach. Casemix adjustment models can be developed for outpatient medical conditions. Sites differ in the severity of patients they treat, and adjusting for these differences can alter judgments of site performance. Casemix adjustment is necessary when <span class="hlt">profiling</span> outpatient medical conditions.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/17480167','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/17480167"><span><span class="hlt">Observations</span> from a 4-year contamination study of a sample depth <span class="hlt">profile</span> through Martian meteorite Nakhla.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Toporski, Jan; Steele, Andrew</p> <p>2007-04-01</p> <p>Morphological, compositional, and biological evidence indicates the presence of numerous well-developed microbial hyphae structures distributed within four different sample splits of the Nakhla meteorite obtained from the British Museum (allocation BM1913,25). By examining depth <span class="hlt">profiles</span> of the sample splits over time, morphological changes displayed by the structures were documented, as well as changes in their distribution on the samples, <span class="hlt">observations</span> that indicate growth, decay, and reproduction of individual microorganisms. Biological staining with DNA-specific molecular dyes followed by epifluorescence microscopy showed that the hyphae structures contain DNA. Our <span class="hlt">observations</span> demonstrate the potential of microbial interaction with extraterrestrial materials, emphasize the need for rapid investigation of Mars return samples as well as any other returned or impactor-delivered extraterrestrial materials, and suggest the identification of appropriate storage conditions that should be followed immediately after samples retrieved from the field are received by a handling/curation facility. The <span class="hlt">observations</span> are further relevant in planetary protection considerations as they demonstrate that microorganisms may endure and reproduce in extraterrestrial materials over long (at least 4 years) time spans. The combination of microscopy images coupled with compositional and molecular staining techniques is proposed as a valid method for detection of life forms in martian materials as a first-order assessment. Time-resolved in situ <span class="hlt">observations</span> further allow <span class="hlt">observation</span> of possible (bio)dynamics within the system.</p> </li> </ol> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_21");'>21</a></li> <li><a href="#" onclick='return showDiv("page_22");'>22</a></li> <li><a href="#" onclick='return showDiv("page_23");'>23</a></li> <li class="active"><span>24</span></li> <li><a href="#" onclick='return showDiv("page_25");'>25</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div><!-- col-sm-12 --> </div><!-- row --> </div><!-- page_24 --> <div id="page_25" class="hiddenDiv"> <div class="row"> <div class="col-sm-12"> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_21");'>21</a></li> <li><a href="#" onclick='return showDiv("page_22");'>22</a></li> <li><a href="#" onclick='return showDiv("page_23");'>23</a></li> <li><a href="#" onclick='return showDiv("page_24");'>24</a></li> <li class="active"><span>25</span></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div> </div> <div class="row"> <div class="col-sm-12"> <ol class="result-class" start="481"> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2005AAS...207.0903A','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2005AAS...207.0903A"><span>FFT Deconvultion of Be Star Hα Line <span class="hlt">Profiles</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Austin, S. J.</p> <p>2005-12-01</p> <p>We have been monitoring the spectroscopic variability of Be stars using the UCA Fiber Fed Spectrograph. The spectra are 0.8 Angstrom/pixel resolution of the Hα line. The <span class="hlt">observed</span> line <span class="hlt">profiles</span> are a convolution of the actual <span class="hlt">profile</span> and the instrumental <span class="hlt">profile</span>. A Fast Fourier Transform (FFT) method has been used to deconvolve the <span class="hlt">observed</span> <span class="hlt">profiles</span>, given the instrument <span class="hlt">profile</span> obtained by <span class="hlt">observing</span> the narrow lines from the HgNe wavelength calibration lamp. The long-term monitoring of the spectroscopic variability of Be stars is crucial for testing the various Be star models. Deconvolved H-α line <span class="hlt">profiles</span>, velocities, and variability are shown for gamma Cas, delta Sco, chi Oph, eta PsA, 48 Lib, and upsilon Sgr (HD181615). Funding has been provided by the UCA University Research Council and the Arkansas Space Grant Consortium.