Sample records for solar activity influences

  1. Test for planetary influences on solar activity. [tidal effects

    NASA Technical Reports Server (NTRS)

    Dingle, L. A.; Van Hoven, G.; Sturrock, P. A.

    1973-01-01

    A method due to Schuster is used to test the hypothesis that solar activity is influenced by tides raised in the sun's atmosphere by planets. We calculate the distribution in longitude of over 1000 flares occurring in a 6 1/2 yr segment of solar cycle 19, referring the longitude system in turn to the orbital positions of Jupiter and Venus. The resulting distributions show no evidence for a tidal effect.

  2. How Large Scales Flows May Influence Solar Activity

    NASA Technical Reports Server (NTRS)

    Hathaway, D. H.

    2004-01-01

    Large scale flows within the solar convection zone are the primary drivers of the Sun's magnetic activity cycle and play important roles in shaping the Sun's magnetic field. Differential rotation amplifies the magnetic field through its shearing action and converts poloidal field into toroidal field. Poleward meridional flow near the surface carries magnetic flux that reverses the magnetic poles at about the time of solar maximum. The deeper, equatorward meridional flow can carry magnetic flux back toward the lower latitudes where it erupts through the surface to form tilted active regions that convert toroidal fields into oppositely directed poloidal fields. These axisymmetric flows are themselves driven by large scale convective motions. The effects of the Sun's rotation on convection produce velocity correlations that can maintain both the differential rotation and the meridional circulation. These convective motions can also influence solar activity directly by shaping the magnetic field pattern. While considerable theoretical advances have been made toward understanding these large scale flows, outstanding problems in matching theory to observations still remain.

  3. How Large Scale Flows in the Solar Convection Zone may Influence Solar Activity

    NASA Technical Reports Server (NTRS)

    Hathaway, D. H.

    2004-01-01

    Large scale flows within the solar convection zone are the primary drivers of the Sun s magnetic activity cycle. Differential rotation can amplify the magnetic field and convert poloidal fields into toroidal fields. Poleward meridional flow near the surface can carry magnetic flux that reverses the magnetic poles and can convert toroidal fields into poloidal fields. The deeper, equatorward meridional flow can carry magnetic flux toward the equator where it can reconnect with oppositely directed fields in the other hemisphere. These axisymmetric flows are themselves driven by large scale convective motions. The effects of the Sun s rotation on convection produce velocity correlations that can maintain the differential rotation and meridional circulation. These convective motions can influence solar activity themselves by shaping the large-scale magnetic field pattern. While considerable theoretical advances have been made toward understanding these large scale flows, outstanding problems in matching theory to observations still remain.

  4. No evidence for planetary influence on solar activity 330 000 years ago

    NASA Astrophysics Data System (ADS)

    Cauquoin, A.; Raisbeck, G. M.; Jouzel, J.; Bard, E.

    2014-01-01

    Context. Abreu et al. (2012, A&A. 548, A88) have recently compared the periodicities in a 14C - 10Be proxy record of solar variability during the Holocene and found a strong similarity with the periodicities predicted on the basis of a model of the time-dependent torque exerted by the planets on the sun's tachocline. If verified, this effect would represent a dramatic advance not only in the basic understanding of the Sun's variable activity, but also in the potential influence of this variability on the Earth's climate. Cameron and Schussler (2013, A&A. 557, A83) have seriously criticized the statistical treatment used by Abreu et al. to test the significance of the coincidences between the periodicities of their model with the Holocene proxy record. Aims: If the Abreu et al. hypothesis is correct, it should be possible to find the same periodicities in the records of cosmogenic nuclides at earlier times. Methods: We present here a high-resolution record of 10Be in the EPICA Dome C (EDC) ice core from Antarctica during the Marine Interglacial Stage 9.3 (MIS 9.3), 325-336 kyr ago, and investigate its spectral properties. Results: We find very limited similarity with the periodicities seen in the proxy record of solar variability during the Holocene, or with that of the model of Abreu et al. Conclusions: We find no support for the hypothesis of a planetary influence on solar activity, and raise the question of whether the centennial periodicities of solar activity observed during the Holocene are representative of solar activity variability in general.

  5. Solar influences on global change

    NASA Technical Reports Server (NTRS)

    1994-01-01

    Monitoring of the Sun and the Earth has yielded new knowledge essential to this debate. There is now no doubt that the total radiative energy from the Sun that heats the Earth's surface changes over decadal time scales as a consequence of solar activity. Observations indicate as well that changes in ultraviolet radiation and energetic particles from the Sun, also connected with the solar activity, modulate the layer of ozone that protects the biosphere from the solar ultraviolet radiation. This report reassesses solar influences on global change in the light of this new knowledge of solar and atmospheric variability. Moreover, the report considers climate change to be encompassed within the broader concept of global change; thus the biosphere is recognized to be part of a larger, coupled Earth system. Implementing a program to continuously monitor solar irradiance over the next several decades will provide the opportunity to estimate solar influences on global change, assuming continued maintenance of observations of climate and other potential forcing mechanisms. In the lower atmosphere, an increase in solar radiation is expected to cause global warming. In the stratosphere, however, the two effects produce temperature changes of opposite sign. A monitoring program that would augment long term observations of tropospheric parameters with similar observations of stratospheric parameters could separate these diverse climate perturbations and perhaps isolate a greenhouse footprint of climate change. Monitoring global change in the troposphere is a key element of all facets of the United States Global Change Research Program (USGCRP), not just of the study of solar influences on global change. The need for monitoring the stratosphere is also important for global change research in its own right because of the stratospheric ozone layer.

  6. Influence of solar activity on the state of the wheat market in medieval England

    NASA Astrophysics Data System (ADS)

    Pustil'Nik, Lev A.; Din, Gregory Yom

    2004-09-01

    The database of professor Rogers (1887), which includes wheat prices in England in the Middle Ages, was used to search for a possible influence of solar activity on the wheat market. Our approach was based on the following: (1) Existence of the correlation between cosmic ray flux entering the terrestrial atmosphere and cloudiness of the atmosphere. (2) Cosmic ray intensity in the solar system changes with solar activity, (3) Wheat production depends on weather conditions as a nonlinear function with threshold transitions. (4) A wheat market with a limited supply (as it was in medieval England) has a highly nonlinear sensitivity to variations in wheat production with boundary states, where small changes in wheat supply could lead to bursts of prices or to prices falling. We present a conceptual model of possible modes for sensitivity of wheat prices to weather conditions, caused by solar cycle variations, and compare expected price fluctuations with price variations recorded in medieval England. We compared statistical properties of the intervals between wheat price bursts during the years 1249-1703 with statistical properties of the intervals between the minima of solar cycles during the years 1700-2000. We show that statistical properties of these two samples are similar, both for characteristics of the distributions and for histograms of the distributions. We analyze a direct link between wheat prices and solar activity in the 17th century, for which wheat prices and solar activity data (derived from 10Be isotope) are available. We show that for all 10 time moments of the solar activity minima the observed prices were higher than prices for the corresponding time moments of maximal solar activity (100% sign correlation, on a significance level < 0.2%). We consider these results a direct evidence of the causal connection between wheat prices bursts and solar activity.

  7. Ninth Workshop 'Solar Influences on the Magnetosphere, Ionosphere and Atmosphere'

    NASA Astrophysics Data System (ADS)

    Georgieva, Kayta; Kirov, Boian; Danov, Dimitar

    2017-08-01

    The 9th Workshop "Solar Influences on the Magnetosphere, Ionosphere and Atmosphere" is an international forum for scientists working in the fields of: Sun and solar activity, Solar wind-magnetosphere-ionosphere interactions, Solar influences on the lower atmosphere and climate, Solar effects in the biosphere, Instrumentation for space weather monitoring and Data processing and modelling.

  8. Statistical analyses of influence of solar and geomagnetic activities on car accident events

    NASA Astrophysics Data System (ADS)

    Alania, M. V.; Gil, A.; Wieliczuk, R.

    2001-01-01

    Statistical analyses of the influence of Solar and geomagnetic activity, sector structure of the interplanetary magnetic field and galactic cosmic ray Forbush effects on car accident events in Poland for the period of 1990-1999 have been carried out. Using auto-correlation, cross-correlation, spectral analyses and superposition epochs methods it has been shown that there are separate periods when car accident events have direct correlation with Ap index of the geomagnetic activity, sector structure of the interplanetary magnetic field and Forbush decreases of galactic cosmic rays. Nevertheless, the single-valued direct correlation is not possible to reveal for the whole period of 1990-1999. Periodicity of 7 days and its second harmonic (3.5 days) has been reliably revealed in the car accident events data in Poland for the each year of the period 1990-1999. It is shown that the maximum car accident events take place in Poland on Friday and practically does not depend on the level of solar and geomagnetic activities.

  9. Influence of Solar Irradiance on Polar Ionospheric Convection

    NASA Astrophysics Data System (ADS)

    Burrell, A. G.; Yeoman, T. K.; Stephen, M.; Lester, M.

    2016-12-01

    Plasma convection over the poles shows the result of direct interactions between the terrestrial atmosphere, magnetosphere, and the sun. The paths that the ionospheric plasma takes in the polar cap form a variety of patterns, which have been shown to depend strongly on the direction of the Interplanetary Magnetic Field (IMF) and the reconnection rate. While the IMF and level of geomagnetic activity clearly alter the plasma convection patterns, the influence of changing solar irradiance is also important. The solar irradiance and magnetospheric particle precipitation regulate the rate of plasma production, and thus the ionospheric conductivity. Previous work has demonstrated how season alters the convection patterns observed over the poles, demonstrating the importance that solar photoionisation has on plasma convection. This study investigates the role of solar photoionisation on convection more directly, using measurements of ionospheric convection made by the Super Dual Auroral Radar Network (SuperDARN) and solar irradiance observations made by the Solar EUV Experiment (SEE) to explore the influence of the solar cycle on ionospheric convection, and the implications this may have on magnetosphere-ionosphere coupling.

  10. Does solar activity affect human happiness?

    NASA Astrophysics Data System (ADS)

    Kristoufek, Ladislav

    2018-03-01

    We investigate the direct influence of solar activity (represented by sunspot numbers) on human happiness (represented by the Twitter-based Happiness Index). We construct four models controlling for various statistical and dynamic effects of the analyzed series. The final model gives promising results. First, there is a statistically significant negative influence of solar activity on happiness which holds even after controlling for the other factors. Second, the final model, which is still rather simple, explains around 75% of variance of the Happiness Index. Third, our control variables contribute significantly as well: happiness is higher in no sunspots days, happiness is strongly persistent, there are strong intra-week cycles and happiness peaks during holidays. Our results strongly contribute to the topical literature and they provide evidence of unique utility of the online data.

  11. The influence of solar active region evolution on solar wind streams, coronal hole boundaries and geomagnetic storms

    NASA Technical Reports Server (NTRS)

    Gold, R. E.; Dodson-Prince, H. W.; Hedeman, E. R.; Roelof, E. C.

    1982-01-01

    Solar and interplanetary data are examined, taking into account the identification of the heliographic longitudes of the coronal source regions of high speed solar wind (SW) streams by Nolte and Roelof (1973). Nolte and Roelof have 'mapped' the velocities measured near earth back to the sun using the approximation of constant radial velocity. The 'Carrington carpet' for rotations 1597-1616 is shown in a graph. Coronal sources of high speed streams appear in the form of solid black areas. The contours of the stream sources are laid on 'evolutionary charts' of solar active region histories for the Southern and Northern Hemispheres. Questions regarding the interplay of active regions and solar wind are investigated, giving attention to developments during the years 1973, 1974, and 1975.

  12. Bacterial Active Community Cycling in Response to Solar Radiation and Their Influence on Nutrient Changes in a High-Altitude Wetland.

    PubMed

    Molina, Verónica; Hernández, Klaudia; Dorador, Cristina; Eissler, Yoanna; Hengst, Martha; Pérez, Vilma; Harrod, Chris

    2016-01-01

    Microbial communities inhabiting high-altitude spring ecosystems are subjected to extreme changes in solar irradiance and temperature throughout the diel cycle. Here, using 16S rRNA gene tag pyrosequencing (cDNA) we determined the composition of actively transcribing bacteria from spring waters experimentally exposed through the day (morning, noon, and afternoon) to variable levels of solar radiation and light quality, and evaluated their influence on nutrient recycling. Solar irradiance, temperature, and changes in nutrient dynamics were associated with changes in the active bacterial community structure, predominantly by Cyanobacteria, Verrucomicrobia, Proteobacteria, and 35 other Phyla, including the recently described Candidate Phyla Radiation (e.g., Parcubacteria, Gracilibacteria, OP3, TM6, SR1). Diversity increased at noon, when the highest irradiances were measured (3.3-3.9 H', 1125 W m -2 ) compared to morning and afternoon (0.6-2.8 H'). This shift was associated with a decrease in the contribution to pyrolibraries by Cyanobacteria and an increase of Proteobacteria and other initially low frequently and rare bacteria phyla (< 0.5%) in the pyrolibraries. A potential increase in the activity of Cyanobacteria and other phototrophic groups, e.g., Rhodobacterales, was observed and associated with UVR, suggesting the presence of photo-activated repair mechanisms to resist high levels of solar radiation. In addition, the percentage contribution of cyanobacterial sequences in the afternoon was similar to those recorded in the morning. The shifts in the contribution by Cyanobacteria also influenced the rate of change in nitrate, nitrite, and phosphate, highlighted by a high level of nitrate accumulation during hours of high radiation and temperature associated with nitrifying bacteria activity. We did not detect ammonia or nitrite oxidizing bacteria in situ , but both functional groups ( Nitrosomona and Nitrospira ) appeared mainly in pyrolibraries generated from

  13. Bacterial Active Community Cycling in Response to Solar Radiation and Their Influence on Nutrient Changes in a High-Altitude Wetland

    PubMed Central

    Molina, Verónica; Hernández, Klaudia; Dorador, Cristina; Eissler, Yoanna; Hengst, Martha; Pérez, Vilma; Harrod, Chris

    2016-01-01

    Microbial communities inhabiting high-altitude spring ecosystems are subjected to extreme changes in solar irradiance and temperature throughout the diel cycle. Here, using 16S rRNA gene tag pyrosequencing (cDNA) we determined the composition of actively transcribing bacteria from spring waters experimentally exposed through the day (morning, noon, and afternoon) to variable levels of solar radiation and light quality, and evaluated their influence on nutrient recycling. Solar irradiance, temperature, and changes in nutrient dynamics were associated with changes in the active bacterial community structure, predominantly by Cyanobacteria, Verrucomicrobia, Proteobacteria, and 35 other Phyla, including the recently described Candidate Phyla Radiation (e.g., Parcubacteria, Gracilibacteria, OP3, TM6, SR1). Diversity increased at noon, when the highest irradiances were measured (3.3–3.9 H′, 1125 W m-2) compared to morning and afternoon (0.6–2.8 H′). This shift was associated with a decrease in the contribution to pyrolibraries by Cyanobacteria and an increase of Proteobacteria and other initially low frequently and rare bacteria phyla (< 0.5%) in the pyrolibraries. A potential increase in the activity of Cyanobacteria and other phototrophic groups, e.g., Rhodobacterales, was observed and associated with UVR, suggesting the presence of photo-activated repair mechanisms to resist high levels of solar radiation. In addition, the percentage contribution of cyanobacterial sequences in the afternoon was similar to those recorded in the morning. The shifts in the contribution by Cyanobacteria also influenced the rate of change in nitrate, nitrite, and phosphate, highlighted by a high level of nitrate accumulation during hours of high radiation and temperature associated with nitrifying bacteria activity. We did not detect ammonia or nitrite oxidizing bacteria in situ, but both functional groups (Nitrosomona and Nitrospira) appeared mainly in pyrolibraries generated from

  14. Heliobiology, its development, successes and tasks. [solar activity effects on life on earth

    NASA Technical Reports Server (NTRS)

    Platonova, A. T.

    1974-01-01

    Heliobiology studies the influence of changes in solar activity on life. Considered are the influence of periodic solar activity on the development and growth of epidemics, mortality from various diseases, the functional activity of the nervous system, the development of psychic disturbances, the details of the development of microorganisms and many other phenomena in the living world.

  15. Solar wind control of auroral zone geomagnetic activity

    NASA Technical Reports Server (NTRS)

    Clauer, C. R.; Mcpherron, R. L.; Searls, C.; Kivelson, M. G.

    1981-01-01

    Solar wind magnetosphere energy coupling functions are analyzed using linear prediction filtering with 2.5 minute data. The relationship of auroral zone geomagnetic activity to solar wind power input functions are examined, and a least squares prediction filter, or impulse response function is designed from the data. Computed impulse response functions are observed to have characteristics of a low pass filter with time delay. The AL index is found well related to solar wind energy functions, although the AU index shows a poor relationship. High frequency variations of auroral indices and substorm expansions are not predictable with solar wind information alone, suggesting influence by internal magnetospheric processes. Finally, the epsilon parameter shows a poorer relationship with auroral geomagnetic activity than a power parameter, having a VBs solar wind dependency.

  16. Evidence for distinct modes of solar activity

    NASA Astrophysics Data System (ADS)

    Usoskin, I. G.; Hulot, G.; Gallet, Y.; Roth, R.; Licht, A.; Joos, F.; Kovaltsov, G. A.; Thébault, E.; Khokhlov, A.

    2014-02-01

    Aims: The Sun shows strong variability in its magnetic activity, from Grand minima to Grand maxima, but the nature of the variability is not fully understood, mostly because of the insufficient length of the directly observed solar activity records and of uncertainties related to long-term reconstructions. Here we present a new adjustment-free reconstruction of solar activity over three millennia and study its different modes. Methods: We present a new adjustment-free, physical reconstruction of solar activity over the past three millennia, using the latest verified carbon cycle, 14C production, and archeomagnetic field models. This great improvement allowed us to study different modes of solar activity at an unprecedented level of details. Results: The distribution of solar activity is clearly bi-modal, implying the existence of distinct modes of activity. The main regular activity mode corresponds to moderate activity that varies in a relatively narrow band between sunspot numbers 20 and 67. The existence of a separate Grand minimum mode with reduced solar activity, which cannot be explained by random fluctuations of the regular mode, is confirmed at a high confidence level. The possible existence of a separate Grand maximum mode is also suggested, but the statistics is too low to reach a confident conclusion. Conclusions: The Sun is shown to operate in distinct modes - a main general mode, a Grand minimum mode corresponding to an inactive Sun, and a possible Grand maximum mode corresponding to an unusually active Sun. These results provide important constraints for both dynamo models of Sun-like stars and investigations of possible solar influence on Earth's climate. Data are only available at the CDS via anonymous ftp to http://cdsarc.u-strasbg.fr (ftp://130.79.128.5) or via http://cdsarc.u-strasbg.fr/viz-bin/qcat?J/A+A/562/L10

  17. The influence of nonstationarity of the solar activity and general solar field on modulation of cosmic rays

    NASA Technical Reports Server (NTRS)

    Zusmanovich, A. G.; Kryakunova, O. N.; Churunova, L. F.; Shvartsman, Y. E.

    1985-01-01

    A numerical model of the propagation of galactic cosmic rays in interplanetary space was constructed for the case when the modulation depth determined by the level of solar activity changed in time. Also the contribution of particle drift in the regular field was calculated, and the agreement with experimental data concerning the ratio of protons and electrons in two solar activity minima is shown.

  18. Influence of solar activity on fibrinolysis and fibrinogenolysis. [statistical correlation between solar flare and blood coagulation indices

    NASA Technical Reports Server (NTRS)

    Marchenko, V. I.

    1974-01-01

    During periods of high solar activity fibrinolysis and fibrinogenolysis are increased. A direct correlative relationship is established between the indices of fibrinolysis, fibrinogenolysis and solar flares which were recorded two days before the blood was collected for analysis.

  19. Geomagnetic activity: Dependence on solar wind parameters

    NASA Technical Reports Server (NTRS)

    Svalgaard, L.

    1977-01-01

    Current ideas about the interaction between the solar wind and the earth's magnetosphere are reviewed. The solar wind dynamic pressure as well as the influx of interplanetary magnetic field lines are both important for the generation of geomagnetic activity. The influence of the geometry of the situation as well as the variability of the interplanetary magnetic field are both found to be important factors. Semi-annual and universal time variations are discussed as well as the 22-year cycle in geomagnetic activity. All three are found to be explainable by the varying geometry of the interaction. Long term changes in geomagnetic activity are examined.

  20. Influence of solar variability on the occurrence of central European weather types from 1763 to 2009

    NASA Astrophysics Data System (ADS)

    Schwander, Mikhaël; Rohrer, Marco; Brönnimann, Stefan; Malik, Abdul

    2017-09-01

    The impact of solar variability on weather and climate in central Europe is still not well understood. In this paper we use a new time series of daily weather types to analyse the influence of the 11-year solar cycle on the tropospheric weather of central Europe. We employ a novel, daily weather type classification over the period 1763-2009 and investigate the occurrence frequency of weather types under low, moderate, and high solar activity level. Results show a tendency towards fewer days with westerly and west-southwesterly flow over central Europe under low solar activity. In parallel, the occurrence of northerly and easterly types increases. For the 1958-2009 period, a more detailed view can be gained from reanalysis data. Mean sea level pressure composites under low solar activity also show a reduced zonal flow, with an increase of the mean blocking frequency between Iceland and Scandinavia. Weather types and reanalysis data show that the 11-year solar cycle influences the late winter atmospheric circulation over central Europe with colder (warmer) conditions under low (high) solar activity.

  1. Initiation of non-tropical thunderstorms by solar activity

    NASA Technical Reports Server (NTRS)

    Herman, J. R.; Goldberg, R. A.

    1976-01-01

    Correlative evidence accumulating since 1926 suggests that there must be some physical coupling mechanism between solar activity and thunderstorm occurrence in middle to high latitudes. Such a link may be provided by alteration of atmospheric electric parameters through the combined influence of high-energy solar protons and decreased cosmic ray intensities, both of which are associated with active solar events. The protons produce excess ionization near and above 20km, while the Forbush decreases a lowered conductivity and enhanced fair-weather atmospheric electric field below that altitude. Consequent effects ultimately lead to a charge distribution similar to that found in thunderclouds, and then other cloud physics processes take over to generate the intense electric fields required for lightning discharge.

  2. The risk characteristics of solar and geomagnetic activity

    NASA Astrophysics Data System (ADS)

    Podolska, Katerina

    2016-04-01

    The main aim of this contribution is a deeper analysis of the influence of solar activity which is expected to have an impact on human health, and therefore on mortality, in particular civilization and degenerative diseases. We have constructed the characteristics that represent the risk of solar and geomagnetic activity on human health on the basis of our previous analysis of association between the daily numbers of death on diseases of the nervous system and diseases of the circulatory system and solar and geomagnetic activity in the Czech Republic during the years 1994 - 2013. We used long period daily time series of numbers of deaths by cause, long period time series of solar activity indices (namely R and F10.7), geomagnetic indicies (Kp planetary index, Dst) and ionospheric parameters (foF2 and TEC). The ionospheric parameters were related to the geographic location of the Czech Republic and adjusted for middle geographic latitudes. The risk characteristics were composed by cluster analysis in time series according to the phases of the solar cycle resp. the seasonal insolation at mid-latitudes or the daily period according to the impact of solar and geomagnetic activity on mortality by cause of death from medical cause groups of death VI. Diseases of the nervous system and IX. Diseases of the circulatory system mortality by 10th Revision of International Classification of Diseases WHO (ICD-10).

  3. The Solar Dynamics Observatory, Studying the Sun and Its Influence on Other Bodies in the Solar System

    NASA Technical Reports Server (NTRS)

    Chamberlin, P. C.

    2011-01-01

    The solar photon output, which was once thought to be constant, varies over all time scales from seconds during solar flares to years due to the solar cycle. These solar variations cause significant deviations in the Earth and space environments on similar time scales, such as affecting the atmospheric densities and composition of particular atoms, molecules, and ions in the atmospheres of the Earth and other planets. Presented and discussed will be examples of unprecedented observations from NASA's new solar observatory, the Solar Dynamics Observatory (SDO). Using three specialized instruments, SDO measures the origins of solar activity from inside the Sun, though its atmosphere, then accurately measuring the Sun's radiative output in X-ray and EUV wavelengths (0.1-121 nm). Along with the visually appealing observations will be discussions of what these measurements can tell us about how the plasma motions in all layers of the Sun modifies and strengthens the weak solar dipole magnetic field to drive large energy releases in solar eruptions. Also presented will be examples of how the release of the Sun's energy, in the form of photons and high energy particles, physically influence other bodies in the solar system such as Earth, Mars, and the Moon, and how these changes drive changes in the technology that we are becoming dependent upon. The presentation will continuously emphasize how SDO, the first satellite in NASA's Living with a Star program, improving our understanding of the variable Sun and its Heliospheric influence.

  4. Resonance of about-weekly human heart rate rhythm with solar activity change.

    PubMed

    Cornelissen, G; Halberg, F; Wendt, H W; Bingham, C; Sothern, R B; Haus, E; Kleitman, E; Kleitman, N; Revilla, M A; Revilla, M; Breus, T K; Pimenov, K; Grigoriev, A E; Mitish, M D; Yatsyk, G V; Syutkina, E V

    1996-12-01

    In several human adults, certain solar activity rhythms may influence an about 7-day rhythm in heart rate. When no about-weekly feature was found in the rate of change in sunspot area, a measure of solar activity, the double amplitude of a circadian heart rate rhythm, approximated by the fit of a 7-day cosine curve, was lower, as was heart rate corresponds to about-weekly features in solar activity and/or relates to a sunspot cycle.

  5. Analysis of regression methods for solar activity forecasting

    NASA Technical Reports Server (NTRS)

    Lundquist, C. A.; Vaughan, W. W.

    1979-01-01

    The paper deals with the potential use of the most recent solar data to project trends in the next few years. Assuming that a mode of solar influence on weather can be identified, advantageous use of that knowledge presumably depends on estimating future solar activity. A frequently used technique for solar cycle predictions is a linear regression procedure along the lines formulated by McNish and Lincoln (1949). The paper presents a sensitivity analysis of the behavior of such regression methods relative to the following aspects: cycle minimum, time into cycle, composition of historical data base, and unnormalized vs. normalized solar cycle data. Comparative solar cycle forecasts for several past cycles are presented as to these aspects of the input data. Implications for the current cycle, No. 21, are also given.

  6. Online educative activities for solar ultraviolet radiation based on measurements of cloud amount and solar exposures.

    PubMed

    Parisi, A V; Downs, N; Turner, J; Amar, A

    2016-09-01

    A set of online activities for children and the community that are based on an integrated real-time solar UV and cloud measurement system are described. These activities use the functionality of the internet to provide an educative tool for school children and the public on the influence of cloud and the angle of the sun above the horizon on the global erythemal UV or sunburning UV, the diffuse erythemal UV, the global UVA (320-400nm) and the vitamin D effective UV. Additionally, the units of UV exposure and UV irradiance are investigated, along with the meaning and calculation of the UV index (UVI). This research will help ensure that children and the general public are better informed about sun safety by improving their personal understanding of the daily and the atmospheric factors that influence solar UV radiation and the solar UV exposures of the various wavebands in the natural environment. The activities may correct common misconceptions of children and the public about UV irradiances and exposure, utilising the widespread reach of the internet to increase the public's awareness of the factors influencing UV irradiances and exposures in order to provide clear information for minimizing UV exposure, while maintaining healthy, outdoor lifestyles. Copyright © 2016 Elsevier B.V. All rights reserved.

  7. Some problems in coupling solar activity to meteorological phenomena

    NASA Technical Reports Server (NTRS)

    Dessler, A. J.

    1975-01-01

    The development of a theory of coupling of solar activity to meteorological phenomena is hindered by the difficulties of devising a mechanism that can modify the behavior of the troposphere while employing only a negligible amount of energy compared with the energy necessary to drive the normal meteorological system, and determining how such a mechanism can effectively couple some relevant magnetospheric process into the troposphere in such a way as to influence the weather. A clue to the nature of the interaction between the weather and solar activity might be provided by the fact that most solar activity undergoes a definite 11-yr cycle, and meteorological phenomena undergo either no closely correlated variation, an 11-yr variation, or a 22-yr variation.

  8. Temporal Variations of Different Solar Activity Indices Through the Solar Cycles 21-23

    NASA Astrophysics Data System (ADS)

    Göker, Ü. D.; Singh, J.; Nutku, F.; Priyal, M.

    2017-12-01

    Here, we compare the sunspot counts and the number of sunspot groups (SGs) with variations of total solar irradiance (TSI), magnetic activity, Ca II K-flux, faculae and plage areas. We applied a time series method for extracting the data over the descending phases of solar activity cycles (SACs) 21, 22 and 23, and the ascending phases 22 and 23. Our results suggest that there is a strong correlation between solar activity indices and the changes in small (A, B, C and H-modified Zurich Classification) and large (D, E and F) SGs. This somewhat unexpected finding suggests that plage regions substantially decreased in spite of the higher number of large SGs in SAC 23 while the Ca II K-flux did not decrease by a large amount nor was it comparable with SAC 22 and relates with C and DEF type SGs. In addition to this, the increase of facular areas which are influenced by large SGs, caused a small percentage decrease in TSI while the decrement of plage areas triggered a higher decrease in the magnetic field flux. Our results thus reveal the potential of such a detailed comparison of the SG analysis with solar activity indices for better understanding and predicting future trends in the SACs.

  9. Deciphering Solar Magnetic Activity: On Grand Minima in Solar Activity

    NASA Astrophysics Data System (ADS)

    Mcintosh, Scott; Leamon, Robert

    2015-07-01

    The Sun provides the energy necessary to sustain our existence. While the Sun provides for us, it is also capable of taking away. The weather and climatic scales of solar evolution and the Sun-Earth connection are not well understood. There has been tremendous progress in the century since the discovery of solar magnetism - magnetism that ultimately drives the electromagnetic, particulate and eruptive forcing of our planetary system. There is contemporary evidence of a decrease in solar magnetism, perhaps even indicators of a significant downward trend, over recent decades. Are we entering a minimum in solar activity that is deeper and longer than a typical solar minimum, a "grand minimum"? How could we tell if we are? What is a grand minimum and how does the Sun recover? These are very pertinent questions for modern civilization. In this paper we present a hypothetical demonstration of entry and exit from grand minimum conditions based on a recent analysis of solar features over the past 20 years and their possible connection to the origins of the 11(-ish) year solar activity cycle.

  10. Some problems in coupling solar activity to meteorological phenomena

    NASA Technical Reports Server (NTRS)

    Dessler, A. J.

    1974-01-01

    The development of a theory of coupling of solar activity to meteorological phenomena has to date foundered on the two difficulties of (1) devising a mechanism that can modify the behavior of the troposphere while employing only a negligible amount of energy compared with the energy necessary to drive the normal meteorological system; and (2) determining how such a mechanism can effectively couple some relevant magnetospheric process into the troposphere in such a way as to influence the weather. A clue to the nature of the interaction between the weather and solar activity might be provided by the fact that most solar activity undergoes a definite 11-year cycle, while meteorological phenomena undergo either no closely correlated variation, or an 11-year variation, or a 22-year variation.

  11. Apparent Relations Between Solar Activity and Solar Tides Caused by the Planets

    NASA Technical Reports Server (NTRS)

    Hung, Ching-Cheh

    2007-01-01

    A solar storm is a storm of ions and electrons from the Sun. Large solar storms are usually preceded by solar flares, phenomena that can be characterized quantitatively from Earth. Twenty-five of the thirty-eight largest known solar flares were observed to start when one or more tide-producing planets (Mercury, Venus, Earth, and Jupiter) were either nearly above the event positions (less than 10 deg. longitude) or at the opposing side of the Sun. The probability for this to happen at random is 0.039 percent. This supports the hypothesis that the force or momentum balance (between the solar atmospheric pressure, the gravity field, and magnetic field) on plasma in the looping magnetic field lines in solar corona could be disturbed by tides, resulting in magnetic field reconnection, solar flares, and solar storms. Separately, from the daily position data of Venus, Earth, and Jupiter, an 11-year planet alignment cycle is observed to approximately match the sunspot cycle. This observation supports the hypothesis that the resonance and beat between the solar tide cycle and nontidal solar activity cycle influences the sunspot cycle and its varying magnitudes. The above relations between the unpredictable solar flares and the predictable solar tidal effects could be used and further developed to forecast the dangerous space weather and therefore reduce its destructive power against the humans in space and satellites controlling mobile phones and global positioning satellite (GPS) systems.

  12. Ion Mediated Nucleation: how is it Influenced by Changes in the Solar Activity?

    NASA Astrophysics Data System (ADS)

    D'Auria, R.; Turco, R. P.

    2003-12-01

    Recently it has been pointed out that tropospheric cloudiness can be correlated with the galactic cosmic rays (GCRs) intensity [Svensmark and Friis-Christensen, 1997]. A possible explanation for such a correlation relies on the fact that GCRs are the main ionization source in the upper troposphere, hence, throughout ionic mediated nucleation, they could possibly influence the global cloud condensation nuclei (CCN) formation [e.g., Yu, 2001; Dickinson, 1975]. Because the GCRs are modulated by the interaction between the solar wind and the Earth's magnetosphere and their intensity generally decreases with increasing solar activity, subtle changes in the solar activity could indirectly affect the Earth's climate. We have been studying the very first steps of ionic nucleation considering the molecular species of atmospheric interest (e.g.,water, nitric acid, sulfuric acid, ammonia etc.). In our approach the formation and evolution of ionic clusters is followed by resolving the time dependent kinetic aggregation process and considering the ions sources (ultimately the atmospheric ionization of neutral species) and sinks. We show how in typical atmospheric conditions stable populations of molecular ions forms. The novelty of our work consists in the determination of the kinetic parameters that govern the molecular ions growth (i.e., the forward and reverse clustering reaction constants for each cluster type and size) at a microscopic level. In fact a thermochemistry data base is built for the species of interest by integrating laboratory measurements, quantum mechanical calculations and, when appropriate, results from the macroscopic liquid droplet model [Thomson, 1928]. Such database is than used to retrieve the reverse clustering reaction coefficients for the molecular ion type and size and for the environmental conditions (pressure and temperature) of interest. The forward reaction is instead determined by calculating the ionic-neutral collisional rate or is assumed

  13. A Forecast of Reduced Solar Activity and Its Implications for NASA

    NASA Technical Reports Server (NTRS)

    Schatten, Kenneth; Franz, Heather

    2005-01-01

    The "Solar Dynamo" method of solar activity forecasting is reviewed. Known generically as a 'precursor" method, insofar as it uses observations which precede solar activity generation, this method now uses the Solar Dynamo Amplitude (SODA) Index to estimate future long-term solar activity. The peak amplitude of the next solar cycle (#24), is estimated at roughly 124 in terms of smoothed F10.7 Radio Flux and 74 in terms of the older, more traditional smoothed international or Zurich Sunspot number (Ri or Rz). These values are significantly smaller than the amplitudes of recent solar cycles. Levels of activity stay large for about four years near the peak in smoothed activity, which is estimated to occur near the 2012 timeflame. Confidence is added to the prediction of low activity by numerous examinations of the Sun s weakened polar field. Direct measurements are obtained by the Mount Wilson Solar Observatory and the Wilcox Solar Observatory. Further support is obtained by examining the Sun s polar faculae (bright features), the shape of coronal soft X-ray "holes," and the shape of the "source surface" - a calculated coronal feature which maps the large scale structure of the Sun s field. These features do not show the characteristics of well-formed polar coronal holes associated with typical solar minima. They show stunted polar field levels, which are thought to result in stunted levels of solar activity during solar cycle #24. The reduced levels of solar activity would have concomitant effects upon the space environment in which satellites orbit. In particular, the largest influences would affect orbit determination of satellites in LEO (Low Earth Orbit), based upon the altered thermospheric and exospheric densities. A decrease in solar activity would result in smaller satellite decay rates, as well as fewer large solar events that can destroy satellite electronic functions. Other effects of reduced solar activity upon the space environment include enhanced

  14. Possible helio-geomagnetic activity influence on cardiological cases

    NASA Astrophysics Data System (ADS)

    Katsavrias, Christos

    Eruptive solar events as flares and coronal mass ejections (CMEs) occur during solar activ-ity periods. Energetic particles, fast solar wind plasma and electromagnetic radiation pass through interplanetary space, arrive on Earth's ionosphere-magnetosphere and produce various disturbances. It is well known the negative influence of geomagnetic substorms on the human technological applications on geospace. During the last 25 years, many studies concerning the possible influence on the human health are published. Increase of the Acute Coronary Syn-dromes and disorders of the Cardiac Rhythm, increase of accidents as well as neurological and psychological disorders (e.g. increase of suicides) during or near to the geomagnetic storms time interval are reported. In this study, we research the problem in Greece, focusing on patients with Acute Myocardial Infraction, hospitalized in the 2nd Cardiological Department of the General Hospital of Nikaea (Piraeus City), for the time interval 1997-2007 (23rd solar cycle) and also to the arrival of emergency cardiological cases to Emergency Department of two greek hospitals, the General Hospital of Lamia City and the General Hospital of Veria City during the selected months, with or without helio-geomagnetic activity, of the 23rd solar cycle. Increase of cases is recorded during the periods with increase helio-geomagnetic activity. The necessity of continuing the research for a longer period and with a bigger sample is high; so as to exact more secure conclusions.

  15. Quasi-biennial modulation of solar neutrino flux: connections with solar activity

    NASA Astrophysics Data System (ADS)

    Vecchio, A.; Laurenza, M.; D'alessi, L.; Carbone, V.; Storini, M.

    2011-12-01

    A quasi-biennial periodicity has been recently found (Vecchio et al., 2010) in the solar neutrino flux, as detected at the Homestake experiment, as well as in the flux of solar energetic protons, by means of the Empirical Modes Decomposition technique. Moreover, both fluxes have been found to be significantly correlated at the quasi-biennial timescale, thus supporting the hypothesis of a connection between solar neutrinos and solar activity. The origin of this connection is investigated, by modeling how the standard Mikheyev-Smirnov-Wolfenstein (MSW) effect (the process for which the well-known neutrino flavor oscillations are modified in passing through the material) could be influenced by matter fluctuations. As proposed by Burgess et al., 2004, by introducing a background magnetic field in the helioseismic model, density fluctuations can be excited in the radiative zone by the resonance between helioseismic g-modes and Alfvén waves. In particular, with reasonable values of the background magnetic field (10-100 kG), the distance between resonant layers could be of the same order of neutrino oscillation length. We study the effect over this distance of a background magnetic field which is variable with a ~2 yr period, in agreement with typical variations of solar activity. Our findings suggest that the quasi-biennial modulation of the neutrino flux is theoretically possible as a consequence of the magnetic field variations in the solar interior. A. Vecchio, M. Laurenza, V. Carbone, M. Storini, The Astrophysical Journal Letters, 709, L1-L5 (2010). C. Burgess, N. S. Dzhalilov, T. I. Rashba, V., B.Semikoz, J. W. F. Valle, Mon. Not. R. Astron. Soc., 348, 609-624 (2004).

  16. Activities for Teaching Solar Energy.

    ERIC Educational Resources Information Center

    Mason, Jack Lee; Cantrell, Joseph S.

    1980-01-01

    Plans and activities are suggested for teaching elementary children about solar energy. Directions are included for constructing a flat plate collector and a solar oven. Activities for a solar field day are given. (SA)

  17. Global Solar Magnetic Field Organization in the Outer Corona: Influence on the Solar Wind Speed and Mass Flux Over the Cycle

    NASA Astrophysics Data System (ADS)

    Réville, Victor; Brun, Allan Sacha

    2017-11-01

    The dynamics of the solar wind depends intrinsically on the structure of the global solar magnetic field, which undergoes fundamental changes over the 11-year solar cycle. For instance, the wind terminal velocity is thought to be anti-correlated with the expansion factor, a measure of how the magnetic field varies with height in the solar corona, usually computed at a fixed height (≈ 2.5 {R}⊙ , the source surface radius that approximates the distance at which all magnetic field lines become open). However, the magnetic field expansion affects the solar wind in a more detailed way, its influence on the solar wind properties remaining significant well beyond the source surface. We demonstrate this using 3D global magnetohydrodynamic (MHD) simulations of the solar corona, constrained by surface magnetograms over half a solar cycle (1989-2001). A self-consistent expansion beyond the solar wind critical point (even up to 10 {R}⊙ ) makes our model comply with observed characteristics of the solar wind, namely, that the radial magnetic field intensity becomes latitude independent at some distance from the Sun, and that the mass flux is mostly independent of the terminal wind speed. We also show that near activity minimum, the expansion in the higher corona has more influence on the wind speed than the expansion below 2.5 {R}⊙ .

  18. The solar activity measurements experiments (SAMEX) for improved scientific understanding of solar activity

    NASA Technical Reports Server (NTRS)

    1989-01-01

    The Solar Activity Measurements Experiments (SAMEX) mission is described. It is designed to provide a look at the interactions of magnetic fields and plasmas that create flares and other explosive events on the sun in an effort to understand solar activity and the nature of the solar magnetic field. The need for this mission, the instruments to be used, and the expected benefits of SAMEX are discussed.

  19. Influence of the solar wind/interplanetary medium on Saturnian kilometric radiation

    NASA Technical Reports Server (NTRS)

    Rucker, Helmut O.; Desch, M. D.

    1990-01-01

    Previous studies on the periodicities of the Saturnian kilometric radiation (SKR) suggested a considerable solar wind influence on the occurrence of SKR, so it was obvious to investigate the relationship between parameters of the solar wind/interplanetary medium and this Saturnian radio component. Voyager 2 data from the Plasma Science experiment, the Magnetometer experiment and the Planetary Radio Astronomy experiment were used to analyze the external control of SKR. Out of the examined quantities known to be important in controlling magnetospheric processes this investigation yielded a dominance of the solar wind momentum, ram pressure and kinetic energy flux, in stimulating SKR and controlling its activity and emitted energy, and confirmed the results of the Voyager 1 analysis.

  20. Solar Activity and Solar Eruptions

    NASA Technical Reports Server (NTRS)

    Sterling, Alphonse C.

    2006-01-01

    Our Sun is a dynamic, ever-changing star. In general, its atmosphere displays major variation on an 11-year cycle. Throughout the cycle, the atmosphere occasionally exhibits large, sudden outbursts of energy. These "solar eruptions" manifest themselves in the form of solar flares, filament eruptions, coronal mass ejections (CMEs), and energetic particle releases. They are of high interest to scientists both because they represent fundamental processes that occur in various astrophysical context, and because, if directed toward Earth, they can disrupt Earth-based systems and satellites. Research over the last few decades has shown that the source of the eruptions is localized regions of energy-storing magnetic field on the Sun that become destabilized, leading to a release of the stored energy. Solar scientists have (probably) unraveled the basic outline of what happens in these eruptions, but many details are still not understood. In recent years we have been studying what triggers these magnetic eruptions, using ground-based and satellite-based solar observations in combination with predictions from various theoretical models. We will present an overview of solar activity and solar eruptions, give results from some of our own research, and discuss questions that remain to be explored.

  1. Solar Spots - Activities to Introduce Solar Energy into the K-8 Curricula.

    ERIC Educational Resources Information Center

    Longe, Karen M.; McClelland, Michael J.

    Following an introduction to solar technology which reviews solar heating and cooling, passive solar systems (direct gain systems, thermal storage walls, sun spaces, roof ponds, and convection loops), active solar systems, solar electricity (photovoltaic and solar thermal conversion systems), wind energy, and biomass, activities to introduce solar…

  2. The Long-term Middle Atmospheric Influence of Very Large Solar Proton Events

    NASA Technical Reports Server (NTRS)

    Jackman, Charles H.; Marsh, Daniel R.; Vitt, Francis M.; Garcia, Rolando R.; Randall, Cora E.; Fleming, Eric L.; Frith, Stacey M.

    2008-01-01

    Long-term variations in ozone have been caused by both natural and humankind related processes. The humankind or anthropogenic influence on ozone originates from the chlorofluorocarbons and halons (chlorine and bromine) and has led to international regulations greatly limiting the release of these substances. Certain natural ozone influences are also important in polar regions and are caused by the impact of solar charged particles on the atmosphere. Such natural variations have been studied in order to better quantify the human influence on polar ozone. Large-scale explosions on the Sun near solar maximum lead to emissions of charged particles (mainly protons and electrons), some of which enter the Earth's magnetosphere and rain down on the polar regions. "Solar proton events" have been used to describe these phenomena since the protons associated with these solar events sometimes create a significant atmospheric disturbance. We have used the National Center for Atmospheric Research (NCAR) Whole Atmosphere Community Climate Model (WACCM) to study the long-term (> few months) influences of solar proton events from 1963 through 2004 on stratospheric ozone and temperature. There were extremely large solar proton events in 1972, 1989,2000,2001, and 2003. These events caused very distinctive polar changes in layers of the Earth's atmosphere known as the stratosphere (12-50 km; -7-30 miles) and mesosphere (50-90 km; 30-55 miles). The solar protons connected with these events created hydrogen- and nitrogen-containing compounds, which led to the polar ozone destruction. The nitrogen-containing compounds, called odd nitrogen, lasted much longer than the hydrogen-containing compounds and led to long-lived stratospheric impacts. An extremely active period for these events occurred in the five-year period, 2000- 2004, and caused increases in odd nitrogen which lasted for several months after individual events. Associated stratospheric ozone decreases of >lo% were calculated

  3. Solar Wind-Magnetosphere Coupling Influences on Pseudo-Breakup Activity

    NASA Technical Reports Server (NTRS)

    Fillingim, M. O.; Brittnacher, M.; Parks, G. K.; Germany, G. A.; Spann, J. F.

    1998-01-01

    Pseudo-breakups are brief, localized aurora[ arc brightening, which do not lead to a global expansion, are historically observed during the growth phase of substorms. Previous studies have demonstrated that phenomenologically there is very little difference between substorm onsets and pseudo-breakups except for the degree of localization and the absence of a global expansion phase. A key open question is what physical mechanism prevents a pseudo-breakup form expanding globally. Using Polar Ultraviolet Imager (UVI) images, we identify periods of pseudo-breakup activity. Foe the data analyzed we find that most pseudo-breakups occur near local midnight, between magnetic local times of 21 and 03, at magnetic latitudes near 70 degrees, through this value may change by several degrees. While often discussed in the context of substorm growth phase events, pseudo-breakups are also shown to occur during prolonged relatively inactive periods. These quiet time pseudo-breakups can occur over a period of several hours without the development of a significant substorm for at least an hour after pseudo-breakup activity stops. In an attempt to understand the cause of quiet time pseudo-breakups, we compute the epsilon parameter as a measure of the efficiency of solar wind-magnetosphere coupling. It is noted that quiet time pseudo-breakups occur typically when epsilon is low; less than about 50 GW. We suggest that quiet time pseudo-breakups are driven by relatively small amounts of energy transferred to the magnetosphere by the solar wind insufficient to initiate a substorm expansion onset.

  4. On the influence of solar activity on the mid-latitude sporadic E layer

    NASA Astrophysics Data System (ADS)

    Pezzopane, Michael; Pignalberi, Alessio; Pietrella, Marco

    2015-09-01

    To investigate the influence of solar cycle variability on the sporadic E layer (Es), hourly measurements of the critical frequency of the Es ordinary mode of propagation, foEs, and of the blanketing frequency of the Es layer, fbEs, recorded from January 1976 to December 2009 at the Rome (Italy) ionospheric station (41.8° N, 12.5° E), were examined. The results are: (1) a high positive correlation between the F10.7 solar index and foEs as well as between F10.7 and fbEs, both for the whole data set and for each solar cycle separately, the correlation between F10.7 and fbEs being much higher than the one between F10.7 and foEs; (2) a decreasing long-term trend of the F10.7, foEs and fbEs time series, with foEs decreasing more rapidly than F10.7 and fbEs; (3) clear and statistically significant peaks at 11 years in the foEs and fbEs time series, inferred from Lomb-Scargle periodograms.

  5. The calculated influence of atmospheric conditions on solar cell ISC under direct and global solar irradiances

    NASA Technical Reports Server (NTRS)

    Mueller, Robert L.

    1987-01-01

    Calculations of the influence of atmospheric conditions on solar cell short-circuit current (Isc) are made using a recently developed computer model for solar spectral irradiance distribution. The results isolate the dependence of Isc on changes in the spectral irradiance distribution without the direct influence of the total irradiance level. The calculated direct normal irradiance and percent diffuse irradiance are given as a reference to indicate the expected irradiance levels. This method can be applied to the calibration of photovoltaic reference cells. Graphic examples are provided for amorphous silicon and monocrystalline silicon solar cells under direct normal and global normal solar irradiances.

  6. Solar activity as driver for the Dark Age Grand Solar Minimum

    NASA Astrophysics Data System (ADS)

    Neuhäuser, Ralph; Neuhäuser, Dagmar

    2017-04-01

    We will discuss the role of solar activity for the temperature variability from AD 550 to 840, roughly the last three centuries of the Dark Ages. This time range includes the so-called Dark Age Grand Solar Minimum, whose deep part is dated to about AD 650 to 700, which is seen in increased radiocarbon, but decreased aurora observations (and a lack of naked-eye sunspot sightings). We present historical reports on aurorae from all human cultures with written reports including East Asia, Near East (Arabia), and Europe. To classify such reports correctly, clear criteria are needed, which are also discussed. We compare our catalog of historical aurorae (and sunspots) as well as C-14 data, i.e. solar activity proxies, with temperature reconstructions (PAGES). After increased solar activity until around AD 600, we see a dearth of aurorae and increased radiocarbon production in particular in the second half of the 7th century, i.e. a typical Grand Solar Minimum. Then, after about AD 690 (the maximum in radiocarbon, the end of the Dark Age Grand Minimum), we see increased auroral activity, decreasing radiocarbon, and increasing temperature until about AD 775. At around AD 775, we see the well-known strong C-14 variability (solar activity drop), then immediately another dearth of aurorae plus high C-14, indicating another solar activity minimum. This is consistent with a temperature depression from about AD 775 on into the beginning of the 9th century. Very high solar activity is then seen in the first four decades with four aurora clusters and three simultaneous sunspot clusters, and low C-14, again also increasing temperature. The period of increasing solar activity marks the end of the so-called Dark Ages: While auroral activity increases since about AD 793, temperature starts to increase quite exactly at AD 800. We can reconstruct the Schwabe cycles with aurorae and C-14 data. In summary, we can see a clear correspondence of the variability of solar activity proxies and

  7. Influence of the Solar Cycle on Turbulence Properties and Cosmic-Ray Diffusion

    NASA Astrophysics Data System (ADS)

    Zhao, L.-L.; Adhikari, L.; Zank, G. P.; Hu, Q.; Feng, X. S.

    2018-04-01

    The solar cycle dependence of various turbulence quantities and cosmic-ray (CR) diffusion coefficients is investigated by using OMNI 1 minute resolution data over 22 years. We employ Elsässer variables z ± to calculate the magnetic field turbulence energy and correlation lengths for both the inwardly and outwardly directed interplanetary magnetic field (IMF). We present the temporal evolution of both large-scale solar wind (SW) plasma variables and small-scale magnetic fluctuations. Based on these observed quantities, we study the influence of solar activity on CR parallel and perpendicular diffusion using quasi-linear theory and nonlinear guiding center theory, respectively. We also evaluate the radial evolution of the CR diffusion coefficients by using the boundary conditions for different solar activity levels. We find that in the ecliptic plane at 1 au (1), the large-scale SW temperature T, velocity V sw, Alfvén speed V A , and IMF magnitude B 0 are positively related to solar activity; (2) the fluctuating magnetic energy density < {{z}+/- }2> , residual energy E D , and corresponding correlation functions all have an obvious solar cycle dependence. The residual energy E D is always negative, which indicates that the energy in magnetic fluctuations is larger than the energy in kinetic fluctuations, especially at solar maximum; (3) the correlation length λ for magnetic fluctuations does not show significant solar cycle variation; (4) the temporally varying shear source of turbulence, which is most important in the inner heliosphere, depends on the solar cycle; (5) small-scale fluctuations may not depend on the direction of the background magnetic field; and (6) high levels of SW fluctuations will increase CR perpendicular diffusion and decrease CR parallel diffusion, but this trend can be masked if the background IMF changes in concert with turbulence in response to solar activity. These results provide quantitative inputs for both turbulence transport

  8. Morphology of equatorial plasma bubbles during low and high solar activity years over Indian sector

    NASA Astrophysics Data System (ADS)

    Kumar, Sanjay

    2017-05-01

    In the present study, slant total electron content (STEC) data computed from ground based GPS measurements over Hyderabad (Geog. Lat. 17.41° N, geog. long. 78.55° E, mag. lat. 08.81° N) and two close stations at Bangalore (Geog. Lat. 13.02°/13.03° N, geog. long. 77.57°/77.51° E, mag. lat. 04.53°/04.55° N) in Indian region during 2007-2012, have been used to study the occurrences and characteristics of equatorial plasma bubbles (EPBs). The analysis found maximum EPB occurrences during the equinoctial months and minimum during the December solstice throughout 2007-2012 except during the solar minimum years in 2007-2009. During 2007-2009, the maximum EPB occurrences were observed in June solstice which could not be predicted by the model proposed by Tsunoda (J. Geophys. Res., 90:447-456, 1985). The equinox maximum in EPB occurrences for high solar activity years could be caused by the vertical F-layer drift due to pre-reversal electric field (PRE), and expected to be maximum when day-night terminator aligns with the magnetic meridian i.e. during the equinox months whereas maximum occurrences during the solstice months of solar minimum could be caused by the seed perturbation in plasma density induced by gravity waves from tropospheric origins. Generally EPB occurrences are found to be more prominent during nighttime hours (2000-2400 hours) than the daytime hours. Peak in EPB occurrences is in early night for high solar activity years whereas same is late night for low solar activity. The day and nighttime EPB occurrences have been analyzed and found to vary in accordance with solar activity with an annual correlation coefficient (R) of ˜0.99 with F_{10.7} cm solar Flux. Additionally, solar activity influence on EPB occurrences is seasonal dependent with a maximum influence during the equinox season (R=0.88) and a minimum during winter season (R =0.73). The solar activity influences on EPB occurrences are found in agreement with the previous works reported in

  9. Solar activities and Climate change hazards

    NASA Astrophysics Data System (ADS)

    Hady, A. A., II

    2014-12-01

    Throughout the geological history of Earth, climate change is one of the recurrent natural hazards. In recent history, the impact of man brought about additional climatic change. Solar activities have had notable effect on palaeoclimatic changes. Contemporary, both solar activities and building-up of green-house gases effect added to the climatic changes. This paper discusses if the global worming caused by the green-house gases effect will be equal or less than the global cooling resulting from the solar activities. In this respect, we refer to the Modern Dalton Minimum (MDM) which stated that starting from year 2005 for the next 40 years; the earth's surface temperature will become cooler than nowadays. However the degree of cooling, previously mentioned in old Dalton Minimum (c. 210 y ago), will be minimized by building-up of green-house gases effect during MDM period. Regarding to the periodicities of solar activities, it is clear that now we have a new solar cycle of around 210 years. Keywords: Solar activities; solar cycles; palaeoclimatic changes; Global cooling; Modern Dalton Minimum.

  10. Solar wind influence on Jupiter's magnetosphere and aurora

    NASA Astrophysics Data System (ADS)

    Vogt, Marissa; Gyalay, Szilard; Withers, Paul

    2016-04-01

    Jupiter's magnetosphere is often said to be rotationally driven, with strong centrifugal stresses due to large spatial scales and a rapid planetary rotation period. For example, the main auroral emission at Jupiter is not due to the magnetosphere-solar wind interaction but is driven by a system of corotation enforcement currents that arises to speed up outflowing Iogenic plasma. Additionally, processes like tail reconnection are also thought to be driven, at least in part, by processes internal to the magnetosphere. While the solar wind is generally expected to have only a small influence on Jupiter's magnetosphere and aurora, there is considerable observational evidence that the solar wind does affect the magnetopause standoff distance, auroral radio emissions, and the position and brightness of the UV auroral emissions. We will report on the results of a comprehensive, quantitative study of the influence of the solar wind on various magnetospheric data sets measured by the Galileo mission from 1996 to 2003. Using the Michigan Solar Wind Model (mSWiM) to predict the solar wind conditions upstream of Jupiter, we have identified intervals of high and low solar wind dynamic pressure. We can use this information to quantify how a magnetospheric compression affects the magnetospheric field configuration, which in turn will affect the ionospheric mapping of the main auroral emission. We also consider whether there is evidence that reconnection events occur preferentially during certain solar wind conditions or that the solar wind modulates the quasi-periodicity seen in the magnetic field dipolarizations and flow bursts.

  11. Cosmic rays, solar activity, magnetic coupling, and lightning incidence

    NASA Technical Reports Server (NTRS)

    Ely, J. T. A.

    1984-01-01

    A theoretical model is presented and described that unifies the complex influence of several factors on spatial and temporal variation of lightning incidence. These factors include the cosmic radiation, solar activity, and coupling between geomagnetic and interplanetary (solar wind) magnetic fields. Atmospheric electrical conductivity in the 10 km region was shown to be the crucial parameter altered by these factors. The theory reconciles several large scale studies of lightning incidence previously misinterpreted or considered contradictory. The model predicts additional strong effects on variations in lightning incidence, but only small effects on the morphology and rate of thunderstorm development.

  12. Solar-terrestrial influences on weather and climate; Proceedings of the Symposium, Ohio State University, Columbus, Ohio, August 24-28, 1978

    NASA Technical Reports Server (NTRS)

    Mccormac, B. M. (Editor); Seliga, T. A.

    1979-01-01

    The book contains most of the invited papers and contributions presented at the symposium/workshop on solar-terrestrial influences on weather and climate. Four main issues dominate the activities of the symposium: whether solar variability relationships to weather and climate is a fundamental scientific question to which answers may have important implications for long-term weather and climate prediction; the sun-weather relationships; other potential solar influences on weather including the 11-year sunspot cycle, the 27-day solar rotation, and special solar events such as flares and coronal holes; and the development of practical use of solar variability as a tool for weather and climatic forecasting, other than through empirical approaches. Attention is given to correlation topics; solar influences on global circulation and climate models; lower and upper atmospheric coupling, including electricity; planetary motions and other indirect factors; experimental approaches to sun-weather relationships; and the role of minor atmospheric constituents.

  13. Solar events and their influence on the interplanetary medium

    NASA Technical Reports Server (NTRS)

    Joselyn, Joann

    1987-01-01

    Aspects of a workshop on Solar events and their influence on the interplanetary medium, held in September 1986, are reviewed, the goal of which was to foster interactions among colleagues, leading to an improved understanding of the unified relationship between solar events and interplanetary disturbances. The workshop consisted of three working groups: (1) flares, eruptives, and other near-Sun activity; (2) coronal mass ejections; and (3) interplanetary events. Each group discussed topics distributed in advance. The flares-eruptives group members agreed that pre-event energy is stored in stressed/sheared magnetic fields, but could not agree that flares and other eruptive events (e.g., eruptive solar prominences) are aspects of the same physical phenomenon. In the coronal mass ejection group, general agreement was reached on the presence of prominences in CMEs, and that they have a significant three-dimensional structure. Some topics identified for further research were the aftermath of CMEs (streamer deflections, transient coronal holes, possible disconnections), identification of the leading edge of CMEs, and studies of the range and prevalence of CME mass sizes and energies.

  14. Influences of CO2 increase, solar cycle variation, and geomagnetic activity on airglow from 1960 to 2015

    NASA Astrophysics Data System (ADS)

    Huang, Tai-Yin

    2018-06-01

    Variations of airglow intensity, Volume Emission Rate (VER), and VER peak height induced by the CO2 increase, and by the F10.7 solar cycle variation and geomagnetic activity were investigated to quantitatively assess their influences on airglow. This study is an extension of a previous study by Huang (2016) covering a time period of 55 years from 1960 to 2015 and includes geomagnetic variability. Two airglow models, OHCD-90 and MACD-90, are used to simulate the induced variations of O(1S) greenline, O2(0,1) atmospheric band, and OH(8,3) airglow for this study. Overall, our results demonstrate that airglow intensity and the peak VER variations of the three airglow emissions are strongly correlated, and in phase, with the F10.7 solar cycle variation. In addition, there is a linear trend, be it increasing or decreasing, existing in the airglow intensities and VERs due to the CO2 increase. On other hand, airglow VER peak heights are strongly correlated, and out of phase, with the Ap index variation of geomagnetic activity. The CO2 increase acts to lower the VER peak heights of OH(8,3) airglow and O(1S) greenline by 0.2 km in 55 years and it has no effect on the VER peak height of O2(0,1) atmospheric band.

  15. Claim of solar influence is on thin ice: are 11-year cycle solar minima associated with severe winters in Europe?

    NASA Astrophysics Data System (ADS)

    van Oldenborgh, G. J.; de Laat, A. T. J.; Luterbacher, J.; Ingram, W. J.; Osborn, T. J.

    2013-06-01

    A recent paper in Geophysical Research Letters, ‘Solar influence on winter severity in central Europe’, by Sirocko et al (2012 Geophys. Res. Lett. 39 L16704) claims that ‘weak solar activity is empirically related to extremely cold winter conditions in Europe’ based on analyses of documentary evidence of freezing of the River Rhine in Germany and of the Reanalysis of the Twentieth Century (20C). However, our attempt to reproduce these findings failed. The documentary data appear to be selected subjectively and agree neither with instrumental observations nor with two other reconstructions based on documentary data. None of these datasets show significant connection between solar activity and winter severity in Europe beyond a common trend. The analysis of Sirocko et al of the 20C circulation and temperature is inconsistent with their time series analysis. A physically-motivated consistent methodology again fails to support the reported conclusions. We conclude that multiple lines of evidence contradict the findings of Sirocko et al.

  16. Statistical properties of solar Hα flare activity

    NASA Astrophysics Data System (ADS)

    Deng, Linhua; Zhang, Xiaojuan; An, Jianmei; Cai, Yunfang

    2017-12-01

    Magnetic field structures on the solar atmosphere are not symmetric distribution in the northern and southern hemispheres, which is an important aspect of quasi-cyclical evolution of magnetic activity indicators that are related to solar dynamo theories. Three standard analysis techniques are applied to analyze the hemispheric coupling (north-south asymmetry and phase asynchrony) of monthly averaged values of solar Hα flare activity over the past 49 years (from 1966 January to 2014 December). The prominent results are as follows: (1) from a global point of view, solar Hα flare activity on both hemispheres are strongly correlated with each other, but the northern hemisphere precedes the southern one with a phase shift of 7 months; (2) the long-range persistence indeed exists in solar Hα flare activity, but the dynamical complexities in the two hemispheres are not identical; (3) the prominent periodicities of Hα flare activity are 17 years full-disk activity cycle and 11 years Schwabe solar cycle, but the short- and mid-term periodicities cannot determined by monthly time series; (4) by comparing the non-parametric rescaling behavior on a point-by-point basis, the hemispheric asynchrony of solar Hα flare activity are estimated to be ranging from several months to tens of months with an average value of 8.7 months. The analysis results could promote our knowledge on the long-range persistence, the quasi-periodic variation, and the hemispheric asynchrony of solar Hα flare activity on both hemispheres, and possibly provide valuable information for the hemispheric interrelation of solar magnetic activity.

  17. How active was solar cycle 22?

    NASA Technical Reports Server (NTRS)

    Hoegy, W. R.; Pesnell, W. D.; Woods, T. N.; Rottman, G. J.

    1993-01-01

    Solar EUV observations from the Langmuir probe on Pioneer Venus Orbiter suggest that at EUV wavelengths solar cycle 22 was more active than solar cycle 21. The Langmuir probe, acting as a photodiode, measured the integrated solar EUV flux over a 13 1/2 year period from January 1979 to June 1992, the longest continuous solar EUV measurement. The Ipe EUV flux correlated very well with the SME measurement of L-alpha during the lifetime of SME and with the UARS SOLSTICE L-alpha from October 1991 to June 1992 when the Ipe measurement ceased. Starting with the peak of solar cycle 21, there was good general agreement of Ipe EUV with the 10.7 cm, Ca K, and He 10830 solar indices, until the onset of solar cycle 22. From 1989 to the start of 1992, the 10.7 cm flux exhibited a broad maximum consisting of two peaks of nearly equal magnitude, whereas Ipe EUV exhibited a strong increase during this time period making the second peak significantly higher than the first. The only solar index that exhibits the same increase in solar activity as Ipe EUV and L-alpha during the cycle 22 peak is the total magnetic flux. The case for high activity during this peak is also supported by the presence of very high solar flare intensity.

  18. Comparing the influence of sunspot activity and geomagnetic activity on winter surface climate

    NASA Astrophysics Data System (ADS)

    Maliniemi, Ville; Mursula, Kalevi; Roy, Indrani; Asikainen, Timo

    2017-04-01

    We compare here the effect of geomagnetic activity (using the aa index) and sunspot activity on surface climate using sea level pressure dataset from Hadley centre during northern winter. Previous studies using the multiple linear regression method have been limited to using sunspots as a solar activity predictor. Sunspots and total solar irradiance indicate a robust positive influence around the Aleutian Low. This is valid up to a lag of one year. However, geomagnetic activity yields a positive NAM pattern at high to polar latitudes and a positive signal around Azores High pressure region. Interestingly, while there is a positive signal around Azores High for a 2-year lag in sunspots, the strongest signal in this region is found for aa index at 1-year lag. There is also a weak but significant negative signature present around central Pacific for both sunspots and aa index. The combined influence of geomagnetic activity and Quasi Biannual Oscillation (QBO 30 hPa) produces a particularly strong response at mid to polar latitudes, much stronger than the combined influence of sunspots and QBO, which was mostly studied in previous studies so far. This signal is robust and insensitive to the selected time period during the last century. Our results provide a useful way for improving the prediction of winter weather at middle to high latitudes of the northern hemisphere.

  19. Dynamo theory prediction of solar activity

    NASA Technical Reports Server (NTRS)

    Schatten, Kenneth H.

    1988-01-01

    The dynamo theory technique to predict decadal time scale solar activity variations is introduced. The technique was developed following puzzling correlations involved with geomagnetic precursors of solar activity. Based upon this, a dynamo theory method was developed to predict solar activity. The method was used successfully in solar cycle 21 by Schatten, Scherrer, Svalgaard, and Wilcox, after testing with 8 prior solar cycles. Schatten and Sofia used the technique to predict an exceptionally large cycle, peaking early (in 1990) with a sunspot value near 170, likely the second largest on record. Sunspot numbers are increasing, suggesting that: (1) a large cycle is developing, and (2) that the cycle may even surpass the largest cycle (19). A Sporer Butterfly method shows that the cycle can now be expected to peak in the latter half of 1989, consistent with an amplitude comparable to the value predicted near the last solar minimum.

  20. Relationship of The Tropical Cyclogenesis With Solar and Magnetospheric Activities

    NASA Astrophysics Data System (ADS)

    Vishnevsky, O. V.; Pankov, V. M.; Erokhine, N. S.

    Formation of tropical cyclones is a badly studied period in their life cycle even though there are many papers dedicated to analysis of influence of different parameters upon cyclones occurrence frequency (see e.g., Gray W.M.). Present paper is dedicated to study of correlation of solar and magnetospheric activity with the appearance of tropical cyclones in north-west region of Pacific ocean. Study of correlation was performed by using both classical statistical methods (including maximum entropy method) and quite modern ones, for example multifractal analysis. Information about Wolf's numbers and cyclogenesis intensity in period of 1944-2000 was received from different Internet databases. It was shown that power spectra maximums of Wolf's numbers and appeared tropical cyclones ones corresponds to 11-year period; solar activity and cyclogenesis processes intensity are in antiphase; maximum of mutual correlation coefficient (~ 0.8) between Wolf's numbers and cyclogenesis intensity is in South-China sea. There is a relation of multifractal characteristics calculated for both time series with the mutual correlation function that is another indicator of correlation between tropical cyclogenesis and solar-magnetospheric activity. So, there is the correlation between solar-magnetospheric activity and tropical cyclone intensity in this region. Possible physical mechanisms of such correlation including anomalous precipitations charged particles from the Earth radiation belts and wind intensity amplification in the troposphere are discussed.

  1. Relationship of The Tropical Cyclogenesis With Solar and Magnetospheric Activities

    NASA Astrophysics Data System (ADS)

    Vishnevsky, O.; Pankov, V.; Erokhine, N.

    Formation of tropical cyclones is a badly studied period in their life cycle even though there are many papers dedicated to analysis of influence of different parameters upon cyclones occurrence frequency (see e.g., Gray W.M.). Present paper is dedicated to study of correlation of solar and magnetospheric activity with the appearance of tropi- cal cyclones in north-west region of Pacific ocean. Study of correlation was performed by using both classical statistical methods (including maximum entropy method) and quite modern ones, for example multifractal analysis. Information about Wolf's num- bers and cyclogenesis intensity in period of 1944-2000 was received from different Internet databases. It was shown that power spectra maximums of Wolf's numbers and appeared tropical cyclones ones corresponds to 11-year period; solar activity and cyclogenesis processes intensity are in antiphase; maximum of mutual correlation co- efficient ( 0.8) between Wolf's numbers and cyclogenesis intensity is in South-China sea. There is a relation of multifractal characteristics calculated for both time series with the mutual correlation function that is another indicator of correlation between tropical cyclogenesis and solar-magnetospheric activity. So, there is the correlation between solar-magnetospheric activity and tropical cyclone intensity in this region. Possible physical mechanisms of such correlation including anomalous precipitations charged particles from the Earth radiation belts and wind intensity amplification in the troposphere are discussed.

  2. Solar activity and myocardial infarction.

    PubMed

    Szczeklik, E; Mergentaler, J; Kotlarek-Haus, S; Kuliszkiewicz-Janus, M; Kucharczyk, J; Janus, W

    1983-01-01

    The correlation between the incidence of myocardial infarction, sudden cardiac death, the solar activity and geomagnetism in the period 1969-1976 was studied, basing on Wrocław hospitals material registered according to WHO standards; sudden death was assumed when a person died within 24 hours after the onset of the disease. The highest number of infarctions and sudden deaths was detected for 1975, which coincided with the lowest solar activity, and the lowest one for the years 1969-1970 coinciding with the highest solar activity. Such an inverse, statistically significant correlation was not found to exist between the studied biological phenomena and geomagnetism.

  3. The ancient Egyptian civilization: maximum and minimum in coincidence with solar activity

    NASA Astrophysics Data System (ADS)

    Shaltout, M.

    It is proved from the last 22 years observations of the total solar irradiance (TSI) from space by artificial satellites, that TSI shows negative correlation with the solar activity (sunspots, flares, and 10.7cm Radio emissions) from day to day, but shows positive correlations with the same activity from year to year (on the base of the annual average for each of them). Also, the solar constant, which estimated fromth ground stations for beam solar radiations observations during the 20 century indicate coincidence with the phases of the 11- year cycles. It is known from sunspot observations (250 years) , and from C14 analysis, that there are another long-term cycles for the solar activity larger than 11-year cycle. The variability of the total solar irradiance affecting on the climate, and the Nile flooding, where there is a periodicities in the Nile flooding similar to that of solar activity, from the analysis of about 1300 years of the Nile level observations atth Cairo. The secular variations of the Nile levels, regularly measured from the 7 toth 15 century A.D., clearly correlate with the solar variations, which suggests evidence for solar influence on the climatic changes in the East African tropics The civilization of the ancient Egyptian was highly correlated with the Nile flooding , where the river Nile was and still yet, the source of the life in the Valley and Delta inside high dry desert area. The study depends on long -time historical data for Carbon 14 (more than five thousands years), and chronical scanning for all the elements of the ancient Egyptian civilization starting from the firs t dynasty to the twenty six dynasty. The result shows coincidence between the ancient Egyptian civilization and solar activity. For example, the period of pyramids building, which is one of the Brilliant periods, is corresponding to maximum solar activity, where the periods of occupation of Egypt by Foreign Peoples corresponding to minimum solar activity. The decline

  4. Manifestations of Influence of Solar Activity and Cosmic Ray Intensity on the Wheat Price in the Medieval England (1259-1703 Years)

    NASA Astrophysics Data System (ADS)

    Pustil'Nik, Lev A.; Dorman, L. I.; Yom Din, G.

    2003-07-01

    The database of Professor Rogers, with wheat prices in England in the Middle Ages (1249-1703) was used to search for possible manifestations of solar activity and cosmic ray variations. The main object of the statistical analysis is investigation of bursts of prices. We present a conceptual model of possible modes for sensitivity of wheat prices to weather conditions, caused by solar cycle variations in cosmic rays, and compare the expected price fluctuations with wheat price variations recorded in the Medieval England. We compared statistical properties of the intervals between price bursts with statistical properties of the intervals between extremes (minimums) of solar cycles during the years 1700-2000. Statistical properties of these two samples are similar both in averaged/median values of intervals and in standard deviation of this values. We show that histogram of intervals distribution for price bursts and solar minimums are coincidence with high confidence level. We analyzed direct links between wheat prices and solar activity in the th 17 Century, for which wheat prices and solar activity data as well as cosmic ray intensity (from 10 Be isotop e) are available. We show that for all seven solar activity minimums the observed prices were higher than prices for the nine intervals of maximal solar activity proceed preceding to the minimums. This result, combined with the conclusion on similarity of statistical properties of the price bursts and solar activity extremes we consider as direct evidence of a causal connection between wheat prices bursts and solar activity.

  5. Observations of hysteresis in solar cycle variations among seven solar activity indicators

    NASA Technical Reports Server (NTRS)

    Bachmann, Kurt T.; White, Oran R.

    1994-01-01

    We show that smoothed time series of 7 indices of solar activity exhibit significant solar cycle dependent differences in their relative variations during the past 20 years. In some cases these observed hysteresis patterns start to repeat over more than one solar cycle, giving evidence that this is a normal feature of solar variability. Among the indices we study, we find that the hysteresis effects are approximately simple phase shifts, and we quantify these phase shifts in terms of lag times behind the leading index, the International Sunspot Number. Our measured lag times range from less than one month to greater than four months and can be much larger than lag times estimated from short-term variations of these same activity indices during the emergence and decay of major active regions. We argue that hysteresis represents a real delay in the onset and decline of solar activity and is an important clue in the search for physical processes responsible for changing solar emission at various wavelengths.

  6. Physics of solar activity

    NASA Technical Reports Server (NTRS)

    Sturrock, Peter A.

    1993-01-01

    The aim of the research activity was to increase our understanding of solar activity through data analysis, theoretical analysis, and computer modeling. Because the research subjects were diverse and many researchers were supported by this grant, a select few key areas of research are described in detail. Areas of research include: (1) energy storage and force-free magnetic field; (2) energy release and particle acceleration; (3) radiation by nonthermal electrons; (4) coronal loops; (5) flare classification; (6) longitude distributions of flares; (7) periodicities detected in the solar activity; (8) coronal heating and related problems; and (9) plasma processes.

  7. Trends of solar-geomagnetic activity, cosmic rays, atmosphere, and climate changes

    NASA Astrophysics Data System (ADS)

    Voronin, N.; Avakyan, S.

    2009-04-01

    The results are presented of the analysis of trends in the solar-geomagnetic activity and intensity of galactic cosmic rays (GCR) for the several eleven-year solar cycles. The indication has been revealed of the change of signs in the long-term changes in geomagnetic activity (aa-index) and the GCR in recent years. These changes correspond to the changes of sings in long-term trends in some of atmospheric parameters (transparency, albedo, cloudness, the content of water vapour, methane, ozone, the erythemal radiation flux). These global changes in atmosphere is most important problem of the up-to-date science. The global warming observed during the several past decades presents a real danger for the mankind. Till present the predominant point of view has been that the main cause of the increase of mean surface air temperature is the increase of concentrations of the anthropogenic gases first of all carbon dioxide CO2 and methane CH_4. Indeed, from the beginning of nineteen century the concentration of CO2 in the atmosphere has been growing and now it exceeds the initial level by the factor of 1.4 and the speed of this increase being growing too. This was the reason of international efforts to accept the Kyoto Protocol which limited the ejections of greenhouse gases. However there are premises which show that the influence of solar variability on the climate should be taken into account in the first place. The obtained results are analyzed from the point of view of well known effects of GCR influence on weather and climate with taken into account also a novel trigger mechanism in solar-terrestrial relations what allows revaluation of the role of solar flares and geomagnetic storms. The mechanism explains how agents of solar and geomagnetic activities affect atmospheric processes. This first agent under consideration is variation of fluxes of solar EUV and X-ray radiation. The second agent is fluxes of electrons and protons which precipitate from radiation belts as a

  8. Using the Solar Polar Magnetic Field for Longterm Predictions of Solar Activity, Solar Cycles 21-25

    NASA Astrophysics Data System (ADS)

    Pesnell, W. D.; Schatten, K. H.

    2017-12-01

    We briefly review the dynamo and geomagnetic precursor methods of long-term solar activity forecasting. These methods depend upon the most basic aspect of dynamo theory to predict future activity, future magnetic field arises directly from the amplification of pre-existing magnetic field. We then generalize the dynamo technique, allowing the method to be used at any phase of the solar cycle, to the Solar Dynamo Amplitude (SODA) index. This index is sensitive to the magnetic flux trapped within the Sun's convection zone but insensitive to the phase of the solar cycle. Since magnetic fields inside the Sun can become buoyant, one may think of the acronym SODA as describing the amount of buoyant flux. We will show how effective the SODA Index has been in predicting Solar Cycles 23 and 24, and present a unified picture of earlier estimates of the polar magnetic configuration in Solar Cycle 21 and 22. Using the present value of the SODA index, we estimate that the next cycle's smoothed peak activity will be about 125 ± 30 solar flux units for the 10.7 cm radio flux and a sunspot number of 70 ± 25. This suggests that Solar Cycle 25 will be comparable to Solar Cycle 24. Since the current approach uses data prior to solar minimum, these estimates may improve when the upcoming solar minimum is reached.

  9. Solar activity and oscillation frequency splittings

    NASA Technical Reports Server (NTRS)

    Woodard, M. F.; Libbrecht, K. G.

    1993-01-01

    Solar p-mode frequency splittings, parameterized by the coefficients through order N = 12 of a Legendre polynomial expansion of the mode frequencies as a function of m/L, were obtained from an analysis of helioseismology data taken at Big Bear Solar Observatory during the 4 years 1986 and 1988-1990 (approximately solar minimum to maximum). Inversion of the even-index splitting coefficients confirms that there is a significant contribution to the frequency splittings originating near the solar poles. The strength of the polar contribution is anti correlated with the overall level or solar activity in the active latitudes, suggesting a relation to polar faculae. From an analysis of the odd-index splitting coefficients we infer an uppor limit to changes in the solar equatorial near-surface rotatinal velocity of less than 1.9 m/s (3 sigma limit) between solar minimum and maximum.

  10. Are Solar Activity Variations Amplified by the QBO: A Modeling Study

    NASA Technical Reports Server (NTRS)

    Mengel, J. G.; Mayr, H. G.; Drob, D. P.; Porter, H. S.; Bhartia, P. K. (Technical Monitor)

    2002-01-01

    Solar cycle activity effects (SCAE) in the lower and middle atmosphere, reported in several studies, are difficult to explain on the basis of the small changes in solar radiation that accompany the 11-year cycle. It is therefore natural to speculate that dynamical processes may come into play to produce a leverage. Such a leverage may be provided by the Quasi-Biennial Oscillation (QBO) in the zonal circulation of the stratosphere, which has been linked to solar activity variations. Driven primarily by wave mean flow interaction, the QBO period and its amplitude are variable but are also strongly influenced by the seasonal cycle in the solar radiation. This influence extends to low altitudes and is referred to as 'downward control'. Small changes in the solar radiative forcing may produce small changes in the period and phase of the QBO, but these in turn may produce measurable differences in the wind field. Thus, the QBO may be an amplifier of solar activity variations and a natural conduit of these variations to lower altitudes. To test this hypothesis, we conducted experiments with a 2D version of our Numerical Spectral Model that incorporates Hines' Doppler Spread Parameterization for small-scale gravity waves (GW). Solar cycle radiance variations (SCRV) are accounted for by changing the radiative heating rate on a logarithmic scale from 0.1% at the surface to 1% at 50 km to 10% at 100 km. With and without SCRV, but with the same GW flux, we then conduct numerical experiments to evaluate the magnitude of the SCAE in the zonal circulation. The numerical results indicate that, under certain conditions, the SCAE is significant and can extend to lower altitudes where the SCRV is small. For a modeled QBO period of 30 months, we find that the seasonal cycle in the solar forcing acts as a strong pacemaker to lock up the phase and period of the QBO. The SCAE then shows up primarily as a distinct but relatively weak amplitude modulation. But with a different QBO period

  11. A Time-Frequency Analysis of the Effects of Solar Activities on Tropospheric Thermodynamics

    NASA Technical Reports Server (NTRS)

    Kiang, Richard K.; Kyle, H. Lee; Wharton, Stephen W. (Technical Monitor)

    2001-01-01

    Whether the Sun has significantly influenced the climate during the last century has been under extensive debates for almost two decades. Since the solar irradiance varies very little in a solar cycle, it is puzzling that some geophysical parameters show proportionally large variations which appear to be responding to the solar cycles. For example, variation in low altitude clouds is shown correlated with solar cycle, and the onset of Forbush decrease is shown correlated with the reduction of the vorticity area index. A possible sun-climate connection is that galactic cosmic rays modulated by solar activities influence cloud formation. In this paper, we apply wavelet transform to satellite and surface data to examine this hypothesis. Data analyzed include the time series for solar irradiance, sunspots, UV index, temperature, cloud coverage, and neutron counter measurements. The interactions among the elements in the Earth System under the external and internal forcings give out very complex signals.The periodicity of the forcings or signals could range widely. Since wavelet transforms can analyze multi-scale phenomena that are both localized in frequency and time, it is a very useful technique for detecting, understanding and monitoring climate changes.

  12. Solar Activity Heading for a Maunder Minimum?

    NASA Astrophysics Data System (ADS)

    Schatten, K. H.; Tobiska, W. K.

    2003-05-01

    Long-range (few years to decades) solar activity prediction techniques vary greatly in their methods. They range from examining planetary orbits, to spectral analyses (e.g. Fourier, wavelet and spectral analyses), to artificial intelligence methods, to simply using general statistical techniques. Rather than concentrate on statistical/mathematical/numerical methods, we discuss a class of methods which appears to have a "physical basis." Not only does it have a physical basis, but this basis is rooted in both "basic" physics (dynamo theory), but also solar physics (Babcock dynamo theory). The class we discuss is referred to as "precursor methods," originally developed by Ohl, Brown and Williams and others, using geomagnetic observations. My colleagues and I have developed some understanding for how these methods work and have expanded the prediction methods using "solar dynamo precursor" methods, notably a "SODA" index (SOlar Dynamo Amplitude). These methods are now based upon an understanding of the Sun's dynamo processes- to explain a connection between how the Sun's fields are generated and how the Sun broadcasts its future activity levels to Earth. This has led to better monitoring of the Sun's dynamo fields and is leading to more accurate prediction techniques. Related to the Sun's polar and toroidal magnetic fields, we explain how these methods work, past predictions, the current cycle, and predictions of future of solar activity levels for the next few solar cycles. The surprising result of these long-range predictions is a rapid decline in solar activity, starting with cycle #24. If this trend continues, we may see the Sun heading towards a "Maunder" type of solar activity minimum - an extensive period of reduced levels of solar activity. For the solar physicists, who enjoy studying solar activity, we hope this isn't so, but for NASA, which must place and maintain satellites in low earth orbit (LEO), it may help with reboost problems. Space debris, and other

  13. Long-Range Solar Activity Predictions: A Reprieve from Cycle #24's Activity

    NASA Technical Reports Server (NTRS)

    Richon, K.; Schatten, K.

    2003-01-01

    We discuss the field of long-range solar activity predictions and provide an outlook into future solar activity. Orbital predictions for satellites in Low Earth Orbit (LEO) depend strongly on exospheric densities. Solar activity forecasting is important in this regard, as the solar ultra-violet (UV) and extreme ultraviolet (EUV) radiations inflate the upper atmospheric layers of the Earth, forming the exosphere in which satellites orbit. Rather than concentrate on statistical, or numerical methods, we utilize a class of techniques (precursor methods) which is founded in physical theory. The geomagnetic precursor method was originally developed by the Russian geophysicist, Ohl, using geomagnetic observations to predict future solar activity. It was later extended to solar observations, and placed within the context of physical theory, namely the workings of the Sun s Babcock dynamo. We later expanded the prediction methods with a SOlar Dynamo Amplitude (SODA) index. The SODA index is a measure of the buried solar magnetic flux, using toroidal and poloidal field components. It allows one to predict future solar activity during any phase of the solar cycle, whereas previously, one was restricted to making predictions only at solar minimum. We are encouraged that solar cycle #23's behavior fell closely along our predicted curve, peaking near 192, comparable to the Schatten, Myers and Sofia (1996) forecast of 182+/-30. Cycle #23 extends from 1996 through approximately 2006 or 2007, with cycle #24 starting thereafter. We discuss the current forecast of solar cycle #24, (2006-2016), with a predicted smoothed F10.7 radio flux of 142+/-28 (1-sigma errors). This, we believe, represents a reprieve, in terms of reduced fuel costs, etc., for new satellites to be launched or old satellites (requiring reboosting) which have been placed in LEO. By monitoring the Sun s most deeply rooted magnetic fields; long-range solar activity can be predicted. Although a degree of uncertainty

  14. Models of the quiet and active solar atmosphere from Harvard OSO data.

    NASA Technical Reports Server (NTRS)

    Noyes, R. W.

    1971-01-01

    Review of some Harvard Observatory programs aimed at defining the physical conditions in quiet and active solar regions on the basis of data obtained from the OSO-IV and OSO-VI spacecraft. The spectral range covered is from 300 A to 1400 A. This spectral range consists of emission lines and continua from abundant elements such as hydrogen, helium, carbon, nitrogen, oxygen, silicon, magnesium, aluminum, neon, iron, and calcium in various ionization states ranging from neutral to 15 times ionized. The structure is discussed of the quiet solar atmosphere as deduced from center-to-limb behavior of spectral lines and continua formed in the chromosphere and corona. In reviewing investigations of solar active regions, it is shown that the structure of these regions varies in a complicated manner from point to point. The local structure is influenced by factors such as the magnetic field configuration within the active region and the age or evolutionary state of the region.