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2012ChPhL..29d9101L','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2012ChPhL..29d9101L"><span>In Situ <span class="hlt">Observation</span> of Gypsum-Anhydrite Transition at High <span class="hlt">Pressure</span> and High Temperature</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Liu, Chuan-Jiang; Zheng, Hai-Fei</p> <p>2012-04-01</p> <p>An in-situ Raman spectroscopic study of gypsum-anhydrite transition under a saturated water condition at high <span class="hlt">pressure</span> and high temperature is performed using a hydrothermal diamond anvil cell (HDAC). The experimental results show that gypsum dissolvs in water at ambient temperature and above 496 MPa. With increasing temperature, the anhydrite (CaSO4) phase precipitates at 250-320°C in the <span class="hlt">pressure</span> range of 1.0-1.5GPa, indicating that under a saturated water condition, both stable conditions of <span class="hlt">pressure</span> and temperature and high levels of Ca and SO4 ion concentrations in aqueous solution are essential for the formation of anhydrite. A linear relationship between the <span class="hlt">pressure</span> and temperature for the precipitation of anhydrite is established as P(GPa) = 0.0068T-0.7126 (250°C<=T<=320°C). Anhydrite remained stable during rapid cooling of the sample chamber, showing that the gypsum-anhydrite transition involving both dissolution and precipitation processes is irreversible at high <span class="hlt">pressure</span> and high temperature.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/23028839','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/23028839"><span>Modulation of invasive phenotype by interstitial <span class="hlt">pressure</span>-driven convection in aggregates of human breast cancer cells.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Tien, Joe; Truslow, James G; Nelson, Celeste M</p> <p>2012-01-01</p> <p>This paper reports the effect of elevated <span class="hlt">pressure</span> on the invasive phenotype of patterned three-dimensional (3D) aggregates of MDA-MB-231 human breast cancer cells. We found that the directionality of the interstitial <span class="hlt">pressure</span> <span class="hlt">profile</span> altered the frequency of invasion by cells located at the surface of an aggregate. In particular, application of <span class="hlt">pressure</span> at one end of an aggregate suppressed invasion at the opposite end. Experimental alteration of the configuration of cell aggregates and computational modeling of the resulting flow and solute concentration <span class="hlt">profiles</span> revealed that elevated <span class="hlt">pressure</span> inhibited invasion by altering the chemical composition of the interstitial fluid near the surface of the aggregate. Our data reveal a link between hydrostatic <span class="hlt">pressure</span>, interstitial convection, and invasion.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://ntrs.nasa.gov/search.jsp?R=19810053538&hterms=viking+lander&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D40%26Ntt%3Dviking%2Blander','NASA-TRS'); return false;" href="https://ntrs.nasa.gov/search.jsp?R=19810053538&hterms=viking+lander&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D40%26Ntt%3Dviking%2Blander"><span>Inference of dust opacities for the 1977 Martian great dust storms from Viking Lander 1 <span class="hlt">pressure</span> data</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Zurek, R. W.</p> <p>1981-01-01</p> <p>The tidal heating components for the dusty Martian atmosphere are computed based on dust optical parameters estimated from Viking Lander imaging data, and used to compute the variation of the tidal surface <span class="hlt">pressure</span> components at the Viking Lander sites as a function of season and the total vertical extinction optical depth of the atmosphere. An atmospheric tidal model is used which is based on the inviscid, hydrostatic primitive equations linearized about a motionless basic state the temperature of which varies only with height, and the <span class="hlt">profiles</span> of the tidal forcing components are computed using a delta-Eddington approximation to the radiative transfer equations. Comparison of the model results with the <span class="hlt">observed</span> variations of surface <span class="hlt">pressure</span> and overhead dust opacity at the Viking Lander 1 site reveal that the dust opacities and optical parameters derived from imaging data are roughly representative of the global dust haze necessary to reproduce the <span class="hlt">observed</span> surface <span class="hlt">pressure</span> amplitudes, with the exception of the model-inferred asymmetry parameter, which is smaller during the onset of a great storm. The <span class="hlt">observed</span> preferential enhancement of the semidiurnal tide with respect to the diurnal tide during dust storm onset is shown to be due primarily to the elevation of the tidal heating source in a very dusty atmosphere.