  15. Global solar magetic field organization in the extended corona: influence on the solar wind speed and density over the cycle.

    NASA Astrophysics Data System (ADS)

    Réville, V.; Velli, M.; Brun, S.

    2017-12-01

    The dynamics of the solar wind depends intrinsically on the structure of the global solar magnetic field, which undergoes fundamental changes over the 11yr solar cycle. For instance, the wind terminal velocity is thought to be anti-correlated with the expansion factor, a measure of how the magnetic field varies with height in the solar corona, usually computed at a fixed height (≈ 2.5 Rȯ, the source surface radius which approximates the distance at which all magnetic field lines become open). However, the magnetic field expansion affects the solar wind in a more detailed way, its influence on the solar wind properties remaining significant well beyond the source surface: we demonstrate this using 3D global MHD simulations of the solar corona, constrained by surface magnetograms over half a solar cycle (1989-2001). For models to comply with the constraints provided by observed characteristics of the solar wind, namely, that the radial magnetic field intensity becomes latitude independent at some distance from the Sun (Ulysses observations beyond 1 AU), and that the terminal wind speed is anti-correlated with the mass flux, they must accurately describe expansion beyond the solar wind critical point (even up to 10Rȯ and higher in our model). We also show that near activity minimum, expansion in the higher corona beyond 2.5 Rȯ is actually the dominant process affecting the wind speed. We discuss the consequences of this result on the necessary acceleration profile of the solar wind, the location of the sonic point and of the energy deposition by Alfvén waves.

  16. Activity Analyses for Solar-type Stars Observed with Kepler. II. Magnetic Feature versus Flare Activity

    NASA Astrophysics Data System (ADS)

    He, Han; Wang, Huaning; Zhang, Mei; Mehrabi, Ahmad; Yan, Yan; Yun, Duo

    2018-05-01

    The light curves of solar-type stars present both periodic fluctuation and flare spikes. The gradual periodic fluctuation is interpreted as the rotational modulation of magnetic features on the stellar surface and is used to deduce magnetic feature activity properties. The flare spikes in light curves are used to derive flare activity properties. In this paper, we analyze the light curve data of three solar-type stars (KIC 6034120, KIC 3118883, and KIC 10528093) observed with Kepler space telescope and investigate the relationship between their magnetic feature activities and flare activities. The analysis shows that: (1) both the magnetic feature activity and the flare activity exhibit long-term variations as the Sun does; (2) unlike the Sun, the long-term variations of magnetic feature activity and flare activity are not in phase with each other; (3) the analysis of star KIC 6034120 suggests that the long-term variations of magnetic feature activity and flare activity have a similar cycle length. Our analysis and results indicate that the magnetic features that dominate rotational modulation and the flares possibly have different source regions, although they may be influenced by the magnetic field generated through a same dynamo process.

  17. Construction of a century solar chromosphere data set for solar activity related research

    NASA Astrophysics Data System (ADS)

    Lin, Ganghua; Wang, Xiao Fan; Yang, Xiao; Liu, Suo; Zhang, Mei; Wang, Haimin; Liu, Chang; Xu, Yan; Tlatov, Andrey; Demidov, Mihail; Borovik, Aleksandr; Golovko, Aleksey

    2017-06-01

    This article introduces our ongoing project "Construction of a Century Solar Chromosphere Data Set for Solar Activity Related Research". Solar activities are the major sources of space weather that affects human lives. Some of the serious space weather consequences, for instance, include interruption of space communication and navigation, compromising the safety of astronauts and satellites, and damaging power grids. Therefore, the solar activity research has both scientific and social impacts. The major database is built up from digitized and standardized film data obtained by several observatories around the world and covers a time span of more than 100 years. After careful calibration, we will develop feature extraction and data mining tools and provide them together with the comprehensive database for the astronomical community. Our final goal is to address several physical issues: filament behavior in solar cycles, abnormal behavior of solar cycle 24, large-scale solar eruptions, and sympathetic remote brightenings. Significant signs of progress are expected in data mining algorithms and software development, which will benefit the scientific analysis and eventually advance our understanding of solar cycles.

  18. Solar active region display system

    NASA Astrophysics Data System (ADS)

    Golightly, M.; Raben, V.; Weyland, M.

    2003-04-01

    The Solar Active Region Display System (SARDS) is a client-server application that automatically collects a wide range of solar data and displays it in a format easy for users to assimilate and interpret. Users can rapidly identify active regions of interest or concern from color-coded indicators that visually summarize each region's size, magnetic configuration, recent growth history, and recent flare and CME production. The active region information can be overlaid onto solar maps, multiple solar images, and solar difference images in orthographic, Mercator or cylindrical equidistant projections. Near real-time graphs display the GOES soft and hard x-ray flux, flare events, and daily F10.7 value as a function of time; color-coded indicators show current trends in soft x-ray flux, flare temperature, daily F10.7 flux, and x-ray flare occurrence. Through a separate window up to 4 real-time or static graphs can simultaneously display values of KP, AP, daily F10.7 flux, GOES soft and hard x-ray flux, GOES >10 and >100 MeV proton flux, and Thule neutron monitor count rate. Climatologic displays use color-valued cells to show F10.7 and AP values as a function of Carrington/Bartel's rotation sequences - this format allows users to detect recurrent patterns in solar and geomagnetic activity as well as variations in activity levels over multiple solar cycles. Users can customize many of the display and graph features; all displays can be printed or copied to the system's clipboard for "pasting" into other applications. The system obtains and stores space weather data and images from sources such as the NOAA Space Environment Center, NOAA National Geophysical Data Center, the joint ESA/NASA SOHO spacecraft, and the Kitt Peak National Solar Observatory, and can be extended to include other data series and image sources. Data and images retrieved from the system's database are converted to XML and transported from a central server using HTTP and SOAP protocols, allowing

  19. The possible effects of the solar and geomagnetic activity on multiple sclerosis.

    PubMed

    Papathanasopoulos, Panagiotis; Preka-Papadema, Panagiota; Gkotsinas, Anastasios; Dimisianos, Nikolaos; Hillaris, Alexandros; Katsavrias, Christos; Antonakopoulos, Gregorios; Moussas, Xenophon; Andreadou, Elisabeth; Georgiou, Vasileios; Papachristou, Pinelopi; Kargiotis, Odysseas

    2016-07-01

    Increasing observational evidence on the biological effects of Space Weather suggests that geomagnetic disturbances may be an environmental risk factor for multiple sclerosis (MS) relapses. In the present study, we aim to investigate the possible effect of geomagnetic disturbances on MS activity. MS patient admittance rates were correlated with the solar and geophysical data covering an eleven-year period (1996-2006, 23rd solar cycle). We also examined the relationship of patterns of the solar flares, the coronal mass ejections (CMEs) and the solar wind with the recorded MS admission numbers. The rate of MS patient admittance due to acute relapses was found to be associated with the solar and geomagnetic events. There was a "primary" peak in MS admittance rates shortly after intense geomagnetic storms followed by a "secondary" peak 7-8 months later. We conclude that the geomagnetic and solar activity may represent an environmental health risk factor for multiple sclerosis and we discuss the possible mechanisms underlying this association. More data from larger case series are needed to confirm these preliminary results and to explore the possible influence of Space Weather on the biological and radiological markers of the disease. Copyright © 2016 Elsevier B.V. All rights reserved.

  20. Propagation of Stationary Planetary Waves in the Upper Atmosphere under Different Solar Activity

    NASA Astrophysics Data System (ADS)

    Koval, A. V.; Gavrilov, N. M.; Pogoreltsev, A. I.; Shevchuk, N. O.

    2018-03-01

    Numerical modeling of changes in the zonal circulation and amplitudes of stationary planetary waves are performed with an accounting for the impact of solar activity variations on the thermosphere. A thermospheric version of the Middle/Upper Atmosphere Model (MUAM) is used to calculate the circulation in the middle and upper atmosphere at altitudes up to 300 km from the Earth's surface. Different values of the solar radio emission flux in the thermosphere are specified at a wavelength of 10.7 cm to take into account the solar activity variations. The ionospheric conductivities and their variations in latitude, longitude, and time are taken into account. The calculations are done for the January-February period and the conditions of low, medium, and high solar activity. It was shown that, during high-activity periods, the zonal wind velocities increases at altitudes exceeding 150 km and decreases in the lower layers. The amplitudes of planetary waves at high solar activity with respect to the altitude above 120 km or below 100 km, respectively, are smaller or larger than those at low activity. These differences correspond to the calculated changes in the refractive index of the atmosphere for stationary planetary waves and the Eliassen-Palm flux. Changes in the conditions for the propagation and reflection of stationary planetary waves in the thermosphere may influence the variations in their amplitudes and the atmospheric circulation, including the lower altitudes of the middle atmosphere.

  1. Ancient cellular structures and modern humans: change of survival strategies before prolonged low solar activity period

    NASA Astrophysics Data System (ADS)

    Ragulskaya, Mariya; Rudenchik, Evgeniy; Gromozova, Elena; Voychuk, Sergei; Kachur, Tatiana

    The study of biotropic effects of modern space weather carries the information about the rhythms and features of adaptation of early biological systems to the outer space influence. The influence of cosmic rays, ultraviolet waves and geomagnetic field on early life has its signs in modern biosphere processes. These phenomena could be experimentally studied on present-day biological objects. Particularly inorganic polyphosphates, so-called "fossil molecules", attracts special attention as the most ancient molecules which arose in inanimate nature and have been accompanying biological objects at all stages of evolution. Polyphosphates-containing graves of yeast's cells of Saccharomyces cerevisiae strain Y-517, , from the Ukrainian Collection of Microorganisms was studied by daily measurements during 2000-2013 years. The IZMIRAN daily data base of physiological parameters dynamics during 2000-2013 years were analyzed simultaneously (25 people). The analysis showed significant simultaneous changes of the statistical parameters of the studied biological systems in 2004 -2006. The similarity of simultaneous changes of adaptation strategies of human organism and the cell structures of Saccharomyces cerevisiae during the 23-24 cycles of solar activity are discussed. This phenomenon could be due to a replacement of bio-effective parameters of space weather during the change from 23rd to 24th solar activity cycle and nonstandard geophysical peculiarities of the 24th solar activity cycle. It could be suggested that the observed similarity arose as the optimization of evolution selection of the living systems in expectation of probable prolonged period of low solar activity (4-6 cycles of solar activity).

  2. Solar Radius at Subterahertz Frequencies and Its Relation to Solar Activity

    NASA Astrophysics Data System (ADS)

    Menezes, Fabian; Valio, Adriana

    2017-12-01

    The Sun emits radiation at several wavelengths of the electromagnetic spectrum. In the optical band, the solar radius is 695 700 km, and this defines the photosphere, which is the visible surface of the Sun. However, as the altitude increases, the electromagnetic radiation is produced at other frequencies, causing the solar radius to change as a function of wavelength. These measurements enable a better understanding of the solar atmosphere, and the radius dependence on the solar cycle is a good indicator of the changes that occur in the atmospheric structure. We measure the solar radius at the subterahertz frequencies of 0.212 and 0.405 THz, which is the altitude at which these emissions are primarily generated, and also analyze the radius variation over the 11-year solar activity cycle. For this, we used radio maps of the solar disk for the period between 1999 and 2017, reconstructed from daily scans made by the Solar Submillimeter-wave Telescope (SST), installed at El Leoncito Astronomical Complex (CASLEO) in the Argentinean Andes. Our measurements yield radii of 966.5'' ±2.8'' for 0.2 THz and 966.5'' ±2.7'' for 0.4 THz. This implies a height of 5.0 ±2.0 ×106 m above the photosphere. Furthermore, we also observed a strong anticorrelation between the radius variation and the solar activity at both frequencies.

  3. Solar Activity Forecasting for use in Orbit Prediction

    NASA Technical Reports Server (NTRS)

    Schatten, Kenneth

    2001-01-01

    Orbital prediction for satellites in low Earth orbit (LEO) or low planetary orbit depends strongly on exospheric densities. Solar activity forecasting is important in orbital prediction, as the solar UV and EUV inflate the upper atmospheric layers of the Earth and planets, forming the exosphere in which satellites orbit. Geomagnetic effects also relate to solar activity. Because of the complex and ephemeral nature of solar activity, with different cycles varying in strength by more than 100%, many different forecasting techniques have been utilized. The methods range from purely numerical techniques (essentially curve fitting) to numerous oddball schemes, as well as a small subset, called 'Precursor techniques.' The situation can be puzzling, owing to the numerous methodologies involved, somewhat akin to the numerous ether theories near the turn of the last century. Nevertheless, the Precursor techniques alone have a physical basis, namely dynamo theory, which provides a physical explanation for why this subset seems to work. I discuss this solar cycle's predictions, as well as the Sun's observed activity. I also discuss the SODA (Solar Dynamo Amplitude) index, which provides the user with the ability to track the Sun's hidden, interior dynamo magnetic fields. As a result, one may then update solar activity predictions continuously, by monitoring the solar magnetic fields as they change throughout the solar cycle. This paper ends by providing a glimpse into what the next solar cycle (#24) portends.

  4. Solar proton fluxes since 1956. [sunspot activity correlation

    NASA Technical Reports Server (NTRS)

    Reedy, R. C.

    1977-01-01

    The fluxes of protons emitted during solar flares since 1956 were evaluated. The depth-versus-activity profiles of Co-56 in several lunar rocks are consistent with the solar proton fluxes detected by experiments on several satellites. Only about 20% of the solar-proton-induced activities of Na-22 and Fe-55 in lunar rocks from early Apollo missions were produced by protons emitted from the sun during solar cycle 20 (1965-1975). The depth-versus-activity data for these radionuclides in several lunar rocks were used to determine the fluxes of protons during solar cycle 19 (1954-1964). The average proton fluxes for cycle 19 are about five times those for both the last million years and for cycle 20 and are about five times the previous estimate for cycle 19 based on neutron-monitor and radio ionospheric measurements. These solar-proton flux variations correlate with changes in sunspot activity.

  5. How calibration and reference spectra affect the accuracy of absolute soft X-ray solar irradiance measured by the SDO/EVE/ESP during high solar activity

    NASA Astrophysics Data System (ADS)

    Didkovsky, Leonid; Wieman, Seth; Woods, Thomas

    2016-10-01

    The Extreme ultraviolet Spectrophotometer (ESP), one of the channels of SDO's Extreme ultraviolet Variability Experiment (EVE), measures solar irradiance in several EUV and soft x-ray (SXR) bands isolated using thin-film filters and a transmission diffraction grating, and includes a quad-diode detector positioned at the grating zeroth-order to observe in a wavelength band from about 0.1 to 7.0 nm. The quad diode signal also includes some contribution from shorter wavelength in the grating's first-order and the ratio of zeroth-order to first-order signal depends on both source geometry, and spectral distribution. For example, radiometric calibration of the ESP zeroth-order at the NIST SURF BL-2 with a near-parallel beam provides a different zeroth-to-first-order ratio than modeled for solar observations. The relative influence of "uncalibrated" first-order irradiance during solar observations is a function of the solar spectral irradiance and the locations of large Active Regions or solar flares. We discuss how the "uncalibrated" first-order "solar" component and the use of variable solar reference spectra affect determination of absolute SXR irradiance which currently may be significantly overestimated during high solar activity.

  6. Correlation of Doppler noise during solar conjunctions with fluctuations in solar activity

    NASA Technical Reports Server (NTRS)

    Berman, A. L.; Rockwell, S. T.

    1975-01-01

    Deviations betweeb observed Doppler noise and the noise model during solar conjunction were analyzed. It is tentatively concluded that these deviations are due to short-term fluctuations in solar activity as seen along the signal path, and not to solar/antenna structure effects or system noise temperature.

  7. Influence of Diffused Solar Radiation on the Solar Concentrating System of a Plant Shoot Configuration

    NASA Astrophysics Data System (ADS)

    Obara, Shin'ya

    Investigation of a plant shoot configuration is used to obtain valuable information concerning the received light system. Additionally, analysis results concerning a plant shoot configuration interaction with direct solar radiation were taken from a past study. However, in order to consider a plant shoot as a received sunlight system, it is necessary to understand the received light characteristics of both direct solar radiation and diffused solar radiation. Under a clear sky, the ratio of direct solar radiation to diffused solar radiation is large. However, under a clouded sky, the amount of diffused solar radiation becomes larger. Therefore, in this paper, we investigate the received light characteristics of a plant shoot configuration under the influence of diffused solar radiation. As a result, we clarify the relationship between the amount of diffused solar radiation and the amount of received light as a function of the characteristics of the plant shoot configuration. In order to obtain diffused solar radiation, it is necessary to correspond to the radiation of the multi-directions. In the analysis, the characteristic of the difference in arrangement of the top leaf and the other leaf was obtained. Therefore, in analysis, leaves other than the top were distributed in the wide range.

  8. Geomagnetic responses to the solar wind and the solar activity

    NASA Technical Reports Server (NTRS)

    Svalgaard, L.

    1975-01-01

    Following some historical notes, the formation of the magnetosphere and the magnetospheric tail is discussed. The importance of electric fields is stressed and the magnetospheric convection of plasma and magnetic field lines under the influence of large-scale magnetospheric electric fields is outlined. Ionospheric electric fields and currents are intimately related to electric fields and currents in the magnetosphere and the strong coupling between the two regions is discussed. The energy input of the solar wind to the magnetosphere and upper atmosphere is discussed in terms of the reconnection model where interplanetary magnetic field lines merge or connect with the terrestrial field on the sunward side of the magnetosphere. The merged field lines are then stretched behind earth to form the magnetotail so that kinetic energy from the solar wind is converted into magnetic energy in the field lines in the tail. Localized collapses of the crosstail current, which is driven by the large-scale dawn/dusk electric field in the magnetosphere, divert part of this current along geomagnetic field lines to the ionosphere, causing substorms with auroral activity and magnetic disturbances. The collapses also inject plasma into the radiation belts and build up a ring current. Frequent collapses in rapid succession constitute the geomagnetic storm.

  9. DASL-Data and Activities for Solar Learning

    NASA Technical Reports Server (NTRS)

    Jones, Harrison P.; Henney, Carl; Hill, Frank; Gearen, Michael; Pompca, Stephen; Stagg, Travis; Stefaniak, Linda; Walker, Connie

    2004-01-01

    DASL-Data and Activities for Solar Learning Data and Activities for Solar Learning (DASL) provides a classroom learning environment based on a twenty-five year record of solar magnetograms from the National Solar Observatory (NSO) at Kitt Peak, AZ. The data, together with image processing software for Macs or PCs, can be used to learn basic facts about the Sun and astronomy at the middle school level. At the high school level, students can study properties of the Sun's magnetic cycle with classroom exercises emphasizing data and error analysis and can participate in a new scientific study, Research in Active Solar Longitudes (RASL), in collaboration with classrooms throughout the country and scientists at NSO and NASA. We present a half-day course to train teachers in the scientific content of the project and its classroom use. We will provide a compact disc with the data and software and will demonstrate software installation and use, classroom exercises, and participation in RASL with computer projection.

  10. Solar-terrestrial predictions proceedings. Volume 4: Prediction of terrestrial effects of solar activity

    NASA Technical Reports Server (NTRS)

    Donnelly, R. E. (Editor)

    1980-01-01

    Papers about prediction of ionospheric and radio propagation conditions based primarily on empirical or statistical relations is discussed. Predictions of sporadic E, spread F, and scintillations generally involve statistical or empirical predictions. The correlation between solar-activity and terrestrial seismic activity and the possible relation between solar activity and biological effects is discussed.

  11. 9,400 years of cosmic radiation and solar activity from ice cores and tree rings

    PubMed Central

    Steinhilber, Friedhelm; Beer, Jürg; Brunner, Irene; Christl, Marcus; Fischer, Hubertus; Heikkilä, Ulla; Kubik, Peter W.; Mann, Mathias; McCracken, Ken G.; Miller, Heinrich; Miyahara, Hiroko; Oerter, Hans

    2012-01-01

    Understanding the temporal variation of cosmic radiation and solar activity during the Holocene is essential for studies of the solar-terrestrial relationship. Cosmic-ray produced radionuclides, such as 10Be and 14C which are stored in polar ice cores and tree rings, offer the unique opportunity to reconstruct the history of cosmic radiation and solar activity over many millennia. Although records from different archives basically agree, they also show some deviations during certain periods. So far most reconstructions were based on only one single radionuclide record, which makes detection and correction of these deviations impossible. Here we combine different 10Be ice core records from Greenland and Antarctica with the global 14C tree ring record using principal component analysis. This approach is only possible due to a new high-resolution 10Be record from Dronning Maud Land obtained within the European Project for Ice Coring in Antarctica in Antarctica. The new cosmic radiation record enables us to derive total solar irradiance, which is then used as a proxy of solar activity to identify the solar imprint in an Asian climate record. Though generally the agreement between solar forcing and Asian climate is good, there are also periods without any coherence, pointing to other forcings like volcanoes and greenhouse gases and their corresponding feedbacks. The newly derived records have the potential to improve our understanding of the solar dynamics and to quantify the solar influence on climate. PMID:22474348

  12. 9,400 years of cosmic radiation and solar activity from ice cores and tree rings.

    PubMed

    Steinhilber, Friedhelm; Abreu, Jose A; Beer, Jürg; Brunner, Irene; Christl, Marcus; Fischer, Hubertus; Heikkilä, Ulla; Kubik, Peter W; Mann, Mathias; McCracken, Ken G; Miller, Heinrich; Miyahara, Hiroko; Oerter, Hans; Wilhelms, Frank

    2012-04-17

    Understanding the temporal variation of cosmic radiation and solar activity during the Holocene is essential for studies of the solar-terrestrial relationship. Cosmic-ray produced radionuclides, such as (10)Be and (14)C which are stored in polar ice cores and tree rings, offer the unique opportunity to reconstruct the history of cosmic radiation and solar activity over many millennia. Although records from different archives basically agree, they also show some deviations during certain periods. So far most reconstructions were based on only one single radionuclide record, which makes detection and correction of these deviations impossible. Here we combine different (10)Be ice core records from Greenland and Antarctica with the global (14)C tree ring record using principal component analysis. This approach is only possible due to a new high-resolution (10)Be record from Dronning Maud Land obtained within the European Project for Ice Coring in Antarctica in Antarctica. The new cosmic radiation record enables us to derive total solar irradiance, which is then used as a proxy of solar activity to identify the solar imprint in an Asian climate record. Though generally the agreement between solar forcing and Asian climate is good, there are also periods without any coherence, pointing to other forcings like volcanoes and greenhouse gases and their corresponding feedbacks. The newly derived records have the potential to improve our understanding of the solar dynamics and to quantify the solar influence on climate.

  13. Solar activity during the deep minimum of 2009

    NASA Astrophysics Data System (ADS)

    Sylwester, Janusz; Siarkowski, Marek; Gburek, Szymon; Gryciuk, Magdalena; Kepa, Anna; Kowaliński, Mirosław; Mrozek, Tomek; Phillips, Kenneth J. H.; Podgórski, Piotr; Sylwester, Barbara

    2014-12-01

    We discuss the character of the unusually deep solar activity minimum of 2009 between Solar Cycles 23 and 24. Levels of solar activity in various parts of the solar atmosphere -- photosphere, chromosphere, transition region, and corona -- were observed to be at their lowest for a century. The soft X-ray emission from the corona (hot outer part of the Sun's atmosphere) was measured throughout most of 2009 with the Polish-built SphinX spectrophotometer. Unlike other X-ray monitoring spacecraft, this sensitive spacecraft-borne instrument was able to continue measurements throughout this extended period of low activity.

  14. Seasonal variations of the atmospheric temperature response in mesosphere and lower thermosphere on solar activity

    NASA Astrophysics Data System (ADS)

    Semenov, A. I.; Shefov, N. N.

    2003-04-01

    On the basis of the measurement data of temperature by rocket and ground-based spectrophotometric (nightglow emissions of hydroxyl,sodium and atomic oxygen of 557.7 nm) methods obtained during 21 and 22 cycles of solar activity, the distributions with height of mean monthly temperature of an atmosphere for region of altitudes Z from 60 to 100 km have been constructed. The periods of maxima and minima of solar activity (1980 and 1991, F10.7=198 and 208; 1976 and 1986, F10.7=73 and 75) were considered. On the basis of these distributions with height of the seasonal variations of dependence of temperature from solar activity S = deltaT(Z)/deltaF, K/100 sfu have been analyzed. It was revealed, that character of seasonal variations essentially changes with growth of height. Mean annual solar response S at heights lower than 70 km is negative, and at higher heights is positive. This solar response S in mesopause region reaches 3 (sigma=1). Such character of influence of solar activity on temperature of the upper atmosphere is caused by features of mean annual and seasonal variations of its distributions with height. The distributions with height of amplitudes and phases of three harmonics of seasonal variations S are presented. This work was supported by the Grant N 2274 of ISTC.

  15. [Fluctuations in biophysical measurements as a result of variations in solar activity].

    PubMed

    Peterson, T F

    1995-01-01

    A theory is proposed to explain variations in the net electrical charge of biological substances at the Earth's surface. These are shown to occur in association with changes in the solar wind and geomagnetic field. It is suggested that a liquid dielectric's net volume charge will imitate pH effects, influence chemical reaction rates, and alter ion transfer mechanisms in biophysical systems. An experiment is described which measures dielectric volume charge, or non-neutrality, to allow correlation of this property with daily, 28-day, and 11-year fluctuation patterns in geophysical and satellite data associated with solar activity and the interplanetary magnetic field.

  16. Seismic Forecasting of Solar Activity

    NASA Technical Reports Server (NTRS)

    Braun, Douglas; Lindsey, Charles

    2001-01-01

    We have developed and improved helioseismic imaging techniques of the far-side of the Sun as part of a synoptic monitor of solar activity. In collaboration with the MIDI team at Stanford University we are routinely applying our analysis to images within 24 hours of their acquisition by SOHO. For the first time, real-time seismic maps of large active regions on the Sun's far surface are publicly available. The synoptic images show examples of active regions persisting for one or more solar rotations, as well as those initially detected forming on the solar far side. Until recently, imaging the far surface of the Sun has been essentially blind to active regions more than about 50 degrees from the antipode of disk center. In a paper recently accepted for publication, we have demonstrated how acoustic travel-time perturbations may be mapped over the entire hemisphere of the Sun facing away from the Earth, including the polar regions. In addition to offering significant improvements to ongoing space weather forecasting efforts, the procedure offers the possibility of local seismic monitoring of both the temporal and spatial variations in the acoustic properties of the Sun over the entire far surface.

  17. A solar activity monitoring platform for SCADM

    NASA Technical Reports Server (NTRS)

    Kissell, K. E.; Ratcliff, D. D.

    1980-01-01

    The adaptation of proven space probe technology is proposed as a means of providing a solar activity monitoring platform which could be injected behind the Earth's orbital position to give 3 to 6 days advanced coverage of the solar phenomenon on the backside hemisphere before it rotates into view and affects terrestrial activities. The probe would provide some three dimensional discrimination within the ecliptic latitude. This relatively simple off-Earth probe could provide very high quality data to support the SCADM program, by transmitting both high resolution video data of the solar surface and such measurements of solar activity as particle, X-ray, ultraviolet, and radio emission fluxes. Topics covered include the orbit; constraints on the spacecraft; subsystems and their embodiments; optical imaging sensors and their operation; and the radiation-pressure attitude control system are described. The platform would be capable of mapping active regions on an hourly basis with one arc-second resolution.

  18. The Influence of Solar Proton Events in Solar Cycle 23 on the Neutral Middle Atmosphere

    NASA Technical Reports Server (NTRS)

    Jackman, Charles H.; vonKonig, Miriam; Anderson, John; Roble, Raymond G.; McPeters, Richard D.; Fleming, Eric L.; Russell, James M.

    2004-01-01

    Solar proton events (SPEs) can cause changes in constituents in the Earth's middle atmosphere. The highly energetic protons cause ionizations, excitations, dissociations, and dissociative ionizations of the background constituents, which lead to the production of HO(x) (H, OH, HO2) and NO(y) (N, NO, NO2, NO3, N2O5, HNO3, HO2NO2, ClONO2, BrONO2). The HO(x) increases lead to short-lived ozone decreases in the mesosphere and upper stratosphere due to the short lifetimes of the HO, constituents. The NO(x) increases lead to long-lived stratospheric ozone changes because of the long lifetime of NO(y) constituents in this region. Solar cycle 23 was quite active with SPEs and very large fluxes of high energy protons occurred in July and November 2000, November 200 1, and April 2002. Smaller, but still substantial, proton fluxes impacted the Earth during other months in the 1997-2003 time period. The impact of the very large SPEs on the neutral middle atmosphere during solar cycle 23 will be discussed, including the HO(x), NO(y), ozone variations and induced atmospheric transport changes. Two multi-dimensional models, the Goddard Space Flight Center (GSFC) Two-dimensional (2D) Model and the Thermosphere Ionosphere Mesosphere Electrodynamic General Circulation Model (TIME-GCM), were used in computing the influence of the SPEs. The results of the GSFC 2D Model and the TIME-GCM will be shown along with comparisons to the Upper Atmosphere Research Satellite (UARS) Halogen Occultation Experiment (HALOE) and Solar Backscatter Ultraviolet 2 (SBUV/2) instruments.

  19. Solar activity and the weather

    NASA Technical Reports Server (NTRS)

    Wilcox, J. M.

    1975-01-01

    The attempts during the past century to establish a connection between solar activity and the weather are discussed; some critical remarks about the quality of much of the literature in this field are given. Several recent investigations are summarized. Use of the solar/interplanetary magnetic sector structure in future investigations is suggested to add an element of cohesiveness and interaction to these investigations.

  20. Solar collector manufacturing activity, 1988

    NASA Astrophysics Data System (ADS)

    1989-11-01

    This report was prepared by the Energy Information Administration, the independent statistical and analytical agency within the U.S. Department of Energy in cooperation with the Office of Conservation and Renewable Energy. The report presents data on producer shipments and end uses obtained from manufacturers and importers of solar thermal collectors and photovoltaic modules. It provides annual data necessary for the Department of Energy to execute its responsibility to: (1) monitor activities and trends in the solar collector manufacturing industry, (2) prepare the national energy strategy, and (3) provide information on the size and status of the industry to interested groups such as the U.S. Congress, government agencies, the Solar Energy Research institute, solar energy specialists, manufacturers, and the general public.

  1. Investigation of relationships between parameters of solar nano-flares and solar activity

    NASA Astrophysics Data System (ADS)

    Safari, Hossein; Javaherian, Mohsen; Kaki, Bardia

    2016-07-01

    Solar flares are one of the important coronal events which are originated in solar magnetic activity. They release lots of energy during the interstellar medium, right after the trigger. Flare prediction can play main role in avoiding eventual damages on the Earth. Here, to interpret solar large-scale events (e.g., flares), we investigate relationships between small-scale events (nano-flares) and large-scale events (e.g., flares). In our method, by using simulations of nano-flares based on Monte Carlo method, the intensity time series of nano-flares are simulated. Then, the solar full disk images taken at 171 angstrom recorded by SDO/AIA are employed. Some parts of the solar disk (quiet Sun (QS), coronal holes (CHs), and active regions (ARs)) are cropped and the time series of these regions are extracted. To compare the simulated intensity time series of nano-flares with the intensity time series of real data extracted from different parts of the Sun, the artificial neural networks is employed. Therefore, we are able to extract physical parameters of nano-flares like both kick and decay rate lifetime, and the power of their power-law distributions. The procedure of variations in the power value of power-law distributions within QS, CH is similar to AR. Thus, by observing the small part of the Sun, we can follow the procedure of solar activity.

  2. Space weather influence on the agriculture technology and wheat prices in the medieval England (1259-1703) through cosmic ray/solar activity cycle variations

    NASA Astrophysics Data System (ADS)

    Dorman, L. I.; Pustil'Nik, L. A.; Yom Din, G.

    2003-04-01

    The database of Professor Rogers (1887), which includes wheat prices in England in the Middle Ages (1249-1703) was used to search for possible manifestations of solar activity and cosmic ray intensity variations. The main object of our statistical analysis is investigation of bursts of prices. Our study shows that bursts and troughs of wheat prices take place at extreme states (maximums or minimums) of solar activity cycles. We present a conceptual model of possible modes for sensitivity of wheat prices to weather conditions, caused by cosmic ray intensity solar cycle variations, and compare the expected price fluctuations with wheat price variations recorded in the Medieval England. We compared statistical properties of the intervals between price bursts with statistical properties of the intervals between extremes (minimums) of solar cycles during the years 1700-2000. The medians of both samples have the values of 11.00 and 10.7 years; standard deviations are 1.44 and 1.53 years for prices and for solar activity, respectively. The hypothesis that the frequency distributions are the same for both of the samples have significance level >95%. In the next step we analyzed direct links between wheat prices and cosmic ray cycle variations in the 17th Century, for which both wheat prices and cosmic ray intensity (derived from Be-10 isotope data) are available. We show that for all seven solar activity minimums (cosmic ray intensity maximums) the observed prices were higher than prices for the seven intervals of maximal solar activity (100% sign correlation). This result, combined with the conclusion of similarity of statistical properties of the price and solar activity extremes can be considered as direct evidence of a causal connection between wheat prices bursts and solar activity/cosmic ray intensity extremes.

  3. Influence of Solar Variability on the North Atlantic / European Sector.

    NASA Astrophysics Data System (ADS)

    Gray, L. J.

    2016-12-01

    The 11year solar cycle signal in December-January-February averaged mean-sea-level pressure and Atlantic/European blocking frequency is examined using multilinear regression with indices to represent variability associated with the solar cycle, volcanic eruptions, the El Nino - Southern Oscillation (ENSO) and the Atlantic Multidecadal Oscillation (AMO). Results from a previous 11-year solar cycle signal study of the period 1870-2010 (140 years; 13 solar cycles) that suggested a 3-4 year lagged signal in SLP over the Atlantic are confirmed by analysis of a much longer reconstructed dataset for the period 1660-2010 (350 years; 32 solar cycles). Apparent discrepancies between earlier studies are resolved and stem primarily from the lagged nature of the response and differences between early- and late-winter responses. Analysis of the separate winter months provide supporting evidence for two mechanisms of influence, one operating via the atmosphere that maximises in late winter at 0-2 year lags and one via the mixd-layer ocean that maximises in early winter at 3-4 year lags. Corresponding analysis of DJF-averaged Atlantic / European blocking frequency shows a highly statistically significant signal at 1-year lag that originates promarily from the late winter response. The 11-year solar signal in DJF blocking frequency is compared with other known influences from ENSO and the AMO and found to be as large in amplitude and have a larger region of statistical significance.

  4. Heliophysics: Evolving Solar Activity and the Climates of Space and Earth

    NASA Astrophysics Data System (ADS)

    Schrijver, Carolus J.; Siscoe, George L.

    2010-09-01

    Preface; 1. Interconnectedness in heliophysics Carolus J. Schrijver and George L. Siscoe; 2. Long-term evolution of magnetic activity of Sun-like stars Carolus J. Schrijver; 3. Formation and early evolution of stars and proto-planetary disks Lee W. Hartmann; 4. Planetary habitability on astronomical time scales Donald E. Brownlee; 5. Solar internal flows and dynamo action Mark S. Miesch; 6. Modeling solar and stellar dynamos Paul Charbonneau; 7. Planetary fields and dynamos Ulrich R. Christensen; 8. The structure and evolution of the 3D solar wind John T. Gosling; 9. The heliosphere and cosmic rays J. Randy Jokipii; 10. Solar spectral irradiance: measurements and models Judith L. Lean and Thomas N. Woods; 11. Astrophysical influences on planetary climate systems Juerg Beer; 12. Evaluating the drivers of Earth's climate system Thomas J. Crowley; 13. Ionospheres of the terrestrial planets Stanley C. Solomon; 14. Long-term evolution of the geospace climate Jan J. Sojka; 15. Waves and transport processes in atmospheres and oceans Richard L. Walterscheid; 16. Solar variability, climate, and atmospheric photochemistry Guy P. Brasseur, Daniel Marsch and Hauke Schmidt; Appendix I. Authors and editors; List of illustrations; List of tables; Bibliography; Index.

  5. Heliophysics: Evolving Solar Activity and the Climates of Space and Earth

    NASA Astrophysics Data System (ADS)

    Schrijver, Carolus J.; Siscoe, George L.

    2012-01-01

    Preface; 1. Interconnectedness in heliophysics Carolus J. Schrijver and George L. Siscoe; 2. Long-term evolution of magnetic activity of Sun-like stars Carolus J. Schrijver; 3. Formation and early evolution of stars and proto-planetary disks Lee W. Hartmann; 4. Planetary habitability on astronomical time scales Donald E. Brownlee; 5. Solar internal flows and dynamo action Mark S. Miesch; 6. Modeling solar and stellar dynamos Paul Charbonneau; 7. Planetary fields and dynamos Ulrich R. Christensen; 8. The structure and evolution of the 3D solar wind John T. Gosling; 9. The heliosphere and cosmic rays J. Randy Jokipii; 10. Solar spectral irradiance: measurements and models Judith L. Lean and Thomas N. Woods; 11. Astrophysical influences on planetary climate systems Juerg Beer; 12. Evaluating the drivers of Earth's climate system Thomas J. Crowley; 13. Ionospheres of the terrestrial planets Stanley C. Solomon; 14. Long-term evolution of the geospace climate Jan J. Sojka; 15. Waves and transport processes in atmospheres and oceans Richard L. Walterscheid; 16. Solar variability, climate, and atmospheric photochemistry Guy P. Brasseur, Daniel Marsch and Hauke Schmidt; Appendix I. Authors and editors; List of illustrations; List of tables; Bibliography; Index.

  6. Studies of the Solar Radiations' Influence About Geomembranes Used in Ecological Landfill

    NASA Astrophysics Data System (ADS)

    Vasiluta, Petre; Cofaru, Ileana Ioana; Cofaru, Nicolae Florin; Popa, Dragos Laurentiu

    2017-12-01

    The study shown in this paper presents the behavior of geomembranes used at the ecological landfills. The influences of the solar radiations has a great importance regarding the correct mounting of the geomembranes. The mathematical model developed for the determination anytime and anywhere in the world for the next values and parameters: apparent solar time, solar declination, solar altitude, solar azimuth and incidence angle, zone angle, angle of sun elevation, solar declination, solar constant, solar flux density, diffuse solar radiation, global radiation, soil albedo, total radiant flux density and relational links of these values. The results of this model was used for creations an AutoCAD subroutines useful for choosing the correct time for correct mounting anywhere of the geomembranes

  7. Science Activities in Energy: Solar Energy II.

    ERIC Educational Resources Information Center

    Oak Ridge Associated Universities, TN.

    Included in this science activities energy package are 14 activities related to solar energy for secondary students. Each activity is outlined on a single card and is introduced by a question such as: (1) how much solar heat comes from the sun? or (2) how many times do you have to run water through a flat-plate collector to get a 10 degree rise in…

  8. Solar activity simulation and forecast with a flux-transport dynamo

    NASA Astrophysics Data System (ADS)

    Macario-Rojas, Alejandro; Smith, Katharine L.; Roberts, Peter C. E.

    2018-06-01

    We present the assessment of a diffusion-dominated mean field axisymmetric dynamo model in reproducing historical solar activity and forecast for solar cycle 25. Previous studies point to the Sun's polar magnetic field as an important proxy for solar activity prediction. Extended research using this proxy has been impeded by reduced observational data record only available from 1976. However, there is a recognised need for a solar dynamo model with ample verification over various activity scenarios to improve theoretical standards. The present study aims to explore the use of helioseismology data and reconstructed solar polar magnetic field, to foster the development of robust solar activity forecasts. The research is based on observationally inferred differential rotation morphology, as well as observed and reconstructed polar field using artificial neural network methods via the hemispheric sunspot areas record. Results show consistent reproduction of historical solar activity trends with enhanced results by introducing a precursor rise time coefficient. A weak solar cycle 25, with slow rise time and maximum activity -14.4% (±19.5%) with respect to the current cycle 24 is predicted.

  9. Ionospheric effects of the extreme solar activity of February 1986

    NASA Technical Reports Server (NTRS)

    Boska, J.; Pancheva, D.

    1989-01-01

    During February 1986, near the minimum of the 11 year Solar sunspot cycle, after a long period of totally quiet solar activity (R sub z = 0 on most days in January) a period of a suddenly enhanced solar activity occurred in the minimum between solar cycles 21 and 22. Two proton flares were observed during this period. A few other flares, various phenomena accompanying proton flares, an extremely severe geomagnetic storm and strong disturbances in the Earth's ionosphere were observed in this period of enhanced solar activity. Two active regions appeared on the solar disc. The flares in both active regions were associated with enhancement of solar high energy proton flux which started on 4 February of 0900 UT. Associated with the flares, the magnetic storm with sudden commencement had its onset on 6 February 1312 UT and attained its maximum on 8 February (Kp = 9). The sudden enhancement in solar activity in February 1986 was accompanied by strong disturbances in the Earth's ionosphere, SIDs and ionospheric storm. These events and their effects on the ionosphere are discussed.

  10. Long-term solar activity explored with wavelet methods

    NASA Astrophysics Data System (ADS)

    Lundstedt, H.; Liszka, L.; Lundin, R.; Muscheler, R.

    2006-03-01

    Long-term solar activity has been studied with a set of wavelet methods. The following indicators of long-term solar activity were used; the group sunspot number, the sunspot number, and the 14C production rate. Scalograms showed the very long-term scales of 2300 years (Hallstat cycle), 900-1000 years, 400-500 years, and 200 years (de Vries cycle). Scalograms of a newly-constructed 14C production rate showed interesting solar modulation during the Maunder minimum. Multi-Resolution Analysis (MRA) revealed the modulation in detail, as well as peaks of solar activity not seen in the sunspot number. In both the group sunspot number scalogram and the 14C production rate scalogram, a process appeared, starting or ending in late 1700. This process has not been discussed before. Its solar origin is unclear.

    The group sunspot number ampligram and the sunspot number ampligram showed the Maunder and the Dalton minima, and the period of high solar activity, which already started about 1900 and then decreased again after mid 1990. The decrease starts earlier for weaker components. Also, weak semiperiodic activity was found.

    Time Scale Spectra (TSS) showed both deterministic and stochastic processes behind the variability of the long-term solar activity. TSS of the 14C production rate, group sunspot number and Mt. Wilson sunspot index and plage index were compared in an attempt to interpret the features and processes behind the long-term variability.

  11. On the possible relations between solar activities and global seismicity in the solar cycle 20 to 23

    NASA Astrophysics Data System (ADS)

    Herdiwijaya, Dhani; Arif, Johan; Nurzaman, Muhamad Zamzam; Astuti, Isna Kusuma Dewi

    2015-09-01

    Solar activities consist of high energetic particle streams, electromagnetic radiation, magnetic and orbital gravitational forces. The well-know solar activity main indicator is the existence of sunspot which has mean variation in 11 years, named by solar cycle, allow for the above fluctuations. Solar activities are also related to the space weather affecting all planetary atmospheric variability, moreover to the Earth's climate variability. Large extreme space and geophysical events (high magnitude earthquakes, explosive volcanic eruptions, magnetic storms, etc.) are hazards for humankind, infrastructure, economies, technology and the activities of civilization. With a growing world population, and with modern reliance on delicate technological systems, human society is becoming increasingly vulnerable to natural hazardous events. The big question arises to the relation between solar forcing energy to the Earth's global seismic activities. Estimates are needed for the long term occurrence-rate probabilities of these extreme natural hazardous events. We studied connectivity from yearly seismic activities that refer to and sunspot number within the solar cycle 20 to 23 of year 1960 to 2013 (53 years). We found clear evidences that in general high magnitude earthquake events and their depth were related to the low solar activity.

  12. FUPSOL: Modelling the Future and Past Solar Influence on Earth Climate

    NASA Astrophysics Data System (ADS)

    Anet, J. G.; Rozanov, E.; Peter, T.

    2012-04-01

    Global warming is becoming one of the main threats to mankind. There is growing evidence that anthropogenic greenhouse gases have become the dominant factor since about 1970. At the same time natural factors of climate change such as solar and volcanic forcings cannot be neglected on longer time scales. Despite growing scientific efforts over the last decades in both, observations and simulations, the uncertainty of the solar contribution to the past climate change remained unacceptably high (IPCC, 2007), the reasons being on one hand missing observations of solar irradiance prior to the satellite era, and on the other hand a majority of models so far not including all processes relevant for solar-climate interactions. This project aims at elucidating the processes governing the effects of solar activity variations on Earth's climate. We use the state-of-the-art coupled atmosphere-ocean-chemistry-climate model (AOCCM) SOCOL (Schraner et al, 2008) developed in Switzerland by coupling the community Earth System Model (ESM) COSMOS distributed by MPI for Meteorology (Hamburg, Germany) with a comprehensive atmospheric chemistry module. The model solves an extensive set of equations describing the dynamics of the atmosphere and ocean, radiative transfer, transport of species, their chemical transformations, cloud formation and the hydrological cycle. The intention is to show how past solar variations affected climate and how the decrease in solar forcing expected for the next decades will affect climate on global and regional scales. We will simulate the global climate system behavior during Dalton minimum (1790 and 1830) and first half of 21st century with a series of multiyear ensemble experiments and perform these experiments using all known anthropogenic and natural climate forcing taken in different combinations to understand the effects of solar irradiance in different spectral regions and particle precipitation variability. Further on, we will quantify the solar

  13. Global Distribution and Variations of NO Infrared Radiative Flux and Its Responses to Solar Activity and Geomagnetic Activity in the Thermosphere

    NASA Astrophysics Data System (ADS)

    Tang, Chaoli; Wei, Yuanyuan; Liu, Dong; Luo, Tao; Dai, Congming; Wei, Heli

    2017-12-01

    The global distribution and variations of NO infrared radiative flux (NO-IRF) are presented during 2002-2016 in the thermosphere covering 100-280 km altitude based on Sounding of the Atmosphere using Broadband Emission Radiometry (SABER) data set. For investigating the spatial variations of the mutual relationship between NO-IRF and solar activity, the altitude ranges from 100 km to 280 km are divided into 90 altitude bins, and the latitude regions of 83°S-83°N are divided into 16 latitude bins. By processing about 1.8E9 NO-IRF observation values from about 5E6 vertical nighttime profiles recorded in SABER data set, we obtained more than 4.1E8 samples of NO-IRF. The annual-mean values of NO-IRF are then calculated by all available NO-IRF samples within each latitude and altitude bin. Local latitudinal maxima in NO-IRF are found between 120 and 145 km altitude, and the maximum NO-IRF located at polar regions are 3 times more than that of the minimum at equatorial region. The influences of solar and geomagnetic activity on the spatial variations of NO-IRF are investigated. Both the NO-IRF and its response to solar and geomagnetic activity show nearly symmetric distribution between the two hemispheres. It is demonstrated that the observed changes in NO-IRF at altitudes between 100 and 225 km correlate well with the changes in solar activity. The NO-IRF at solar maximum is about 4 times than that at solar minimum, and the current maximum of NO-IRF in 2014 is less than 70% of the prior maximum in 2001. For the first time, the response ranges of the NO-IRF to solar and geomagnetic activity at different altitudes and latitudes are reported.

  14. Solar Irradiance Variations on Active Region Time Scales

    NASA Technical Reports Server (NTRS)

    Labonte, B. J. (Editor); Chapman, G. A. (Editor); Hudson, H. S. (Editor); Willson, R. C. (Editor)

    1984-01-01

    The variations of the total solar irradiance is an important tool for studying the Sun, thanks to the development of very precise sensors such as the ACRIM instrument on board the Solar Maximum Mission. The largest variations of the total irradiance occur on time scales of a few days are caused by solar active regions, especially sunspots. Efforts were made to describe the active region effects on total and spectral irradiance.

  15. Evaluation of long term solar activity effects on GPS derived TEC

    NASA Astrophysics Data System (ADS)

    Mansoori, Azad A.; Khan, Parvaiz A.; Ahmad, Rafi; Atulkar, Roshni; M, Aslam A.; Bhardwaj, Shivangi; Malvi, Bhupendra; Purohit, P. K.; Gwal, A. K.

    2016-10-01

    The solar activity hence the solar radiance follows a long term periodic variability with eleven years periodicity, known as solar cycle. This drives the long term variability of the ionosphere. In the present problem we investigate the long term behaviour of the ionosphere with the eleven year cyclic solar activity. Under the present study we characterize the ionospheric variability by Total Electron Content (TEC) using measurements made by Global Positioning System (GPS) and solar cycle variability by various solar activity indices. We make use of five solar activity indices viz. sunspot number (Rz), solar radio Flux (F10.7 cm), EUV Flux (26-34 nm), flare index and CME occurrences. The long term variability of these solar activity indices were then compared and correlated with the variability of ionospheric TEC, at a mid latitude station, Usuda (36.13N, 138.36E), of Japan, during the solar cycle 23 and ascending phase of cycle 24. From our study, we found that long term changes in the ionospheric TEC vary synchronously with corresponding changes in the solar activity indices. The correlation analysis shows that all the solar activity indices exhibit a very strong correlation with TEC (R =0.76 -0.99). Moreover the correlation between the two is stronger in the descending phase of the solar cycle. The correlation is found to be remarkably strongest during the deep minimum of the solar cycle 24 i.e. between 2007- 2009. Also we noticed a hysteresis effect exists with solar radio flux (F10.7 cm) and solar EUV flux (26-34 nm). This effect is absent with other parameters.

  16. Influences of misprediction costs on solar flare prediction

    NASA Astrophysics Data System (ADS)

    Huang, Xin; Wang, HuaNing; Dai, XingHua

    2012-10-01

    The mispredictive costs of flaring and non-flaring samples are different for different applications of solar flare prediction. Hence, solar flare prediction is considered a cost sensitive problem. A cost sensitive solar flare prediction model is built by modifying the basic decision tree algorithm. Inconsistency rate with the exhaustive search strategy is used to determine the optimal combination of magnetic field parameters in an active region. These selected parameters are applied as the inputs of the solar flare prediction model. The performance of the cost sensitive solar flare prediction model is evaluated for the different thresholds of solar flares. It is found that more flaring samples are correctly predicted and more non-flaring samples are wrongly predicted with the increase of the cost for wrongly predicting flaring samples as non-flaring samples, and the larger cost of wrongly predicting flaring samples as non-flaring samples is required for the higher threshold of solar flares. This can be considered as the guide line for choosing proper cost to meet the requirements in different applications.

  17. An interaction of a NR3C1 polymorphism and antenatal solar activity impacts both hippocampus volume and neuroticism in adulthood

    PubMed Central

    Montag, Christian; Eichner, Markus; Markett, Sebastian; Quesada, Carlos M.; Schoene-Bake, Jan-Christoph; Melchers, Martin; Plieger, Thomas; Weber, Bernd; Reuter, Martin

    2013-01-01

    The investigation of the interaction of genes and environment in the context of mental health and personality yields important new insights for a better understanding of human nature. Both antenatal and postnatal environmental factors have been considered as potential modulators of genetic activity. Antenatally, especially smoking or alcohol drinking habits of the mother dramatically influence the health of the child during pregnancy and even later on in life. In the present study we would like to introduce a more “distant” factor that is not under the control of the becoming mother but that nevertheless plays a potential role for the health of the unborn child later on in adulthood. Here, we retrospectively investigate the influence of solar activity (while the child is still in the uterus of the becoming mother) on brain structure (with a focus on hippocampus and amygdala volume) and personality in adulthood. We observe an interaction of a genetic variant (rs41423247) of the glucocorticoid receptor gene (NR3C1) and solar activity in the first trimester after conception on both hippocampal volume and the personality trait neuroticism in adulthood in N = 254 participants. The NR3C1 gene is the focus of interest, because of its influence on the hypothalamic-pituitary-adrenal (HPA) axis and negative emotionality. Carriers of the CC variant of rs41423247 grown in the womb under the influence of high sun radiation (high solar activity) show both the highest hippocampal volume in the left hemisphere and lowest neuroticism scores. The present findings should encourage researchers in psychology and psychiatry to include also environmental influences such as solar activity besides genetics to better understand the etiogenesis of psychiatric disorders. PMID:23761749

  18. Solar cycle activity and atmospheric dynamics revealed by Be-7

    NASA Astrophysics Data System (ADS)

    Kulan, A.; Aldahan, A.; Possnert, G.; Vintersved, I.

    2003-04-01

    In this study we present ^7Be and 137Cs concentrations in aerosols collected on surface air filters for the period 1972-2000 from three stations in Sweden covering latitudes 56^o to 70^o. The cosmogenic isotope ^7Be (T1/2 = 53.4 days) is produced by interaction of cosmic rays with the atmosphere. ^7Be is adsorbed onto aerosol particles after its formation, and removed from the atmosphere by both dry and wet deposition (atmospheric residence time of about one year). Maximum production of ^7Be occurs in the polar regions and the maximum deposition is found in the middle latitudes. After its production (mainly in the stratosphere) the ^7Be isotope is subjected to vertical and horizontal transport processes within the atmosphere and accordingly can act as a tracer of air mass origin and its approximate age. Furthermore, the production of cosmogenic isotopes is strongly influenced by the solar wind (solar activity, mainly energetic protons) and hence terrestrial records of ^7Be are directly reflecting the activity of the sun. Our ^7Be results reveal seasonal changes and together with the 137Cs records confirm a long-term transport and a strong coupling with air masses from middle and low latitudes. An apparent correlation between the 11-year solar cycle activity and ^7Be is found and we also observe that precipitation effectively depletes ^7Be from the atmosphere through washout of aerosols.

  19. Study of seismic activity during the ascending and descending phases of solar activity

    NASA Astrophysics Data System (ADS)

    Sukma, Indriani; Abidin, Zamri Zainal

    2017-06-01

    The study of the solar cycle and geomagnetic index associated with the seismic activity from the year 1901 to the end of 2015 has been done for an area that covers the majority of China and its bordering countries. Data of sunspot number, solar wind speed, daily storm time index and earthquake number are collected from NOAA, NASA, WDC, OMNI and USGS databases and websites. The earthquakes are classified into small (M < 5) and large (M ≥ 5) magnitudes (in Richter scale). We investigated the variation of earthquake activities with the geomagnetic storm index due to the solar wind. We focused on their variation in the ascending and descending phases of solar cycle. From our study, we conclude that there is a correlation between the phases' geomagnetic index and solar wind speed. We have also suggested that there is a certain degree of correlation between solar activity and seismicity in these phases. For every solar cycle, we find that there is a trend for earthquakes to occur in greater numbers during the descending phase. This can be explained by the increment in the solar wind speed and geomagnetic storm index during this phase.

  20. Influence of synoptic weather patterns on solar irradiance variability in Europe

    NASA Astrophysics Data System (ADS)

    Parding, Kajsa; Hinkelman, Laura; Liepert, Beate; Ackerman, Thomas; Dagestad, Knut-Frode; Asle Olseth, Jan

    2014-05-01

    Solar radiation is important for many aspects of existence on Earth, including the biosphere, the hydrological cycle, and creatures living on the planet. Previous studies have reported decadal trends in observational records of surface shortwave (SW) irradiance around the world, too strong to be caused by varying solar output. These observed decadal trends have been dubbed "solar dimming and brightening" and are believed to be related to changes in atmospheric aerosols and cloud cover. Because the observed solar variability coincides with qualitative air pollution histories, the dimming and brightening have become almost synonymous with shortwave attenuation by anthropogenic aerosols. However, there are indications that atmospheric circulation patterns have influenced the dimming and brightening in some regions, e.g., Alaska and Scandinavia. In this work, we focus on the role of atmospheric circulation patterns in modifying shortwave irradiance. An examination of European SW irradiance data from the Global Energy Balance Archive (GEBA) shows that while there are periods of predominantly decreasing (~1970-1985) and increasing (~1985-2007) SW irradiance, the changes are not spatially uniform within Europe and in a majority of locations not statistically significant. To establish a connection between weather patterns and sunshine, regression models of SW irradiance are fitted using a daily classification of European weather called Grosswetterlagen (GWL). The GWL reconstructions of shortwave irradiance represent the part of the solar variability that is related to large scale weather patterns, which should be effectively separated from the influence of varying anthropogenic aerosol emissions. The correlation (R) between observed and reconstruced SW irradiance is between 0.31 and 0.75, depending on station and season, all statistically significant (p<0.05, estimated with a bootstrap test). In central and eastern parts of Europe, the observed decadal SW variability is

  1. Solar Energy Educational Material, Activities and Science Projects

    Science.gov Websites

    ;The sun has produced energy for billions of years. Solar energy is the solar radiation that reaches Energy - Energy from the Sun DOE Documents with Activities/Projects: Web Pages Solar Energy Education , Part I. Energy, Society, and the Sun Solar Energy Education. Reader, Part II. Sun Story. [Includes

  2. Solar activity variations of nocturnal thermospheric meridional winds over Indian longitude sector

    NASA Astrophysics Data System (ADS)

    Madhav Haridas, M. K.; Manju, G.; Arunamani, T.

    2016-09-01

    The night time F-layer base height information from ionosondes located at two equatorial stations Trivandrum (TRV 8.5°N, 77°E) and Sriharikota (SHAR 13.7°N, 80.2°E) spanning over two decades are used to derive the climatology of equatorial nocturnal Thermospheric Meridional Winds (TMWs) prevailing during High Solar Activity (HSA) and Low Solar Activity (LSA) epochs. The important inferences from the analysis are 1) Increase in mean equatorward winds observed during LSA compared to HSA during pre midnight hours; 25 m/s for VE (Vernal Equinox) and 20 m/s for SS (Summer Solstice), AE (autumnal Equinox) and WS (Winter Solstice). 2) Mean wind response to Solar Flux Unit (SFU) is established quantitatively for all seasons for pre-midnight hours; rate of increase is 0.25 m/s/SFU for VE, 0.2 m/s/SFU for SS and WS and 0.08 m/s/SFU for AE. 3) Theoretical estimates of winds for the two epochs are performed and indicate the role of ion drag forcing as a major factor influencing TMWs. 4) Observed magnitude of winds and rate of flux dependencies are compared to thermospheric wind models. 5) Equinoctial asymmetry in TMWs is observed for HSA at certain times, with more equatorward winds during AE. These observations lend a potential to parameterize the wind components and effectively model the winds, catering to solar activity variations.

  3. Active power control of solar PV generation for large interconnection frequency regulation and oscillation damping

    DOE PAGES

    Liu, Yong; Zhu, Lin; Zhan, Lingwei; ...

    2015-06-23

    Because of zero greenhouse gas emission and decreased manufacture cost, solar photovoltaic (PV) generation is expected to account for a significant portion of future power grid generation portfolio. Because it is indirectly connected to the power grid via power electronic devices, solar PV generation system is fully decoupled from the power grid, which will influence the interconnected power grid dynamic characteristics as a result. In this study, the impact of solar PV penetration on large interconnected power system frequency response and inter-area oscillation is evaluated, taking the United States Eastern Interconnection (EI) as an example. Furthermore, based on the constructedmore » solar PV electrical control model with additional active power control loops, the potential contributions of solar PV generation to power system frequency regulation and oscillation damping are examined. The advantages of solar PV frequency support over that of wind generator are also discussed. Finally, simulation results demonstrate that solar PV generations can effectively work as ‘actuators’ in alleviating the negative impacts they bring about.« less

  4. Influence of solar activity on the development of calcareous nannofossils from a Middle Holocene costal paleo-ria (SW Portugal)

    NASA Astrophysics Data System (ADS)

    Hernández, Armand; Cachão, Mário; Trigo, Ricardo M.; Conceição Freitas, M.

    2015-04-01

    periodogram unveils only one significant periodicity (228-yrs). Phases with oceanic influence (downwelling) would be related to 450, 350 and 236-yrs frequencies and the phase with coastal influence (upwelling) would be linked to 228-yrs periodicity. These periodicities fit with previous solar activity reconstructions at millennial-to-centennial scale based on different proxies (Bond et al. 2001, Vaquero et al. 2002, Solanki et al. 2004), which, in turn, are conditioning the earth's climate system. Finally, performed time-frequency analyses on F1 and F2 scores show a higher activity of the 228-yrs periodicity during the whole studied period (spanning between 8.8k and 4.8k cal yr BP) with maximum values between 8k to 7k cal yr BP and 6k to 5k cal yr BP. By contrast, higher periodicities (450, 350 and 236-yrs) would be mainly confined to prior 7.5k cal yrs BP. These results highlight the possibility to use the calcareous nannofossils as indirect proxies of solar activity in cases of ultra-high resolution (centennial) sedimentary sequences. References Alday et al., Estuar Coast Shelf S, 66, 532 (2006). Bond et al., Science, 294, 2130 (2001). Solanki et al., Nature, 431, 1084 (2004). Vaquero et al., Geophys Res Lett, 29, 1997 (2002).

  5. Active Longitude and Solar Flare Occurrences

    NASA Astrophysics Data System (ADS)

    Gyenge, N.; Ludmány, A.; Baranyi, T.

    2016-02-01

    The aim of the present work is to specify the spatio-temporal characteristics of flare activity observed by the Reuven Ramaty High Energy Solar Spectroscopic Imager (RHESSI) and the Geostationary Operational Environmental Satellite (GOES) in connection with the behavior of the longitudinal domain of enhanced sunspot activity known as active longitude (AL). By using our method developed for this purpose, we identified the AL in every Carrington Rotation provided by the Debrecen Photoheliographic Data. The spatial probability of flare occurrence has been estimated depending on the longitudinal distance from AL in the northern and southern hemispheres separately. We have found that more than 60% of the RHESSI and GOES flares is located within +/- 36^\\circ from the AL. Hence, the most flare-productive active regions tend to be located in or close to the active longitudinal belt. This observed feature may allow for the prediction of the geo-effective position of the domain of enhanced flaring probability. Furthermore, we studied the temporal properties of flare occurrence near the AL and several significant fluctuations were found. More precisely, the results of the method are the following fluctuations: 0.8, 1.3, and 1.8 years. These temporal and spatial properties of the solar flare occurrence within the active longitudinal belts could provide us with an enhanced solar flare forecasting opportunity.

  6. Magnetic Reconfiguration in Explosive Solar Activity

    NASA Technical Reports Server (NTRS)

    Antiochos, Spiro K.

    2008-01-01

    A fundamental property of the Sun's corona i s that it is violently dynamic. The most spectacular and most energetic manifestations of this activity are the giant disruptions that give rise to coronal mass ejections (CME) and eruptive flares. These major events are of critical importance, because they drive the most destructive forms of space weather at Earth and in the solar system, and they provide a unique opportunity to study, in revealing detail, the interaction of magnetic field and matter, in particular, magnetohydrodynamic instability and nonequilibrium -- processes that are at the heart of laboratory and astrophysical plasma physics. Recent observations by a number of NASA space missions have given us new insights into the physical mechanisms that underlie coronal explosions. Furthermore, massively-parallel computation have now allowed us to calculate fully three-dimensional models for solar activity. In this talk I will present some of the latest observations of the Sun, including those from the just-launched Hinode and STEREO mission, and discuss recent advances in the theory and modeling of explosive solar activity.

  7. Radio Imaging Observations of Solar Activity Cycle and Its Anomaly

    NASA Astrophysics Data System (ADS)

    Shibasaki, K.

    2011-12-01

    The 24th solar activity cycle has started and relative sunspot numbers are increasing. However, their rate of increase is rather slow compared to previous cycles. Active region sizes are small, lifetime is short, and big (X-class) flares are rare so far. We study this anomalous situation using data from Nobeyama Radioheliograph (NoRH). Radio imaging observations have been done by NoRH since 1992. Nearly 20 years of daily radio images of the Sun at 17 GHz are used to synthesize a radio butterfly diagram. Due to stable operation of the instrument and a robust calibration method, uniform datasets are available covering the whole period of observation. The radio butterfly diagram shows bright features corresponding to active region belts and their migration toward low latitude as the solar cycle progresses. In the present solar activity cycle (24), increase of radio brightness is delayed and slow. There are also bright features around both poles (polar brightening). Their brightness show solar cycle dependence but peaks around solar minimum. Comparison between the last minimum and the previous one shows decrease of its brightness. This corresponds to weakening of polar magnetic field activity between them. In the northern pole, polar brightening is already weakened in 2011, which means it is close to solar maximum in the northern hemisphere. Southern pole does not show such feature yet. Slow rise of activity in active region belt, weakening of polar activity during the minimum, and large north-south asymmetry in polar activity imply that global solar activity and its synchronization are weakening.

  8. [Correlations between functional activity of animal blood lymphocytes and change in solar activity].

    PubMed

    Karnaukhova, N A; Sergievich, L A

    1999-01-01

    It is shown that increase of Solar activity as measurement of the intensity of solar radio emissions at frequency of 2804 MHz leads to the reducing of the functional activity of immunocompetent cells in animal blood defining by parameter alpha.

  9. Evidence of active region imprints on the solar wind structure

    NASA Technical Reports Server (NTRS)

    Hick, P.; Jackson, B. V.

    1995-01-01

    A common descriptive framework for discussing the solar wind structure in the inner heliosphere uses the global magnetic field as a reference: low density, high velocity solar wind emanates from open magnetic fields, with high density, low speed solar wind flowing outward near the current sheet. In this picture, active regions, underlying closed magnetic field structures in the streamer belt, leave little or no imprint on the solar wind. We present evidence from interplanetary scintillation measurements of the 'disturbance factor' g that active regions play a role in modulating the solar wind and possibly contribute to the solar wind mass output. Hence we find that the traditional view of the solar wind, though useful in understanding many features of solar wind structure, is oversimplified and possibly neglects important aspects of solar wind dynamics

  10. Relationships between solar activity and climate change

    NASA Technical Reports Server (NTRS)

    Roberts, W. O.

    1975-01-01

    The relationship between recurrent droughts in the High Plains of the United States and the double sunspot cycle is discussed in detail. It is suggested that high solar activity is generally related to an increase in meridional circulation and blocking patterns at high and intermediate latitudes, especially in winter, and the effect is related to the sudden formation of cirrus clouds during strong geomagnetic activity that originates in the solar corpuscular emission.

  11. Predicting Solar Activity Using Machine-Learning Methods

    NASA Astrophysics Data System (ADS)

    Bobra, M.

    2017-12-01

    Of all the activity observed on the Sun, two of the most energetic events are flares and coronal mass ejections. However, we do not, as of yet, fully understand the physical mechanism that triggers solar eruptions. A machine-learning algorithm, which is favorable in cases where the amount of data is large, is one way to [1] empirically determine the signatures of this mechanism in solar image data and [2] use them to predict solar activity. In this talk, we discuss the application of various machine learning algorithms - specifically, a Support Vector Machine, a sparse linear regression (Lasso), and Convolutional Neural Network - to image data from the photosphere, chromosphere, transition region, and corona taken by instruments aboard the Solar Dynamics Observatory in order to predict solar activity on a variety of time scales. Such an approach may be useful since, at the present time, there are no physical models of flares available for real-time prediction. We discuss our results (Bobra and Couvidat, 2015; Bobra and Ilonidis, 2016; Jonas et al., 2017) as well as other attempts to predict flares using machine-learning (e.g. Ahmed et al., 2013; Nishizuka et al. 2017) and compare these results with the more traditional techniques used by the NOAA Space Weather Prediction Center (Crown, 2012). We also discuss some of the challenges in using machine-learning algorithms for space science applications.

  12. Influence of interplanetary magnetic field and solar wind on auroral brightness in different regions

    NASA Astrophysics Data System (ADS)

    Yang, Y. F.; Lu, J. Y.; Wang, J.-S.; Peng, Z.; Zhou, L.

    2013-01-01

    Abstract<p label="1">By integrating and averaging the auroral brightness from Polar Ultraviolet Imager auroral images, which have the whole auroral ovals, and combining the observation data of interplanetary magnetic field (IMF) and <span class="hlt">solar</span> wind from NASA Operating Missions as a Node on the Internet (OMNI), we investigate the <span class="hlt">influence</span> of IMF and <span class="hlt">solar</span> wind on auroral <span class="hlt">activities</span>, and analyze the separate roles of the <span class="hlt">solar</span> wind dynamic pressure, density, and velocity on aurora, respectively. We statistically analyze the relations between the interplanetary conditions and the auroral brightness in dawnside, dayside, duskside, and nightside. It is found that the three components of the IMF have different effects on the auroral brightness in the different regions. Different from the nightside auroral brightness, the dawnside, dayside, and duskside auroral brightness are affected by the IMF Bx, and By components more significantly. The IMF Bx and By components have different effects on these three regional auroral brightness under the opposite polarities of the IMF Bz. As expected, the nightside aurora is mainly affected by the IMF Bz, and under southward IMF, the larger the |Bz|, the brighter the nightside aurora. The IMF Bx and By components have no visible effects. On the other hand, it is also found that the aurora is not intensified singly with the increase of the <span class="hlt">solar</span> wind dynamic pressure: when only the dynamic pressure is high, but the <span class="hlt">solar</span> wind velocity is not very fast, the aurora will not necessarily be intensified significantly. These results can be used to qualitatively predict the auroral <span class="hlt">activities</span> in different regions for various interplanetary conditions.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2014cosp...40E1114G','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2014cosp...40E1114G"><span>What are the evidences of <span class="hlt">solar</span> <span class="hlt">activity</span> <span class="hlt">influence</span> on coronary heart disease?</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Gurfinkel, Yury; Breus, Tamara</p> <p></p> <p>Researches of last two decades have shown that the cardiovascular system represents the most probable target for <span class="hlt">influence</span> of helio - and geomagnetic <span class="hlt">activity</span>. Both cardiovascular system and blood connect very closely: one system cannot exist without another. For the same reason the effects perceived by one system, are easily transferred to another. Laboratory tests as blood coagulation, platelet aggregation, and capillary blood velocity performed in our hospital in patients suffering from coronary heart disease (CHD) revealed a high their dependence on a level of geomagnetic <span class="hlt">activity</span> (Gurfinkel et al., 1995, 1998). Later Gmitrov and Ohkubo (2002) in experiments on animals also found a significant negative correlation between geomagnetic field disturbances and capillary blood velocity. The analyzing data collected by the Moscow ambulance services covering more then one million observations over three years, cleaned up by seasonal effects of meteorological and social causes, showed that the number of cases of myocardial infarction increased during geomagnetic storms (Breus et al., 1995). During 14 years we collected more than 25000 cases of acute myocardial infarction and brain stroke at seven medical hospitals located in Russia, China and some other countries. We used only cases with established date of acute attack of diseases. Undated cases were excluded from the analysis. Average numbers of patients on geomagnetic <span class="hlt">active</span> days and days with quiet geomagnetic condition were compared. It was shown statistically that during geomagnetic disturbances the frequency of myocardial infarction and brain stroke cases increased on the average by a factor of two in comparison with quiet geomagnetic conditions. These results are close to results obtained by (Stoupel, 1999), for patients suffering with acute cardiological pathology. Our recent study (with L.Parfeonova) revealed the relation between heart ventricular ectopic <span class="hlt">activity</span> (VEA) and geomagnetic conditions in patients</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2010ERL.....5b1001B','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2010ERL.....5b1001B"><span>PERSPECTIVE: Low <span class="hlt">solar</span> <span class="hlt">activity</span> is blamed for winter chill over Europe</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Benestad, Rasmus E.</p> <p>2010-06-01</p> <p> the direct effect from changes in the <span class="hlt">solar</span> brightness (0.1%) was estimated to be too low to explain the temperature changes on Earth. The <span class="hlt">solar</span> <span class="hlt">influence</span> on changes in the global mean temperature has so far been found to be weak (Lean 2010, Benestad and Schmidt 2009). The important difference between recent and early studies is, however, that the latter lacked a theoretical framework based on physical mechanisms. Now we understand that stratospheric conditions vary, and are affected by chemical reactions as well as the absorption of UV light. Furthermore, we know that such variations affect temperature profiles, wave propagations, and winds (Schindell et al 2001). Lean (2010) and Haigh (2003) provide nice reviews of recent progress on <span class="hlt">solar</span>-terrestrial relationships, although questions regarding the quality of the oldest <span class="hlt">solar</span> data records are still unanswered (Benestad 2005). All these studies still rely on empirical data analysis. Much of the focus of the recent work has been on climate variation on global scales. The recent paper by Lockwood et al (2010) represents current progress, albeit that they emphasize that the relationship they identify has a regional rather than global character. Indeed, they stress that a change in the global mean temperature should not be confused with regional and seasonal means. The physical picture they provide is plausible, yet empirical relationships between <span class="hlt">solar</span> <span class="hlt">activity</span> and any of the indices describing the north Atlantic oscillation, the Arctic oscillation or the polar vortex are regarded as weak. My impression is nevertheless that the explanation provided by the Lockwood et al (2010) study reflects real aspects of our climate, especially if the effect is asymmetric. They argue that <span class="hlt">solar</span>-induced changes in the stratosphere in turn affect the occurrence of persistent wintertime blocking. But one comprehensive, definite, consistent, and convincing documentation of the entire chain causality is still not in place, due to the lack</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2018MS%26E..335a2029H','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2018MS%26E..335a2029H"><span><span class="hlt">Solar</span> Cell Polymer Based <span class="hlt">Active</span> Ingredients PPV and PCBM</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Hardeli, H.; Sanjaya, H.; Resikarnila, R.; Nitami H, R.</p> <p>2018-04-01</p> <p>A polymer <span class="hlt">solar</span> cell is a <span class="hlt">solar</span> cell based on a polymer bulk heterojunction structure using the method of thin film, which can convert <span class="hlt">solar</span> energy into electrical energy. Absorption of light is carried by <span class="hlt">active</span> material layer PPV: PCBM. This study aims to make <span class="hlt">solar</span> cells tandem and know the value of converting <span class="hlt">solar</span> energy into electrical energy and increase the value of efficiency generated through morphological control, ie annealing temperature and the ratio of <span class="hlt">active</span> layer mixture. The <span class="hlt">active</span> layer is positioned above the PEDOT:PSS layer on ITO glass substrate. The characterization results show the surface morphology of the PPV:PCBM <span class="hlt">active</span> layer is quite evenly at annealing temperature of 165 ° C. The result of conversion of electrical energy with a UV light source in annealing samples with temperature 165 ° C is 0.03 mA and voltage of 4.085 V with an efficiency of 2.61% and mixed ratio variation was obtained in comparison of P3HT: PCBM is 1: 3</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017JGRA..12210796S','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017JGRA..12210796S"><span>Characteristics of Seasonal Variation and <span class="hlt">Solar</span> <span class="hlt">Activity</span> Dependence of the Geomagnetic <span class="hlt">Solar</span> Quiet Daily Variation</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Shinbori, Atsuki; Koyama, Yukinobu; Nosé, Masahito; Hori, Tomoaki; Otsuka, Yuichi</p> <p>2017-10-01</p> <p>Characteristics of seasonal variation and <span class="hlt">solar</span> <span class="hlt">activity</span> dependence of the X and Y components of the geomagnetic <span class="hlt">solar</span> quiet (Sq) daily variation at Memambetsu in midlatitudes and Guam near the equator have been investigated using long-term geomagnetic field data with 1 h time resolution from 1957 to 2016. The monthly mean Sq variation in the X and Y components (Sq-X and Sq-Y) shows a clear seasonal variation and <span class="hlt">solar</span> <span class="hlt">activity</span> dependence. The amplitude of seasonal variation increases significantly during high <span class="hlt">solar</span> <span class="hlt">activities</span> and is proportional to the <span class="hlt">solar</span> F10.7 index. The pattern of the seasonal variation is quite different between Sq-X and Sq-Y. The result of the correlation analysis between the <span class="hlt">solar</span> F10.7 index and the Sq-X and Sq-Y shows an almost linear relationship, but the slope of the linear fitted line varies as a function of local time and month. This implies that the sensitivity of Sq-X and Sq-Y to the <span class="hlt">solar</span> <span class="hlt">activity</span> is different for different local times and seasons. The pattern of the local time and seasonal variations of Sq-Y at Guam shows good agreement with that of a magnetic field produced by interhemispheric field-aligned currents (FACs), which flow from the summer to winter hemispheres in the dawn and dusk sectors and from the winter to summer hemispheres in the prenoon to afternoon sectors. The direction of the interhemispheric FAC in the dusk sector is opposite to the concept of Fukushima's model.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2018PhPl...25d2901E','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2018PhPl...25d2901E"><span>A study of the asymmetrical distribution of <span class="hlt">solar</span> <span class="hlt">activity</span> features on <span class="hlt">solar</span> and plasma parameters (1967-2016)</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>El-Borie, M. A.; El-Taher, A. M.; Aly, N. E.; Bishara, A. A.</p> <p>2018-04-01</p> <p>The impact of asymmetrical distribution of hemispheric sunspot areas (SSAs) on the interplanetary magnetic field, plasma, and <span class="hlt">solar</span> parameters from 1967 to 2016 has been studied. The N-S asymmetry of <span class="hlt">solar</span>-plasma <span class="hlt">activities</span> based on SSAs has a northern dominance during <span class="hlt">solar</span> cycles 20 and 24. However, it has a tendency to shift to the southern hemisphere in cycles 21, 22, and 23. The <span class="hlt">solar</span> cycle 23 showed that the sorted southern SSAs days predominated over the northern days by ˜17%. Through the <span class="hlt">solar</span> cycles 21-24, the SSAs of the southern hemisphere were more <span class="hlt">active</span>. In contrast, the northern SSAs predominate over the southern one by 9% throughout <span class="hlt">solar</span> cycle 20. On the other hand, the average differences of field magnitude for the sorted northern and southern groups during <span class="hlt">solar</span> cycles 20-24 are statistically insignificant. Clearly, twenty years showed that the <span class="hlt">solar</span> plasma ion density from the sorted northern group was denser than that of southern group and a highest northern dominant peak occurred in 1971. In contrast, seventeen out of fifty years showed the reverse. In addition, there are fifteen clear asymmetries of <span class="hlt">solar</span> wind speed (SWS), with SWS (N) > SWS (S), and during the years 1972, 2002, and 2008, the SWS from the sorted northern group was faster than that of southern <span class="hlt">activity</span> group by 6.16 ± 0.65 km/s, 5.70 ± 0.86 km/s, and 5.76 ± 1.35 km/s, respectively. For the <span class="hlt">solar</span> cycles 20-24, the grand-averages of P from the sorted <span class="hlt">solar</span> northern and southern have nearly the same parameter values. The <span class="hlt">solar</span> plasma was hotter for the sorted northern <span class="hlt">activity</span> group than the southern ones for 17 years out of 50. Most significant northern prevalent asymmetries were found in 1972 (5.76 ± 0.66 × 103 K) and 1996 (4.7 ± 0.8 × 103 K), while two significant equivalent dominant southern asymmetries (˜3.8 ± 0.3 × 103 K) occurred in 1978 and 1993. The grand averages of sunspot numbers have symmetric <span class="hlt">activity</span> for the two sorted northern and southern hemispheres</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2010AIPC.1295..251B','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2010AIPC.1295..251B"><span>Low Latitude Aurora: Index of <span class="hlt">Solar</span> <span class="hlt">Activity</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Bekli, M. R.; Aissani, D.; Chadou, I.</p> <p>2010-10-01</p> <p>Observations of aurora borealis at low latitudes are rare, and are clearly associated with high <span class="hlt">solar</span> <span class="hlt">activity</span>. In this paper, we analyze some details of the <span class="hlt">solar</span> <span class="hlt">activity</span> during the years 1769-1792. Moreover, we describe in detail three low latitude auroras. The first event was reported by ash-Shalati and observed in North Africa (1770 AD). The second and third events were reported by l'Abbé Mann and observed in Europe (1770 and 1777 AD).</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2013JASTP..98...12P','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2013JASTP..98...12P"><span>The relationship between thunderstorm and <span class="hlt">solar</span> <span class="hlt">activity</span> for Brazil from 1951 to 2009</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Pinto Neto, Osmar; Pinto, Iara R. C. A.; Pinto, Osmar</p> <p>2013-06-01</p> <p>The goal of this article is to investigate the <span class="hlt">influence</span> of <span class="hlt">solar</span> <span class="hlt">activity</span> on thunderstorm <span class="hlt">activity</span> in Brazil. For this purpose, thunder day data from seven cities in Brazil from 1951 to 2009 are analyzed with the wavelet method for the first time. To identify the 11-year <span class="hlt">solar</span> cycle in thunder day data, a new quantity is defined. It is named TD1 and represents the power in 1-year in a wavelet spectrum of monthly thunder day data. The wavelet analysis of TD1 values shows more clear the 11-year periodicity than when it is applied directly to annual thunder day data, as it has been normally investigated in the literature. The use of this new quantity is shown to enhance the capability to identify the 11-year periodicity in thunderstorm data. Wavelet analysis of TD1 indicates that six out seven cities investigated exhibit periodicities near 11 years, three of them significant at a 1% significance level (p<0.01). Furthermore, wavelet coherence analysis demonstrated that the 11-year periodicity of TD1 and <span class="hlt">solar</span> <span class="hlt">activity</span> are correlated with an anti-phase behavior, three of them (the same cities with periodicities with 1% significance level) significant at a 5% significance level (p<0.05). The results are compared with those obtained from the same data set but using annual thunder day data. Finally, the results are compared with previous results obtained for other regions and a discussion about possible mechanisms to explain them is done. The existence of periodicities around 11 years in six out of seven cities and their anti-phase behavior with respect to 11-year <span class="hlt">solar</span> cycle suggest a global mechanism probably related to a <span class="hlt">solar</span> magnetic shielding effect acting on galactic cosmic rays as an explanation for the relationship of thunderstorm and <span class="hlt">solar</span> <span class="hlt">activity</span>, although more studies are necessary to clarify its physical origin.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/1992AAS...180.4204V','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/1992AAS...180.4204V"><span>The Structure of <span class="hlt">Solar</span> <span class="hlt">Active</span> Regions</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Vourlidas, A.; Bastian, T. S.</p> <p>1992-05-01</p> <p>In past years, x-ray observations of <span class="hlt">solar</span> <span class="hlt">active</span> regions have lead to the expectation of greater brightness temperatures at radio wavelengths than those typically observed. It has been suggested that cool plasma in the corona along the line of sight attenuates radio emission via free-free absorption. If such plasma is present, it has consequences for both the microwave spectrum and its polarization properties. In order to test these ideas, high quality radio and x-ray maps are required. We present a comprehensive set of observations of a large <span class="hlt">solar</span> <span class="hlt">active</span> region (NOAO/USAF number 5131) made during the IAU sanctioned International <span class="hlt">Solar</span> Month in September, 1988. The VLA was used to image the Sun in the 90, 20, 6 and 3.6 cm bands between 1--4 September. To improve the image quality we used the technique of frequency synthesis at 3.6, 6 and 20 cm. The final maps are among the best in dynamic range yet obtained. In addition to the radio maps, the data base includes images from the SMM XRP in Fe XVII, magnetograms, and Hα observations. We reconcile the x-ray and radio observations with a simple model which differs somewhat from past models. Rather than relying on a screen of cool plasma between the source and the observer, we take explicit account of the highly inhomogeneous structure of <span class="hlt">solar</span> <span class="hlt">active</span> regions. We briefly compare and contrast the consequences of this model with existing models.</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('https://www.ncbi.nlm.nih.gov/pubmed/28856184','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/28856184"><span>Data on the detail information of <span class="hlt">influence</span> of substrate temperature on the film morphology and photovoltaic performance of non-fullerene organic <span class="hlt">solar</span> cells.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Zhang, Jicheng; Xie, SuFei; Lu, Zhen; Wu, Yang; Xiao, Hongmei; Zhang, Xuejuan; Li, Guangwu; Li, Cuihong; Chen, Xuebo; Ma, Wei; Bo, Zhishan</p> <p>2017-10-01</p> <p>This data contains additional data related to the article "<span class="hlt">Influence</span> of Substrate Temperature on the Film Morphology and Photovoltaic Performance of Non-fullerene Organic <span class="hlt">Solar</span> Cells" (Jicheng Zhang et al., In press) [1]. Data include measurement and characterization instruments and condition, detail condition to fabricate norfullerene <span class="hlt">solar</span> cell devices, hole-only and electron-only devices. Detail condition about how to control the film morphology of devices via tuning the temperature of substrates was also displayed. More information and more convincing data about the change of film morphology for <span class="hlt">active</span> layers fabricated from different temperature, which is attached to the research article of "<span class="hlt">Influence</span> of Substrate Temperature on the Film Morphology and Photovoltaic Performance of Non-fullerene Organic <span class="hlt">Solar</span> Cells" was given.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.osti.gov/pages/biblio/1260817-do-solar-cycles-influence-giant-cell-arteritis-rheumatoid-arthritis-incidence','SCIGOV-DOEP'); return false;" href="https://www.osti.gov/pages/biblio/1260817-do-solar-cycles-influence-giant-cell-arteritis-rheumatoid-arthritis-incidence"><span>Do <span class="hlt">solar</span> cycles <span class="hlt">influence</span> giant cell arteritis and rheumatoid arthritis incidence?</span></a></p> <p><a target="_blank" href="http://www.osti.gov/pages">DOE PAGES</a></p> <p>Wing, Simon; Rider, Lisa G.; Johnson, Jay R.; ...</p> <p>2015-05-15</p> <p>Our objective was to examine the <span class="hlt">influence</span> of <span class="hlt">solar</span> cycle and geomagnetic effects on the incidence of giant cell arteritis (GCA) and rheumatoid arthritis (RA). Methods: We used data from patients with GCA (1950-2004) and RA (1955-2007) obtained from population-based cohorts. Yearly trends in age-adjusted and sex-adjusted incidence were correlated with the F10.7 index (<span class="hlt">solar</span> radiation at 10.7 cm wavelength, a proxy for the <span class="hlt">solar</span> extreme ultraviolet radiation) and AL index (a proxy for the westward auroral electrojet and a measure of geomagnetic <span class="hlt">activity</span>). Fourier analysis was performed on AL, F10.7, and GCA and RA incidence rates. Results: The correlationmore » of GCA incidence with AL is highly significant: GCA incidence peaks 0-1 year after the AL reaches its minimum (ie, auroral electrojet reaches a maximum). The correlation of RA incidence with AL is also highly significant. RA incidence rates are lowest 5-7 years after AL reaches maximum. AL, GCA and RA incidence power spectra are similar: they have a main peak (periodicity) at about 10 years and a minor peak at 4-5 years. However, the RA incidence power spectrum main peak is broader (8-11 years), which partly explains the lower correlation between RA onset and AL. The auroral electrojets may be linked to the decline of RA incidence more strongly than the onset of RA. The incidences of RA and GCA are aligned in geomagnetic latitude. Conclusions: AL and the incidences of GCA and RA all have a major periodicity of about 10 years and a secondary periodicity at 4-5 years. Geomagnetic <span class="hlt">activity</span> may explain the temporal and spatial variations, including east-west skewness in geographic coordinates, in GCA and RA incidence, although the mechanism is unknown. Lastly, the link with <span class="hlt">solar</span>, geospace and atmospheric parameters need to be investigated. These novel findings warrant examination in other populations and with other autoimmune diseases.« less</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=4442155','PMC'); return false;" href="https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=4442155"><span>Do <span class="hlt">solar</span> cycles <span class="hlt">influence</span> giant cell arteritis and rheumatoid arthritis incidence?</span></a></p> <p><a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pmc">PubMed Central</a></p> <p>Wing, Simon; Rider, Lisa G; Johnson, Jay R; Miller, Federick W; Matteson, Eric L; Gabriel, Sherine E</p> <p>2015-01-01</p> <p>Objective To examine the <span class="hlt">influence</span> of <span class="hlt">solar</span> cycle and geomagnetic effects on the incidence of giant cell arteritis (GCA) and rheumatoid arthritis (RA). Methods We used data from patients with GCA (1950–2004) and RA (1955–2007) obtained from population-based cohorts. Yearly trends in age-adjusted and sex-adjusted incidence were correlated with the F10.7 index (<span class="hlt">solar</span> radiation at 10.7 cm wavelength, a proxy for the <span class="hlt">solar</span> extreme ultraviolet radiation) and AL index (a proxy for the westward auroral electrojet and a measure of geomagnetic <span class="hlt">activity</span>). Fourier analysis was performed on AL, F10.7, and GCA and RA incidence rates. Results The correlation of GCA incidence with AL is highly significant: GCA incidence peaks 0–1 year after the AL reaches its minimum (ie, auroral electrojet reaches a maximum). The correlation of RA incidence with AL is also highly significant. RA incidence rates are lowest 5–7 years after AL reaches maximum. AL, GCA and RA incidence power spectra are similar: they have a main peak (periodicity) at about 10 years and a minor peak at 4–5 years. However, the RA incidence power spectrum main peak is broader (8–11 years), which partly explains the lower correlation between RA onset and AL. The auroral electrojets may be linked to the decline of RA incidence more strongly than the onset of RA. The incidences of RA and GCA are aligned in geomagnetic latitude. Conclusions AL and the incidences of GCA and RA all have a major periodicity of about 10 years and a secondary periodicity at 4–5 years. Geomagnetic <span class="hlt">activity</span> may explain the temporal and spatial variations, including east-west skewness in geographic coordinates, in GCA and RA incidence, although the mechanism is unknown. The link with <span class="hlt">solar</span>, geospace and atmospheric parameters need to be investigated. These novel findings warrant examination in other populations and with other autoimmune diseases. PMID:25979866</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.osti.gov/servlets/purl/1260817','SCIGOV-STC'); return false;" href="https://www.osti.gov/servlets/purl/1260817"><span>Do <span class="hlt">solar</span> cycles <span class="hlt">influence</span> giant cell arteritis and rheumatoid arthritis incidence?</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>Wing, Simon; Rider, Lisa G.; Johnson, Jay R.</p> <p></p> <p>Our objective was to examine the <span class="hlt">influence</span> of <span class="hlt">solar</span> cycle and geomagnetic effects on the incidence of giant cell arteritis (GCA) and rheumatoid arthritis (RA). Methods: We used data from patients with GCA (1950-2004) and RA (1955-2007) obtained from population-based cohorts. Yearly trends in age-adjusted and sex-adjusted incidence were correlated with the F10.7 index (<span class="hlt">solar</span> radiation at 10.7 cm wavelength, a proxy for the <span class="hlt">solar</span> extreme ultraviolet radiation) and AL index (a proxy for the westward auroral electrojet and a measure of geomagnetic <span class="hlt">activity</span>). Fourier analysis was performed on AL, F10.7, and GCA and RA incidence rates. Results: The correlationmore » of GCA incidence with AL is highly significant: GCA incidence peaks 0-1 year after the AL reaches its minimum (ie, auroral electrojet reaches a maximum). The correlation of RA incidence with AL is also highly significant. RA incidence rates are lowest 5-7 years after AL reaches maximum. AL, GCA and RA incidence power spectra are similar: they have a main peak (periodicity) at about 10 years and a minor peak at 4-5 years. However, the RA incidence power spectrum main peak is broader (8-11 years), which partly explains the lower correlation between RA onset and AL. The auroral electrojets may be linked to the decline of RA incidence more strongly than the onset of RA. The incidences of RA and GCA are aligned in geomagnetic latitude. Conclusions: AL and the incidences of GCA and RA all have a major periodicity of about 10 years and a secondary periodicity at 4-5 years. Geomagnetic <span class="hlt">activity</span> may explain the temporal and spatial variations, including east-west skewness in geographic coordinates, in GCA and RA incidence, although the mechanism is unknown. Lastly, the link with <span class="hlt">solar</span>, geospace and atmospheric parameters need to be investigated. These novel findings warrant examination in other populations and with other autoimmune diseases.« less</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/20120009855','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/20120009855"><span>The Magnetic Origins of <span class="hlt">Solar</span> <span class="hlt">Activity</span></span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Antiochos, S. K.</p> <p>2012-01-01</p> <p>The defining physical property of the Sun's corona is that the magnetic field dominates the plasma. This property is the genesis for all <span class="hlt">solar</span> <span class="hlt">activity</span> ranging from quasi-steady coronal loops to the giant magnetic explosions observed as coronal mass ejections/eruptive flares. The coronal magnetic field is also the fundamental driver of all space weather; consequently, understanding the structure and dynamics of the field, especially its free energy, has long been a central objective in Heliophysics. The main obstacle to achieving this understanding has been the lack of accurate direct measurements of the coronal field. Most attempts to determine the magnetic free energy have relied on extrapolation of photospheric measurements, a notoriously unreliable procedure. In this presentation I will discuss what measurements of the coronal field would be most effective for understanding <span class="hlt">solar</span> <span class="hlt">activity</span>. Not surprisingly, the key process for driving <span class="hlt">solar</span> <span class="hlt">activity</span> is magnetic reconnection. I will discuss, therefore, how next-generation measurements of the coronal field will allow us to understand not only the origins of space weather, but also one of the most important fundamental processes in cosmic and laboratory plasmas.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/19750022914','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/19750022914"><span>The <span class="hlt">solar</span> atmosphere and the structure of <span class="hlt">active</span> regions. [aircraft accidents, weather</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Sturrock, P. A.</p> <p>1975-01-01</p> <p>Numerical analyses of <span class="hlt">solar</span> <span class="hlt">activities</span> are presented. The effect of these <span class="hlt">activities</span> on aircraft and weather conditions was studied. Topics considered are: (1) <span class="hlt">solar</span> flares; (2) <span class="hlt">solar</span> X-rays; and (3) <span class="hlt">solar</span> magnetic fields (charts are shown).</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://ntrs.nasa.gov/search.jsp?R=19760044011&hterms=activity+Physics&qs=N%3D0%26Ntk%3DAll%26Ntx%3Dmode%2Bmatchall%26Ntt%3Dactivity%2BPhysics','NASA-TRS'); return false;" href="https://ntrs.nasa.gov/search.jsp?R=19760044011&hterms=activity+Physics&qs=N%3D0%26Ntk%3DAll%26Ntx%3Dmode%2Bmatchall%26Ntt%3Dactivity%2BPhysics"><span>Recent perspectives in <span class="hlt">solar</span> physics - Elemental composition, coronal structure and magnetic fields, <span class="hlt">solar</span> <span class="hlt">activity</span></span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Newkirk, G., Jr.</p> <p>1975-01-01</p> <p>Elemental abundances in the <span class="hlt">solar</span> corona are studied. Abundances in the corona, <span class="hlt">solar</span> wind and <span class="hlt">solar</span> cosmic rays are compared to those in the photosphere. The variation in silicon and iron abundance in the <span class="hlt">solar</span> wind as compared to helium is studied. The coronal small and large scale structure is investigated, emphasizing magnetic field <span class="hlt">activity</span> and examining cosmic ray generation mechanisms. The corona is observed in the X-ray and EUV regions. The nature of coronal transients is discussed with emphasis on <span class="hlt">solar</span>-wind modulation of galactic cosmic rays. A schematic plan view of the interplanetary magnetic field during sunspot minimum is given showing the presence of magnetic bubbles and their concentration in the region around 4-5 AU by a fast <span class="hlt">solar</span> wind stream.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2012EGUGA..14.5513O','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2012EGUGA..14.5513O"><span>Towards understanding the nature of any relationship between <span class="hlt">Solar</span> <span class="hlt">Activity</span> and Cosmic Rays with thunderstorm <span class="hlt">activity</span> and lightning discharge</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>O'Regan, J.; Muller, J.-P.; Matthews, S.</p> <p>2012-04-01</p> <p> both sign and significance over small geographic distances, similar to previous results [3,4,6], highlighting the complexity of the atmospheric processes contributing to the mechanism of thunderstorm generation and lightning discharge. We find correlations are generally more significant over larger timescales, as daily meteorological variability is smoothened out, suggesting a role for changing <span class="hlt">Solar</span> <span class="hlt">activity</span> levels in <span class="hlt">influencing</span> thunderstorm development and onset of lightning discharge. Comparisons of small-scale correlation results to planetary wave patterns suggests an <span class="hlt">influence</span> over the correlations of lightning <span class="hlt">activity</span> to the above indices, as proposed by Schlegel et al. [6], and previously suggested by the results of Fritz [3] and Brooks [4]. Our results show agreement with Schlegel et al. [6] for the same region over Germany, but are in disagreement with their results for Austria. This lends support to the idea of the theory of planetary waves <span class="hlt">influence</span> over correlation signs and significance across short geographic distances, as discussed by Schlegel et al. [6]. Acknowledgement: The authors wish to thank the World Wide Lightning Location Network (http://wwlln.net), a collaboration among over 50 universities and institutions (including MSSL) for providing the lightning location data used in this paper. [1] Ermakov, V.I. and Stozhkov, Yu.I., 2003. Cosmic rays in the mechanism of thundercloud production. 28th International Cosmic Ray Conference, pp. 4157-4160. [2] Kirkby, J., 2007. Cosmic rays and climate. Surv Geophys, vol. 28 (5-6) pp. 333-375. [3] Fritz, H., 1878. Die wichtigsten periodischen Erscheinungen der Meteorologie und Kosmologie. Natuurkundige Verhandelingen van de Hollandsche Maatschappij der Wetenschappen te Haarlem, Deel III, Haarlem. [4] Brooks, C.E.P., 1934. The variation of the annual frequency of thunderstorms in relation to sunspots. Quarterly Journal of the Royal Meteorological Society 60, 153-165. [5] Stringfellow, M.F., 1974. Lightning</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017RaSc...52.1253W','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017RaSc...52.1253W"><span>Temperature Distribution and <span class="hlt">Influence</span> Mechanism on Large Reflector Antennas under <span class="hlt">Solar</span> Radiation</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Wang, C. S.; Yuan, S.; Liu, X.; Xu, Q.; Wang, M.; Zhu, M. B.; Chen, G. D.; Duan, Y. H.</p> <p>2017-10-01</p> <p>The <span class="hlt">solar</span> impact on antenna must be lessened for the large reflector antenna operating at high frequencies to have great electromagnetic performances. Therefore, researching the temperature distribution and its <span class="hlt">influence</span> on large reflector antenna is necessary. The variation of <span class="hlt">solar</span> incidence angle is first calculated. Then the model is simulated by the I-DEAS software, with the temperature, thermal stress, and thermal distortion distribution through the day obtained. In view of the important <span class="hlt">influence</span> of shadow on antenna structure, a newly proposed method makes a comprehensive description of the temperature distribution on the reflector and its <span class="hlt">influence</span> through the day by dividing a day into three different periods. The sound discussions and beneficial summary serve as the scientific foundation for the engineers to compensate the thermal distortion and optimize the antenna structure.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/12653182','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/12653182"><span>Is motivation <span class="hlt">influenced</span> by geomagnetic <span class="hlt">activity</span>?</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Starbuck, S; Cornélissen, G; Halberg, F</p> <p>2002-01-01</p> <p>To eventually build a scientific bridge to religion by examining whether non-photic, non-thermic <span class="hlt">solar</span> effects may <span class="hlt">influence</span> (religious) motivation, invaluable yearly world wide data on <span class="hlt">activities</span> from 1950 to 1999 by Jehovah's Witnesses on behalf of their church were analyzed chronobiologically. The time structure (chronome) of these archives, insofar as it is able to be evaluated in yearly means for up to half a century, was assessed. Least squares spectra in a frequency range from one cycle in 42 to one in 2.1 years of data on the average number of hours per month spent in work for the church, available from 103 different geographic locations, as well as grand totals also including other sites, revealed a large peak at one cycle in about 21 years. The non-linear least squares fit of a model consisting of a linear trend and a cosine curve with a trial period of 21.0 years, numerically approximating that of the Hale cycle, validated the about 21.0-year component in about 70% of the data series, with the non-overlap of zero by the 95% confidence interval of the amplitude estimate. Estimates of MESOR (midline-estimating statistic of rhythm, a rhythm (or chronome) adjusted mean), amplitude and period were further regressed with geomagnetic latitude. The period estimate did not depend on geomagnetic latitude. The about 21.0-year amplitude tends to be larger at low and middle than at higher latitudes and the resolution of the about 21.0-year cycle, gauged by the width of 95% confidence intervals for the period and amplitude, is higher (the 95% confidence intervals are statistically significantly smaller) at higher than at lower latitudes. Near-matches of periods in <span class="hlt">solar</span> <span class="hlt">activity</span> and human motivation hint that the former may <span class="hlt">influence</span> the latter, while the dependence on latitude constitutes evidence that geomagnetic <span class="hlt">activity</span> may affect certain brain areas involved in motivation, just as it was earlier found that it is associated with effects on the electrocardiogram</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2015EGUGA..17.9902C','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2015EGUGA..17.9902C"><span>Testing the potential of 10Be in varved sediments from two lakes for <span class="hlt">solar</span> <span class="hlt">activity</span> reconstruction</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Czymzik, Markus; Muscheler, Raimund; Brauer, Achim; Adolphi, Florian; Ott, Florian; Kienel, Ulrike; Dräger, Nadine; Slowinski, Michal; Aldahan, Ala; Possnert, Göran</p> <p>2015-04-01</p> <p>The potential of 10Be in annually laminated (varved) lake sediments for <span class="hlt">solar</span> <span class="hlt">activity</span> reconstruction is, to date, largely unexplored. It is hypothesized that 10Be contents in sediments from well-chosen lakes reflect the <span class="hlt">solar</span> induced atmospheric production signal. The varved nature of these archives provides the chance to establish <span class="hlt">solar</span> <span class="hlt">activity</span> time-series with very high temporal precision. However, so far <span class="hlt">solar</span> <span class="hlt">activity</span> reconstruction from 10Be in varved lake sediments is hampered due to a lack of detailed knowledge of the process chain from production in the atmosphere to deposition on the lake floor. Calibrating 10Be time-series from varved lake sediments against complementary proxy records from the same sediment archive as well as instrumental meteorological and <span class="hlt">solar</span> <span class="hlt">activity</span> data will allow a process-based understanding of 10Be deposition in these lakes and a quantitative evaluation of their potential for <span class="hlt">solar</span> <span class="hlt">activity</span> reconstruction. 10Be concentration and flux time-series at annual resolution were constructed for the period 1983 to 2007 (approx. <span class="hlt">solar</span> cycles 22 and 23) conducting accelerator mass spectrometry and varve chronology on varved sediments of Lakes Tiefer See and Czechowski, located on an east-west transect at a distance of about 450 km in the lowlands of northern-central Europe. 10Be concentrations vary between 0.9 and 1.8*108atoms/g, with a mean of 1.3*108atoms/g in Lake Tiefer See and between 0.6 and 1.6*108atoms/g, with a mean of 1*108atoms/g in Lake Czechowski. Calculated mean 10Be flux is 2.3*108atoms/cm2/year for Lake Tiefer See and 0.7*108atoms/cm2/year for Lake Czechowski. Calibrating the 10Be time-series against corresponding geochemical μ-XRF profiles, varve thickness and total organic carbon records as well as precipitation data from the nearby stations Schwerin for Lake Tiefer See and Koscierzyna for Lake Czechowski and a neutron monitor record of <span class="hlt">solar</span> <span class="hlt">activity</span> suggests (1) a complex interaction of varying processes <span class="hlt">influencing</span></p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2018JAP...123e5705A','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2018JAP...123e5705A"><span>Recombination <span class="hlt">activity</span> of grain boundaries in high-performance multicrystalline Si during <span class="hlt">solar</span> cell processing</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Adamczyk, Krzysztof; Søndenâ, Rune; Stokkan, Gaute; Looney, Erin; Jensen, Mallory; Lai, Barry; Rinio, Markus; Di Sabatino, Marisa</p> <p>2018-02-01</p> <p>In this work, we applied internal quantum efficiency mapping to study the recombination <span class="hlt">activity</span> of grain boundaries in High Performance Multicrystalline Silicon under different processing conditions. Wafers were divided into groups and underwent different thermal processing, consisting of phosphorus diffusion gettering and surface passivation with hydrogen rich layers. After these thermal treatments, wafers were processed into heterojunction with intrinsic thin layer <span class="hlt">solar</span> cells. Light Beam Induced Current and Electron Backscatter Diffraction were applied to analyse the <span class="hlt">influence</span> of thermal treatment during standard <span class="hlt">solar</span> cell processing on different types of grain boundaries. The results show that after cell processing, most random-angle grain boundaries in the material are well passivated, but small-angle grain boundaries are not well passivated. Special cases of coincidence site lattice grain boundaries with high recombination <span class="hlt">activity</span> are also found. Based on micro-X-ray fluorescence measurements, a change in the contamination level is suggested as the reason behind their increased <span class="hlt">activity</span>.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://ntrs.nasa.gov/search.jsp?R=19800010203&hterms=xie&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAuthor-Name%26Nf%3DPublication-Date%257CLT%2B20031231%26N%3D0%26No%3D60%26Ntt%3Dxie','NASA-TRS'); return false;" href="https://ntrs.nasa.gov/search.jsp?R=19800010203&hterms=xie&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAuthor-Name%26Nf%3DPublication-Date%257CLT%2B20031231%26N%3D0%26No%3D60%26Ntt%3Dxie"><span>Short-term <span class="hlt">solar</span> <span class="hlt">activity</span> forecasting</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Xie-Zhen, C.; Ai-Di, Z.</p> <p>1979-01-01</p> <p>A method of forecasting the level of <span class="hlt">activity</span> of every <span class="hlt">active</span> region on the surface of the Sun within one to three days is proposed in order to estimate the possibility of the occurrence of ionospheric disturbances and proton events. The forecasting method is a probability process based on statistics. In many of the cases, the accuracy in predicting the short term <span class="hlt">solar</span> <span class="hlt">activity</span> was in the range of 70%, although there were many false alarms.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/20170012221','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/20170012221"><span>Building Reliable Forecasts of <span class="hlt">Solar</span> <span class="hlt">Activity</span></span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Kitiashvili, Irina; Wray, Alan; Mansour, Nagi</p> <p>2017-01-01</p> <p><span class="hlt">Solar</span> ionizing radiation critically depends on the level of the Sun’s magnetic <span class="hlt">activity</span>. For robust physics-based forecasts, we employ the procedure of data assimilation, which combines theoretical modeling and observational data such that uncertainties in both the model and the observations are taken into account. Currently we are working in two major directions: 1) development of a new long-term forecast procedure on time-scales of the 11-year <span class="hlt">solar</span> cycle, using a 2-dimensional mean-field dynamo model and synoptic magnetograms; 2) development of 3-dimensional radiative MHD (Magnetohydrodynamic) simulations to investigate the origin and precursors of local manifestations of magnetic <span class="hlt">activity</span>, such as the formation of magnetic structures and eruptive dynamics.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2014EGUGA..16.2614P','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2014EGUGA..16.2614P"><span>The Impact of Level of <span class="hlt">Solar</span> <span class="hlt">Activity</span> on Mortality by Cause in Longtime Period</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Podolska, Katerina</p> <p>2014-05-01</p> <p>The aim of this presentation is to show the dependence of the intensity of mortality in the Czech Republic, according to the chosen causes of death according to ICD-10, on the <span class="hlt">solar</span> <span class="hlt">activity</span> during the increasing and decreasing phase of the <span class="hlt">solar</span> cycle No.23 in the period 1994-2011. We use the methods of multivariate statistical analysis. The typology of time profiles for the causes of death is identified with the help of cluster analysis using time. The <span class="hlt">solar</span> <span class="hlt">activity</span> is represented by the indices R, Kp, F10.7 and Dst, and also by the height of the F2 layer and TEC for the Czech Republic. There are investigated groups of causes of death according to ICD-10 II. Neoplasms, VI. Diseases of the nervous system, XII. Diseases of the skin and subcutaneous tissue and XVII. Congenital malformations, deformations and chromosomal abnormalities. The correlation between the intensity of mortality from cardiovascular disease e.g. I21 (acute myocardial infarction) and I64 (stroke) and birth defect e.g. Q91 (Edwards' and Pataus' syndrom) and the <span class="hlt">solar</span> <span class="hlt">activity</span> parameters is discovered, as well as a stronger dependence on the height of the F2 layer and TEC. We also explored the <span class="hlt">influence</span> of the above parameters on mortality by causes on degenerative diseases. Typology of time profiles for these causes of death are identified by cluster analysis using time and have found large differences between diagnoses.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2014SoPh..289..579G','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2014SoPh..289..579G"><span>Migration and Extension of <span class="hlt">Solar</span> <span class="hlt">Active</span> Longitudinal Zones</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Gyenge, N.; Baranyi, T.; Ludmány, A.</p> <p>2014-02-01</p> <p><span class="hlt">Solar</span> <span class="hlt">active</span> longitudes show a characteristic migration pattern in the Carrington coordinate system if they can be identified at all. By following this migration, the longitudinal <span class="hlt">activity</span> distribution around the center of the band can be determined. The half-width of the distribution is found to be varying in Cycles 21 - 23, and in some time intervals it was as narrow as 20 - 30 degrees. It was more extended around a maximum but it was also narrow when the <span class="hlt">activity</span> jumped to the opposite longitude. Flux emergence exhibited a quasi-periodic variation within the <span class="hlt">active</span> zone with a period of about 1.3 years. The path of the <span class="hlt">active</span>-longitude migration does not support the view that it might be associated with the 11-year <span class="hlt">solar</span> cycle. These results were obtained for a limited time interval of a few <span class="hlt">solar</span> cycles and, bearing in mind uncertainties of the migration-path definition, are only indicative. For the major fraction of the dataset no systematic <span class="hlt">active</span> longitudes were found. Sporadic migration of <span class="hlt">active</span> longitudes was identified only for Cycles 21 - 22 in the northern hemisphere and Cycle 23 in the southern hemisphere.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/19780015051','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/19780015051"><span><span class="hlt">Solar</span> <span class="hlt">activity</span> during Skylab: Its distribution and relation to coronal holes</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Speich, D. M.; Smith, J. B., Jr.; Wilson, R. M.; Mcintosh, P. S.</p> <p>1978-01-01</p> <p><span class="hlt">Solar</span> <span class="hlt">active</span> regions observed during the period of Skylab observations (May 1973-February 1974) were examined for properties that varied systematically with location on the sun, particularly with respect to the location of coronal holes. Approximately 90 percent of the optical and X-ray flare <span class="hlt">activity</span> occurred in one <span class="hlt">solar</span> hemisphere (136-315 heliographic degrees longitude). <span class="hlt">Active</span> regions within 20 heliographic degrees of coronal holes were below average in lifetimes, flare production, and magnetic complexity. Histograms of <span class="hlt">solar</span> flares as a function of <span class="hlt">solar</span> longitude were aligned with H alpha synoptic charts on which <span class="hlt">active</span> region serial numbers and coronal hole boundaries were added.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/1984EOSTr..65.1232B','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/1984EOSTr..65.1232B"><span>Geophysical and <span class="hlt">solar</span> <span class="hlt">activity</span> indices</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Bossy, L.; Lemaire, J.</p> <p>1984-04-01</p> <p>A large number of geophysicists try to correlate their observations with one or even a series of different geophysical or <span class="hlt">solar</span> <span class="hlt">activity</span> indices. Yet the right choice of the most appropriate index with which to correlate depends mainly on our understanding of the physical cause-effect relationship between the new set of observations and the index chosen. This best choice will therefore depend on our good understanding of the methods of measurement and derivation of the adopted index in such correlative studies. It relies also on our awareness of the range of applicability of the indices presently available as well as on our understanding of their limitations. It was to achieve these goals that a series of general lectures on geophysical and <span class="hlt">solar</span> <span class="hlt">activity</span> indices was organized by L. Bossy and J. Lemaire (Institut d'Aeronomie Spatiale de Belgique (IASB), Brussels), March 26-29, 1984 at Han-sur-Lesse, Belgium.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2018AnGeo..36..633M','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2018AnGeo..36..633M"><span><span class="hlt">Solar</span> rotational cycle in lightning <span class="hlt">activity</span> in Japan during the 18-19th centuries</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Miyahara, Hiroko; Kataoka, Ryuho; Mikami, Takehiko; Zaiki, Masumi; Hirano, Junpei; Yoshimura, Minoru; Aono, Yasuyuki; Iwahashi, Kiyomi</p> <p>2018-04-01</p> <p>Thunderstorm and cloud <span class="hlt">activities</span> sometimes show a 27-day period, and this has long been studied to uncover a possible important link to <span class="hlt">solar</span> rotation. Because the 27-day variations in the <span class="hlt">solar</span> forcing parameters such as <span class="hlt">solar</span> ultraviolet and galactic cosmic rays become more prominent when the <span class="hlt">solar</span> <span class="hlt">activity</span> is high, it is expected that the signal of the 27-day period in meteorological phenomena may wax and wane according to the changes in the <span class="hlt">solar</span> <span class="hlt">activity</span> level. In this study, we examine in detail the intensity variations in the signal of the 27-day <span class="hlt">solar</span> rotational period in thunder and lightning <span class="hlt">activity</span> from the 18th to the 19th centuries based on 150-year-long records found in old diaries kept in Japan and discuss their relation with the <span class="hlt">solar</span> <span class="hlt">activity</span> levels. Such long records enable us to examine the signals of <span class="hlt">solar</span> rotation at both high and low <span class="hlt">solar</span> <span class="hlt">activity</span> levels. We found that the signal of the <span class="hlt">solar</span> rotational period in the thunder and lightning <span class="hlt">activity</span> increases as the <span class="hlt">solar</span> <span class="hlt">activity</span> increases. In this study, we also discuss the possibility of the impact of the long-term climatological conditions on the signals of the 27-day period in thunder/lightning <span class="hlt">activities</span>.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://eric.ed.gov/?q=heat+AND+exchanger&pg=2&id=EJ310571','ERIC'); return false;" href="https://eric.ed.gov/?q=heat+AND+exchanger&pg=2&id=EJ310571"><span>A Practical Application of Microcomputers to Control an <span class="hlt">Active</span> <span class="hlt">Solar</span> System.</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>Goldman, David S.; Warren, William</p> <p>1984-01-01</p> <p>Describes the design and implementation of a microcomputer-based model <span class="hlt">active</span> <span class="hlt">solar</span> heating system. Includes discussions of: (1) the <span class="hlt">active</span> <span class="hlt">solar</span> components (<span class="hlt">solar</span> collector, heat exchanger, pump, and fan necessary to provide forced air heating); (2) software components; and (3) hardware components (in the form of sensors and actuators). (JN)</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('http://adsabs.harvard.edu/abs/1999spro.proc...41G','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/1999spro.proc...41G"><span>Physics of the <span class="hlt">Solar</span> <span class="hlt">Active</span> Regions from Radio Observations</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Gelfreikh, G. B.</p> <p>1999-12-01</p> <p>Localized increase of the magnetic field observed by routine methods on the photosphere result in the growth of a number of <span class="hlt">active</span> processes in the <span class="hlt">solar</span> atmosphere and the heliosphere. These localized regions of increased magnetic field are called <span class="hlt">active</span> regions (AR). The main processes of transfer, accumulation and release of energy in an AR is, however, out of scope of photospheric observations being essentially a 3D-process and happening either under photosphere or up in the corona. So, to investigate these plasma structures and processes we are bound to use either extrapolation of optical observational methods or observations in EUV, X-rays and radio. In this review, we stress and illustrate the input to the problem gained from radio astronomical methods and discuss possible future development of their applicatications. Historically speaking each new step in developing radio technique of observations resulted in detecting some new physics of ARs. The most significant progress in the last few years in radio diagnostics of the plasma structures of magnetospheres of the <span class="hlt">solar</span> ARs is connected with the developing of the 2D full disk analysis on regular basis made at Nobeyama and detailed multichannel spectral-polarization (but one-dimensional and one per day) <span class="hlt">solar</span> observations at the RATAN-600. In this report the bulk of attention is paid to the new approach to the study of <span class="hlt">solar</span> <span class="hlt">activity</span> gained with the Nobeyama radioheliograph and analyzing the ways for future progress. The most important new features of the multicomponent radio sources of the ARs studied using Nobeyama radioheliograph are as follow: 1. The analysis of magnetic field structures in <span class="hlt">solar</span> corona above sunspot with 2000 G. Their temporal evolution and fluctuations with the periods around 3 and 5 minutes, due to MHD-waves in sunspot magnetic tubes and surrounding plasma. These investigations are certainly based on an analysis of thermal cyclotron emission of lower corona and CCTR above sunspot</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2016IAUTA..29..245S','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2016IAUTA..29..245S"><span>Division E Commission 10: <span class="hlt">Solar</span> <span class="hlt">Activity</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Schrijver, Carolus J.; Fletcher, Lyndsay; van Driel-Gesztelyi, Lidia; Asai, Ayumi; Cally, Paul S.; Charbonneau, Paul; Gibson, Sarah E.; Gomez, Daniel; Hasan, Siraj S.; Veronig, Astrid M.; Yan, Yihua</p> <p>2016-04-01</p> <p>After more than half a century of community support related to the science of ``<span class="hlt">solar</span> <span class="hlt">activity</span>'', IAU's Commission 10 was formally discontinued in 2015, to be succeeded by C.E2 with the same area of responsibility. On this occasion, we look back at the growth of the scientific disciplines involved around the world over almost a full century. <span class="hlt">Solar</span> <span class="hlt">activity</span> and fields of research looking into the related physics of the heliosphere continue to be vibrant and growing, with currently over 2,000 refereed publications appearing per year from over 4,000 unique authors, publishing in dozens of distinct journals and meeting in dozens of workshops and conferences each year. The size of the rapidly growing community and of the observational and computational data volumes, along with the multitude of connections into other branches of astrophysics, pose significant challenges; aspects of these challenges are beginning to be addressed through, among others, the development of new systems of literature reviews, machine-searchable archives for data and publications, and virtual observatories. As customary in these reports, we highlight some of the research topics that have seen particular interest over the most recent triennium, specifically <span class="hlt">active</span>-region magnetic fields, coronal thermal structure, coronal seismology, flares and eruptions, and the variability of <span class="hlt">solar</span> <span class="hlt">activity</span> on long time scales. We close with a collection of developments, discoveries, and surprises that illustrate the range and dynamics of the discipline.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://ntrs.nasa.gov/search.jsp?R=19960014136&hterms=hot+spot&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D20%26Ntt%3Dhot%2Bspot','NASA-TRS'); return false;" href="https://ntrs.nasa.gov/search.jsp?R=19960014136&hterms=hot+spot&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D20%26Ntt%3Dhot%2Bspot"><span>Hot spots and <span class="hlt">active</span> longitudes: Organization of <span class="hlt">solar</span> <span class="hlt">activity</span> as a probe of the interior</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Bai, Taeil; Hoeksema, J. Todd; Scherrer, Phil H.</p> <p>1995-01-01</p> <p>In order to investigate how <span class="hlt">solar</span> <span class="hlt">activity</span> is organized in longitude, major <span class="hlt">solar</span> flares, large sunspot groups, and large scale photospheric magnetic field strengths were analyzed. The results of these analyses are reported. The following results are discussed: hot spots, initially recognized as areas of high concentration of major flares, are the preferred locations for the emergence of big sunspot groups; double hot spots appear in pairs that rotate at the same rate separated by about 180 deg in longitude, whereas, single hot spots have no such companions; the northern and southern hemispheres behave differently in organizing <span class="hlt">solar</span> <span class="hlt">activity</span> in longitude; the lifetime of hot spots range from one to several <span class="hlt">solar</span> cycles; a hot spot is not always <span class="hlt">active</span> throughout its lifetime, but goes through dormant periods; and hot spots with different rotational periods coexist in the same hemisphere during the same <span class="hlt">solar</span> cycle.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2016PhDT........14C','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2016PhDT........14C"><span>A study of <span class="hlt">solar</span> magnetic fields below the surface, at the surface, and in the <span class="hlt">solar</span> atmosphere - understanding the cause of major <span class="hlt">solar</span> <span class="hlt">activity</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Chintzoglou, Georgios</p> <p>2016-04-01</p> <p>Magnetic fields govern all aspects of <span class="hlt">solar</span> <span class="hlt">activity</span> from the 11-year <span class="hlt">solar</span> cycle to the most energetic events in the <span class="hlt">solar</span> system, such as <span class="hlt">solar</span> flares and Coronal Mass Ejections (CMEs). As seen on the surface of the sun, this <span class="hlt">activity</span> emanates from localized concentrations of magnetic fields emerging sporadically from the <span class="hlt">solar</span> interior. These locations are called <span class="hlt">solar</span> <span class="hlt">Active</span> Regions (ARs). However, the fundamental processes regarding the origin, emergence and evolution of <span class="hlt">solar</span> magnetic fields as well as the generation of <span class="hlt">solar</span> <span class="hlt">activity</span> are largely unknown or remain controversial. In this dissertation, multiple important issues regarding <span class="hlt">solar</span> magnetism and <span class="hlt">activities</span> are addressed, based on advanced observations obtained by AIA and HMI instruments aboard the SDO spacecraft. First, this work investigates the formation of coronal magnetic flux ropes (MFRs), structures associated with major <span class="hlt">solar</span> <span class="hlt">activity</span> such as CMEs. In the past, several theories have been proposed to explain the cause of this major <span class="hlt">activity</span>, which can be categorized in two contrasting groups (a) the MFR is formed in the eruption, and (b) the MFR pre-exists the eruption. This remains a topic of heated debate in modern <span class="hlt">solar</span> physics. This dissertation provides a complete treatment of the role of MFRs from their genesis all the way to their eruption and even destruction. The study has uncovered the pre-existence of two weakly twisted MFRs, which formed during confined flaring 12 hours before their associated CMEs. Thus, it provides unambiguous evidence for MFRs truly existing before the CME eruptions, resolving the pre-existing MFR controversy. Second, this dissertation addresses the 3-D magnetic structure of complex emerging ARs. In ARs the photospheric fields might show all aspects of complexity, from simple bipolar regions to extremely complex multi-polar surface magnetic distributions. In this thesis, we introduce a novel technique to infer the subphotospheric configuration of emerging</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/19920019627','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/19920019627"><span>Nonlinear techniques for forecasting <span class="hlt">solar</span> <span class="hlt">activity</span> directly from its time series</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Ashrafi, S.; Roszman, L.; Cooley, J.</p> <p>1992-01-01</p> <p>Numerical techniques for constructing nonlinear predictive models to forecast <span class="hlt">solar</span> flux directly from its time series are presented. This approach makes it possible to extract dynamical invariants of our system without reference to any underlying <span class="hlt">solar</span> physics. We consider the dynamical evolution of <span class="hlt">solar</span> <span class="hlt">activity</span> in a reconstructed phase space that captures the attractor (strange), given a procedure for constructing a predictor of future <span class="hlt">solar</span> <span class="hlt">activity</span>, and discuss extraction of dynamical invariants such as Lyapunov exponents and attractor dimension.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/1981STIN...8128533.','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/1981STIN...8128533."><span>Energy data report: <span class="hlt">Solar</span> collector manufacturing <span class="hlt">activity</span>, July - December 1980</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p></p> <p>1981-03-01</p> <p>Statistics on <span class="hlt">solar</span> collector manufacturing <span class="hlt">activity</span> for both <span class="hlt">solar</span> thermal collectors and photovoltaic modules through 1980 are presented. Summary data are given for the number of manufacturers and collector area produced each year from 1974 through 1980; data for collector type are included, i.e., low temperature or medium temperature and special collectors. Producer shipments are tabulated according to location of company headquarters, producer size, and collector types. headquarters The number of companies engaged in <span class="hlt">activities</span> related to <span class="hlt">solar</span> collector manufacturing for 1978 through 1980 are listed; and the number of manufacturers and market sector are tabulated for photovoltaic modules manufacturing <span class="hlt">activities</span>.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/19930015527','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/19930015527"><span>Nonlinear techniques for forecasting <span class="hlt">solar</span> <span class="hlt">activity</span> directly from its time series</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Ashrafi, S.; Roszman, L.; Cooley, J.</p> <p>1993-01-01</p> <p>This paper presents numerical techniques for constructing nonlinear predictive models to forecast <span class="hlt">solar</span> flux directly from its time series. This approach makes it possible to extract dynamical in variants of our system without reference to any underlying <span class="hlt">solar</span> physics. We consider the dynamical evolution of <span class="hlt">solar</span> <span class="hlt">activity</span> in a reconstructed phase space that captures the attractor (strange), give a procedure for constructing a predictor of future <span class="hlt">solar</span> <span class="hlt">activity</span>, and discuss extraction of dynamical invariants such as Lyapunov exponents and attractor dimension.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2016Ap%26SS.361..295Z','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2016Ap%26SS.361..295Z"><span>Geomagnetic and <span class="hlt">solar</span> <span class="hlt">activity</span> dependence of ionospheric upflowing O+: FAST observations</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Zhao, K.; Jiang, Y.; Chen, K. W.; Huang, L. F.</p> <p>2016-09-01</p> <p>This paper investigates the dependence of the occurrence frequency of ionospheric upflowing oxygen (O+) ions on the sunspot cycle and geomagnetic <span class="hlt">activity</span>. We examine the upflows response to the geomagnetic disturbances as well as the <span class="hlt">influence</span> of the ion energy factor in controlling the magnitude of the occurrence frequency and the net energy flux. We discuss the spatial distribution of the upflow occurrence frequency and construct a regression model as a function of the magnetic latitude. The results show an overall enhancement of the upflow occurrence frequency during magnetically disturbed periods and indicate that the high-occurrence area spreads out from the source regions during magnetically quiet periods. The high-occurrence areas are located at 70° magnetic latitude (mLat) in the dayside auroral oval zone and between 76-80° mLat in the dayside polar cusp region. In the nightside auroral oval zone, these areas are near 60° mLat, penetrating further equatorward to 55° mLat during magnetically disturbed periods. High energy (≥1 keV) upflowing ions are common in the nightside auroral oval zone while low energy (<1 keV) upflowing ions are found escaping from the high latitude dayside cusp region. A Gaussian function is shown to be a good fit to the occurrence frequency over the magnetic latitude. For high energy upflowing O+ ions, the occurrence frequency exhibits a single peak located at about 60° mLat in the nightside auroral oval zone while for low energy upflowing O+ ions, it exhibits two peaks, one near 60° mLat in the auroral oval zone and the other near 78° mLat in the cusp region. We study the <span class="hlt">solar</span> <span class="hlt">activity</span> dependence by analyzing the relationship between the upflow occurrence frequency and the sunspot number (RZ). The statistical result shows that the frequency decreases with declining <span class="hlt">solar</span> <span class="hlt">activity</span> level, from ˜30 % at <span class="hlt">solar</span> maximum to ˜5 % at <span class="hlt">solar</span> minimum. In addition, the correlation coefficient between the occurrence frequency and RZ</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2018SPIE10615E..59D','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2018SPIE10615E..59D"><span>Hilbert-Huang transform analysis of long-term <span class="hlt">solar</span> magnetic <span class="hlt">activity</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Deng, Linhua</p> <p>2018-04-01</p> <p>Astronomical time series analysis is one of the hottest and most important problems, and becomes the suitable way to deal with the underlying dynamical behavior of the considered nonlinear systems. The quasi-periodic analysis of <span class="hlt">solar</span> magnetic <span class="hlt">activity</span> has been carried out by various authors during the past fifty years. In this work, the novel Hilbert-Huang transform approach is applied to investigate the yearly numbers of polar faculae in the time interval from 1705 to 1999. The detected periodicities can be allocated to three components: the first one is the short-term variations with periods smaller than 11 years, the second one is the mid- term variations with classical periods from 11 years to 50 years, and the last one is the long-term variations with periods larger than 50 years. The analysis results improve our knowledge on the quasi-periodic variations of <span class="hlt">solar</span> magnetic <span class="hlt">activity</span> and could be provided valuable constraints for <span class="hlt">solar</span> dynamo theory. Furthermore, our analysis results could be useful for understanding the long-term variations of <span class="hlt">solar</span> magnetic <span class="hlt">activity</span>, providing crucial information to describe and forecast <span class="hlt">solar</span> magnetic <span class="hlt">activity</span> indicators.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2014cosp...40E1494K','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2014cosp...40E1494K"><span>Evidence of plasma heating in <span class="hlt">solar</span> microflares during the minimum of <span class="hlt">solar</span> <span class="hlt">activity</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Kirichenko, Alexey; Bogachev, Sergey</p> <p></p> <p>We present a statistical study of 80 <span class="hlt">solar</span> microflares observed during the deep minimum of <span class="hlt">solar</span> <span class="hlt">activity</span> between 23 and 24 <span class="hlt">solar</span> cycles. Our analysis covers the following characteristics of the flares: thermal energy of flaring plasma, its temperature and its emission measure in soft X-rays. The data were obtained during the period from April to July of 2009, which was favorable for observations of weak events because of very low level of <span class="hlt">solar</span> <span class="hlt">activity</span>. The most important part of our analysis was an investigation of extremely weak microflares corresponding to X-ray class below A1.0. We found direct evidence of plasma heating in more than 90% of such events. Temperature of flaring plasma was determined under the isothermal approximation using the data of two <span class="hlt">solar</span> instruments: imaging spectroheliometer MISH onboard Coronas-Photon spacecraft and X-ray spectrophotometer SphinX operating in energy range 0.8 - 15 keV. The main advantage of MISH is the ability to image high temperature plasma (T above 4 MK) without a low-temperature background. The SphinX data was selected due to its high sensitivity, which makes available the registration of X-ray emission from extremely weak microflares corresponding GOES A0.1 - A0.01 classes. The temperature we obtained lies in the range from 2.6 to 13.6 MK, emission measure, integrated over the range 1 - 8 Å - 2.7times10(43) - 4.9times10(47) cm (-3) , thermal energy of flaring region - 5times10(26) - 1.6times10(29) erg. We compared our results with the data obtained by Feldman et. al. 1996 and Ryan et. al. 2012 for <span class="hlt">solar</span> flares with X-ray classes above A2.0 and conclude that the relation between X-ray class of <span class="hlt">solar</span> flare and its temperature is strongly different for ordinary flares (above A2.0) and for weak microflares (A0.01 - A2.0). Our result supports the idea that weak <span class="hlt">solar</span> events (microflares and nanoflares) may play significant a role in plasma heating in <span class="hlt">solar</span> corona.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2001ICRC....8.3359A','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2001ICRC....8.3359A"><span>Forecast for <span class="hlt">solar</span> cycle 23 <span class="hlt">activity</span>: a progress report</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Ahluwalia, H. S.</p> <p>2001-08-01</p> <p>At the 25th International Cosmic Ray Conference (ICRC) at Durban, South Africa, I announced the discovery of a three cycle quasi-periodicity in the ion chamber data string assembled by me, for the 1937 to 1994 period (Conf. Pap., v. 2, p. 109, 1997). It corresponded in time with a similar quasi-periodicity observed in the dataset for the planetary index Ap. At the 26th ICRC at Salt Lake City, UT, I reported on our analysis of the Ap data to forecast the amplitude of <span class="hlt">solar</span> cycle 23 <span class="hlt">activity</span> (Conf. Pap., v. 2, pl. 260, 1999). I predicted that cycle 23 will be moderate (a la cycle 17), notwithstanding the early exuberant forecasts of some <span class="hlt">solar</span> astronomers that cycle 23, "may be one of the greatest cycles in recent times, if not the greatest." Sunspot number data up to April 2001 indicate that our forecast appears to be right on the mark. We review the <span class="hlt">solar</span>, interplanetary and geophysical data and describe the important lessons learned from this experience. 1. Introduction Ohl (1971) was the first to realize that Sun may be sending us a subliminal message as to its intent for its <span class="hlt">activity</span> (Sunspot Numbers, SSN) in the next cycle. He posited that the message was embedded in the geomagnetic <span class="hlt">activity</span> (given by sum Kp). Schatten at al (1978) suggested that Ohl hypothesis could be understood on the basis of the model proposed by Babcock (1961) who suggested that the high latitude <span class="hlt">solar</span> poloidal fields, near a minimum, emerge as the toroidal fields on opposite sides of the <span class="hlt">solar</span> equator. This is known as the <span class="hlt">Solar</span> Dynamo Model. One can speculate that the precursor poloidal <span class="hlt">solar</span> field is entrained in the high speed <span class="hlt">solar</span> wind streams (HSSWS) from the coronal holes which are observed at Earth's orbit during the descending phase of the previous cycle. The interaction</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2014EGUGA..16.5253Z','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2014EGUGA..16.5253Z"><span>On dependence of seismic <span class="hlt">activity</span> on 11 year variations in <span class="hlt">solar</span> <span class="hlt">activity</span> and/or cosmic rays</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Zhantayev, Zhumabek; Khachikyan, Galina; Breusov, Nikolay</p> <p>2014-05-01</p> <p>It is found in the last decades that seismic <span class="hlt">activity</span> of the Earth has a tendency to increase with decreasing <span class="hlt">solar</span> <span class="hlt">activity</span> (increasing cosmic rays). A good example of this effect may be the growing number of catastrophic earthquakes in the recent rather long <span class="hlt">solar</span> minimum. Such results support idea on existence a <span class="hlt">solar</span>-lithosphere relationship which, no doubts, is a part of total pattern of <span class="hlt">solar</span>-terrestrial relationships. The physical mechanism of <span class="hlt">solar</span>-terrestrial relationships is not developed yet. It is believed at present that one of the main contenders for such mechanism may be the global electric circuit (GEC) - vertical current loops, piercing and electrodynamically coupling all geospheres. It is also believed, that the upper boundary of the GEC is located at the magnetopause, where magnetic field of the <span class="hlt">solar</span> wind reconnects with the geomagnetic field, that results in penetrating <span class="hlt">solar</span> wind energy into the earth's environment. The effectiveness of the GEC operation depends on intensity of cosmic rays (CR), which ionize the air in the middle atmosphere and provide its conductivity. In connection with the foregoing, it can be expected: i) quantitatively, an increasing seismic <span class="hlt">activity</span> from <span class="hlt">solar</span> maximum to <span class="hlt">solar</span> minimum may be in the same range as increasing CR flux; and ii) in those regions of the globe, where the crust is shipped by the magnetic field lines with number L= ~ 2.0, which are populated by anomalous cosmic rays (ACR), the relationship of seismic <span class="hlt">activity</span> with variations in <span class="hlt">solar</span> <span class="hlt">activity</span> will be manifested most clearly, since there is a pronounced dependence of ACR on <span class="hlt">solar</span> <span class="hlt">activity</span> variations. Checking an assumption (i) with data of the global seismological catalog of the NEIC, USGS for 1973-2010, it was found that yearly number of earthquake with magnitude M≥4.5 varies into the 11 year <span class="hlt">solar</span> cycle in a quantitative range of about 7-8% increasing to <span class="hlt">solar</span> minimum, that qualitatively and quantitatively as well is in agreement with the</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/19900018855','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/19900018855"><span>The QBO and weak external forcing by <span class="hlt">solar</span> <span class="hlt">activity</span>: A three dimensional model study</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Dameris, M.; Ebel, A.</p> <p>1989-01-01</p> <p>A better understanding is attempted of the physical mechanisms leading to significant correlations between oscillations in the lower and middle stratosphere and <span class="hlt">solar</span> variability associated with the sun's rotation. A global 3-d mechanistic model of the middle atmosphere is employed to investigate the effects of minor artificially induced perturbations. The aim is to explore the physical mechanisms of the dynamical response especially of the stratosphere to weak external forcing as it may result from UV flux changes due to <span class="hlt">solar</span> rotation. First results of numerical experiments dealing about the external forcing of the middle atmosphere by <span class="hlt">solar</span> <span class="hlt">activity</span> were presented elsewhere. Different numerical studies regarding the excitation and propagation of weak perturbations have been continued since then. The model calculations presented are made to investigate the <span class="hlt">influence</span> of the quasi-biennial oscillation (QBO) on the dynamical response of the middle atmosphere to weak perturbations by employing different initial wind fields which represent the west and east phase of the QBO.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://ntrs.nasa.gov/search.jsp?R=19870059798&hterms=origin+mass&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D20%26Ntt%3Dorigin%2Bmass','NASA-TRS'); return false;" href="https://ntrs.nasa.gov/search.jsp?R=19870059798&hterms=origin+mass&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D20%26Ntt%3Dorigin%2Bmass"><span><span class="hlt">Activity</span> associated with the <span class="hlt">solar</span> origin of coronal mass ejections</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Webb, D. F.; Hundhausen, A. J.</p> <p>1987-01-01</p> <p><span class="hlt">Solar</span> coronal mass ejections (CMEs) observed in 1980 with the HAO Coronagraph/Polarimeter on the <span class="hlt">Solar</span> Maximum Mission (SMM) satellite are compared with other forms of <span class="hlt">solar</span> <span class="hlt">activity</span> that might be physically related to the ejections. The <span class="hlt">solar</span> phenomena checked and the method of association used were intentionally patterned after those of Munro et al.'s (1979) analysis of mass ejections observed with the Skylab coronagraph to facilitate comparison of the two epochs. Comparison of the results reveals that the types and degree of CME associations are similar near <span class="hlt">solar</span> <span class="hlt">activity</span> minimum and at maximum. For both epochs, most CMEs with associations had associated eruptive prominences, and the proportions of association of all types of <span class="hlt">activity</span> were similar. A high percentage of association between SMM CMEs and X-ray long duration events is also found, in agreement with Skylab results. It is concluded that most CMEs are the result of the destabilization and eruption of a prominence and its overlying coronal structure, or of a magnetic structure capable of supporting a prominence.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/19850026753','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/19850026753"><span>The <span class="hlt">solar</span> wind effect on cosmic rays and <span class="hlt">solar</span> <span class="hlt">activity</span></span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Fujimoto, K.; Kojima, H.; Murakami, K.</p> <p>1985-01-01</p> <p>The relation of cosmic ray intensity to <span class="hlt">solar</span> wind velocity is investigated, using neutron monitor data from Kiel and Deep River. The analysis shows that the regression coefficient of the average intensity for a time interval to the corresponding average velocity is negative and that the absolute effect increases monotonously with the interval of averaging, tau, that is, from -0.5% per 100km/s for tau = 1 day to -1.1% per 100km/s for tau = 27 days. For tau 27 days the coefficient becomes almost constant independently of the value of tau. The analysis also shows that this tau-dependence of the regression coefficiently is varying with the <span class="hlt">solar</span> <span class="hlt">activity</span>.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.osti.gov/biblio/5518436-solar-equatorial-qbo-influences-stratospheric-circulation-during-early-northern-hemisphere-winter-quasi-biennial-oscillation','SCIGOV-STC'); return false;" href="https://www.osti.gov/biblio/5518436-solar-equatorial-qbo-influences-stratospheric-circulation-during-early-northern-hemisphere-winter-quasi-biennial-oscillation"><span>The <span class="hlt">solar</span> and equatorial QBO <span class="hlt">influences</span> on the stratospheric circulation during the early northern-hemisphere winter. [Quasi-Biennial Oscillation</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>Kodera, Kunihiko</p> <p>1991-06-01</p> <p>A case study was conducted to investigate the mechanism of how the <span class="hlt">solar</span> cycle and the equatorial quasi-biennial oscillation (QBO) <span class="hlt">influence</span> the stratospheric circulation during the Northern-Hemisphere winter. It was found that the <span class="hlt">solar</span> and QBO <span class="hlt">influences</span> on the stratospheric jet exist rather independently in the upper stratosphere during December. The mean-zonal wind anomalies produced in early winter persist by deformation until late winter through wave-mean flow interactions with planetary waves. The modulation effect of the <span class="hlt">solar</span> <span class="hlt">influence</span> by the QBO takes place during this process.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/19900018880','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/19900018880"><span><span class="hlt">Solar</span> <span class="hlt">activity</span> <span class="hlt">influences</span> on atmospheric electricity and on some structures in the middle atmosphere</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Reiter, Reinhold</p> <p>1989-01-01</p> <p>Only processes in the troposphere and the lower stratosphere are reviewed. General aspects of global atmospheric electricity are summarized in Chapter 3 of NCR (1986); Volland (1984) has outlined the overall problems of atmospheric electrodynamics; and Roble and Hays (1982) published a summary of <span class="hlt">solar</span> effects on the global circuit. The <span class="hlt">solar</span> variability and its atmospheric effects (overview by Donelly et al, 1987) and the <span class="hlt">solar</span>-planetary relationships (survey by James et al. 1983) are so extremely complex that only particular results and selected papers of direct relevance or historical importance are compiled herein.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017AGUFMSA33B..03S','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017AGUFMSA33B..03S"><span>Characteristics of seasonal variation and <span class="hlt">solar</span> <span class="hlt">activity</span> dependence of the geomagnetic <span class="hlt">solar</span> quiet daily variation</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Shinbori, A.; Koyama, Y.; Nose, M.; Hori, T.</p> <p>2017-12-01</p> <p>Characteristics of seasonal variation and <span class="hlt">solar</span> <span class="hlt">activity</span> dependence of the X- and Y-components of the geomagnetic <span class="hlt">solar</span> quiet (Sq) daily variation at Memanbetsu in mid-latitudes and Guam near the equator have been investigated using long-term geomagnetic field data with 1-h time resolution from 1957 to 2016. In this analysis, we defined the quiet day when the maximum value of the Kp index is less than 3 for that day. In this analysis, we used the monthly average of the adjusted daily F10.7 corresponding to geomagnetically quiet days. For identification of the monthly mean Sq variation in the X and Y components (Sq-X and Sq-Y), we first determined the baseline of the X and Y components from the average value from 22 to 2 h (LT: local time) for each quiet day. Next, we calculated a deviation from the baseline of the X- and Y-components of the geomagnetic field for each quiet day, and computed the monthly mean value of the deviation for each local time. As a result, Sq-X and Sq-Y shows a clear seasonal variation and <span class="hlt">solar</span> <span class="hlt">activity</span> dependence. The amplitude of seasonal variation increases significantly during high <span class="hlt">solar</span> <span class="hlt">activities</span>, and is proportional to the <span class="hlt">solar</span> F10.7 index. The pattern of the seasonal variation is quite different between Sq-X and Sq-Y. The result of the correlation analysis between the <span class="hlt">solar</span> F10.7 index and Sq-X and Sq-Y shows almost the linear relationship, but the slope and intercept of the linear fitted line varies as function of local time and month. This implies that the sensitivity of Sq-X and Sq-Y to the <span class="hlt">solar</span> <span class="hlt">activity</span> is different for different local times and seasons. The local time dependence of the offset value of Sq-Y at Guam and its seasonal variation suggest a magnetic field produced by inter-hemispheric field-aligned currents (FACs). From the sign of the offset value of Sq-Y, it is infer that the inter-hemispheric FACs flow from the summer to winter hemispheres in the dawn and dusk sectors and from the winter to summer hemispheres in</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/19750024923','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/19750024923"><span>H-alpha synoptic charts of <span class="hlt">solar</span> <span class="hlt">activity</span> during the first year of <span class="hlt">solar</span> cycle 20, October 1964 - August 1965. [Skylab program</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Mcintosh, P. S.</p> <p>1975-01-01</p> <p><span class="hlt">Solar</span> <span class="hlt">activity</span> during the period October 28, 1964 through August 27, 1965 is presented in the form of charts for each <span class="hlt">solar</span> rotation constructed from observations made with the chromospheric H-alpha spectra line. These H-alpha synoptic charts are identical in format and method of construction to those published for the period of Skylab observations. The sunspot minimum marking the start of <span class="hlt">Solar</span> Cycle 20 occurred in October, 1964; therefore, charts represent <span class="hlt">solar</span> <span class="hlt">activity</span> during the first year of this <span class="hlt">solar</span> cycle.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.osti.gov/pages/biblio/1260986-multi-scale-statistical-analysis-coronal-solar-activity','SCIGOV-DOEP'); return false;" href="https://www.osti.gov/pages/biblio/1260986-multi-scale-statistical-analysis-coronal-solar-activity"><span>Multi-scale statistical analysis of coronal <span class="hlt">solar</span> <span class="hlt">activity</span></span></a></p> <p><a target="_blank" href="http://www.osti.gov/pages">DOE PAGES</a></p> <p>Gamborino, Diana; del-Castillo-Negrete, Diego; Martinell, Julio J.</p> <p>2016-07-08</p> <p>Multi-filter images from the <span class="hlt">solar</span> corona are used to obtain temperature maps that are analyzed using techniques based on proper orthogonal decomposition (POD) in order to extract dynamical and structural information at various scales. Exploring <span class="hlt">active</span> regions before and after a <span class="hlt">solar</span> flare and comparing them with quiet regions, we show that the multi-scale behavior presents distinct statistical properties for each case that can be used to characterize the level of <span class="hlt">activity</span> in a region. Information about the nature of heat transport is also to be extracted from the analysis.</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('https://www.ncbi.nlm.nih.gov/pubmed/27901473','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/27901473"><span><span class="hlt">Influence</span> of <span class="hlt">solar</span> and geomagnetic <span class="hlt">activity</span> in Gymnodinium catenatum (Dinophyceae) cultures.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Vale, Paulo</p> <p>2017-01-01</p> <p>Laboratory cultures of the paralytic shellfish poisoning producing microalga Gymnodinium catenatum were subjected to a hypo-osmotic shock and changes in cell concentration were observed in two separate experiments of 8 and 24 hours duration, respectively. The increase in geomagnetic <span class="hlt">activity</span> (GMA), radio and X-ray fluxes and <span class="hlt">solar</span> X-ray flares were negatively correlated with cell numbers. Cell losses were observed in the short experiment, but not in the longest one. GMA action was related to the course of the experimental period, while electromagnetic radiation (EMR) was only significantly related when the previous hours before the experiments were considered. The differential action windows might be indicative of two differential disruptive mechanisms: EMR might act on DNA synthesis and mitosis phases of the cell cycle (taking place in the dark period) and GMA might be more disruptive at the end of mytosis or cytokinesis phases taking place in the light period. Formation of long chains (> 4 cells/chain) was reduced with salinity and with temperatures above 27ºC but increased with EMR and GMA, particularly when grown at the highest temperatures recorded during the study period (≥28ºC).</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/20090017773','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/20090017773"><span>Evidence for <span class="hlt">Solar</span> Cycle <span class="hlt">Influence</span> on the Infrared Energy Budget and Radiative Cooling of the Thermosphere</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Mlynczak, Martin G.; Martin-Torres, F. Javier; Marshall, B. Thomas; Thompson, R. Earl; Williams, Joshua; Turpin, TImothy; Kratz, D. P.; Russell, James M.; Woods, Tom; Gordley, Larry L.</p> <p>2007-01-01</p> <p>We present direct observational evidence for <span class="hlt">solar</span> cycle <span class="hlt">influence</span> on the infrared energy budget and radiative cooling of the thermosphere. By analyzing nearly five years of data from the Sounding of the Atmosphere using Broadband Emission Radiometry (SABER) instrument, we show that the annual mean infrared power radiated by the nitric oxide (NO) molecule at 5.3 m has decreased by a factor of 2.9. This decrease is correlated (r = 0.96) with the decrease in the annual mean F10.7 <span class="hlt">solar</span> index. Despite the sharp decrease in radiated power (which is equivalent to a decrease in the vertical integrated radiative cooling rate), the variability of the power as given in the standard deviation of the annual means remains approximately constant. A simple relationship is shown to exist between the infrared power radiated by NO and the F10.7 index, thus providing a fundamental relationship between <span class="hlt">solar</span> <span class="hlt">activity</span> and the thermospheric cooling rate for use in thermospheric models. The change in NO radiated power is also consistent with changes in absorbed ultraviolet radiation over the same time period.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/26151833','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/26151833"><span>Improved Power Conversion Efficiency of Inverted Organic <span class="hlt">Solar</span> Cells by Incorporating Au Nanorods into <span class="hlt">Active</span> Layer.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>He, Yeyuan; Liu, Chunyu; Li, Jinfeng; Zhang, Xinyuan; Li, Zhiqi; Shen, Liang; Guo, Wenbin; Ruan, Shengping</p> <p>2015-07-29</p> <p>This Research Article describes a cooperative plasmonic effect on improving the performance of organic <span class="hlt">solar</span> cells. When Au nanorods(NRs) are incorporated into the <span class="hlt">active</span> layers, the designed project shows superior enhanced light absorption behavior comparing with control devices, which leads to the realization of organic <span class="hlt">solar</span> cell with power conversion efficiency of 6.83%, accounting for 18.9% improvement. Further investigations unravel the <span class="hlt">influence</span> of plasmonic nanostructures on light trapping, exciton generation, dissociation, and charge recombination and transport inside the thin films devices. Moreover, the introduction of high-conductivity Au NRs improves electrical conductivity of the whole device, which contributes to the enhanced fill factor.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2012AGUFMSH13A2249S','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2012AGUFMSH13A2249S"><span>Evidence for a <span class="hlt">Solar</span> <span class="hlt">Influence</span> on Gamma Radiation from Radon</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Sturrock, P. A.; Steinitz, G.; Fischbach, E.; Javorsek, D.; Jenkins, J.</p> <p>2012-12-01</p> <p>We have analyzed 29,000 measurements of gamma radiation associated with the decay of radon confined to an airtight vessel at the Geological Survey of Israel (GSI) Laboratory in Jerusalem between January 28 2007 and May 10 2010. These measurements exhibit strong variations in time of year and time of day, which may be due in part to environmental <span class="hlt">influences</span>. However, time-series analysis reveals a number of strong periodicities, including two at approximately 11.2 year-1 and 12.5 year-1. We consider it significant that these same oscillations have previously been detected in nuclear-decay data acquired at the Brookhaven National Laboratory and at the Physiklisch-Technische Bundesanstalt. We have suggested that these oscillations are due to some form of <span class="hlt">solar</span> radiation (possibly neutrinos) that has its origin in the deep <span class="hlt">solar</span> interior. A curious property of the GSI data is that the annual oscillation is much stronger in daytime data than in nighttime data, but the opposite is true for all other oscillations. Time-frequency analysis also yields quite different results from daytime and nighttime data. These procedures have also been applied to data collected from subsurface geological sites in Israel, Tenerife, and Italy, which have a variety of geological and geophysical scenarios, different elevations, and depths below the surface ranging from several meters to 1000 meters. In view of these results, and in view of the fact that there is at present no clear understanding of the behavior of radon in its natural environment, there would appear to be a need for multi-disciplinary research. Investigations that clarify the nature and mechanisms of <span class="hlt">solar</span> <span class="hlt">influences</span> may help clarify the nature and mechanisms of geological <span class="hlt">influences</span>.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://www.agu.org/pubs/crossref/2011/2011GL046751.shtml','USGSPUBS'); return false;" href="http://www.agu.org/pubs/crossref/2011/2011GL046751.shtml"><span>Spring-fall asymmetry of substorm strength, geomagnetic <span class="hlt">activity</span> and <span class="hlt">solar</span> wind: Implications for semiannual variation and <span class="hlt">solar</span> hemispheric asymmetry</span></a></p> <p><a target="_blank" href="http://pubs.er.usgs.gov/pubs/index.jsp?view=adv">USGS Publications Warehouse</a></p> <p>Marsula, K.; Tanskanen, E.; Love, J.J.</p> <p>2011-01-01</p> <p>We study the seasonal variation of substorms, geomagnetic <span class="hlt">activity</span> and their <span class="hlt">solar</span> wind drivers in 1993–2008. The number of substorms and substorm mean duration depict an annual variation with maxima in Winter and Summer, respectively, reflecting the annual change of the local ionosphere. In contradiction, substorm mean amplitude, substorm total efficiency and global geomagnetic <span class="hlt">activity</span> show a dominant annual variation, with equinoctial maxima alternating between Spring in <span class="hlt">solar</span> cycle 22 and Fall in cycle 23. The largest annual variations were found in 1994 and 2003, in the declining phase of the two cycles when high-speed streams dominate the <span class="hlt">solar</span> wind. A similar, large annual variation is found in the <span class="hlt">solar</span> wind driver of substorms and geomagnetic <span class="hlt">activity</span>, which implies that the annual variation of substorm strength, substorm efficiency and geomagnetic <span class="hlt">activity</span> is not due to ionospheric conditions but to a hemispherically asymmetric distribution of <span class="hlt">solar</span> wind which varies from one cycle to another. Our results imply that the overall semiannual variation in global geomagnetic <span class="hlt">activity</span> has been seriously overestimated, and is largely an artifact of the dominant annual variation with maxima alternating between Spring and Fall. The results also suggest an intimate connection between the asymmetry of <span class="hlt">solar</span> magnetic fields and some of the largest geomagnetic disturbances, offering interesting new pathways for forecasting disturbances with a longer lead time to the future.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://pubs.er.usgs.gov/publication/70034109','USGSPUBS'); return false;" href="https://pubs.er.usgs.gov/publication/70034109"><span>Spring-fall asymmetry of substorm strength, geomagnetic <span class="hlt">activity</span> and <span class="hlt">solar</span> wind: Implications for semiannual variation and <span class="hlt">solar</span> hemispheric asymmetry</span></a></p> <p><a target="_blank" href="http://pubs.er.usgs.gov/pubs/index.jsp?view=adv">USGS Publications Warehouse</a></p> <p>Mursula, K.; Tanskanen, E.; Love, J.J.</p> <p>2011-01-01</p> <p>We study the seasonal variation of substorms, geomagnetic <span class="hlt">activity</span> and their <span class="hlt">solar</span> wind drivers in 1993-2008. The number of substorms and substorm mean duration depict an annual variation with maxima in Winter and Summer, respectively, reflecting the annual change of the local ionosphere. In contradiction, substorm mean amplitude, substorm total efficiency and global geomagnetic <span class="hlt">activity</span> show a dominant annual variation, with equinoctial maxima alternating between Spring in <span class="hlt">solar</span> cycle 22 and Fall in cycle 23. The largest annual variations were found in 1994 and 2003, in the declining phase of the two cycles when high-speed streams dominate the <span class="hlt">solar</span> wind. A similar, large annual variation is found in the <span class="hlt">solar</span> wind driver of substorms and geomagnetic <span class="hlt">activity</span>, which implies that the annual variation of substorm strength, substorm efficiency and geomagnetic <span class="hlt">activity</span> is not due to ionospheric conditions but to a hemispherically asymmetric distribution of <span class="hlt">solar</span> wind which varies from one cycle to another. Our results imply that the overall semiannual variation in global geomagnetic <span class="hlt">activity</span> has been seriously overestimated, and is largely an artifact of the dominant annual variation with maxima alternating between Spring and Fall. The results also suggest an intimate connection between the asymmetry of <span class="hlt">solar</span> magnetic fields and some of the largest geomagnetic disturbances, offering interesting new pathways for forecasting disturbances with a longer lead time to the future. Copyright ?? 2011 by the American Geophysical Union.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2014AcASn..55..447S','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2014AcASn..55..447S"><span>Multi-wavelength and High-resolution Observations of <span class="hlt">Solar</span> Eruptive <span class="hlt">Activities</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Shen, Y. D.</p> <p>2014-09-01</p> <p>In recent years, various <span class="hlt">solar</span> eruptive <span class="hlt">activities</span> have been observed in the <span class="hlt">solar</span> atmosphere, such as <span class="hlt">solar</span> flares, filament eruptions, jets, coronal mass ejections (CMEs), and magnetohydrodynamics (MHD) waves. Previous observations have indicated that <span class="hlt">solar</span> magnetic field plays a dominant role in the processes of all kinds of <span class="hlt">solar</span> <span class="hlt">activities</span>. Since many large-scale <span class="hlt">solar</span> eruptive <span class="hlt">activities</span> can cause significant effects on the space environment of the Earth as well as the human life, studying and forecasting the <span class="hlt">solar</span> <span class="hlt">activities</span> are urgent tasks for us. In addition, the Sun is the nearest star to the Earth, so that people can directly observe and study it in detail. Hence, studying the Sun can also provide a reference to study other stars in the universe. This thesis focuses on the multi-wavelength and high-resolution observations of three types of <span class="hlt">solar</span> eruptive <span class="hlt">activities</span>: filament eruptions, coronal jets, and coronal MHD waves. By analyzing various observations taken by ground-based and space-borne instruments, we try to understand the inherent physical mechanisms, and construct models to interpret different kinds of <span class="hlt">solar</span> eruptive <span class="hlt">activities</span>. The triggering mechanism and the cause of a failed filament eruption are studied in Chapter 3, which indicates that the energy released in the flare is a key factor to the fate of the filament. Two successive filament eruptions are studied in Chapter 4, which indicates that the magnetic implosion could be the physical linkage between them, and the structures of coronal magnetic fields are important for producing sympathetic eruptions. A magnetic unwinding jet and a blowout jet are studied in Chapters 5 and 6, respectively. The former exhibits obvious radial expansion, which undergoes three distinct phases: the slow expansion phase, the fast expansion phase, and the steady phase. In addition, calculation indicates that the non-potential magnetic field in the jet can supply sufficient energy for producing the unwinding</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/19790004819','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/19790004819"><span>Effects of long-period <span class="hlt">solar</span> <span class="hlt">activity</span> fluctuation on temperature and pressure of the terrestrial atmosphere</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Rubashev, B. M.</p> <p>1978-01-01</p> <p>The present state of research on the <span class="hlt">influence</span> of <span class="hlt">solar</span> sunspot <span class="hlt">activity</span> on tropospheric temperature and pressure is reviewed. The existence of an 11-year temperature cycle of 5 different types is affirmed. A cyclic change in atmospheric pressure, deducing characteristic changes between 11-year cycles is discussed. The existence of 80-year and 5-to-6-year cycles of temperature is established, and physical causes for birth are suggested.