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2016IAUS..314..139V','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2016IAUS..314..139V"><span>Gas Cavities inside Dust Cavities in Disks Inferred from ALMA <span class="hlt">Observations</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>van der Marel, Nienke; van Dishoeck, Ewine F.; Bruderer, Simon; Pinilla, Paola; van Kempen, Tim; Perez, Laura; Isella, Andrea</p> <p>2016-01-01</p> <p>Protoplanetary disks with cavities in their dust distribution, also named transitional disks, are expected to be in the middle of active evolution and possibly planet formation. In recent years, millimeter-dust rings <span class="hlt">observed</span> by ALMA have been suggested to have their origin in dust traps, caused by <span class="hlt">pressure</span> bumps. One of the ways to generate these is by the presence of planets, which lower the gas density along their orbit and create <span class="hlt">pressure</span> bumps at the edge. We present spatially resolved ALMA Cycle 0 and Cycle 1 <span class="hlt">observations</span> of CO and CO isotopologues of several famous transitional disks. Gas is found to be present inside the dust cavities, but at a reduced level compared with the gas surface density <span class="hlt">profile</span> of the outer disk. The dust and gas emission are quantified using the physical-chemical modeling code DALI. In the majority of these disks we find clear evidence for a drop in gas density of at least a factor of 10 inside the cavity, whereas the dust density drops by at least a factor 1000. The CO isotopologue <span class="hlt">observations</span> reveal that the gas cavities are significantly smaller than the dust cavities. These gas structures suggest clearing by one or more planetary-mass companions.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017AGUFM.A23C2356A','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017AGUFM.A23C2356A"><span>The High Accuracy Measurement of CO2 Mixing Ratio <span class="hlt">Profiles</span> Using Ground Based 1.6 μm CO2-DIAL with Temperature Measurement Techniques in the Lower-Atmosphere</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Abo, M.; Shibata, Y.; Nagasawa, C.</p> <p>2017-12-01</p> <p>We have developed a ground based direct detection three-wavelength 1.6 μm differential absorption lidar (DIAL) to achieve measurements of vertical CO2 concentration and temperature <span class="hlt">profiles</span> in the atmosphere. As the spectra of absorption lines of any molecules are influenced basically by the temperature and <span class="hlt">pressure</span> in the atmosphere, it is important to measure them simultaneously so that the better accuracy of the DIAL measurement is realized. Conventionally, we have obtained the vertical <span class="hlt">profile</span> of absorption cross sections using the atmospheric temperature <span class="hlt">profile</span> by the objective analysis and the atmospheric <span class="hlt">pressure</span> <span class="hlt">profile</span> calculated by the <span class="hlt">pressure</span> height equation. Comparison of atmospheric <span class="hlt">pressure</span> <span class="hlt">profiles</span> calculated from this equation and those obtained from radiosonde <span class="hlt">observations</span> at Tateno, Japan is consistent within 0.2 % below 3 km altitude. But the temperature dependency of the CO2 density is 0.25 %/°C near the surface. Moreover, the CO2 concentration is often evaluated by the mixing ratio. Because the air density is related by the ideal gas law, the mixing ratio is also related by the atmospheric temperature. Therefore, the temperature affects not only accuracy of CO2 concentration but the CO2 mixing ratio. In this paper, some experimental results of the simultaneous measurement of atmospheric temperature <span class="hlt">profiles</span> and CO2 mixing ratio <span class="hlt">profiles</span> are reported from 0.4 to 2.5 km altitude using the three-wavelength 1.6 μm DIAL system. Temperature <span class="hlt">profiles</span> of CO2 DIAL measurement were sometimes different from those of objective analysis below 1.5 km altitude. These differences are considered to be due to regionality at the lidar site. The temperature difference of 5.0 °C corresponds to a CO2 mixing ratio difference of 8.0 ppm at 500 m altitude. This cannot be ignored in estimates of regional sources and sinks of CO2. This three-wavelength CO2 DIAL technique can estimate accurately temporal behavior of CO2 mixing ratio <span class="hlt">profiles</span> in the lower atmosphere</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.osti.gov/servlets/purl/877208','SCIGOV-STC'); return false;" href="https://www.osti.gov/servlets/purl/877208"><span>Chemical Evolution in Sersic 159-03 <span class="hlt">Observed</span> with Xmm-Newton</span></a></p> <p><a target="_blank" href="http://www.osti.gov/search">DOE Office of Scientific and Technical Information (OSTI.GOV)</a></p> <p>de Plaa, Jelle; Werner, N.; Bykov, A.M.</p> <p>2006-03-10</p> <p>Using a new long X-ray <span class="hlt">observation</span> of the cluster of galaxies Sersic 159-03 with XMM-Newton, we derive radial temperature and abundance <span class="hlt">profiles</span> using single- and multi-temperature models. The fits to the EPIC and RGS spectra prefer multi-temperature models especially in the core. The radial <span class="hlt">profiles</span> of oxygen and iron measured with EPIC/RGS and the line <span class="hlt">profiles</span> in RGS suggest that there is a dip in the O/Fe ratio in the centre of the cluster compared to its immediate surroundings. A possible explanation for the large scale metallicity distribution is that SNIa and SNII products are released in the ICM throughmore » ram-<span class="hlt">pressure</span> stripping of in-falling galaxies. This causes a peaked metallicity distribution. In addition, SNIa in the central cD galaxy enrich mainly the centre of the cluster with iron. This excess of SNIa products is consistent with the low O/Fe ratio we detect in the centre of the cluster. We fit the abundances we obtain with yields from SNIa, SNII and Population-III stars to derive the clusters chemical evolution. We find that the measured abundance pattern does not require a Population-III star contribution. The relative contribution of the number of SNIa with respect to the total number of SNe which enrich the ICM is about 25-50%. Furthermore, we discuss the possible presence of a non-thermal component in the EPIC spectra. A potential source of this non-thermal emission can be inverse-Compton scattering between Cosmic Microwave Background (CMB) photons and relativistic electrons, which are accelerated in bow shocks associated with ram-<span class="hlt">pressure</span> stripping of in-falling galaxies.