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/19920024232','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/19920024232"><span><span class="hlt">Influence</span> of mass moment of inertia on normal modes of preloaded <span class="hlt">solar</span> array mast</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Armand, Sasan C.; Lin, Paul</p> <p>1992-01-01</p> <p>Earth-orbiting spacecraft often contain <span class="hlt">solar</span> arrays or antennas supported by a preloaded mast. Because of weight and cost considerations, the structures supporting the spacecraft appendages are extremely light and flexible; therefore, it is vital to investigate the <span class="hlt">influence</span> of all physical and structural parameters that may <span class="hlt">influence</span> the dynamic behavior of the overall structure. The study primarily focuses on the mast for the space station <span class="hlt">solar</span> arrays, but the formulations and the techniques developed in this study apply to any large and flexible mast in zero gravity. Furthermore, to determine the <span class="hlt">influence</span> on the circular frequencies, the mass moment of inertia of the mast was incorporated into the governing equation of motion for bending. A finite element technique (MSC/NASTRAN) was used to verify the formulation. Results indicate that when the mast is relatively flexible and long, the mass moment inertia <span class="hlt">influences</span> the circular frequencies.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2002cosp...34E2656L','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2002cosp...34E2656L"><span>On the <span class="hlt">Influence</span> of the <span class="hlt">Solar</span> Bi-Cycle on Comic Ray Modulatio</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Lifter, N. Part Xxvii: A. Defect Of The Solar Dynamo. B.; Scissors, K.; Sprucener, H.</p> <p></p> <p>In this presentation we propose a new paradigm that explains the different lengths of individual <span class="hlt">solar</span> Hale cycles. It proves beneficial to distinguish between a so-called inHale and ex-Hale cycle, which together form the <span class="hlt">solar</span> bi-cycle. We carefully analyzed the <span class="hlt">influence</span> of so-called complex mode excitations (CMEs) on comic ray modulation, in particular on the drifts of the comic isotope O+3 , which we found to induce characteristic anisotropies. This comic isotope anisotropy (CIA) is caused by the wellknown north-south asymmetry (NSA) and can be observed as a rare Forbush increase (FBI). The latter is linked to the <span class="hlt">solar</span> magnetic field which appears to have a chaotic behaviour (for details see part I-XXVI). Especially during an ex-Hale cycle magnetic flux is pseudo-pneumatically escaping through a coronal hole. Consequently, the <span class="hlt">solar</span> dynamo can no longer operate efficiently, i.e. is defect.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2014cosp...40E3124S','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2014cosp...40E3124S"><span>Transient flows of the <span class="hlt">solar</span> wind associated with small-scale <span class="hlt">solar</span> <span class="hlt">activity</span> in <span class="hlt">solar</span> minimum</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Slemzin, Vladimir; Veselovsky, Igor; Kuzin, Sergey; Gburek, Szymon; Ulyanov, Artyom; Kirichenko, Alexey; Shugay, Yulia; Goryaev, Farid</p> <p></p> <p>The data obtained by the modern high sensitive EUV-XUV telescopes and photometers such as CORONAS-Photon/TESIS and SPHINX, STEREO/EUVI, PROBA2/SWAP, SDO/AIA provide good possibilities for studying small-scale <span class="hlt">solar</span> <span class="hlt">activity</span> (SSA), which is supposed to play an important role in heating of the corona and producing transient flows of the <span class="hlt">solar</span> wind. During the recent unusually weak <span class="hlt">solar</span> minimum, a large number of SSA events, such as week <span class="hlt">solar</span> flares, small CMEs and CME-like flows were observed and recorded in the databases of flares (STEREO, SWAP, SPHINX) and CMEs (LASCO, CACTUS). On the other hand, the <span class="hlt">solar</span> wind data obtained in this period by ACE, Wind, STEREO contain signatures of transient ICME-like structures which have shorter duration (<10h), weaker magnetic field strength (<10 nT) and lower proton temperature than usual ICMEs. To verify the assumption that ICME-like transients may be associated with the SSA events we investigated the number of weak flares of C-class and lower detected by SPHINX in 2009 and STEREO/EUVI in 2010. The flares were classified on temperature and emission measure using the diagnostic means of SPHINX and Hinode/EIS and were confronted with the parameters of the <span class="hlt">solar</span> wind (velocity, density, ion composition and temperature, magnetic field, pitch angle distribution of the suprathermal electrons). The outflows of plasma associated with the flares were identified by their coronal signatures - CMEs (only in few cases) and dimmings. It was found that the mean parameters of the <span class="hlt">solar</span> wind projected to the source surface for the times of the studied flares were typical for the ICME-like transients. The results support the suggestion that weak flares can be indicators of sources of transient plasma flows contributing to the slow <span class="hlt">solar</span> wind at <span class="hlt">solar</span> minimum, although these flows may be too weak to be considered as separate CMEs and ICMEs. The research leading to these results has received funding from the European Union’s Seventh Programme</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2009AdSpR..43..641D','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2009AdSpR..43..641D"><span>Possible <span class="hlt">influence</span> of <span class="hlt">solar</span> extreme events and related geomagnetic disturbances on human cardio-vascular state: Results of collaborative Bulgarian-Azerbaijani studies</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Dimitrova, S.; Mustafa, F. R.; Stoilova, I.; Babayev, E. S.; Kazimov, E. A.</p> <p>2009-02-01</p> <p>This collaborative study is based on the analysis and comparison of results of coordinated experimental investigations conducted in Bulgaria and Azerbaijan for revealing a possible <span class="hlt">influence</span> of <span class="hlt">solar</span> <span class="hlt">activity</span> changes and related geomagnetic <span class="hlt">activity</span> variations on the human cardio-vascular state. Arterial blood pressure and heart rate of 86 healthy volunteers were measured on working days during a period of comparatively high <span class="hlt">solar</span> and geomagnetic <span class="hlt">activity</span> (2799 measurements in autumn 2001 and spring 2002) in Sofia. Daily experimental investigations of parameters of cardio-vascular health state were performed in Azerbaijan with a permanent group of examined persons. Heart rate and electrocardiograms were digitally registered (in total 1532 records) for seven functionally healthy persons on working days and Saturdays, in the Laboratory of Heliobiology at the Medical Center INAM in Baku, from 15.07.2006 to 13.11.2007. Obtained digital recordings were subjected to medical, statistical and spectral analyses. Special attention was paid to effects of <span class="hlt">solar</span> extreme events, particularly those of November 2001 and December 2006. The statistical method of the analysis of variance (ANOVA) and post hoc analysis were applied to check the significance of the <span class="hlt">influence</span> of geomagnetic <span class="hlt">activity</span> on the cardio-vascular parameters under consideration. Results revealed statistically significant increments for the mean systolic and diastolic blood pressure values of the group with geomagnetic <span class="hlt">activity</span> increase. Arterial blood pressure values started increasing two days prior to geomagnetic storms and kept their high values up to two days after the storms. Heart rate reaction was ambiguous and not significant for healthy persons examined (for both groups) under conditions with geomagnetic <span class="hlt">activity</span> changes. It is concluded that heart rate for healthy persons at middle latitudes can be considered as a more stable physiological parameter which is not so sensitive to environmental changes</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/19940006941','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/19940006941"><span>NASDA <span class="hlt">activities</span> in space <span class="hlt">solar</span> power system research, development and applications</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Matsuda, Sumio; Yamamoto, Yasunari; Uesugi, Masato</p> <p>1993-01-01</p> <p>NASDA <span class="hlt">activities</span> in <span class="hlt">solar</span> cell research, development, and applications are described. First, current technologies for space <span class="hlt">solar</span> cells such as Si, GaAs, and InP are reviewed. Second, future space <span class="hlt">solar</span> cell technologies intended to be used on satellites of 21st century are discussed. Next, the flight data of <span class="hlt">solar</span> cell monitor on ETS-V is shown. Finally, establishing the universal space <span class="hlt">solar</span> cell calibration system is proposed.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2018Ge%26Ae..58..201K','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2018Ge%26Ae..58..201K"><span>Geomagnetic Storm Effects at F1 Layer Altitudes in Various Periods of <span class="hlt">Solar</span> <span class="hlt">Activity</span> (Irkutsk Station)</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Kushnarenko, G. P.; Yakovleva, O. E.; Kuznetsova, G. M.</p> <p>2018-03-01</p> <p>The <span class="hlt">influence</span> of geomagnetic disturbances on electron density Ne at F1 layer altitudes in different conditions of <span class="hlt">solar</span> <span class="hlt">activity</span> during the autumnal and vernal seasons of 2003-2015, according to the data from the Irkutsk digital ionospheric station (52° N, 104° E) is examined. Variations of Ne at heights of 150-190 km during the periods of twenty medium-scale and strong geomagnetic storms have been analyzed. At these specified heights, a vernal-autumn asymmetry of geomagnetic storm effects is discovered in all periods of <span class="hlt">solar</span> <span class="hlt">activity</span> of 2003-2015: a considerable Ne decrease at a height of 190 km and a weaker effect at lower levels during the autumnal storms. During vernal storms, no significant Ne decrease as compared with quiet conditions was registered over the entire analyzed interval of 150-190 km.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2011CoSka..41..137M','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2011CoSka..41..137M"><span>The green corona database and the coronal index of <span class="hlt">solar</span> <span class="hlt">activity</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Minarovjech, M.; Rušin, V.; Saniga, M.</p> <p>2011-10-01</p> <p>The green coronal line Fe XIV 530.3 nm ranks amongst the most pronounced emission lines in the visible part of the <span class="hlt">solar</span> spectrum. Its observations outside <span class="hlt">solar</span> eclipses started sporadically in 1939 (the Arosa coronal station), being extended, in 1946, to more coronal stations. It was found that the green corona intensities vary with <span class="hlt">solar</span> cycle, so they are a good candidate to express <span class="hlt">solar</span> <span class="hlt">activity</span> in the corona. Several attempts have been made to create a single homogeneous coronal data set from different coronal stations. We will present our homogeneous coronal data set, based on the Lomnický Štít photometric scale. Also, the coronal index of <span class="hlt">solar</span> <span class="hlt">activity</span> as created from this database in the period 1939—2010 will be discussed.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2003E%26PSL.206...15G','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2003E%26PSL.206...15G"><span>Changes in the relationship NAO-Northern hemisphere temperature due to <span class="hlt">solar</span> <span class="hlt">activity</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Gimeno, Luis; de la Torre, Laura; Nieto, Raquel; García, Ricardo; Hernández, Emiliano; Ribera, Pedro</p> <p>2003-01-01</p> <p>The <span class="hlt">influence</span> of the North Atlantic Oscillation (NAO) on wintertime Northern Hemisphere Temperature (NHT) is investigated. The results suggest that this relationship has different sign according to the phase of the <span class="hlt">solar</span> cycle. For <span class="hlt">solar</span> maximum phases NAO and NHT are positively correlated - a result assumed up to the moment - but for <span class="hlt">solar</span> minimum phases correlations are not significant or even negative. This result is in agreement with the different extension of the NAO for <span class="hlt">solar</span> cycle phases [Kodera, Geophys. Res. Lett. 29 (2002) 14557-14560] - almost hemispheric for maximum phases and confined to the eastern Atlantic for minimum phases.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017AGUFMSA51A2381A','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017AGUFMSA51A2381A"><span>NmF2 Morphology during four-classes of <span class="hlt">solar</span> and magnetic <span class="hlt">activity</span> conditions at an African station around the EIA trough and comparison with IRI-2016 Map</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Adebesin, B.; Rabiu, B.; Obrou, O. K.</p> <p>2017-12-01</p> <p>Better understanding of the electrodynamics between parameters used in describing the ionospheric layer and their <span class="hlt">solar</span> and geomagnetic <span class="hlt">influences</span> goes a long way in furthering the expansion of space weather knowledge. Telecommunication and scientific radar launch <span class="hlt">activities</span> can however be interrupted either on a larger/smaller scales by geomagnetic <span class="hlt">activities</span> which is susceptible to changes in <span class="hlt">solar</span> <span class="hlt">activity</span> and effects. Consequently, the ionospheric NmF2 electrodynamics was investigated for a station near the magnetic dip in the African sector (Korhogo, Geomagnetic: -1.26°N, 67.38°E). Data covering years 1996 and 2000 were investigated for four categories of magnetic and <span class="hlt">solar</span> <span class="hlt">activities</span> viz (i) F10.7 < 85 sfu, ap ≤ 7 nT (low <span class="hlt">solar</span> quiet, LSQ); (ii) F10.7 < 85 sfu, ap > 7 nT (low <span class="hlt">solar</span> disturbed, LSD); (iii) F10.7 > 150 sfu, ap ≤ 7 nT (high <span class="hlt">solar</span> quiet, HSQ); and (iv) F10.7 > 150 sfu, ap > 7 nT (high <span class="hlt">solar</span> disturbed, HSD). NmF2 revealed a pre-noon peak higher than the post-noon peak during high <span class="hlt">solar</span> <span class="hlt">activity</span> irrespective of magnetic <span class="hlt">activity</span> condition and overturned during low <span class="hlt">solar</span> <span class="hlt">activity</span>. Higher NmF2 peak amplitude however characterise disturbed magnetic <span class="hlt">activity</span> than quiet magnetic condition for any <span class="hlt">solar</span> <span class="hlt">activity</span>. The maximum pre-/post-noon peaks appeared in equinox season. June solstice noon-time bite out lagged other seasons by 1-2 h. Daytime variability increases with increasing magnetic <span class="hlt">activity</span>. Equinox/June solstice recorded the highest pre-sunrise/post-sunset peak variability magnitudes with the lowest emerging in June solstice/equinox for all <span class="hlt">solar</span> and magnetic conditions. The nighttime annual variability amplitude is higher during disturbed than quiet condition regardless of <span class="hlt">solar</span> <span class="hlt">activity</span> period; while the range is similar for daytime observations. The noon-time trough characteristics is not significant in the IRI NmF2 pattern during high <span class="hlt">solar</span> <span class="hlt">activity</span> but evident during low <span class="hlt">solar</span> conditions. IRI-2016 map performed best during disturbed</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2013IAUS..294...65G','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2013IAUS..294...65G"><span>Comparison of <span class="hlt">solar</span> <span class="hlt">activity</span> during last two minima on turn of <span class="hlt">Activity</span> Cycles 22/23 and 23/24</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; Gburek, Szymon; Siarkowski, Marek; Podgorski, Piotr; Sylwester, Janusz; Farnik, Frantisek</p> <p>2013-07-01</p> <p>The subject of our work is the review and comparison of <span class="hlt">solar</span> <span class="hlt">activity</span> during the last two <span class="hlt">solar</span> minima that occurred between recent <span class="hlt">activity</span> cycles. We use the soft X-ray global <span class="hlt">solar</span> corona observations covering the two nine-months long time intervals in 1997/98 and 2009. Data from RF15-I multichannel photometer are used for the penultimate minimum. For the last unusually deep and prolonged <span class="hlt">solar</span> <span class="hlt">activity</span> minimum in 2009 the data from SphinX spectrophotometer are used. Comparison of measurements from both minima takes place in the overlapping energy range 2-15 keV. We focus on the <span class="hlt">active</span> region formation, evolution and flaring productivity during respective minima.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2016AGUFMSH12B..07L','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2016AGUFMSH12B..07L"><span><span class="hlt">Solar</span> Eruptive <span class="hlt">Activity</span> at Mars' Orbit and its Potential Impacts</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Luhmann, J. G.; Lee, C. O.; Curry, S.; Hara, T.; Halekas, J. S.; Li, Y.; Dong, C.; Ma, Y.; Lillis, R. J.; Dunn, P.; Gruesbeck, J.; Espley, J. R.; Brain, D.; Connerney, J. E. P.; Larson, D. E.; Jakosky, B. M.; Russell, C. T.</p> <p>2016-12-01</p> <p>While a number of studies exist relating to ICME signatures at Venus (PVO and VEX) and Mercury (Helios and Messenger), relatively few analyses exist for Mars' orbit. Nevertheless plasma and field signatures of ICMEs have been observed in the space near Mars by Phobos-2, Mars Global Surveyor (MGS), Mars Express (MEX), and now MAVEN. Of these, MAVEN is arguably best-instrumented, space weather-wise, to characterize such events. However, the weak <span class="hlt">solar</span> <span class="hlt">activity</span> over the past decade has limited what MAVEN, whose mission is to study Mars' atmospheric response to <span class="hlt">solar</span> <span class="hlt">activity</span>, including escape to space, has been able to observe. While the major October 1989 event, that produced at Earth one of the largest geomagnetic storms on record, occurred during the short Phobos-2 mission, and the notable series of Halloween 2003 storms occurred during the MGS mission, MAVEN has detected only moderate <span class="hlt">solar</span> eruptive <span class="hlt">activity</span>-related interplanetary disturbances at Mars. We compare the largest ICME observed by MAVEN with some of these other more extreme <span class="hlt">activity</span> episodes for perspective. These comparisons hint at the potential impact of the magnitude of <span class="hlt">solar</span> eruptions on what is experienced at Mars orbit, and on our ability to investigate planetary responses over the full range -when missions are at the mercy of what the <span class="hlt">solar</span> cycle produces during their lifetimes.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2010cosp...38.1763V','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2010cosp...38.1763V"><span>The Little Ice Age and <span class="hlt">Solar</span> <span class="hlt">Activity</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Velasco Herrera, Victor Manuel; Leal Silva, C. M. Carmen; Velasco Herrera, Graciela</p> <p></p> <p>We analyze the ice winter severity index on the Baltic region since 1501-1995. We found that the variability of this index is modulated among other factors by the secular <span class="hlt">solar</span> <span class="hlt">activity</span>. The little ice ages that have appeared in the North Hemisphere occurred during periods of low <span class="hlt">solar</span> <span class="hlt">activity</span>. Seemingly our star is experiencing a new quiet stage compared with Maunder or Dalton minimum, this is important because it is estimated that even small changes in weather can represent a great impact in ice index. These results are relevant since ice is a very important element in the climate system of the Baltic region and it can affect directly or indirectly many of the oceanographic, climatic, eco-logical, economical and cultural patterns.</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.osti.gov/biblio/22520075-activity-analyses-solar-type-stars-observed-kepler-proxies-magnetic-activity','SCIGOV-STC'); return false;" href="https://www.osti.gov/biblio/22520075-activity-analyses-solar-type-stars-observed-kepler-proxies-magnetic-activity"><span><span class="hlt">ACTIVITY</span> ANALYSES FOR <span class="hlt">SOLAR</span>-TYPE STARS OBSERVED WITH KEPLER. I. PROXIES OF MAGNETIC <span class="hlt">ACTIVITY</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>He, Han; Wang, Huaning; Yun, Duo, E-mail: hehan@nao.cas.cn</p> <p>2015-11-15</p> <p>Light curves of <span class="hlt">solar</span>-type stars often show gradual fluctuations due to rotational modulation by magnetic features (starspots and faculae) on stellar surfaces. Two quantitative measures of modulated light curves are employed as the proxies of magnetic <span class="hlt">activity</span> for <span class="hlt">solar</span>-type stars observed with Kepler telescope. The first is named autocorrelation index i{sub AC}, which describes the degree of periodicity of the light curve; the second is the effective fluctuation range of the light curve R{sub eff}, which reflects the depth of rotational modulation. The two measures are complementary and depict different aspects of magnetic <span class="hlt">activities</span> on <span class="hlt">solar</span>-type stars. By using themore » two proxies i{sub AC} and R{sub eff}, we analyzed <span class="hlt">activity</span> properties of two carefully selected <span class="hlt">solar</span>-type stars observed with Kepler (Kepler ID: 9766237 and 10864581), which have distinct rotational periods (14.7 versus 6.0 days). We also applied the two measures to the Sun for a comparative study. The result shows that both the measures can reveal cyclic <span class="hlt">activity</span> variations (referred to as i{sub AC}-cycle and R{sub eff}-cycle) on the two Kepler stars and the Sun. For the Kepler star with the faster rotation rate, i{sub AC}-cycle and R{sub eff}-cycle are in the same phase, while for the Sun (slower rotator), they are in the opposite phase. By comparing the <span class="hlt">solar</span> light curve with simultaneous photospheric magnetograms, it is identified that the magnetic feature that causes the periodic light curve during <span class="hlt">solar</span> minima is the faculae of the enhanced network region, which can also be a candidate of magnetic features that dominate the periodic light curves on the two Kepler stars.« less</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/19760007440','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/19760007440"><span>Possible relationships between <span class="hlt">solar</span> <span class="hlt">activity</span> and meteorological phenomena</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Bandeen, W. R. (Editor); Maran, S. P. (Editor)</p> <p>1975-01-01</p> <p>A symposium was conducted in which the following questions were discussed: (1) the evidence concerning possible relationships between <span class="hlt">solar</span> <span class="hlt">activity</span> and meteorological phenomena; (2) plausible physical mechanisms to explain these relationships; and (3) kinds of critical measurements needed to determine the nature of <span class="hlt">solar</span>/meteorological relationships and/or the mechanisms to explain them, and which of these measurements can be accomplished best from space.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/27822328','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/27822328"><span><span class="hlt">Solar</span> optics-based <span class="hlt">active</span> panel for <span class="hlt">solar</span> energy storage and disinfection of greywater.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Lee, W; Song, J; Son, J H; Gutierrez, M P; Kang, T; Kim, D; Lee, L P</p> <p>2016-09-01</p> <p>Smart city and innovative building strategies are becoming increasingly more necessary because advancing a sustainable building system is regarded as a promising solution to overcome the depleting water and energy. However, current sustainable building systems mainly focus on energy saving and miss a holistic integration of water regeneration and energy generation. Here, we present a theoretical study of a <span class="hlt">solar</span> optics-based <span class="hlt">active</span> panel (SOAP) that enables both <span class="hlt">solar</span> energy storage and photothermal disinfection of greywater simultaneously. <span class="hlt">Solar</span> collector efficiency of energy storage and disinfection rate of greywater have been investigated. Due to the light focusing by microlens, the <span class="hlt">solar</span> collector efficiency is enhanced from 25% to 65%, compared to that without the microlens. The simulation of greywater sterilization shows that 100% disinfection can be accomplished by our SOAP for different types of bacteria including Escherichia coli . Numerical simulation reveals that our SOAP as a lab-on-a-wall system can resolve the water and energy problem in future sustainable building systems.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=5085975','PMC'); return false;" href="https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=5085975"><span><span class="hlt">Solar</span> optics-based <span class="hlt">active</span> panel for <span class="hlt">solar</span> energy storage and disinfection of greywater</span></a></p> <p><a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pmc">PubMed Central</a></p> <p>Lee, W.; Song, J.; Son, J. H.; Gutierrez, M. P.; Kang, T.; Kim, D.; Lee, L. P.</p> <p>2016-01-01</p> <p>Smart city and innovative building strategies are becoming increasingly more necessary because advancing a sustainable building system is regarded as a promising solution to overcome the depleting water and energy. However, current sustainable building systems mainly focus on energy saving and miss a holistic integration of water regeneration and energy generation. Here, we present a theoretical study of a <span class="hlt">solar</span> optics-based <span class="hlt">active</span> panel (SOAP) that enables both <span class="hlt">solar</span> energy storage and photothermal disinfection of greywater simultaneously. <span class="hlt">Solar</span> collector efficiency of energy storage and disinfection rate of greywater have been investigated. Due to the light focusing by microlens, the <span class="hlt">solar</span> collector efficiency is enhanced from 25% to 65%, compared to that without the microlens. The simulation of greywater sterilization shows that 100% disinfection can be accomplished by our SOAP for different types of bacteria including Escherichia coli. Numerical simulation reveals that our SOAP as a lab-on-a-wall system can resolve the water and energy problem in future sustainable building systems. PMID:27822328</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://ntrs.nasa.gov/search.jsp?R=20070018224&hterms=Beer&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D20%26Ntt%3DBeer','NASA-TRS'); return false;" href="https://ntrs.nasa.gov/search.jsp?R=20070018224&hterms=Beer&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D20%26Ntt%3DBeer"><span><span class="hlt">Solar</span> Forced Dansgaard/Oeschger Events?</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Muscheler, R.; Beer, J.</p> <p>2006-01-01</p> <p>Climate records for the last ice age (which ended 11,500 years ago) show enormous climate fluctuations in the North Atlantic region - the so-called Dansgaard/Oeschger events. During these events air temperatures in Greenland changed on the order of 10 degrees Celsius within a few decades. These changes were attributed to shifts in ocean circulation which <span class="hlt">influences</span> the warm water supply from lower latitudes to the North Atlantic region. Interestingly, the rapid warmings tend to recur approximately every 1500 years or multiples thereof. This has led researchers to speculate about an external cause for these changes with the variable Sun being one possible candidate. Support for this hypothesis came from climate reconstructions, which suggested that the Sun <span class="hlt">influenced</span> the climate in the North Atlantic region on these time scales during the last approximately 12,000 years of relatively stable Holocene climate. However, Be-10 measurements in ice cores do not indicate that the Sun caused or triggered the Dansgaard/Oeschger events. Depending on the <span class="hlt">solar</span> magnetic shielding more or less Be-10 is produced in the Earth's atmosphere. Therefore, 10Be can be used as a proxy for <span class="hlt">solar</span> <span class="hlt">activity</span> changes. Since Be-10 can be measured in ice cores, it is possible to compare the variable <span class="hlt">solar</span> forcing directly with the climate record from the same ice core. This removes any uncertainties in the relative dating, and the <span class="hlt">solar</span>-climate link can be reliably studied. Notwithstanding that some Dansgaard/Oeschger warmings could be related to increased <span class="hlt">solar</span> <span class="hlt">activity</span>, there is no indication that this is the case for all of the Dansgaard/Oeschger events. Therefore, during the last ice age the Be-10 and ice core climate data do not indicate a persistent <span class="hlt">solar</span> <span class="hlt">influence</span> on North Atlantic climate.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2011AAS...21841102H','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2011AAS...21841102H"><span>The <span class="hlt">Solar</span> System Ballet: A Kinesthetic Spatial Astronomy <span class="hlt">Activity</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Heyer, Inge; Slater, T. F.; Slater, S. J.; Astronomy, Center; Education ResearchCAPER, Physics</p> <p>2011-05-01</p> <p>The <span class="hlt">Solar</span> System Ballet was developed in order for students of all ages to learn about the planets, their motions, their distances, and their individual characteristics. To teach people about the structure of our <span class="hlt">Solar</span> System can be revealing and rewarding, for students and teachers. Little ones (and some bigger ones, too) often cannot yet grasp theoretical and spatial ideas purely with their minds. Showing a video is better, but being able to learn with their bodies, essentially being what they learn about, will help them understand and remember difficult concepts much more easily. There are three segments to this <span class="hlt">activity</span>, which can be done together or separately, depending on time limits and age of the students. Part one involves a short introductory discussion about what students know about the planets. Then students will act out the orbital motions of the planets (and also moons for the older ones) while holding a physical model. During the second phase we look at the structure of the <span class="hlt">Solar</span> System as well as the relative distances of the planets from the Sun, first by sketching it on paper, then by recreating a scaled version in the class room. Again the students act out the parts of the <span class="hlt">Solar</span> System bodies with their models. The third segment concentrates on recreating historical measurements of Earth-Moon-Sun system. The <span class="hlt">Solar</span> System Ballet <span class="hlt">activity</span> is suitable for grades K-12+ as well as general public informal learning <span class="hlt">activities</span>.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/20120015708','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/20120015708"><span>Wavelength Dependence of <span class="hlt">Solar</span> Flare Irradiation and its <span class="hlt">Influence</span> on the Thermosphere</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Huang, Yanshi; Richmond, Arthur D.; Deng, Yue; Qian, L.; Solomon, S.; Chamberlin, P.</p> <p>2012-01-01</p> <p>The wavelength dependence of <span class="hlt">solar</span> flare enhancement is one of the important factors determining how the Thermosphere-Ionosphere (T-I) system response to flares. To investigate the wavelength dependence of <span class="hlt">solar</span> flare, the Flare Irradiance Spectral Model (FISM) has been run for 34 X-class flares. The results show that the percentage increases of <span class="hlt">solar</span> irradiance at flare peak comparing to pre-flare condition have a clear wavelength dependence. In the wavelength range between 0 - 195 nm, it can vary from 1% to 10000%. The <span class="hlt">solar</span> irradiance enhancement is largest ( 1000%) in the XUV range (0 - 25 nm), and is about 100% in EUV range (25 - 120 nm). The <span class="hlt">influence</span> of different wavebands on the T-I system during the October 28th, 2003 flare (X17.2-class) has also been examined using the latest version of National Center for Atmospheric Research (NCAR) Thermosphere- Ionosphere-Electrodynamics General Circulation Model (TIE-GCM). While the globally integrated <span class="hlt">solar</span> energy deposition is largest in the 0 - 14 nm waveband, the impact of <span class="hlt">solar</span> irradiance enhancement on the thermosphere at 400 km is largest for 25 - 105 nm waveband. The effect of 122 - 195 nm is small in magnitude, but it decays slowly.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://ntrs.nasa.gov/search.jsp?R=19960021256&hterms=activity+Physics&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D50%26Ntt%3Dactivity%2BPhysics','NASA-TRS'); return false;" href="https://ntrs.nasa.gov/search.jsp?R=19960021256&hterms=activity+Physics&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D50%26Ntt%3Dactivity%2BPhysics"><span>Helioseismology: A probe of the <span class="hlt">solar</span> interior, atmosphere, and <span class="hlt">activity</span> cycle</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Rhodes, E. J., Jr.</p> <p>1995-01-01</p> <p>Helioseismology began in earnest in the mid 1970's. In the two decades which have elapsed since that time this branch of <span class="hlt">solar</span> physics has become a mature field of research. Helioseismology has demonstrated that the <span class="hlt">solar</span> convection zone is about twice as deep as was generally thought to be the case before 1977. Helioseismology has also provided measurements of the <span class="hlt">solar</span> internal angular velocity over much of the sun's interior. Helioseismology has also ruled out models which would solve the <span class="hlt">solar</span> neutrino problem by a lowering of the temperature of the core. Recently, some of the seismic properties of the sun have been demonstrated to vary with changing levels of <span class="hlt">solar</span> <span class="hlt">activity</span>. Also, helioseismology has recently provided evidence for helical flow patterns in the shallow, sub-photosphere layers. The techniques of helioseismology are also expanding to include seismic probes of <span class="hlt">solar</span> <span class="hlt">active</span> regions. Some work is also being conducted into the possible contributions of the <span class="hlt">solar</span> acoustic models to the heating of the <span class="hlt">solar</span> atmosphere. In this talk I will highlight a few of the above results and concentrate on current areas of research in the field.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2007AGUFMED51B0423H','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2007AGUFMED51B0423H"><span>Caught in the <span class="hlt">Solar</span> Wind: A Study of Space Weather and its <span class="hlt">Influence</span> on Earth</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Hill, R.; Chuckran, A.; Erickson, P. J.</p> <p>2007-12-01</p> <p>Space weather is a phenomenon that is becoming more familiar to the general public. As people are increasingly reliant on 21st century technology, the potential for disruption to their daily lives also rises. As the sun approaches its next <span class="hlt">solar</span> maximum in 2011 or 2012, the peak of Cycle 24 is expected to be the highest of the satellite age, perhaps surpassing that of Cycle 19 in 1957-58. In this teaching unit, we have attempted to create a series of lessons that sheds light on the concept of space weather and the sun's <span class="hlt">influences</span> on earth's magnetic field and upper atmosphere. Within this unit, we have provided ample opportunities for students to access and interpret real scientific data from a variety of sources. The main location is the web site www.spaceweather.com , which has near real time data from satellites such as SOHO, STEREO, ACE and POES. This data is easily viewed and explained within the site, and with appropriate instruction, students can regularly gather data, make predictions, and draw conclusions based on the current behavior of the sun. Examples include sunspot number and development, speed and density of <span class="hlt">solar</span> wind, orientation and strength of the interplanetary magnetic field, location of coronal holes, planetary K index and X-ray <span class="hlt">solar</span> flares. Depending on the level of the students, some or all of this data can be compiled over a period of time to better understand the behavior of the sun as well as its <span class="hlt">influence</span> on Earth. The goal of this unit is to provide a vehicle for students to understand how data is used by scientists. Once they have the base knowledge, students may be able to construct their own questions and follow through with research. An inquiry-based approach is incorporated whenever possible. With the onset of a potentially <span class="hlt">active</span> <span class="hlt">solar</span> cycle in the near future, teachers have the opportunity to make a dramatic connection between the natural world and their daily lives. <span class="hlt">Solar</span> storms can cause disruption to telephone communication</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2018SFZ.....4a..33M','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2018SFZ.....4a..33M"><span>Fe/O ratio behavior as an indicator of <span class="hlt">solar</span> plasma state at different <span class="hlt">solar</span> <span class="hlt">activity</span> manifestations and in periods of their absence</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Minasyants, Gennady; Minasyants, Tamara; Tomozov, Vladimir</p> <p>2018-03-01</p> <p> the decisive <span class="hlt">influence</span> of galactic cosmic rays on the composition of impurity elements in the <span class="hlt">solar</span> wind under <span class="hlt">solar</span> minimum conditions. The relative content of heavy elements in galactic cosmic rays 30-500 MeV/n is similar to values in fluxes from gradual flares during high <span class="hlt">solar</span> <span class="hlt">activity</span>. During <span class="hlt">solar</span> minimum without sunspots, the behavior of Fe/O for different ion energy ranges in plasma flows from coronal holes (CH) and in the <span class="hlt">solar</span> wind exhibits only minor deviations. At the same time, plasma flows associated with the disturbed frontal CH region can be sources of moderate geomagnetic storms.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=5099841','PMC'); return false;" href="https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=5099841"><span><span class="hlt">Influence</span> of chemically p-type doped <span class="hlt">active</span> organic semiconductor on the film thickness versus performance trend in cyanine/C60 bilayer <span class="hlt">solar</span> 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>Jenatsch, Sandra; Geiger, Thomas; Heier, Jakob; Kirsch, Christoph; Nüesch, Frank; Paracchino, Adriana; Rentsch, Daniel; Ruhstaller, Beat; C Véron, Anna; Hany, Roland</p> <p>2015-01-01</p> <p>Simple bilayer organic <span class="hlt">solar</span> cells rely on very thin coated films that allow for effective light absorption and charge carrier transport away from the heterojunction at the same time. However, thin films are difficult to coat on rough substrates or over large areas, resulting in adverse shorting and low device fabrication yield. Chemical p-type doping of organic semiconductors can reduce Ohmic losses in thicker transport layers through increased conductivity. By using a Co(III) complex as chemical dopant, we studied doped cyanine dye/C60 bilayer <span class="hlt">solar</span> cell performance for increasing dye film thickness. For films thicker than 50 nm, doping increased the power conversion efficiency by more than 30%. At the same time, the yield of working cells increased to 80%. We addressed the fate of the doped cyanine dye, and found no <span class="hlt">influence</span> of doping on <span class="hlt">solar</span> cell long term stability. PMID:27877804</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://ntrs.nasa.gov/search.jsp?R=19950031090&hterms=activity+Physics&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D50%26Ntt%3Dactivity%2BPhysics','NASA-TRS'); return false;" href="https://ntrs.nasa.gov/search.jsp?R=19950031090&hterms=activity+Physics&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D50%26Ntt%3Dactivity%2BPhysics"><span>Long-term persistence of <span class="hlt">solar</span> <span class="hlt">activity</span></span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Ruzmaikin, Alexander; Feynman, Joan; Robinson, Paul</p> <p>1994-01-01</p> <p>We examine the question of whether or not the non-periodic variations in <span class="hlt">solar</span> <span class="hlt">activity</span> are caused by a white-noise, random process. The Hurst exponent, which characterizes the persistence of a time series, is evaluated for the series of C-14 data for the time interval from about 6000 BC to 1950 AD. We find a constant Hurst exponent, suggesting that <span class="hlt">solar</span> <span class="hlt">activity</span> in the frequency range from 100 to 3000 years includes an important continuum component in addition to the well-known periodic variations. The value we calculate, H approximately 0.8, is significantly larger than the value of 0.5 that would correspond to variations produced by a white-noise process. This value is in good agreement with the results for the monthly sunspot data reported elsewhere, indicating that the physics that produces the continuum is a correlated random process and that it is the same type of process over a wide range of time interval lengths.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://ntrs.nasa.gov/search.jsp?R=19790037880&hterms=Krieger&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D20%26Ntt%3DKrieger','NASA-TRS'); return false;" href="https://ntrs.nasa.gov/search.jsp?R=19790037880&hterms=Krieger&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D20%26Ntt%3DKrieger"><span>The relationship between <span class="hlt">solar</span> <span class="hlt">activity</span> and coronal hole evolution</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Nolte, J. T.; Davis, J. M.; Gerassimenko, M.; Krieger, A. S.; Solodyna, C. V.; Golub, L.</p> <p>1978-01-01</p> <p>The relationship between coronal hole evolution and <span class="hlt">solar</span> <span class="hlt">active</span> regions during the Skylab period is examined. A tendency is found for holes to grow or remain stable when the <span class="hlt">activity</span> nearby, seen as calcium plages and bright regions in X-rays, is predominantly large, long-lived regions. It is also found that there is a significantly higher number of small, short-lived <span class="hlt">active</span> regions, as indicated by X-ray bright points, in the vicinity of decaying holes than there is near other holes. This is interpreted to mean that holes disappear at least in part because they become filled with many small scale, magnetically closed, X-ray emitting features. This interpretation, together with the observation that the number of X-ray bright points was much larger near <span class="hlt">solar</span> minimum than it was during the Skylab period, provides a possible explanation for the disappearance of the large, near-equatorial coronal holes at the time of <span class="hlt">solar</span> minimum.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2003EAEJA.....2835D','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2003EAEJA.....2835D"><span>Changes in the relationship NAO-Northern Hemisphere Temperature due to <span class="hlt">solar</span> <span class="hlt">activity</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>de La Torre, L.; Gimeno, L.; Añel, J. A.; Nieto, R.; Tesouro, M.; Ribera, P.; García, R.; Hernández, E.</p> <p>2003-04-01</p> <p>The <span class="hlt">influence</span> of the North Atlantic Oscillation (NAO) on wintertime Northern Hemisphere Temperature (NHT) is investigated. To check the hypothesis that the <span class="hlt">solar</span> cycle is modulating this relationship, the sample was divided into two groups, one included the years corresponding to the three consecutive lowest values of sunspots number for every 11-years cycle (43 years) and the other the ones corresponding to the three consecutive highest numbers (39 years) for every 11-years cycle. If the data of each year were independent, the correlation coefficients between NAO index and NHT for 43 (39) years would be 0.30 (0.32) at 95% confidence level. Correlation index corresponding to the <span class="hlt">solar</span> minimum phases was -0.17 and to the <span class="hlt">solar</span> maximum phases was 0.35. The second result is statistically significant and indicates that there are periods when a positive phase of the NAO is related to positive anomalies of NHT- result that supports our current idea of the <span class="hlt">influence</span> of the NAO on temperature- but there are other periods when NAO and NHT are not correlated. So, results suggest that this relationship has different sign according to the phase of the <span class="hlt">solar</span> cycle. For <span class="hlt">solar</span> maximum phases NAO and NHT are positively correlated -result assumed up to the moment- but for <span class="hlt">solar</span> minimum phases correlations are not significant or even negative. This result is in agreement with the different extension of the NAO for <span class="hlt">solar</span> cycle phases [1] - almost hemispheric for maximum phases and confined to the eastern Atlantic for minimum phases-.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://ntrs.nasa.gov/search.jsp?R=20070001986&hterms=Vantage&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D80%26Ntt%3DVantage','NASA-TRS'); return false;" href="https://ntrs.nasa.gov/search.jsp?R=20070001986&hterms=Vantage&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D80%26Ntt%3DVantage"><span>The Heliosphere Through the <span class="hlt">Solar</span> <span class="hlt">Activity</span> Cycle</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Balogh, A.; Lanzerotti, L. J.; Suess, S. T.</p> <p>2006-01-01</p> <p>Understanding how the Sun changes though its 11-year sunspot cycle and how these changes affect the vast space around the Sun the heliosphere has been one of the principal objectives of space research since the advent of the space age. This book presents the evolution of the heliosphere through an entire <span class="hlt">solar</span> <span class="hlt">activity</span> cycle. The last <span class="hlt">solar</span> cycle (cycle 23) has been the best observed from both the Earth and from a fleet of spacecraft. Of these, the joint ESA-NASA Ulysses probe has provided continuous observations of the state of the heliosphere since 1990 from a unique vantage point, that of a nearly polar orbit around the Sun. Ulysses results affect our understanding of the heliosphere from the interior of the Sun to the interstellar medium - beyond the outer boundary of the heliosphere. Written by scientists closely associated with the Ulysses mission, the book describes and explains the many different aspects of changes in the heliosphere in response to <span class="hlt">solar</span> <span class="hlt">activity</span>. In particular, the authors describe the rise in <span class="hlt">solar</span> ESA and NASA have now unamiously agreed a third extension to operate the highly successful Ulysses spacecraft until March 2008 and, in 2007 and 2008, the European-built space probe will fly over the poles of the Sun for a third time. This will enable Ulysses to add an important chapter to its survey of the high-latitude heliosphere and this additional material would be included in a 2nd edition of this book.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/20080022945','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/20080022945"><span>On the Relationship Between <span class="hlt">Solar</span> Wind Speed, Geomagnetic <span class="hlt">Activity</span>, and the <span class="hlt">Solar</span> Cycle Using Annual Values</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Wilson, Robert M.; Hathaway, David H.</p> <p>2008-01-01</p> <p>The aa index can be decomposed into two separate components: the leading sporadic component due to <span class="hlt">solar</span> <span class="hlt">activity</span> as measured by sunspot number and the residual or recurrent component due to interplanetary disturbances, such as coronal holes. For the interval 1964-2006, a highly statistically important correlation (r = 0.749) is found between annual averages of the aa index and the <span class="hlt">solar</span> wind speed (especially between the residual component of aa and the <span class="hlt">solar</span> wind speed, r = 0.865). Because cyclic averages of aa (and the residual component) have trended upward during cycles 11-23, cyclic averages of <span class="hlt">solar</span> wind speed are inferred to have also trended upward.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2018AdSpR..61..639D','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2018AdSpR..61..639D"><span>Non-stationarity and cross-correlation effects in the MHD <span class="hlt">solar</span> <span class="hlt">activity</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Demin, S. A.; Nefedyev, Y. A.; Andreev, A. O.; Demina, N. Y.; Timashev, S. F.</p> <p>2018-01-01</p> <p>The analysis of turbulent processes in sunspots and pores which are self-organizing long-lived magnetic structures is a complicated and not yet solved problem. The present work focuses on studying such magneto-hydrodynamic (MHD) formations on the basis of flicker-noise spectroscopy using a new method of multi-parametric analysis. The non-stationarity and cross-correlation effects taking place in <span class="hlt">solar</span> <span class="hlt">activity</span> dynamics are considered. The calculated maximum values of non-stationarity factor may become precursors of significant restructuring in <span class="hlt">solar</span> magnetic <span class="hlt">activity</span>. The introduced cross-correlation functions enable us to judge synchronization effects between the signals of various <span class="hlt">solar</span> <span class="hlt">activity</span> indicators registered simultaneously.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2014cosp...40E3353T','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2014cosp...40E3353T"><span>Major geomagnetic storm due to <span class="hlt">solar</span> <span class="hlt">activity</span> (2006-2013).</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Tiwari, Bhupendra Kumar</p> <p></p> <p>Major geomagnetic storm due to <span class="hlt">solar</span> <span class="hlt">activity</span> (2006-2013). Bhupendra Kumar Tiwari Department of Physics, A.P.S.University, Rewa(M.P.) Email: - btiwtari70@yahoo.com mobile 09424981974 Abstract- The geospace environment is dominated by disturbances created by the sun, it is observed that coronal mass ejection (CME) and <span class="hlt">solar</span> flare events are the causal link to <span class="hlt">solar</span> <span class="hlt">activity</span> that produces geomagnetic storm (GMS).CMEs are large scale magneto-plasma structures that erupt from the sun and propagate through the interplanetary medium with speeds ranging from only a few km/s to as large as 4000 km/s. When the interplanetary magnetic field associated with CMEs impinges upon the earth’s magnetosphere and reconnect occur geomagnetic storm. Based on the observation from SOHO/LASCO spacecraft for <span class="hlt">solar</span> <span class="hlt">activity</span> and WDC for geomagnetism Kyoto for geomagnetic storm events are characterized by the disturbance storm time (Dst) index during the period 2006-2013. We consider here only intense geomagnetic storm Dst <-100nT, are 12 during 2006-2013.Geomagnetic storm with maximum Dst< -155nT occurred on Dec15, 2006 associated with halo CME with Kp-index 8+ and also verify that halo CME is the main cause to produce large geomagnetic storms.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/20170003802','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/20170003802"><span>Hinode: A Decade of Success in Capturing <span class="hlt">Solar</span> <span class="hlt">Activity</span></span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Savage, S.; Elrod, S.; Deluca, E.; Doschek, G.; Tarbell, T.</p> <p>2017-01-01</p> <p>As the present <span class="hlt">solar</span> cycle passes into its minimum phase, the Hinode mission marks its tenth year of investigating <span class="hlt">solar</span> <span class="hlt">activity</span>. Hinode's decade of successful observations have provided us with immeasurable insight into the <span class="hlt">solar</span> processes that invoke space weather and thereby affect the interplanetary environment in which we reside. The mission's complementary suite of instruments allows us to probe transient, high energy events alongside long-term, cycle-dependent phenomena from magnetic fields at the Sun's surface out to highly thermalized coronal plasma enveloping <span class="hlt">active</span> regions (ARs). These rich data sets have already changed the face of <span class="hlt">solar</span> physics and will continue to provoke exciting research as new observational paradigms are pursued. Hinode was launched as part of the Science Mission Directorate's (SMD) <span class="hlt">Solar</span> Terrestrial Probes Program in 2006. It is a sophisticated spacecraft equipped with a <span class="hlt">Solar</span> Optical Telescope (SOT), an Extreme-ultraviolet Imaging Spectrometer (EIS), and an X-Ray Telescope (XRT) (see x 4). With high resolution and sensitivity, Hinode serves as a microscope for the Sun, providing us with unique capabilities for observing magnetic fields near the smallest scales achievable, while also rendering full-Sun coronal context in the highest thermal regimes. The 2014 NASA SMD strategic goals objective to "Understand the Sun and its interactions with the Earth and the <span class="hlt">solar</span> system, including space weather" forms the basis of three underlying Heliophysics Science Goals. While Hinode relates to all three, the observatory primarily addresses: Explore the physical processes in the space environment from the Sun to the Earth and through the <span class="hlt">solar</span> system. Within the NASA National Research Council (NRC) Decadal Survey Priorities, Hinode targets: (a) Determine the origins of the Sun's <span class="hlt">activity</span> and predict the variations of the space environment and (d) Discover and characterize fundamental processes that occur both within the heliosphere and</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.nrel.gov/solar/seeds/webinars.html','SCIGOVWS'); return false;" href="https://www.nrel.gov/solar/seeds/webinars.html"><span><span class="hlt">Solar</span> Energy Evolution and Diffusion Studies Webinars | <span class="hlt">Solar</span> Research |</span></a></p> <p><a target="_blank" href="http://www.science.gov/aboutsearch.html">Science.gov Websites</a></p> <p></p> <p></p> <p>video Download the transcript Agent-based Models of How Segregation and Peer Effects <em><span class="hlt">Influence</span></em> <span class="hlt">Solar</span> PV to estimate the relative <em><span class="hlt">influence</span></em> of peer effects, cognitive factors, and economic factors in <span class="hlt">solar</span></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.osti.gov/biblio/22518569-magnetic-classification-solar-active-regions','SCIGOV-STC'); return false;" href="https://www.osti.gov/biblio/22518569-magnetic-classification-solar-active-regions"><span>THE MAGNETIC CLASSIFICATION OF <span class="hlt">SOLAR</span> <span class="hlt">ACTIVE</span> REGIONS 1992–2015</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>Jaeggli, S. A.; Norton, A. A., E-mail: sarah.jaeggli@nasa.gov</p> <p></p> <p>The purpose of this Letter is to address a blindspot in our knowledge of <span class="hlt">solar</span> <span class="hlt">active</span> region (AR) statistics. To the best of our knowledge, there are no published results showing the variation of the Mount Wilson magnetic classifications as a function of <span class="hlt">solar</span> cycle based on modern observations. We show statistics for all ARs reported in the daily <span class="hlt">Solar</span> Region Summary from 1992 January 1 to 2015 December 31. We find that the α and β class ARs (including all sub-groups, e.g., βγ, βδ) make up fractions of approximately 20% and 80% of the sample, respectively. This fraction ismore » relatively constant during high levels of <span class="hlt">activity</span>; however, an increase in the α fraction to about 35% and and a decrease in the β fraction to about 65% can be seen near each <span class="hlt">solar</span> minimum and are statistically significant at the 2σ level. Over 30% of all ARs observed during the years of <span class="hlt">solar</span> maxima were appended with the classifications γ and/or δ, while these classifications account for only a fraction of a percent during the years near the <span class="hlt">solar</span> minima. This variation in the AR types indicates that the formation of complex ARs may be due to the pileup of frequent emergence of magnetic flux during <span class="hlt">solar</span> maximum, rather than the emergence of complex, monolithic flux structures.« less</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017SoPh..292..167N','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017SoPh..292..167N"><span>The Effect of "Rogue" <span class="hlt">Active</span> Regions on the <span class="hlt">Solar</span> Cycle</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Nagy, Melinda; Lemerle, Alexandre; Labonville, François; Petrovay, Kristóf; Charbonneau, Paul</p> <p>2017-11-01</p> <p>The origin of cycle-to-cycle variations in <span class="hlt">solar</span> <span class="hlt">activity</span> is currently the focus of much interest. It has recently been pointed out that large individual <span class="hlt">active</span> regions with atypical properties can have a significant impact on the long-term behavior of <span class="hlt">solar</span> <span class="hlt">activity</span>. We investigate this possibility in more detail using a recently developed 2×2D dynamo model of the <span class="hlt">solar</span> magnetic cycle. We find that even a single "rogue" bipolar magnetic region (BMR) in the simulations can have a major effect on the further development of <span class="hlt">solar</span> <span class="hlt">activity</span> cycles, boosting or suppressing the amplitude of subsequent cycles. In extreme cases, an individual BMR can completely halt the dynamo, triggering a grand minimum. Rogue BMRs also have the potential to induce significant hemispheric asymmetries in the <span class="hlt">solar</span> cycle. To study the effect of rogue BMRs in a more systematic manner, a series of dynamo simulations were conducted, in which a large test BMR was manually introduced in the model at various phases of cycles of different amplitudes. BMRs emerging in the rising phase of a cycle can modify the amplitude of the ongoing cycle, while BMRs emerging in later phases will only affect subsequent cycles. In this model, the strongest effect on the subsequent cycle occurs when the rogue BMR emerges around cycle maximum at low latitudes, but the BMR does not need to be strictly cross-equatorial. <span class="hlt">Active</span> regions emerging as far as 20° from the equator can still have a significant effect. We demonstrate that the combined effect of the magnetic flux, tilt angle, and polarity separation of the BMR on the dynamo is via their contribution to the dipole moment, δ D_{BMR}. Our results indicate that prediction of the amplitude, starting epoch, and duration of a cycle requires an accurate accounting of a broad range of <span class="hlt">active</span> regions emerging in the previous cycle.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017EnMan..60..630S','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017EnMan..60..630S"><span>The <span class="hlt">Influence</span> of <span class="hlt">Solar</span> Power Plants on Microclimatic Conditions and the Biotic Community in Chilean Desert Environments</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Suuronen, Anna; Muñoz-Escobar, Christian; Lensu, Anssi; Kuitunen, Markku; Guajardo Celis, Natalia; Espinoza Astudillo, Pablo; Ferrú, Marcos; Taucare-Ríos, Andrés; Miranda, Marcelo; Kukkonen, Jussi V. K.</p> <p>2017-10-01</p> <p>The renewable energy sector is growing at a rapid pace in northern Chile and the <span class="hlt">solar</span> energy potential is one of the best worldwide. Therefore, many types of <span class="hlt">solar</span> power plant facilities are being built to take advantage of this renewable energy resource. <span class="hlt">Solar</span> energy is considered a clean source of energy, but there are potential environmental effects of <span class="hlt">solar</span> technology, such as landscape fragmentation, extinction of local biota, microclimate changes, among others. To be able to minimize environmental impacts of <span class="hlt">solar</span> power plants, it is important to know what kind of environmental conditions <span class="hlt">solar</span> power plants create. This study provides information about abiotic and biotic conditions in the vicinity of photovoltaic <span class="hlt">solar</span> power plants. Herein, the <span class="hlt">influence</span> of these power plants as drivers of new microclimate conditions and arthropods diversity composition in the Atacama Desert was evaluated. Microclimatic conditions between panel mounts was found to be more extreme than in the surrounding desert yet beneath the panels temperature is lower and relative humidity higher than outside the panel area. Arthropod species composition was altered in fixed-mount panel installations. In contrast, <span class="hlt">solar</span> tracking technology showed less <span class="hlt">influence</span> on microclimate and species composition between Sun and Shade in the power plant. Shady conditions provided a refuge for arthropod species in both installation types. For example, Dipterans were more abundant in the shade whereas Solifugaes were seldom present in the shade. The presented findings have relevance for the sustainable planning and construction of <span class="hlt">solar</span> power plants.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/28643082','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/28643082"><span>The <span class="hlt">Influence</span> of <span class="hlt">Solar</span> Power Plants on Microclimatic Conditions and the Biotic Community in Chilean Desert Environments.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Suuronen, Anna; Muñoz-Escobar, Christian; Lensu, Anssi; Kuitunen, Markku; Guajardo Celis, Natalia; Espinoza Astudillo, Pablo; Ferrú, Marcos; Taucare-Ríos, Andrés; Miranda, Marcelo; Kukkonen, Jussi V K</p> <p>2017-10-01</p> <p>The renewable energy sector is growing at a rapid pace in northern Chile and the <span class="hlt">solar</span> energy potential is one of the best worldwide. Therefore, many types of <span class="hlt">solar</span> power plant facilities are being built to take advantage of this renewable energy resource. <span class="hlt">Solar</span> energy is considered a clean source of energy, but there are potential environmental effects of <span class="hlt">solar</span> technology, such as landscape fragmentation, extinction of local biota, microclimate changes, among others. To be able to minimize environmental impacts of <span class="hlt">solar</span> power plants, it is important to know what kind of environmental conditions <span class="hlt">solar</span> power plants create. This study provides information about abiotic and biotic conditions in the vicinity of photovoltaic <span class="hlt">solar</span> power plants. Herein, the <span class="hlt">influence</span> of these power plants as drivers of new microclimate conditions and arthropods diversity composition in the Atacama Desert was evaluated. Microclimatic conditions between panel mounts was found to be more extreme than in the surrounding desert yet beneath the panels temperature is lower and relative humidity higher than outside the panel area. Arthropod species composition was altered in fixed-mount panel installations. In contrast, <span class="hlt">solar</span> tracking technology showed less <span class="hlt">influence</span> on microclimate and species composition between Sun and Shade in the power plant. Shady conditions provided a refuge for arthropod species in both installation types. For example, Dipterans were more abundant in the shade whereas Solifugaes were seldom present in the shade. The presented findings have relevance for the sustainable planning and construction of <span class="hlt">solar</span> power plants.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.osti.gov/servlets/purl/5686767','SCIGOV-STC'); return false;" href="https://www.osti.gov/servlets/purl/5686767"><span><span class="hlt">Solar</span> Energy Education. Humanities: <span class="hlt">activities</span> and teacher's guide. Field test edition</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>Not Available</p> <p>1982-01-01</p> <p><span class="hlt">Activities</span> are outlined to introduce students to information on <span class="hlt">solar</span> energy while performing ordinary classroom work. In this teaching manual <span class="hlt">solar</span> energy is integrated with the humanities. The <span class="hlt">activities</span> include such things as stories, newspapers, writing assignments, and art and musical presentations all filled with energy related terms. An energy glossary is provided. (BCS)</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.osti.gov/biblio/22654142-coronal-dynamic-activities-declining-phase-solar-cycle','SCIGOV-STC'); return false;" href="https://www.osti.gov/biblio/22654142-coronal-dynamic-activities-declining-phase-solar-cycle"><span>CORONAL DYNAMIC <span class="hlt">ACTIVITIES</span> IN THE DECLINING PHASE OF A <span class="hlt">SOLAR</span> CYCLE</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>Jang, Minhwan; Choe, G. S.; Woods, T. N.</p> <p>2016-12-10</p> <p>It has been known that some <span class="hlt">solar</span> <span class="hlt">activity</span> indicators show a double-peak feature in their evolution through a <span class="hlt">solar</span> cycle, which is not conspicuous in sunspot number. In this Letter, we investigate the high <span class="hlt">solar</span> dynamic <span class="hlt">activity</span> in the declining phase of the sunspot cycle by examining the evolution of polar and low-latitude coronal hole (CH) areas, splitting and merging events of CHs, and coronal mass ejections (CMEs) detected by SOHO /LASCO C3 in <span class="hlt">solar</span> cycle 23. Although the total CH area is at its maximum near the sunspot minimum, in which polar CHs prevail, it shows a comparable secondmore » maximum in the declining phase of the cycle, in which low-latitude CHs are dominant. The events of CH splitting or merging, which are attributed to surface motions of magnetic fluxes, are also mostly populated in the declining phase of the cycle. The far-reaching C3 CMEs are also overpopulated in the declining phase of the cycle. From these results we suggest that <span class="hlt">solar</span> dynamic <span class="hlt">activities</span> due to the horizontal surface motions of magnetic fluxes extend far in the declining phase of the sunspot cycle.« less</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/20180001284','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/20180001284"><span><span class="hlt">Solar</span> <span class="hlt">Activity</span> Across the Scales: From Small-Scale Quiet-Sun Dynamics to Magnetic <span class="hlt">Activity</span> Cycles</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Kitiashvili, Irina N.; Collins, Nancy N.; Kosovichev, Alexander G.; Mansour, Nagi N.; Wray, Alan A.</p> <p>2017-01-01</p> <p>Observations as well as numerical and theoretical models show that <span class="hlt">solar</span> dynamics is characterized by complicated interactions and energy exchanges among different temporal and spatial scales. It reveals magnetic self-organization processes from the smallest scale magnetized vortex tubes to the global <span class="hlt">activity</span> variation known as the <span class="hlt">solar</span> cycle. To understand these multiscale processes and their relationships, we use a two-fold approach: 1) realistic 3D radiative MHD simulations of local dynamics together with high resolution observations by IRIS, Hinode, and SDO; and 2) modeling of <span class="hlt">solar</span> <span class="hlt">activity</span> cycles by using simplified MHD dynamo models and mathematical data assimilation techniques. We present recent results of this approach, including the interpretation of observational results from NASA heliophysics missions and predictive capabilities. In particular, we discuss the links between small-scale dynamo processes in the convection zone and atmospheric dynamics, as well as an early prediction of <span class="hlt">Solar</span> Cycle 25.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017AGUFMSH13A2466K','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017AGUFMSH13A2466K"><span><span class="hlt">Solar</span> <span class="hlt">activity</span> across the scales: from small-scale quiet-Sun dynamics to magnetic <span class="hlt">activity</span> cycles</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Kitiashvili, I.; Collins, N.; Kosovichev, A. G.; Mansour, N. N.; Wray, A. A.</p> <p>2017-12-01</p> <p>Observations as well as numerical and theoretical models show that <span class="hlt">solar</span> dynamics is characterized by complicated interactions and energy exchanges among different temporal and spatial scales. It reveals magnetic self-organization processes from the smallest scale magnetized vortex tubes to the global <span class="hlt">activity</span> variation known as the <span class="hlt">solar</span> cycle. To understand these multiscale processes and their relationships, we use a two-fold approach: 1) realistic 3D radiative MHD simulations of local dynamics together with high-resolution observations by IRIS, Hinode, and SDO; and 2) modeling of <span class="hlt">solar</span> <span class="hlt">activity</span> cycles by using simplified MHD dynamo models and mathematical data assimilation techniques. We present recent results of this approach, including the interpretation of observational results from NASA heliophysics missions and predictive capabilities. In particular, we discuss the links between small-scale dynamo processes in the convection zone and atmospheric dynamics, as well as an early prediction of <span class="hlt">Solar</span> Cycle 25.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2005JGRA..110.4211J','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2005JGRA..110.4211J"><span>A <span class="hlt">solar</span> cycle dependence of nonlinearity in magnetospheric <span class="hlt">activity</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Johnson, Jay R.; Wing, Simon</p> <p>2005-04-01</p> <p>The nonlinear dependencies inherent to the historical Kp data stream (1932-2003) are examined using mutual information and cumulant-based cost as discriminating statistics. The discriminating statistics are compared with surrogate data streams that are constructed using the corrected amplitude adjustment Fourier transform (CAAFT) method and capture the linear properties of the original Kp data. Differences are regularly seen in the discriminating statistics a few years prior to <span class="hlt">solar</span> minima, while no differences are apparent at the time of <span class="hlt">solar</span> maxima. These results suggest that the dynamics of the magnetosphere tend to be more linear at <span class="hlt">solar</span> maximum than at <span class="hlt">solar</span> minimum. The strong nonlinear dependencies tend to peak on a timescale around 40-50 hours and are statistically significant up to 1 week. Because the <span class="hlt">solar</span> wind driver variables, VBs, and dynamical pressure exhibit a much shorter decorrelation time for nonlinearities, the results seem to indicate that the nonlinearity is related to internal magnetospheric dynamics. Moreover, the timescales for the nonlinearity seem to be on the same order as that for storm/ring current relaxation. We suggest that the strong <span class="hlt">solar</span> wind driving that occurs around <span class="hlt">solar</span> maximum dominates the magnetospheric dynamics, suppressing the internal magnetospheric nonlinearity. On the other hand, in the descending phase of the <span class="hlt">solar</span> cycle just prior to <span class="hlt">solar</span> minimum, when magnetospheric <span class="hlt">activity</span> is weaker, the dynamics exhibit a significant nonlinear internal magnetospheric response that may be related to increased <span class="hlt">solar</span> wind speed.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017JASS...34..257K','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017JASS...34..257K"><span><span class="hlt">Solar</span> <span class="hlt">Influence</span> on Tropical Cyclone in Western North Pacific Ocean</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Kim, Jung-Hee; Kim, Ki-Beom; Chang, Heon-Young</p> <p>2017-12-01</p> <p><span class="hlt">Solar</span> <span class="hlt">activity</span> is known to be linked to changes in the Earth’s weather and climate. Nonetheless, for other types of extreme weather, such as tropical cyclones (TCs), the available evidence is less conclusive. In this study the modulation of TC genesis over the western North Pacific by the <span class="hlt">solar</span> <span class="hlt">activity</span> is investigated, in comparison with a large-scale environmental parameter, i.e., El-Niño-Southern Oscillation (ENSO). For this purpose, we have obtained the best track data for TCs in the western North Pacific from 1977 to 2016, spanning from the <span class="hlt">solar</span> cycle 21 to the <span class="hlt">solar</span> cycle 24. We have confirmed that in the El-Niño periods TCs tend to form in the southeast, reach its maximum strength in the southeast, and end its life as TSs in the northeast, compared with the La-Niña periods. TCs occurring in the El-Niño periods are found to last longer compared with the La-Niña periods. Furthermore, TCs occurring in the El-Niño periods have a lower central pressure at their maximum strength than those occurring in the La-Niña periods. We have found that TCs occurring in the <span class="hlt">solar</span> maximum periods resemble those in the El-Niño periods in their properties. We have also found that TCs occurring in the <span class="hlt">solar</span> descending periods somehow resemble those in the El-Niño periods in their properties. To make sure that it is not due to the ENSO effect, we have excluded TCs both in the El-Niño periods and in the La-Niña periods from the data set and repeated the analysis. In addition to this test, we have also reiterated our analysis twice with TCs whose maximum sustained winds speed exceeds 17 m/s, instead of 33 m/s, as well as TCs designated as a typhoon, which ends up with the same conclusions.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2008ApPhL..92c3306A','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2008ApPhL..92c3306A"><span>Polymer based organic <span class="hlt">solar</span> cells using ink-jet printed <span class="hlt">active</span> layers</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Aernouts, T.; Aleksandrov, T.; Girotto, C.; Genoe, J.; Poortmans, J.</p> <p>2008-01-01</p> <p>Ink-jet printing is used to deposit polymer:fullerene blends suitable as <span class="hlt">active</span> layer for organic <span class="hlt">solar</span> cells. We show that merging of separately deposited ink droplets into a continuous, pinhole-free organic thin film results from a balance between ink viscosity and surface wetting, whereas for certain of the studied solutions clear coffee drop effect occurs for single droplets; this can be minimized for larger printed areas, yielding smooth layers with minimal surface roughness. Resulting organic films are used as <span class="hlt">active</span> layer for <span class="hlt">solar</span> cells with power conversion efficiency of 1.4% under simulated AM1.5 <span class="hlt">solar</span> illumination.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2016ASPC..504..299S','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2016ASPC..504..299S"><span>The <span class="hlt">SOLAR</span>-C Mission: Science Objectives and Current Status</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Suematsu, Y.; Solar-C Working Group</p> <p>2016-04-01</p> <p>The <span class="hlt">SOLAR</span>-C is a Japan-led international <span class="hlt">solar</span> mission for mid-2020s designed to investigate the magnetic <span class="hlt">activities</span> of the Sun, focusing on the study in heating and dynamical phenomena of the chromosphere and corona, and to advance algorithms for predicting short and long term <span class="hlt">solar</span> magnetic <span class="hlt">activities</span>. For these purposes, <span class="hlt">SOLAR</span>-C will carry three dedicated instruments; the <span class="hlt">Solar</span> UV-Vis-IR Telescope (SUVIT), the EUV Spectroscopic Telescope (EUVST) and the High Resolution Coronal Imager (HCI), to jointly observe the entire visible <span class="hlt">solar</span> atmosphere with essentially the same high spatial resolution (0.1"-0.3"), performing high resolution spectroscopic measurements over all atmospheric regions and spectro-polarimetric measurements from the photosphere through the upper chromosphere. <span class="hlt">SOLAR</span>-C will also contribute to understand the <span class="hlt">solar</span> <span class="hlt">influence</span> on the Sun-Earth environments with synergetic wide-field observations from ground-based and other space missions.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2016AIPC.1734g0003B','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2016AIPC.1734g0003B"><span><span class="hlt">Influence</span> of spatiotemporally distributed irradiance data input on temperature evolution in parabolic trough <span class="hlt">solar</span> field simulations</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Bubolz, K.; Schenk, H.; Hirsch, T.</p> <p>2016-05-01</p> <p>Concentrating <span class="hlt">solar</span> field operation is affected by shadowing through cloud movement. For line focusing systems the impact of varying irradiance has been studied before by several authors with simulations of relevant thermodynamics assuming spatially homogeneous irradiance or using artificial test signals. While today's simulation capabilities allow more and more a higher spatiotemporal resolution of plant processes there are only few studies on <span class="hlt">influence</span> of spatially distributed irradiance due to lack of available data. Based on recent work on generating real irradiance maps with high spatial resolution this paper demonstrates their <span class="hlt">influence</span> on <span class="hlt">solar</span> field thermodynamics. For a case study an irradiance time series is chosen. One <span class="hlt">solar</span> field section with several loops and collecting header is modeled for simulation purpose of parabolic trough collectors and oil as heat transfer medium. Assuming homogeneous mass flow distribution among all loops we observe spatially varying temperature characteristics. They are analysed without and with mass flow control and their impact on <span class="hlt">solar</span> field control design is discussed. Finally, the potential of distributed irradiance data is outlined.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/20020087931','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/20020087931"><span>Sources of Geomagnetic <span class="hlt">Activity</span> during Nearly Three <span class="hlt">Solar</span> Cycles (1972-2000)</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Richardson, I. G.; Cane, H. V.; Cliver, E. W.; White, Nicholas E. (Technical Monitor)</p> <p>2002-01-01</p> <p>We examine the contributions of the principal <span class="hlt">solar</span> wind components (corotating highspeed streams, slow <span class="hlt">solar</span> wind, and transient structures, i.e., interplanetary coronal mass ejections (CMEs), shocks, and postshock flows) to averages of the aa geomagnetic index and the interplanetary magnetic field (IMF) strength in 1972-2000 during nearly three <span class="hlt">solar</span> cycles. A prime motivation is to understand the <span class="hlt">influence</span> of <span class="hlt">solar</span> cycle variations in <span class="hlt">solar</span> wind structure on long-term (e.g., approximately annual) averages of these parameters. We show that high-speed streams account for approximately two-thirds of long-term aa averages at <span class="hlt">solar</span> minimum, while at <span class="hlt">solar</span> maximum, structures associated with transients make the largest contribution (approx. 50%), though contributions from streams and slow <span class="hlt">solar</span> wind continue to be present. Similarly, high-speed streams are the principal contributor (approx. 55%) to <span class="hlt">solar</span> minimum averages of the IMF, while transient-related structures are the leading contributor (approx. 40%) at <span class="hlt">solar</span> maximum. These differences between <span class="hlt">solar</span> maximum and minimum reflect the changing structure of the near-ecliptic <span class="hlt">solar</span> wind during the <span class="hlt">solar</span> cycle. For minimum periods, the Earth is embedded in high-speed streams approx. 55% of the time versus approx. 35% for slow <span class="hlt">solar</span> wind and approx. 10% for CME-associated structures, while at <span class="hlt">solar</span> maximum, typical percentages are as follows: high-speed streams approx. 35%, slow <span class="hlt">solar</span> wind approx. 30%, and CME-associated approx. 35%. These compositions show little cycle-to-cycle variation, at least for the interval considered in this paper. Despite the change in the occurrences of different types of <span class="hlt">solar</span> wind over the <span class="hlt">solar</span> cycle (and less significant changes from cycle to cycle), overall, variations in the averages of the aa index and IMF closely follow those in corotating streams. Considering <span class="hlt">solar</span> cycle averages, we show that high-speed streams account for approx. 44%, approx. 48%, and approx. 40% of the <span class="hlt">solar</span></p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://www.dtic.mil/docs/citations/ADA103522','DTIC-ST'); return false;" href="http://www.dtic.mil/docs/citations/ADA103522"><span>Fabrication of Integral <span class="hlt">Solar</span> Cell Covers by the Plasma <span class="hlt">Activated</span> Source.</span></a></p> <p><a target="_blank" href="http://www.dtic.mil/">DTIC Science & Technology</a></p> <p></p> <p>1981-01-01</p> <p>1 Average Intrinsic Deposition Stress of Pyrolitic Silicon Oxynitride Films vs. Composition ................................... 7 2 Coefficient of...source for <span class="hlt">activated</span> oxygen molecules which were reacted with, for example, silane at a <span class="hlt">solar</span> cell surface to deposit amorphous silicon dioxide on the... Silicon <span class="hlt">Solar</span> Cells ........ 51 44.6 SiO 2 Coatings in GaAs <span class="hlt">Solar</span> Cells ........... 58 5.0 CONCLUSIONS..................................... 61 5.1</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://files.eric.ed.gov/fulltext/ED395826.pdf','ERIC'); return false;" href="http://files.eric.ed.gov/fulltext/ED395826.pdf"><span><span class="hlt">Solar</span> System Puzzle Kit: An <span class="hlt">Activity</span> for Earth and Space Science.</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>Vogt, Gregory L.; Rosenberg, Carla B.</p> <p></p> <p>This <span class="hlt">Solar</span> System Puzzle Kit for grades 5-8, allows students to create an eight-cube paper puzzle of the <span class="hlt">solar</span> system and may be duplicated for classroom use or used as a take home <span class="hlt">activity</span> for children and parents. By assembling the puzzle, hand-coloring the bodies of the <span class="hlt">solar</span> system, and viewing the puzzle's 12 sides, students can reinforce…</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017EPSC...11..102P','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017EPSC...11..102P"><span>Transits in our <span class="hlt">Solar</span> System for educational <span class="hlt">activities</span>: Mercury Transit 2016 and Total <span class="hlt">Solar</span> Eclipse 2017</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Pérez-Ayúcar, M.; Breitfelner, M.</p> <p>2017-09-01</p> <p><span class="hlt">Solar</span> transits are rare astronomical event of profound historical importance and with an enormous potential to engage nowadays students and general public into Planetary Sciences and Space. Mercury transits occur only about every 13-14 times per century. Total <span class="hlt">solar</span> eclipses occur around 18 months apart somewhere on Earth, but they recur only every 3-4 centuries on the same location. Although its historic scientific importance (examples, to measure the distances in the <span class="hlt">solar</span> system, to observe the <span class="hlt">solar</span> corona) has diminished since humanity roams our <span class="hlt">solar</span> system with robotic spacecrafts, transits remain a spectacular astronomical event that is used very effectively to engage general public and students to Science and Space in general. The educational project CESAR (Cooperation through Education in Science and Astronomy Research) has been covering since 2012 such events (Venus transit 2012, live Sun transmissions, <span class="hlt">solar</span> eclipses, ISS transits ...). We report the outstanding outcome of the two public educational and outreach events since last year: the May 2016 Mercury Transit, and the recent August 2017 Total Eclipse. And the follow up <span class="hlt">activities</span> expected for future transits.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2005IJBm...50....1S','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2005IJBm...50....1S"><span>Chromosome aberration and environmental physical <span class="hlt">activity</span>: Down syndrome and <span class="hlt">solar</span> and cosmic ray <span class="hlt">activity</span>, Israel, 1990-2000</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Stoupel, Eliahu G.; Frimer, Helena; Appelman, Zvi; Ben-Neriah, Ziva; Dar, Hanna; Fejgin, Moshe D.; Gershoni-Baruch, Ruth; Manor, Esther; Barkai, Gad; Shalev, Stavit; Gelman-Kohan, Zully; Reish, Orit; Lev, Dorit; Davidov, Bella; Goldman, Boleslaw; Shohat, Mordechai</p> <p>2005-09-01</p> <p>The possibility that environmental effects are associated with chromosome aberrations and various congenital pathologies has been discussed previously. Recent advances in the collection and computerization of data make studying these potential associations more feasible. The aim of this study was to investigate a possible link between the number of Down syndrome (DS) cases detected prenatally or at birth yearly in Israel over a 10-year period compared with the levels of <span class="hlt">solar</span> and cosmic ray <span class="hlt">activity</span> 1 year before the detection or birth of each affected child. Information about 1,108,449 births was collected for the years 1990-2000, excluding 1991, when data were unavailable. A total of 1,310 cases of DS were detected prenatally or at birth—138 in the non-Jewish community and 1,172 in the Jewish population. <span class="hlt">Solar</span> <span class="hlt">activity</span> indices—sunspot number and <span class="hlt">solar</span> radio flux 2,800 MHz at 10.7 cm wavelength for 1989-1999—were compared with the number of DS cases detected. Pearson correlation coefficients (r) and their probabilities (P) were established for the percentage of DS cases in the whole population. There was a significant inverse correlation between the indices of <span class="hlt">solar</span> <span class="hlt">activity</span> and the number of cases of DS detected—r=-0.78, P=0.008 for sunspot number and r=-0.76, P=0.01 for <span class="hlt">solar</span> flux. The possibility that cosmophysical factors inversely related to <span class="hlt">solar</span> <span class="hlt">activity</span> play a role in the pathogenesis of chromosome aberrations should be considered. We have confirmed a strong trend towards an association between the cosmic ray <span class="hlt">activity</span> level and the incidence of DS.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/20120016041','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/20120016041"><span>Near-Earth <span class="hlt">Solar</span> Wind Flows and Related Geomagnetic <span class="hlt">Activity</span> During more than Four <span class="hlt">Solar</span> Cycles (1963-2011)</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Richardson, Ian G.; Cane, Hilary V.</p> <p>2012-01-01</p> <p>In past studies, we classified the near-Earth <span class="hlt">solar</span> wind into three basic flow types based on inspection of <span class="hlt">solar</span> wind plasma and magnetic field parameters in the OMNI database and additional data (e.g., geomagnetic indices, energetic particle, and cosmic ray observations). These flow types are: (1) High-speed streams associated with coronal holes at the Sun, (2) Slow, interstream <span class="hlt">solar</span> wind, and (3) Transient flows originating with coronal mass ejections at the Sun, including interplanetary coronal mass ejections and the associated upstream shocks and post-shock regions. The <span class="hlt">solar</span> wind classification in these previous studies commenced with observations in 1972. In the present study, as well as updating this classification to the end of 2011, we have extended the classification back to 1963, the beginning of near-Earth <span class="hlt">solar</span> wind observations, thereby encompassing the complete <span class="hlt">solar</span> cycles 20 to 23 and the ascending phase of cycle 24. We discuss the cycle-to-cycle variations in near-Earth <span class="hlt">solar</span> wind structures and l1e related geomagnetic <span class="hlt">activity</span> over more than four <span class="hlt">solar</span> cycles, updating some of the results of our earlier studies.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2013OAP....26..294P','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2013OAP....26..294P"><span>Endothelial Dysfunction and Blood Viscosity Inpatients with Unstable Angina in Different Periods of a <span class="hlt">Solar</span> <span class="hlt">Activity</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Parshina, S. S.; Tokaeva, L. K.; Dolgova, E. M.; Afanas'yeva, T. N.; Strelnikova, O. A.</p> <p></p> <p>The origin of hemorheologic and endothelial defects in patients with unstable angina (comparing with healthy persons) is determined by a <span class="hlt">solar</span> <span class="hlt">activity</span> period: the blood viscosity increases in a period of high <span class="hlt">solar</span> <span class="hlt">activity</span> in the vessels of small, medium and macro diameters, a local decompensate dysfunction of small vessels endothelium had been fixed (microcirculation area). In the period of a low <span class="hlt">solar</span> <span class="hlt">activity</span> there is an increase of a blood viscosity in vessels of all diameters, generalized subcompensated endothelial dysfunction is developed (on the background of the III phase blood clotting <span class="hlt">activating</span>). In the period of a high <span class="hlt">solar</span> <span class="hlt">activity</span> a higher blood viscosity had been fixed, comparing with the period of a low <span class="hlt">solar</span> <span class="hlt">activity</span>.</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('http://hdl.handle.net/2060/20170011530','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/20170011530"><span>Using Data Assimilation Methods of Prediction of <span class="hlt">Solar</span> <span class="hlt">Activity</span></span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Kitiashvili, Irina N.; Collins, Nancy S.</p> <p>2017-01-01</p> <p>The variable <span class="hlt">solar</span> magnetic <span class="hlt">activity</span> known as the 11-year <span class="hlt">solar</span> cycle has the longest history of <span class="hlt">solar</span> observations. These cycles dramatically affect conditions in the heliosphere and the Earth's space environment. Our current understanding of the physical processes that make up global <span class="hlt">solar</span> dynamics and the dynamo that generates the magnetic fields is sketchy, resulting in unrealistic descriptions in theoretical and numerical models of the <span class="hlt">solar</span> cycles. The absence of long-term observations of <span class="hlt">solar</span> interior dynamics and photospheric magnetic fields hinders development of accurate dynamo models and their calibration. In such situations, mathematical data assimilation methods provide an optimal approach for combining the available observational data and their uncertainties with theoretical models in order to estimate the state of the <span class="hlt">solar</span> dynamo and predict future cycles. In this presentation, we will discuss the implementation and performance of an Ensemble Kalman Filter data assimilation method based on the Parker migratory dynamo model, complemented by the equation of magnetic helicity conservation and long-term sunspot data series. This approach has allowed us to reproduce the general properties of <span class="hlt">solar</span> cycles and has already demonstrated a good predictive capability for the current cycle, 24. We will discuss further development of this approach, which includes a more sophisticated dynamo model, synoptic magnetogram data, and employs the DART Data Assimilation Research Testbed.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2014AdSpR..54.2430T','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2014AdSpR..54.2430T"><span>Effect of <span class="hlt">solar</span> <span class="hlt">activity</span> on the repetitiveness of some meteorological phenomena</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Todorović, Nedeljko; Vujović, Dragana</p> <p>2014-12-01</p> <p>In this paper we research the relationship between <span class="hlt">solar</span> <span class="hlt">activity</span> and the weather on Earth. This research is based on the assumption that every ejection of magnetic field energy and particles from the Sun (also known as <span class="hlt">Solar</span> wind) has direct effects on the Earth's weather. The impact of coronal holes and <span class="hlt">active</span> regions on cold air advection (cold fronts, precipitation, and temperature decrease on the surface and higher layers) in the Belgrade region (Serbia) was analyzed. Some <span class="hlt">active</span> regions and coronal holes appear to be in a geo-effective position nearly every 27 days, which is the duration of a <span class="hlt">solar</span> rotation. A similar period of repetitiveness (27-29 days) of the passage of the cold front, and maximum and minimum temperatures measured at surface and at levels of 850 and 500 hPa were detected. We found that 10-12 days after <span class="hlt">Solar</span> wind velocity starts significantly increasing, we could expect the passage of a cold front. After eight days, the maximum temperatures in the Belgrade region are measured, and it was found that their minimum values appear after 12-16 days. The maximum amount of precipitation occurs 14 days after <span class="hlt">Solar</span> wind is observed. A recurring period of nearly 27 days of different phases of development for hurricanes Katrina, Rita and Wilma was found. This analysis confirmed that the intervals of time between two occurrences of some particular meteorological parameter correlate well with <span class="hlt">Solar</span> wind and A index.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2016cosp...41E1414N','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2016cosp...41E1414N"><span>Non-Stationary Effects and Cross Correlations in <span class="hlt">Solar</span> <span class="hlt">Activity</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Nefedyev, Yuri; Panischev, Oleg; Demin, Sergey</p> <p>2016-07-01</p> <p>In this paper within the framework of the Flicker-Noise Spectroscopy (FNS) we consider the dynamic properties of the <span class="hlt">solar</span> <span class="hlt">activity</span> by analyzing the Zurich sunspot numbers. As is well-known astrophysics objects are the non-stationary open systems, whose evolution are the quite individual and have the alternation effects. The main difference of FNS compared to other related methods is the separation of the original signal reflecting the dynamics of <span class="hlt">solar</span> <span class="hlt">activity</span> into three frequency bands: system-specific "resonances" and their interferential contributions at lower frequencies, chaotic "random walk" ("irregularity-jump") components at larger frequencies, and chaotic "irregularity-spike" (inertial) components in the highest frequency range. Specific parameters corresponding to each of the bands are introduced and calculated. These irregularities as well as specific resonance frequencies are considered as the information carriers on every hierarchical level of the evolution of a complex natural system with intermittent behavior, consecutive alternation of rapid chaotic changes in the values of dynamic variables on small time intervals with small variations of the values on longer time intervals ("laminar" phases). The jump and spike irregularities are described by power spectra and difference moments (transient structural functions) of the second order. FNS allows revealing the most crucial points of the <span class="hlt">solar</span> <span class="hlt">activity</span> dynamics by means of "spikiness" factor. It is shown that this variable behaves as the predictor of crucial changes of the sunspot number dynamics, particularly when the number comes up to maximum value. The change of averaging interval allows revealing the non-stationary effects depending by 11-year cycle and by inside processes in a cycle. To consider the cross correlations between the different variables of <span class="hlt">solar</span> <span class="hlt">activity</span> we use the Zurich sunspot numbers and the sequence of corona's radiation energy. The FNS-approach allows extracting the</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2018AAS...23115807M','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2018AAS...23115807M"><span>Multi-wavelength Observations of <span class="hlt">Solar</span> Acoustic Waves Near <span class="hlt">Active</span> Regions</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Monsue, Teresa; Pesnell, Dean; Hill, Frank</p> <p>2018-01-01</p> <p><span class="hlt">Active</span> region areas on the Sun are abundant with a variety of waves that are both acoustically helioseismic and magnetohydrodynamic in nature. The occurrence of a <span class="hlt">solar</span> flare can disrupt these waves, through MHD mode-mixing or scattering by the excitation of these waves. We take a multi-wavelength observational approach to understand the source of theses waves by studying <span class="hlt">active</span> regions where flaring <span class="hlt">activity</span> occurs. Our approach is to search for signals within a time series of images using a Fast Fourier Transform (FFT) algorithm, by producing multi-frequency power map movies. We study <span class="hlt">active</span> regions both spatially and temporally and correlate this method over multiple wavelengths using data from NASA’s <span class="hlt">Solar</span> Dynamics Observatory. By surveying the <span class="hlt">active</span> regions on multiple wavelengths we are able to observe the behavior of these waves within the <span class="hlt">Solar</span> atmosphere, from the photosphere up through the corona. We are able to detect enhancements of power around <span class="hlt">active</span> regions, which could be acoustic power halos and of an MHD-wave propagating outward by the flaring event. We are in the initial stages of this study understanding the behaviors of these waves and could one day contribute to understanding the mechanism responsible for their formation; that has not yet been explained.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017SoPh..292..179R','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017SoPh..292..179R"><span>A Relationship Between the <span class="hlt">Solar</span> Rotation and <span class="hlt">Activity</span> Analysed by Tracing Sunspot Groups</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Ruždjak, Domagoj; Brajša, Roman; Sudar, Davor; Skokić, Ivica; Poljančić Beljan, Ivana</p> <p>2017-12-01</p> <p>The sunspot position published in the data bases of the Greenwich Photoheliographic Results (GPR), the US Air Force <span class="hlt">Solar</span> Optical Observing Network and National Oceanic and Atmospheric Administration (USAF/NOAA), and of the Debrecen Photoheliographic Data (DPD) in the period 1874 to 2016 were used to calculate yearly values of the <span class="hlt">solar</span> differential-rotation parameters A and B. These differential-rotation parameters were compared with the <span class="hlt">solar-activity</span> level. We found that the Sun rotates more differentially at the minimum than at the maximum of <span class="hlt">activity</span> during the epoch 1977 - 2016. An inverse correlation between equatorial rotation and <span class="hlt">solar</span> <span class="hlt">activity</span> was found using the recently revised sunspot number. The secular decrease of the equatorial rotation rate that accompanies the increase in <span class="hlt">activity</span> stopped in the last part of the twentieth century. It was noted that when a significant peak in equatorial rotation velocity is observed during <span class="hlt">activity</span> minimum, the next maximum is weaker than the previous one.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://eric.ed.gov/?q=solar+AND+system+AND+movement&id=EJ561858','ERIC'); return false;" href="https://eric.ed.gov/?q=solar+AND+system+AND+movement&id=EJ561858"><span>Moving through the <span class="hlt">Solar</span> System: Using Movement <span class="hlt">Activities</span> To Learn about the <span class="hlt">Solar</span> System.</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>Nygard, Bonnie; Shaw, Donna Gail</p> <p>1997-01-01</p> <p>Presents a rationale for acknowledging the importance of movement to learning to help children understand abstract concepts. Includes seven <span class="hlt">activities</span> that employ movement to enable students to understand the nature of the <span class="hlt">solar</span> system. (DDR)</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://ntrs.nasa.gov/search.jsp?R=19900018869&hterms=Physical+Review&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D50%26Ntt%3DPhysical%2BReview','NASA-TRS'); return false;" href="https://ntrs.nasa.gov/search.jsp?R=19900018869&hterms=Physical+Review&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D50%26Ntt%3DPhysical%2BReview"><span>Physical mechanisms of <span class="hlt">solar</span> <span class="hlt">activity</span> effects in the middle atmosphere</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Ebel, A.</p> <p>1989-01-01</p> <p>A great variety of physical mechanisms of possibly <span class="hlt">solar</span> induced variations in the middle atmosphere has been discussed in the literature during the last decades. The views which have been put forward are often controversial in their physical consequences. The reason may be the complexity and non-linearity of the atmospheric response to comparatively weak forcing resulting from <span class="hlt">solar</span> <span class="hlt">activity</span>. Therefore this review focuses on aspects which seem to indicate nonlinear processes in the development of <span class="hlt">solar</span> induced variations. Results from observations and numerical simulations are discussed.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://images.nasa.gov/#/details-GSFC_20171208_Archive_e002116.html','SCIGOVIMAGE-NASA'); return false;" href="https://images.nasa.gov/#/details-GSFC_20171208_Archive_e002116.html"><span><span class="hlt">Solar</span> <span class="hlt">activity</span> and erupting prominences [HD Video</span></a></p> <p><a target="_blank" href="https://images.nasa.gov/">NASA Image and Video Library</a></p> <p></p> <p>2017-12-08</p> <p><span class="hlt">Solar</span> <span class="hlt">activity</span> and erupting prominences. EIT 304A (Jan. 8-10, 2000) Credit: NASA/GSFC/SOHO/ESA To learn more go to the SOHO website: sohowww.nascom.nasa.gov/home.html To learn more about NASA's Sun Earth Day go here: sunearthday.nasa.gov/2010/index.php</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/29469566','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/29469566"><span>Commercially Available <span class="hlt">Activated</span> Carbon Fiber Felt Enables Efficient <span class="hlt">Solar</span> Steam Generation.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Li, Haoran; He, Yurong; Hu, Yanwei; Wang, Xinzhi</p> <p>2018-03-21</p> <p>Sun-driven steam generation is now possible and has the potential to help meet future energy needs. Current technologies often use <span class="hlt">solar</span> condensers to increase <span class="hlt">solar</span> irradiance. More recently, a technology for <span class="hlt">solar</span> steam generation that uses heated surface water and low optical concentration is reported. In this work, a commercially available <span class="hlt">activated</span> carbon fiber felt is used to generate steam efficiently under one sun illumination. The evaporation rate and <span class="hlt">solar</span> conversion efficiency reach 1.22 kg m -2 h -1 and 79.4%, respectively. The local temperature of the evaporator with a floating <span class="hlt">activated</span> carbon fiber felt reaches 48 °C. Apart from the high absorptivity (about 94%) of the material, the evaporation performance is enhanced thanks to the well-developed pores for improved water supply and steam escape and the low thermal conductivity, which enables reduced bulk water temperature increase. This study helps to find a promising material for <span class="hlt">solar</span> steam generation using a water evaporator that can be produced economically (∼6 $/m 2 ) with long-term stability.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://ntrs.nasa.gov/search.jsp?R=19950046615&hterms=activity+Physics&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D50%26Ntt%3Dactivity%2BPhysics','NASA-TRS'); return false;" href="https://ntrs.nasa.gov/search.jsp?R=19950046615&hterms=activity+Physics&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D50%26Ntt%3Dactivity%2BPhysics"><span>Long-term persistence of <span class="hlt">solar</span> <span class="hlt">activity</span>. [Abstract only</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Ruzmaikin, Alexander; Feynman, Joan; Robinson, Paul</p> <p>1994-01-01</p> <p>The <span class="hlt">solar</span> irradiance has been found to change by 0.1% over the recent <span class="hlt">solar</span> cycle. A change of irradiance of about 0.5% is required to effect the Earth's climate. How frequently can a variation of this size be expected? We examine the question of the persistence of non-periodic variations in <span class="hlt">solar</span> <span class="hlt">activity</span>. The Huerst exponent, which characterizes the persistence of a time series (Mandelbrot and Wallis, 1969), is evaluated for the series of C-14 data for the time interval from about 6000 BC to 1950 AD (Stuiver and Pearson, 1986). We find a constant Huerst exponent, suggesting that <span class="hlt">solar</span> <span class="hlt">activity</span> in the frequency range of from 100 to 3000 years includes an important continuum component in addition to the well-known periodic variations. The value we calculate, H approximately equal to 0.8, is significantly larger than the value of 0.5 that would correspond to variations produced by a white-noise process. This value is in good agreement with the results for the monthly sunspot data reported elsewhere, indicating that the physics that produces the continuum is a correlated random process (Ruzmaikin et al., 1992), and that is is the same type of process over a wide range of time interval lengths. We conclude that the time period over which an irradiance change of 0.5% can be expected to occur is significantly shorter than that which would be expected for variations produced by a white-noise process.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.osti.gov/biblio/22654254-controlling-influence-magnetic-field-solar-wind-outflow-investigation-using-current-sheet-source-surface-model','SCIGOV-STC'); return false;" href="https://www.osti.gov/biblio/22654254-controlling-influence-magnetic-field-solar-wind-outflow-investigation-using-current-sheet-source-surface-model"><span>CONTROLLING <span class="hlt">INFLUENCE</span> OF MAGNETIC FIELD ON <span class="hlt">SOLAR</span> WIND OUTFLOW: AN INVESTIGATION USING CURRENT SHEET SOURCE SURFACE MODEL</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>Poduval, B., E-mail: bpoduval@spacescience.org</p> <p>2016-08-10</p> <p>This Letter presents the results of an investigation into the controlling <span class="hlt">influence</span> of large-scale magnetic field of the Sun in determining the <span class="hlt">solar</span> wind outflow using two magnetostatic coronal models: current sheet source surface (CSSS) and potential field source surface. For this, we made use of the Wang and Sheeley inverse correlation between magnetic flux expansion rate (FTE) and observed <span class="hlt">solar</span> wind speed (SWS) at 1 au. During the period of study, extended over <span class="hlt">solar</span> cycle 23 and beginning of <span class="hlt">solar</span> cycle 24, we found that the coefficients of the fitted quadratic equation representing the FTE–SWS inverse relation exhibited significantmore » temporal variation, implying the changing pattern of the <span class="hlt">influence</span> of FTE on SWS over time. A particularly noteworthy feature is an anomaly in the behavior of the fitted coefficients during the extended minimum, 2008–2010 (CRs 2073–2092), which is considered due to the particularly complex nature of the <span class="hlt">solar</span> magnetic field during this period. However, this variation was significant only for the CSSS model, though not a systematic dependence on the phase of the <span class="hlt">solar</span> cycle. Further, we noticed that the CSSS model demonstrated better <span class="hlt">solar</span> wind prediction during the period of study, which we attribute to the treatment of volume and sheet currents throughout the corona and the more accurate tracing of footpoint locations resulting from the geometry of the model.« less</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017ChA%26A..41..517S','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017ChA%26A..41..517S"><span><span class="hlt">Influence</span> of Convective Effect of <span class="hlt">Solar</span> Winds on the CME Transit Time</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Sun, Lu-yuan</p> <p>2017-10-01</p> <p>Based on an empirical model for predicting the transit time of coronal mass ejections (CMEs) proposed by Gopalswamy, 52 CME events which are related to the geomagnetic storms of Dst < -50 nT, and 10 CME events which caused extremely strong geomagnetic storms (Dst < -200 nT) in 1996- 2007 are selected, and combined with the observational data of the interplanetary <span class="hlt">solar</span> winds that collected by the ACE satellite at 1AU, to analyze the <span class="hlt">influence</span> of convective effect of ambient <span class="hlt">solar</span> winds on the prediction of the CME transit time when it arrives at a place of 1 AU. After taking the convective effect of ambient <span class="hlt">solar</span> winds into account, the standard deviation of predictions is reduced from 16.5 to 11.4 hours for the 52 CME events, and the prediction error is less than 15 hours for 68% of these events; while the standard deviation of predictions is reduced from 10.6 to 6.5 hours for the 10 CME events that caused extremely strong geomagnetic storms, and the prediction error is less than 5 hours for 6 of the 10 events. These results show that taking the convective effect of ambient <span class="hlt">solar</span> winds into account can reduce the standard deviation of the predicted CME transit time, hence the convective effect of <span class="hlt">solar</span> winds plays an important role for predicting the transit times of CME events.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017ARep...61..461S','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017ARep...61..461S"><span>Spots and <span class="hlt">activity</span> of <span class="hlt">solar</span>-type stars from Kepler observations</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Savanov, I. S.; Dmitrienko, E. S.</p> <p>2017-05-01</p> <p>The spot coverages S for 2846 <span class="hlt">solar</span>-type stars with effective temperatures from 5700 K to 5800 K and gravities from 4.4 to 4.5 have been measured. An analysis based on the MAST catalog, which presents photometric measurements obtained with the Kepler Space Telescope during Q9 is presented. The existence of two groups of <span class="hlt">solar</span>-type stars, with S values between 0.001 and 0.007 and with S > 0.007, is inferred. The second group (<span class="hlt">active</span> stars) contains 279 stars (about 10% of the total number of stars analyzed). The mean S parameter for the entire sample is 0.004, comparable to the mean spot coverage of the Sun. In general, the dependence of S on the rotation period for <span class="hlt">solar</span>-type stars has characteristics similar to those found earlier for stars with exoplanets. For the vast majority of the stars in the sample, the <span class="hlt">activity</span> is constant, and independent of age. The <span class="hlt">activity</span> of the small number of <span class="hlt">active</span> stars with S > 0.007 decreases with age. The age variations of the chromospheric <span class="hlt">activity</span> index R'HK are compared to variations of the spot coverage S. The relations analyzed have common characteristic features. It is likely that both the spot <span class="hlt">activity</span> level and the chromospheric <span class="hlt">activity</span> level abruptly decrease for stars older than 4 billion yrs.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/19900018867','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/19900018867"><span>Variation of D-region nitric-oxide density with <span class="hlt">solar</span> <span class="hlt">activity</span> and season at the dip equator</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Chakrabarty, D. K.; Pakhomov, S. V.; Beig, G.</p> <p>1989-01-01</p> <p>To study the <span class="hlt">solar</span> control on electron density (N sub e) in the equatorial D region, a program was initiated with Soviet collaboration in 1979. A total of 31 rockets were launched during the high <span class="hlt">solar</span> <span class="hlt">activity</span> period, and 47 rockets during the low <span class="hlt">solar</span> <span class="hlt">activity</span> period, from Thumba to measure the N sub e profiles. Analysis of the data shows that the average values of N sub e for the high <span class="hlt">solar</span> <span class="hlt">activity</span> period are higher by a factor of about 2 to 3 compared to the low <span class="hlt">solar</span> <span class="hlt">activity</span> values. It was found that a single nitric oxide density, (NO), profile cannot reproduce all the observed N sub e profiles. An attempt was made to reproduce theoretically the observed N sub e profiles by introducing variation in (NO) for the different <span class="hlt">solar</span> <span class="hlt">activity</span> periods and seasons.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2018yCat..18450036D','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2018yCat..18450036D"><span>VizieR Online Data Catalog: Complex network for <span class="hlt">solar</span> <span class="hlt">active</span> regions (Daei+, 2017)</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Daei, F.; Safari, H.; Dadashi, N.</p> <p>2018-03-01</p> <p>The <span class="hlt">solar</span> monitor (www.solarmonitor.org) records the <span class="hlt">solar</span> data observed by several <span class="hlt">solar</span> space observatories and missions (e.g., GOES, GONG, ACE, STEREO, SDO, etc.). 4227 <span class="hlt">solar</span> <span class="hlt">active</span> regions (ARs) during 1999 January 1 to 2017 April 14 used for building the AR network are listed in table 1. See section 2 for further details. (1 data file).</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2003EAEJA.....2865D','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2003EAEJA.....2865D"><span>Length of the <span class="hlt">solar</span> cycle <span class="hlt">influence</span> on the relationship NAO-Northern Hemisphere Temperature</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>de La Torre, L.; Gimeno, L.; Tesouro, M.; Añel, J. A.; Nieto, R.; Ribera, P.; García, R.; Hernández, E.</p> <p>2003-04-01</p> <p>The <span class="hlt">influence</span> of the length of the <span class="hlt">solar</span> cycle on the relationship North Atlantic Oscillation (NAO)-Northern Hemisphere Temperature (NHT) is investigated. The results suggest that this relationship is different according to the length of the <span class="hlt">solar</span> cycle. When the sunspot cycle is 10 or 11 years long, wintertime NAO and NHT are positively correlated, being the signal more intense during 11 years period, but when the sunspot cycle is longer (12 years) correlations between wintertime NAO and NHT are not significant. In fact there are significant negative correlations between wintertime NAO and spring NHT, with predictive potential.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.osti.gov/servlets/purl/837854','SCIGOV-STC'); return false;" href="https://www.osti.gov/servlets/purl/837854"><span>A <span class="hlt">Solar</span> Cycle Dependence of Nonlinearity in Magnetospheric <span class="hlt">Activity</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>Johnson, Jay R; Wing, Simon</p> <p>2005-03-08</p> <p>The nonlinear dependencies inherent to the historical K(sub)p data stream (1932-2003) are examined using mutual information and cumulant based cost as discriminating statistics. The discriminating statistics are compared with surrogate data streams that are constructed using the corrected amplitude adjustment Fourier transform (CAAFT) method and capture the linear properties of the original K(sub)p data. Differences are regularly seen in the discriminating statistics a few years prior to <span class="hlt">solar</span> minima, while no differences are apparent at the time of <span class="hlt">solar</span> maximum. These results suggest that the dynamics of the magnetosphere tend to be more linear at <span class="hlt">solar</span> maximum than at solarmore » minimum. The strong nonlinear dependencies tend to peak on a timescale around 40-50 hours and are statistically significant up to one week. Because the <span class="hlt">solar</span> wind driver variables, VB(sub)s and dynamical pressure exhibit a much shorter decorrelation time for nonlinearities, the results seem to indicate that the nonlinearity is related to internal magnetospheric dynamics. Moreover, the timescales for the nonlinearity seem to be on the same order as that for storm/ring current relaxation. We suggest that the strong <span class="hlt">solar</span> wind driving that occurs around <span class="hlt">solar</span> maximum dominates the magnetospheric dynamics suppressing the internal magnetospheric nonlinearity. On the other hand, in the descending phase of the <span class="hlt">solar</span> cycle just prior to <span class="hlt">solar</span> minimum, when magnetospheric <span class="hlt">activity</span> is weaker, the dynamics exhibit a significant nonlinear internal magnetospheric response that may be related to increased <span class="hlt">solar</span> wind speed.« less</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/26085362','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/26085362"><span>Effects of Space Weather on Biomedical Parameters during the <span class="hlt">Solar</span> <span class="hlt">Activity</span> Cycles 23-24.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Ragul'skaya, M V; Rudenchik, E A; Chibisov, S M; Gromozova, E N</p> <p>2015-06-01</p> <p>The results of long-term (1998-2012) biomedical monitoring of the biotropic effects of space weather are discussed. A drastic change in statistical distribution parameters in the middle of 2005 was revealed that did not conform to usual sinusoidal distribution of the biomedical data reflecting changes in the number of <span class="hlt">solar</span> spots over a <span class="hlt">solar</span> <span class="hlt">activity</span> cycle. The dynamics of space weather of 2001-2012 is analyzed. The authors hypothesize that the actual change in statistical distributions corresponds to the adaptation reaction of the biosphere to nonstandard geophysical characteristics of the 24th <span class="hlt">solar</span> <span class="hlt">activity</span> cycle and the probable long-term decrease in <span class="hlt">solar</span> <span class="hlt">activity</span> up to 2067.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2002EGSGA..27.2261Z','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2002EGSGA..27.2261Z"><span>Long-term Variations of The <span class="hlt">Solar</span> <span class="hlt">Activity</span> -- Lower Atmosphere Relationship</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Zaitseva, S.; Akhremtchik, S.; Pudovkin, M.; Besser, B.; Rijnbeek, R.</p> <p></p> <p>Long-term variations of the air temperature in St.Petersburg, Stockholm, Salzburg and English Midlands are considered. There is shown that in the regions under consider- ation the air temperature distinctly depends on the intensity of the lower atmospheric zonal circulation (Blinova index and North Atlantic Oscillation index (NAO)). In turn, the NAO-index is shown to depend on the <span class="hlt">solar</span> <span class="hlt">activity</span>. However, this dependence is rather complicated and exhibits long-period variations associated with secular varia- tions of the <span class="hlt">solar</span> <span class="hlt">activity</span>. A possible mechanism of this phenomena is discussed.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2013AGUFMAE33A0323W','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2013AGUFMAE33A0323W"><span>Effects of <span class="hlt">Solar</span> <span class="hlt">Activities</span> on the Transient Luminous Events</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Wu, Y.; Williams, E.; Chou, J.; Lee, L.; Huang, S.; Chang, S.; Chen, A. B.; Kuo, C.; Su, H.; Hsu, R.; Frey, H. U.; Takahashi, Y.; Lee, L.</p> <p>2013-12-01</p> <p>The Imager of Sprite and Upper Atmosphere Lightning (ISUAL) onboard the Formosat-2 was launched in May 2004; since then, it has continuously observed transient luminous events (TLEs) within the +/-60 degree of latitude for nearly 10 years. Due to ISUAL's long-term observations, the possible correlation between the TLE and the <span class="hlt">solar</span> <span class="hlt">activity</span> can be explored. Among the ISUAL TLEs, elves, which occur at the mesospheric altitude ~90 km and are caused by the heating incurred by the lightning-launched electromagnetic pulse of the lower ionosphere boundary are the most numerous and are the most suitable for this type of study. In previous studies, the elve distribution has proved to be a good surrogate for the lightning with exceptional peak current globally. ISUAL records the occurrence time and the height and location of elves, and the spectral emission intensities at six different band pass including the FUV N2 Lyman-Birge-Hopfield (LBH) band, which is a dominant emission in elves. The LBH intensity not only reflects the peak current of parent lightning, but may also represent the <span class="hlt">solar-activity</span>-driven-lighting's perturbation to the ionosphere. In this study, we first examine whether the 11-year <span class="hlt">solar</span> cycle affects the elve <span class="hlt">activity</span> and altitude by analyzing the elve occurrence rates and heights in different latitudinal regions. To avoid the climatological and instrumental biases in the elve observations, the effects arising from the ENSO and moonlight must be carefully eliminated. Besides, we will discuss the elve variation in shorter time scale due to strong and sudden change of <span class="hlt">solar</span> <span class="hlt">activity</span>. Since the ion density of the mesosphere at mid-latitude may be significantly altered during/after a strong corona mass ejection (CME).Furthermore, it has been proven that the changes in the <span class="hlt">solar</span> X-ray flux dominate the variations in the conductivity profile within the upper characteristic ELF layer (the 90-100km portion of the E-region). we will compare the variation of</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://ntrs.nasa.gov/search.jsp?R=19920036827&hterms=SMM&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D10%26Ntt%3DSMM','NASA-TRS'); return false;" href="https://ntrs.nasa.gov/search.jsp?R=19920036827&hterms=SMM&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D10%26Ntt%3DSMM"><span><span class="hlt">Activity</span> associated with coronal mass ejections at <span class="hlt">solar</span> minimum - SMM observations from 1984-1986</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>St. Cyr, O. C.; Webb, D. F.</p> <p>1991-01-01</p> <p>Seventy-three coronal mass ejections (CMEs) observed by the coronagraph aboard SMM between 1984 and 1986 were examined in order to determine the distribution of various forms of <span class="hlt">solar</span> <span class="hlt">activity</span> that were spatially and temporally associated with mass ejections during <span class="hlt">solar</span> minimum phase. For each coronal mass ejection a speed was measured, and the departure time of the transient from the lower corona estimated. Other forms of <span class="hlt">solar</span> <span class="hlt">activity</span> that appeared within 45 deg longitude and 30 deg latitude of the mass ejection and within +/-90 min of its extrapolated departure time were explored. The statistical results of the analysis of these 73 CMEs are presented, and it is found that slightly less than half of them were infrequently associated with other forms of <span class="hlt">solar</span> <span class="hlt">activity</span>. It is suggested that the distribution of the various forms of <span class="hlt">activity</span> related to CMEs does not change at different phases of the <span class="hlt">solar</span> cycle. For those CMEs with associations, it is found that eruptive prominences and soft X-rays were the most likely forms of <span class="hlt">activity</span> to accompany the appearance of mass ejections.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/19910003165','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/19910003165"><span><span class="hlt">Solar</span> <span class="hlt">Activity</span> and the Sea-surface Temperature Record-evidence of a Long-period Variation in <span class="hlt">Solar</span> Total Irradiance</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Reid, George C.</p> <p>1990-01-01</p> <p>There have been many suggestions over the years of a connection between <span class="hlt">solar</span> <span class="hlt">activity</span> and the Earth's climate on time scales long compared to the 11-year sunspot cycle. They have remained little more than suggestions largely because of the major uncertainties in the climate record itself, and the difficulty in trying to compile a global average from an assembly of measurements that are uneven in both quality and distribution. Different climate time response to <span class="hlt">solar</span> <span class="hlt">activity</span>, some suggesting a positive correlation, some a negative correlation, and some no correlation at all. The only excuse for making yet another such suggestion is that much effort has been devoted in recent years to compiling climate records for the past century or more that are internally consistent and believable, and that a decadal-scale record of <span class="hlt">solar</span> total irradiance is emerging from spacecraft measurements, and can be used to set limits on the variation that is likely to have occurred on these time scales. The work described here was originally inspired by the observation that the time series of globally averaged sea-surface temperatures over the past 120 years or so, as compiled by the British Meteorological Office group (Folland and Kates, 1984), bore a resonable similarity to the long-term average sunspot number, which is an indicator of the secular variability of <span class="hlt">solar</span> <span class="hlt">activity</span>. The two time series are shown where the sunspot number is shown as the 135-month running mean, and the SST variation is shown as the departure from an arbitrary average value. The simplest explanation of the similarity, if one accepts it as other than coincidental, is that the sun's luminosity may have been varying more or less in step with the level of <span class="hlt">solar</span> <span class="hlt">activity</span>, or in other words that there is a close coupling between the sun's magnetic condition and its radiative output on time scales longer than the 11-year cycle. Such an idea is not new, and in fact the time series shown can be regarded as a modern</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2006ihy..workE..76I','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2006ihy..workE..76I"><span>A <span class="hlt">Solar</span> Station for Education and Research on <span class="hlt">Solar</span> <span class="hlt">Activity</span> at a National University in Peru</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Ishitsuka, J. K.</p> <p>2006-11-01</p> <p>pepe@geo.igp.gob.pe Beginning in 1937, the Carnegie Institution of Washington made <span class="hlt">active</span> regional observations with a spectro-helioscope at the Huancayo Observatory. In 1957, during the celebration of the International Geophysical Year Mutsumi Ishitsuka arrived at the Geophysical Institute of Peru and restarted <span class="hlt">solar</span> observations from the Huancayo Observatory. Almost 69 years have passed and many contributions for the geophysical and <span class="hlt">solar</span> sciences have been made. Now the Instituto Geofisico del Peru (IGP), in cooperation with the Faculty of Sciences of the Universidad Nacional San Luis Gonzaga de Ica (UNICA), and with the support of the National Astronomical Observatory of Japan, are planning to construct a <span class="hlt">solar</span> station refurbishing a coelostat that worked for many years at the Huancayo Observatory. A 15 cm refractor telescope is already installed at the university, for the observation of sunspots. A <span class="hlt">solar</span> Flare Monitor Telescope (FMT) from Hida Observatory of Kyoto University could be sent to Peru and installed at the <span class="hlt">solar</span> station at UNICA. As the refurbished coelostat, FMT will become a good tool to improve education and research in sciences.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.osti.gov/servlets/purl/6325484','SCIGOV-STC'); return false;" href="https://www.osti.gov/servlets/purl/6325484"><span>Annual DOE <span class="hlt">active</span> <span class="hlt">solar</span> heating and cooling contractors' review meeting. Premeeting proceedings and project summaries</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>None,</p> <p>1981-09-01</p> <p>Ninety-three project summaries are presented which discuss the following aspects of <span class="hlt">active</span> <span class="hlt">solar</span> heating and cooling: Rankine <span class="hlt">solar</span> cooling systems; absorption <span class="hlt">solar</span> cooling systems; desiccant <span class="hlt">solar</span> cooling systems; <span class="hlt">solar</span> heat pump systems; <span class="hlt">solar</span> hot water systems; special projects (such as the National <span class="hlt">Solar</span> Data Network, hybrid <span class="hlt">solar</span> thermal/photovoltaic applications, and heat transfer and water migration in soils); administrative/management support; and <span class="hlt">solar</span> collector, storage, controls, analysis, and materials technology. (LEW)</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=3556150','PMC'); return false;" href="https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=3556150"><span>Thin-film fixed-bed reactor for <span class="hlt">solar</span> photocatalytic inactivation of Aeromonas hydrophila: <span class="hlt">influence</span> of water quality</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>2012-01-01</p> <p>Background Controlling fish disease is one of the major concerns in contemporary aquaculture. The use of antibiotics or chemical disinfection cannot provide a healthy aquaculture system without residual effects. Water quality is also important in determining the success or failure of fish production. Several <span class="hlt">solar</span> photocatalytic reactors have been used to treat drinking water or waste water without leaving chemical residues. This study has investigated the impact of several key aspects of water quality on the inactivation of the pathogenic bacterium Aeromonas hydrophila using a pilot-scale thin-film fixed-bed reactor (TFFBR) system. Results The level of inactivation of Aeromonas hydrophila ATCC 35654 was determined using a TFFBR with a photocatalytic area of 0.47 m2 under the <span class="hlt">influence</span> of various water quality variables (pH, conductivity, turbidity and colour) under high <span class="hlt">solar</span> irradiance conditions (980–1100 W m-2), at a flow rate of 4.8 L h-1 through the reactor. Bacterial enumeration were obtained through conventional plate count using trypticase soy agar media, cultured in conventional aerobic conditions to detect healthy cells and under ROS-neutralised conditions to detect both healthy and sub-lethally injured (oxygen-sensitive) cells. The results showed that turbidity has a major <span class="hlt">influence</span> on <span class="hlt">solar</span> photocatalytic inactivation of A. hydrophila. Humic acids appear to decrease TiO2 effectiveness under full sunlight and reduce microbial inactivation. pH in the range 7–9 and salinity both have no major effect on the extent of photoinactivation or sub-lethal injury. Conclusions This study demonstrates the effectiveness of the TFFBR in the inactivation of Aeromonas hydrophila under the <span class="hlt">influence</span> of several water quality variables at high <span class="hlt">solar</span> irradiance, providing an opportunity for the application of <span class="hlt">solar</span> photocatalysis in aquaculture systems, as long as turbidity remains low. PMID:23194331</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2013SoPh..286..157S','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2013SoPh..286..157S"><span>Signatures of Slow <span class="hlt">Solar</span> Wind Streams from <span class="hlt">Active</span> Regions in the Inner Corona</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Slemzin, V.; Harra, L.; Urnov, A.; Kuzin, S.; Goryaev, F.; Berghmans, D.</p> <p>2013-08-01</p> <p>The identification of <span class="hlt">solar</span>-wind sources is an important question in <span class="hlt">solar</span> physics. The existing <span class="hlt">solar</span>-wind models ( e.g., the Wang-Sheeley-Arge model) provide the approximate locations of the <span class="hlt">solar</span> wind sources based on magnetic field extrapolations. It has been suggested recently that plasma outflows observed at the edges of <span class="hlt">active</span> regions may be a source of the slow <span class="hlt">solar</span> wind. To explore this we analyze an isolated <span class="hlt">active</span> region (AR) adjacent to small coronal hole (CH) in July/August 2009. On 1 August, Hinode/EUV Imaging Spectrometer observations showed two compact outflow regions in the corona. Coronal rays were observed above the <span class="hlt">active</span>-region coronal hole (ARCH) region on the eastern limb on 31 July by STEREO-A/EUVI and at the western limb on 7 August by CORONAS- Photon/TESIS telescopes. In both cases the coronal rays were co-aligned with open magnetic-field lines given by the potential field source surface model, which expanded into the streamer. The <span class="hlt">solar</span>-wind parameters measured by STEREO-B, ACE, Wind, and STEREO-A confirmed the identification of the ARCH as a source region of the slow <span class="hlt">solar</span> wind. The results of the study support the suggestion that coronal rays can represent signatures of outflows from ARs propagating in the inner corona along open field lines into the heliosphere.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2000AAS...197.8709S','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2000AAS...197.8709S"><span>Real Research In The Classroom - <span class="hlt">Solar</span> <span class="hlt">Active</span> Longitudes</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Stagg, T.; Gearen, M.; Jacoby, S. H.; Jones, H. P.; Henney, C. J.; Hill, F.</p> <p>2000-12-01</p> <p>We present a high-school level educational/research module for a project that improves computer and analytical skills and contributes new scientific results to the field of <span class="hlt">solar</span> astronomy and physics. The module has been developed within the RET (Research Experience for Teachers) program as a new application of a cooperative project between the RBSE (Research-Based Science Education) initiative of the NSF and the NASA Education/Public Outreach program. The research goal is to improve our knowledge of the characteristics of <span class="hlt">solar</span> <span class="hlt">active</span> longitudes, where sunspots tend to cluster. In particular, the rotation rate of these regions is poorly known. It is suspected that the <span class="hlt">active</span> longitude rotation rate (ALRR) is different from the rotation rate of the <span class="hlt">solar</span> surface. If this is true, the ALRR can be compared with the internal rotation rate deduced by helioseismology providing an estimate of the <span class="hlt">active</span> region depth. A good determination of the ALRR requires the measurement of the position of thousands of individual <span class="hlt">active</span> regions, a step best done by interactive examination of images, selection of regions, and determination of heliographic position. These tasks are well-suited for high school students, who are thus provided with a motivation to improve their computer and scientific thinking skills. ScionImage (PC)/NIH Image (Macs) macros for this purpose have been developed which access a CD-ROM of 25 years of NSO/Kitt Peak magnetogram data and laboratory exercises developed previously for classroom use. In the future, a web site will be created for collecting the data from classrooms across the US, and for status reports on the results.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/28722128','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/28722128"><span><span class="hlt">Solar</span> insolation in springtime <span class="hlt">influences</span> age of onset of bipolar I disorder.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Bauer, M; Glenn, T; Alda, M; Aleksandrovich, M A; Andreassen, O A; Angelopoulos, E; Ardau, R; Ayhan, Y; Baethge, C; Bharathram, S R; Bauer, R; Baune, B T; Becerra-Palars, C; Bellivier, F; Belmaker, R H; Berk, M; Bersudsky, Y; Bicakci, Ş; Birabwa-Oketcho, H; Bjella, T D; Bossini, L; Cabrera, J; Cheung, E Y W; Del Zompo, M; Dodd, S; Donix, M; Etain, B; Fagiolini, A; Fountoulakis, K N; Frye, M A; Gonzalez-Pinto, A; Gottlieb, J F; Grof, P; Harima, H; Henry, C; Isometsä, E T; Janno, S; Kapczinski, F; Kardell, M; Khaldi, S; Kliwicki, S; König, B; Kot, T L; Krogh, R; Kunz, M; Lafer, B; Landén, M; Larsen, E R; Lewitzka, U; Licht, R W; Lopez-Jaramillo, C; MacQueen, G; Manchia, M; Marsh, W; Martinez-Cengotitabengoa, M; Melle, I; Meza-Urzúa, F; Yee Ming, M; Monteith, S; Morken, G; Mosca, E; Munoz, R; Mythri, S V; Nacef, F; Nadella, R K; Nery, F G; Nielsen, R E; O'Donovan, C; Omrani, A; Osher, Y; Østermark Sørensen, H; Ouali, U; Pica Ruiz, Y; Pilhatsch, M; Pinna, M; da Ponte, F D R; Quiroz, D; Ramesar, R; Rasgon, N; Reddy, M S; Reif, A; Ritter, P; Rybakowski, J K; Sagduyu, K; Scippa, Â M; Severus, E; Simhandl, C; Stein, D J; Strejilevich, S; Subramaniam, M; Sulaiman, A H; Suominen, K; Tagata, H; Tatebayashi, Y; Tondo, L; Torrent, C; Vaaler, A E; Veeh, J; Vieta, E; Viswanath, B; Yoldi-Negrete, M; Zetin, M; Zgueb, Y; Whybrow, P C</p> <p>2017-12-01</p> <p>To confirm prior findings that the larger the maximum monthly increase in <span class="hlt">solar</span> insolation in springtime, the younger the age of onset of bipolar disorder. Data were collected from 5536 patients at 50 sites in 32 countries on six continents. Onset occurred at 456 locations in 57 countries. Variables included <span class="hlt">solar</span> insolation, birth-cohort, family history, polarity of first episode and country physician density. There was a significant, inverse association between the maximum monthly increase in <span class="hlt">solar</span> insolation at the onset location, and the age of onset. This effect was reduced in those without a family history of mood disorders and with a first episode of mania rather than depression. The maximum monthly increase occurred in springtime. The youngest birth-cohort had the youngest age of onset. All prior relationships were confirmed using both the entire sample, and only the youngest birth-cohort (all estimated coefficients P < 0.001). A large increase in springtime <span class="hlt">solar</span> insolation may impact the onset of bipolar disorder, especially with a family history of mood disorders. Recent societal changes that affect light exposure (LED lighting, mobile devices backlit with LEDs) may <span class="hlt">influence</span> adaptability to a springtime circadian challenge. © 2017 John Wiley & Sons A/S. Published by John Wiley & Sons Ltd.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/19920020961','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/19920020961"><span>Investigation of <span class="hlt">solar</span> <span class="hlt">active</span> regions at high resolution by balloon flights of the <span class="hlt">solar</span> optical universal polarimeter, definition phase</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Tarbell, Theodore D.; Topka, Kenneth P.</p> <p>1992-01-01</p> <p>The definition phase of a scientific study of <span class="hlt">active</span> regions on the sun by balloon flight of a former Spacelab instrument, the <span class="hlt">Solar</span> Optical Universal Polarimeter (SOUP) is described. SOUP is an optical telescope with image stabilization, tunable filter and various cameras. After the flight phase of the program was cancelled due to budgetary problems, scientific and engineering studies relevant to future balloon experiments of this type were completed. High resolution observations of the sun were obtained using SOUP components at the Swedish <span class="hlt">Solar</span> Observatory in the Canary Islands. These were analyzed and published in studies of <span class="hlt">solar</span> magnetic fields and <span class="hlt">active</span> regions. In addition, testing of low-voltage piezoelectric transducers was performed, which showed they were appropriate for use in image stabilization on a balloon.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://ntrs.nasa.gov/search.jsp?R=19900032622&hterms=kessler&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAuthor-Name%26N%3D0%26No%3D70%26Ntt%3Dkessler','NASA-TRS'); return false;" href="https://ntrs.nasa.gov/search.jsp?R=19900032622&hterms=kessler&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAuthor-Name%26N%3D0%26No%3D70%26Ntt%3Dkessler"><span>Effects on the orbital debris environment due to <span class="hlt">solar</span> <span class="hlt">activity</span></span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Kessler, Donald J.; Anz-Meador, Phillip D.</p> <p>1990-01-01</p> <p>The rate that earth-orbiting debris is removed from the environment is dependent on a number of factors which include orbital altitude and <span class="hlt">solar</span> <span class="hlt">activity</span>. It is generally believed that at lower altitudes and especially during periods of high <span class="hlt">solar</span> <span class="hlt">activity</span>, debris generated in the past will be eliminated from the environment. While some debris is eliminated, most is replaced by old debris from higher altitudes or new debris from recent launches. Some low altitude debris, which would reenter if the debris were in circular orbits, does not reenter because the debris is in higher-energy elliptical orbits.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/19850025584','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/19850025584"><span>Simultaneous <span class="hlt">Solar</span> Maximum Mission and Very Large Array (VLA) observations of <span class="hlt">solar</span> <span class="hlt">active</span> regions</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Lang, K. R.</p> <p>1985-01-01</p> <p>Simultaneous observations of <span class="hlt">solar</span> <span class="hlt">active</span> regions with the <span class="hlt">Solar</span> Maximum Mission (SMM) Satellite and the Very Large Array (VLA) have been obtained and analyzed. Combined results enhance the scientific return for beyond that expeted from using either SMM or VLA alone. A total of two weeks of simultaneous SMM/VLA data were obtained. The multiple wavelength VLA observations were used to determine the temperature and magnetic structure at different heights within coronal loops. These data are compared with simultaneous SMM observations. Several papers on the subject are in progress. They include VLA observations of compact, transient sources in the transition region; simultaneous SMM/VLA observations of the coronal loops in one <span class="hlt">active</span> region and the evolution of another one; and sampling of the coronal plasma using thermal cyclotron lines (magnetic field - VLA) and soft X ray spectral lines (electron density and electron temperaure-SMM).</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/19860008385','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/19860008385"><span><span class="hlt">Influence</span> of design variables on radiation hardness of silicon MINP <span class="hlt">solar</span> cells</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Anderson, W. A.; Solaun, S.; Rao, B. B.; Banerjee, S.</p> <p>1985-01-01</p> <p>Metal-insulator-N/P silicon (MINP) <span class="hlt">solar</span> cells were fabricated using different substrate resistivity values, different N-layer designs, and different I-layer designs. A shallow junction into an 0.3 ohm-cm substrate gave best efficiency whereas a deeper junction into a 1 to 4 ohm-cm substrate gave improved radiation hardness. I-layer design variation did little to <span class="hlt">influence</span> radiation hardness.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2018JGRA..123.2116C','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2018JGRA..123.2116C"><span>Responses of <span class="hlt">Solar</span> Irradiance and the Ionosphere to an Intense <span class="hlt">Activity</span> Region</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Chen, Yiding; Liu, Libo; Le, Huijun; Wan, Weixing</p> <p>2018-03-01</p> <p><span class="hlt">Solar</span> rotation (SR) variation dominates <span class="hlt">solar</span> extremely ultraviolet (EUV) changes on the timescale of days. The F10.7 index is usually used as an indicator for <span class="hlt">solar</span> EUV. The SR variation of F10.7 significantly enhanced during the 2008th-2009th Carrington rotations (CRs) owing to an intense <span class="hlt">active</span> region; F10.7 increased about 180 units during that SR period. That was the most prominent SR variation of F10.7 during <span class="hlt">solar</span> cycle 23. In this paper, global electron content (GEC) is used to investigate ionospheric response to that strong variation of <span class="hlt">solar</span> irradiance indicated by F10.7. The variation of GEC with F10.7 was anomalous (GEC-F10.7 slope significantly decreased) during the 2008th-2009th CRs; however, GEC versus EUV variation during that period was consistent with that during adjacent time intervals when using <span class="hlt">Solar</span> Heliospheric Observatory/<span class="hlt">Solar</span> EUV Monitor 26-34 nm EUV measurements. The reason is that F10.7 response to that intense <span class="hlt">active</span> region was much stronger than EUV response; thus, the EUV-F10.7 slope decreased. We confirmed decreased EUV-F10.7 slope during the 2008th-2009th CRs for different wavelengths within 27-120 nm using Thermosphere, Ionosphere, Mesosphere Energetics and Dynamics/<span class="hlt">Solar</span> EUV Experiment high spectral resolution EUV measurements. And on the basis of <span class="hlt">Solar</span> Heliospheric Observatory/<span class="hlt">Solar</span> EUV Monitor EUV measurements during <span class="hlt">solar</span> cycle 23, we further presented that EUV-F10.7 slope statistically tends to decrease when the SR variation of F10.7 significantly enhances. Moreover, we found that ionospheric time lag effect to EUV is exaggerated when using F10.7, owing to the time lag effect of EUV to F10.7.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://ntrs.nasa.gov/search.jsp?R=19740020960&hterms=Climate+change+Effects&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D10%26Ntt%3DClimate%2Bchange%2BEffects','NASA-TRS'); return false;" href="https://ntrs.nasa.gov/search.jsp?R=19740020960&hterms=Climate+change+Effects&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D10%26Ntt%3DClimate%2Bchange%2BEffects"><span>Relationships between <span class="hlt">solar</span> <span class="hlt">activity</span> and climate change. [sunspot cycle effects on lower atmosphere</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Roberts, W. O.</p> <p>1974-01-01</p> <p>Recurrent droughts are related to the double sunspot cycle. It is suggested that high <span class="hlt">solar</span> <span class="hlt">activity</span> generally increases meridional circulations and blocking patterns at high and intermediate latitudes, especially in winter. This effect is related to the sudden formation of cirrus clouds during strong geomagnetic <span class="hlt">activity</span> that originates in the <span class="hlt">solar</span> corpuscular emission.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2015EGUGA..17.6745Y','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2015EGUGA..17.6745Y"><span>A new simple dynamo model for <span class="hlt">solar</span> <span class="hlt">activity</span> cycle</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Yokoi, Nobumitsu; Schmitt, Dieter</p> <p>2015-04-01</p> <p>The <span class="hlt">solar</span> magnetic <span class="hlt">activity</span> cycle has been investigated in an elaborated manner with several types of dynamo models [1]. In most of the current mean-field approaches, the inhomogeneity of the large-scale flow is treated as an essential ingredient in the mean magnetic field equation whereas it is completely neglected in the turbulence equation. In this work, a new simple model for the <span class="hlt">solar</span> <span class="hlt">activity</span> cycle is proposed. The present model differs from the previous ones mainly in two points. First, in addition to the helicity coefficient α, we consider a term related to the cross helicity, which represents the effect of the inhomogeneous mean flow, in the turbulent electromotive force [2, 3]. Second, this transport coefficient (γ) is not treated as an adjustable parameter, but the evolution equation for γ is simultaneously solved. The basic scenario for the <span class="hlt">solar</span> <span class="hlt">activity</span> cycle in this approach is as follows: The toroidal field is induced by the toroidal rotation in mediation by the turbulent cross helicity. Then due to the α or helicity effect, the poloidal field is generated from the toroidal field. The poloidal field induced by the α effect produces a turbulent cross helicity whose sign is opposite to the original one (negative cross-helicity production). The cross helicity with this opposite sign induces a reversed toroidal field. Results of the eigenvalue analysis of the model equations are shown, which confirm the above scenario. References [1] Charbonneau, Living Rev. <span class="hlt">Solar</span> Phys. 7, 3 (2010). [2] Yoshizawa, A. Phys. Fluids B 2, 1589 (1990). [3] Yokoi, N. Geophys. Astrophys. Fluid Dyn. 107, 114 (2013).</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2018JASTP.167...30L','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2018JASTP.167...30L"><span>Can <span class="hlt">solar</span> cycle modulate the ENSO effect on the Pacific/North American pattern?</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Li, Delin; Xiao, Ziniu</p> <p>2018-01-01</p> <p>The ENSO effect on the Pacific/North American pattern (PNA) is well-known robust. Recent studies from observations and model simulations have reported that some important atmospheric circulation systems of extratropics are markedly modulated by the 11-year <span class="hlt">solar</span> cycle. But less effort has been devoted to revealing the <span class="hlt">solar</span> <span class="hlt">influence</span> on the PNA. We thus hypothesize that the instability and uncertainty in the relationship between <span class="hlt">solar</span> <span class="hlt">activity</span> and PNA could be due to the ENSO impacts. In this study, <span class="hlt">solar</span> cycle modulation of the ENSO effect on the PNA has been statistically examined by the observations from NOAA and NCEP/NCAR for the period of 1950-2014. Results indicate that during the high <span class="hlt">solar</span> <span class="hlt">activity</span> (HS) years, the PNA has stronger relevance to the ENSO, and the response of tropospheric geopotential height to ENSO variability is broadly similar to the typical positive PNA pattern. However, in the case of low <span class="hlt">solar</span> <span class="hlt">activity</span> (LS) years, the correlation between ENSO and PNA decreases relatively and the response has some resemblance to the negative phase of Arctic Oscillation (AO). Also, we find the impacts of <span class="hlt">solar</span> <span class="hlt">activity</span> on the middle troposphere are asymmetric during the different <span class="hlt">solar</span> cycle phases, and the weak PNA-like response to <span class="hlt">solar</span> <span class="hlt">activity</span> only presents in the HS years. Closer inspection suggests that the higher <span class="hlt">solar</span> <span class="hlt">activity</span> has a much more remarkable modulation on the PNA-like response to the warm ENSO (WE) than that to the cold ENSO (CE), particularly over the Northeast Pacific region. The possible cause of the different responses might be the <span class="hlt">solar</span> <span class="hlt">influence</span> on the subtropical westerlies of upper troposphere. When the sea surface temperature (SST) of east-central tropical Pacific is anomalously warm, the upper tropospheric westerlies are significantly modulated by the higher <span class="hlt">solar</span> <span class="hlt">activity</span>, resulting in the acceleration and eastward shift of the North Pacific subtropical jet, which favors the propagation of WE signal from the tropical Pacific</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2016EGUGA..18.9626C','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2016EGUGA..18.9626C"><span>Tsunami related to <span class="hlt">solar</span> and geomagnetic <span class="hlt">activity</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Cataldi, Gabriele; Cataldi, Daniele; Straser, Valentino</p> <p>2016-04-01</p> <p>The authors of this study wanted to verify the existence of a correlation between earthquakes of high intensity capable of generating tsunami and variations of <span class="hlt">solar</span> and Earth's geomagnetic <span class="hlt">activity</span>. To confirming or not the presence of this kind of correlation, the authors analyzed the conditions of Spaceweather "near Earth" and the characteristics of the Earth's geomagnetic field in the hours that preceded the four earthquakes of high intensity that have generated tsunamis: 1) Japan M9 earthquake occurred on March 11, 2011 at 05:46 UTC; 2) Japan M7.1 earthquake occurred on October 25, 2013 at 17:10 UTC; 3) Chile M8.2 earthquake occurred on April 1, 2014 at 23:46 UTC; 4) Chile M8.3 earthquake occurred on September 16, 2015 at 22:54 UTC. The data relating to the four earthquakes were provided by the United States Geological Survey (USGS). The data on ion density used to realize the correlation study are represented by: <span class="hlt">solar</span> wind ion density variation detected by ACE (Advanced Composition Explorer) Satellite, in orbit near the L1 Lagrange point, at 1.5 million of km from Earth, in direction of the Sun. The instrument used to perform the measurement of the <span class="hlt">solar</span> wind ion density is the Electron, Proton, and Alpha Monitor (EPAM) instrument, equipped on the ACE Satellite. To conduct the study, the authors have taken in consideration the variation of the <span class="hlt">solar</span> wind protons density of three different energy fractions: differential proton flux 1060-1900 keV (p/cm^2-sec-ster-MeV); differential proton flux 761-1220 keV (p/cm^2-sec-ster-MeV); differential proton flux 310-580 keV (p/cm^2-sec-ster-MeV). Geomagnetic <span class="hlt">activity</span> data were provided by Tromsø Geomagnetic Observatory (TGO), Norway; by Scoresbysund Geomagnetic Observatory (SCO), Greenland, Denmark and by Space Weather Prediction Center of Pushkov Institute of terrestrial magnetism, ionosphere and radio wave propagation (IZMIRAN), Troitsk, Moscow Region. The results of the study, in agreement with what already</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2016GPC...145....1P','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2016GPC...145....1P"><span>Evidence of <span class="hlt">solar</span> <span class="hlt">activity</span> and El Niño signals in tree rings of Araucaria araucana and A. angustifolia in South America</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Perone, A.; Lombardi, F.; Marchetti, M.; Tognetti, R.; Lasserre, B.</p> <p>2016-10-01</p> <p>Tree rings reveal climatic variations through years, but also the effect of <span class="hlt">solar</span> <span class="hlt">activity</span> in <span class="hlt">influencing</span> the climate on a large scale. In order to investigate the role of <span class="hlt">solar</span> cycles on climatic variability and to analyse their <span class="hlt">influences</span> on tree growth, we focused on tree-ring chronologies of Araucaria angustifolia and Araucaria araucana in four study areas: Irati and Curitiba in Brazil, Caviahue in Chile, and Tolhuaca in Argentina. We obtained an average tree-ring chronology of 218, 117, 439, and 849 years for these areas, respectively. Particularly, the older chronologies also included the period of the Maunder and Dalton minima. To identify periodicities and trends observable in tree growth, the time series were analysed using spectral, wavelet and cross-wavelet techniques. Analysis based on the Multitaper method of annual growth rates identified 2 cycles with periodicities of 11 (Schwebe cycle) and 5.5 years (second harmonic of Schwebe cycle). In the Chilean and Argentinian sites, significant agreement between the time series of tree rings and the 11-year <span class="hlt">solar</span> cycle was found during the periods of maximum <span class="hlt">solar</span> <span class="hlt">activity</span>. Results also showed oscillation with periods of 2-7 years, probably induced by local environmental variations, and possibly also related to the El-Niño events. Moreover, the Morlet complex wavelet analysis was applied to study the most relevant variability factors affecting tree-ring time series. Finally, we applied the cross-wavelet spectral analysis to evaluate the time lags between tree-ring and sunspot-number time series, as well as for the interaction between tree rings, the Southern Oscillation Index (SOI) and temperature and precipitation. Trees sampled in Chile and Argentina showed more evident responses of fluctuations in tree-ring time series to the variations of short and long periodicities in comparison with the Brazilian ones. These results provided new evidence on the <span class="hlt">solar</span> <span class="hlt">activity</span>-climate pattern-tree ring connections over</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2011AGUFMPP41C1781O','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2011AGUFMPP41C1781O"><span>Mid-Holocene paleoclimatic changes and <span class="hlt">solar</span> <span class="hlt">activity</span> in San'in District, mid-latitude North Pacific Region</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Okazaki, Y.; Seto, K.; Sakai, T.; Ooki, A.; yamada, K.; Dettman, D. L.</p> <p>2011-12-01</p> <p>Evidence shows that <span class="hlt">solar</span> <span class="hlt">activity</span> <span class="hlt">influences</span> climate on a global scale. In the mid-latitude region, climate change is expected to change precipitation patterns. Concurrently, variation in <span class="hlt">solar</span> <span class="hlt">activity</span> may <span class="hlt">influence</span> phytoplankton productivity. It seems that these changes should be recorded in sediment and organic matter deposits in coastal lagoons. In this study, we discuss the relationship between climate change and <span class="hlt">solar</span> <span class="hlt">activity</span> in the mid-Holocene in the northern hemisphere mid-latitude region based on grain size analysis, total organic carbon (TOC) content and organic carbon accumulation rates (Corg A.R.) in coastal lagoon sediment core samples. The INB core was drilled to produce a high resolution record of Holocene paleoenvironmental change in the San'in District, western Japan. The core is 19.17m in total length and is divided into Unit I~VII by lithofacies. Holocene sediment, primarily organic silt, forms Unit III and above in this core. Unit III was deposited from 8.4 to 5.4 ka, when sea level rose during the Jomon transgression; its depositional environment is a coastal lagoon. Progradation of the river mouth during the sea level rise lead to an increase in the C/N ratio of organic matter. Unit IV contains the volcanic Shigaku pyroclastic flow (the sixth stage of volcanic <span class="hlt">activity</span> of the Sanbe volcano), and Unit V reflects deposition in a freshwater lake or swamp. Above this aggredational sediments were deposited by small rivers. This study focused on the coastal lagoon sediments of Unit III (8.4 to 5.4 ka); we carried out CNS elemental analysis and grain size analysis with a resolution of approximately five years. TOC content is variable and increases from 0.5 to 5%. Variation in TOC content is relatively well correlated with atmospheric radiocarbon 14C (Delta 14C) and therefore with <span class="hlt">solar</span> <span class="hlt">activity</span>, although the relationship is unclear in the upper portion of Unit III. The trend in Corg A.R. is different than TOC contents, about 40g/m/yr at ~8ka and</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://ntrs.nasa.gov/search.jsp?R=19750008353&hterms=activity+Physics&qs=N%3D0%26Ntk%3DAll%26Ntx%3Dmode%2Bmatchall%26Ntt%3Dactivity%2BPhysics','NASA-TRS'); return false;" href="https://ntrs.nasa.gov/search.jsp?R=19750008353&hterms=activity+Physics&qs=N%3D0%26Ntk%3DAll%26Ntx%3Dmode%2Bmatchall%26Ntt%3Dactivity%2BPhysics"><span><span class="hlt">Solar</span> and terrestrial physics. [effects of <span class="hlt">solar</span> <span class="hlt">activities</span> on earth environment</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p></p> <p>1975-01-01</p> <p>The effects of <span class="hlt">solar</span> radiation on the near space and biomental earth, the upper atmosphere, and the magnetosphere are discussed. Data obtained from the OSO satellites pertaining to the <span class="hlt">solar</span> cycle variation of extreme ultraviolet (EUV) radiation are analyzed. The effects of <span class="hlt">solar</span> cycle variation of the characteristics of the <span class="hlt">solar</span> wind are examined. The fluid mechanics of shock waves and the specific relationship to the characteristics of <span class="hlt">solar</span> shock waves are investigated. The <span class="hlt">solar</span> and corpuscular heating of the upper atmosphere is reported based on the findings of the AEROS and NATE experiments. Seasonal variations of the upper atmosphere composition are plotted based on OGO-6 mass spectrometer data.</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://hdl.handle.net/2060/20170010267','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/20170010267"><span>Early Estimation of <span class="hlt">Solar</span> <span class="hlt">Activity</span> Cycle: Potential Capability and Limits</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Kitiashvili, Irina N.; Collins, Nancy S.</p> <p>2017-01-01</p> <p>The variable <span class="hlt">solar</span> magnetic <span class="hlt">activity</span> known as the 11-year <span class="hlt">solar</span> cycle has the longest history of <span class="hlt">solar</span> observations. These cycles dramatically affect conditions in the heliosphere and the Earth's space environment. Our current understanding of the physical processes that make up global <span class="hlt">solar</span> dynamics and the dynamo that generates the magnetic fields is sketchy, resulting in unrealistic descriptions in theoretical and numerical models of the <span class="hlt">solar</span> cycles. The absence of long-term observations of <span class="hlt">solar</span> interior dynamics and photospheric magnetic fields hinders development of accurate dynamo models and their calibration. In such situations, mathematical data assimilation methods provide an optimal approach for combining the available observational data and their uncertainties with theoretical models in order to estimate the state of the <span class="hlt">solar</span> dynamo and predict future cycles. In this presentation, we will discuss the implementation and performance of an Ensemble Kalman Filter data assimilation method based on the Parker migratory dynamo model, complemented by the equation of magnetic helicity conservation and longterm sunspot data series. This approach has allowed us to reproduce the general properties of <span class="hlt">solar</span> cycles and has already demonstrated a good predictive capability for the current cycle, 24. We will discuss further development of this approach, which includes a more sophisticated dynamo model, synoptic magnetogram data, and employs the DART Data Assimilation Research Testbed.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2004AGUFMED13D0740A','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2004AGUFMED13D0740A"><span>Hands-on <span class="hlt">Activities</span> for Exploring the <span class="hlt">Solar</span> System in K-14 Formal and Informal Education Settings</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Allen, J. S.; Tobola, K. W.</p> <p>2004-12-01</p> <p>Introduction: <span class="hlt">Activities</span> developed by NASA scientists and teachers focus on integrating Planetary Science <span class="hlt">activities</span> with existing Earth science, math, and language arts curriculum. Educators may choose <span class="hlt">activities</span> that fit a particular concept or theme within their curriculum from <span class="hlt">activities</span> that highlight missions and research pertaining to exploring the <span class="hlt">solar</span> system. Most of the <span class="hlt">activities</span> use simple, inexpensive techniques that help students understand the how and why of what scientists are learning about comets, asteroids, meteorites, moons and planets. The web sites for the <span class="hlt">activities</span> contain current information so students experience recent mission information such as data from Mars rovers or the status of Stardust sample return. The Johnson Space Center Astromaterials Research and Exploration Science education team has compiled a variety of NASA <span class="hlt">solar</span> system <span class="hlt">activities</span> to produce an annotated thematic syllabus useful to classroom educators and informal educators as they teach space science. An important aspect of the syllabus is that it highlights appropriate science content information and key science and math concepts so educators can easily identify <span class="hlt">activities</span> that will enhance curriculum development. The outline contains URLs for the <span class="hlt">activities</span> and NASA educator guides as well as links to NASA mission science and technology. In the informal setting, educators can use <span class="hlt">solar</span> system exploration <span class="hlt">activities</span> to reinforce learning in association with thematic displays, planetarium programs, youth group gatherings, or community events. In both the informal and the primary education levels the <span class="hlt">activities</span> are appropriately designed to excite interest, arouse curiosity and easily take the participants from pre-awareness to the awareness stage. Middle school educators will find <span class="hlt">activities</span> that enhance thematic science and encourage students to think about the scientific process of investigation. Some of the <span class="hlt">activities</span> offered may easily be adapted for the upper</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2005JSR....53..319V','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2005JSR....53..319V"><span>Are <span class="hlt">solar</span> <span class="hlt">activity</span> and sperm whale Physeter macrocephalus strandings around the North Sea related?</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Vanselow, Klaus Heinrich; Ricklefs, Klaus</p> <p>2005-04-01</p> <p>In the final decades of the last century, an increasing number of strandings of male sperm whales ( Physeter macrocephalus) around the North Sea led to an increase in public interest. Anthropogenic <span class="hlt">influences</span> (such as contaminants or intensive sound disturbances) are supposed to be the main causes, but natural environmental effects may also explain the disorientation of the animals. We compared the documented sperm whale strandings in the period from 1712 to 2003 with <span class="hlt">solar</span> <span class="hlt">activity</span>, especially with sun spot number periodicity and found that 90% of 97 sperm whale stranding events around the North Sea took place when the smoothed sun spot period length was below the mean value of 11 years, while only 10% happened during periods of longer sun spot cycles. The relation becomes even more pronounced (94% to 6%, n = 70) if a smaller time window from November to March is used (which seems to be the main southward migration period of male sperm whales). Adequate chi-square tests of the data give a significance of 1% error probability that sperm whale strandings can depend on <span class="hlt">solar</span> <span class="hlt">activity</span>. As an alternative explanation, we suggest that variations of the earth's magnetic field, due to variable energy fluxes from the sun to the earth, may cause a temporary disorientation of migrating animals.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2015AGUFMSH21C..03S','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2015AGUFMSH21C..03S"><span>The <span class="hlt">SOLAR</span>-C Mission</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Suematsu, Y.</p> <p>2015-12-01</p> <p>The <span class="hlt">Solar</span>-C is a Japan-led international <span class="hlt">solar</span> mission planned to be launched in mid2020. It is designed to investigate the magnetic <span class="hlt">activities</span> of the Sun, focusing on the study in heating and dynamical phenomena of the chromosphere and corona, and also to develop an algorithm for predicting short and long term <span class="hlt">solar</span> evolution. Since it has been revealed that the different parts of the magnetized <span class="hlt">solar</span> atmosphere are essentially coupled, the <span class="hlt">SOLAR</span>-C should tackle the spatial scales and temperature regimes that need to be observed in order to achieve a comprehensive physical understanding of this coupling. The science of <span class="hlt">Solar</span>-C will greatly advance our understanding of the Sun, of basic physical processes operating throughout the universe. To dramatically improve the situation, <span class="hlt">SOLAR</span>-C will carry three dedicated instruments; the <span class="hlt">Solar</span> UV-Vis-IR Telescope (SUVIT), the EUV Spectroscopic Telescope (EUVST) and the High Resolution Coronal Imager (HCI), to jointly observe the entire visible <span class="hlt">solar</span> atmosphere with essentially the same high spatial resolution (0.1-0.3 arcsec), performing high resolution spectroscopic measurements over all atmospheric regions and spectro-polarimetric measurements from the photosphere through the upper chromosphere. In addition, <span class="hlt">Solar</span>-C will contribute to our understanding on the <span class="hlt">influence</span> of the Sun-Earth environments with synergetic wide-field observations from ground-based and other space missions. Some leading science objectives and the mission concept, including designs of the three instruments aboard <span class="hlt">SOLAR</span>-C will be presented.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2016AdSpR..58.2116A','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2016AdSpR..58.2116A"><span><span class="hlt">Influence</span> of geomagnetic <span class="hlt">activity</span> and atmospheric pressure on human arterial pressure during the <span class="hlt">solar</span> cycle 24</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Azcárate, T.; Mendoza, B.; Levi, J. R.</p> <p>2016-11-01</p> <p>We performed a study of the systolic (SBP) and diastolic (DBP) arterial blood pressure behavior under natural variables such as the atmospheric pressure (AtmP) and the horizontal geomagnetic field component (H). We worked with a sample of 304 healthy normotense volunteers, 152 men and 152 women, with ages between 18 and 84 years in Mexico City during the period 2008-2014, corresponding to the minimum, ascending and maximum phases of the <span class="hlt">solar</span> cycle 24. The data was divided by gender, age and day/night cycle. We studied the time series using three methods: Correlations, bivariate and superposed epochs (within a window of three days around the day of occurrence of a geomagnetic storm) analysis, between the SBP and DBP and the natural variables (AtmP and H). The correlation analysis indicated correlation between the SBP and DBP and AtmP and H, being the largest during the night. Furthermore, the correlation and bivariate analysis showed that the largest correlations are between the SBP and DBP and the AtmP. The superposed epoch analysis found that the largest number of significant SBP and DBP changes occurred for women. Finally, the blood pressure changes are larger during the <span class="hlt">solar</span> minimum and ascending <span class="hlt">solar</span> cycle phases than during the <span class="hlt">solar</span> maximum; the storms of the minimum were more intense than those of the maximum and this could be the reason of behavior of the blood pressure changes along the <span class="hlt">solar</span> cycle.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.osti.gov/biblio/5596810-guide-preparing-active-solar-heating-systems-operation-maintenance-manuals','SCIGOV-STC'); return false;" href="https://www.osti.gov/biblio/5596810-guide-preparing-active-solar-heating-systems-operation-maintenance-manuals"><span>Guide for preparing <span class="hlt">active</span> <span class="hlt">solar</span> heating systems operation and maintenance manuals</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>Not Available</p> <p>1991-01-01</p> <p>This book presents a systematic and standardized approach to the preparation of operation and maintenance manuals for <span class="hlt">active</span> <span class="hlt">solar</span> heating systems. Provides an industry consensus of the best operating and maintenance procedures for large commercial-scale <span class="hlt">solar</span> service water and space heating systems. A sample O M manual is included. 3-ring binder included.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/20070019764','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/20070019764"><span><span class="hlt">Solar</span> Systems</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p></p> <p>1979-01-01</p> <p>The <span class="hlt">solar</span> collectors shown are elements of domestic <span class="hlt">solar</span> hot water systems produced by <span class="hlt">Solar</span> One Ltd., Virginia Beach, Virginia. Design of these systems benefited from technical expertise provided <span class="hlt">Solar</span> One by NASA's Langley Research Center. The company obtained a NASA technical support package describing the d e sign and operation of <span class="hlt">solar</span> heating equipment in NASA's Tech House, a demonstration project in which aerospace and commercial building technology are combined in an energy- efficient home. <span class="hlt">Solar</span> One received further assistance through personal contact with Langley <span class="hlt">solar</span> experts. The company reports that the technical information provided by NASA <span class="hlt">influenced</span> <span class="hlt">Solar</span> One's panel design, its selection of a long-life panel coating which increases <span class="hlt">solar</span> collection efficiency, and the method adopted for protecting <span class="hlt">solar</span> collectors from freezing conditions.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2010AGUFMNH13A1139D','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2010AGUFMNH13A1139D"><span><span class="hlt">Solar</span>-terrestrial effect controls seismic <span class="hlt">activity</span> to a large extent (Invited)</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Duma, G.</p> <p>2010-12-01</p> <p>Several observational results and corresponding publications in the 20 century indicate that earthquakes in many regions happen systematically in dependence on the time of day and on the season as well. In the recent decade, studies on this topic have also been intensively performed at the Central Institute for Meteorology and Geodynamics (ZAMG), Vienna. Any natural effect on Earth which systematically appears at certain hours of the day or at a special season can solely be caused by a <span class="hlt">solar</span> or lunar <span class="hlt">influence</span>. And actually, statistic results on seismic <span class="hlt">activity</span> reveal a correlation with the <span class="hlt">solar</span> cycles. Examples of this seismic performance are shown. To gain more clarity about these effects, the three-hour magnetic index Kp, which characterizes the magnetic field disturbances, mainly caused by the <span class="hlt">solar</span> particle radiation, the <span class="hlt">solar</span> wind, was correlated with the seismic energy released by earthquakes over decades. Kp is determined from magnetic records of 13 observatories worldwide and continuously published by ISGI, France. It is demonstrated that a highly significant correlation between the geomagnetic index Kp and the annual seismic energy release in regions at latitudes between 35 and 60° N exists. Three regions of continental size were investigated, using the USGS (PDE) earthquake catalogue data. In the period 1974-2009 the Kp cycle periods range between 9 and 12 years, somewhat different to the sunspot number cycles of 11 years. Seismicity follows the Kp cycles with high coincidence. A detailed analysis of this correlation for N-America reveals, that the sum of released energy by earthquakes per year changes by a factor up to 100 with Kp. It is shown that during years of high Kp there happen e.g. 1 event M7, 4 events M6 and 30 events M5 per year, instead of only 10 events M5 in years with lowest Kp. Almost the same relation appears in other regions of continental size, with the same significance. The seismicity in S-America clearly follows the Kp cycles</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/20090026490','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/20090026490"><span>Overview of the Temperature Response in the Mesosphere and Lower Thermosphere to <span class="hlt">Solar</span> <span class="hlt">Activity</span></span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Beig, Gufran; Scheer, Juergen; Mlynczak, Martin G.; Keckhut, Philippe</p> <p>2008-01-01</p> <p>The natural variability in the terrestrial mesosphere needs to be known to correctly quantify global change. The response of the thermal structure to <span class="hlt">solar</span> <span class="hlt">activity</span> variations is an important factor. Some of the earlier studies highly overestimated the mesospheric <span class="hlt">solar</span> response. Modeling of the mesospheric temperature response to <span class="hlt">solar</span> <span class="hlt">activity</span> has evolved in recent years, and measurement techniques as well as the amount of data have improved. Recent investigations revealed much smaller <span class="hlt">solar</span> signatures and in some case no significant <span class="hlt">solar</span> signal at all. However, not much effort has been made to synthesize the results available so far. This article presents an overview of the energy budget of the mesosphere and lower thermosphere (MLT) and an up-to-date status of <span class="hlt">solar</span> response in temperature structure based on recently available observational data. An objective evaluation of the data sets is attempted and important factors of uncertainty are discussed.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2006AGUFMSM31A0298L','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2006AGUFMSM31A0298L"><span>A Coupling Function Linking <span class="hlt">Solar</span> Wind /IMF Variations and Geomagnetic <span class="hlt">Activity</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Lyatsky, W.; Lyatskaya, S.; Tan, A.</p> <p>2006-12-01</p> <p>From a theoretical consideration we have obtained expressions for the coupling function linking <span class="hlt">solar</span> wind and IMF parameters to geomagnetic <span class="hlt">activity</span>. While deriving these expressions, we took into account (1) a scaling factor due to polar cap expansion while increasing a reconnected magnetic flux in the dayside magnetosphere, and (2) a modified Akasofu function for the reconnected flux for combined IMF Bz and By components. The resulting coupling function may be written as Fa = aVsw B^1/2 sina (q/2), where Vsw is the <span class="hlt">solar</span> wind speed, B^ is the magnitude of the IMF vector in the Y-Z plane, q is the clock angle between the Z axis and IMF vector in the Y-Z plane, a is a coefficient, and the exponent, a, is derived from the experimental data and equals approximately to 2. The Fa function differs primary by the power of B^ from coupling functions proposed earlier. For testing the obtained coupling function, we used <span class="hlt">solar</span> wind and interplanetary magnetic field data for four years for maximum and minimum <span class="hlt">solar</span> <span class="hlt">activity</span>. We computed 2-D contour plots for correlation coefficients for the dependence of geomagnetic <span class="hlt">activity</span> indices on <span class="hlt">solar</span> wind parameters for different coupling functions. The obtained diagrams showed a good correspondence to the theoretic coupling function Fa for a »2. The maximum correlation coefficient for the dependence of the polar cap PC index on the Fa coupling function is significantly higher than that computed for other coupling functions used researchers, for the same time intervals.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/1992stct.symp.....C','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/1992stct.symp.....C"><span>An overview of current <span class="hlt">activities</span> at the National <span class="hlt">Solar</span> Thermal Test Facility</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Cameron, C. P.; Klimas, P. C.</p> <p></p> <p>This paper is a description of the United States Department of Energy's National <span class="hlt">Solar</span> Thermal Test Facility, highlighting current test programs. In the central receiver area, research underway supports commercialization of molten nitrate salt technology, including receivers, thermal energy transport, and corrosion experiments. Concentrator research includes large-area, glass-metal heliostats and stretched-membrane heliostats and dishes. Test <span class="hlt">activities</span> in support of dish-Stirling systems with reflux receivers are described. Research on parabolic troughs includes characterization of several receiver configurations. Other test facility <span class="hlt">activities</span> include <span class="hlt">solar</span> detoxification experiments, design assistance testing of commercially-available <span class="hlt">solar</span> hardware, and non-DOE-funded work, including thermal exposure tests and testing of volumetric and PV central receiver concepts.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2018HMT....54..593A','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2018HMT....54..593A"><span>Different parameter and technique affecting the rate of evaporation on <span class="hlt">active</span> <span class="hlt">solar</span> still -a review</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>A, Muthu Manokar; D, Prince Winston; A. E, Kabeel; Sathyamurthy, Ravishankar; T, Arunkumar</p> <p>2018-03-01</p> <p>Water is one of the essential sources for the endurance of human on the earth. As earth having only a small amount of water resources for consumption purpose people in rural and urban areas are getting affected by consuming dirty water that leads to water-borne diseases. Even though ground water is available in small quantity, it has to be treated properly before its use for internal consumption. Brackish water contains dissolve and undissolved contents, and hence it is not suitable for the household purpose. Nowadays, distillation process is done by using passive and <span class="hlt">active</span> <span class="hlt">solar</span> stills. The major problem in using passive <span class="hlt">solar</span> still is meeting higher demand for fresh water. The fresh water production from passive <span class="hlt">solar</span> still is critically low to meet the demand. To improve the productivity of conventional <span class="hlt">solar</span> still, input feed water is preheated by integrating the <span class="hlt">solar</span> still to different collector panels. In this review article, the different parameters that affect the rate of evaporation in an <span class="hlt">active</span> <span class="hlt">solar</span> still and the different methods incorporated has been presented. In addition to <span class="hlt">active</span> distillation system, forced convection technique can be incorporated to increase the yield of fresh water by decreasing the temperature of cover. Furthermore, it is identified that the yield of fresh water from the <span class="hlt">active</span> desalination system can be improved by sensible and latent heat energy storage. This review will motivate the researchers to decide appropriate <span class="hlt">active</span> <span class="hlt">solar</span> still technology for promoting development.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2005AGUFMPP21A1544T','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2005AGUFMPP21A1544T"><span>Evidence for a possible modern and mid-Holocene <span class="hlt">solar</span> <span class="hlt">influence</span> on climate from Lake Titicaca, South America</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Theissen, K. M.; Dunbar, R. B.</p> <p>2005-12-01</p> <p>In tropical regions, there are few paleoclimate archives with the necessary resolution to investigate climate variability at interannual-to-decadal timescales prior to the onset of the instrumental record. Interannual variability associated with the El Niño Southern Oscillation (ENSO) is well documented in the instrumental record and the importance of the precessional forcing of millennial variability has been established in studies of tropical paleoclimate records. In contrast, decade-to-century variability is still poorly understood. Here, we examine interannual to decadal variability in the northern Altiplano of South America using digital image analysis of a floating interval of varved sediments of middle Holocene age (~6160-6310 yr BP) from Lake Titicaca. Multi-taper method (MTM) and wavelet frequency-domain analyses were performed on a time series generated from a gray-scaled digital image of the mm-thick laminations. Our results indicate significant power at a decadal periodicity (10-12 years) associated with the Schwabe cycle of <span class="hlt">solar</span> <span class="hlt">activity</span>. Frequency-domain analysis also indicates power at 2-2.5 year periodicities associated with ENSO. Similarly, spectral analysis of a 75 year instrumental record of Titicaca lake level shows significant power at both <span class="hlt">solar</span> and ENSO periodicities. Although both of the examined records are short, our results imply that during both the mid-Holocene and modern times, <span class="hlt">solar</span> and ENSO variability may have contributed to high frequency climate fluctuations over the northern Altiplano. We suspect that <span class="hlt">solar</span> <span class="hlt">influence</span> on large-scale atmospheric circulation features may account for the decadal variability in the mid-Holocene and present-day water balance of the Altiplano.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://ntrs.nasa.gov/search.jsp?R=19910045711&hterms=dynamo&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D60%26Ntt%3Ddynamo','NASA-TRS'); return false;" href="https://ntrs.nasa.gov/search.jsp?R=19910045711&hterms=dynamo&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D60%26Ntt%3Ddynamo"><span>Dynamo-based scheme for forecasting the magnitude of <span class="hlt">solar</span> <span class="hlt">activity</span> cycles</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Layden, A. C.; Fox, P. A.; Howard, J. M.; Sarajedini, A.; Schatten, K. H.</p> <p>1991-01-01</p> <p>This paper presents a general framework for forecasting the smoothed maximum level of <span class="hlt">solar</span> <span class="hlt">activity</span> in a given cycle, based on a simple understanding of the <span class="hlt">solar</span> dynamo. This type of forecasting requires knowledge of the sun's polar magnetic field strength at the preceding <span class="hlt">activity</span> minimum. Because direct measurements of this quantity are difficult to obtain, the quality of a number of proxy indicators already used by other authors is evaluated, which are physically related to the sun's polar field. These indicators are subjected to a rigorous statistical analysis, and the analysis technique for each indicator is specified in detail in order to simplify and systematize reanalysis for future use. It is found that several of these proxies are in fact poorly correlated or uncorrelated with <span class="hlt">solar</span> <span class="hlt">activity</span>, and thus are of little value for predicting <span class="hlt">activity</span> maxima. Also presented is a scheme in which the predictions of the individual proxies are combined via an appropriately weighted mean to produce a compound prediction. The scheme is then applied to the current cycle 22, and a maximum smoothed international sunspot number of 171 + or - 26 is estimated.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2010EGUGA..1211532P','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2010EGUGA..1211532P"><span>10Be in ice at high resolution: <span class="hlt">Solar</span> <span class="hlt">activity</span> and climate signals observed and GCM-modeled in Law Dome ice cores</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Pedro, Joel; Heikkilä, Ulla; van Ommen, T. D.; Smith, A. M.</p> <p>2010-05-01</p> <p>Changes in <span class="hlt">solar</span> <span class="hlt">activity</span> modulate the galactic cosmic ray flux, and in turn, the production rate of 10Be in the earth's atmosphere. The best archives of past changes in 10Be production rate are the polar ice cores. Key challenges in interpreting these archives as proxies for past <span class="hlt">solar</span> <span class="hlt">activity</span> lie in separating the useful <span class="hlt">solar</span> <span class="hlt">activity</span> (or production) signal from the interfering meteorological (or climate) signal, and furthermore, in determining the atmospheric source regions of 10Be deposited to the ice core site. In this study we use a new monthly resolution composite 10Be record, which spans the past decade, and a general circulation model (ECHAM5-HAM), to constrain both the production and climate signals in 10Be concentrations at the Law Dome ice core site, East Antarctica. This study differs from most previous work on 10Be in Antarctica due to the very high sample resolution achieved. This high resolution, through a time period where accurate instrumental measurements of <span class="hlt">solar</span> <span class="hlt">activity</span> and climate are available, allows us to examine the response of 10Be concentrations in ice to short-term (monthly to annual) variations in <span class="hlt">solar</span> <span class="hlt">activity</span>, and to short-term variations in climate, including seasonality. We find a significant correlation (r2 = 0.56, P < 0.005, n = 92) between observed 10Be concentrations and <span class="hlt">solar</span> <span class="hlt">activity</span> (represented by the neutron counting rate). The most pervasive climate <span class="hlt">influence</span> is a seasonal cycle, which shows maximum concentrations in mid-to-late-summer and minimum concentrations in winter. Model results show reasonable agreement with observations; both a <span class="hlt">solar</span> <span class="hlt">activity</span> signal and seasonal cycle in 10Be are captured. However, the modeled snow accumulation rate is too high by approximately 60%. According to the model, the main atmospheric source region of 10Be deposited to Law Dome is the 30-90°S stratosphere (~50%), followed by the 30-90°S troposphere (~30%). An enhancement in the fraction of 10Be arriving to Law Dome from the</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2014cosp...40E.159A','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2014cosp...40E.159A"><span>Reaction of physiological factors on the <span class="hlt">solar</span>-geomagnetic <span class="hlt">activity</span> (the physical mechanisms)</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Avakyan, Sergey; Voronin, Nikolai; Dubarenko, Konstantin</p> <p></p> <p>This presentation proposes and provides substantiation for a hypothesis concerning the mechanism by which <span class="hlt">solar</span> and geomagnetic <span class="hlt">activity</span> (mainly of <span class="hlt">solar</span> flares and magnetic storms) affects the biosphere, including man. The hypothesis, including a physical mechanism introduced by the authors, is that high-lying (Rydberg) states of all gases of the earth’s upper atmosphere are excited by ionospheric energetic electrons. Rydberg atoms, molecules and ions of all atmospheric gases emit characteristic radio emission in the spectral range from decimeters to millimeters. This radiation can easily penetrate to low atmosphere and biosphere carrying complete information about power and duration of <span class="hlt">solar</span> flare and geomagnetic storms to biosphere. The microwave radioemission have the resonances at the spectral range 109 ÷ 1012 Hz at the cells and membranes, DNA and RNA, molecules of haemoglobin, erythrocytes, and this fact can explain the extremely small threshold for <span class="hlt">influence</span> of ionospheric radioemission at the monochromatic (characteristic) transitions on biological objects, including the viscosity of blood. The energy estimates of the flux intensity of microwave radiation of the ionosphere from Rydberg states are used to prove for the first time that the values of this flux agree with the experimental data. A method is proposed for distinguishing the contributions of microwave radiation and magnetic perturbation in the geo-biocorrelations, taking into account the effect that the magnetic-field variations are not in phase with the flux of corpuscles from the radiation belts in the ionosphere during the period of a geomagnetic storm. Quanta of microwave radiation are emitted from the heights of 90 - 360 km, i.e. in the basic ionosphere regions. Their energy by almost 10 orders of magnitude exceeds that of the quanta of low-frequency electromagnetic background of the ionosphere (with the frequencies lower than 100 Hz, which coincide with those of biorhythms). Thereby</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2016JGRA..121.7245T','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2016JGRA..121.7245T"><span>The response of the temperature of cold-point mesopause to <span class="hlt">solar</span> <span class="hlt">activity</span> based on SABER data set</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Tang, Chaoli; Liu, Dong; Wei, Heli; Wang, Yingjian; Dai, Congming; Wu, Pengfei; Zhu, Wenyue; Rao, Ruizhong</p> <p>2016-07-01</p> <p>The thermal structure and energy balance of upper atmosphere are dominated by <span class="hlt">solar</span> <span class="hlt">activity</span>. The response of cold-point mesopause (CPM) to <span class="hlt">solar</span> <span class="hlt">activity</span> is an important form. This article presents the response of the temperature of CPM (T-CPM) to <span class="hlt">solar</span> <span class="hlt">activity</span> using 14 year Sounding of the Atmosphere using Broadband Emission Radiometry data series over 80°S-80°N regions. These regions are divided into 16 latitude zones with 10° interval, and the spatial areas of 80°S-80°N, 180°W-180°E are divided into 96 lattices with 10°(latitude) × 60°(longitude) grid. The annual-mean values of T-CPM and F10.7 are calculated. The least squares regression method and correlation analysis are applied to these annual-mean series. First, the results show that the global T-CPM is significantly correlated to <span class="hlt">solar</span> <span class="hlt">activity</span> at the 0.05 level of significance with correlation coefficient of 0.90. The global <span class="hlt">solar</span> response of T-CPM is 4.89 ± 0.67 K/100 <span class="hlt">solar</span> flux unit. Then, for each latitude zone, the <span class="hlt">solar</span> response of T-CPM and its fluctuation are obtained. The <span class="hlt">solar</span> response of T-CPM becomes stronger with increasing latitude. The fluctuation ranges of <span class="hlt">solar</span> response at middle-latitude regions are smaller than those of the equator and high-latitude regions, and the global distribution takes on W shape. The corelationship analysis shows that the T-CPM is significantly correlated to <span class="hlt">solar</span> <span class="hlt">activity</span> at the 0.05 level of significance for each latitude zone. The correlation coefficients at middle-latitude regions are higher than those of the equator and high-latitude regions, and the global distribution takes on M shape. At last, for each grid cell, the response of T-CPM to <span class="hlt">solar</span> <span class="hlt">activity</span> and their correlation coefficient are presented.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2013SoPh..287..161R','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2013SoPh..287..161R"><span>Revisiting the <span class="hlt">Solar</span> Oblateness: Is Relevant Astrophysics Possible?</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Rozelot, J. P.; Fazel, Z.</p> <p>2013-10-01</p> <p>The measurement of <span class="hlt">solar</span> oblateness has a rich history extending well back into the past. Until recently, its estimate has been <span class="hlt">actively</span> disputed, as has its temporal dependence. Recent accurate observations of the <span class="hlt">solar</span> shape gave cause for doubt, and so far only balloon flights or satellite experiments, such as those onboard SDO, seem to achieve the required sensitivity to measure the expected small deviations from sphericity. A shrinking or an expanding shape is ultimately linked to <span class="hlt">solar</span> <span class="hlt">activity</span> (likely not homologously with its change), as gravitational or magnetic fields, which are existing mechanisms for storing energy during a <span class="hlt">solar</span> cycle, lead to distinct perturbations in the equilibrium <span class="hlt">solar</span>-structure and changes in the diameter. It follows that a sensitive determination of the <span class="hlt">solar</span> radius fluctuations might give information about the origin of the <span class="hlt">solar</span> cycle. In periods of higher <span class="hlt">activity</span>, the outer photospheric shape seems to become aspheric under the <span class="hlt">influence</span> of higher-order multipole moments of the Sun, resulting both from the centrifugal force and the core rotation. An accurate determination of the shape of the Sun is thus one of the ways that we have now for peering into its interior, learning empirically about flows and motions there that would otherwise only be guessed at from theoretical considerations, developing more precise inferences, and ultimately building possible alternative gravitational theories.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2015JGRA..12010640L','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2015JGRA..12010640L"><span>Semiannual and <span class="hlt">solar</span> <span class="hlt">activity</span> variations of daytime plasma observed by DEMETER in the ionosphere-plasmasphere transition region</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Li, L. Y.; Cao, J. B.; Yang, J. Y.; Berthelier, J. J.; Lebreton, J.-P.</p> <p>2015-12-01</p> <p>Using the plasma data of Detection of Electro-Magnetic Emissions Transmitted from Earthquake Regions (DEMETER) satellite and the NRLMSISE-00 atmospheric model, we examined the semiannual and <span class="hlt">solar</span> <span class="hlt">activity</span> variations of the daytime plasma and neutral composition densities in the ionosphere-plasmasphere transition region (~670-710 km). The results demonstrate that the semiannually latitudinal variation of the daytime oxygen ions (O+) is basically controlled by that of neutral atomic oxygen (O), whereas the latitude distributions of the helium and hydrogen ions (He+ and H+) do not fully depend on the neutral atomic helium (He) and hydrogen (H). The summer enhancement of the heavy oxygen ions is consistent with the neutral O enhancement in the summer hemisphere, and the oxygen ion density has significantly the summer-dense and winter-tenuous hemispheric asymmetry with respect to the dip equator. Although the winter enhancements of the lighter He+ and H+ ions are also associated with the neutral He and H enhancements in the winter hemisphere, the high-density light ions (He+ and H+) and electrons (e-) mainly appear at the low and middle magnetic latitudes (|λ| < 50°). The equatorial accumulations of the light plasma species indicate that the light charged particles (He+, H+, and e-) are easily transported by some equatorward forces (e.g., the magnetic mirror force and centrifugal force). The frequent Coulomb collisions between the charged particles probably lead to the particle trappings at different latitudes. Moreover, the neutral composition densities also <span class="hlt">influence</span> their ion concentrations during different <span class="hlt">solar</span> <span class="hlt">activities</span>. From the low-F10.7 year (2007-2008) to the high-F10.7 year (2004-2005), the daytime oxygen ions and electrons increase with the increasing neutral atomic oxygen, whereas the daytime hydrogen ions tend to decrease with the decreasing neutral atomic hydrogen. The helium ion density has no obvious <span class="hlt">solar</span> <span class="hlt">activity</span> variation, suggesting that the</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017EGUGA..19.3512L','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017EGUGA..19.3512L"><span>Is <span class="hlt">solar</span> correction for long-term trend studies stable?</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Laštovička, Jan</p> <p>2017-04-01</p> <p>When calculating long-term trends in the ionosphere, the effect of the 11-year <span class="hlt">solar</span> cycle (i.e. of <span class="hlt">solar</span> <span class="hlt">activity</span>) must be removed from data, because it is much stronger than the long-term trend. When a data series is analyzed for trend, usual approach is first to calculate from all data their dependence on <span class="hlt">solar</span> <span class="hlt">activity</span> and create an observational model of dependence on <span class="hlt">solar</span> <span class="hlt">activity</span>. Then the model data are subtracted from observations and trend is computed from residuals. This means that it is assumed that the <span class="hlt">solar</span> <span class="hlt">activity</span> dependence is stable over the whole data series period of time. But what happens if it is not the case? As an ionospheric parameter we consider foE from two European stations with the best long data series of parameters of the ionospheric E layer, Slough/Chilton and Juliusruh over 1975-2014 (40 years). Noon-time medians (10-14 LT) are analyzed. The trend pattern after removing <span class="hlt">solar</span> <span class="hlt">influence</span> with one correction for the whole period is complex. For yearly average values for both stations first foE is slightly decreasing in 1975-1990, then the trend levels off or a very little increase occurs in 1990-2005, and finally in 2006-2014 a remarkable decrease is observed. This does not seem to be physically plausible. However, when the <span class="hlt">solar</span> correction is calculated separately for the three above periods, we obtain a smooth slightly negative trend which changes after the mid-1990 into no trend in coincidence with change of ozone trend. While <span class="hlt">solar</span> corrections for the first two periods are similar (even though not equal), the <span class="hlt">solar</span> <span class="hlt">activity</span> dependence of foE in the third period (lower <span class="hlt">solar</span> <span class="hlt">activity</span>) is clearly different. Also foF2 trend revealed some effect of unstable <span class="hlt">solar</span> correction. Thus the stability of <span class="hlt">solar</span> correction should be carefully tested when calculating ionospheric trends. This could perhaps explain some of differences between the past published trend results.</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('http://hdl.handle.net/2060/19760017036','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/19760017036"><span>The 3-D <span class="hlt">solar</span> radioastronomy and the structure of the corona and the <span class="hlt">solar</span> wind. [<span class="hlt">solar</span> probes of <span class="hlt">solar</span> <span class="hlt">activity</span></span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Steinberg, J. L.; Caroubalos, C.</p> <p>1976-01-01</p> <p>The mechanism causing <span class="hlt">solar</span> radio bursts (1 and 111) is examined. It is proposed that a nonthermal energy source is responsible for the bursts; nonthermal energy is converted into electromagnetic energy. The advantages are examined for an out-of-the-ecliptic <span class="hlt">solar</span> probe mission, which is proposed as a means of stereoscopically viewing <span class="hlt">solar</span> radio bursts, <span class="hlt">solar</span> magnetic fields, coronal structure, and the <span class="hlt">solar</span> wind.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017IJMPC..2850075O','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017IJMPC..2850075O"><span>High <span class="hlt">solar</span> <span class="hlt">activity</span> predictions through an artificial neural network</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Orozco-Del-Castillo, M. G.; Ortiz-Alemán, J. C.; Couder-Castañeda, C.; Hernández-Gómez, J. J.; Solís-Santomé, A.</p> <p></p> <p>The effects of high-energy particles coming from the Sun on human health as well as in the integrity of outer space electronics make the prediction of periods of high <span class="hlt">solar</span> <span class="hlt">activity</span> (HSA) a task of significant importance. Since periodicities in <span class="hlt">solar</span> indexes have been identified, long-term predictions can be achieved. In this paper, we present a method based on an artificial neural network to find a pattern in some harmonics which represent such periodicities. We used data from 1973 to 2010 to train the neural network, and different historical data for its validation. We also used the neural network along with a statistical analysis of its performance with known data to predict periods of HSA with different confidence intervals according to the three-sigma rule associated with <span class="hlt">solar</span> cycles 24-26, which we found to occur before 2040.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.osti.gov/biblio/21300733-new-observation-failed-filament-eruptions-influence-asymmetric-coronal-background-fields-solar-eruptions','SCIGOV-STC'); return false;" href="https://www.osti.gov/biblio/21300733-new-observation-failed-filament-eruptions-influence-asymmetric-coronal-background-fields-solar-eruptions"><span>NEW OBSERVATION OF FAILED FILAMENT ERUPTIONS: THE <span class="hlt">INFLUENCE</span> OF ASYMMETRIC CORONAL BACKGROUND FIELDS ON <span class="hlt">SOLAR</span> ERUPTIONS</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>Liu, Y.; Xu, Z.; Su, J.</p> <p>2009-05-01</p> <p>Failed filament eruptions not associated with a coronal mass ejection (CME) have been observed and reported as evidence for <span class="hlt">solar</span> coronal field confinement on erupting flux ropes. In those events, each filament eventually returns to its origin on the <span class="hlt">solar</span> surface. In this Letter, a new observation of two failed filament eruptions is reported which indicates that the mass of a confined filament can be ejected to places far from the original filament channel. The jetlike mass motions in the two failed filament eruptions are thought to be due to the asymmetry of the background coronal magnetic fields with respectmore » to the locations of the filament channels. The asymmetry of the coronal fields is confirmed by an extrapolation based on a potential field model. The obvious imbalance between the positive and negative magnetic flux (with a ratio of 1:3) in the bipolar <span class="hlt">active</span> region is thought to be the direct cause of the formation of the asymmetric coronal fields. We think that the asymmetry of the background fields can not only <span class="hlt">influence</span> the trajectories of ejecta, but also provide a relatively stronger confinement for flux rope eruptions than the symmetric background fields do.« less</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2014IAUS..300..235P','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2014IAUS..300..235P"><span>A <span class="hlt">solar</span> tornado caused by flares</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Panesar, N. K.; Innes, D. E.; Tiwari, S. K.; Low, B. C.</p> <p>2014-01-01</p> <p>An enormous <span class="hlt">solar</span> tornado was observed by SDO/AIA on 25 September 2011. It was mainly associated with a quiescent prominence with an overlying coronal cavity. We investigate the triggering mechanism of the <span class="hlt">solar</span> tornado by using the data from two instruments: SDO/AIA and STEREO-A/EUVI, covering the Sun from two directions. The tornado appeared near to the <span class="hlt">active</span> region NOAA 11303 that produced three flares. The flares directly <span class="hlt">influenced</span> the prominence-cavity system. The release of free magnetic energy from the <span class="hlt">active</span> region by flares resulted in the contraction of the <span class="hlt">active</span> region field. The cavity, owing to its superior magnetic pressure, expanded to fill this vacated space in the corona. We propose that the tornado developed on the top of the prominence due to the expansion of the prominence-cavity system.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2003EAEJA.....3510S','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2003EAEJA.....3510S"><span>QBO of temperature in mesopause and lower thermosphere caused by <span class="hlt">solar</span> <span class="hlt">activity</span> variations</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Shefov, N. N.; Semenov, A. I.