« less</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2014JPhCS.500c2010Z','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2014JPhCS.500c2010Z"><span>Experimental investigation of dynamic compression and spallation of Cerium at <span class="hlt">pressures</span> up to 6 GPa</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Zubareva, A. N.; Kolesnikov, S. A.; Utkin, A. V.</p> <p>2014-05-01</p> <p>In this study the experiments on one-dimensional dynamic compression of Cerium (Ce) samples to <span class="hlt">pressures</span> of 0.5 to 6 GPa using various types of explosively driven generators were conducted. VISAR laser velocimeter was used to obtain Ce free surface velocity <span class="hlt">profiles</span>. The isentropic compression wave was registered for γ-phase of Ce at <span class="hlt">pressures</span> lower than 0.76 GPa that corresponds to γ-α phase transition <span class="hlt">pressure</span> in Ce. Shock rarefaction waves were also registered in several experiments. Both <span class="hlt">observations</span> were the result of the anomalous compressibility of γ-phase of Ce. On the basis of our experimental results the compression isentrope of Ce γ-phase was constructed. Its comparison with volumetric compression curves allowed to estimate the magnitude of shear stress at dynamic compression conditions for Ce. Spall strength measurements were also conducted for several samples. They showed a strong dependence of the spall strength of Ce on the strain rate.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2012JChPh.136k4510S','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2012JChPh.136k4510S"><span>The effect of <span class="hlt">pressure</span> on the hydration structure around hydrophobic solute: A molecular dynamics simulation study</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Sarma, Rahul; Paul, Sandip</p> <p>2012-03-01</p> <p>Molecular dynamics simulations are performed to study the effects of <span class="hlt">pressure</span> on the hydrophobic interactions between neopentane molecules immersed in water. Simulations are carried out for five different <span class="hlt">pressure</span> values ranging from 1 atm to 8000 atm. From potential of mean force calculations, we find that with enhancement of <span class="hlt">pressure</span>, there is decrease in the well depth of contact minimum (CM) and the relative stability of solvent separated minimum over CM increases. Lower clustering of neopentane at high <span class="hlt">pressure</span> is also <span class="hlt">observed</span> in association constant and cluster-structure analysis. Selected site-site radial distribution functions suggest efficient packing of water molecules around neopentane molecules at elevated <span class="hlt">pressure</span>. The orientational <span class="hlt">profile</span> calculations of water molecules show that the orientation of water molecules in the vicinity of solute molecule is anisotropic and this distribution becomes flatter as we move away from the solute. Increasing <span class="hlt">pressure</span> slightly changes the water distribution. Our hydrogen bond properties and dynamics calculations reveal <span class="hlt">pressure</span>-induced formation of more and more number of water molecules with five and four hydrogen bond at the expense of breaking of two and three hydrogen bonded water molecules. We also find lowering of water-water continuous hydrogen bond lifetime on application of <span class="hlt">pressure</span>. Implication of these results for relative dispersion of hydrophobic molecules at high <span class="hlt">pressure</span> are discussed.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/19800018910','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/19800018910"><span>STS-1 operational flight <span class="hlt">profile</span>. Volume 3: Ascent, cycle 3</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p></p> <p>1980-01-01</p> <p>The ascent opeational flight <span class="hlt">profile</span> for the space transportation system 1 flight is designed (1) to limit the maximum undispersed dynamic <span class="hlt">pressure</span> to 580 lb/sq ft, (2) to follow the design load indicator <span class="hlt">profiles</span> where q alpha is a specified <span class="hlt">profile</span> and q beta is desired to be as close to zero as passible, and (3) to maximize nominal and abort performance. Significant trajectory parameters achieved are presented. A maximum dynamic <span class="hlt">pressure</span> of 575 lb/sq ft was achieved, a minimum q alpha of -2187 lb-deg/sq ft was achieved, and q beta was limited to approximately + or - 100 lb-deg/sq ft in the high q region of the trajectory. The trajectory performance allows a press to main engine cutoff capability with one space shuttle main engine out at 262 seconds ground elapsed time. The orbital maneuvering system burns achieve a final orbit of 150.9 x 149.9 x 149.8 n. mi. and the desired inclination of 40.3 degrees.