</p> <p>2003-04-01</p> <p>On the basis of the data of the emission (hydroxyl, sodium and atomic oxygen 557.7 nm) and radiophysical (87-107 km) measurements some regularities of quasi-biennial oscillation (QBO) of the atmospheric temperature at heights of the mesopause and lower thermosphere are investigated. It is shown, that they are closely connected with quasi-biennial variations of <span class="hlt">solar</span> <span class="hlt">activity</span> and form within the limits of a cycle of <span class="hlt">solar</span> <span class="hlt">activity</span> the fading wave train of oscillations. Such behaviour of the wave train can be adequately described by the Airy function. As a result of the analysis of characteristics of QBO of <span class="hlt">solar</span> <span class="hlt">activity</span> during 17-23rd cycles it is shown, that to each 11-years cycle correspond its wave train of QBO. Amplitudes and periods of this wave train decrease during a cycle, i.e. it represents Not harmonious oscillation but it is a cyclic aperiodic oscillation (CAO). Therefore usual methods of Fourier analysis used earlier did not result in the same values of the period. The wave train of the current cycle begins at the end of previous and some time together with the subsequent cycle proceeds. Thus, the time sequence of <span class="hlt">activity</span> during <span class="hlt">solar</span> cycle represents superposition of three wave trains. Period of CAO in the beginning of a cycle has ~ 38 months and decreases to the end of a cycle up to ~ 21 months. The first wide negative minimum of Airy function describing of the wave train of CAO corresponds to <span class="hlt">solar</span> <span class="hlt">activity</span> minimum in the 11-year cycle. The time scale of the wave train varies from one cycle to another. Full duration of individual wave train is ~ 22 years. Owing to a mutual interference of the consecutive wave trains in the 11-year cycles the observable variations of <span class="hlt">solar</span> <span class="hlt">activity</span> are not identical. Structure of CAO obviously displays magnetohydrodynamic processes inside the Sun. This work was supported by the Grant No. 2274 of ISTC.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2018JASTP.171...94P','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2018JASTP.171...94P"><span>Tropospheric weather <span class="hlt">influenced</span> by <span class="hlt">solar</span> wind through atmospheric vertical coupling downward control</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Prikryl, Paul; Bruntz, Robert; Tsukijihara, Takumi; Iwao, Koki; Muldrew, Donald B.; Rušin, Vojto; Rybanský, Milan; Turňa, Maroš; Šťastný, Pavel</p> <p>2018-06-01</p> <p>Occurrence of severe weather in the context of <span class="hlt">solar</span> wind coupling to the magnetosphere-ionosphere-atmosphere (MIA) system is investigated. It is observed that significant snowfall, wind and heavy rain, particularly if caused by low pressure systems in winter, tend to follow arrivals of high-speed <span class="hlt">solar</span> wind. Previously published statistical evidence that explosive extratropical cyclones in the northern hemisphere tend to occur within a few days after arrivals of high-speed <span class="hlt">solar</span> wind streams from coronal holes (Prikryl et al., 2009, 2016) is corroborated for the southern hemisphere. Cases of severe weather events are examined in the context of the magnetosphere-ionosphere-atmosphere (MIA) coupling. Physical mechanism to explain these observations is proposed. The leading edge of high-speed <span class="hlt">solar</span> wind streams is a locus of large-amplitude magneto-hydrodynamic waves that modulate Joule heating and/or Lorentz forcing of the high-latitude lower thermosphere generating medium-scale atmospheric gravity waves that propagate upward and downward through the atmosphere. Simulations of gravity wave propagation in a model atmosphere using the Transfer Function Model (Mayr et al., 1990) reveal that propagating waves originating in the lower thermosphere can excite a spectrum of gravity waves in the lower atmosphere. In spite of significantly reduced amplitudes but subject to amplification upon reflection in the upper troposphere, these gravity waves can provide a lift of unstable air to release instabilities in the troposphere and initiate convection to form cloud/precipitation bands. It is primarily the energy provided by release of latent heat that leads to intensification of storms. These results indicate that vertical coupling in the atmosphere exerts downward control from <span class="hlt">solar</span> wind to the lower atmospheric levels <span class="hlt">influencing</span> tropospheric weather development.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2018Nanot..29y5201L','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2018Nanot..29y5201L"><span><span class="hlt">Influence</span> of hole transport material/metal contact interface on perovskite <span class="hlt">solar</span> cells</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Lei, Lei; Zhang, Shude; Yang, Songwang; Li, Xiaomin; Yu, Yu; Wei, Qingzhu; Ni, Zhichun; Li, Ming</p> <p>2018-06-01</p> <p>Interfaces have a significant impact on the performance of perovskite <span class="hlt">solar</span> cells. This work investigated the <span class="hlt">influence</span> of hole transport material/metal contact interface on photovoltaic behaviours of perovskite <span class="hlt">solar</span> devices. Different hole material/metal contact interfaces were obtained by depositing the metal under different conditions. High incident kinetic energy metal particles were proved to penetrate and embed into the hole transport material. These isolated metal particles in hole transport materials capture holes and increase the apparent carrier transport resistance of the hole transport layer. Sample temperature was found to be of great significance in metal deposition. Since metal vapour has a high temperature, the deposition process accumulated a large amount of heat. The heat evaporated the additives in the hole transport layer and decreased the hole conductivity. On the other hand, high temperature may cause iodization of the metal contact.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/29676282','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/29676282"><span><span class="hlt">Influence</span> of hole transport material/metal contact interface on perovskite <span class="hlt">solar</span> cells.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Lei, Lei; Zhang, Shude; Yang, Songwang; Li, Xiaomin; Yu, Yu; Wei, Qingzhu; Ni, Zhichun; Li, Ming</p> <p>2018-06-22</p> <p>Interfaces have a significant impact on the performance of perovskite <span class="hlt">solar</span> cells. This work investigated the <span class="hlt">influence</span> of hole transport material/metal contact interface on photovoltaic behaviours of perovskite <span class="hlt">solar</span> devices. Different hole material/metal contact interfaces were obtained by depositing the metal under different conditions. High incident kinetic energy metal particles were proved to penetrate and embed into the hole transport material. These isolated metal particles in hole transport materials capture holes and increase the apparent carrier transport resistance of the hole transport layer. Sample temperature was found to be of great significance in metal deposition. Since metal vapour has a high temperature, the deposition process accumulated a large amount of heat. The heat evaporated the additives in the hole transport layer and decreased the hole conductivity. On the other hand, high temperature may cause iodization of the metal contact.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/19780019594','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/19780019594"><span>Preliminary design <span class="hlt">activities</span> for <span class="hlt">solar</span> heating and cooling systems</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p></p> <p>1978-01-01</p> <p>Information on the development of <span class="hlt">solar</span> heating and cooling systems is presented. The major emphasis is placed on program organization, system size definition, site identification, system approaches, heat pump and equipment design, collector procurement, and other preliminary design <span class="hlt">activities</span>.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2013CEAB...37..417G','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2013CEAB...37..417G"><span>Variations of <span class="hlt">Solar</span> Non-axisymmetric <span class="hlt">Activity</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Gyenge, N.; Baranyi, T.; Ludmány, A.</p> <p></p> <p>The temporal behaviour of <span class="hlt">solar</span> <span class="hlt">active</span> longitudes has been examined by using two sunspot catalogues, the Greenwich Photoheliographic Results (GPR) and the Debrecen Photoheliographic Data (DPD). The time-longitude diagrams of the <span class="hlt">activity</span> distribution reveal the preferred longitudinal zones and their migration with respect to the Carrington frame. The migration paths outline a set of patterns in which the <span class="hlt">activity</span> zone has alternating prograde/retrograde angular velocities with respect to the Carrington rotation rate. The time profiles of these variations can be described by a set of successive parabolae. Two similar migration paths have been selected from these datasets, one northern path during cycles 21 - 22 and one southern path during cycles 13 - 14, for closer examination and comparison of their dynamical behaviours. The rates of sunspot emergence exhibited in both migration paths similar periodicities, close to 1.3 years. This behaviour may imply that the <span class="hlt">active</span> longitude is connected to the bottom of convection zone.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/19720005158','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/19720005158"><span><span class="hlt">Solar</span> <span class="hlt">activity</span> prediction</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Slutz, R. J.; Gray, T. B.; West, M. L.; Stewart, F. G.; Leftin, M.</p> <p>1971-01-01</p> <p>A statistical study of formulas for predicting the sunspot number several years in advance is reported. By using a data lineup with cycle maxima coinciding, and by using multiple and nonlinear predictors, a new formula which gives better error estimates than former formulas derived from the work of McNish and Lincoln is obtained. A statistical analysis is conducted to determine which of several mathematical expressions best describes the relationship between 10.7 cm <span class="hlt">solar</span> flux and Zurich sunspot numbers. Attention is given to the autocorrelation of the observations, and confidence intervals for the derived relationships are presented. The accuracy of predicting a value of 10.7 cm <span class="hlt">solar</span> flux from a predicted sunspot number is dicussed.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=3568686','PMC'); return false;" href="https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=3568686"><span>High-resolution analysis of upper Miocene lake deposits: Evidence for the <span class="hlt">influence</span> of Gleissberg-band <span class="hlt">solar</span> forcing</span></a></p> <p><a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pmc">PubMed Central</a></p> <p>Kern, Andrea K.; Harzhauser, Mathias; Soliman, Ali; Piller, Werner E.; Mandic, Oleg</p> <p>2013-01-01</p> <p>A high-resolution multi-proxy analysis was conducted on a 1.5-m-long core of Tortonian age (~ 10.5 Ma; Late Miocene) from Austria (Europe). The lake sediments were studied with a 1-cm resolution to detect all small-scale variations based on palynomorphs (pollen and dinoflagellate cysts), ostracod abundance, geochemistry (carbon and sulfur) and geophysics (magnetic susceptibility and natural gamma radiation). Based on an already established age model for a longer interval of the same core, this sequence can be limited to approx. two millennia of Late Miocene time with a resolution of ~ 13.7 years per sample. The previous study documented the presence of <span class="hlt">solar</span> forcing, which was verified within various proxies on this 1.5-m core by a combination of REDFIT spectra and Gaussian filters. Significant repetitive signals ranged in two discrete intervals corresponding roughly to 55–82 and 110–123 years, fitting well within the lower and upper Gleissberg cycle ranges. Based on these results, the environmental changes along the 2000-year Late Miocene sequence are discussed. No major ecological turnovers are expected in this very short interval. Nonetheless, even within this brief time span, dinoflagellates document rapid changes between oligotrophic and eutrophic conditions, which are frequently coupled with lake stratification and dysoxic bottom waters. These phases prevented ostracods and molluscs from settling and promoted the <span class="hlt">activity</span> of sulfur bacteria. The pollen record indicates rather stable wetland vegetation with a forested hinterland. Shifts in the pollen spectra can be mainly attributed to variations in transport mechanisms. These are represented by a few phases of fluvial input but mainly by changes in wind intensity and probably also wind direction. Such <span class="hlt">influence</span> is most likely caused by <span class="hlt">solar</span> cycles, leading to a change in source area for the input into the lake. Furthermore, these <span class="hlt">solar</span>-induced variations seem to be modulated by longer <span class="hlt">solar</span> cycles</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/19920018978','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/19920018978"><span>Future missions studies: Combining Schatten's <span class="hlt">solar</span> <span class="hlt">activity</span> prediction model with a chaotic prediction model</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Ashrafi, S.</p> <p>1991-01-01</p> <p>K. Schatten (1991) recently developed a method for combining his prediction model with our chaotic model. The philosophy behind this combined model and his method of combination is explained. Because the Schatten <span class="hlt">solar</span> prediction model (KS) uses a dynamo to mimic <span class="hlt">solar</span> dynamics, accurate prediction is limited to long-term <span class="hlt">solar</span> behavior (10 to 20 years). The Chaotic prediction model (SA) uses the recently developed techniques of nonlinear dynamics to predict <span class="hlt">solar</span> <span class="hlt">activity</span>. It can be used to predict <span class="hlt">activity</span> only up to the horizon. In theory, the chaotic prediction should be several orders of magnitude better than statistical predictions up to that horizon; beyond the horizon, chaotic predictions would theoretically be just as good as statistical predictions. Therefore, chaos theory puts a fundamental limit on predictability.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.osti.gov/biblio/22342192-periodic-analysis-solar-activity-its-link-arctic-oscillation-phenomenon','SCIGOV-STC'); return false;" href="https://www.osti.gov/biblio/22342192-periodic-analysis-solar-activity-its-link-arctic-oscillation-phenomenon"><span>Periodic analysis of <span class="hlt">solar</span> <span class="hlt">activity</span> and its link with the Arctic oscillation phenomenon</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>Qu, Weizheng; Li, Chun; Du, Ling</p> <p>2014-12-01</p> <p>Based on spectrum analysis, we provide the arithmetic expressions of the quasi 11 yr cycle, 110 yr century cycle of relative sunspot numbers, and quasi 22 yr cycle of <span class="hlt">solar</span> magnetic field polarity. Based on a comparative analysis of the monthly average geopotential height, geopotential height anomaly, and temperature anomaly of the northern hemisphere at locations with an air pressure of 500 HPa during the positive and negative phases of AO (Arctic Oscillation), one can see that the abnormal warming period in the Arctic region corresponds to the negative phase of AO, while the anomalous cold period corresponds to itsmore » positive phase. This shows that the abnormal change in the Arctic region is an important factor in determining the anomalies of AO. In accordance with the analysis performed using the successive filtering method, one can see that the AO phenomenon occurring in January shows a clear quasi 88 yr century cycle and quasi 22 yr decadal cycle, which are closely related to <span class="hlt">solar</span> <span class="hlt">activities</span>. The results of our comparative analysis show that there is a close inverse relationship between the <span class="hlt">solar</span> <span class="hlt">activities</span> (especially the <span class="hlt">solar</span> magnetic field index changes) and the changes in the 22 yr cycle of the AO occurring in January, and that the two trends are basically opposite of each other. That is to say, in most cases after the <span class="hlt">solar</span> magnetic index MI rises from the lowest value, the <span class="hlt">solar</span> magnetic field turns from north to south, and the high-energy particle flow entering the Earth's magnetosphere increases to heat the polar atmosphere, thus causing the AO to drop from the highest value; after the <span class="hlt">solar</span> magnetic index MI drops from the highest value, the <span class="hlt">solar</span> magnetic field turns from south to north, and the <span class="hlt">solar</span> high-energy particle flow passes through the top of the Earth's magnetosphere rather than entering it to heat the polar atmosphere. Thus the polar temperature drops, causing the AO to rise from the lowest value. In summary, the variance</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2002EGSGA..27.6576G','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2002EGSGA..27.6576G"><span>The Pechora River Runoff, Atmospheric Circulation and <span class="hlt">Solar</span> <span class="hlt">Activity</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Golovanov, O. F.</p> <p></p> <p>This study presents an attempt to define and estimate the factors effecting and possi- bly, determining the spatial-temporal characteristics of the Pechora River hydrological regime. The time-series of hydrometeorological observations (runoff, precipitation, air temperature) carried out within the basin of the impact object U the Pechora River U are close to secular and include the year of the century maximum of the <span class="hlt">solar</span> <span class="hlt">activ</span>- ity (1957). The joint statistical analysis of these characteristics averaged both for a year and for the low water periods in spring (V-VII), summer-autumn (VIII-IX) and winter (X-IV) demonstrated the majority of integral curves to have minimums coin- ciding or slightly differing from the <span class="hlt">solar</span> <span class="hlt">activity</span> maximum in 1957. It is especially typical for the spring high water runoff along the entire length of the Pechora River. Only the curves of the air temperature in the summer-autumn low water period are in the opposite phase relative to all other elements. In the upper Pechora the inte- gral curves of winter and annual precipitation are synchronous to the runoff curves. The multiyear variability of the Pechora runoff corresponds to that of the atmospheric circulation in the northern hemisphere. This is clearly illustrated by the decrease of the Pechora runoff and increase of the climate continentality in its basin, that is ac- companied with predominating of the meridional circulation, anticyclone invasion and precipitation decrease while the <span class="hlt">solar</span> <span class="hlt">activity</span> grows. This process takes place at the background of the prevailing mass transport of E+C type, increase of number of the elementary synoptic processes (ESP). The maximum number of ESP (observed in 1963) was recorded soon after the century maximum of the <span class="hlt">solar</span> <span class="hlt">activity</span>. This fact may be explained by the anticyclone circulation prevalence which results in growth of the climate continentality in the Pechora basin in this period. The enumerated in- flection points of the integral curves of</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/20070031866','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/20070031866"><span>Application of Semi <span class="hlt">Active</span> Control Techniques to the Damping Suppression Problem of <span class="hlt">Solar</span> Sail Booms</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Adetona, O.; Keel, L. H.; Whorton, M. S.</p> <p>2007-01-01</p> <p><span class="hlt">Solar</span> sails provide a propellant free form for space propulsion. These are large flat surfaces that generate thrust when they are impacted by light. When attached to a space vehicle, the thrust generated can propel the space vehicle to great distances at significant speeds. For optimal performance the sail must be kept from excessive vibration. <span class="hlt">Active</span> control techniques can provide the best performance. However, they require an external power-source that may create significant parasitic mass to the <span class="hlt">solar</span> sail. However, <span class="hlt">solar</span> sails require low mass for optimal performance. Secondly, <span class="hlt">active</span> control techniques typically require a good system model to ensure stability and performance. However, the accuracy of <span class="hlt">solar</span> sail models validated on earth for a space environment is questionable. An alternative approach is passive vibration techniques. These do not require an external power supply, and do not destabilize the system. A third alternative is referred to as semi-<span class="hlt">active</span> control. This approach tries to get the best of both <span class="hlt">active</span> and passive control, while avoiding their pitfalls. In semi-<span class="hlt">active</span> control, an <span class="hlt">active</span> control law is designed for the system, and passive control techniques are used to implement it. As a result, no external power supply is needed so the system is not destabilize-able. Though it typically underperforms <span class="hlt">active</span> control techniques, it has been shown to out-perform passive control approaches and can be unobtrusively installed on a <span class="hlt">solar</span> sail boom. Motivated by this, the objective of this research is to study the suitability of a Piezoelectric (PZT) patch actuator/sensor based semi-<span class="hlt">active</span> control system for the vibration suppression problem of <span class="hlt">solar</span> sail booms. Accordingly, we develop a suitable mathematical and computer model for such studies and demonstrate the capabilities of the proposed approach with computer simulations.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://ntrs.nasa.gov/search.jsp?R=19790017442&hterms=Electricity&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D40%26Ntt%3DElectricity','NASA-TRS'); return false;" href="https://ntrs.nasa.gov/search.jsp?R=19790017442&hterms=Electricity&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D40%26Ntt%3DElectricity"><span><span class="hlt">Solar</span>-terrestrial coupling through atmospheric electricity</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Roble, R. G.; Hays, P. B.</p> <p>1979-01-01</p> <p>There are a number of measurements of electrical variations that suggest a <span class="hlt">solar</span>-terrestrial <span class="hlt">influence</span> on the global atmospheric electrical circuit. The measurements show variations associated with <span class="hlt">solar</span> flares, <span class="hlt">solar</span> magnetic sector boundary crossings, geomagnetic <span class="hlt">activity</span>, aurorae, differences between ground current and potential gradients at high and low latitudes, and <span class="hlt">solar</span> cycle variations. The evidence for each variation is examined. Both the experimental evidence and the calculations made with a global model of atmospheric electricity indicate that there is <span class="hlt">solar</span>-terrestrial coupling through atmospheric electricity which operates by altering the global electric current and field distribution. A global redistribution of currents and fields can be caused by large-scale changes in electrical conductivity, by alteration of the columnar resistance between thunderstorm cloud tops and the ionosphere, or by both. If the columnar resistance is altered above thunderstorms, more current will flow in the global circuit, changing the ionospheric potential and basic circuit variables such as current density and electric fields. The observed variations of currents and fields during <span class="hlt">solar</span>-induced disturbances are generally less than 50% of mean values near the earth's surface.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2005AGUFM.A33A0873B','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2005AGUFM.A33A0873B"><span>A Novel Analysis Of The Connection Between Indian Monsoon Rainfall And <span class="hlt">Solar</span> <span class="hlt">Activity</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Bhattacharyya, S.; Narasimha, R.</p> <p>2005-12-01</p> <p>The existence of possible correlations between the <span class="hlt">solar</span> cycle period as extracted from the yearly means of sunspot numbers and any periodicities that may be present in the Indian monsoon rainfall has been addressed using wavelet analysis. The wavelet transform coefficient maps of sunspot-number time series and those of the homogeneous Indian monsoon rainfall annual time series data reveal striking similarities, especially around the 11-year period. A novel method to analyse and quantify this similarity devising statistical schemes is suggested in this paper. The wavelet transform coefficient maxima at the 11-year period for the sunspot numbers and the monsoon rainfall have each been modelled as a point process in time and a statistical scheme for identifying a trend or dependence between the two processes has been devised. A regression analysis of parameters in these processes reveals a nearly linear trend with small but systematic deviations from the regressed line. Suitable function models for these deviations have been obtained through an unconstrained error minimisation scheme. These models provide an excellent fit to the time series of the given wavelet transform coefficient maxima obtained from actual data. Statistical significance tests on these deviations suggest with 99% confidence that the deviations are sample fluctuations obtained from normal distributions. In fact our earlier studies (see, Bhattacharyya and Narasimha, 2005, Geophys. Res. Lett., Vol. 32, No. 5) revealed that average rainfall is higher during periods of greater <span class="hlt">solar</span> <span class="hlt">activity</span> for all cases, at confidence levels varying from 75% to 99%, being 95% or greater in 3 out of 7 of them. Analysis using standard wavelet techniques reveals higher power in the 8--16 y band during the higher <span class="hlt">solar</span> <span class="hlt">activity</span> period, in 6 of the 7 rainfall time series, at confidence levels exceeding 99.99%. Furthermore, a comparison between the wavelet cross spectra of <span class="hlt">solar</span> <span class="hlt">activity</span> with rainfall and noise (including</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2008AGUFM.B21C0384V','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2008AGUFM.B21C0384V"><span><span class="hlt">Solar</span> <span class="hlt">Activity</span>, Ultraviolet Radiation and Consequences in Birds in Mexico City, 2001- 2002</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Valdes, M.; Velasco, V.</p> <p>2008-12-01</p> <p>Anomalous behavior in commercial and pet birds in Mexico City was reported during 2002 by veterinarians at the Universidad Nacional Autonoma de Mexico. This was attributed to variations in the surrounding luminosity. The <span class="hlt">solar</span> components, direct, diffuse, global, ultraviolet band A and B, as well as some meteorological parameters, temperature, relative humidity, and precipitation, were then analyzed at the <span class="hlt">Solar</span> Radiation Laboratory. Although the total annual radiance of the previously mentioned radiation components did not show important changes, ultraviolet Band-B <span class="hlt">solar</span> radiation did vary significantly. During 2001 the total annual irradiance , 61.05 Hjcm² to 58.32 Hjcm², was 1.6 standard deviations lower than one year later, in 2002 and increased above the mean total annual irradiance, to 65.75 Hjcm², 2.04 standard deviations, giving a total of 3.73 standard deviations for 2001-2002. Since these differences did not show up clearly in the other <span class="hlt">solar</span> radiation components, daily extra-atmosphere irradiance was analyzed and used to calculate the total annual extra-atmosphere irradiance, which showed a descent for 2001. Our conclusions imply that Ultraviolet Band-B <span class="hlt">solar</span> radiation is representative of <span class="hlt">solar</span> <span class="hlt">activity</span> and has an important impact on commercial <span class="hlt">activity</span> related with birds.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2016AGUFMSM33C2518C','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2016AGUFMSM33C2518C"><span><span class="hlt">Solar</span> Cycle and Geomagnetic <span class="hlt">Activity</span> Variation of Topside Ionospheric Upflow as Measured by DMSP</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Coley, W. R.; Hairston, M. R.</p> <p>2016-12-01</p> <p>Under the proper conditions a considerable amount of plasma can escape the Earth's ionosphere into the magnetosphere. Indeed, there are indications that at least part of the time the ionosphere may be the dominant source of ions for the plasma sheet and near-Earth portion of the magnetosphere. The upward flux of thermal O+ from the lower part of the topside ionosphere <span class="hlt">actively</span> provides plasma into intermediate altitudes where they may be given escape energy by various mechanisms. Previous work has indicated that there is considerable time variation of upwelling low energy ionospheric plasma to these intermediate altitudes during moderate to high <span class="hlt">solar</span> <span class="hlt">activity</span>. Here we use the SSIES thermal plasma instruments on board the Defense Meteorological Satellite Program (DMSP) F13-F19 series of spacecraft to examine the vertical flux of thermal O+ from the deep <span class="hlt">solar</span> minimum of 2008-2009 to the moderately <span class="hlt">active</span> period of 2012-2015. Separately integrating the upward and downward fluxes over the high-latitude region (auroral zone and polar cap) allows the observation of the total upflow/downflow as a function of the current geomagnetic conditions, <span class="hlt">solar</span> cycle, and <span class="hlt">solar</span> wind conditions. In particular we investigate the incidence of high upward flux events as a function of <span class="hlt">solar</span> wind velocity and density during the deepest <span class="hlt">solar</span> minimum since the space age began.</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('http://hdl.handle.net/2060/19900003172','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/19900003172"><span>The onset of the <span class="hlt">solar</span> <span class="hlt">active</span> cycle 22</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Ahluwalia, H. S.</p> <p>1989-01-01</p> <p>There is a great deal of interest in being able to predict the main characteristics of a <span class="hlt">solar</span> <span class="hlt">activity</span> cycle (SAC). One would like to know, for instance, how large the amplitude (R sub m) of a cycle is likely to be, i.e., the annual mean of the sunspot numbers at the maximum of SAC. Also, how long a cycle is likely to last, i.e., its period. It would also be interesting to be able to predict the details, like how steep the ascending phase of a cycle is likely to be. Questions like these are of practical importance to NASA in planning the launch schedule for the low altitude, expensive spacecrafts like the Hubble Space Telescope, the Space Station, etc. Also, one has to choose a proper orbit, so that once launched the threat of an atmospheric drag on the spacecraft is properly taken into account. Cosmic ray data seem to indicate that <span class="hlt">solar</span> <span class="hlt">activity</span> cycle 22 will surpass SAC 21 in <span class="hlt">activity</span>. The value of R sub m for SAC 22 may approach that of SAC 19. It would be interesting to see whether this prediction is borne out. Researchers are greatly encouraged to proceed with the development of a comprehensive prediction model which includes information provided by cosmic ray data.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2018SpWea..16..230A','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2018SpWea..16..230A"><span>Ionospheric Peak Electron Density and Performance Evaluation of IRI-CCIR Near Magnetic Equator in Africa During Two Extreme <span class="hlt">Solar</span> <span class="hlt">Activities</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Adebesin, B. O.; Rabiu, A. B.; Obrou, O. K.; Adeniyi, J. O.</p> <p>2018-03-01</p> <p>The F2 layer peak electron density (NmF2) was investigated over Korhogo (Geomagnetic: 1.26°S, 67.38°E), a station near the magnetic equator in the African sector. Data for 1996 and 2000 were, respectively, categorized into low <span class="hlt">solar</span> quiet and disturbed and high <span class="hlt">solar</span> quiet and disturbed. NmF2 prenoon peak was higher than the postnoon peak during high <span class="hlt">solar</span> <span class="hlt">activity</span> irrespective of magnetic <span class="hlt">activity</span> condition, while the postnoon peak was higher for low <span class="hlt">solar</span> <span class="hlt">activity</span>. Higher NmF2 peak amplitude characterizes disturbed magnetic <span class="hlt">activity</span> than quiet magnetic condition for any <span class="hlt">solar</span> <span class="hlt">activity</span>. The maximum peaks appeared in equinox. June solstice noontime bite out lagged other seasons by 1-2 h. For any condition of <span class="hlt">solar</span> and magnetic <span class="hlt">activities</span>, the daytime NmF2 percentage variability (%VR) measured by the relative standard deviation maximizes/minimizes in June solstice/equinox. Daytime variability increases with increasing magnetic <span class="hlt">activity</span>. The highest peak in the morning time NmF2 variability occurs in equinox, while the highest evening/nighttime variability appeared in June solstice for all <span class="hlt">solar</span>/magnetic conditions. The nighttime annual variability amplitude is higher during disturbed than quiet condition regardless of <span class="hlt">solar</span> <span class="hlt">activity</span> period. At daytime, variability is similar for all conditions of <span class="hlt">solar</span> <span class="hlt">activities</span>. NmF2 at Korhogo is well represented on the International Reference Ionosphere-International Radio Consultative Committee (IRI-CCIR) option. The model/observation relationship performed best between local midnight and postmidnight period (00-08 LT). The noontime trough characteristics is not prominent in the IRI pattern during high <span class="hlt">solar</span> <span class="hlt">activity</span> but evident during low <span class="hlt">solar</span> conditions when compared with Korhogo observations. The Nash-Sutcliffe coefficients revealed better model performance during disturbed <span class="hlt">activities</span>.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2006ihy..workE.102V','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2006ihy..workE.102V"><span><span class="hlt">Solar</span> Cycle Effects on Equatorial Electrojet Strength and Low Latitude Ionospheric Variability (P10)</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Veenadhari, B.; Alex, S.</p> <p>2006-11-01</p> <p>veena_iig@yahoo.co.in The most obvious indicators of the <span class="hlt">activity</span> of a <span class="hlt">solar</span> cycle are sunspots, flares, plages, and soon. These are intimately linked to the <span class="hlt">solar</span> magnetic fields, heliospheric processes which exhibit complex but systematic variations. The changes in geomagnetic <span class="hlt">activity</span>, as observed in the ground magnetic records follow systematic correspondence with the <span class="hlt">solar</span> <span class="hlt">activity</span> conditions. Thus the transient variations in the magnetic field get modified by differing <span class="hlt">solar</span> conditions. Also the <span class="hlt">solar</span> cycle <span class="hlt">influences</span> the Earth causing changes in geomagnetic <span class="hlt">activity</span>, the magnetosphere and the ionosphere. Daily variations in the ground magnetic field are produced by different current systems in the earth’s space environment flowing in the ionosphere and magnetosphere which has a strong dependence on latitude and longitude of the location. The north-south (Horizontal) configuration of the earth’s magnetic field over the equator is responsible for the narrow band of current system over the equatorial latitudes and is called the Equatorial electrojet (EEJ) and is a primary driver for Equatorial Ionization anomaly (EIA). Equatorial electric fields and plasma drifts play the fundamental roles on the morphology of the low latitude ionosphere and strongly vary during geomagnetically quiet and disturbed periods. Quantitative study is done to illustrate the development process of EEJ and its <span class="hlt">influence</span> on ionospheric parameters. An attempt is also made to examine and discuss the response of the equatorial electrojet parameters to the fast varying conditions of <span class="hlt">solar</span> wind and interplanetary parameters.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://ntrs.nasa.gov/search.jsp?R=19780025037&hterms=solar+use&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D70%26Ntt%3Dsolar%2Buse','NASA-TRS'); return false;" href="https://ntrs.nasa.gov/search.jsp?R=19780025037&hterms=solar+use&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D70%26Ntt%3Dsolar%2Buse"><span>A new use of high resolution magnetograms. [<span class="hlt">solar</span> <span class="hlt">activity</span> and magnetic flux</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Baum, P. J.; Bratenahl, A.</p> <p>1978-01-01</p> <p>Ground-based <span class="hlt">solar</span> magnetograms are frequently in error by as much as twenty percent and contribute to the poor correlation between magnetic changes and <span class="hlt">solar</span> flares. High resolution measurement of the magnetic field component, which is normal to the photosphere and measured at photospheric height, can be used to construct a magnetic flux partition function F. Therefore, dF/dt is an EMF which drives atmospheric currents in reconnecting <span class="hlt">solar</span> <span class="hlt">active</span> regions. With a high quality magnetograph, the <span class="hlt">solar</span> probe can be used to obtain good estimates of F and dF/dt and thereby the energy stored as induced <span class="hlt">solar</span> atmospheric currents during quiescent interflare periods. Should a flare occur during a favorable observing period, the present method of analysis should show characteristic signatures in F, DF/dt, and especially, in the stored flux computed from dF/dt.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2011AdSpR..47.1135V','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2011AdSpR..47.1135V"><span>Birthdates of patients affected by mental illness and <span class="hlt">solar</span> <span class="hlt">activity</span>: A study from Italy</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Ventriglio, Antonio; Borelli, Albacenzina; Bellomo, Antonello; Lepore, Alberto</p> <p>2011-04-01</p> <p>PurposeThis epidemiologic study tested an hypothesized association between the year of birth of persons with major mental illnesses and <span class="hlt">solar</span> <span class="hlt">activity</span> over the past century. MethodsWe collected data on diagnoses and birthdates of psychiatric patients born between 1926 and 1975 (N = 1954) in south Italy for comparison to yearly <span class="hlt">solar</span> <span class="hlt">activity</span> as registered by the International Observatories. ResultsWe found a strong inverse correlation between high <span class="hlt">solar</span> <span class="hlt">activity</span> (HSA) and incidence of schizophrenia and bipolar disorder in a 20-year period whereas the incidence of non-affective/non-psychotic disorders was moderately associated with HSA in the same period. ConclusionsInterpretation of the observed correlations between HSA during years of birth and the incidence of mental illnesses remains unclear, but the findings encourage further study.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/28949585','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/28949585"><span><span class="hlt">Solar</span> Irradiance Variability is Caused by the Magnetic <span class="hlt">Activity</span> on the <span class="hlt">Solar</span> Surface.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Yeo, Kok Leng; Solanki, Sami K; Norris, Charlotte M; Beeck, Benjamin; Unruh, Yvonne C; Krivova, Natalie A</p> <p>2017-09-01</p> <p>The variation in the radiative output of the Sun, described in terms of <span class="hlt">solar</span> irradiance, is important to climatology. A common assumption is that <span class="hlt">solar</span> irradiance variability is driven by its surface magnetism. Verifying this assumption has, however, been hampered by the fact that models of <span class="hlt">solar</span> irradiance variability based on <span class="hlt">solar</span> surface magnetism have to be calibrated to observed variability. Making use of realistic three-dimensional magnetohydrodynamic simulations of the <span class="hlt">solar</span> atmosphere and state-of-the-art <span class="hlt">solar</span> magnetograms from the <span class="hlt">Solar</span> Dynamics Observatory, we present a model of total <span class="hlt">solar</span> irradiance (TSI) that does not require any such calibration. In doing so, the modeled irradiance variability is entirely independent of the observational record. (The absolute level is calibrated to the TSI record from the Total Irradiance Monitor.) The model replicates 95% of the observed variability between April 2010 and July 2016, leaving little scope for alternative drivers of <span class="hlt">solar</span> irradiance variability at least over the time scales examined (days to years).</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/24668282','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/24668282"><span>Tantalum-based semiconductors for <span class="hlt">solar</span> water splitting.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Zhang, Peng; Zhang, Jijie; Gong, Jinlong</p> <p>2014-07-07</p> <p><span class="hlt">Solar</span> energy utilization is one of the most promising solutions for the energy crises. Among all the possible means to make use of <span class="hlt">solar</span> energy, <span class="hlt">solar</span> water splitting is remarkable since it can accomplish the conversion of <span class="hlt">solar</span> energy into chemical energy. The produced hydrogen is clean and sustainable which could be used in various areas. For the past decades, numerous efforts have been put into this research area with many important achievements. Improving the overall efficiency and stability of semiconductor photocatalysts are the research focuses for the <span class="hlt">solar</span> water splitting. Tantalum-based semiconductors, including tantalum oxide, tantalate and tantalum (oxy)nitride, are among the most important photocatalysts. Tantalum oxide has the band gap energy that is suitable for the overall <span class="hlt">solar</span> water splitting. The more negative conduction band minimum of tantalum oxide provides photogenerated electrons with higher potential for the hydrogen generation reaction. Tantalates, with tunable compositions, show high <span class="hlt">activities</span> owning to their layered perovskite structure. (Oxy)nitrides, especially TaON and Ta3N5, have small band gaps to respond to visible-light, whereas they can still realize overall <span class="hlt">solar</span> water splitting with the proper positions of conduction band minimum and valence band maximum. This review describes recent progress regarding the improvement of photocatalytic <span class="hlt">activities</span> of tantalum-based semiconductors. Basic concepts and principles of <span class="hlt">solar</span> water splitting will be discussed in the introduction section, followed by the three main categories regarding to the different types of tantalum-based semiconductors. In each category, synthetic methodologies, <span class="hlt">influencing</span> factors on the photocatalytic <span class="hlt">activities</span>, strategies to enhance the efficiencies of photocatalysts and morphology control of tantalum-based materials will be discussed in detail. Future directions to further explore the research area of tantalum-based semiconductors for <span class="hlt">solar</span> water splitting</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017SerAJ.194...71G','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017SerAJ.194...71G"><span><span class="hlt">Solar</span> Spectral Irradiance Variability of Some Chromospheric Emission Lines Through the <span class="hlt">Solar</span> <span class="hlt">Activity</span> Cycles 21-23</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Göker, Ü. D.; Gigolashvili, M. Sh.; Kapanadze, N.</p> <p>2017-06-01</p> <p>A study of variations of <span class="hlt">solar</span> spectral irradiance (SSI) in the wavelength ranges 121.5 nm-300.5 nm for the period 1981-2009 is presented. We used various data for ultraviolet (UV) spectral lines and international sunspot number (ISSN) from interactive data centers such as SME (NSSDC), UARS (GDAAC), SORCE (LISIRD) and SIDC, respectively. We reduced these data by using the MATLAB software package. In this respect, we revealed negative correlations of intensities of UV (289.5 nm-300.5 nm) spectral lines originating in the <span class="hlt">solar</span> chromosphere with the ISSN index during the unusually prolonged minimum between the <span class="hlt">solar</span> <span class="hlt">activity</span> cycles (SACs) 23 and 24. We also compared our results with the variations of <span class="hlt">solar</span> <span class="hlt">activity</span> indices obtained by the ground-based telescopes. Therefore, we found that plage regions decrease while facular areas are increasing in SAC 23. However, the decrease in plage regions is seen in small sunspot groups (SGs), contrary to this, these regions in large SGs are comparable to previous SACs or even larger as is also seen in facular areas. Nevertheless, negative correlations between ISSN and SSI data indicate that these variations are in close connection with the classes of sunspots/SGs, faculae and plage regions. Finally, we applied the time series analysis of spectral lines corresponding to the wavelengths 121.5 nm-300.5 nm and made comparisons with the ISSN data. We found an unexpected increase in the 298.5 nm line for the Fe II ion. The variability of Fe II ion 298.5 nm line is in close connection with the facular areas and plage regions, and the sizes of these <span class="hlt">solar</span> surface indices play an important role for the SSI variability, as well. So, we compared the connection between the sizes of faculae and plage regions, sunspots/SGs, chemical elements and SSI variability. Our future work will be the theoretical study of this connection and developing of a corresponding model.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2016SPIE10002E..05S','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2016SPIE10002E..05S"><span>Characterization of optical turbulence at the GREGOR <span class="hlt">solar</span> telescope: temporal and local behavior and its <span class="hlt">influence</span> on the <span class="hlt">solar</span> observations</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Sprung, D.; Sucher, E.; Stein, K.; von der Lühe, O.; Berkefeld, Th.</p> <p>2016-10-01</p> <p>Local atmospheric turbulence at the telescope level is regarded as a major reason for affecting the performance of the adaptive optics systems using wavelengths in the visible and infrared for <span class="hlt">solar</span> observations. During the day the air masses around the telescope dome are <span class="hlt">influenced</span> by flow distortions. Additionally heating of the infrastructure close to telescope causes thermal turbulence. Thereby optical turbulence is produced and leads to quality changes in the local seeing throughout the day. Image degradation will be yielded affecting the performance of adaptive optical systems. The spatial resolution of the <span class="hlt">solar</span> observations will be reduced. For this study measurements of the optical turbulence, represented by the structure function parameter of the refractive index Cn2 were performed on several locations at the GREGOR telescope at the Teide observatory at Tenerife at the Canary Islands / Spain. Since September 2012 measurements of Cn2 were carried out between the towers of the Vacuum Tower Telescope (VTT) and of GREGOR with a laser-scintillometer. The horizontal distance of the measurement path was about 75 m. Additional from May 2015 up to March 2016 the optical turbulence was determined at three additional locations close to the <span class="hlt">solar</span> telescope GREGOR. The optical turbulence is derived from sonic anemometer measurements. Time series of the sonic temperature are analyzed and compared to the direct measurements of the laser scintillometer. Meteorological conditions are investigated, especially the <span class="hlt">influence</span> of the wind direction. Turbulence of upper atmospheric layers is not regarded. The measured local turbulence is compared to the system performance of the GREGOR telescopes. It appears that the mountain ridge effects on turbulence are more relevant than any local causes of seeing close to the telescope. Results of these analyses and comparison of nearly one year of measurements are presented and discussed.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.osti.gov/biblio/22370310-prediction-solar-activity-from-solar-background-magnetic-field-variations-cycles','SCIGOV-STC'); return false;" href="https://www.osti.gov/biblio/22370310-prediction-solar-activity-from-solar-background-magnetic-field-variations-cycles"><span>Prediction of <span class="hlt">solar</span> <span class="hlt">activity</span> from <span class="hlt">solar</span> background magnetic field variations in cycles 21-23</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>Shepherd, Simon J.; Zharkov, Sergei I.; Zharkova, Valentina V., E-mail: s.j.shepherd@brad.ac.uk, E-mail: s.zharkov@hull.ac.uk, E-mail: valentina.zharkova@northumbria.ac.uk</p> <p>2014-11-01</p> <p>A comprehensive spectral analysis of both the <span class="hlt">solar</span> background magnetic field (SBMF) in cycles 21-23 and the sunspot magnetic field in cycle 23 reported in our recent paper showed the presence of two principal components (PCs) of SBMF having opposite polarity, e.g., originating in the northern and southern hemispheres, respectively. Over a duration of one <span class="hlt">solar</span> cycle, both waves are found to travel with an increasing phase shift toward the northern hemisphere in odd cycles 21 and 23 and to the southern hemisphere in even cycle 22. These waves were linked to <span class="hlt">solar</span> dynamo waves assumed to form in differentmore » layers of the <span class="hlt">solar</span> interior. In this paper, for the first time, the PCs of SBMF in cycles 21-23 are analyzed with the symbolic regression technique using Hamiltonian principles, allowing us to uncover the underlying mathematical laws governing these complex waves in the SBMF presented by PCs and to extrapolate these PCs to cycles 24-26. The PCs predicted for cycle 24 very closely fit (with an accuracy better than 98%) the PCs derived from the SBMF observations in this cycle. This approach also predicts a strong reduction of the SBMF in cycles 25 and 26 and, thus, a reduction of the resulting <span class="hlt">solar</span> <span class="hlt">activity</span>. This decrease is accompanied by an increasing phase shift between the two predicted PCs (magnetic waves) in cycle 25 leading to their full separation into the opposite hemispheres in cycle 26. The variations of the modulus summary of the two PCs in SBMF reveals a remarkable resemblance to the average number of sunspots in cycles 21-24 and to predictions of reduced sunspot numbers compared to cycle 24: 80% in cycle 25 and 40% in cycle 26.« less</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/1983ApJ...265.1056G','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/1983ApJ...265.1056G"><span>Large-scale patterns formed by <span class="hlt">solar</span> <span class="hlt">active</span> regions during the ascending phase of cycle 21</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Gaizauskas, V.; Harvey, K. L.; Harvey, J. W.; Zwaan, C.</p> <p>1983-02-01</p> <p>Synoptic maps of photospheric magnetic fields prepared at the Kitt Peak National Observatory are used in investigating large-scale patterns in the spatial and temporal distribution of <span class="hlt">solar</span> <span class="hlt">active</span> regions for 27 <span class="hlt">solar</span> rotations between 1977 and 1979. The <span class="hlt">active</span> regions are found to be distributed in 'complexes of <span class="hlt">activity</span>' (Bumba and Howard, 1965). With the working definition of a complex of <span class="hlt">activity</span> based on continuity and proximity of the constituent <span class="hlt">active</span> regions, the phenomenology of complexes is explored. It is found that complexes of <span class="hlt">activity</span> form within one month and that they are typically maintained for 3 to 6 <span class="hlt">solar</span> rotations by fresh injections of magnetic flux. During the <span class="hlt">active</span> lifetime of a complex of <span class="hlt">activity</span>, the total magnetic flux in the complex remains steady to within a factor of 2. The magnetic polarities are closely balanced, and each complex rotates about the sun at its own special, constant rate. In certain cases, the complexes form two diverging branches.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017ResPh...7..385S','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017ResPh...7..385S"><span>Search for possible <span class="hlt">solar</span> <span class="hlt">influences</span> in Ra-226 decays</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Stancil, Daniel D.; Balci Yegen, Sümeyra; Dickey, David A.; Gould, Chris R.</p> <p></p> <p>Measurements of Ra-226 <span class="hlt">activity</span> from eight HPGe gamma ray detectors at the NC State University PULSTAR Reactor were analyzed for evidence of periodic variations, with particular attention to annual variations. All measurements were made using the same reference source, and data sets were of varying length taken over the time period from September 1996 through August 2014. Clear evidence of annual variations was observed in data from four of the detectors. Short time periodograms from the data sets suggest temporal variability of both the amplitude and frequency of these variations. The annual variations in two of the data sets show peak values near the first of February, while surprisingly, the annual variations in the other two are roughly out of phase with the first two. Three of the four detectors exhibited annual variations over approximately the same time period. A joint statistic constructed by combining spectra from these three shows peaks approximating the frequencies of <span class="hlt">solar</span> r-mode oscillations with νR = 11.74 cpy, m = 1, and l = 3, 5, 6. The fact that similar variations were not present in all detectors covering similar time periods rules out variations in <span class="hlt">activity</span> as the cause, and points to differing sensitivities to unspecified environmental parameters instead. In addition to seasonal variations, the modulation of environmental parameters by <span class="hlt">solar</span> processes remains a possible explanation of periodogram features, but without requiring new physics.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/19910009603','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/19910009603"><span>Simultaneous <span class="hlt">Solar</span> Maximum Mission (SMM) and Very Large Array (VLA) observations of <span class="hlt">solar</span> <span class="hlt">active</span> regions</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Willson, Robert F.</p> <p>1991-01-01</p> <p>Very Large Array observations at 20 cm wavelength can detect the hot coronal plasma previously observed at soft x ray wavelengths. Thermal cyclotron line emission was detected at the apex of coronal loops where the magnetic field strength is relatively constant. Detailed comparison of simultaneous <span class="hlt">Solar</span> Maximum Mission (SMM) Satellite and VLA data indicate that physical parameters such as electron temperature, electron density, and magnetic field strength can be obtained, but that some coronal loops remain invisible in either spectral domain. The unprecedent spatial resolution of the VLA at 20 cm wavelength showed that the precursor, impulsive, and post-flare components of <span class="hlt">solar</span> bursts originate in nearby, but separate loops or systems of loops.. In some cases preburst heating and magnetic changes are observed from loops tens of minutes prior to the impulsive phase. Comparisons with soft x ray images and spectra and with hard x ray data specify the magnetic field strength and emission mechanism of flaring coronal loops. At the longer 91 cm wavelength, the VLA detected extensive emission interpreted as a hot 10(exp 5) K interface between cool, dense H alpha filaments and the surrounding hotter, rarefield corona. Observations at 91 cm also provide evidence for time-correlated bursts in <span class="hlt">active</span> regions on opposite sides of the <span class="hlt">solar</span> equator; they are attributed to flare triggering by relativistic particles that move along large-scale, otherwise-invisible, magnetic conduits that link <span class="hlt">active</span> regions in opposite hemispheres of the Sun.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.osti.gov/biblio/22661432-magnetic-properties-solar-active-regions-govern-large-solar-flares-eruptions','SCIGOV-STC'); return false;" href="https://www.osti.gov/biblio/22661432-magnetic-properties-solar-active-regions-govern-large-solar-flares-eruptions"><span>MAGNETIC PROPERTIES OF <span class="hlt">SOLAR</span> <span class="hlt">ACTIVE</span> REGIONS THAT GOVERN LARGE <span class="hlt">SOLAR</span> FLARES AND ERUPTIONS</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>Toriumi, Shin; Schrijver, Carolus J.; Harra, Louise K.</p> <p></p> <p><span class="hlt">Solar</span> flares and coronal mass ejections (CMEs), especially the larger ones, emanate from <span class="hlt">active</span> regions (ARs). With the aim of understanding the magnetic properties that govern such flares and eruptions, we systematically survey all flare events with Geostationary Orbiting Environmental Satellite levels of ≥M5.0 within 45° from disk center between 2010 May and 2016 April. These criteria lead to a total of 51 flares from 29 ARs, for which we analyze the observational data obtained by the <span class="hlt">Solar</span> Dynamics Observatory . More than 80% of the 29 ARs are found to exhibit δ -sunspots, and at least three ARs violatemore » Hale’s polarity rule. The flare durations are approximately proportional to the distance between the two flare ribbons, to the total magnetic flux inside the ribbons, and to the ribbon area. From our study, one of the parameters that clearly determine whether a given flare event is CME-eruptive or not is the ribbon area normalized by the sunspot area, which may indicate that the structural relationship between the flaring region and the entire AR controls CME productivity. AR characterization shows that even X-class events do not require δ -sunspots or strong-field, high-gradient polarity inversion lines. An investigation of historical observational data suggests the possibility that the largest <span class="hlt">solar</span> ARs, with magnetic flux of 2 × 10{sup 23} Mx, might be able to produce “superflares” with energies of the order of 10{sup 34} erg. The proportionality between the flare durations and magnetic energies is consistent with stellar flare observations, suggesting a common physical background for <span class="hlt">solar</span> and stellar flares.« less</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.osti.gov/biblio/22667286-data-assimilation-approach-forecast-solar-activity-cycles','SCIGOV-STC'); return false;" href="https://www.osti.gov/biblio/22667286-data-assimilation-approach-forecast-solar-activity-cycles"><span>DATA ASSIMILATION APPROACH FOR FORECAST OF <span class="hlt">SOLAR</span> <span class="hlt">ACTIVITY</span> CYCLES</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>Kitiashvili, Irina N., E-mail: irina.n.kitiashvili@nasa.gov</p> <p></p> <p>Numerous attempts to predict future <span class="hlt">solar</span> cycles are mostly based on empirical relations derived from observations of previous cycles, and they yield a wide range of predicted strengths and durations of the cycles. Results obtained with current dynamo models also deviate strongly from each other, thus raising questions about criteria to quantify the reliability of such predictions. The primary difficulties in modeling future <span class="hlt">solar</span> <span class="hlt">activity</span> are shortcomings of both the dynamo models and observations that do not allow us to determine the current and past states of the global <span class="hlt">solar</span> magnetic structure and its dynamics. Data assimilation is a relativelymore » new approach to develop physics-based predictions and estimate their uncertainties in situations where the physical properties of a system are not well-known. This paper presents an application of the ensemble Kalman filter method for modeling and prediction of <span class="hlt">solar</span> cycles through use of a low-order nonlinear dynamo model that includes the essential physics and can describe general properties of the sunspot cycles. Despite the simplicity of this model, the data assimilation approach provides reasonable estimates for the strengths of future <span class="hlt">solar</span> cycles. In particular, the prediction of Cycle 24 calculated and published in 2008 is so far holding up quite well. In this paper, I will present my first attempt to predict Cycle 25 using the data assimilation approach, and discuss the uncertainties of that prediction.« less</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017EGUGA..19.2646N','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017EGUGA..19.2646N"><span>Study the gradient characteristics of the ionosphere at equatorial latitude during the latest cycle of <span class="hlt">solar</span> <span class="hlt">activity</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Nguyen Thai, Chinh; Temitope Seun, Oluwadare; Le Thi, Nhung; Schuh, Harald</p> <p>2017-04-01</p> <p>The sun has its own seasons with an average duration of about 11 years. In this time, the sun enters a period of increased <span class="hlt">activity</span> called the <span class="hlt">solar</span> maximum and a period of decreased <span class="hlt">activity</span> called the <span class="hlt">solar</span> minimum. Cycles span from one minimum to the next. The current <span class="hlt">solar</span> cycle is 24, which began on January 4, 2008 and is expected to be ended in 2019. During this period, the ionosphere changes its thickness and its characteristics as well. The change is most complicated and unpredictable at the equatorial latitudes in a band around 150 northward and 150 southward from the equator. Thailand is located in these regions is known as one of the countries most affected by the ionosphere change. Ionospheric information such as the vertical total electron content (VTEC) and scintillation indices can be extracted from the measurements of GNSS dual-frequency receivers. In this study, a Matlab tool is programmed to calculate some ionosphere parameters from the normal RINEX observation file including VTEC value, amplitude scintillation S4 index and others. The value of VTEC at one IGS station in Thailand (13.740N, 100.530E) is computed for almost one full <span class="hlt">solar</span> cycle, that is 8 years, from 2009 to 2016. From these results, we are able to derive the rules of TEC variation over time and its dependence on <span class="hlt">solar</span> <span class="hlt">activity</span> in the equatorial regions. The change of VTEC is estimated in diurnal, seasonal and annual variation for the latest <span class="hlt">solar</span> cycle. The <span class="hlt">solar</span> cycle can be represented in several ways, in this paper we use the sunspot number and the F10.7 cm radio flux to describe the <span class="hlt">solar</span> <span class="hlt">activity</span>. The correlation coefficients between these <span class="hlt">solar</span> indices and the monthly maximum of VTEC value are around 0.87, this indicates a high dependence of the ionosphere on <span class="hlt">solar</span> <span class="hlt">activity</span>. Besides, a scintillation map derived from GNSS data is displayed to indicate the intensity of scintillation <span class="hlt">activity</span>.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2016cosp...41E1762S','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2016cosp...41E1762S"><span>Geomagnetic <span class="hlt">activity</span> during 10 - 11 <span class="hlt">solar</span> cycles that has been observed by old Russian observatories.</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Seredyn, Tomasz; Wysokinski, Arkadiusz; Kobylinski, Zbigniew; Bialy, Jerzy</p> <p>2016-07-01</p> <p>A good knowledge of <span class="hlt">solar</span>-terrestrial relations during past <span class="hlt">solar</span> <span class="hlt">activity</span> cycles could give the appropriate tools for a correct space weather forecast. The paper focuses on the analysis of the historical collections of the ground based magnetic observations and their operational indices from the period of two sunspot <span class="hlt">solar</span> cycles 10 - 11, period 1856 - 1878 (Bartels rotations 324 - 635). We use hourly observations of H and D geomagnetic field components registered at Russian stations: St. Petersburg - Pavlovsk, Barnaul, Ekaterinburg, Nertshinsk, Sitka, and compare them to the data obtained from the Helsinki observatory. We compare directly these records and also calculated from the data of the every above mentioned station IHV indices introduced by Svalgaard (2003), which have been used for further comparisons in epochs of assumed different polarity of the heliospheric magnetic field. We used also local index C9 derived by Zosimovich (1981) from St. Petersburg - Pavlovsk data. <span class="hlt">Solar</span> <span class="hlt">activity</span> is represented by sunspot numbers. The correlative and continuous wavelet analyses are applied for estimation of the correctness of records from different magnetic stations. We have specially regard to magnetic storms in the investigated period and the special Carrington event of 1-2 Sep 1859. Generally studied magnetic time series correctly show variability of the geomagnetic <span class="hlt">activity</span>. Geomagnetic <span class="hlt">activity</span> presents some delay in relation to <span class="hlt">solar</span> one as it is seen especially during descending and minimum phase of the even 11-year cycle. This pattern looks similarly in the case of 16 - 17 <span class="hlt">solar</span> cycles.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=3848890','PMC'); return false;" href="https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=3848890"><span>The <span class="hlt">influence</span> of passivation and photovoltaic properties of α-Si:H coverage on silicon nanowire array <span class="hlt">solar</span> 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></p> <p>2013-01-01</p> <p>Silicon nanowire (SiNW) arrays for radial p-n junction <span class="hlt">solar</span> cells offer potential advantages of light trapping effects and quick charge collection. Nevertheless, lower open circuit voltages (Voc) lead to lower energy conversion efficiencies. In such cases, the performance of the <span class="hlt">solar</span> cells depends critically on the quality of the SiNW interfaces. In this study, SiNW core-shell <span class="hlt">solar</span> cells have been fabricated by growing crystalline silicon (c-Si) nanowires via the metal-assisted chemical etching method and by depositing hydrogenated amorphous silicon (α-Si:H) via the plasma-enhanced chemical vapor deposition (PECVD) method. The <span class="hlt">influence</span> of deposition parameters on the coverage and, consequently, the passivation and photovoltaic properties of α-Si:H layers on SiNW <span class="hlt">solar</span> cells have been analyzed. PMID:24059343</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2018AnGeo..36..555F','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2018AnGeo..36..555F"><span>Effects of <span class="hlt">solar</span> <span class="hlt">activity</span> and galactic cosmic ray cycles on the modulation of the annual average temperature at two sites in southern Brazil</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Frigo, Everton; Antonelli, Francesco; da Silva, Djeniffer S. S.; Lima, Pedro C. M.; Pacca, Igor I. G.; Bageston, José V.</p> <p>2018-04-01</p> <p>Quasi-periodic variations in <span class="hlt">solar</span> <span class="hlt">activity</span> and galactic cosmic rays (GCRs) on decadal and bidecadal timescales have been suggested as a climate forcing mechanism for many regions on Earth. One of these regions is southern Brazil, where the lowest values during the last century were observed for the total geomagnetic field intensity at the Earth's surface. These low values are due to the passage of the center of the South Atlantic Magnetic Anomaly (SAMA), which crosses the Brazilian territory from east to west following a latitude of ˜ 26°. In areas with low geomagnetic intensity, such as the SAMA, the incidence of GCRs is increased. Consequently, possible climatic effects related to the GCRs tend to be maximized in this region. In this work, we investigate the relationship between the ˜ 11-year and ˜ 22-year cycles that are related to <span class="hlt">solar</span> <span class="hlt">activity</span> and GCRs and the annual average temperature recorded between 1936 and 2014 at two weather stations, both located near a latitude of 26° S but at different longitudes. The first of these stations (Torres - TOR) is located in the coastal region, and the other (Iraí - IRA) is located in the interior, around 450 km from the Atlantic Ocean. Sunspot data and the <span class="hlt">solar</span> modulation potential for cosmic rays were used as proxies for the <span class="hlt">solar</span> <span class="hlt">activity</span> and the GCRs, respectively. Our investigation of the <span class="hlt">influence</span> of decadal and bidecadal cycles in temperature data was carried out using the wavelet transform coherence (WTC) spectrum. The results indicate that periodicities of 11 years may have continuously modulated the climate at TOR via a nonlinear mechanism, while at IRA, the effects of this 11-year modulation period were intermittent. Four temperature maxima, separated by around 20 years, were detected in the same years at both weather stations. These temperature maxima are almost coincident with the maxima of the odd <span class="hlt">solar</span> cycles. Furthermore, these maxima occur after transitions from even to odd <span class="hlt">solar</span> cycles, that is</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017Ge%26Ae..57..524D','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017Ge%26Ae..57..524D"><span>Paleoclimate of the Earth and <span class="hlt">solar</span> <span class="hlt">activity</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Dergachev, V. A.</p> <p>2017-09-01</p> <p>The paper focuses on climate variations caused by the orbital effect and <span class="hlt">solar</span> <span class="hlt">activity</span> over the last one million years and oscillations (warming or cooling) of the climate since the last ice age retreat. Attention is paid to a significant discrepancy in the trend of global temperature change during the modern interglacial epoch (Holocene) obtained by various methods. A long-term cooling trend was observed in the summer temperature of the Northern Hemisphere during the last 2000 years.</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('http://hdl.handle.net/2060/20080012635','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/20080012635"><span><span class="hlt">Solar</span> Cycle #24 and the <span class="hlt">Solar</span> Dynamo</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Schatten, Kenneth; Pesnell, W. Dean</p> <p>2007-01-01</p> <p>We focus on two <span class="hlt">solar</span> aspects related to flight dynamics. These are the <span class="hlt">solar</span> dynamo and long-term <span class="hlt">solar</span> <span class="hlt">activity</span> predictions. The nature of the <span class="hlt">solar</span> dynamo is central to <span class="hlt">solar</span> <span class="hlt">activity</span> predictions, and these predictions are important for orbital planning of satellites in low earth orbit (LEO). The reason is that the <span class="hlt">solar</span> ultraviolet (UV) and extreme ultraviolet (EUV) spectral irradiances inflate the upper atmospheric layers of the Earth, forming the thermosphere and exosphere through which these satellites orbit. Concerning the dynamo, we discuss some recent novel approaches towards its understanding. For <span class="hlt">solar</span> predictions we concentrate on a <span class="hlt">solar</span> precursor method, in which the Sun's polar field plays a major role in forecasting the next cycle s <span class="hlt">activity</span> based upon the Babcock-Leighton dynamo. With a current low value for the Sun s polar field, this method predicts that <span class="hlt">solar</span> cycle #24 will be one of the lowest in recent times, with smoothed F10.7 radio flux values peaking near 130 plus or minus 30 (2 sigma), in the 2013 timeframe. One may have to consider <span class="hlt">solar</span> <span class="hlt">activity</span> as far back as the early 20th century to find a cycle of comparable magnitude. Concomitant effects of low <span class="hlt">solar</span> <span class="hlt">activity</span> upon satellites in LEO will need to be considered, such as enhancements in orbital debris. Support for our prediction of a low <span class="hlt">solar</span> cycle #24 is borne out by the lack of new cycle sunspots at least through the first half of 2007. Usually at the present epoch in the <span class="hlt">solar</span> cycle (approx. 7+ years after the last <span class="hlt">solar</span> maximum), for a normal size following cycle, new cycle sunspots would be seen. The lack of their appearance at this time is only consistent with a low cycle #24. Polar field observations of a weak magnitude are consistent with unusual structures seen in the Sun s corona. Polar coronal holes are the hallmarks of the Sun's open field structures. At present, it appears that the polar coronal holes are relatively weak, and there have been many equatorial coronal holes</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/20070032658','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/20070032658"><span><span class="hlt">Solar</span> Cycle #24 and the <span class="hlt">Solar</span> Dynamo</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Pesnell, W. Dean; Schatten, Kenneth</p> <p>2007-01-01</p> <p>We focus on two <span class="hlt">solar</span> aspects related to flight dynamics. These are the <span class="hlt">solar</span> dynamo and long-term <span class="hlt">solar</span> <span class="hlt">activity</span> predictions. The nature of the <span class="hlt">solar</span> dynamo is central to <span class="hlt">solar</span> <span class="hlt">activity</span> predictions, and these predictions are important for orbital planning of satellites in low earth orbit (LEO). The reason is that the <span class="hlt">solar</span> ultraviolet (UV) and extreme ultraviolet (EUV) spectral irradiances inflate the upper atmospheric layers of the Earth, forming the thermosphere and exosphere through which these satellites orbit. Concerning the dynamo, we discuss some recent novel approaches towards its understanding. For <span class="hlt">solar</span> predictions we concentrate on a <span class="hlt">solar</span> precursor method, in which the Sun s polar field plays a major role in forecasting the next cycle s <span class="hlt">activity</span> based upon the Babcock- Leighton dynamo. With a current low value for the Sun s polar field, this method predicts that <span class="hlt">solar</span> cycle #24 will be one of the lowest in recent times, with smoothed F10.7 radio flux values peaking near 130+ 30 (2 4, in the 2013 timeframe. One may have to consider <span class="hlt">solar</span> <span class="hlt">activity</span> as far back as the early 20th century to find a cycle of comparable magnitude. Concomitant effects of low <span class="hlt">solar</span> <span class="hlt">activity</span> upon satellites in LEO will need to be considered, such as enhancements in orbital debris. Support for our prediction of a low <span class="hlt">solar</span> cycle #24 is borne out by the lack of new cycle sunspots at least through the first half of 2007. Usually at the present epoch in the <span class="hlt">solar</span> cycle (-7+ years after the last <span class="hlt">solar</span> maximum), for a normal size following cycle, new cycle sunspots would be seen. The lack of their appearance at this time is only consistent with a low cycle #24. Polar field observations of a weak magnitude are consistent with unusual structures seen in the Sun s corona. Polar coronal holes are the hallmarks of the Sun s open field structures. At present, it appears that the polar coronal holes are relatively weak, and there have been many equatorial coronal holes. This appears</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/25353240','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/25353240"><span>Radiation exposure of German aircraft crews under the impact of <span class="hlt">solar</span> cycle 23 and airline business factors.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Frasch, Gerhard; Kammerer, Lothar; Karofsky, Ralf; Schlosser, Andrea; Stegemann, Ralf</p> <p>2014-12-01</p> <p>The exposure of German aircraft crews to cosmic radiation varies both with <span class="hlt">solar</span> <span class="hlt">activity</span> and operational factors of airline business. Data come from the German central dose registry and cover monthly exposures of up to 37,000 German aircraft crewmembers that were under official monitoring. During the years 2004 to 2009 of <span class="hlt">solar</span> cycle 23 (i.e., in the decreasing phase of <span class="hlt">solar</span> <span class="hlt">activity</span>), the annual doses of German aircraft crews increased by an average of 20%. Decreasing <span class="hlt">solar</span> <span class="hlt">activity</span> allows more galactic radiation to reach the atmosphere, increasing high-altitude doses. The rise results mainly from the less effective protection from the <span class="hlt">solar</span> wind but also from airline business factors. Both cockpit and cabin personnel differ in age-dependent professional and social status. This status determines substantially the annual effective dose: younger cabin personnel and the elder pilots generally receive higher annual doses than their counterparts. They also receive larger increases in their annual dose when the <span class="hlt">solar</span> <span class="hlt">activity</span> decreases. The doses under this combined <span class="hlt">influence</span> of <span class="hlt">solar</span> <span class="hlt">activity</span> and airline business factors result in a maximum of exposure for German aircrews for this <span class="hlt">solar</span> cycle. With the increasing <span class="hlt">solar</span> <span class="hlt">activity</span> of the current <span class="hlt">solar</span> cycle 24, the doses are expected to decrease again.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2012IzAOP..48..738V','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2012IzAOP..48..738V"><span>Grand minima of <span class="hlt">solar</span> <span class="hlt">activity</span> and sociodynamics of culture</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Vladimirsky, B. M.</p> <p>2012-12-01</p> <p>Indices of creative productivity introduced by C. Murrey were used to verify S. Ertel's conclusion about a global increase in creative productivity during the prolonged minimum of <span class="hlt">solar</span> <span class="hlt">activity</span> in 1640-1710. It was found that these indices for mathematicians, philosophers, and scientists increase in the Maunder era by factor of 1.6 in comparison with intervals of the same length before and after the minimum. A similar effect was obtained for mathematicians and philosophers for five earlier equitype minima in total (an increase by a factor of 1.9). The regularity that is revealed is confirmed by the fact that the most important achievements of high-ranking mathematicians and philosophers during the whole time period (2300 years) considered in this study fall on epochs of reduced levels of <span class="hlt">solar</span> <span class="hlt">activity</span>. The rise in the probability of the generation of rational ideas during grand minima is reflected also in the fact that they precede the appearance of written language and farming. Ultra-low-frequency electromagnetic fields appear to serve as a physical agent stimulating the <span class="hlt">activity</span> of the brain's left hemisphere during the epochs of minima.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2016BlgAJ..25...78K','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2016BlgAJ..25...78K"><span>Sub- and Quasi-Centurial Cycles in <span class="hlt">Solar</span> and Geomagnetic <span class="hlt">Activity</span> Data Series</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Komitov, B.; Sello, S.; Duchlev, P.; Dechev, M.; Penev, K.; Koleva, K.</p> <p>2016-07-01</p> <p>The subject of this paper is the existence and stability of <span class="hlt">solar</span> cycles with durations in the range of 20-250 years. Five types of data series are used: 1) the Zurich series (1749-2009 AD), the mean annual International sunspot number Ri, 2) the Group sunspot number series Rh (1610-1995 AD), 3) the simulated extended sunspot number from Extended time series of <span class="hlt">Solar</span> <span class="hlt">Activity</span> Indices (ESAI) (1090-2002 AD), 4) the simulated extended geomagnetic aa-index from ESAI (1099-2002 AD), 5) the Meudon filament series (1919-1991 AD). Two principally independent methods of time series analysis are used: the T-R periodogram analysis (both in standard and ``scanning window'' regimes) and the wavelet-analysis. The obtained results are very similar. A strong cycle with a mean duration of 55-60 years is found to exist in all series. On the other hand, a strong and stable quasi 110-120 years and ˜200-year cycles are obtained in all of these series except in the Ri one. The high importance of the long term <span class="hlt">solar</span> <span class="hlt">activity</span> dynamics for the aims of <span class="hlt">solar</span> dynamo modeling and predictions is especially noted.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2006IAUSS...2E...4K','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2006IAUSS...2E...4K"><span>Life of the Earth in the <span class="hlt">solar</span> atmosphere (multimedia manual)</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Kononovich, E. V.; Smirnova, O. B.; Matveychuk, T. V.; Jakunina, G. V.; Krasotkin, S. A.</p> <p>2006-08-01</p> <p>The purpose of this manual is to illustrate the major physical processes occurring in the Sun - Earth system and ecology of the planet life. The material includes three individual parts: "The Earth", "The Sun" and "The <span class="hlt">solar</span>-terrestrial connections". Sections do not require cross-references since each of them is self-complete. Inside the sections the material is located in sequences based on the principle: from simple to complex. The material is designed for students of the senior classes of high school and junior university level interested by the problem. The section "The Earth" is devoted to the description of the basic characteristics of the planet: internal structure, magnetic field, lithosphere and an atmosphere together with various occurring in them tectonic, hydro- and atmospheric processes. The top layers of an atmosphere, an ionosphere, a zone of polar lights, radiating belts, magnetosphere are also considered. The section "The Sun" includes the following subsections: the Sun as a star, internal structure of the Sun, <span class="hlt">Solar</span> atmosphere, <span class="hlt">solar</span> <span class="hlt">activity</span>, cyclicity of the <span class="hlt">solar</span> <span class="hlt">activity</span>, helioseismology. In the section "The <span class="hlt">solar</span>-terrestrial connections" the previous material is used to present the <span class="hlt">influence</span> of the <span class="hlt">active</span> <span class="hlt">solar</span> processes on the most various aspects of a terrestrial life: ecological, biological, mental, social, economic and so forth. The problem of forecasting of the <span class="hlt">solar</span> <span class="hlt">activity</span> as the key parameter determining a condition of the so-called space weather is considered.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/27714661','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/27714661"><span>The role of visible light <span class="hlt">active</span> TiO2 specimens on the <span class="hlt">solar</span> photocatalytic disinfection of E. coli.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Birben, Nazmiye Cemre; Tomruk, Ayse; Bekbolet, Miray</p> <p>2017-05-01</p> <p><span class="hlt">Solar</span> photocatalytic disinfection efficiency of novel visible light <span class="hlt">activated</span> (VLA) photocatalysts was evaluated with the aim of assessing inactivation of Escherichia coli as the pathogen indicator organism present in drinking water. <span class="hlt">Influence</span> of humic acid (HA) on the photocatalytic disinfection efficiency of the specified VLA TiO 2 specimens i.e., N-doped, Se-doped, and Se-N co-doped TiO 2 was also investigated. Photocatalytic disinfection efficiency was assessed by the enumeration of bacteria following selected irradiation periods. Degradation and compositional changes in organic matter (OM) was also tracked by means of UV-vis and advanced fluorescence spectroscopic (EEM features) parameters. Photocatalytic mineralization of the organic matter was followed by dissolved organic carbon contents. Presence of HA as a model organic compound of natural organic matter (NOM) displayed a retardation effect on <span class="hlt">solar</span> photocatalytic abatement of E. coli. However, no distinctly different effect was observed under <span class="hlt">solar</span> photolytic conditions due to the presence of HA. Regrowth of E. coli could not be assessed under the specified experimental conditions. A comparison was introduced with respect to the use of undoped TiO 2 P-25 as the photocatalyst.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/18031791','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/18031791"><span>The extreme <span class="hlt">solar</span> cosmic ray particle event on 20 January 2005 and its <span class="hlt">influence</span> on the radiation dose rate at aircraft altitude.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Bütikofer, R; Flückiger, E O; Desorgher, L; Moser, M R</p> <p>2008-03-01</p> <p>In January 2005 toward the end of <span class="hlt">solar</span> <span class="hlt">activity</span> cycle 23 the Sun was very <span class="hlt">active</span>. Between 15 and 20 January 2005, the <span class="hlt">solar</span> <span class="hlt">active</span> region NOAA AR 10720 produced five powerful <span class="hlt">solar</span> flares. In association with this major <span class="hlt">solar</span> <span class="hlt">activity</span> several pronounced variations in the ground-level cosmic ray intensity were observed. The fifth of these flares (X7.1) produced energetic <span class="hlt">solar</span> cosmic rays that caused a giant increase in the count rates of the ground-based cosmic ray detectors (neutron monitors). At southern polar neutron monitor stations the increase of the count rate reached several thousand percent. From the recordings of the worldwide network of neutron monitors, we determined the characteristics of the <span class="hlt">solar</span> particle flux near Earth. In the initial phase of the event, the <span class="hlt">solar</span> cosmic ray flux near Earth was extremely anisotropic. The energy spectrum of the <span class="hlt">solar</span> cosmic rays was fairly soft during the main and the decay phase. We investigated also the flux of different secondary particle species in the atmosphere and the radiation dosage at flight altitude. Our analysis shows a maximum increment of the effective dose rate due to <span class="hlt">solar</span> cosmic rays in the south polar region around 70 degrees S and 130 degrees E at flight altitude of almost three orders of magnitude.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://eric.ed.gov/?q=solar+AND+energy&pg=5&id=ED179793','ERIC'); return false;" href="https://eric.ed.gov/?q=solar+AND+energy&pg=5&id=ED179793"><span>Collecting <span class="hlt">Solar</span> Energy. <span class="hlt">Solar</span> Energy Education Project.</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>O'Brien, Alexander</p> <p></p> <p>This <span class="hlt">solar</span> energy learning module for use with junior high school students offers a list of <span class="hlt">activities</span>, a pre-post test, job titles, basic <span class="hlt">solar</span> energy vocabulary, and diagrams of <span class="hlt">solar</span> energy collectors and installations. The purpose is to familiarize students with applications of <span class="hlt">solar</span> energy and titles of jobs where this knowledge could be…</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://files.eric.ed.gov/fulltext/ED270294.pdf','ERIC'); return false;" href="http://files.eric.ed.gov/fulltext/ED270294.pdf"><span>Climate Fundamentals for <span class="hlt">Solar</span> Heating.</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>Conservation and Renewable Energy Inquiry and Referral Service (DOE), Silver Spring, MD.</p> <p></p> <p>The design of any <span class="hlt">solar</span> heating system is <span class="hlt">influenced</span> heavily by climate; in this bulletin, information on climate as related to <span class="hlt">solar</span> heating is as related to <span class="hlt">solar</span> heating is provided. Topics discussed include: (1) <span class="hlt">solar</span> radiation; (2) degree days; (3) climate and calculations which make use of <span class="hlt">solar</span> radiation and degree days; and (4)…</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://ntrs.nasa.gov/search.jsp?R=19770041233&hterms=Krieger&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D50%26Ntt%3DKrieger','NASA-TRS'); return false;" href="https://ntrs.nasa.gov/search.jsp?R=19770041233&hterms=Krieger&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D50%26Ntt%3DKrieger"><span>Skylab observations of X-ray loops connecting separate <span class="hlt">active</span> regions. [<span class="hlt">solar</span> <span class="hlt">activity</span></span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Chase, R. C.; Krieger, A. S.; Svestka, Z.; Vaiana, G. S.</p> <p>1976-01-01</p> <p>One hundred loops interconnecting 94 separate <span class="hlt">active</span> <span class="hlt">solar</span> regions detectable in soft X-rays were identified during the Skylab mission. While close <span class="hlt">active</span> regions are commonly interconnected with loops, the number of such interconnections decreases steeply for longer distances; the longest interconnecting loop observed in the Skylab data connected regions separated by 37 deg. Several arguments are presented which support the point of view that this is the actual limit of the size of magnetic interconnections between <span class="hlt">active</span> regions. No sympathetic flares could be found in the interconnected regions. These results cast doubt on the hypothesis that accelerated particles can be guided in interconnecting loops from one <span class="hlt">active</span> region to another over distances of 100 deg or more and eventually produce sympathetic flares in them.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://ntrs.nasa.gov/search.jsp?R=19900033508&hterms=Volcanic+eruptions&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D30%26Ntt%3DVolcanic%2Beruptions','NASA-TRS'); return false;" href="https://ntrs.nasa.gov/search.jsp?R=19900033508&hterms=Volcanic+eruptions&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D30%26Ntt%3DVolcanic%2Beruptions"><span>Volcanic eruptions and <span class="hlt">solar</span> <span class="hlt">activity</span></span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Stothers, Richard B.</p> <p>1989-01-01</p> <p>The historical record of large volcanic eruptions from 1500 to 1980 is subjected to detailed time series analysis. In two weak but probably statistically significant periodicities of about 11 and 80 yr, the frequency of volcanic eruptions increases (decreases) slightly around the times of <span class="hlt">solar</span> minimum (maximum). Time series analysis of the volcanogenic acidities in a deep ice core from Greenland reveals several very long periods ranging from about 80 to about 350 yr which are similar to the very slow <span class="hlt">solar</span> cycles previously detected in auroral and C-14 records. <span class="hlt">Solar</span> flares may cause changes in atmospheric circulation patterns that abruptly alter the earth's spin. The resulting jolt probably triggers small earthquakes which affect volcanism.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2018ApJ...854L...2M','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2018ApJ...854L...2M"><span>Proton Fluxes Measured by the PAMELA Experiment from the Minimum to the Maximum <span class="hlt">Solar</span> <span class="hlt">Activity</span> for <span class="hlt">Solar</span> Cycle 24</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Martucci, M.; Munini, R.; Boezio, M.; Di Felice, V.; Adriani, O.; Barbarino, G. C.; Bazilevskaya, G. A.; Bellotti, R.; Bongi, M.; Bonvicini, V.; Bottai, S.; Bruno, A.; Cafagna, F.; Campana, D.; Carlson, P.; Casolino, M.; Castellini, G.; De Santis, C.; Galper, A. M.; Karelin, A. V.; Koldashov, S. V.; Koldobskiy, S.; Krutkov, S. Y.; Kvashnin, A. N.; Leonov, A.; Malakhov, V.; Marcelli, L.; Marcelli, N.; Mayorov, A. G.; Menn, W.; Mergè, M.; Mikhailov, V. V.; Mocchiutti, E.; Monaco, A.; Mori, N.; Osteria, G.; Panico, B.; Papini, P.; Pearce, M.; Picozza, P.; Ricci, M.; Ricciarini, S. B.; Simon, M.; Sparvoli, R.; Spillantini, P.; Stozhkov, Y. I.; Vacchi, A.; Vannuccini, E.; Vasilyev, G.; Voronov, S. A.; Yurkin, Y. T.; Zampa, G.; Zampa, N.; Potgieter, M. S.; Raath, J. L.</p> <p>2018-02-01</p> <p>Precise measurements of the time-dependent intensity of the low-energy (<50 GeV) galactic cosmic rays (GCRs) are fundamental to test and improve the models that describe their propagation inside the heliosphere. In particular, data spanning different <span class="hlt">solar</span> <span class="hlt">activity</span> periods, i.e., from minimum to maximum, are needed to achieve comprehensive understanding of such physical phenomena. The minimum phase between <span class="hlt">solar</span> cycles 23 and 24 was peculiarly long, extending up to the beginning of 2010 and followed by the maximum phase, reached during early 2014. In this Letter, we present proton differential spectra measured from 2010 January to 2014 February by the PAMELA experiment. For the first time the GCR proton intensity was studied over a wide energy range (0.08–50 GeV) by a single apparatus from a minimum to a maximum period of <span class="hlt">solar</span> <span class="hlt">activity</span>. The large statistics allowed the time variation to be investigated on a nearly monthly basis. Data were compared and interpreted in the context of a state-of-the-art three-dimensional model describing the GCRs propagation through the heliosphere.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://ntrs.nasa.gov/search.jsp?R=19880050091&hterms=1095&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D40%26Ntt%3D%2526%25231095','NASA-TRS'); return false;" href="https://ntrs.nasa.gov/search.jsp?R=19880050091&hterms=1095&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D40%26Ntt%3D%2526%25231095"><span><span class="hlt">Solar</span> luminosity variations in <span class="hlt">solar</span> cycle 21</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Willson, Richard C.; Hudson, H. S.</p> <p>1988-01-01</p> <p>Long-term variations in the <span class="hlt">solar</span> total irradiance found in the ACRIM I experiment on the SMM satellite have revealed a downward trend during the declining phase of <span class="hlt">solar</span> cycle 21 of the sunspot cycle, a flat period between mid-1095 and mid-1987, and an upturn in late 1987 which suggests a direct correlation of luminosity and <span class="hlt">solar</span> <span class="hlt">active</span> region population. If the upturn continues into the <span class="hlt">activity</span> maximum of <span class="hlt">solar</span> cycle 22, a relation between <span class="hlt">solar</span> <span class="hlt">activity</span> and luminosity of possible climatological significance could be ascertained. The best-fit relationship for the variation of total irradiance S with sunspot number Rz and 10-cm flux F(10) are S = 1366.82 + 7.71 x 10 to the -3rd Rz and S = 1366.27 + 8.98 x 10 to the -3rd F(10)(W/sq m). These findings could be used to approximate total irradiance variations over the periods for which these indices have been compiled.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/24616370','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/24616370"><span><span class="hlt">Influence</span> of structural variations in push-pull zinc porphyrins on photovoltaic performance of dye-sensitized <span class="hlt">solar</span> cells.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Yi, Chenyi; Giordano, Fabrizio; Cevey-Ha, Ngoc-Le; Tsao, Hoi Nok; Zakeeruddin, Shaik M; Grätzel, Michael</p> <p>2014-04-01</p> <p>We designed and synthesized two new zinc porphyrin dyes for dye-sensitized <span class="hlt">solar</span> cells (DSCs). Subtle molecular structural variation in the dyes significantly <span class="hlt">influenced</span> the performance of the DSC devices. By utilizing these dyes in combination with a cobalt-based redox electrolyte using a photoanode made of mesoporous TiO2 , we achieved a power conversion efficiency (PCE) of up to 12.0 % under AM 1.5 G (100 mW cm(-2)) simulated <span class="hlt">solar</span> light. Moreover, we obtained a high PCE of 6.4 % for solid-state dye-sensitized <span class="hlt">solar</span> cells by using 2,2',7,7'-tetrakis-(N,N-di-p-methoxyphenylamine)-9,9'-spirobifluorene as a hole-transporting material. © 2014 WILEY-VCH Verlag GmbH & Co. KGaA, Weinheim.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/19930017840','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/19930017840"><span>Investigation of <span class="hlt">solar</span> <span class="hlt">active</span> regions at high resolution by balloon flights of the <span class="hlt">solar</span> optical universal polarimeter, extended definition phase</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Tarbell, Theodore D.</p> <p>1993-01-01</p> <p>Technical studies of the feasibility of balloon flights of the former Spacelab instrument, the <span class="hlt">Solar</span> Optical Universal Polarimeter, with a modern charge-coupled device (CCD) camera, to study the structure and evolution of <span class="hlt">solar</span> <span class="hlt">active</span> regions at high resolution, are reviewed. In particular, different CCD cameras were used at ground-based <span class="hlt">solar</span> observatories with the SOUP filter, to evaluate their performance and collect high resolution images. High resolution movies of the photosphere and chromosphere were successfully obtained using four different CCD cameras. Some of this data was collected in coordinated observations with the Yohkoh satellite during May-July, 1992, and they are being analyzed scientifically along with simultaneous X-ray observations.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2014yCat..35629010U','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2014yCat..35629010U"><span>VizieR Online Data Catalog: <span class="hlt">Solar</span> <span class="hlt">activity</span> reconstructed for 3 millennia (Usoskin+, 2014)</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Usoskin, I. G.; Hulot, G.; Gallet, Y.; Roth, R.; Licht, A.; Joos, F.; Kovaltsov, G. A.; Thebault, E.; Khokhlov, A.</p> <p>2014-02-01</p> <p>Indices of <span class="hlt">solar</span> <span class="hlt">activity</span> reconstructed from 14C using the m used in the paper. Two indices are provided - the sunspot number and the cosmic ray modulation potential, both with the 95% confidence intervals. The data sets are provided with decadal resolution, thus the individual <span class="hlt">solar</span> cycles are not resolved. (2 data files).</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://ntrs.nasa.gov/search.jsp?R=20080018955&hterms=wind+monitor&qs=N%3D0%26Ntk%3DAll%26Ntx%3Dmode%2Bmatchall%26Ntt%3Dwind%2Bmonitor','NASA-TRS'); return false;" href="https://ntrs.nasa.gov/search.jsp?R=20080018955&hterms=wind+monitor&qs=N%3D0%26Ntk%3DAll%26Ntx%3Dmode%2Bmatchall%26Ntt%3Dwind%2Bmonitor"><span>The <span class="hlt">Solar</span> Wind and Geomagnetic <span class="hlt">Activity</span> as a Function of Time Relative to Corotating Interaction Regions</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>McPherron, Robert L.; Weygand, James</p> <p>2006-01-01</p> <p>Corotating interaction regions during the declining phase of the <span class="hlt">solar</span> cycle are the cause of recurrent geomagnetic storms and are responsible for the generation of high fluxes of relativistic electrons. These regions are produced by the collision of a high-speed stream of <span class="hlt">solar</span> wind with a slow-speed stream. The interface between the two streams is easily identified with plasma and field data from a <span class="hlt">solar</span> wind monitor upstream of the Earth. The properties of the <span class="hlt">solar</span> wind and interplanetary magnetic field are systematic functions of time relative to the stream interface. Consequently the coupling of the <span class="hlt">solar</span> wind to the Earth's magnetosphere produces a predictable sequence of events. Because the streams persist for many <span class="hlt">solar</span> rotations it should be possible to use terrestrial observations of past magnetic <span class="hlt">activity</span> to predict future <span class="hlt">activity</span>. Also the high-speed streams are produced by large unipolar magnetic regions on the Sun so that empirical models can be used to predict the velocity profile of a stream expected at the Earth. In either case knowledge of the statistical properties of the <span class="hlt">solar</span> wind and geomagnetic <span class="hlt">activity</span> as a function of time relative to a stream interface provides the basis for medium term forecasting of geomagnetic <span class="hlt">activity</span>. In this report we use lists of stream interfaces identified in <span class="hlt">solar</span> wind data during the years 1995 and 2004 to develop probability distribution functions for a variety of different variables as a function of time relative to the interface. The results are presented as temporal profiles of the quartiles of the cumulative probability distributions of these variables. We demonstrate that the storms produced by these interaction regions are generally very weak. Despite this the fluxes of relativistic electrons produced during those storms are the highest seen in the <span class="hlt">solar</span> cycle. We attribute this to the specific sequence of events produced by the organization of the <span class="hlt">solar</span> wind relative to the stream interfaces. We also</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2014cosp...40E.149A','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2014cosp...40E.149A"><span>MASC: Magnetic <span class="hlt">Activity</span> of the <span class="hlt">Solar</span> Corona</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Auchere, Frederic; Fineschi, Silvano; Gan, Weiqun; Peter, Hardi; Vial, Jean-Claude; Zhukov, Andrei; Parenti, Susanna; Li, Hui; Romoli, Marco</p> <p></p> <p>We present MASC, an innovative payload designed to explore the magnetic <span class="hlt">activity</span> of the <span class="hlt">solar</span> corona. It is composed of three complementary instruments: a Hard-X-ray spectrometer, a UV / EUV imager, and a Visible Light / UV polarimetric coronagraph able to measure the coronal magnetic field. The <span class="hlt">solar</span> corona is structured in magnetically closed and open structures from which slow and fast <span class="hlt">solar</span> winds are respectively released. In spite of much progress brought by two decades of almost uninterrupted observations from several space missions, the sources and acceleration mechanisms of both types are still not understood. This continuous expansion of the <span class="hlt">solar</span> atmosphere is disturbed by sporadic but frequent and violent events. Coronal mass ejections (CMEs) are large-scale massive eruptions of magnetic structures out of the corona, while <span class="hlt">solar</span> flares trace the sudden heating of coronal plasma and the acceleration of electrons and ions to high, sometimes relativistic, energies. Both phenomena are most probably driven by instabilities of the magnetic field in the corona. The relations between flares and CMEs are still not understood in terms of initiation and energy partition between large-scale motions, small-scale heating and particle acceleration. The initiation is probably related to magnetic reconnection which itself results magnetic topological changes due to e.g. flux emergence, footpoints motions, etc. Acceleration and heating are also strongly coupled since the atmospheric heating is thought to result from the impact of accelerated particles. The measurement of both physical processes and their outputs is consequently of major importance. However, despite its fundamental importance as a driver for the physics of the Sun and of the heliosphere, the magnetic field of our star’s outer atmosphere remains poorly understood. This is due in large part to the fact that the magnetic field is a very difficult quantity to measure. Our knowledge of its strength and</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017A%26A...607A..62W','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017A%26A...607A..62W"><span>Long-term <span class="hlt">influence</span> of asteroids on planet longitudes and chaotic dynamics of the <span class="hlt">solar</span> system</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Woillez, E.; Bouchet, F.