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/19720024765','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/19720024765"><span>Interrelated structure of high altitude atmospheric <span class="hlt">profiles</span></span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Engler, N. A.; Goldschmidt, M. A.</p> <p>1972-01-01</p> <p>A preliminary development of a mathematical model to compute probabilities of thermodynamic <span class="hlt">profiles</span> is presented. The model assumes an exponential expression for <span class="hlt">pressure</span> and utilizes the hydrostatic law and equation of state in the determination of density and temperature. It is shown that each thermodynamic variable can be factored into the produce of steady state and perturbation functions. The steady state functions have <span class="hlt">profiles</span> similar to those of the 1962 standard atmosphere while the perturbation functions oscillate about 1. Limitations of the model and recommendations for future work are presented.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/19950014629','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/19950014629"><span>Statistics of <span class="hlt">pressure</span> and <span class="hlt">pressure</span> gradient in homogeneous isotropic turbulence</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Gotoh, T.; Rogallo, R. S.</p> <p>1994-01-01</p> <p>The statistics of <span class="hlt">pressure</span> and <span class="hlt">pressure</span> gradient in stationary isotropic turbulence are measured within direct numerical simulations at low to moderate Reynolds numbers. It is found that the one-point pdf of the <span class="hlt">pressure</span> is highly skewed and that the pdf of the <span class="hlt">pressure</span> gradient is of stretched exponential form. The power spectrum of the <span class="hlt">pressure</span> P(k) is found to be larger than the corresponding spectrum P(sub G)(k) computed from a Gaussian velocity field having the same energy spectrum as that of the DNS field. The ratio P(k)/P(sub G)(k), a measure of the <span class="hlt">pressure</span>-field intermittence, grows with wavenumber and Reynolds number as -R(sub lambda)(exp 1/2)log(k/k(sub d)) for k less than k(sub d)/2 where k(sub d) is the Kolmogorov wavenumber. The Lagrangian correlations of <span class="hlt">pressure</span> gradient and velocity are compared and the Lagrangian time scale of the <span class="hlt">pressure</span> gradient is <span class="hlt">observed</span> to be much shorter than that of the velocity.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2016APS..DPPN10121R','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2016APS..DPPN10121R"><span>Radial and Azimuthal Velocity <span class="hlt">Profiles</span> in Gas-Puff Z-Pinches</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Rocco, Sophia; Engelbrecht, Joseph; Banasek, Jacob; de Grouchy, Philip; Qi, Niansheng; Hammer, David</p> <p>2016-10-01</p> <p>The dynamics of neon, argon, and krypton (either singly or in combination) gas puff z-pinch plasmas are studied on Cornell's 1MA, 100-200ns rise-time COBRA pulsed power generator. The triple-nozzle gas puff valve, consisting of two annular gas puffs and a central jet, allows radial tailoring of the gas puff mass-density <span class="hlt">profile</span> and the use of 1, 2 or 3 different gases at different <span class="hlt">pressures</span>. Interferometry supplies information on sheath thickness and electron density, variously filtered PCDs and silicon diodes measure hard and soft x-ray production, and multi frame visible and extreme UV imaging systems allow tracking of the morphology of the plasma. A 527nm, 10J Thomson scattering diagnostic system is used to determine radial and azimuthal velocities. Implosion velocities of 170km/s (Kr) and 300km/s (Ne/Ar) are <span class="hlt">observed</span>. We are investigating the correlations between instability growth, plasma density <span class="hlt">profile</span>, velocity partitioning as a function of radius, and radiation production. Research supported by the NNSA Stewardship Sciences Academic Programs under DOE Cooperative Agreement No. DE-NA0001836.