</p> <p>2017-11-01</p> <p>Over timescales much longer than an orbital period, the <span class="hlt">solar</span> system exhibits large-scale chaotic behavior and can thus be viewed as a stochastic dynamical system. The aim of the present paper is to compare different sources of stochasticity in the <span class="hlt">solar</span> system. More precisely we studied the importance of the long term <span class="hlt">influence</span> of asteroids on the chaotic dynamics of the <span class="hlt">solar</span> system. We show that the effects of asteroids on planets is similar to a white noise process, when those effects are considered on a timescale much larger than the correlation time τϕ ≃ 104 yr of asteroid trajectories. We computed the timescale τe after which the effects of the stochastic evolution of the asteroids lead to a loss of information for the initial conditions of the perturbed Laplace-Lagrange secular dynamics. The order of magnitude of this timescale is precisely determined by theoretical argument, and we find that τe ≃ 104 Myr. Although comparable to the full main-sequence lifetime of the sun, this timescale is considerably longer than the Lyapunov time τI ≃ 10 Myr of the <span class="hlt">solar</span> system without asteroids. This shows that the external sources of chaos arise as a small perturbation in the stochastic secular behavior of the <span class="hlt">solar</span> system, rather due to intrinsic chaos.</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://ntrs.nasa.gov/search.jsp?R=20010059955&hterms=Qbo&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D20%26Ntt%3DQbo','NASA-TRS'); return false;" href="https://ntrs.nasa.gov/search.jsp?R=20010059955&hterms=Qbo&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D20%26Ntt%3DQbo"><span>Downward Link of <span class="hlt">Solar</span> <span class="hlt">Activity</span> Variations Through Wave Driven Equatorial Oscillations (QBO and SAO)</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Mengel, J. G.; Mayr, H. G.; Chan, K. L.; Porter, H. S.; Einaudi, Franco (Technical Monitor)</p> <p>2000-01-01</p> <p>Signatures of the 11-year <span class="hlt">solar</span> <span class="hlt">activity</span>/irradiance cycle are observed in the Quasi Biennial Oscillation (QBO) of the lower stratosphere. At these altitudes, the QBO is understood to be the result of "downward control" exerted by the wave mean flow interactions that drive the phenomenon. It is reasonable then to speculate that the QBO is a natural conduit to lower altitudes of <span class="hlt">solar</span> <span class="hlt">activity</span> variations in radiance (SAV). To test this hypothesis, we conducted experiments with a 2D version of our Numerical Spectral Model that incorporates Hines' Doppler Spread Parameterization for small-scale gravity waves (GW). To account for the SAV, we change the <span class="hlt">solar</span> heating rate on a logarithmic scale from 0.1% at the surface to 1% at 50 kin to 10% at 100 km. With the same GW flux, we then conduct numerical experiments to evaluate the magnitude of the <span class="hlt">solar</span> <span class="hlt">activity</span> irradiance effect (SAE) on the zonal circulation at low latitudes. The numerical results obtained show that, under certain conditions, the SAE is significant in the zonal circulation and does extend to lower altitudes where the SAV is small. The differences in the wind velocities can be as large as 5 m/s at 20 kin. We carried out two numerical experiments with integrations over more than 20 years: 1) With the QBO period "tuned" to be 30 months, of academic interest but instructive, the seasonal cycle in the <span class="hlt">solar</span> forcing [through the Semi-annual Oscillation (SAO)] acts as a strong pacemaker to produce a firm lock on the period and phase of the QBO. The SAE then shows up primarily as a distinct but relatively weak amplitude modulation. 2) With the QBO period between 30 and 34 (or less than 30, presumably) months, the seasonal phase lock is weak compared with (1). The SAV in the seasonal cycle then causes variations in the QBO period and phase, and this amplifies the SAE to produce relatively large variations in the wind field. We conclude that, under realistic conditions as in (2), the <span class="hlt">solar</span> seasonal forcing, with</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017SPD....4811009N','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017SPD....4811009N"><span>Science with the Expanded Owens Valley <span class="hlt">Solar</span> Array</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Nita, Gelu M.; Gary, Dale E.; Fleishman, Gregory D.; Chen, Bin; White, Stephen M.; Hurford, Gordon J.; McTiernan, James; Hickish, Jack; Yu, Sijie; Nelin, Kjell B.</p> <p>2017-08-01</p> <p>The Expanded Owens Valley <span class="hlt">Solar</span> Array (EOVSA) is a <span class="hlt">solar</span>-dedicated radio array that makes images and spectra of the full Sun on a daily basis. Our main science goals are to understand the basic physics of <span class="hlt">solar</span> <span class="hlt">activity</span>, such as how the Sun releases stored magnetic energy on timescales of seconds, and how that <span class="hlt">solar</span> <span class="hlt">activity</span>, in the form of <span class="hlt">solar</span> flares and coronal mass ejections, <span class="hlt">influences</span> the Earth and near-Earth space environment, through disruptions of communication and navigation systems, and effects on satellites and systems on the ground. The array, which is composed out of thirteen 2.1 m dishes and two 27 m dishes (used only for calibration), has a footprint of 1.1 km EW x 1.2 km NS and it is capable of producing, every second, microwave images at two polarizations and 500 science channels spanning the 1-18 GHz frequency range. Such ability to make multi-frequency images of the Sun in this broad range of frequencies, with a frequency dependent resolution ranging from ˜53” at 1 GHz to ˜3”at 18 GHz, is unique in the world. Here we present an overview of the EOVSA instrument and a first set of science-quality <span class="hlt">active</span> region and <span class="hlt">solar</span> flare images produced from data taken during April 2017.This research is supported by NSF grant AST-1615807 and NASA grant NNX14AK66G to New Jersey Institute of Technology.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://ntrs.nasa.gov/search.jsp?R=19810064399&hterms=fossils&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D80%26Ntt%3Dfossils','NASA-TRS'); return false;" href="https://ntrs.nasa.gov/search.jsp?R=19810064399&hterms=fossils&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D80%26Ntt%3Dfossils"><span>Nature of the fossil evidence - Moon and meteorites. [<span class="hlt">solar</span> <span class="hlt">activity</span> effects</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Walker, R. M.</p> <p>1980-01-01</p> <p>The nature of the fossil evidence to be found in extraterrestrial materials concerning the history of <span class="hlt">solar</span> <span class="hlt">activity</span> is reviewed. The various types of lunar rocks and meteorites containing evidence of exposure to <span class="hlt">solar</span> radiations are distinguished, including igneous rocks, breccias, glassy agglutinates, single mineral crystals, carbonaceous meteorites, and the Antarctic meteorites, some of which fell to earth as much as a million years ago. The characteristic effects of energetic particles from space in materials are then examined, including ion implantation and surface radiation damage to a depth of several hundred A by the <span class="hlt">solar</span> wind, radioactivity, electron trapping and track production induced by <span class="hlt">solar</span> flares to depths from millimeters to centimeters, and spallation due to galactic cosmic rays at depths from centimeters to meters. Complications in the interpretation of radiation exposure histories represented by dynamic surface processes, the nonsolar origin of some trapped elements, and difficulties in determining the duration and epoch of surface exposure of individual crystals are also noted.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/1990PDHO....7...80G','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/1990PDHO....7...80G"><span>The role of <span class="hlt">activity</span> complexes in the distribution of <span class="hlt">solar</span> magnetic fields.</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>García de La Rosa, J. I.; Reyes, R. C.</p> <p></p> <p>Using published data on the large-scale distribution of <span class="hlt">solar</span> <span class="hlt">activity</span>, the authors conclude that the longlived coronal holes are formed and maintained by the unbalanced magnetic flux which developes at both extremes of the complexes of <span class="hlt">activity</span>.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/22865444','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/22865444"><span>Acute myocardial infarction (AMI) (n-11026) on days of zero geomagnetic <span class="hlt">activity</span> (GMA) and the following week: differences at months of maximal and minimal <span class="hlt">solar</span> <span class="hlt">activity</span> (SA) in <span class="hlt">solar</span> cycles 23 and 24.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Stoupel, Eliyahu; Tamoshiunas, Abdonas; Radishauskas, Richardas; Bernotiene, Gailute; Abramson, Evgeny; Israelevich, Peter</p> <p>2012-01-01</p> <p>Acute myocardial infarction (AMI) is one of most common cardiovascular pathologies in the industrial world. In addition to known risk factors, environmental physical <span class="hlt">activity</span> factors such as <span class="hlt">solar</span> <span class="hlt">activity</span> (SA), geomagnetic <span class="hlt">activity</span> (GMA), and cosmic ray <span class="hlt">activity</span> (CRA) could be also involved in the timing of AMI. The aim of this study was to study AMI admissions at days of zero GMA, accompanied by high CRA, and the following week in the higher and lowest parts of <span class="hlt">solar</span> cycles 23 and 24. Patients admitted for AMI (n=11,026, 59.5% men) in years 2000-2009 at the Department of Cardiology of Lithuanian University of Medical Sciences were studied for all periods and separately for the higher part of the 11-year <span class="hlt">solar</span> <span class="hlt">activity</span> in cycles 23 and 24 (2000-2007) and its lowest part (2008-2009). Admissions at day of zero GMA as well as 1, 2, 6, and 7 days after zero-GMA day were compared. At high SA, zero-GMA days were rare and isolated (36 in years 2000-2007). They have been followed by significant increase in admissions on the following days. In the two lowest years of SA 2008-2009, there were 57 days of zero GMA, many of which were consecutive and in groups. For the whole <span class="hlt">solar</span> cycle, there was a more gradual increase in AMI from 1 to 2 days after zero-GMA day, and there were significantly higher AMI admissions at 6 days after the first zero-GMA day (p=0.018). Zero-GMA/high-neutron <span class="hlt">activity</span> is followed by increase in AMI admissions at the days that follow. The effects are different at high and low parts of the 11-year <span class="hlt">solar</span> cycle.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2006cosp...36..876P','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2006cosp...36..876P"><span>Possible space weather <span class="hlt">influence</span> on the Earth wheat prices</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Pustil'Nik, L.; Yom Din, G.; Dorman, L.</p> <p></p> <p>We present development of our study of possible <span class="hlt">influence</span> of space weather modulated by cycle of <span class="hlt">solar</span> <span class="hlt">activity</span> on the price bursts in the Earth markets In our previous works 1 2 we showed that correspondent response may have place in the specific locations characterized by a high sensitivity of the weather cloudiness in particular to cosmic ray variation b risk zone agriculture c isolated wheat market with limited external supply of agriculture production We showed that in this situation we may wait specific price burst reaction on unfavorable phase of <span class="hlt">solar</span> <span class="hlt">activity</span> and space weather what lead to corresponding abnormalities in the local weather and next crop failure We showed that main types of manifestation of this connection are a Distribution of intervals between price bursts must be like to the distribution of intervals between correspondent extremes of <span class="hlt">solar</span> <span class="hlt">activity</span> minimums or maximums b price asymmetry between opposite states of <span class="hlt">solar</span> <span class="hlt">activity</span> price in the one type of <span class="hlt">activity</span> state is systematically higher then in the opposite one We showed in our previous publications that this <span class="hlt">influence</span> in interval distribution is detected with high reliability in Mediaeval England 1250-1700 both for wheat prices and price of consumables basket We showed that for period of Maunder Minimum price asymmetry of wheat prices observed all prices in minimum state of <span class="hlt">solar</span> <span class="hlt">activity</span> was higher the prices in the next maximum state We showed later that this price asymmetry had place in 20-th century in USA durum prices too In</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2016EGUGA..1811429K','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2016EGUGA..1811429K"><span>On searching applicants for mechanism of <span class="hlt">solar</span>-lithosphere relations</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Kairatkyzy, Dina; Andreyev, Alexey; Zhumabayeva, Saltanat; Seraliyev, Alibek</p> <p>2016-04-01</p> <p>It is <span class="hlt">actively</span> discussed at present a question on possible <span class="hlt">influence</span> of <span class="hlt">solar</span> <span class="hlt">activity</span> (high-speed <span class="hlt">solar</span> wind streams bearing the "frozen" magnetic field lines of the Sun) on the stress status of the lithosphere and, consequently, on the Earth's seismic <span class="hlt">activity</span> (e.g. Zhang, 1998, Acta Seismologica Sinica; Khachikyan et al., EGU2016-2754-1; IUGG2015-3132). There are at least two ideas on possible applicants for physical mechanism of <span class="hlt">solar</span>-lithosphere relations: (i) - the muons of cosmic rays, which can penetrate the Earth's crust to a depth of at least the first ten kilometers and in tense seismic environment generate nuclear-electromagnetic cascade which energy can be a trigger of earthquake (Tsarev and Chechin, 1988, Preprint № 179, Physical Institute after Lebedev, Moscow); (ii) - the geomagnetic storms (Sobolev et al., 1998, Physics of the Earth #7) when the high-frequency oscillations of the geomagnetic field during the main phase of the storm generate significant induction currents which electric energy entering into the crust can be converted into mechanical energy increasing the stress status of the lithosphere (Sobolev and Demin, Mechano-electric phenomena into the Earth. M . Nauka. 1980). Besides this, among the possible cosmogenic factors changing the stress state of the lithosphere, could be the variation of the angular velocity of rotation of the Earth (e.g. Bostrom, 2000. Tectonic consequence of the Earth's Rotation), if it depends on <span class="hlt">solar</span> <span class="hlt">activity</span> variations. More of 50 years ago, Munk and Donald (The Rotation of the Earth, Cambrige University Press, 1960) suggested that the interaction between <span class="hlt">solar</span> wind and geomagnetic field would probably <span class="hlt">influence</span> the short period variation of angular velocity of the Earth. In this work, we check up this suggestion on the base of very precise data on the length of day (LOD) from 1986 to the present, which are presented by the International Earth Rotation and Reference Systems Service (IERS). Using the methods</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017SoPh..292..159K','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017SoPh..292..159K"><span>Non-neutralized Electric Currents in <span class="hlt">Solar</span> <span class="hlt">Active</span> Regions and Flare Productivity</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Kontogiannis, Ioannis; Georgoulis, Manolis K.; Park, Sung-Hong; Guerra, Jordan A.</p> <p>2017-11-01</p> <p>We explore the association of non-neutralized currents with <span class="hlt">solar</span> flare occurrence in a sizable sample of observations, aiming to show the potential of such currents in <span class="hlt">solar</span> flare prediction. We used the high-quality vector magnetograms that are regularly produced by the Helioseismic Magnetic Imager, and more specifically, the Space weather HMI <span class="hlt">Active</span> Region Patches (SHARP). Through a newly established method that incorporates detailed error analysis, we calculated the non-neutralized currents contained in <span class="hlt">active</span> regions (AR). Two predictors were produced, namely the total and the maximum unsigned non-neutralized current. Both were tested in AR time-series and a representative sample of point-in-time observations during the interval 2012 - 2016. The average values of non-neutralized currents in flaring <span class="hlt">active</span> regions are higher by more than an order of magnitude than in non-flaring regions and correlate very well with the corresponding flare index. The temporal evolution of these parameters appears to be connected to physical processes, such as flux emergence and/or magnetic polarity inversion line formation, that are associated with increased <span class="hlt">solar</span> flare <span class="hlt">activity</span>. Using Bayesian inference of flaring probabilities, we show that the total unsigned non-neutralized current significantly outperforms the total unsigned magnetic flux and other well-established current-related predictors. It therefore shows good prospects for inclusion in an operational flare-forecasting service. We plan to use the new predictor in the framework of the FLARECAST project along with other highly performing predictors.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2012P%26SS...61...15Y','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2012P%26SS...61...15Y"><span><span class="hlt">Influence</span> of upstream <span class="hlt">solar</span> wind on thermospheric flows at Jupiter</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Yates, J. N.; Achilleos, N.; Guio, P.</p> <p>2012-02-01</p> <p>The coupling of Jupiter's magnetosphere and ionosphere plays a vital role in creating its auroral emissions. The strength of these emissions is dependent on the difference in speed of the rotational flows within Jupiter's high-latitude thermosphere and the planet's magnetodisc. Using an azimuthally symmetric global circulation model, we have simulated how upstream <span class="hlt">solar</span> wind conditions affect the energy and direction of atmospheric flows. In order to simulate the effect of a varying dynamic pressure in the upstream <span class="hlt">solar</span> wind, we calculated three magnetic field profiles representing compressed, averaged and expanded ‘middle’ magnetospheres. These profiles were then used to solve for the angular velocity of plasma in the magnetosphere. This angular velocity determines the strength of currents flowing between the ionosphere and magnetosphere. We examine the <span class="hlt">influence</span> of variability in this current system upon the global winds and energy inputs within the Jovian thermosphere. We find that the power dissipated by Joule heating and ion drag increases by ∼190% and ∼185% from our compressed to expanded model respectively. We investigated the effect of exterior boundary conditions on our models and found that by reducing the radial current at the outer edge of the magnetodisc, we also limit the thermosphere's ability to transmit angular momentum to this region.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/27220094','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/27220094"><span><span class="hlt">Solar</span> and atmospheric forcing on mountain lakes.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Luoto, Tomi P; Nevalainen, Liisa</p> <p>2016-10-01</p> <p>We investigated the <span class="hlt">influence</span> of long-term external forcing on aquatic communities in Alpine lakes. Fossil microcrustacean (Cladocera) and macrobenthos (Chironomidae) community variability in four Austrian high-altitude lakes, determined as ultra-sensitive to climate change, were compared against records of air temperature, North Atlantic Oscillation (NAO) and <span class="hlt">solar</span> forcing over the past ~400years. Summer temperature variability affected both aquatic invertebrate groups in all study sites. The <span class="hlt">influence</span> of NAO and <span class="hlt">solar</span> forcing on aquatic invertebrates was also significant in the lakes except in the less transparent lake known to have remained uniformly cold during the past centuries due to summertime snowmelt input. The results suggest that external forcing plays an important role in these pristine ecosystems through their impacts on limnology of the lakes. Not only does the air temperature variability <span class="hlt">influence</span> the communities but also larger-scale external factors related to atmospheric circulation patterns and <span class="hlt">solar</span> <span class="hlt">activity</span> cause long-term changes in high-altitude aquatic ecosystems, through their connections to hydroclimatic conditions and light environment. These findings are important in the assessment of climate change impacts on aquatic ecosystems and in greater understanding of the consequences of external forcing on lake ontogeny. Copyright © 2016 Elsevier B.V. All rights reserved.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2018Ge%26Ae..58..169K','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2018Ge%26Ae..58..169K"><span>Galactic Cosmic Ray Intensity in the Upcoming Minimum of the <span class="hlt">Solar</span> <span class="hlt">Activity</span> Cycle</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Krainev, M. B.; Bazilevskaya, G. A.; Kalinin, M. S.; Svirzhevskaya, A. K.; Svirzhevskii, N. S.</p> <p>2018-03-01</p> <p>During the prolonged and deep minimum of <span class="hlt">solar</span> <span class="hlt">activity</span> between cycles 23 and 24, an unusual behavior of the heliospheric characteristics and increased intensity of galactic cosmic rays (GCRs) near the Earth's orbit were observed. The maximum of the current <span class="hlt">solar</span> cycle 24 is lower than the previous one, and the decline in <span class="hlt">solar</span> and, therefore, heliospheric <span class="hlt">activity</span> is expected to continue in the next cycle. In these conditions, it is important for an understanding of the process of GCR modulation in the heliosphere, as well as for applied purposes (evaluation of the radiation safety of planned space flights, etc.), to estimate quantitatively the possible GCR characteristics near the Earth in the upcoming <span class="hlt">solar</span> minimum ( 2019-2020). Our estimation is based on the prediction of the heliospheric characteristics that are important for cosmic ray modulation, as well as on numeric calculations of GCR intensity. Additionally, we consider the distribution of the intensity and other GCR characteristics in the heliosphere and discuss the intercycle variations in the GCR characteristics that are integral for the whole heliosphere (total energy, mean energy, and charge).</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://ntrs.nasa.gov/search.jsp?R=20070034012&hterms=dynamo&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D10%26Ntt%3Ddynamo','NASA-TRS'); return false;" href="https://ntrs.nasa.gov/search.jsp?R=20070034012&hterms=dynamo&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D10%26Ntt%3Ddynamo"><span><span class="hlt">Solar</span> Cycle 24 and the <span class="hlt">Solar</span> Dynamo</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Pesnell, W. D.; Schatten, K.</p> <p>2007-01-01</p> <p>We will discuss the polar field precursor method for <span class="hlt">solar</span> <span class="hlt">activity</span> prediction, which predicts cycle 24 will be significantly lower than recent <span class="hlt">activity</span> cycles, and some new ideas rejuvenating Babcock's shallow surface dynamo. The polar field precursor method is based on Babcock and Leighton's dynamo models wherein the polar field at <span class="hlt">solar</span> minimum plays a major role in generating the next cycle's toroidal field and sunspots. Thus, by examining the polar fields of the Sun near <span class="hlt">solar</span> minimum, a forecast for the next cycle's <span class="hlt">activity</span> is obtained. With the current low value for the Sun's polar fields, this method predicts <span class="hlt">solar</span> cycle 24 will be one of the lowest in recent times, with smoothed F10.7 radio flux values peaking near 135 plus or minus 35 (2 sigma), in the 2012-2013 timeframe (equivalent to smoothed Rz near 80 plus or minus 35 [2 sigma]). One may have to consider <span class="hlt">solar</span> <span class="hlt">activity</span> as far back as the early 20th century to find a cycle of comparable magnitude. We discuss unusual behavior in the Sun's polar fields that support this prediction. Normally, the <span class="hlt">solar</span> precursor method is consistent with the geomagnetic precursor method, wherein geomagnetic variations are thought to be a good measure of the Sun's polar field strength. Because of the unusual polar field, the Earth does not appear to be currently bathed in the Sun's extended polar field (the interplanetary field), hence negating the primal cause behind the geomagnetic precursor technique. We also discuss how percolation may support Babcock's original shallow <span class="hlt">solar</span> dynamo. In this process ephemeral regions from the <span class="hlt">solar</span> magnetic carpet, guided by shallow surface fields, may collect to form pores and sunspots.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.osti.gov/biblio/22521773-magnetic-flux-transport-long-term-evolution-solar-active-regions','SCIGOV-STC'); return false;" href="https://www.osti.gov/biblio/22521773-magnetic-flux-transport-long-term-evolution-solar-active-regions"><span>MAGNETIC FLUX TRANSPORT AND THE LONG-TERM EVOLUTION OF <span class="hlt">SOLAR</span> <span class="hlt">ACTIVE</span> REGIONS</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>Ugarte-Urra, Ignacio; Upton, Lisa; Warren, Harry P.</p> <p>2015-12-20</p> <p>With multiple vantage points around the Sun, <span class="hlt">Solar</span> Terrestrial Relations Observatory (STEREO) and <span class="hlt">Solar</span> Dynamics Observatory imaging observations provide a unique opportunity to view the <span class="hlt">solar</span> surface continuously. We use He ii 304 Å data from these observatories to isolate and track ten <span class="hlt">active</span> regions and study their long-term evolution. We find that <span class="hlt">active</span> regions typically follow a standard pattern of emergence over several days followed by a slower decay that is proportional in time to the peak intensity in the region. Since STEREO does not make direct observations of the magnetic field, we employ a flux-luminosity relationship to infermore » the total unsigned magnetic flux evolution. To investigate this magnetic flux decay over several rotations we use a surface flux transport model, the Advective Flux Transport model, that simulates convective flows using a time-varying velocity field and find that the model provides realistic predictions when information about the <span class="hlt">active</span> region's magnetic field strength and distribution at peak flux is available. Finally, we illustrate how 304 Å images can be used as a proxy for magnetic flux measurements when magnetic field data is not accessible.« less</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/19900018845','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/19900018845"><span>Middle Atmosphere Program. Handbook for MAP, volume 29. Part 1: Extended Abstracts, International Symposium on <span class="hlt">Solar</span> <span class="hlt">Activity</span> Forcing of the Middle Atmosphere. Part 2: MASH Workshop</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Lastovicka, Jan (Editor); Miles, Thomas (Editor); Oneill, Alan (Editor)</p> <p>1989-01-01</p> <p>The proceedings of the symposium is presented. Eight different sessions were presented: (1) Papers generally related to the subject; (2) Papers on the <span class="hlt">influence</span> of the Quasi Biennial Oscillation; (3) Papers on the <span class="hlt">influence</span> of the <span class="hlt">solar</span> electromagnetic radiation variability; (4) Papers on the <span class="hlt">solar</span> wind and high energy particle <span class="hlt">influence</span>; (5) Papers on atmospheric circulation; (6) Papers on atmospheric electricity; (7) Papers on lower ionospheric variability; and (8) <span class="hlt">Solar</span> posters, which are not included in this compilation.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/20140006613','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/20140006613"><span>Deep <span class="hlt">Solar</span> <span class="hlt">Activity</span> Minimum 2007-2009: <span class="hlt">Solar</span> Wind Properties and Major Effects on the Terrestrial Magnetosphere</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Farrugia, C. J.; Harris, B.; Leitner, M.; Moestl, C.; Galvin, A. B.; Simunac, K. D. C.; Torbert, R. B.; Temmer, M. B.; Veronig, A. M.; Erkaev, N. V.; <a style="text-decoration: none; " href="javascript:void(0); " onClick="displayelement('author_20140006613'); toggleEditAbsImage('author_20140006613_show'); toggleEditAbsImage('author_20140006613_hide'); "> <img style="display:inline; width:12px; height:12px; " src="images/arrow-up.gif" width="12" height="12" border="0" alt="hide" id="author_20140006613_show"> <img style="width:12px; height:12px; display:none; " src="images/arrow-down.gif" width="12" height="12" border="0" alt="hide" id="author_20140006613_hide"></p> <p>2012-01-01</p> <p>We discuss the temporal variations and frequency distributions of <span class="hlt">solar</span> wind and interplanetary magnetic field parameters during the <span class="hlt">solar</span> minimum of 2007 - 2009 from measurements returned by the IMPACT and PLASTIC instruments on STEREO-A.We find that the density and total field strength were significantly weaker than in the previous minimum. The Alfven Mach number was higher than typical. This reflects the weakness of magnetohydrodynamic (MHD) forces, and has a direct effect on the <span class="hlt">solar</span> wind-magnetosphere interactions.We then discuss two major aspects that this weak <span class="hlt">solar</span> <span class="hlt">activity</span> had on the magnetosphere, using data from Wind and ground-based observations: i) the dayside contribution to the cross-polar cap potential (CPCP), and ii) the shapes of the magnetopause and bow shock. For i) we find a low interplanetary electric field of 1.3+/-0.9 mV/m and a CPCP of 37.3+/-20.2 kV. The auroral <span class="hlt">activity</span> is closely correlated to the prevalent stream-stream interactions. We suggest that the Alfven wave trains in the fast streams and Kelvin-Helmholtz instability were the predominant agents mediating the transfer of <span class="hlt">solar</span> wind momentum and energy to the magnetosphere during this three-year period. For ii) we determine 328 magnetopause and 271 bow shock crossings made by Geotail, Cluster 1, and the THEMIS B and C spacecraft during a three-month interval when the daily averages of the magnetic and kinetic energy densities attained their lowest value during the three years under survey.We use the same numerical approach as in Fairfield's empirical model and compare our findings with three magnetopause models. The stand-off distance of the subsolar magnetopause and bow shock were 11.8 R(sub E) and 14.35 R(sub E), respectively. When comparing with Fairfield's classic result, we find that the subsolar magnetosheath is thinner by approx. 1 R(sub E). This is mainly due to the low dynamic pressure which results in a sunward shift of the magnetopause. The magnetopause is more flared</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2008AGUFMPP31B1484Y','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2008AGUFMPP31B1484Y"><span>Fluctuations in Tree Ring Cellulose d18O during the Little Ice Age Correlate with <span class="hlt">Solar</span> <span class="hlt">Activity</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Yamaguchi, Y. T.; Yokoyama, Y.; Miyahara, H.; Nakatsuka, T.</p> <p>2008-12-01</p> <p>The Maunder Minimum (AD1645-1715), when sunspots became exceedingly rare, is known to coincide with the coldest period during the Little Ice Age. This is a useful period to investigate possible linkage between <span class="hlt">solar</span> <span class="hlt">activity</span> and climate because variation in <span class="hlt">solar</span> <span class="hlt">activity</span> was different from that of today. The <span class="hlt">solar</span> cycle length was longer (14 and 28 years) than that of today (11 and 22 years) hence any climate archives that have similar periodic changes could be separated from other internal climate forcing. We have reported that Greenland temperature variations coincided with decadal-scale variability in <span class="hlt">solar</span> <span class="hlt">activity</span> during the Maunder Minimum (Miyahara et al. 2008). Here we report interannual and intra-annual relative humidity (RH) variations in central Japan during that period, using tree ring cellulose d18O in a 382-year-old Japanese cedar tree (Cryptomeria japonica). The isotopic composition of tree rings can be a powerful tool to study the relationship between <span class="hlt">solar</span> <span class="hlt">activity</span> and climate, because we can directly compare <span class="hlt">solar</span> <span class="hlt">activity</span> (D14C) and climate (d18O) with little dating error. The climate proxy obtained using tree ring cellulose d18O is correlated both negatively and positively with RH and d18O in precipitation, respectively. Since d18O in precipitation is negatively correlated with the amount of precipitation in the monsoon area, tree ring cellulose d18O can be a reliable proxy for past RH and/or amount of precipitation in the area of the interest. Tree ring cellulose d18O of the cedar tree during AD1938-1998 in fact correlates significantly with the mean RH in June in central Japan. Tree ring d18O inferred RH variability during the Maunder Minimum shows distinct high RH spikes with an approximate 14-year quasiperiodicity. All nine <span class="hlt">solar</span> minima during AD1640-1756 deduced from tree ring D14C coincided with high RH spikes, and seven of which coincided within 1-year. Interannual RH variations also coincided with Greenland temperature during this</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/19930003826','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/19930003826"><span><span class="hlt">Solar</span> prediction analysis</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Smith, Jesse B.</p> <p>1992-01-01</p> <p><span class="hlt">Solar</span> <span class="hlt">Activity</span> prediction is essential to definition of orbital design and operational environments for space flight. This task provides the necessary research to better understand <span class="hlt">solar</span> predictions being generated by the <span class="hlt">solar</span> community and to develop improved <span class="hlt">solar</span> prediction models. The contractor shall provide the necessary manpower and facilities to perform the following tasks: (1) review, evaluate, and assess the time evolution of the <span class="hlt">solar</span> cycle to provide probable limits of <span class="hlt">solar</span> cycle behavior near maximum end during the decline of <span class="hlt">solar</span> cycle 22, and the forecasts being provided by the <span class="hlt">solar</span> community and the techniques being used to generate these forecasts; and (2) develop and refine prediction techniques for short-term <span class="hlt">solar</span> behavior flare prediction within <span class="hlt">solar</span> <span class="hlt">active</span> regions, with special emphasis on the correlation of magnetic shear with flare occurrence.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017SPD....4810106M','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017SPD....4810106M"><span>The Role of Small-Scale Processes in <span class="hlt">Solar</span> <span class="hlt">Active</span> Region Decay</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Meyer, Karen; Mackay, Duncan</p> <p>2017-08-01</p> <p><span class="hlt">Active</span> regions are locations of intense magnetic <span class="hlt">activity</span> on the Sun, whose evolution can result in highly energetic eruptive phenomena such as <span class="hlt">solar</span> flares and coronal mass ejections (CMEs). Therefore, fast and accurate simulation of their evolution and decay is essential in the prediction of Space Weather events. In this talk we present initial results from our new model for the photospheric evolution of <span class="hlt">active</span> region magnetic fields. Observations show that small-scale processes appear to play a role in the dispersal and decay of <span class="hlt">solar</span> <span class="hlt">active</span> regions, for example through cancellation at the boundary of sunspot outflows and erosion of flux by surrounding convective cells. Our <span class="hlt">active</span> region model is coupled to our existing model for the evolution of small-scale photospheric magnetic features. Focusing first on the <span class="hlt">active</span> region decay phase, we consider the evolution of its magnetic field due to both large-scale (e.g. differential rotation) and small-scale processes, such as its interaction with surrounding small-scale magnetic features and convective flows.This project is funded by The Carnegie Trust for the Universities of Scotland, through their Research Incentives Grant scheme.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://ntrs.nasa.gov/search.jsp?R=20070031229&hterms=Qbo&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D10%26Ntt%3DQbo','NASA-TRS'); return false;" href="https://ntrs.nasa.gov/search.jsp?R=20070031229&hterms=Qbo&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D10%26Ntt%3DQbo"><span>QBO as Potential Amplifier of <span class="hlt">Solar</span> Cycle <span class="hlt">Influence</span></span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Mayr, Hans G.; Mangel, John G.; Wolff, Charles L.; Porter, Hayden S.</p> <p>2006-01-01</p> <p>The <span class="hlt">solar</span> cycle (SC) effect in the lower atmosphere has been linked observationally to the quasi-biennial oscillation (QBO) of the zonal circulation. Salby and Callaghan (2000) in particular analyzed the QBO covering more than 40 years and found that it contains a large SC signature at 20 km. We discuss a 3D study in which we simulate the QBO under the <span class="hlt">influence</span> of the SC. For a SC period of 10 years, the relative amplitude of radiative forcing is taken to vary with height: 0.2% (surface), 2% (50 km), 20% (100 km and above). This model produces in the lower stratosphere a relatively large modulation of the QBO, which appears to come from the SC and qualitatively agrees with the observations. The modulation of the QBO, with constant phase relative to the SC, is shown to persist at least for 50 years, and it is induced by a SC modulated annual oscillation that is hemispherically symmetric and confined to low latitudes.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2018JIEIB..99..301S','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2018JIEIB..99..301S"><span>Single-Phase Single-Stage Grid Tied <span class="hlt">Solar</span> PV System with <span class="hlt">Active</span> Power Filtering Using Power Balance Theory</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Singh, Yashi; Hussain, Ikhlaq; Singh, Bhim; Mishra, Sukumar</p> <p>2018-06-01</p> <p>In this paper, power quality features such as harmonics mitigation, power factor correction with <span class="hlt">active</span> power filtering are addressed in a single-stage, single-phase <span class="hlt">solar</span> photovoltaic (PV) grid tied system. The Power Balance Theory (PBT) with perturb and observe based maximum power point tracking algorithm is proposed for the mitigation of power quality problems in a <span class="hlt">solar</span> PV grid tied system. The <span class="hlt">solar</span> PV array is interfaced to a single phase AC grid through a Voltage Source Converter (VSC), which provides <span class="hlt">active</span> power flow from a <span class="hlt">solar</span> PV array to the grid as well as to the load and it performs harmonics mitigation using PBT based control. The <span class="hlt">solar</span> PV array power varies with sunlight and due to this, the <span class="hlt">solar</span> PV grid tied VSC works only 8-10 h per day. At night, when PV power is zero, the VSC works as an <span class="hlt">active</span> power filter for power quality improvement, and the load <span class="hlt">active</span> power is delivered by the grid to the load connected at the point of common coupling. This increases the effective utilization of a VSC. The system is modelled and simulated using MATLAB and simulated responses of the system at nonlinear loads and varying environmental conditions are also validated experimentally on a prototype developed in the laboratory.</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/2018JIEIB.tmp...25S','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2018JIEIB.tmp...25S"><span>Single-Phase Single-Stage Grid Tied <span class="hlt">Solar</span> PV System with <span class="hlt">Active</span> Power Filtering Using Power Balance Theory</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Singh, Yashi; Hussain, Ikhlaq; Singh, Bhim; Mishra, Sukumar</p> <p>2018-03-01</p> <p>In this paper, power quality features such as harmonics mitigation, power factor correction with <span class="hlt">active</span> power filtering are addressed in a single-stage, single-phase <span class="hlt">solar</span> photovoltaic (PV) grid tied system. The Power Balance Theory (PBT) with perturb and observe based maximum power point tracking algorithm is proposed for the mitigation of power quality problems in a <span class="hlt">solar</span> PV grid tied system. The <span class="hlt">solar</span> PV array is interfaced to a single phase AC grid through a Voltage Source Converter (VSC), which provides <span class="hlt">active</span> power flow from a <span class="hlt">solar</span> PV array to the grid as well as to the load and it performs harmonics mitigation using PBT based control. The <span class="hlt">solar</span> PV array power varies with sunlight and due to this, the <span class="hlt">solar</span> PV grid tied VSC works only 8-10 h per day. At night, when PV power is zero, the VSC works as an <span class="hlt">active</span> power filter for power quality improvement, and the load <span class="hlt">active</span> power is delivered by the grid to the load connected at the point of common coupling. This increases the effective utilization of a VSC. The system is modelled and simulated using MATLAB and simulated responses of the system at nonlinear loads and varying environmental conditions are also validated experimentally on a prototype developed in the laboratory.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://ntrs.nasa.gov/search.jsp?R=19900049510&hterms=Butterfly&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D60%26Ntt%3DButterfly','NASA-TRS'); return false;" href="https://ntrs.nasa.gov/search.jsp?R=19900049510&hterms=Butterfly&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D60%26Ntt%3DButterfly"><span>A <span class="hlt">solar</span> cycle timing predictor - The latitude of <span class="hlt">active</span> regions</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Schatten, Kenneth H.</p> <p>1990-01-01</p> <p>A 'Spoerer butterfly' method is used to examine <span class="hlt">solar</span> cycle 22. It is shown from the latitude of <span class="hlt">active</span> regions that the cycle can now be expected to peak near November 1989 + or - 8 months, basically near the latter half of 1989.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2016EGUGA..18.2839Y','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2016EGUGA..18.2839Y"><span>({The) <span class="hlt">Solar</span> System Large Planets <span class="hlt">influence</span> on a new Maunder Miniμm}</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Yndestad, Harald; Solheim, Jan-Erik</p> <p>2016-04-01</p> <p>In 1890´s G. Spörer and E. W. Maunder (1890) reported that the <span class="hlt">solar</span> <span class="hlt">activity</span> stopped in a period of 70 years from 1645 to 1715. Later a reconstruction of the <span class="hlt">solar</span> <span class="hlt">activity</span> confirms the grand minima Maunder (1640-1720), Spörer (1390-1550), Wolf (1270-1340), and the minima Oort (1010-1070) and Dalton (1785-1810) since the year 1000 A.D. (Usoskin et al. 2007). These minimum periods have been associated with less irradiation from the Sun and cold climate periods on Earth. An identification of a three grand Maunder type periods and two Dalton type periods in a period thousand years, indicates that sooner or later there will be a colder climate on Earth from a new Maunder- or Dalton- type period. The cause of these minimum periods, are not well understood. An expected new Maunder-type period is based on the properties of <span class="hlt">solar</span> variability. If the <span class="hlt">solar</span> variability has a deterministic element, we can estimate better a new Maunder grand minimum. A random <span class="hlt">solar</span> variability can only explain the past. This investigation is based on the simple idea that if the <span class="hlt">solar</span> variability has a deterministic property, it must have a deterministic source, as a first cause. If this deterministic source is known, we can compute better estimates the next expected Maunder grand minimum period. The study is based on a TSI ACRIM data series from 1700, a TSI ACRIM data series from 1000 A.D., sunspot data series from 1611 and a <span class="hlt">Solar</span> Barycenter orbit data series from 1000. The analysis method is based on a wavelet spectrum analysis, to identify stationary periods, coincidence periods and their phase relations. The result shows that the TSI variability and the sunspots variability have deterministic oscillations, controlled by the large planets Jupiter, Uranus and Neptune, as the first cause. A deterministic model of TSI variability and sunspot variability confirms the known minimum and grand minimum periods since 1000. From this deterministic model we may expect a new Maunder type sunspot</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017SoPh..292..122K','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017SoPh..292..122K"><span><span class="hlt">Solar</span>-Cycle Variation of Subsurface-Flow Divergence: A Proxy of Magnetic <span class="hlt">Activity</span>?</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Komm, R.; Howe, R.; Hill, F.</p> <p>2017-09-01</p> <p>We study the <span class="hlt">solar</span>-cycle variation of subsurface flows from the surface to a depth of 16 Mm. We have analyzed Global Oscillation Network Group (GONG) Dopplergrams with a ring-diagram analysis covering about 15 years and Helioseismic and Magnetic Imager (HMI) Dopplergrams covering more than 6 years. After subtracting the average rotation rate and meridional flow, we have calculated the divergence of the horizontal residual flows from the maximum of <span class="hlt">Solar</span> Cycle 23 through the declining phase of Cycle 24. The subsurface flows are mainly divergent at quiet regions and convergent at locations of high magnetic <span class="hlt">activity</span>. The relationship is essentially linear between divergence and magnetic <span class="hlt">activity</span> at all <span class="hlt">activity</span> levels at depths shallower than about 10 Mm. At greater depths, the relationship changes sign at locations of high <span class="hlt">activity</span>; the flows are increasingly divergent at locations with a magnetic <span class="hlt">activity</span> index (MAI) greater than about 24 G. The flows are more convergent by about a factor of two during the rising phase of Cycle 24 than during the declining phase of Cycle 23 at locations of medium and high <span class="hlt">activity</span> (about 10 to 40 G MAI) from the surface to at least 10 Mm. The subsurface divergence pattern of <span class="hlt">Solar</span> Cycle 24 first appears during the declining phase of Cycle 23 and is present during the extended minimum. It appears several years before the magnetic pattern of the new cycle is noticeable in synoptic maps. Using linear regression, we estimate the amount of magnetic <span class="hlt">activity</span> that would be required to generate the precursor pattern and find that it should be almost twice the amount of <span class="hlt">activity</span> that is observed.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/19800021766','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/19800021766"><span><span class="hlt">Influence</span> of magnetic pressure on stellar structure: A Mechanism for <span class="hlt">solar</span> variability</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Schatten, K. H.; Endal, A. S.</p> <p>1980-01-01</p> <p>A physical mechanism is proposed that couples the Sun's dynamo magnetic field to its gravitational potential energy. The mechanism involves the isotropic field pressure resulting in a lifting force on the convective envelope, thereby raising its potential energy. Decay of the field due to <span class="hlt">solar</span> <span class="hlt">activity</span> allows the envelop to subside and releases this energy, which can augment the otherwise steady <span class="hlt">solar</span> luminosity. Equations are developed and applied to the Sun for several field configurations. The best estimate model suggests that uniform luminosity variations as large as 0.02% for half a sunspot cycle may occur. Brief temporal variations or the rotation of spatial structures could allow larger excursions in the energy released.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2014EGUGA..1616241V','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2014EGUGA..1616241V"><span>Possible external sources of terrestrial cloud cover variability: the <span class="hlt">solar</span> wind</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Voiculescu, Mirela; Usoskin, Ilya; Condurache-Bota, Simona</p> <p>2014-05-01</p> <p>Cloud cover plays an important role in the terrestrial radiation budget. The possible <span class="hlt">influence</span> of the <span class="hlt">solar</span> <span class="hlt">activity</span> on cloud cover is still an open question with contradictory answers. An extraterrestrial factor potentially affecting the cloud cover is related to fields associated with <span class="hlt">solar</span> wind. We focus here on a derived quantity, the interplanetary electric field (IEF), defined as the product between the <span class="hlt">solar</span> wind speed and the meridional component, Bz, of the interplanetary magnetic field (IMF) in the Geocentric <span class="hlt">Solar</span> Magnetospheric (GSM) system. We show that cloud cover at mid-high latitudes systematically correlates with positive IEF, which has a clear energetic input into the atmosphere, but not with negative IEF, in general agreement with predictions of the global electric circuit (GEC)-related mechanism. Since the IEF responds differently to <span class="hlt">solar</span> <span class="hlt">activity</span> than, for instance, cosmic ray flux or <span class="hlt">solar</span> irradiance, we also show that such a study allows distinguishing one <span class="hlt">solar</span>-driven mechanism of cloud evolution, via the GEC, from others. We also present results showing that the link between cloud cover and IMF varies depending on composition and altitude of clouds.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://ntrs.nasa.gov/search.jsp?R=19910044882&hterms=activity+Physics&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D70%26Ntt%3Dactivity%2BPhysics','NASA-TRS'); return false;" href="https://ntrs.nasa.gov/search.jsp?R=19910044882&hterms=activity+Physics&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D70%26Ntt%3Dactivity%2BPhysics"><span>The <span class="hlt">solar</span> cycle variation of the rates of CMEs and related <span class="hlt">activity</span></span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Webb, David F.</p> <p>1991-01-01</p> <p>Coronal mass ejections (CMEs) are an important aspect of the physics of the corona and heliosphere. This paper presents results of a study of occurrence frequencies of CMEs and related <span class="hlt">activity</span> tracers over more than a complete <span class="hlt">solar</span> <span class="hlt">activity</span> cycle. To properly estimate occurrence rates, observed CME rates must be corrected for instrument duty cycles, detection efficiencies away from the skyplane, mass detection thresholds, and geometrical considerations. These corrections are evaluated using CME data from 1976-1989 obtained with the Skylab, SMM and SOLWIND coronagraphs and the Helios-2 photometers. The major results are: (1) the occurrence rate of CMEs tends to track the <span class="hlt">activity</span> cycle in both amplitude and phase; (2) the corrected rates from different instruments are reasonably consistent; and (3) over the long term, no one class of <span class="hlt">solar</span> <span class="hlt">activity</span> tracer is better correlated with CME rate than any other (with the possible exception of type II bursts).</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017SPIE10420E..1ND','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017SPIE10420E..1ND"><span>Relative phase asynchrony and long-range correlation of long-term <span class="hlt">solar</span> magnetic <span class="hlt">activity</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Deng, Linhua</p> <p>2017-07-01</p> <p>Statistical signal processing is one of the most important tasks in a large amount of areas of scientific studies, such as astrophysics, geophysics, and space physics. Phase recurrence analysis and long-range persistence are the two dynamical structures of the underlying processes for the given natural phenomenon. Linear and nonlinear time series analysis approaches (cross-correlation analysis, cross-recurrence plot, wavelet coherent transform, and Hurst analysis) are combined to investigate the relative phase interconnection and long-range correlation between <span class="hlt">solar</span> <span class="hlt">activity</span> and geomagnetic <span class="hlt">activity</span> for the time interval from 1932 January to 2017 January. The following prominent results are found: (1) geomagnetic <span class="hlt">activity</span> lags behind sunspot numbers with a phase shift of 21 months, and they have a high level of asynchronous behavior; (2) their relative phase interconnections are in phase for the periodic scales during 8-16 years, but have a mixing behavior for the periodic belts below 8 years; (3) both sunspot numbers and geomagnetic <span class="hlt">activity</span> can not be regarded as a stochastic phenomenon because their dynamical behaviors display a long-term correlation and a fractal nature. We believe that the presented conclusions could provide further information on understanding the dynamical coupling of <span class="hlt">solar</span> dynamo process with geomagnetic <span class="hlt">activity</span> variation, and the crucial role of <span class="hlt">solar</span> and geomagnetic <span class="hlt">activity</span> in the long-term climate change.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://eric.ed.gov/?q=solar+AND+radiation&pg=7&id=EJ246282','ERIC'); return false;" href="https://eric.ed.gov/?q=solar+AND+radiation&pg=7&id=EJ246282"><span><span class="hlt">Solar</span> Cookers.</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>King, Richard C.</p> <p>1981-01-01</p> <p>Describes the use of <span class="hlt">solar</span> cookers in the science classroom. Includes instructions for construction of a <span class="hlt">solar</span> cooker, an explanation of how <span class="hlt">solar</span> cookers work, and a number of suggested <span class="hlt">activities</span>. (DS)</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://ntrs.nasa.gov/search.jsp?R=20090001864&hterms=activity+Physics&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D20%26Ntt%3Dactivity%2BPhysics','NASA-TRS'); return false;" href="https://ntrs.nasa.gov/search.jsp?R=20090001864&hterms=activity+Physics&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D20%26Ntt%3Dactivity%2BPhysics"><span>Triennial Report 2006-2009. Commission 10: <span class="hlt">Solar</span> <span class="hlt">Activity</span></span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Klimchuk, James A.</p> <p>2008-01-01</p> <p>Commission 10 deals with <span class="hlt">solar</span> <span class="hlt">activity</span> in all of its forms, ranging from the smallest nanoflares to the largest coronal mass ejections. This report reviews scientific progress over the roughly two-year period ending in the middle of 2008. This has been an exciting time in <span class="hlt">solar</span> physics, highlighted by the launches of the Hinode and STEREO missions late in 2006. The report is reasonably comprehensive, though it is far from exhaustive. Limited space prevents the inclusion of many significant results. The report is divided into following sections: Photosphere and Chromosphere; Transition Region; Corona and Coronal Heating; Coronal Jets; Flares; Coronal Mass Ejection Initiation; Global Coronal Waves and Shocks; Coronal Dimming; The Link Between Low Coronal CME signatures and Magnetic Clouds; Coronal Mass Ejections in the Heliosphere; and Coronal Mass Ejections and Space Weather. Primary authorship is indicated at the beginning of each section.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2014EGUGA..16.9519L','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2014EGUGA..16.9519L"><span><span class="hlt">Influence</span> of interplanetary <span class="hlt">solar</span> wind sector polarity on the ionosphere</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>liu, jing</p> <p>2014-05-01</p> <p>Knowledge of <span class="hlt">solar</span> sector polarity effects on the ionosphere may provide some clues in understanding of the ionospheric day-to-day variability. A <span class="hlt">solar</span>-terrestrial connection ranging from <span class="hlt">solar</span> sector boundary (SB) crossings, geomagnetic disturbance and ionospheric perturbations has been demonstrated. The increases in interplanetary <span class="hlt">solar</span> wind speed within three days are seen after SB crossings, while the decreases in <span class="hlt">solar</span> wind dynamic pressure and magnetic field intensity immediately after SB crossings are confirmed by the superposed epoch analysis results. Furthermore, the interplanetary magnetic field (IMF) Bz component turns from northward to southward in March equinox and June solstice as the Earth passes from a <span class="hlt">solar</span> sector of outward to inward directed magnetic fields, whereas the reverse situation occurs for the transition from toward to away sectors. The F2 region critical frequency (foF2) covering about four <span class="hlt">solar</span> cycles and total electron content (TEC) during 1998-2011 are utilized to extract the related information, revealing that they are not modified significantly and vary within the range of 15% on average. The responses of the ionospheric TEC to SB crossings exhibit complex temporal and spatial variations and have strong dependencies on season, latitude, and <span class="hlt">solar</span> cycle. This effect is more appreciable in equinoctial months than in solstitial months, which is mainly caused by larger southward Bz components in equinox. In September equinox, latitudinal profile of relative variations of foF2 at noon is featured by depressions at high latitudes and enhancements in low-equatorial latitudes during IMF away sectors. The negative phase of foF2 is delayed at <span class="hlt">solar</span> minimum relative to it during other parts of <span class="hlt">solar</span> cycle, which might be associated with the difference in longevity of major interplanetary <span class="hlt">solar</span> wind drivers perturbing the Earth's environment in different phases of <span class="hlt">solar</span> cycle.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2010EGUGA..1214629S','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2010EGUGA..1214629S"><span>Ground-based Observations of Large <span class="hlt">Solar</span> Flares Precursors</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Sheyner, Olga; Smirnova, Anna; Snegirev, Sergey</p> <p>2010-05-01</p> <p>The importance problem of <span class="hlt">Solar</span>-terrestrial physics is regular forecasting of <span class="hlt">solar</span> <span class="hlt">activity</span> phenomena, which negatively <span class="hlt">influence</span> the human's health, operating safety, communication, radar sets and others. The opportunity of development of short-term forecasting technique of geoeffective <span class="hlt">solar</span> flares is presented in this study. This technique is based on the effect of growth of pulsations of horizontal component of geomagnetic field before the <span class="hlt">solar</span> proton flares. The long-period (30-60 minutes) pulsations of H-component of geomagnetic field are detected for the events of different intensity on March 22, 1991, November 4, 2001, and November 17, 2001 using the method of wavelet-analysis. Amplitudes of fluctuations of horizontal component of geomagnetic field with the 30-60 minute's periods grow at the most of tested stations during 0.5-3.5 days before the <span class="hlt">solar</span> flares. The particularities of spectral component are studied for the stations situated on different latitudes. The assumptions about the reason of such precursors-fluctuations appearance are made.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://ntrs.nasa.gov/search.jsp?R=19870052703&hterms=active+site&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D70%26Ntt%3Dactive%2Bsite','NASA-TRS'); return false;" href="https://ntrs.nasa.gov/search.jsp?R=19870052703&hterms=active+site&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D70%26Ntt%3Dactive%2Bsite"><span>Measurement and interpretation of magnetic shear in <span class="hlt">solar</span> <span class="hlt">active</span> regions</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Hagyard, M. J.; Rabin, D. M.</p> <p>1986-01-01</p> <p>In this paper a summary and synthesis are presented for results on the role of magnetic shear in the flare process that have been derived from the series of Flare Buildup Study Workshops in the <span class="hlt">Solar</span> Maximum Analysis program. With emphasis on observations, the mechanisms that seem to produce the sheared magnetic configurations observed in flaring <span class="hlt">active</span> regions are discussed. The spatial and temporal correlations of this shear with the onset of <span class="hlt">solar</span> flares are determined from quantitative analyses of measurements of the vector magnetic field. The question of why some areas of sheared magnetic fields are the sites of flares and others are not is investigated observationally.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017WRCM...27..272X','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017WRCM...27..272X"><span>Phase fluctuations model for EM wave propagation through <span class="hlt">solar</span> scintillation at superior <span class="hlt">solar</span> conjunction</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Xu, Guanjun; Song, Zhaohui</p> <p>2017-04-01</p> <p>Traveling <span class="hlt">solar</span> wind disturbances have a significant <span class="hlt">influence</span> on radio wave characteristics during the superior <span class="hlt">solar</span> conjunction communication. This paper considers the impact of <span class="hlt">solar</span> scintillation on phase fluctuations of electromagnetic (EM) wave propagation during the superior <span class="hlt">solar</span> conjunction. Based on the Geometric Optics approximation, the close-form approximation model for phase fluctuations is developed. Both effects of anisotropic temporal variations function of plasma irregularities and their power spectrum are presented and analyzed numerically. It is found that phase fluctuations rapidly decrease with increasing Sun-Earth-Probe angle and decrease with increasing frequency at the rate of 1/f2. Moreover, the role of various features of the <span class="hlt">solar</span> wind irregularities and their <span class="hlt">influence</span> on the EM wave characteristic parameters is studied and discussed. Finally, we study the phase fluctuations of typical cases in order to better understand the impact of phase fluctuations in future deep space communication scenarios during <span class="hlt">solar</span> conjunction periods.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/27194958','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/27194958"><span>The <span class="hlt">Solar</span> Cycle.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Hathaway, David H</p> <p></p> <p>The <span class="hlt">solar</span> cycle is reviewed. The 11-year cycle of <span class="hlt">solar</span> <span class="hlt">activity</span> is characterized by the rise and fall in the numbers and surface area of sunspots. A number of other <span class="hlt">solar</span> <span class="hlt">activity</span> indicators also vary in association with the sunspots including; the 10.7 cm radio flux, the total <span class="hlt">solar</span> irradiance, the magnetic field, flares and coronal mass ejections, geomagnetic <span class="hlt">activity</span>, galactic cosmic ray fluxes, and radioisotopes in tree rings and ice cores. Individual <span class="hlt">solar</span> cycles are characterized by their maxima and minima, cycle periods and amplitudes, cycle shape, the equatorward drift of the <span class="hlt">active</span> latitudes, hemispheric asymmetries, and <span class="hlt">active</span> longitudes. Cycle-to-cycle variability includes the Maunder Minimum, the Gleissberg Cycle, and the Gnevyshev-Ohl (even-odd) Rule. Short-term variability includes the 154-day periodicity, quasi-biennial variations, and double-peaked maxima. We conclude with an examination of prediction techniques for the <span class="hlt">solar</span> cycle and a closer look at cycles 23 and 24. Supplementary material is available for this article at 10.1007/lrsp-2015-4.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017SPD....4830201C','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017SPD....4830201C"><span>From Emergence to Eruption: The Physics and Diagnostics of <span class="hlt">Solar</span> <span class="hlt">Active</span> Regions</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Cheung, Mark</p> <p>2017-08-01</p> <p>The <span class="hlt">solar</span> photosphere is continuously seeded by the emergence of magnetic fields from the <span class="hlt">solar</span> interior. In turn, photospheric evolution shapes the magnetic terrain in the overlying corona. Magnetic fields in the corona store the energy needed to power coronal mass ejections (CMEs) and <span class="hlt">solar</span> flares. In this talk, we recount a physics-based narrative of <span class="hlt">solar</span> eruptive events from cradle to grave, from emergence to eruption, from evaporation to condensation. We review the physical processes which are understood to transport magnetic flux from the interior to the surface, inject free energy and twist into the corona, disentangle the coronal field to permit explosive energy release, and subsequently convert the released energy into observable signatures. Along the way, we review observational diagnostics used to constrain theories of <span class="hlt">active</span> region evolution and eruption. Finally, we discuss the opportunities and challenges enabled by the large existing repository of <span class="hlt">solar</span> observations. We argue that the synthesis of physics and diagnostics embodied in (1) data-driven modeling and (2) machine learning efforts will be an accelerating agent for scientific discovery.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2004AAS...204.3601A','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2004AAS...204.3601A"><span>The Stellar-<span class="hlt">Solar</span> Connection</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Ayres, T. R.</p> <p>2004-05-01</p> <p>Many <span class="hlt">solar</span>-stellar astronomers believe that the <span class="hlt">solar</span>-stellar connection primarily is a one-way street: the exquisitely detailed studies of the <span class="hlt">solar</span> surface, interior, and heliosphere strongly mold our views of the distant, unresolved stars. Perhaps many <span class="hlt">solar</span> physicists have gone so far as to adopt the myopic view that stellar astronomy, by and large, is merely sponging up the fabulous insights from ever deeper examinations of our local star, but the ``dark side'' is not really capable of returning the favor. What could we possibly learn from the stars, that we don't already know from much better observations of the Sun? In my Introduction to this Topical Session, I will discuss two broad issues: (1) the present divergence between <span class="hlt">solar</span> and stellar physics (driven by the different goals and tools of the two disciplines); and (2) the diversity of stars in the H-R diagram, to help inform our understanding of <span class="hlt">solar</span> processes. Today, there are observations of stars that greatly exceed the quality of analogous <span class="hlt">solar</span> measurements: e.g., HST/STIS UV echelle spectra of Alpha Cen A; Chandra transmission grating spectra of <span class="hlt">solar</span>-type stars; and only recently have we obtained a definitive understanding of the Sun's soft X-ray luminosity in the key ROSAT/PSPC band. The lack of equivalent <span class="hlt">solar</span> observations hinders practical applications of the <span class="hlt">solar</span>-stellar connection. On the more informative side, the evolutionary paths of other stars can be quite different from the Sun's, with potentially dramatic <span class="hlt">influences</span> on phenomena such as magnetic <span class="hlt">activity</span>. Equally important, examples of Sun-like stars can be found at all stages of evolution, from proplyds to red giants, in the volume of nearby space out to 500 pc. In short, the <span class="hlt">solar</span>-stellar connection need not be a one-way street, but rather a powerful tool to explore <span class="hlt">solar</span> processes within the broader context of stars and stellar evolution. This work was supported by NASA grant NAG5-13058.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017AGUFMSM33C2679S','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017AGUFMSM33C2679S"><span><span class="hlt">Influence</span> of the <span class="hlt">solar</span> wind and IMF on Jupiter's magnetosphere: Results from global MHD simulations</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Sarkango, Y.; Jia, X.; Toth, G.; Hansen, K. C.</p> <p>2017-12-01</p> <p>Due to its large size, rapid rotation and presence of substantial internal plasma sources, Jupiter's magnetosphere is fundamentally different from that of the Earth. How and to what extent do the external factors, such as the <span class="hlt">solar</span> wind and interplanetary magnetic field (IMF), <span class="hlt">influence</span> the internally-driven magnetosphere is an open question. In this work, we solve the 3D semi-relativistic magnetohydrodynamic (MHD) equations using a well-established code, BATSRUS, to model the Jovian magnetosphere and study its interaction with the <span class="hlt">solar</span> wind. Our global model adopts a non-uniform mesh covering the region from 200 RJ upstream to 1800 RJ downstream with the inner boundary placed at a radial distance of 2.5 RJ. The Io plasma torus centered around 6 RJ is generated in our model through appropriate mass-loading terms added to the set of MHD equations. We perform systematic numerical experiments in which we vary the upstream <span class="hlt">solar</span> wind properties to investigate the impact of <span class="hlt">solar</span> wind events, such as interplanetary shock and IMF rotation, on the global magnetosphere. From our simulations, we extract the location of the magnetopause boundary, the bow shock and the open-closed field line boundary (OCB), and determine their dependence on the <span class="hlt">solar</span> wind properties and the IMF orientation. For validation, we compare our simulation results, such as density, temperature and magnetic field, to published empirical models based on in-situ measurements.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/26074647','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/26074647"><span><span class="hlt">Influence</span> of <span class="hlt">solar</span> variability on the infrared radiative cooling of the thermosphere from 2002 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>Mlynczak, Martin G; Hunt, Linda A; Mertens, Christopher J; Thomas Marshall, B; Russell, James M; Woods, Thomas; Earl Thompson, R; Gordley, Larry L</p> <p>2014-04-16</p> <p>Infrared radiative cooling of the thermosphere by carbon dioxide (CO 2 , 15 µm) and by nitric oxide (NO, 5.3 µm) has been observed for 12 years by the Sounding of the Atmosphere using Broadband Emission Radiometry (SABER) instrument on the Thermosphere-Ionosphere-Mesosphere Energetics and Dynamics satellite. For the first time we present a record of the two most important thermospheric infrared cooling agents over a complete <span class="hlt">solar</span> cycle. SABER has documented dramatic variability in the radiative cooling on time scales ranging from days to the 11 year <span class="hlt">solar</span> cycle. Deep minima in global mean vertical profiles of radiative cooling are observed in 2008-2009. Current <span class="hlt">solar</span> maximum conditions, evidenced in the rates of radiative cooling, are substantially weaker than prior maximum conditions in 2002-2003. The observed changes in thermospheric cooling correlate well with changes in <span class="hlt">solar</span> ultraviolet irradiance and geomagnetic <span class="hlt">activity</span> during the prior maximum conditions. NO and CO 2 combine to emit 7 × 10 18 more Joules annually at <span class="hlt">solar</span> maximum than at <span class="hlt">solar</span> minimum. First record of thermospheric IR cooling rates over a complete <span class="hlt">solar</span> cycleIR cooling in current <span class="hlt">solar</span> maximum conditions much weaker than prior maximumVariability in thermospheric IR cooling observed on scale of days to 11 years.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/15496131','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/15496131"><span>Glacial <span class="hlt">influences</span> on <span class="hlt">solar</span> radiation in a subarctic sea.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Barron, Mace G; Barron, Kyle J</p> <p>2005-01-01</p> <p>Understanding macroscale processes controlling <span class="hlt">solar</span> radiation in marine systems will be important in interpreting the potential effects of global change from increasing ultraviolet radiation (UV) and glacial retreat. This study provides the first quantitative assessment of UV in the water column of Prince William Sound, a subarctic, semienclosed sea surrounded by mountains, glaciers, rivers, bays and fjords in south central Alaska. Glacial <span class="hlt">influences</span> on diffuse attenuation coefficients (Kd) were determined along an approximate 120 km transect running NE (61 degrees 07'43''N, 146 degrees 17'1''W) to SW (60 degrees 27'25''N, 148 degrees 05'27'' W). Glacial meltwater and flour caused a 10-fold increase in Kd for visible light, UV-A and UV-B, whereas high optical clarity was present in a diversity of areas away from glacial <span class="hlt">influences</span>. Transition areas and locations affected by calving of a tidewater glacier had intermediate Kd values. Depths at 99% attenuation ranged from less than 0.2 m near glacial streams to greater than 5 m in bays and open ocean distant from sources of glacial sediments. These results suggest that potential global change from increasing UV and glacial retreat may have heterogeneous effects on subarctic marine systems.</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('http://adsabs.harvard.edu/abs/2015AdSpR..55..401K','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2015AdSpR..55..401K"><span>Variations of <span class="hlt">solar</span>, interplanetary, and geomagnetic parameters with <span class="hlt">solar</span> magnetic multipole fields during <span class="hlt">Solar</span> Cycles 21-24</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Kim, Bogyeong; Lee, Jeongwoo; Yi, Yu; Oh, Suyeon</p> <p>2015-01-01</p> <p>In this study we compare the temporal variations of the <span class="hlt">solar</span>, interplanetary, and geomagnetic (SIG) parameters with that of open <span class="hlt">solar</span> magnetic flux from 1976 to 2012 (from <span class="hlt">Solar</span> Cycle 21 to the early phase of Cycle 24) for a purpose of identifying their possible relationships. By the open flux, we mean the average magnetic field over the source surface (2.5 <span class="hlt">solar</span> radii) times the source area as defined by the potential field source surface (PFSS) model of the Wilcox <span class="hlt">Solar</span> Observatory (WSO). In our result, most SIG parameters except the <span class="hlt">solar</span> wind dynamic pressure show rather poor correlations with the open <span class="hlt">solar</span> magnetic field. Good correlations are recovered when the contributions from individual multipole components are counted separately. As expected, <span class="hlt">solar</span> <span class="hlt">activity</span> indices such as sunspot number, total <span class="hlt">solar</span> irradiance, 10.7 cm radio flux, and <span class="hlt">solar</span> flare occurrence are highly correlated with the flux of magnetic quadrupole component. The dynamic pressure of <span class="hlt">solar</span> wind is strongly correlated with the dipole flux, which is in anti-phase with <span class="hlt">Solar</span> Cycle (SC). The geomagnetic <span class="hlt">activity</span> represented by the Ap index is correlated with higher order multipole components, which show relatively a slow time variation with SC. We also found that the unusually low geomagnetic <span class="hlt">activity</span> during SC 23 is accompanied by the weak open <span class="hlt">solar</span> fields compared with those in other SCs. It is argued that such dependences of the SIG parameters on the individual multipole components of the open <span class="hlt">solar</span> magnetic flux may clarify why some SIG parameters vary in phase with SC and others show seemingly delayed responses to SC variation.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017E%26ES...93a2080X','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017E%26ES...93a2080X"><span>Research on temperature control and <span class="hlt">influence</span> of the vacuum tubes with inserted tubes <span class="hlt">solar</span> heater</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Xiao, L. X.; He, Y. T.; Hua, J. Q.</p> <p>2017-11-01</p> <p>A novel snake-shape vacuum tube with inserted tubes <span class="hlt">solar</span> collector is designed in this paper, the heat transfer characteristics of the collector are analyzed according to its structural characteristics, and the <span class="hlt">influence</span> of different working temperature on thermal characteristics of the collector is studied. The <span class="hlt">solar</span> water heater prototype consisting of 14 vacuum tubes with inserted tubes is prepared, and the hot water storage control subsystem is designed by hysteresis comparison algorithm. The heat characteristic of the prototype was experimentally studied under hot water output temperature of 40-45°C, 50-55°C and 60-65°C. The daily thermal efficiency was 64%, 50% and 46%, respectively. The experimental results are basically consistent with the theoretical analysis.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=5510962','PMC'); return false;" href="https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=5510962"><span>Global conditions in the <span class="hlt">solar</span> corona from 2010 to 2017</span></a></p> <p><a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pmc">PubMed Central</a></p> <p>Morgan, Huw; Taroyan, Youra</p> <p>2017-01-01</p> <p>Through reduction of a huge data set spanning 2010–2017, we compare mean global changes in temperature, emission measure (EM), and underlying photospheric magnetic field of the <span class="hlt">solar</span> corona over most of the last <span class="hlt">activity</span> cycle. The quiet coronal mean temperature rises from 1.4 to 1.8 MK, whereas EM increases by almost a factor of 50% from <span class="hlt">solar</span> minimum to maximum. An increased high-temperature component near 3 MK at <span class="hlt">solar</span> maximum drives the increase in quiet coronal mean temperature, whereas the bulk of the plasma remains near 1.6 MK throughout the cycle. The mean, spatially smoothed magnitude of the quiet Sun magnetic field rises from 1.6 G in 2011 to peak at 2.0 G in 2015. <span class="hlt">Active</span> region conditions are highly variable, but their mean remains approximately constant over the cycle, although there is a consistent decrease in <span class="hlt">active</span> region high-temperature emission (near 3 MK) between the peak of <span class="hlt">solar</span> maximum and present. <span class="hlt">Active</span> region mean temperature, EM, and magnetic field magnitude are highly correlated. Correlation between sunspot/<span class="hlt">active</span> region area and quiet coronal conditions shows the important <span class="hlt">influence</span> of decaying sunspots in driving global changes, although we find no appreciable delay between changes in <span class="hlt">active</span> region area and quiet Sun magnetic field strength. The hot coronal contribution to extreme ultraviolet (EUV) irradiance is dominated by the quiet corona throughout most of the cycle, whereas the high variability is driven by <span class="hlt">active</span> regions. <span class="hlt">Solar</span> EUV irradiance cannot be predicted accurately by sunspot index alone, highlighting the need for continued measurements. PMID:28740861</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2018ARep...62..243I','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2018ARep...62..243I"><span>Proton Flares in <span class="hlt">Solar</span> <span class="hlt">Activity</span> Complexes: Possible Origins and Consequences</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Isaeva, E. S.; Tomozov, V. M.; Yazev, S. A.</p> <p>2018-03-01</p> <p><span class="hlt">Solar</span> flares observed during the 24th <span class="hlt">solar-activity</span> cycle and accompanied by fluxes of particles detected at the Earth's orbit with intensities exceeding 10 particles cm-2 s-1 and energies of more than 10 MeV per particle mainly occurred in <span class="hlt">activity</span> complexes (82% of cases), with 80% of these occurring no more than 20 heliographic degrees from the nearest coronal holes. The correlation between the X-ray classes of flares and the proton fluxes detected at the Earth's orbit is weak. The work presented here supports the hypothesis that the leakage of particles into the heliosphere is due to the existence of long-lived magnetic channels, which facilitate the transport of flare-accelerated particles into the boundary regions of open magnetic structures of coronal holes. The possible contribution of exchange reconnection in the formation of such channels and the role of exchange reconnection in the generation of flares are discussed.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2018AAS...23124214S','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2018AAS...23124214S"><span><span class="hlt">Solar</span> Eclipse Education and Outreach <span class="hlt">Activities</span> at APSU</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Smith, J. Allyn; Buckner, Spencer L.; Adams, Mitzi; Meisch, Karen; Sudbrink, Don; Wright, Amy; Adams, Angela; Fagan, Ben</p> <p>2018-01-01</p> <p>The path of totality for the 21 August 2017 total <span class="hlt">solar</span> eclipse passed directly over the APSU campus in north-central Tennessee. We discuss our public outreach and education efforts, both on campus and in the community, and present results and lessons learned from this event. We reached nearly 20,000 people via our efforts and hosted nearly 3000 viewers on campus on eclipse day. We also present our science <span class="hlt">activities</span> and early results from those. On the whole, this event could be viewed as a large success for the university and the region, and the experiences will guide us in our efforts as we plan future eclipse <span class="hlt">activities</span>.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2012APS..MART49007P','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2012APS..MART49007P"><span>Self-assembly Columnar Structure in <span class="hlt">Active</span> Layer of Bulk Heterojunction <span class="hlt">Solar</span> Cell</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Pan, Cheng; Segui, Jennifer; Yu, Yingjie; Li, Hongfei; Akgun, Bulent; Satijia, Sushil. K.; Gersappe, Dilip; Nam, Chang-Yong; Rafailovich, Miriam</p> <p>2012-02-01</p> <p>Bulk Heterojunction (BHJ) polymer <span class="hlt">solar</span> cells are an area of intense interest due to their flexibility and relatively low cost. However, due to the disordered inner structure in <span class="hlt">active</span> layer, the power conversion efficiency of BHJ <span class="hlt">solar</span> cell is relatively low. Our research provides the method to produce ordered self-assembly columnar structure within <span class="hlt">active</span> layer of bulk heterojunction (BHJ) <span class="hlt">solar</span> cell by introducing polystyrene (PS) into the <span class="hlt">active</span> layer. The blend thin film of polystyrene, poly (3-hexylthiophene-2,5-diyl) (P3HT) and [6,6]-phenyl C61 butyric acid methyl ester (PCBM) at different ratio are spin coated on substrate and annealed in vacuum oven for certain time. Atomic force microscopy (AFM) images show uniform phase segregation on the surface of polymer blend thin film and highly ordered columnar structure is then proven by etching the film with ion sputtering. TEM cross-section technology is also used to investigate the column structure. Neutron reflectometry was taken to establish the confinement of PCBM at the interface of PS and P3HT. The different morphological structures formed via phase segregation will be correlated with the performance of the PEV cells to be fabricated at the BNL-CFN.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/29677828','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/29677828"><span><span class="hlt">Influence</span> of Post-Heat Treatment of ZnO:Al Transparent Electrode for Copper Indium Gallium Selenide Thin Film <span class="hlt">Solar</span> Cell.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Eom, Taewoo; Park, Jeong Eun; Park, Sang Yong; Park, Jeong Hoon; Bweupe, Jackson; Lim, Donggun</p> <p>2018-09-01</p> <p>Copper indium gallium selenide (CIGS) thin film <span class="hlt">solar</span> cells have been regarded as a candidate for energy conversion devices owing to their high absorption coefficient, high temperature stability, and low cost. ZnO:Al thin film is commonly used in CIGS <span class="hlt">solar</span> cells as a window layer. In this study, ZnO:Al films were deposited on glass under various post-heat temperature using RF sputtering to observe the characteristics of ZnO:Al films such as Hall mobility, carrier concentration, and resistivity; subsequently, the ZnO:Al films were applied to a CIGS <span class="hlt">solar</span> cell as a window. CIGS <span class="hlt">solar</span> cells fabricated with various ZnO:Al films were analyzed in order to investigate their <span class="hlt">influence</span>. The test results showed that the improvement of ZnO:Al characteristics affects Jsc and Voc in the <span class="hlt">solar</span> cell through reduced recombination and increase of optical property.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2014cosp...40E3540V','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2014cosp...40E3540V"><span>Particle acceleration in <span class="hlt">solar</span> <span class="hlt">active</span> regions being in the state of self-organized criticality.</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Vlahos, Loukas</p> <p></p> <p>We review the recent observational results on flare initiation and particle acceleration in <span class="hlt">solar</span> <span class="hlt">active</span> regions. Elaborating a statistical approach to describe the spatiotemporally intermittent electric field structures formed inside a flaring <span class="hlt">solar</span> <span class="hlt">active</span> region, we investigate the efficiency of such structures in accelerating charged particles (electrons and protons). The large-scale magnetic configuration in the <span class="hlt">solar</span> atmosphere responds to the strong turbulent flows that convey perturbations across the <span class="hlt">active</span> region by initiating avalanche-type processes. The resulting unstable structures correspond to small-scale dissipation regions hosting strong electric fields. Previous research on particle acceleration in strongly turbulent plasmas provides a general framework for addressing such a problem. This framework combines various electromagnetic field configurations obtained by magnetohydrodynamical (MHD) or cellular automata (CA) simulations, or by employing a statistical description of the field’s strength and configuration with test particle simulations. We work on data-driven 3D magnetic field extrapolations, based on a self-organized criticality models (SOC). A relativistic test-particle simulation traces each particle’s guiding center within these configurations. Using the simulated particle-energy distributions we test our results against observations, in the framework of the collisional thick target model (CTTM) of <span class="hlt">solar</span> hard X-ray (HXR) emission and compare our results with the current observations.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/19990109083','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/19990109083"><span>The <span class="hlt">Influence</span> of Extremely Large <span class="hlt">Solar</span> Proton Events in a Changing Stratosphere. Stratospheric <span class="hlt">Influence</span> of <span class="hlt">Solar</span> Proton Events</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Jackman, Charles H.; Fleming, Eric L.; Vitt, Francis M.</p> <p>1999-01-01</p> <p>Two periods of extremely large <span class="hlt">solar</span> proton events (SPEs) occurred in the past thirty years, which forced significant long-term polar stratospheric changes. The August 2-10, 1972 and October 19-27, 1989 SPEs happened in stratospheres that were quite different chemically. The stratospheric chlorine levels were relatively small in 1972 (approximately 1.2 ppbv) and were fairly substantial in 1989 at about (approximately 3 ppbv). Although these SPEs produced both HO(x) and NO(y) constituents in the mesosphere and stratosphere, only the NO(y) constituents had lifetimes long enough to affect ozone for several months to years past the events. Our recently improved two-dimensional chemistry and transport atmospheric model was used to compute the effects of these gigantic SPEs in a changing stratosphere. Significant upper stratospheric ozone depletions > 10% are computed to last for a few months past these SPEs. The long-lived SPE-produced NO(y) constituents were transported to lower levels during winter after these huge SPEs and caused impacts in the middle and lower stratosphere. During periods of high halogen loading these impacts resulted in interference with the chlorine and bromine loss cycles for ozone destruction. The chemical state of the atmosphere, including the stratospheric sulfate aerosol density, substantially affected the predicted stratospheric <span class="hlt">influence</span> of these extremely large SPEs.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://images.nasa.gov/#/details-PIA18169.html','SCIGOVIMAGE-NASA'); return false;" href="https://images.nasa.gov/#/details-PIA18169.html"><span><span class="hlt">Solar</span> Dynamics Observatory Artist Concept</span></a></p> <p><a target="_blank" href="https://images.nasa.gov/">NASA Image and Video Library</a></p> <p></p> <p>2010-02-11</p> <p>The <span class="hlt">Solar</span> Dynamics Observatory SDO spacecraft, shown above the Earth as it faces toward the Sun. SDO is designed to study the <span class="hlt">influence</span> of the Sun on the Earth and the inner <span class="hlt">solar</span> system by studying the <span class="hlt">solar</span> atmosphere. http://photojournal.jpl.nasa.gov/catalog/PIA18169</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2015NatCo...6E6491M','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2015NatCo...6E6491M"><span>The <span class="hlt">solar</span> magnetic <span class="hlt">activity</span> band interaction and instabilities that shape quasi-periodic variability</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>McIntosh, Scott W.; Leamon, Robert J.; Krista, Larisza D.; Title, Alan M.; Hudson, Hugh S.; Riley, Pete; Harder, Jerald W.; Kopp, Greg; Snow, Martin; Woods, Thomas N.; Kasper, Justin C.; Stevens, Michael L.; Ulrich, Roger K.</p> <p>2015-04-01</p> <p><span class="hlt">Solar</span> magnetism displays a host of variational timescales of which the enigmatic 11-year sunspot cycle is most prominent. Recent work has demonstrated that the sunspot cycle can be explained in terms of the intra- and extra-hemispheric interaction between the overlapping <span class="hlt">activity</span> bands of the 22-year magnetic polarity cycle. Those <span class="hlt">activity</span> bands appear to be driven by the rotation of the Sun's deep interior. Here we deduce that <span class="hlt">activity</span> band interaction can qualitatively explain the `Gnevyshev Gap'--a well-established feature of flare and sunspot occurrence. Strong quasi-annual variability in the number of flares, coronal mass ejections, the radiative and particulate environment of the heliosphere is also observed. We infer that this secondary variability is driven by surges of magnetism from the <span class="hlt">activity</span> bands. Understanding the formation, interaction and instability of these <span class="hlt">activity</span> bands will considerably improve forecast capability in space weather and <span class="hlt">solar</span> <span class="hlt">activity</span> over a range of timescales.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=4396379','PMC'); return false;" href="https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=4396379"><span>The <span class="hlt">solar</span> magnetic <span class="hlt">activity</span> band interaction and instabilities that shape quasi-periodic variability</span></a></p> <p><a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pmc">PubMed Central</a></p> <p>McIntosh, Scott W.; Leamon, Robert J.; Krista, Larisza D.; Title, Alan M.; Hudson, Hugh S.; Riley, Pete; Harder, Jerald W.; Kopp, Greg; Snow, Martin; Woods, Thomas N.; Kasper, Justin C.; Stevens, Michael L.; Ulrich, Roger K.</p> <p>2015-01-01</p> <p><span class="hlt">Solar</span> magnetism displays a host of variational timescales of which the enigmatic 11-year sunspot cycle is most prominent. Recent work has demonstrated that the sunspot cycle can be explained in terms of the intra- and extra-hemispheric interaction between the overlapping <span class="hlt">activity</span> bands of the 22-year magnetic polarity cycle. Those <span class="hlt">activity</span> bands appear to be driven by the rotation of the Sun's deep interior. Here we deduce that <span class="hlt">activity</span> band interaction can qualitatively explain the ‘Gnevyshev Gap'—a well-established feature of flare and sunspot occurrence. Strong quasi-annual variability in the number of flares, coronal mass ejections, the radiative and particulate environment of the heliosphere is also observed. We infer that this secondary variability is driven by surges of magnetism from the <span class="hlt">activity</span> bands. Understanding the formation, interaction and instability of these <span class="hlt">activity</span> bands will considerably improve forecast capability in space weather and <span class="hlt">solar</span> <span class="hlt">activity</span> over a range of timescales. PMID:25849045</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://ntrs.nasa.gov/search.jsp?R=20080038051&hterms=activity+Physics&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D20%26Ntt%3Dactivity%2BPhysics','NASA-TRS'); return false;" href="https://ntrs.nasa.gov/search.jsp?R=20080038051&hterms=activity+Physics&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D20%26Ntt%3Dactivity%2BPhysics"><span>The Role of Magnetic Reconnection in <span class="hlt">Solar</span> <span class="hlt">Activity</span></span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Antiochos, Spiro; DeVore, C. R.</p> <p>2008-01-01</p> <p>The central challenge in <span class="hlt">solar</span>/heliospheric physics is to understand how the emergence and transport of magnetic flux at the photosphere drives the structure and dynamics that we observe in the corona and heliosphere. This presentation focuses on the role of magnetic reconnection in determining <span class="hlt">solar</span>/heliospheric <span class="hlt">activity</span>. We demonstrate that two generic properties of the photospheric magnetic and velocity fields are responsible for the ubiquitous reconnection in the corona. First, the photospheric velocities are complex, which leads to the injection of energy and helicity into the coronal magnetic fields and to the efficient, formation of small-scale structure. Second, the flux distribution at the photosphere is multi-polar, which implies that topological discontinuities and, consequently, current sheets, must be present in the coronal magnetic field. We: present numerical simulations showing that photospherically-driven reconnection is responsible for the heating and dynamics of coronal plasma, and for the topology of the coronal/heliospheric magnetic field.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017AGUFMSH23D2703P','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017AGUFMSH23D2703P"><span>The <span class="hlt">Solar</span> Wind from Pseudostreamers and their Environs: Opportunities for Observations with Parker <span class="hlt">Solar</span> Probe and <span class="hlt">Solar</span> Orbiter</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Panasenco, O.; Velli, M.; Panasenco, A.; Lionello, R.</p> <p>2017-12-01</p> <p>The <span class="hlt">solar</span> dynamo and photospheric convection lead to three main types of structures extending from the <span class="hlt">solar</span> surface into the corona - <span class="hlt">active</span> regions, <span class="hlt">solar</span> filaments (prominences when observed at the limb) and coronal holes. These structures exist over a wide range of scales, and are interlinked with each other in evolution and dynamics. <span class="hlt">Active</span> regions can form clusters of magnetic <span class="hlt">activity</span> and the strongest overlie sunspots. In the decay of <span class="hlt">active</span> regions, the boundaries separating opposite magnetic polarities (neutral lines) develop specific structures called filament channels above which filaments form. In the presence of flux imbalance decaying <span class="hlt">active</span> regions can also give birth to lower latitude coronal holes. The accumulation of magnetic flux at coronal hole boundaries also creates conditions for filament formation: polar crown filaments are permanently present at the boundaries of the polar coronal holes. Mid-latitude and equatorial coronal holes - the result of <span class="hlt">active</span> region evolution - can create pseudostreamers if other coronal holes of the same polarity are present. While helmet streamers form between open fields of opposite polarities, the pseudostreamer, characterized by a smaller coronal imprint, typically shows a more prominent straight ray or stalk extending from the corona. The pseudostreamer base at photospheric heights is multipolar; often one observes tripolar magnetic configurations with two neutral lines - where filaments can form - separating the coronal holes. Here we discuss the specific role of filament channels on pseudostreamer topology and on <span class="hlt">solar</span> wind properties. 1D numerical analysis of pseudostreamers shows that the properties of the <span class="hlt">solar</span> wind from around PSs depend on the presence/absence of filament channels, number of channels and chirality at thepseudostreamer base low in the corona. We review and model possible coronal magnetic configurations and <span class="hlt">solar</span> wind plasma properties at different distances from the <span class="hlt">solar</span> surface that</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2015AN....336..225N','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2015AN....336..225N"><span><span class="hlt">Solar</span> <span class="hlt">activity</span> around AD 775 from aurorae and radiocarbon</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Neuhäuser, R.; Neuhäuser, D. L.</p> <p>2015-04-01</p> <p>A large variation in 14C around AD 775 has been considered to be caused by one or more <span class="hlt">solar</span> super-flares within one year. We critically review all known aurora reports from Europe as well as the Near, Middle, and Far East from AD 731 to 825 and find 39 likely true aurorae plus four more potential aurorae and 24 other reports about halos, meteors, thunderstorms etc., which were previously misinterpreted as aurorae or misdated; we assign probabilities for all events according to five aurora criteria. We find very likely true aurorae in AD 743, 745, 762, 765, 772, 773, 793, 796, 807, and 817. There were two aurorae in the early 770s observed near Amida (now Diyarbak\\i r in Turkey near the Turkish-Syrian border), which were not only red, but also green-yellow - being at a relatively low geomagnetic latitude, they indicate a relatively strong <span class="hlt">solar</span> storm. However, it cannot be argued that those aurorae (geomagnetic latitude 43 to 50°, considering five different reconstructions of the geomagnetic pole) could be connected to one or more <span class="hlt">solar</span> super-flares causing the 14C increase around AD 775: There are several reports about low- to mid-latitude aurorae at 32 to 44° geomagnetic latitude in China and Iraq; some of them were likely observed (quasi-)simultaneously in two of three areas (Europe, Byzantium/Arabia, East Asia), one lasted several nights, and some indicate a particularly strong geomagnetic storm (red colour and dynamics), namely in AD 745, 762, 793, 807, and 817 - always without 14C peaks. We use 39 likely true aurorae as well as historic reports about sunspots together with the radiocarbon content from tree rings to reconstruct the <span class="hlt">solar</span> <span class="hlt">activity</span>: From AD {˜ 733} to {˜ 823}, we see at least nine Schwabe cycles; instead of one of those cycles, there could be two short, weak cycles - reflecting the rapid increase to a high 14C level since AD 775, which lies at the end of a strong cycle. In order to show the end of the dearth of naked-eye sunspots, we</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2013AIPC.1551..165D','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2013AIPC.1551..165D"><span>The technical analysis of the stock exchange and physics: Japanese candlesticks for <span class="hlt">solar</span> <span class="hlt">activity</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Dineva, C.; Atanasov, V.</p> <p>2013-09-01</p> <p>In this article, we use the Japanese candlesticks, a method popular in the technical analysis of the Stock/Forex markets and apply it to a variable in physics-the <span class="hlt">solar</span> <span class="hlt">activity</span>. This method is invented and used exclusively for economic analysis and its application to a physical problem produced unexpected results. We found that the Japanese candlesticks are convenient tool in the analysis of the variables in the physics of the Sun. Based on our observations, we differentiated a new cycle in the <span class="hlt">solar</span> <span class="hlt">activity</span>.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/20020069117','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/20020069117"><span><span class="hlt">Solar</span> Cycle Variations and Equatorial Oscillations: Modeling Study</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Mayr, H. G.; Mengel, J. G.; Drob, D. P.; Chan, K. L.; Porter, H. S.; Bhartia, P. K. (Technical Monitor)</p> <p>2001-01-01</p> <p><span class="hlt">Solar</span> cycle <span class="hlt">activity</span> effects (SCAE) in the lower and middle atmosphere, reported in several studies, are difficult to explain on the basis of the small changes in <span class="hlt">solar</span> radiation that accompany the 11-year cycle, It is therefore natural to speculate that dynamical processes may come into play to produce a leverage. Such a leverage may be provided by the Quasi-Biennial Oscillation (QBO) in the zonal circulation of the stratosphere, which has been linked to <span class="hlt">solar</span> <span class="hlt">activity</span> variations. Driven primarily by wave mean flow interaction, the QBO period and its amplitude are variable but are also strongly <span class="hlt">influenced</span> by the seasonal cycle in the <span class="hlt">solar</span> radiation. This <span class="hlt">influence</span> extends to low altitudes referred to as "downward control". Relatively small changes in <span class="hlt">solar</span> radiative forcing can produce small changes in the period and phase of the QBO, but this in turn can produce measurable differences in the wind field. Thus, the QBO may be an amplifier of <span class="hlt">solar</span> <span class="hlt">activity</span> variations and a natural conduit of these variations to lower altitudes. To test this hypothesis, we conducted experiments with a 2D (two-dimensional) version of our Numerical Spectral Model that incorporates Hines' Doppler Spread Parameterization for small-scale gravity waves (GW). <span class="hlt">Solar</span> cycle radiance variations (SCRV) are accounted for by changing the radiative heating rate on a logarithmic scale from 0.1 % at the surface to 1 % at 50 km to 10% at 100 km. With and without SCRV, but with the same GW flux, we then conduct numerical experiments to evaluate the magnitude of the SCAE in the zonal circulation. The numerical results indicate that, under certain conditions, the SCAE is significant and can extend to lower altitudes where the SCRV is inconsequential. At 20-km the differences in the modeled wind velocities are as large as 5 m/s. For a modeled QBO period of 30 months, we find that the seasonal cycle in the <span class="hlt">solar</span> forcing (through the Semi-annual Oscillation (SAO)) acts as a strong pacemaker to lockup the</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2013AGUFMED52A..01K','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2013AGUFMED52A..01K"><span>Tools, Resources, and Innovations for <span class="hlt">Active</span> Learning of <span class="hlt">Solar</span> and Geospace Environment Content in the Undergraduate Classrooms</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Knipp, D. J.