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/20120014208','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/20120014208"><span>Assimilation of Quality Controlled AIRS Temperature <span class="hlt">Profiles</span> using the NCEP GFS</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Susskind, Joel; Reale, Oreste; Iredell, Lena; Rosenberg, Robert</p> <p>2013-01-01</p> <p>We have previously conducted a number of data assimilation experiments using AIRS Version-5 quality controlled temperature <span class="hlt">profiles</span> as a step toward finding an optimum balance of spatial coverage and sounding accuracy with regard to improving forecast skill. The data assimilation and forecast system we used was the Goddard Earth <span class="hlt">Observing</span> System Model , Version-5 (GEOS-5) Data Assimilation System (DAS), which represents a combination of the NASA GEOS-5 forecast model with the National Centers for Environmental Prediction (NCEP) operational Grid Point Statistical Interpolation (GSI) global analysis scheme. All analyses and forecasts were run at a 0.5deg x 0.625deg spatial resolution. Data assimilation experiments were conducted in four different seasons, each in a different year. Three different sets of data assimilation experiments were run during each time period: Control; AIRS T(p); and AIRS Radiance. In the "Control" analysis, all the data used operationally by NCEP was assimilated, but no AIRS data was assimilated. Radiances from the Aqua AMSU-A instrument were also assimilated operationally by NCEP and are included in the "Control". The AIRS Radiance assimilation adds AIRS <span class="hlt">observed</span> radiance <span class="hlt">observations</span> for a select set of channels to the data set being assimilated, as done operationally by NCEP. In the AIRS T(p) assimilation, all information used in the Control was assimilated as well as Quality Controlled AIRS Version-5 temperature <span class="hlt">profiles</span>, i.e., AIRS T(p) information was substituted for AIRS radiance information. The AIRS Version-5 temperature <span class="hlt">profiles</span> were presented to the GSI analysis as rawinsonde <span class="hlt">profiles</span>, assimilated down to a case-by-case appropriate <span class="hlt">pressure</span> level p(sub best) determined using the Quality Control procedure. Version-5 also determines case-by-case, level-by-level error estimates of the temperature <span class="hlt">profiles</span>, which were used as the uncertainty of each temperature measurement. These experiments using GEOS-5 have shown that forecasts</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2018IzPSE..54..214L','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2018IzPSE..54..214L"><span>Determining the Positions of Seismically Active Faults in Platform Regions Based on the Integrated <span class="hlt">Profile</span> <span class="hlt">Observations</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Levshenko, V. T.; Grigoryan, A. G.</p> <p>2018-03-01</p> <p>By the examples of the Roslavl'skii, Grafskii, and Platava-Varvarinskii faults, the possibility is demonstrated of mapping the geological objects by the measurement algorithm that includes successively measuring the spectra of microseisms at the points of the measurement network by movable instruments and statistical accumulation of the ratios of the power spectra of the amplitudes. Based on this technique, the positions of these seismically active faults are determined by the integrated <span class="hlt">profile</span> <span class="hlt">observations</span> of the parameters of microseismic and radon fields. The refined positions of the faults can be used in estimating the seismic impacts on the critical objects in the vicinity of these faults.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=1301343','PMC'); return false;" href="https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=1301343"><span><span class="hlt">Pressure</span>-jump small-angle x-ray scattering detected kinetics of staphylococcal nuclease folding.</span></a></p> <p><a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pmc">PubMed Central</a></p> <p>Woenckhaus, J; Köhling, R; Thiyagarajan, P; Littrell, K C; Seifert, S; Royer, C A; Winter, R</p> <p>2001-01-01</p> <p>The kinetics of chain disruption and collapse of staphylococcal nuclease after positive or negative <span class="hlt">pressure</span> jumps was monitored by real-time small-angle x-ray scattering under <span class="hlt">pressure</span>. We used this method to probe the overall conformation of the protein by measuring its radius of gyration and pair-distance-distribution function p(r) which are sensitive to the spatial extent and shape of the particle. At all <span class="hlt">pressures</span> and temperatures tested, the relaxation <span class="hlt">profiles</span> were well described by a single exponential function. No fast collapse was <span class="hlt">observed</span>, indicating that the rate limiting step for chain collapse is the same as that for secondary and tertiary structure formation. Whereas refolding at low <span class="hlt">pressures</span> occurred in a few seconds, at high <span class="hlt">pressures</span> the relaxation was quite slow, approximately 1 h, due to a large positive activation volume for the rate-limiting step for chain collapse. A large increase in the system volume upon folding implies significant dehydration of the transition state and a high degree of similarity in terms of the packing density between the native and transition states in this system. This study of the time-dependence of the tertiary structure in <span class="hlt">pressure</span>-induced folding/unfolding reactions demonstrates that novel information about the nature of protein folding transitions and transition states can be obtained from a combination of small-angle x-ray scattering using high intensity synchrotron radiation with the high <span class="hlt">pressure</span> perturbation technique. PMID:11222312</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2016AMT.....9.1063O','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2016AMT.....9.1063O"><span>New temperature and <span class="hlt">pressure</span> retrieval algorithm for high-resolution infrared solar occultation spectroscopy: analysis and validation against ACE-FTS and COSMIC</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Olsen, Kevin S.; Toon, Geoffrey C.; Boone, Chris D.; Strong, Kimberly</p> <p>2016-03-01</p> <p>Motivated by the initial selection of a high-resolution solar occultation Fourier transform spectrometer (FTS) to fly to Mars on the ExoMars Trace Gas Orbiter, we have been developing algorithms for retrieving volume mixing ratio vertical <span class="hlt">profiles</span> of trace gases, the primary component of which is a new algorithm and software for retrieving vertical <span class="hlt">profiles</span> of temperature and <span class="hlt">pressure</span> from the spectra. In contrast to Earth-<span class="hlt">observing</span> instruments, which can rely on accurate meteorological models, a priori information, and spacecraft position, Mars retrievals require a method with minimal reliance on such data. The temperature and <span class="hlt">pressure</span> retrieval algorithms developed for this work were evaluated using Earth-<span class="hlt">observing</span> spectra from the Atmospheric Chemistry Experiment (ACE) FTS, a solar occultation instrument in orbit since 2003, and the basis for the instrument selected for a Mars mission. ACE-FTS makes multiple measurements during an occultation, separated in altitude by 1.5-5 km, and we analyse 10 CO2 vibration-rotation bands at each altitude, each with a different usable altitude range. We describe the algorithms and present results of their application and their comparison to the ACE-FTS data products. The Constellation <span class="hlt">Observing</span> System for Meteorology, Ionosphere, and Climate (COSMIC) provides vertical <span class="hlt">profiles</span> of temperature up to 40 km with high vertical resolution. Using six satellites and GPS radio occultation, COSMIC's data product has excellent temporal and spatial coverage, allowing us to find coincident measurements with ACE with very tight criteria: less than 1.5 h and 150 km. We present an intercomparison of temperature <span class="hlt">profiles</span> retrieved from ACE-FTS using our algorithm, that of the ACE Science Team (v3.5), and from COSMIC. When our retrievals are compared to ACE-FTS v3.5, we find mean differences between -5 and +2 K and that our retrieved <span class="hlt">profiles</span> have no seasonal or zonal biases but do have a warm bias in the stratosphere and a cold bias in the</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=4053470','PMC'); return false;" href="https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=4053470"><span>Genomic and Metabolomic <span class="hlt">Profile</span> Associated to Microalbuminuria</span></a></p> <p><a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pmc">PubMed Central</a></p> <p>Marrachelli, Vannina G.; Monleon, Daniel; Rentero, Pilar; Mansego, María L.; Morales, Jose Manuel; Galan, Inma; Segura, Remedios; Martinez, Fernando; Martin-Escudero, Juan Carlos; Briongos, Laisa; Marin, Pablo; Lliso, Gloria; Chaves, Felipe Javier; Redon, Josep</p> <p>2014-01-01</p> <p>To identify factors related with the risk to develop microalbuminuria using combined genomic and metabolomic values from a general population study. One thousand five hundred and two subjects, Caucasian, more than 18 years, representative of the general population, were included. Blood <span class="hlt">pressure</span> measurement and albumin/creatinine ratio were measured in a urine sample. Using SNPlex, 1251 SNPs potentially associated to urinary albumin excretion (UAE) were analyzed. Serum metabolomic <span class="hlt">profile</span> was assessed by 1H NMR spectra using a Brucker Advance DRX 600 spectrometer. From the total population, 1217 (mean age 54±19, 50.6% men, ACR>30 mg/g in 81 subjects) with high genotyping call rate were analysed. A characteristic metabolomic <span class="hlt">profile</span>, which included products from mitochondrial and extra mitochondrial metabolism as well as branched amino acids and their derivative signals, were <span class="hlt">observed</span> in microalbuminuric as compare to normoalbuminuric subjects. The comparison of the metabolomic <span class="hlt">profile</span> between subjects with different UAE status for each of the genotypes associated to microalbuminuria revealed two SNPs, the rs10492025_TT of RPH3A gene and the rs4359_CC of ACE gene, with minimal or no statistically significant differences. Subjects with and without microalbuminuria, who shared the same genotype and metabolomic <span class="hlt">profile</span>, differed in age. Microalbuminurics with the CC genotype of the rs4359 polymorphism and with the TT genotype of the rs10492025 polymorphism were seven years older and seventeen years younger, respectively as compared to the whole microalbuminuric subjects. With the same metabolomic environment, characteristic of subjects with microalbuminuria, the TT genotype of the rs10492025 polymorphism seems to increase and the CC genotype of the rs4359 polymorphism seems to reduce risk to develop microalbuminuria. PMID:24918908</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.osti.gov/servlets/purl/1073043','SCIGOV-DOEDE'); return false;" href="https://www.osti.gov/servlets/purl/1073043"><span>ARM - Midlatitude Continental Convective Clouds Experiment (MC3E): Multi-Frequency <span class="hlt">Profilers</span>, 449 MHz <span class="hlt">Profiler</span>(williams-449_prof)</span></a></p> <p><a target="_blank" href="http://www.osti.gov/dataexplorer">DOE Data Explorer</a></p> <p>Williams, Christopher; Jensen, Mike</p> <p>2012-11-06</p> <p>This data was collected by the NOAA 449-MHz and 2.8-GHz <span class="hlt">profilers</span> in support of the Department of Energy (DOE) and NASA sponsored Mid-latitude Continental Convective Cloud Experiment (MC3E). The <span class="hlt">profiling</span> radars were deployed in Northern Oklahoma at the DOE Atmospheric Radiation Mission (ARM) Southern Great Plans (SGP) Central Facility from 22 April through 6 June 2011. NOAA deployed three instruments: a Parsivel disdrometer, a 2.8-GHz <span class="hlt">profiler</span>, and a 449-MHz <span class="hlt">profiler</span>. The parasivel provided surface estimates of the raindrop size distribution and is the reference used to absolutely calibrate the 2.8 GHz <span class="hlt">profiler</span>. The 2.8-GHz <span class="hlt">profiler</span> provided unattenuated reflectivity <span class="hlt">profiles</span> of the precipitation. The 449-MHz <span class="hlt">profiler</span> provided estimates of the vertical air motion during precipitation from near the surface to just below the freezing level. By using the combination of 2.8-GHz and 449-MHz <span class="hlt">profiler</span> <span class="hlt">observations</span>, vertical <span class="hlt">profiles</span> of raindrop size distributions can be retrieved. The <span class="hlt">profilers</span> are often reference by their frequency band: the 2.8-GHz <span class="hlt">profiler</span> operates in the S-band and the 449-MHz <span class="hlt">profiler</span> operates in the UHF band. The raw <span class="hlt">observations</span> are available as well as calibrated spectra and moments. This document describes how the instruments were deployed, how the data was collected, and the format of the archived data.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/24865620','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/24865620"><span>Resonance tube phonation in water: High-speed imaging, electroglottographic and oral <span class="hlt">pressure</span> <span class="hlt">observations</span> of vocal fold vibrations--a pilot study.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Granqvist, Svante; Simberg, Susanna; Hertegård, Stellan; Holmqvist, Sofia; Larsson, Hans; Lindestad, Per-Åke; Södersten, Maria; Hammarberg, Britta</p> <p>2015-10-01</p> <p>Phonation into glass tubes ('resonance tubes'), keeping the free end of the tube in water, has been a frequently used voice therapy method in Finland and more recently also in other countries. The purpose of this exploratory study was to investigate what effects tube phonation with and without water has on the larynx. Two participants were included in the study. The methods used were high-speed imaging, electroglottographic <span class="hlt">observations</span> of vocal fold vibrations, and measurements of oral <span class="hlt">pressure</span> during tube phonation. Results showed that the fluctuation in the back <span class="hlt">pressure</span> during tube phonation in water altered the vocal fold vibrations. In the high-speed imaging, effects were found in the open quotient and amplitude variation of the glottal opening. The open quotient increased with increasing water depth (from 2 cm to 6 cm). A modulation effect by the water bubbles on the vocal fold vibrations was seen both in the high-speed glottal area tracings and in the electroglottography signal. A second experiment revealed that the increased average oral <span class="hlt">pressure</span> was largely determined by the water depth. The increased open quotient can possibly be explained by an increased abduction of the vocal folds and/or a reduced transglottal <span class="hlt">pressure</span>. The back <span class="hlt">pressure</span> of the bubbles also modulates glottal vibrations with a possible 'massage' effect on the vocal folds. This effect and the well-defined average <span class="hlt">pressure</span> increase due to the known water depth are different from those of other methods using a semi-occluded vocal tract.</p> </li> </ol> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_21");'>21</a></li> <li><a href="#" onclick='return showDiv("page_22");'>22</a></li> <li><a href="#" onclick='return showDiv("page_23");'>23</a></li> <li><a href="#" onclick='return showDiv("page_24");'>24</a></li> <li class="active"><span>25</span></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div><!-- col-sm-12 --> </div><!-- row --> </div><!-- page_25 --> <div class="footer-extlink text-muted" style="margin-bottom:1rem; text-align:center;">Some links on this page may take you to non-federal websites. 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