</p> <p>2013-12-01</p> <p>An undergraduate course in <span class="hlt">solar</span> and geospace (helio) physics should link fundamental principles from introductory physics and astronomy courses to concepts that appear unique, or are uniquely named in the heliophysics course. This paper discusses short topics and <span class="hlt">activities</span> that can be addressed in an approximately 15-min class segment, that introduce students to aspects of <span class="hlt">solar</span>, <span class="hlt">solar</span> wind, and geospace storms that are a step beyond, or a special application of, an introductory physics concept. Some of these <span class="hlt">activities</span> could be assigned as pre- or post- class <span class="hlt">activities</span> as well. Many of the <span class="hlt">actives</span> are aligned with images or diagrams in textbook, "Understanding Space Weather and the Physics Behind It," but could be easily adapted to other texts. We also address <span class="hlt">activities</span> that link to information from space weather forecasting and/or modeling websites.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/28386482','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/28386482"><span>Long-term global temperature variations under total <span class="hlt">solar</span> irradiance, cosmic rays, and volcanic <span class="hlt">activity</span>.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Biktash, Lilia</p> <p>2017-07-01</p> <p>The effects of total <span class="hlt">solar</span> irradiance (TSI) and volcanic <span class="hlt">activity</span> on long-term global temperature variations during <span class="hlt">solar</span> cycles 19-23 were studied. It was shown that a large proportion of climate variations can be explained by the mechanism of action of TSI and cosmic rays (CRs) on the state of the lower atmosphere and other meteorological parameters. The role of volcanic signals in the 11-year variations of the Earth's climate can be expressed as several years of global temperature drop. Conversely, it was shown that the effects of <span class="hlt">solar</span>, geophysical, and human <span class="hlt">activity</span> on climate change interact. It was concluded that more detailed investigations of these very complicated relationships are required, in order to be able to understand issues that affect ecosystems on a global scale.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2018SoPh..293...69W','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2018SoPh..293...69W"><span>A Test of the <span class="hlt">Active</span>-Day Fraction Method of Sunspot Group Number Calibration: Dependence on the Level of <span class="hlt">Solar</span> <span class="hlt">Activity</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Willamo, T.; Usoskin, I. G.; Kovaltsov, G. A.</p> <p>2018-04-01</p> <p>The method of <span class="hlt">active</span>-day fraction (ADF) was proposed recently to calibrate different <span class="hlt">solar</span> observers to standard observational conditions. The result of the calibration may depend on the overall level of <span class="hlt">solar</span> <span class="hlt">activity</span> during the observational period. This dependency is studied quantitatively using data of the Royal Greenwich Observatory by formally calibrating synthetic pseudo-observers to the full reference dataset. It is shown that the sunspot group number is precisely estimated by the ADF method for periods of moderate <span class="hlt">activity</span>, may be slightly underestimated by 0.5 - 1.5 groups ({≤} 10%) for strong and very strong <span class="hlt">activity</span>, and is strongly overestimated by up to 2.5 groups ({≤} 30%) for weak-to-moderate <span class="hlt">activity</span>. The ADF method becomes inapplicable for the periods of grand minima of <span class="hlt">activity</span>. In general, the ADF method tends to overestimate the overall level of <span class="hlt">activity</span> and to reduce the long-term trends.</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://adsabs.harvard.edu/abs/2016JSWSC...6A..38B','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2016JSWSC...6A..38B"><span>Rotation, <span class="hlt">activity</span>, and stellar obliquities in a large uniform sample of Kepler <span class="hlt">solar</span> analogs</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Buzasi, Derek; Lezcano, Andy; Preston, Heather L.</p> <p>2016-10-01</p> <p>In this study, we undertook a deep photometric examination of a narrowly-defined sample of <span class="hlt">solar</span> analogs in the Kepler field, with the goals of producing a uniform and statistically meaningful sample of such stars, comparing the properties of planet hosts to those of the general stellar population, and examining the behavior of rotation and photometric <span class="hlt">activity</span> among stars with similar overall physical parameters. We successfully derived photometric <span class="hlt">activity</span> indicators and rotation periods for 95 planet hosts (Kepler objects of interest [KOIs]) and 954 <span class="hlt">solar</span> analogs without detected planets; 573 of these rotation periods are reported here for the first time. Rotation periods average roughly 20 d, but the distribution has a wide dispersion, with a tail extending to P > 35 d which appears to be inconsistent with published gyrochronological relations. We observed a weak rotation-<span class="hlt">activity</span> relation for stars with rotation periods less than about 12 d; for slower rotators, the relation is dominated by scatter. However, we are able to state that the <span class="hlt">solar</span> <span class="hlt">activity</span> level derived from Virgo data is consistent with the majority of stars with similar rotation periods in our sample. Finally, our KOI sample is consistently approximately 0.3 dex more variable than our non-KOIs; we ascribe the difference to a selection effect due to low orbital obliquity in the planet-hosting stars and derive a mean obliquity for our sample of χ = 6+5°-6, similar to that seen in the <span class="hlt">solar</span> system.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017EGUGA..1917470P','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017EGUGA..1917470P"><span>Is tropospheric weather <span class="hlt">influenced</span> by <span class="hlt">solar</span> wind through atmospheric vertical coupling downward control?</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Prikryl, Paul; Tsukijihara, Takumi; Iwao, Koki; Muldrew, Donald B.; Bruntz, Robert; Rušin, Vojto; Rybanský, Milan; Turňa, Maroš; Šťastný, Pavel; Pastirčák, Vladimír</p> <p>2017-04-01</p> <p> (Prikryl et al., Ann. Geophys., 27, 31-57, 2009). It is primarily the energy provided by release of latent heat that leads to intensification of storms. These results indicate that vertical coupling in the atmosphere exerts downward control from <span class="hlt">solar</span> wind to the lower atmospheric levels <span class="hlt">influencing</span> tropospheric weather development.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/20160010512','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/20160010512"><span><span class="hlt">Solar</span> <span class="hlt">Activity</span> Studies using Microwave Imaging Observations</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Gopalswamy, N.</p> <p>2016-01-01</p> <p>We report on the status of <span class="hlt">solar</span> cycle 24 based on polar prominence eruptions (PEs) and microwave brightness enhancement (MBE) information obtained by the Nobeyama radioheliograph. The north polar region of the Sun had near-zero field strength for more than three years (2012-2015) and ended only in September 2015 as indicated by the presence of polar PEs and the lack of MBE. The zero-polar-field condition in the south started only around 2013, but it ended by June 2014. Thus the asymmetry in the times of polarity reversal switched between cycle 23 and 24. The polar MBE is a good proxy for the polar magnetic field strength as indicated by the high degree of correlation between the two. The cross-correlation between the high- and low-latitude MBEs is significant for a lag of approximately 5.5 to 7.3 years, suggesting that the polar field of one cycle indicates the sunspot number of the next cycle in agreement with the Babcock-Leighton mechanism of <span class="hlt">solar</span> cycles. The extended period of near-zero field in the north-polar region should result in a weak and delayed sunspot <span class="hlt">activity</span> in the northern hemisphere in cycle 25.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2014AdSpR..54..185B','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2014AdSpR..54..185B"><span>Ionospheric disturbances under low <span class="hlt">solar</span> <span class="hlt">activity</span> conditions</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Buresova, D.; Lastovicka, J.; Hejda, P.; Bochnicek, J.</p> <p>2014-07-01</p> <p>The paper is focused on ionospheric response to occasional magnetic disturbances above selected ionospheric stations located at middle latitudes of the Northern and Southern Hemisphere under extremely low <span class="hlt">solar</span> <span class="hlt">activity</span> conditions of 2007-2009. We analyzed changes in the F2 layer critical frequency foF2 and the F2 layer peak height hmF2 against 27-days running mean obtained for different longitudinal sectors of both hemispheres for the initial, main and recovery phases of selected magnetic disturbances. Our analysis showed that the effects on the middle latitude ionosphere of weak-to-moderate CIR-related magnetic storms, which mostly occur around <span class="hlt">solar</span> minimum period, could be comparable with the effects of strong magnetic storms. In general, both positive and negative deviations of foF2 and hmF2 have been observed independent on season and location. However positive effects on foF2 prevailed and were more significant. Observations of stormy ionosphere also showed large departures from the climatology within storm recovery phase, which are comparable with those usually observed during the storm main phase. The IRI STORM model gave no reliable corrections of foF2 for analyzed events.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017AGUFMSH21A2647M','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017AGUFMSH21A2647M"><span>The role of MEXART in the National Space Weather Laboratory of Mexico: Detection of <span class="hlt">solar</span> wind, CMEs, ionosphere, <span class="hlt">active</span> regions and flares.</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Mejia-Ambriz, J.; Gonzalez-Esparza, A.; De la Luz, V.; Villanueva-Hernandez, P.; Andrade, E.; Aguilar-Rodriguez, E.; Chang, O.; Romero Hernandez, E.; Sergeeva, M. A.; Perez Alanis, C. A.; Reyes-Marin, P. A.</p> <p>2017-12-01</p> <p>The National Space Weather Laboratory - Laboratorio Nacional de Clima Espacial (LANCE) - of Mexico has different ground based instruments to study and monitor the space weather. One of these instruments is the Mexican Array Radio Telescope (MEXART) which is principally dedicated to remote sensing the <span class="hlt">solar</span> wind and coronal mass ejections (CMEs) at 140 MHz, the instrument can detect <span class="hlt">solar</span> wind densities and speeds from about 0.4 to 1 AU by modeling observations of interplanetary scintillation (IPS). MEXART is also able to detect ionospheric disturbances associated with transient space weather events by the analysis of ionospheric scintillation (IONS) . Additionally, MEXART has followed the Sun since the beginning of the current <span class="hlt">Solar</span> Cycle 24 with records of 8 minutes per day, and occasionally, has partially detected the process of strong <span class="hlt">solar</span> flares. Here we show the contributions of MEXART to the LANCE by reporting recent detections of CMEs by IPS, the arrive of transient events at Earth by IONS, the <span class="hlt">influence</span> of <span class="hlt">active</span> regions in the flux of the Sun at 140 MHz and the detection of a M6.5 class flare. Furthermore we report the status of a near real time analysis of IPS data for forecast purposes and the potential contribution to the Worldwide IPS Stations network (WIPSS), which is an effort to achieve a better coverage of the <span class="hlt">solar</span> wind observations in the inner heliosphere.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://ntrs.nasa.gov/search.jsp?R=19920060693&hterms=targeting+strategy&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D90%26Ntt%3Dtargeting%2Bstrategy','NASA-TRS'); return false;" href="https://ntrs.nasa.gov/search.jsp?R=19920060693&hterms=targeting+strategy&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D90%26Ntt%3Dtargeting%2Bstrategy"><span>The role of predicted <span class="hlt">solar</span> <span class="hlt">activity</span> in TOPEX/Poseidon orbit maintenance maneuver design</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Frauenholz, Raymond B.; Shapiro, Bruce E.</p> <p>1992-01-01</p> <p>Following launch in June 1992, the TOPEX/Poseidon satellite will be placed in a near-circular frozen orbit at an altitude of about 1336 km. Orbit maintenance maneuvers are planned to assure all nodes of the 127-orbit 10-day repeat ground track remain within a 2 km equatorial longitude bandwidth. Orbit determination, maneuver execution, and atmospheric drag prediction errors limit overall targeting performance. This paper focuses on the effects of drag modeling errors, with primary emphasis on the role of SESC <span class="hlt">solar</span> <span class="hlt">activity</span> predictions, especially the 27-day outlook of the 10.7 cm <span class="hlt">solar</span> flux and geomagnetic index used by a simplified version of the Jacchia-Roberts density model developed for this TOPEX/Poseidon application. For data evaluated from 1983-90, the SESC outlook performed better than a simpler persistence strategy, especially during the first 7-10 days. A targeting example illustrates the use of ground track biasing to compensate for expected orbit predictions errors, emphasizing the role of <span class="hlt">solar</span> <span class="hlt">activity</span> prediction errors.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2018JAsGe...7...15H','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2018JAsGe...7...15H"><span>Forecasting the peak of the present <span class="hlt">solar</span> <span class="hlt">activity</span> cycle 24</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Hamid, R. H.; Marzouk, B. A.</p> <p>2018-06-01</p> <p><span class="hlt">Solar</span> forecasting of the level of sun <span class="hlt">Activity</span> is very important subject for all space programs. Most predictions are based on the physical conditions prevailing at or before the <span class="hlt">solar</span> cycle minimum preceding the maximum in question. Our aim is to predict the maximum peak of cycle 24 using precursor techniques in particular those using spotless event, geomagnetic aamin. index and <span class="hlt">solar</span> flux F10.7. Also prediction of exact date of the maximum (Tr) is taken in consideration. A study of variation over previous spotless event for cycles 7-23 and that for even cycles (8-22) are carried out for the prediction. Linear correlation between maximum of <span class="hlt">solar</span> cycles (RM) and spotless event around the preceding minimum gives R24t = 88.4 with rise time Tr = 4.6 years. For the even cycles R24E = 77.9 with rise time Tr = 4.5 y's. Based on the average aamin. index for cycles (12-23), we estimate the expected amplitude for cycle 24 to be Raamin = 99.4 and 98.1 with time rise of Traamin = 4.04 & 4.3 years for both the total and even cycles in consecutive. The application of the data of <span class="hlt">solar</span> flux F10.7 which cover only cycles (19-23) was taken in consideration and gives predicted maximum amplitude R24 10.7 = 126 with rise time Tr107 = 3.7 years, which are over estimation. Our result indicating to somewhat weaker of cycle 24 as compared to cycles 21-23.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2008PFR.....2S1012S','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2008PFR.....2S1012S"><span>Multi-Wavelength Imaging of <span class="hlt">Solar</span> Plasma - High-Beta Disruption Model of <span class="hlt">Solar</span> Flares -</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Shibasaki, Kiyoto</p> <p></p> <p><span class="hlt">Solar</span> atmosphere is filled with plasma and magnetic field. <span class="hlt">Activities</span> in the atmosphere are due to plasma instabilities in the magnetic field. To understand the physical mechanisms of <span class="hlt">activities</span> / instabilities, it is necessary to know the physical conditions of magnetized plasma, such as temperature, density, magnetic field, and their spatial structures and temporal developments. Multi-wavelength imaging is essential for this purpose. Imaging observations of the Sun at microwave, X-ray, EUV and optical ranges are routinely going on. Due to free exchange of original data among <span class="hlt">solar</span> physics and related field communities, we can easily combine images covering wide range of spectrum. Even under such circumstances, we still do not understand the cause of <span class="hlt">activities</span> in the <span class="hlt">solar</span> atmosphere well. The current standard model of <span class="hlt">solar</span> <span class="hlt">activities</span> is based on magnetic reconnection: release of stored magnetic energy by reconnection is the cause of <span class="hlt">solar</span> <span class="hlt">activities</span> on the Sun such as <span class="hlt">solar</span> flares. However, recent X-ray, EUV and microwave observations with high spatial and temporal resolution show that dense plasma is involved in <span class="hlt">activities</span> from the beginning. Based on these observations, I propose a high-beta model of <span class="hlt">solar</span> <span class="hlt">activities</span>, which is very similar to high-beta disruptions in magnetically confined fusion experiments.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.osti.gov/servlets/purl/1033557','SCIGOV-STC'); return false;" href="https://www.osti.gov/servlets/purl/1033557"><span><span class="hlt">Solar</span> Design Workbook</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>Franta, G.; Baylin, F.; Crowther, R.</p> <p>1981-06-01</p> <p>This <span class="hlt">Solar</span> Design Workbook presents <span class="hlt">solar</span> building design applications for commercial buildir^s. The book is divided into four sections. The first section describes the variety of <span class="hlt">solar</span> applications in buildings including conservation aspects, <span class="hlt">solar</span> fundamentals, passive systems, <span class="hlt">active</span> systems, daylighting, and other <span class="hlt">solar</span> options. <span class="hlt">Solar</span> system design evaluation techniques including considerations for building energy requirements, passive systems, <span class="hlt">active</span> systems, and economics are presented in Section II. The third section attempts to assist the designer in the building design process for energy conservation and <span class="hlt">solar</span> applications including options and considerations for pre-design, design, and post-design phases. The information required for themore » <span class="hlt">solar</span> design proee^ has not been fully developed at this time. Therefore, Section III is incomplete, but an overview of the considerations with some of the design proces elements is presented. Section IV illustrates ease studies that utilize <span class="hlt">solar</span> applications in the building design.« less</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2015CliPD..11.4833C','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2015CliPD..11.4833C"><span><span class="hlt">Solar</span> modulation of flood frequency in Central Europe during spring and summer on inter-annual to millennial time-scales</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Czymzik, M.; Muscheler, R.; Brauer, A.</p> <p>2015-10-01</p> <p><span class="hlt">Solar</span> <span class="hlt">influences</span> on climate variability are one of the most controversially discussed topics in climate research. We analyze <span class="hlt">solar</span> forcing of flood frequency in Central Europe on inter-annual to millennial time-scales using daily discharge data of River Ammer (southern Germany) back to AD 1926 and revisiting the 5500 year flood layer time-series from varved sediments of the downstream Lake Ammersee. Flood frequency in the discharge record is significantly correlated to changes in <span class="hlt">solar</span> <span class="hlt">activity</span> during <span class="hlt">solar</span> cycles 16-23 (r = -0.47, p < 0.0001, n = 73). Flood layer frequency (n = 1501) in the sediment record depicts distinct multi-decadal variability and significant correlations to 10Be fluxes from a Greenland ice core (r = 0.45, p < 0.0001) and 14C production rates (r =0.36, p < 0.0001), proxy records of <span class="hlt">solar</span> <span class="hlt">activity</span>. Flood frequency is higher when <span class="hlt">solar</span> <span class="hlt">activity</span> is reduced. These correlations between flood frequency and <span class="hlt">solar</span> <span class="hlt">activity</span> might provide empirical support for the <span class="hlt">solar</span> top-down mechanism expected to modify the mid-latitude storm tracks over Europe by model studies. A lag of flood frequency responses in the Ammer discharge record to changes in <span class="hlt">solar</span> <span class="hlt">activity</span> of about one to three years could be explained by a modelled ocean-atmosphere feedback delaying the atmospheric reaction to <span class="hlt">solar</span> <span class="hlt">activity</span> variations up to a few years.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017JGRD..12210369D','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017JGRD..12210369D"><span><span class="hlt">Influence</span> of <span class="hlt">Solar</span> and Lunar Tides on the Mesopause Region as Observed in Polar Mesosphere Summer Echoes Characteristics</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Dalin, P.; Kirkwood, S.; Pertsev, N.; Perminov, V.</p> <p>2017-10-01</p> <p>Long-term observations of polar mesosphere summer echoes (PMSE) from 2002 to 2012 are investigated with the aim to statistically study the effects of <span class="hlt">solar</span> thermal migrating and lunar gravitational tides on aerosol layers and their environment at altitudes 80-90 km. The <span class="hlt">solar</span> and lunar tidal periodicities are clearly present in PMSE data. For the first time, both amplitudes and phases of <span class="hlt">solar</span> and lunar tides are estimated using PMSE data from the ESRAD radar located at Esrange (Sweden). The diurnal, semidiurnal, and terdiurnal <span class="hlt">solar</span> migrating tides show pronounced periodicities in the PMSE strength and wind velocity components. Lunar tides demonstrate clear oscillations in the PMSE strength and wind velocities as well. "canonical" lunar gravitational tides, corresponding to the lunar gravitational potential, produce rather large amplitudes and are comparable to the <span class="hlt">solar</span> thermal tides, whereas "noncanonical" lunar oscillations have minor effects on PMSE layers, but are still statistically significant. The <span class="hlt">influence</span> of diurnal/semidiurnal tides and monthly/semimonthly tidal components is studied separately. Our estimations of <span class="hlt">solar</span> thermal and lunar tidal amplitudes are in good agreement with those of previous model and experimental studies. A new mechanism of quadratic demodulation of the <span class="hlt">solar</span> semidiurnal and lunar semidiurnal tides is shown to be valid at the summer mesopause and can explain periodical PMSE oscillations due to the lunar synodic semimonthly tide with period of 14.77 days. Two harmonics with periods of 27.0 and 13.5 days supposedly representing the <span class="hlt">solar</span> rotation cycle are also clearly present in PMSE data.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017ApJ...835...61Z','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017ApJ...835...61Z"><span>Chromospherically <span class="hlt">Active</span> Stars in the RAVE Survey. II. Young Dwarfs in the <span class="hlt">Solar</span> Neighborhood</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Žerjal, M.; Zwitter, T.; Matijevič, G.; Grebel, E. K.; Kordopatis, G.; Munari, U.; Seabroke, G.; Steinmetz, M.; Wojno, J.; Bienaymé, O.; Bland-Hawthorn, J.; Conrad, C.; Freeman, K. C.; Gibson, B. K.; Gilmore, G.; Kunder, A.; Navarro, J.; Parker, Q. A.; Reid, W.; Siviero, A.; Watson, F. G.; Wyse, R. F. G.</p> <p>2017-01-01</p> <p>A large sample of over 38,000 chromospherically <span class="hlt">active</span> candidate <span class="hlt">solar</span>-like stars and cooler dwarfs from the RAVE survey is addressed in this paper. An improved <span class="hlt">activity</span> identification with respect to the previous study was introduced to build a catalog of field stars in the <span class="hlt">solar</span> neighborhood with an excess emission flux in the calcium infrared triplet wavelength region. The central result of this work is the calibration of the age-<span class="hlt">activity</span> relation for main-sequence dwarfs in a range from a few 10 {Myr} up to a few Gyr. It enabled an order of magnitude age estimation of the entire <span class="hlt">active</span> sample. Almost 15,000 stars are shown to be younger than 1 {Gyr} and ˜2000 younger than 100 {Myr}. The young age of the most <span class="hlt">active</span> stars is confirmed by their position off the main sequence in the J - K versus {N}{UV}-V diagram showing strong ultraviolet excess, mid-infrared excess in the J - K versus {W}1-{W}2 diagram, and very cool temperatures (J-K> 0.7). They overlap with the reference pre-main-sequence RAVE stars often displaying X-ray emission. The <span class="hlt">activity</span> level increasing with the color reveals their different nature from the <span class="hlt">solar</span>-like stars and probably represents an underlying dynamo-generating magnetic fields in cool stars. Of the RAVE objects from DR5, 50% are found in the TGAS catalog and supplemented with accurate parallaxes and proper motions by Gaia. This makes the database of a large number of young stars in a combination with RAVE’s radial velocities directly useful as a tracer of the very recent large-scale star formation history in the <span class="hlt">solar</span> neighborhood. The data are available online in the Vizier database.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://ntrs.nasa.gov/search.jsp?R=19780039118&hterms=Krieger&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D30%26Ntt%3DKrieger','NASA-TRS'); return false;" href="https://ntrs.nasa.gov/search.jsp?R=19780039118&hterms=Krieger&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D30%26Ntt%3DKrieger"><span>The gross energy balance of <span class="hlt">solar</span> <span class="hlt">active</span> regions</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Evans, K. D.; Pye, J. P.; Hutcheon, R. J.; Gerassimenko, M.; Krieger, A. S.; Davis, J. M.; Vesecky, J. F.</p> <p>1977-01-01</p> <p>Parker's (1974) model in which sunspots denote regions of increased heat transport from the convection zone is briefly described. The amount of excess mechanically transported power supposed to be delivered to the atmosphere is estimated for a typical <span class="hlt">active</span> region, and the total radiative power output of the <span class="hlt">active</span>-region atmosphere is computed. It is found that only a very small fraction (about 0.001) of the sunspot 'missing flux' can be accounted for by radiative emission from the atmosphere above a spot group in the manner suggested by Parker. The power-loss mechanism associated with mass loss to the <span class="hlt">solar</span> wind is briefly considered and shown not to be sufficient to account for the sunspot missing flux.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2002AstHe..95..179T','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2002AstHe..95..179T"><span>Observation of the total <span class="hlt">solar</span> eclipse on 21 June 2001 in Zambia</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Takahashi, Noritsugu; Yumoto, Kiyohumi; Ichimoto, Kiyoshi</p> <p>2002-04-01</p> <p>On 21 June 2001, path of totality in Angola, Zambia, Zimbabwe, Mozambique, and Madagascar in Africa. The Japan Scientific Observation Team, consisting primarily of the members of the <span class="hlt">Solar</span> Eclipse Subcommittee of the Committee for International Collaboration in Astronomy of the Science Council of JAPAN, visited Lusaka in Zambia to observe the total <span class="hlt">solar</span> eclipse. Blessed with fine weather, the observation was successful. The outline of the <span class="hlt">influence</span> of <span class="hlt">solar</span> eclipse on the terrestrial magnetism, polarization of the flash spectrum, and other observation data, as well as the way educational <span class="hlt">activities</span> were carried out, are reported.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2013AGUSMSA21A..03V','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2013AGUSMSA21A..03V"><span>Changes of Linearity in MF2 Index with R12 and <span class="hlt">Solar</span> <span class="hlt">Activity</span> Maximum</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Villanueva, L.</p> <p>2013-05-01</p> <p>Critical frequency of F2 layer is related to the <span class="hlt">solar</span> <span class="hlt">activity</span>, and the sunspot number has been the standard index for ionospheric prediction programs. This layer, being considered the most important in HF radio communications due to its highest electron density, determines the maximum frequency coming back from ground base transmitter signals, and shows irregular variation in time and space. Nowadays the spatial variation, better understood due to the availability of TEC measurements, let Space Weather Centers have observations almost in real time. However, it is still the most difficult layer to predict in time. Short time variations are improved in IRI model, but long term predictions are only related to the well-known CCIR and URSI coefficients and <span class="hlt">Solar</span> <span class="hlt">activity</span> R12 predictions, (or ionospheric indexes in regional models). The concept of the "saturation" of the ionosphere is based on data observations around 3 <span class="hlt">solar</span> cycles before 1970, (NBS, 1968). There is a linear relationship among MUF (0Km) and R12, for smooth Sunspot numbers R12 less than 100, but constant for higher R12, so, no rise of MUF is expected for R12 higher than 100. This recommendation has been used in most of the known Ionospheric prediction programs for HF Radio communication. In this work, observations of smoothed ionospheric index MF2 related to R12 are presented to find common features of the linear relationship, which is found to persist in different ranges of R12 depending on the specific maximum level of each <span class="hlt">solar</span> cycle. In the analysis of individual <span class="hlt">solar</span> cycles, the lapse of linearity is less than 100 for a low <span class="hlt">solar</span> cycle and higher than 100 for a high <span class="hlt">solar</span> cycle. To improve ionospheric predictions we can establish levels for <span class="hlt">solar</span> cycle maximum sunspot numbers R12 around low 100, medium 150 and high 200 and specify the ranges of linearity of MUF(0Km) related to R12 which is not only 100 as assumed for all the <span class="hlt">solar</span> cycles. For lower levels of <span class="hlt">solar</span> cycle, discussions of present</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.osti.gov/biblio/22663416-understanding-solar-cycle-variability','SCIGOV-STC'); return false;" href="https://www.osti.gov/biblio/22663416-understanding-solar-cycle-variability"><span>Understanding <span class="hlt">Solar</span> Cycle Variability</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>Cameron, R. H.; Schüssler, M., E-mail: cameron@mps.mpg.de</p> <p></p> <p>The level of <span class="hlt">solar</span> magnetic <span class="hlt">activity</span>, as exemplified by the number of sunspots and by energetic events in the corona, varies on a wide range of timescales. Most prominent is the 11-year <span class="hlt">solar</span> cycle, which is significantly modulated on longer timescales. Drawing from dynamo theory, together with the empirical results of past <span class="hlt">solar</span> <span class="hlt">activity</span> and similar phenomena for <span class="hlt">solar</span>-like stars, we show that the variability of the <span class="hlt">solar</span> cycle can be essentially understood in terms of a weakly nonlinear limit cycle affected by random noise. In contrast to ad hoc “toy models” for the <span class="hlt">solar</span> cycle, this leads to amore » generic normal-form model, whose parameters are all constrained by observations. The model reproduces the characteristics of the variable <span class="hlt">solar</span> <span class="hlt">activity</span> on timescales between decades and millennia, including the occurrence and statistics of extended periods of very low <span class="hlt">activity</span> (grand minima). Comparison with results obtained with a Babcock–Leighton-type dynamo model confirm the validity of the normal-mode approach.« less</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2016cosp...41E.441D','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2016cosp...41E.441D"><span>On the Dependence of the Ionospheric E-Region Electric Field of the <span class="hlt">Solar</span> <span class="hlt">Activity</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Denardini, Clezio Marcos; Schuch, Nelson Jorge; Moro, Juliano; Araujo Resende, Laysa Cristina; Chen, Sony Su; Costa, D. Joaquim</p> <p>2016-07-01</p> <p>We have being studying the zonal and vertical E region electric field components inferred from the Doppler shifts of type 2 echoes (gradient drift irregularities) detected with the 50 MHz backscatter coherent (RESCO) radar set at Sao Luis, Brazil (SLZ, 2.3° S, 44.2° W) during the <span class="hlt">solar</span> cycle 24. In this report we present the dependence of the vertical and zonal components of this electric field with the <span class="hlt">solar</span> <span class="hlt">activity</span>, based on the <span class="hlt">solar</span> flux F10.7. For this study we consider the geomagnetically quiet days only (Kp <= 3+). A magnetic field-aligned-integrated conductivity model was developed for proving the conductivities, using the IRI-2007, the MISIS-2000 and the IGRF-11 models as input parameters for ionosphere, neutral atmosphere and Earth magnetic field, respectively. The ion-neutron collision frequencies of all the species are combined through the momentum transfer collision frequency equation. The mean zonal component of the electric field, which normally ranged from 0.19 to 0.35 mV/m between the 8 and 18 h (LT) in the Brazilian sector, show a small dependency with the <span class="hlt">solar</span> <span class="hlt">activity</span>. Whereas, the mean vertical component of the electric field, which normally ranges from 4.65 to 10.12 mV/m, highlight the more pronounced dependency of the <span class="hlt">solar</span> flux.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/20170005305','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/20170005305"><span>The MSFC <span class="hlt">Solar</span> <span class="hlt">Activity</span> Future Estimation (MSAFE) Model</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Suggs, Ronnie J.</p> <p>2017-01-01</p> <p>The MSAFE model provides forecasts for the <span class="hlt">solar</span> indices SSN, F10.7, and Ap. These <span class="hlt">solar</span> indices are used as inputs to many space environment models used in orbital spacecraft operations and space mission analysis. Forecasts from the MSAFE model are provided on the MSFC Natural Environments Branch's <span class="hlt">solar</span> webpage and are updated as new monthly observations come available. The MSAFE prediction routine employs a statistical technique that calculates deviations of past <span class="hlt">solar</span> cycles from the mean cycle and performs a regression analysis to predict the deviation from the mean cycle of the <span class="hlt">solar</span> index at the next future time interval. The prediction algorithm is applied recursively to produce monthly smoothed <span class="hlt">solar</span> index values for the remaining of the cycle. The forecasts are initiated for a given cycle after about 8 to 12 months of observations are collected. A forecast made at the beginning of cycle 24 using the MSAFE program captured the cycle fairly well with some difficulty in discerning the double peak that occurred at <span class="hlt">solar</span> cycle maximum.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/20170005363','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/20170005363"><span>The MSFC <span class="hlt">Solar</span> <span class="hlt">Activity</span> Future Estimation (MSAFE) Model</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Suggs, Ron</p> <p>2017-01-01</p> <p>The Natural Environments Branch of the Engineering Directorate at Marshall Space Flight Center (MSFC) provides <span class="hlt">solar</span> cycle forecasts for NASA space flight programs and the aerospace community. These forecasts provide future statistical estimates of sunspot number, <span class="hlt">solar</span> radio 10.7 cm flux (F10.7), and the geomagnetic planetary index, Ap, for input to various space environment models. For example, many thermosphere density computer models used in spacecraft operations, orbital lifetime analysis, and the planning of future spacecraft missions require as inputs the F10.7 and Ap. The <span class="hlt">solar</span> forecast is updated each month by executing MSAFE using historical and the latest month's observed <span class="hlt">solar</span> indices to provide estimates for the balance of the current <span class="hlt">solar</span> cycle. The forecasted <span class="hlt">solar</span> indices represent the 13-month smoothed values consisting of a best estimate value stated as a 50 percentile value along with approximate +/- 2 sigma values stated as 95 and 5 percentile statistical values. This presentation will give an overview of the MSAFE model and the forecast for the current <span class="hlt">solar</span> cycle.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2014Ge%26Ae..54..633G','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2014Ge%26Ae..54..633G"><span>Estimate of the effect of the 11-year <span class="hlt">solar</span> <span class="hlt">activity</span> cycle on the ozone content in the stratosphere</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Gruzdev, A. N.</p> <p>2014-09-01</p> <p>Using spectral, cross-spectral, and regression methods, we analyzed the effect of the 11-year cycle of <span class="hlt">solar</span> <span class="hlt">activity</span> on the ozone content in the stratosphere and lower mesosphere via satellite measurement data obtained with the help of SBUV/SBUV2 instruments in 1978-2003. We revealed a high coherence between the ozone content and <span class="hlt">solar</span> <span class="hlt">activity</span> level on the <span class="hlt">solar</span> cycle scale. In much of this area, the ozone content varies approximately in phase with the <span class="hlt">solar</span> cycle; however, in areas of significant gradients of ozone mixing ratio in the middle stratosphere, the phase shift between ozone and <span class="hlt">solar</span> oscillations can be considerable, up to π/2. This can be caused by dynamical processes. The altitude maxima of ozone sensitivity to the 11-year <span class="hlt">solar</span> cycle were found in the upper vicinity of the stratopause (50-55 km), in the middle stratosphere (35-40 km), and the lower stratosphere (below 25 km). Maximal changes in ozone content in the <span class="hlt">solar</span> cycle (up to 10% and more) were found in winter and spring in polar regions.</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('http://adsabs.harvard.edu/abs/2017Ge%26Ae..57..896P','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017Ge%26Ae..57..896P"><span>Cyclotron Line in <span class="hlt">Solar</span> Microwave Radiation by Radio Telescope RATAN-600 Observations of the <span class="hlt">Solar</span> <span class="hlt">Active</span> Region NOAA 12182</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Peterova, N. G.; Topchilo, N. A.</p> <p>2017-12-01</p> <p>This paper presents the results of observation of a rare phenomenon—a narrowband increase in the brightness of cyclotron radiation of one of the structural details of a radio source located in the <span class="hlt">solar</span> corona above the <span class="hlt">solar</span> <span class="hlt">active</span> region NOAA 12182 in October 2014 at a frequency of 4.2 ± 0.1 GHz. The brightness of radiation in the maximum of the phenomenon has reached 10 MK; its duration was equal to 3 s. The exact location of the source of the narrowband cyclotron radiation is indicated: it is a corona above a fragmented (4-nuclear) sunspot, on which a small UV flare loop was closed.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2009ClDy...32....1S','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2009ClDy...32....1S"><span><span class="hlt">Influence</span> of the 11-year <span class="hlt">solar</span> cycle on the effects of the equatorial quasi-biennial oscillation, manifesting in the extratropical northern atmosphere</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Sitnov, S. A.</p> <p>2009-01-01</p> <p>Using the longest and most reliable ozonesonde data sets grouped for four regions (Japan, Europe, as well as temperate and polar latitudes of Canada) the comparative analysis of regional responses of ozone, temperature, horizontal wind, tropopause and surface pressure on the equatorial quasi-biennial oscillation (QBO effects), manifesting in opposite phases of the 11-year <span class="hlt">solar</span> cycle (11-yr SC) was carried out. The impact of <span class="hlt">solar</span> cycle is found to be the strongest at the Canadian Arctic, near one of two climatological centres of polar vortex, where in <span class="hlt">solar</span> maximum conditions the QBO signals in ozone and temperature have much larger amplitudes, embrace greater range of heights, and are maximized much higher than those in <span class="hlt">solar</span> minimum conditions. The strengthening of the temperature QBO effect during <span class="hlt">solar</span> maxima can explain why correlation between the 11-yr SC and polar winter stratospheric temperature is reversed in the opposite QBO phases. At the border of polar vortex the 11-yr SC also modulates the QBO effect in zonal wind, strengthening the quasi-biennial modulation of polar vortex during <span class="hlt">solar</span> maxima that is associated with strong negative correlation between stratospheric QBO signals in zonal wind and temperature. Above Japan the QBO effects of ozone, temperature, and zonal wind, manifesting in <span class="hlt">solar</span> maxima reveal the downward phase dynamics, reminding similar feature of the zonal wind in the equatorial stratosphere. Above Europe, the QBO effects in <span class="hlt">solar</span> maxima reveal more similarity with those above Japan, while in <span class="hlt">solar</span> minima with the effects obtained at the Canadian middle-latitude stations. It is revealed that the 11-yr SC <span class="hlt">influences</span> regional QBO effects in tropopause height, tropopause temperature and surface pressure. The <span class="hlt">influence</span> most distinctly manifest itself in tropopause characteristics above Japan. The results of the accompanying analysis of the QBO reference time series testify that in the period of 1965-2006 above 50-hPa level the duration</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://ntrs.nasa.gov/search.jsp?R=19920016082&hterms=activity+Physics&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D70%26Ntt%3Dactivity%2BPhysics','NASA-TRS'); return false;" href="https://ntrs.nasa.gov/search.jsp?R=19920016082&hterms=activity+Physics&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D70%26Ntt%3Dactivity%2BPhysics"><span>Report of the <span class="hlt">solar</span> physics panel</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Withbroe, George L.; Fisher, Richard R.; Antiochos, Spiro; Brueckner, Guenter; Hoeksema, J. Todd; Hudson, Hugh; Moore, Ronald; Radick, Richard R.; Rottman, Gary; Scherrer, Philip</p> <p>1991-01-01</p> <p>Recent accomplishments in <span class="hlt">solar</span> physics can be grouped by the three regions of the Sun: the <span class="hlt">solar</span> interior, the surface, and the exterior. The future scientific problems and areas of interest involve: generation of magnetic <span class="hlt">activity</span> cycle, energy storage and release, <span class="hlt">solar</span> <span class="hlt">activity</span>, <span class="hlt">solar</span> wind and <span class="hlt">solar</span> interaction. Finally, the report discusses a number of future space mission concepts including: High Energy <span class="hlt">Solar</span> Physics Mission, Global <span class="hlt">Solar</span> Mission, Space Exploration Initiative, <span class="hlt">Solar</span> Probe Mission, <span class="hlt">Solar</span> Variability Explorer, Janus, as well as <span class="hlt">solar</span> physics on Space Station Freedom.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/15835175','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/15835175"><span>Property <span class="hlt">influence</span> of polyanilines on photovoltaic behaviors of dye-sensitized <span class="hlt">solar</span> cells.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Tan, Shuxin; Zhai, Jin; Xue, Bofei; Wan, Meixiang; Meng, Qingbo; Li, Yuliang; Jiang, Lei; Zhu, Daoben</p> <p>2004-03-30</p> <p>The <span class="hlt">influence</span> of polyanilines (PANIs) as hole conductors on the photovoltaic behaviors of dye-sensitized <span class="hlt">solar</span> cells is studied. The current-voltage (I-V) characteristics and the incident photon to current conversion efficiency (IPCE) curves of the devices are determined as the function of different conductivities and morphologies of PANIs. The results show that the conductivity of PANIs affects the performance of the devices greatly, and PANI with the intermediate conductivity value (3.5 S/cm) is optimum. In addition, the effects of both the film formation property and the cluster size of polyanilines on the photovoltaic behaviors of the devices are also discussed.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2018ACP....18.3363G','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2018ACP....18.3363G"><span><span class="hlt">Influence</span> of geomagnetic <span class="hlt">activity</span> on mesopause temperature over Yakutia</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Gavrilyeva, Galina; Ammosov, Petr</p> <p>2018-03-01</p> <p>The long-term temperature changes of the mesopause region at the hydroxyl molecule OH (6-2) nighttime height and its connection with the geomagnetic <span class="hlt">activity</span> during the 23rd and beginning of the 24th <span class="hlt">solar</span> cycles are presented. Measurements were conducted with an infrared digital spectrograph at the Maimaga station (63° N, 129.5° E). The hydroxyl rotational temperature (TOH) is assumed to be equal to the neutral atmosphere temperature at the altitude of ˜ 87 km. The average temperatures obtained for the period 1999 to 2015 are considered. The season of observations starts at the beginning of August and lasts until the middle of May. The maximum of the seasonally averaged temperatures is delayed by 2 years relative to the maximum of the <span class="hlt">solar</span> radio emission flux (wavelength of 10.7 cm), and correlates with a change in geomagnetic <span class="hlt">activity</span> (Ap index). Temperature grouping in accordance with the geomagnetic <span class="hlt">activity</span> level showed that in years with high <span class="hlt">activity</span> (Ap > 8), the mesopause temperature from October to February is about 10 K higher than in years with low <span class="hlt">activity</span> (Ap < = 8). Cross-correlation analysis showed no temporal shift between geomagnetic <span class="hlt">activity</span> and temperature. The correlation coefficient is equal to 0.51 at the 95 % level.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/20030002519','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/20030002519"><span>SORCE: <span class="hlt">Solar</span> Radiation and Climate Experiment</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Cahalan, Robert; Rottman, Gary; Lau, William K. M. (Technical Monitor)</p> <p>2002-01-01</p> <p>Contents include the following: Understanding the Sun's <span class="hlt">influence</span> on the Earth; How the Sun affect Earth's climate; By how much does the Sun's radiation very; Understanding <span class="hlt">Solar</span> irradiance; History of <span class="hlt">Solar</span> irradiance observations; The SORCE mission; How do the SORCE instruments measure <span class="hlt">solar</span> radiation; Total irradiance monitor (TIM); Spectral irradiance monitor (SIM); <span class="hlt">Solar</span> stellar irradiance comparison experiment (SOLSTICE); XUV photometer system (XPS).</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/29422633','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/29422633"><span>Long-Term Study of Heart Rate Variability Responses to Changes in the <span class="hlt">Solar</span> and Geomagnetic Environment.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Alabdulgader, Abdullah; McCraty, Rollin; Atkinson, Michael; Dobyns, York; Vainoras, Alfonsas; Ragulskis, Minvydas; Stolc, Viktor</p> <p>2018-02-08</p> <p>This long-term study examined relationships between <span class="hlt">solar</span> and magnetic factors and the time course and lags of autonomic nervous system (ANS) responses to changes in <span class="hlt">solar</span> and geomagnetic <span class="hlt">activity</span>. Heart rate variability (HRV) was recorded for 72 consecutive hours each week over a five-month period in 16 participants in order to examine ANS responses during normal background environmental periods. HRV measures were correlated with <span class="hlt">solar</span> and geomagnetic variables using multivariate linear regression analysis with Bonferroni corrections for multiple comparisons after removing circadian <span class="hlt">influences</span> from both datasets. Overall, the study confirms that daily ANS <span class="hlt">activity</span> responds to changes in geomagnetic and <span class="hlt">solar</span> <span class="hlt">activity</span> during periods of normal undisturbed <span class="hlt">activity</span> and it is initiated at different times after the changes in the various environmental factors and persist over varying time periods. Increase in <span class="hlt">solar</span> wind intensity was correlated with increases in heart rate, which we interpret as a biological stress response. Increase in cosmic rays, <span class="hlt">solar</span> radio flux, and Schumann resonance power was all associated with increased HRV and parasympathetic <span class="hlt">activity</span>. The findings support the hypothesis that energetic environmental phenomena affect psychophysical processes that can affect people in different ways depending on their sensitivity, health status and capacity for self-regulation.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/20110013276','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/20110013276"><span>Prominences: The Key to Understanding <span class="hlt">Solar</span> <span class="hlt">Activity</span></span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Karpen, Judy T.</p> <p>2011-01-01</p> <p>Prominences are spectacular manifestations of both quiescent and eruptive <span class="hlt">solar</span> <span class="hlt">activity</span>. The largest examples can be seen with the naked eye during eclipses, making prominences among the first <span class="hlt">solar</span> features to be described and catalogued. Steady improvements in temporal and spatial resolution from both ground- and space-based instruments have led us to recognize how complex and dynamic these majestic structures really are. Their distinguishing characteristics - cool knots and threads suspended in the hot corona, alignment along inversion lines in the photospheric magnetic field within highly sheared filament channels, and a tendency to disappear through eruption - offer vital clues as to their origin and dynamic evolution. Interpreting these clues has proven to be contentious, however, leading to fundamentally different models that address the basic questions: What is the magnetic structure supporting prominences, and how does so much cool, dense plasma appear in the corona? Despite centuries of increasingly detailed observations, the magnetic and plasma structures in prominences are poorly known. Routine measurements of the vector magnetic field in and around prominences have become possible only recently, while long-term monitoring of the underlying filament-channel formation process also remains scarce. The process responsible for prominence mass is equally difficult to establish, although we have long known that the chromosphere is the only plausible source. As I will discuss, however, the motions and locations of prominence material can be used to trace the coronal field, thus defining the magnetic origins of <span class="hlt">solar</span> eruptions. A combination of observations, theory, and numerical modeling must be used to determine whether any of the competing theories accurately represents the physics of prominences. I will discuss the criteria for a successful prominence model, compare the leading models, and present in detail one promising, comprehensive scenario for</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://ntrs.nasa.gov/search.jsp?R=20080043898&hterms=anticipation&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D30%26Ntt%3Danticipation','NASA-TRS'); return false;" href="https://ntrs.nasa.gov/search.jsp?R=20080043898&hterms=anticipation&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D30%26Ntt%3Danticipation"><span>If We Can't Predict <span class="hlt">Solar</span> Cycle 24, What About <span class="hlt">Solar</span> Cycle 34?</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Pesnell. William Dean</p> <p>2008-01-01</p> <p>Predictions of <span class="hlt">solar</span> <span class="hlt">activity</span> in <span class="hlt">Solar</span> Cycle 24 range from 50% larger than SC 23 to the onset of a Grand Minimum. Because low levels of <span class="hlt">solar</span> <span class="hlt">activity</span> are associated with global cooling in paleoclimate and isotopic records, anticipating these extremes is required in any longterm extrapolation of climate variability. Climate models often look forward 100 or more years, which would mean 10 <span class="hlt">solar</span> cycles into the future. Predictions of <span class="hlt">solar</span> <span class="hlt">activity</span> are derived from a number of methods, most of which, such as climatology and physics-based models, will be familiar to atmospheric scientists. More than 50 predictions of the maximum amplitude of SC 24 published before <span class="hlt">solar</span> minimum will be discussed. Descriptions of several methods that result in the extreme predictions and some anticipation of even longer term predictions will be presented.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017BlgAJ..27...27N','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017BlgAJ..27...27N"><span>The investigation of <span class="hlt">solar</span> <span class="hlt">activity</span> signals by analyzing of tree ring chronological scales</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Nickiforov, M. G.</p> <p>2017-07-01</p> <p>The present study examines the ability of detecting short-cycles and global minima of <span class="hlt">solar</span> <span class="hlt">activity</span> by analyzing dendrochronologies. Starting with the study of Douglass, which was devoted to the question of climatic cycles and the growth of trees, it is believed that the analysis of dendrochronologies allows to detect the cycle of Wolf-Schwabe. According to his results, the cycle was absent during Maunder's minimum and appeared after its completion. Having checked Douglass's conclusions by using 10 dendrochronologies of yellow pines from Arizona, which cover the time period from 1600 to 1900, we have come to the opposite results. The verification shows that: a) none of the considered dendroscale allows to detect an 11-year cycle; 2) the behaviour of a short peroid-signal does not undergo significant changes before, during or after Maunder's minimum. A similar attempt to detect global minima of <span class="hlt">solar</span> <span class="hlt">activity</span> by using five dendrochronologies from different areas has not led to positive results. On the one hand, the signal of global extremum is not always recorded in dendrochronology, on the other hand, the deep depression of annual rings allows to suppose the existence of a global minimum of <span class="hlt">solar</span> <span class="hlt">activity</span>, which is actually absent.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2013ASPC..478..145S','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2013ASPC..478..145S"><span>Differences of the <span class="hlt">Solar</span> Magnetic <span class="hlt">Activity</span> Signature in Velocity and Intensity Helioseismic Observations</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Salabert, D.; García, R. A.; Jiménez, A.</p> <p>2013-12-01</p> <p>The high-quality, full-disk helioseismic observations continuously collected by the spectrophotometer GOLF and the three photometers VIRGO/SPMs onboard the SoHO spacecraft for 17 years now (since April 11, 1996, apart from the SoHO “vacations”) are absolutely unique for the study of the interior of the Sun and its variability with magnetic <span class="hlt">activity</span>. Here, we look at the differences in the low-degree oscillation p-mode frequencies between radial velocity and intensity measurements taking into account all the known features of the p-mode profiles (e.g., the opposite peak asymmetry), and of the power spectrum (e.g., the presence of the higher degrees ℓ = 4 and 5 in the signal). We show that the intensity frequencies are higher than the velocity frequencies during the <span class="hlt">solar</span> cycle with a clear temporal dependence. The response between the individual angular degrees is also different. Time delays are observed between the temporal variations in GOLF and VIRGO frequencies. Such analysis is important in order to put new constraints and to better understand the mechanisms responsible for the temporal variations of the oscillation frequencies with the <span class="hlt">solar</span> magnetic <span class="hlt">activity</span> as well as their height dependences in the <span class="hlt">solar</span> atmosphere. It is also important for the study of the stellar magnetic <span class="hlt">activity</span> using asteroseismic data.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2018JPhCS.993a2034S','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2018JPhCS.993a2034S"><span><span class="hlt">Influence</span> of interface layer preparation on the electrical and spectral characteristics of GaN/Si <span class="hlt">solar</span> cells</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Shugurov, K. U.; Mozharov, A. M.; Sapunov, G. A.; Fedorov, V. V.; Bolshakov, A. D.; Mukhin, I. S.</p> <p>2018-03-01</p> <p>Volt-ampere and spectral characteristics of GaN/Si <span class="hlt">solar</span> cell samples differing in interface layer preparation are obtained and analyzed. External quantum efficiency curves are experimentally determined via excitation with a 532 nm incident radiation wavelength. It is demonstrated that interface preparation has a significant <span class="hlt">influence</span> on photovoltaic characteristics of the studied samples.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017EGUGA..1913063H','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017EGUGA..1913063H"><span><span class="hlt">Solar</span> causes of strong geomagnetic disturbances during the period 1996—2013</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Hejda, Pavel; Bochníček, Josef; Valach, Fridrich; Revallo, Miloš</p> <p>2017-04-01</p> <p>The purpose of this research is to assess the contribution of CMEs and CIRs to geomagnetic <span class="hlt">activity</span> during the period 1996—2013, covering the 23rd <span class="hlt">solar</span> cycle, the <span class="hlt">solar</span> minimum between the 23rd and the 24th <span class="hlt">solar</span> cycles as well as the ascending part of the current 24th <span class="hlt">solar</span> cycle. Both CMEs and CIRs are capable of driving significant space weather effects on the Earth. Current study is not primarily aimed at construction of prediction models but can contribute to this topic by answering two principal questions: (1) what is the contribution of CME and CIR type <span class="hlt">solar</span> events to various levels of geomagnetic disturbances and how it varies during the <span class="hlt">solar</span> cycle (2) how does the successive emergence of CME and CIR events <span class="hlt">influence</span> the geomagnetic response. Sometimes it can be difficult to assign the response to a particular event properly, especially in the case of several successive events. We noticed that the CIRs appeared to play important role also in years when strongly geoeffective CMEs occurred. An interesting finding, which we have revealed on this subject, concerned the year 2009; then the extremely low geomagnetic <span class="hlt">activity</span> was probably caused by very slow <span class="hlt">solar</span> wind from coronal holes along with the rare occurrences of CIRs.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://www.dtic.mil/docs/citations/ADA497586','DTIC-ST'); return false;" href="http://www.dtic.mil/docs/citations/ADA497586"><span><span class="hlt">Influence</span> of Different <span class="hlt">Solar</span> Drivers on the Winds in the Middle Atmosphere and on Geomagnetic Disturbances</span></a></p> <p><a target="_blank" href="http://www.dtic.mil/">DTIC Science & Technology</a></p> <p></p> <p>2007-05-18</p> <p>number and intensity are highest in sunspot maximum. CME’s are considered the sources of the most intense geomagnetic storms (Gonzalez et al., 2002... storm . High speed <span class="hlt">solar</span> wind The geomagnetic <span class="hlt">activity</span> during the declining phase of the <span class="hlt">solar</span> cycle can be even higher that at sunspot maximum. In...characteristic “calm before the storm ” – the decrease a couple of days before the maximum disturbance – in the case of high speed streams (Borovsky and</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/20170005301','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/20170005301"><span>The MSFC <span class="hlt">Solar</span> <span class="hlt">Activity</span> Future Estimation (MSAFE) Model</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Suggs, Ron</p> <p>2017-01-01</p> <p>The MSAFE model provides forecasts for the <span class="hlt">solar</span> indices SSN, F10.7, and Ap. These <span class="hlt">solar</span> indices are used as inputs to space environment models used in orbital spacecraft operations and space mission analysis. Forecasts from the MSAFE model are provided on the MSFC Natural Environments Branch's <span class="hlt">solar</span> web page and are updated as new monthly observations become available. The MSAFE prediction routine employs a statistical technique that calculates deviations of past <span class="hlt">solar</span> cycles from the mean cycle and performs a regression analysis to calculate the deviation from the mean cycle of the <span class="hlt">solar</span> index at the next future time interval. The forecasts are initiated for a given cycle after about 8 to 9 monthly observations from the start of the cycle are collected. A forecast made at the beginning of cycle 24 using the MSAFE program captured the cycle fairly well with some difficulty in discerning the double peak that occurred at <span class="hlt">solar</span> cycle maximum.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2013hell.conf....8T','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2013hell.conf....8T"><span>Particle Acceleration in a Statistically Modeled <span class="hlt">Solar</span> <span class="hlt">Active</span>-Region Corona</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Toutounzi, A.; Vlahos, L.; Isliker, H.; Dimitropoulou, M.; Anastasiadis, A.; Georgoulis, M.</p> <p>2013-09-01</p> <p>Elaborating a statistical approach to describe the spatiotemporally intermittent electric field structures formed inside a flaring <span class="hlt">solar</span> <span class="hlt">active</span> region, we investigate the efficiency of such structures in accelerating charged particles (electrons). The large-scale magnetic configuration in the <span class="hlt">solar</span> atmosphere responds to the strong turbulent flows that convey perturbations across the <span class="hlt">active</span> region by initiating avalanche-type processes. The resulting unstable structures correspond to small-scale dissipation regions hosting strong electric fields. Previous research on particle acceleration in strongly turbulent plasmas provides a general framework for addressing such a problem. This framework combines various electromagnetic field configurations obtained by magnetohydrodynamical (MHD) or cellular automata (CA) simulations, or by employing a statistical description of the field's strength and configuration with test particle simulations. Our objective is to complement previous work done on the subject. As in previous efforts, a set of three probability distribution functions describes our ad-hoc electromagnetic field configurations. In addition, we work on data-driven 3D magnetic field extrapolations. A collisional relativistic test-particle simulation traces each particle's guiding center within these configurations. We also find that an interplay between different electron populations (thermal/non-thermal, ambient/injected) in our simulations may also address, via a re-acceleration mechanism, the so called `number problem'. Using the simulated particle-energy distributions at different heights of the cylinder we test our results against observations, in the framework of the collisional thick target model (CTTM) of <span class="hlt">solar</span> hard X-ray (HXR) emission. The above work is supported by the Hellenic National Space Weather Research Network (HNSWRN) via the THALIS Programme.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://eric.ed.gov/?q=race+AND+cars&id=EJ776749','ERIC'); return false;" href="https://eric.ed.gov/?q=race+AND+cars&id=EJ776749"><span><span class="hlt">Solar</span> Sprint</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>Tabor, Richard; Anderson, Stephen</p> <p>2007-01-01</p> <p>In the "<span class="hlt">Solar</span> Sprint" <span class="hlt">activity</span>, students design, test, and race a <span class="hlt">solar</span>-powered car built with Legos. The use of ratios is incorporated to simulate the actual work of scientists and engineers. This method encourages fourth-grade students to think about multiple variables and stimulates their curiosity when an <span class="hlt">activity</span> doesn't come out as…</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2014APh....55...33K','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2014APh....55...33K"><span>Long-term measurements of 36Cl to investigate potential <span class="hlt">solar</span> <span class="hlt">influence</span> on the decay rate</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Kossert, Karsten; Nähle, Ole J.</p> <p>2014-03-01</p> <p>Recently, Jenkins et al. [6] reported on fluctuations in the detected decay events of 36Cl which were measured with a Geiger-Müller counter. Experimental data of 32Si measured by means of an end-window gas-flow proportional counter at the Brookhaven National Laboratory show similar periodicity, albeit a different amplitude. Jenkins et al. interpret the fluctuations as evidence of <span class="hlt">solar</span> <span class="hlt">influence</span> on the decay rates of beta-decaying radionuclides.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/28160420','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/28160420"><span>Assessment of skin pigmentation by confocal microscopy: <span class="hlt">Influence</span> of <span class="hlt">solar</span> exposure and protection habits on cutaneous hyperchromias.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Martini, Ana Paula M; Mercurio, Daiane G; Maia Campos, Patrícia M B G</p> <p>2017-09-01</p> <p>Cutaneous hyperchromias are disorders of skin pigmentation involving an increase of melanin production and its irregular accumulation in skin cells. It is known that the use of sunscreens helps to prevent changes in the skin pigmentation pattern, but the structural and morphological alterations that occur in the different types of hyperpigmentations need better elucidation. To assess the <span class="hlt">influence</span> of <span class="hlt">solar</span> exposure and protection habits on the pattern of skin pigmentation using reflectance confocal microscopy (RCM). Forty volunteers aged 18-39 years with skin hyperpigmentation participated in the study. Skin characterization was performed by imaging techniques and by assessing the habits of <span class="hlt">solar</span> exposure and protection by applying questionnaires to the volunteers. RCM was used to record sequences of confocal sections at areas of interest and to examine cell shape and brightness in the basal cell layer of the lesion and in normal perilesional skin. Furthermore, high-resolution images were obtained for analysis of the spots. Sunlight <span class="hlt">influences</span> the number and location of spots as the face of volunteers with higher <span class="hlt">solar</span> exposure was covered with spots, whereas volunteers with less exposure had fewer spots located in the nose and cheeks region due to greater exposure of these areas to the sun. The data showed the importance of sun protection for preventing changes in the pattern of skin pigmentation, and RCM proved to be an important tool for skin characterization. © 2017 Wiley Periodicals, Inc.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://eric.ed.gov/?q=influencers&pg=3&id=ED571069','ERIC'); return false;" href="https://eric.ed.gov/?q=influencers&pg=3&id=ED571069"><span>College Student Environmental <span class="hlt">Activism</span>: How Experiences and Identities <span class="hlt">Influence</span> Environmental <span class="hlt">Activism</span> Approaches</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>King, Laura A. H.</p> <p>2016-01-01</p> <p>College student environmental <span class="hlt">activism</span> is one way students civically engage in addressing social issues. This study explores the environmental <span class="hlt">activism</span> of twelve college students and how their experiences outside of college and in college <span class="hlt">influenced</span> their <span class="hlt">activism</span>. In addition, how students' identities <span class="hlt">influenced</span> their approach to <span class="hlt">activism</span> was…</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('http://adsabs.harvard.edu/abs/2017nova.pres.1978K','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017nova.pres.1978K"><span>Simulations of <span class="hlt">Solar</span> Jets</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Kohler, Susanna</p> <p>2017-02-01</p> <p>Formation of a coronal jet from twisted field lines that have reconnected with the ambient field. The colors show the radial velocity of the plasma. [Adapted from Szente et al. 2017]How do jets emitted from the Suns surface contribute to its corona and to the <span class="hlt">solar</span> wind? In a recent study, a team of scientists performed complex three-dimensional simulations of coronal jets to answer these questions.Small ExplosionsCoronal jets are relatively small eruptions from the Suns surface, with heights of roughly 100 to 10,000 km, speeds of 10 to 1,000 km/s, and lifetimes of a few minutes to around ten hours. These jets are constantly present theyre emitted even from the quiet Sun, when <span class="hlt">activity</span> is otherwise low and weve observed them with a fleet of Sun-watching space telescopes spanning the visible, extreme ultraviolet (EUV), and X-ray wavelength bands.A comparison of simulated observations based on the authors model (left panels) to actual EUV and X-ray observations of jets (right panels). [Szente et al. 2017]Due to their ubiquity, we speculate that these jets might contribute to heating the global <span class="hlt">solar</span> corona (which is significantly hotter than the surface below it, a curiosity known as the coronal heating problem). We can also wonder what role these jets might play in driving the overall <span class="hlt">solar</span> wind.Launching a JetLed by Judit Szente (University of Michigan), a team of scientists has explored the impact of coronal jets on the global corona and <span class="hlt">solar</span> wind with a series of numerical simulations. Szente and collaborators used three-dimensional, magnetohydrodynamic simulations that provide realistic treatment of the <span class="hlt">solar</span> atmosphere, the <span class="hlt">solar</span> wind acceleration, and the complexities of heat transfer throughout the corona.In the authors simulations, a jet is initiated as a magnetic dipole rotates at the <span class="hlt">solar</span> surface, winding up field lines. Magnetic reconnection between the twisted lines and the background field then launches the jet from the dense and hot <span class="hlt">solar</span></p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/20160006934','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/20160006934"><span>Eruptions that Drive Coronal Jets in a <span class="hlt">Solar</span> <span class="hlt">Active</span> Region</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Sterling, Alphonse C.; Moore, Ronald L.; Falconer, David A.; Panesar, Navdeep K.; Akiyama, Sachiko; Yashiro, Seiji; Gopalswamy, Nat</p> <p>2016-01-01</p> <p><span class="hlt">Solar</span> coronal jets are common in both coronal holes and in <span class="hlt">active</span> regions (e.g., Shibata et al. 1992, Shimojo et al. 1996, Cirtain et al. 2007. Savcheva et al. 2007). Recently, Sterling et al. (2015), using data from Hinode/XRT and SDO/AIA, found that coronal jets originating in polar coronal holes result from the eruption of small-scale filaments (minifilaments). The jet bright point (JBP) seen in X-rays and hotter EUV channels off to one side of the base of the jet's spire develops at the location where the minifilament erupts, consistent with the JBPs being miniature versions of typical <span class="hlt">solar</span> flares that occur in the wake of large-scale filament eruptions. Here we consider whether <span class="hlt">active</span> region coronal jets also result from the same minifilament-eruption mechanism, or whether they instead result from a different mechanism (e.g. Yokoyama & Shibata 1995). We present observations of an on-disk <span class="hlt">active</span> region (NOAA AR 11513) that produced numerous jets on 2012 June 30, using data from SDO/AIA and HMI, and from GOES/SXI. We find that several of these <span class="hlt">active</span> region jets also originate with eruptions of miniature filaments (size scale 20'') emanating from small-scale magnetic neutral lines of the region. This demonstrates that <span class="hlt">active</span> region coronal jets are indeed frequently driven by minifilament eruptions. Other jets from the <span class="hlt">active</span> region were also consistent with their drivers being minifilament eruptions, but we could not confirm this because the onsets of those jets were hidden from our view. This work was supported by funding from NASA/LWS, NASA/HGI, and Hinode. A full report of this study appears in Sterling et al. (2016).</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2015EGUGA..17.8612L','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2015EGUGA..17.8612L"><span>Carbon cycle dynamics and <span class="hlt">solar</span> <span class="hlt">activity</span> embedded in a high-resolution 14C speleothem record from Belize, Central America</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Lechleitner, Franziska A.; Breitenbach, Sebastian F. M.; McIntyre, Cameron; Asmerom, Yemane; Prufer, Keith M.; Polyak, Victor; Culleton, Brendan J.; Kennett, Douglas J.; Eglinton, Timothy I.; Baldini, James U. L.</p> <p>2015-04-01</p> <p> of old recalcitrant carbon to the soil water, and resulting in closer coupling between atmosphere and cave environment. The resolution of the record (0.3-0.7 mm/sample) permits identification of the dominant drivers of stalagmite 14C during different intervals. For example, hydrologic control on 14C appears dominant during the 11th century drought, while in the 16th to 18th century a clear <span class="hlt">solar</span> <span class="hlt">influence</span> exists. <span class="hlt">Solar</span> <span class="hlt">activity</span> is reflected in YOK-I as lower a14Cinit, reflecting the atmospheric a14C. We apply simple hydrological models to investigate the different factors <span class="hlt">influencing</span> 14C in YOK-I. We estimate the importance of mean SOM age to signal dampening, and quantify the strength of the <span class="hlt">solar</span> <span class="hlt">influence</span> and the global carbon cycle on the record. References: Genty, D., Baker, A., Massault, M., Proctor, C., Gilmour, M., Pons-Branchu, E., Hamelin, B. (2001) Dead carbon in stalagmites: carbonate bedrock paleodissolution vs. ageing of soil organic matter. Implications for 13C variations in speleothems, GCA, 65 Griffiths, M.L., Fohlmeister, J., Drysdale, R.N., Hua, Q., Johnson, K.R., Hellstrom, J.C., Gagan, M.K., Zhao, J.-x. (2012) Hydrological control of the dead carbon fraction in a Holocene tropical speleothem, Quat. Geochron. 14 Ridley, H.E., Baldini, J.U.L., Prufer, K.M., Walczak, I.W., Breitenbach, S.F.M. (in press) High resolution monitoring of a tropical cave system reveals dynamic ventilation and hydrologic resilience to seismic <span class="hlt">activity</span>, Journal of Cave and Karst Studies</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2018SuMi..118..137C','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2018SuMi..118..137C"><span>Voc enhancement of a <span class="hlt">solar</span> cell with doped Li+-PbS as the <span class="hlt">active</span> layer</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Chávez Portillo, M.; Alvarado Pulido, J.; Gallardo Hernández, S.; Soto Cruz, B. S.; Alcántara Iniesta, S.; Gutiérrez Pérez, R.; Portillo Moreno, O.</p> <p>2018-06-01</p> <p>In this report, we investigate the fabrication of <span class="hlt">solar</span> cells obtained by chemical bath technique, based on CdS as window layer and PbS and PbS-Li+-doped as the <span class="hlt">active</span> layer. We report open-circuit-voltage Voc values of ∼392 meV for PbS and ∼630 meV for PbSLi+-doped, a remarkable enhanced in the open circuit voltage is shown for <span class="hlt">solar</span> cells with doped <span class="hlt">active</span> layer. Li+ ion passivate the dangling bonds in PbS-metal layer interface in consequence reducing the recombination centers.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2010cosp...38.1785V','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2010cosp...38.1785V"><span>Evolution of the <span class="hlt">solar</span> radiative forcing on climate during the Holocene</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Vieira, Luis Eduardo; Solanki, Sami K.; Krivova, Natalie</p> <p></p> <p>The main external heating source of the Earth's coupled atmosphere-ocean system is the <span class="hlt">solar</span> radiative energy input. The variability of this energy source produces corresponding changes on the coupled system. However, there is still significant uncertainty on the level of changes. One way to distinguish the <span class="hlt">influence</span> of the Sun on the climate from other sources is to search for its <span class="hlt">influence</span> in the pre-industrial period, when the <span class="hlt">influence</span> of human <span class="hlt">activities</span> on the atmosphere composition and Earth's surface properties can be neglected. Such studies require long time series of <span class="hlt">solar</span> and geophysical parameters, ideally covering the whole Holocene. Here, we compute the total and spectral irradiance for the Holocene employing the reconstructions of the open flux and sunspot number obtained from the cosmogenic isotope 14C. The model employed in this study is identical to the spectral and total irradiance reconstruction (SATIRE) models employed to study these parameters on time scales from days to centuries, but adapted to work with decadal averaged data. The model is tested by comparing to the total and spectral <span class="hlt">solar</span> irradiance reconstructions from the sunspot number for the last 4 centuries. We also discuss limits and uncertainties of the model.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.osti.gov/biblio/21464720-intermittency-multifractality-spectra-magnetic-field-solar-active-regions','SCIGOV-STC'); return false;" href="https://www.osti.gov/biblio/21464720-intermittency-multifractality-spectra-magnetic-field-solar-active-regions"><span>INTERMITTENCY AND MULTIFRACTALITY SPECTRA OF THE MAGNETIC FIELD IN <span class="hlt">SOLAR</span> <span class="hlt">ACTIVE</span> REGIONS</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>Abramenko, Valentyna; Yurchyshyn, Vasyl</p> <p></p> <p>We present the results of a study of intermittency and multifractality of magnetic structures in <span class="hlt">solar</span> <span class="hlt">active</span> regions (ARs). Line-of-sight magnetograms for 214 ARs of different flare productivity observed at the center of the <span class="hlt">solar</span> disk from 1997 January until 2006 December are utilized. Data from the Michelson Doppler Imager (MDI) instrument on board the <span class="hlt">Solar</span> and Heliospheric Observatory operating in the high resolution mode, the Big Bear <span class="hlt">Solar</span> Observatory digital magnetograph, and the Hinode SOT/SP instrument were used. Intermittency spectra were derived from high-order structure functions and flatness functions. The flatness function exponent is a measure of the degreemore » of intermittency. We found that the flatness function exponent at scales below approximately 10 Mm is correlated with flare productivity (the correlation coefficient is -0.63). The Hinode data show that the intermittency regime is extended toward small scales (below 2 Mm) as compared to the MDI data. The spectra of multifractality, derived from the structure functions and flatness functions, are found to be broader for ARs of higher flare productivity as compared to those of low flare productivity. The magnetic structure of high-flaring ARs consists of a voluminous set of monofractals, and this set is much richer than that for low-flaring ARs. The results indicate the relevance of the multifractal organization of the photospheric magnetic fields to the flaring <span class="hlt">activity</span>. The strong intermittency observed in complex and high-flaring ARs is a hint that we observe a photospheric imprint of enhanced sub-photospheric dynamics.« less</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://files.eric.ed.gov/fulltext/ED270293.pdf','ERIC'); return false;" href="http://files.eric.ed.gov/fulltext/ED270293.pdf"><span><span class="hlt">Solar</span> Energy and You.</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>Conservation and Renewable Energy Inquiry and Referral Service (DOE), Silver Spring, MD.</p> <p></p> <p>This booklet provides an introduction to <span class="hlt">solar</span> energy by discussing: (1) how a home is heated; (2) how <span class="hlt">solar</span> energy can help in the heating process; (3) the characteristics of passive <span class="hlt">solar</span> houses; (4) the characteristics of <span class="hlt">active</span> <span class="hlt">solar</span> houses; (5) how <span class="hlt">solar</span> heat is stored; and (6) other uses of <span class="hlt">solar</span> energy. Also provided are 10 questions to…</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/20070035127','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/20070035127"><span>Short- and Medium-term Atmospheric Effects of Very Large <span class="hlt">Solar</span> Proton Events</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Jackman, Charles H.; Marsh, Daniel R.; Vitt, Francis M.; Garcia, Rolando R.; Fleming, Eric L.; Labow, Gordon J.; Randall, Cora E.; Lopez-Puertas, Manuel; Funke, Bernd</p> <p>2007-01-01</p> <p>Long-term variations in ozone have been caused by both natural and humankind related processes. In particular, the humankind or anthropogenic <span class="hlt">influence</span> on ozone from chlorofluorocarbons and halons (chlorine and bromine) has led to international regulations greatly limiting the release of these substances. These anthropogenic effects on ozone are most important in polar regions and have been significant since the 1970s. Certain natural ozone <span class="hlt">influences</span> are also important in polar regions and are caused by the impact of <span class="hlt">solar</span> charged particles on the atmosphere. Such natural variations have been studied in order to better quantify the human <span class="hlt">influence</span> on polar ozone. Large-scale explosions on the Sun near <span class="hlt">solar</span> maximum lead to emissions of charged particles (mainly protons and electrons), some of which enter the Earth's magnetosphere and rain down on the polar regions. "<span class="hlt">Solar</span> proton events" have been used to describe these phenomena since the protons associated with these <span class="hlt">solar</span> events sometimes create a significant atmospheric disturbance. We have used the National Center for Atmospheric Research (NCAR) Whole Atmosphere Community Climate Model (WACCM) to study the short- and medium-term (days to a few months) <span class="hlt">influences</span> of <span class="hlt">solar</span> proton events between 1963 and 2005 on stratospheric ozone. The four largest events in the past 45 years (August 1972; October 1989; July 2000; and October-November 2003) caused very distinctive polar changes in layers of the Earth's atmosphere known as the stratosphere (12-50 km; -7-30 miles) and mesosphere (50-90 km; 30-55 miles). The <span class="hlt">solar</span> protons connected with these events created hydrogen- and nitrogen- containing compounds, which led to the polar ozone destruction. The hydrogen-containing compounds have very short lifetimes and lasted for only a few days (typically the duration of the <span class="hlt">solar</span> proton event). On the other hand, the nitrogen-containing compounds lasted much longer, especially in the Winter. The nitrogen oxides were predicted</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2016AAS...22710506R','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2016AAS...22710506R"><span>What Makes Red Giants Tick? Linking Tidal Forces, <span class="hlt">Activity</span>, and <span class="hlt">Solar</span>-Like Oscillations via Eclipsing Binaries</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Rawls, Meredith L.; Gaulme, Patrick; McKeever, Jean; Jackiewicz, Jason</p> <p>2016-01-01</p> <p>Thanks to advances in asteroseismology, red giants have become astrophysical laboratories for studying stellar evolution and probing the Milky Way. However, not all red giants show <span class="hlt">solar</span>-like oscillations. It has been proposed that stronger tidal interactions from short-period binaries and increased magnetic <span class="hlt">activity</span> on spotty giants are linked to absent or damped <span class="hlt">solar</span>-like oscillations, yet each star tells a nuanced story. In this work, we characterize a subset of red giants in eclipsing binaries observed by Kepler. The binaries exhibit a range of orbital periods, <span class="hlt">solar</span>-like oscillation behavior, and stellar <span class="hlt">activity</span>. We use orbital solutions together with a suite of modeling tools to combine photometry and spectroscopy in a detailed analysis of tidal synchronization timescales, star spot <span class="hlt">activity</span>, and stellar evolution histories. These red giants offer an unprecedented opportunity to test stellar physics and are important benchmarks for ensemble asteroseismology.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/19900018878','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/19900018878"><span>Lower thermosphere (80-100 km) dynamics response to <span class="hlt">solar</span> and geomagnetic <span class="hlt">activity</span>: Overview</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Kazimirovsky, E. S.</p> <p>1989-01-01</p> <p>The variations of <span class="hlt">solar</span> and geomagnetic <span class="hlt">activity</span> may affect the thermosphere circulation via plasma heating and electric fields, especially at high latitudes. The possibility exists that the energy involved in auroral and magnetic storms can produce significant changes of mesosphere and lower thermosphere wind systems. A study of global radar measurements of winds at 80 to 100 km region revealed the short term effects (correlation between wind field and geomagnetic storms) and long term variations over a <span class="hlt">solar</span> cycle. It seems likely that the correlation results from a modification of planetary waves and tides propagated from below, thus altering the dynamical regime of the thermosphere. Sometimes the long term behavior points rather to a climatic variation with the internal atmospheric cause than to a direct <span class="hlt">solar</span> control.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017EGUGA..19.7285N','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017EGUGA..19.7285N"><span>Reconstructing the 11-year <span class="hlt">solar</span> cycle length from cosmogenic radionuclides for the last 600 years</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Nilsson, Emma; Adolphi, Florian; Mekhaldi, Florian; Muscheler, Raimund</p> <p>2017-04-01</p> <p>The cyclic behavior of the <span class="hlt">solar</span> magnetic field has been known for centuries and the 11-year <span class="hlt">solar</span> cycle is one of the most important features directly visible on the <span class="hlt">solar</span> disc. Using sunspot records it is evident that the length of this cycle is variable. A hypothesis of an inverse relationship between the average <span class="hlt">solar</span> <span class="hlt">activity</span> level and the <span class="hlt">solar</span> cycle length has been put forward (e.g. Friis-Christensen & Lassen, 1991), indicating longer <span class="hlt">solar</span> cycles during periods of low <span class="hlt">solar</span> <span class="hlt">activity</span> and vice versa. So far, studies of the behavior of the 11-year <span class="hlt">solar</span> cycle have largely been limited for the last 4 centuries where observational sunspot data are available. However, cosmogenic radionuclides, such as 10Be and 14C from ice cores and tree rings allow an assessment of the strength of the open <span class="hlt">solar</span> magnetic field due to its shielding <span class="hlt">influence</span> on galactic cosmic rays in the heliosphere. Similarly, very strong <span class="hlt">solar</span> storms can leave their imprint in cosmogenic radionuclide records via <span class="hlt">solar</span> proton-induced direct production of cosmogenic radionuclides in the Earth atmosphere. Here, we test the hypothesis of an inverse relationship between <span class="hlt">solar</span> cycle length and the longer-term <span class="hlt">solar</span> <span class="hlt">activity</span> level by using cosmogenic radionuclide records as a proxy for <span class="hlt">solar</span> <span class="hlt">activity</span>. Our results for the last six centuries suggest significant <span class="hlt">solar</span> cycle length variations that could exceed the range directly inferred from sunspot records. We discuss the occurrence of SPEs within the 11-year <span class="hlt">solar</span> cycle from a radionuclide perspective, specifically the largest one known yet, at AD 774-5 (Mekhaldi et al., 2015). References: Friis-Christensen, E. & Lassen, K. Length of the <span class="hlt">solar</span>-cycle - An indicator of <span class="hlt">solar</span> <span class="hlt">activity</span> closely associated with climate. Science 254, 698-700, doi:10.1126/science.254.5032.698 (1991). Mekhaldi, F., Muscheler, R., Adolphi, F., Aldahan, A., Beer, J., McConnell, J. R., Possnert, G., Sigl, M., Svensson, A., Synal, H. A., Welten, K. C. & Woodruff, T. E</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2016usc..confE..83I','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2016usc..confE..83I"><span>Project for <span class="hlt">Solar</span>-Terrestrial Environment Prediction (PSTEP): Towards Predicting Next <span class="hlt">Solar</span> Cycle</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Imada, S.; Iijima, H.; Hotta, H.; Shiota, D.; Kanou, O.; Fujiyama, M.; Kusano, K.</p> <p>2016-10-01</p> <p>It is believed that the longer-term variations of the <span class="hlt">solar</span> <span class="hlt">activity</span> can affect the Earth's climate. Therefore, predicting the next <span class="hlt">solar</span> cycle is crucial for the forecast of the "<span class="hlt">solar</span>-terrestrial environment". To build prediction schemes for the <span class="hlt">activity</span> level of the next <span class="hlt">solar</span> cycle is a key for the long-term space weather study. Although three-years prediction can be almost achieved, the prediction of next <span class="hlt">solar</span> cycle is very limited, so far. We are developing a five-years prediction scheme by combining the Surface Flux Transport (SFT) model and the most accurate measurements of <span class="hlt">solar</span> magnetic fields as a part of the PSTEP (Project for <span class="hlt">Solar</span>-Terrestrial Environment Prediction),. We estimate the meridional flow, differential rotation, and turbulent diffusivity from recent modern observations (Hinode and <span class="hlt">Solar</span> Dynamics Observatory). These parameters are used in the SFT models to predict the polar magnetic fields strength at the <span class="hlt">solar</span> minimum. In this presentation, we will explain the outline of our strategy to predict the next <span class="hlt">solar</span> cycle. We also report the present status and the future perspective of our project.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2016JASTP.149..207V','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2016JASTP.149..207V"><span>Cloud cover anomalies at middle latitudes: Links to troposphere dynamics and <span class="hlt">solar</span> variability</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Veretenenko, S.; Ogurtsov, M.</p> <p>2016-11-01</p> <p>In this work we study links between low cloud anomalies (LCA) at middle latitudes of the Northern and Southern hemispheres and galactic cosmic ray (GCR) variations used as a proxy of <span class="hlt">solar</span> variability on the decadal time scale. It was shown that these links are not direct, but realized through GCR/<span class="hlt">solar</span> <span class="hlt">activity</span> phenomena <span class="hlt">influence</span> on the development of extratropical baric systems (cyclones and troughs) which form cloud field. The violation of a positive correlation between LCA and GCR intensity which was observed in the 1980s-1990s occurred simultaneously in the Northern and Southern hemispheres in the early 2000s and coincided with the sign reversal of GCR effects on troposphere circulation. It was suggested that a possible reason for the correlation reversal between cyclonic <span class="hlt">activity</span> at middle latitudes and GCR fluxes is the change of the stratospheric polar vortex intensity which <span class="hlt">influences</span> significantly the troposphere-stratosphere coupling. The evidences for a noticeable weakening of the polar vortices in the Arctic and Antarctic stratosphere in the early 2000s are provided. The results obtained suggest an important role of the polar vortex evolution as a reason for a temporal variability of <span class="hlt">solar</span> <span class="hlt">activity</span> effects on the lower atmosphere.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2015A%26A...578A.137S','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2015A%26A...578A.137S"><span>Seismic sensitivity to sub-surface <span class="hlt">solar</span> <span class="hlt">activity</span> from 18 yr of GOLF/SoHO observations</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Salabert, D.; García, R. A.; Turck-Chièze, S.</p> <p>2015-06-01</p> <p><span class="hlt">Solar</span> <span class="hlt">activity</span> has significantly changed over the last two Schwabe cycles. After a long and deep minimum at the end of Cycle 23, the weaker <span class="hlt">activity</span> of Cycle 24 contrasts with the previous cycles. In this work, the response of the <span class="hlt">solar</span> acoustic oscillations to <span class="hlt">solar</span> <span class="hlt">activity</span> is used in order to provide insights into the structural and magnetic changes in the sub-surface layers of the Sun during this on-going unusual period of low <span class="hlt">activity</span>. We analyze 18 yr of continuous observations of the <span class="hlt">solar</span> acoustic oscillations collected by the Sun-as-a-star GOLF instrument on board the SoHO spacecraft. From the fitted mode frequencies, the temporal variability of the frequency shifts of the radial, dipolar, and quadrupolar modes are studied for different frequency ranges that are sensitive to different layers in the <span class="hlt">solar</span> sub-surface interior. The low-frequency modes show nearly unchanged frequency shifts between Cycles 23 and 24, with a time evolving signature of the quasi-biennial oscillation, which is particularly visible for the quadrupole component revealing the presence of a complex magnetic structure. The modes at higher frequencies show frequency shifts that are 30% smaller during Cycle 24, which is in agreement with the decrease observed in the surface <span class="hlt">activity</span> between Cycles 23 and 24. The analysis of 18 yr of GOLF oscillations indicates that the structural and magnetic changes responsible for the frequency shifts remained comparable between Cycle 23 and Cycle 24 in the deeper sub-surface layers below 1400 km as revealed by the low-frequency modes. The frequency shifts of the higher-frequency modes, sensitive to shallower regions, show that Cycle 24 is magnetically weaker in the upper layers of Sun. Appendices are available in electronic form at http://www.aanda.orgThe following 68 GOLF frequency tables are available and Table A.1 is also available at the CDS via anonymous ftp to http://cdsarc.u-strasbg.fr (ftp://130.79.128.5) or via http</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2018ApJ...859...61B','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2018ApJ...859...61B"><span>Differential Rotation in <span class="hlt">Solar</span>-like Convective Envelopes: <span class="hlt">Influence</span> of Overshoot and Magnetism</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Beaudoin, Patrice; Strugarek, Antoine; Charbonneau, Paul</p> <p>2018-05-01</p> <p>We present a set of four global Eulerian/semi-Lagrangian fluid solver (EULAG) hydrodynamical (HD) and magnetohydrodynamical (MHD) simulations of <span class="hlt">solar</span> convection, two of which are restricted to the nominal convection zone, and the other two include an underlying stably stratified fluid layer. While all four simulations generate reasonably <span class="hlt">solar</span>-like latitudinal differential rotation profiles where the equatorial region rotates faster than the polar regions, the rotational isocontours vary significantly among them. In particular, the purely HD simulation with a stable layer alone can break the Taylor–Proudman theorem and produce approximately radially oriented rotational isocontours at medium to high latitudes. We trace this effect to the buildup of a significant latitudinal temperature gradient in the stable fluid immediately beneath the convection zone, which imprints itself on the lower convection zone. It develops naturally in our simulations as a consequence of convective overshoot and rotational <span class="hlt">influence</span> of rotation on convective energy fluxes. This favors the establishment of a thermal wind balance that allows evading the Taylor–Proudman constraint. A much smaller latitudinal temperature gradient develops in the companion MHD simulation that includes a stable fluid layer, reflecting the tapering of deep convective overshoot that occurs at medium to high latitudes, which is caused by the strong magnetic fields that accumulate across the base of the convection zone. The stable fluid layer also has a profound impact on the large-scale magnetic cycles developing in the two MHD simulations. Even though both simulations operate in the same convective parameter regime, the simulation that includes a stable layer eventually loses cyclicity and transits to a non-<span class="hlt">solar</span>, steady quadrupolar state.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2013AdSpR..51...96K','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2013AdSpR..51...96K"><span>Helio-geomagnetic <span class="hlt">influence</span> in cardiological cases</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Katsavrias, Ch.; Preka-Papadema, P.; Moussas, X.; Apostolou, Th.; Theodoropoulou, A.; Papadima, Th.</p> <p>2013-01-01</p> <p>The effects of the energetic phenomena of the Sun, flares and coronal mass ejections (CMEs) on the Earth's ionosphere-magnetosphere, through the <span class="hlt">solar</span> wind, are the sources of the geomagnetic disturbances and storms collectively known as Space Weather. The research on the <span class="hlt">influence</span> of Space Weather on biological and physiological systems is open. In this work we study the Space Weather impact on Acute Coronary Syndromes (ACS) distinguishing between ST-segment elevation acute coronary syndromes (STE-ACS) and non-ST-segment elevation acute coronary syndromes (NSTE-ACS) cases. We compare detailed patient records from the 2nd Cardiologic Department of the General Hospital of Nicaea (Piraeus, Greece) with characteristics of geomagnetic storms (DST), <span class="hlt">solar</span> wind speed and statistics of flares and CMEs which cover the entire <span class="hlt">solar</span> cycle 23 (1997-2007). Our results indicate a relationship of ACS to helio-geomagnetic <span class="hlt">activity</span> as the maximum of the ACS cases follows closely the maximum of the <span class="hlt">solar</span> cycle. Furthermore, within very <span class="hlt">active</span> periods, the ratio NSTE-ACS to STE-ACS, which is almost constant during periods of low to medium <span class="hlt">activity</span>, changes favouring the NSTE-ACS. Most of the ACS cases exhibit a high degree of association with the recovery phase of the geomagnetic storms; a smaller, yet significant, part was found associated with periods of fast <span class="hlt">solar</span> wind without a storm.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2018AdSpR..61.1850R','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2018AdSpR..61.1850R"><span>Characteristics of nighttime E-region over Arecibo: Dependence on <span class="hlt">solar</span> flux and geomagnetic variations</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Raizada, Shikha; Brum, Christiano G. M.; Mathews, John D.; Gonzalez, Cristina; Franco, Efmi</p> <p>2018-04-01</p> <p>Electron concentration (Ne) inferred from Incoherent Scatter Radar (ISR) measurements has been used to determine the <span class="hlt">influence</span> of <span class="hlt">solar</span> flux and geomagnetic <span class="hlt">activity</span> in the ionospheric E-region over Arecibo Observatory (AO). The approach is based on the determination of column integrated Ne, referred to as E-region total electron content (ErTEC) between 80 and 150 km altitude regions. The results discussed in this work are for the AO nighttime period. The study reveals higher ErTEC values during the low <span class="hlt">solar</span> flux periods for all the seasons except for summer period. It is found that the E-region column abundance is higher in equinox periods than in the winter for low <span class="hlt">solar</span> <span class="hlt">activity</span> conditions. The column integrated Ne during the post-sunset/pre-sunrise periods always exceeds the midnight minima, independent of season or <span class="hlt">solar</span> <span class="hlt">activity</span>. This behavior has been attributed to the variations in the coupling processes from the F-region. The response of ErTEC to the geomagnetic variability is also examined for different <span class="hlt">solar</span> flux conditions and seasons. During high <span class="hlt">solar</span> flux periods, changes in Kp cause an ErTEC increase in summer and equinox, while producing a negative storm-like effect during the winter. Variations in ErTEC due to geomagnetic <span class="hlt">activity</span> during low <span class="hlt">solar</span> flux periods produce maximum variability in the E-region during equinox periods, while resulting in an increase/decrease in ErTEC before local midnight during the winter/summer periods, respectively.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/19760011136','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/19760011136"><span><span class="hlt">Solar</span> Energy Monitor In Space (SEMIS)</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Thekaekara, M. P.</p> <p>1974-01-01</p> <p>Measurements made at high altitudes from aircraft have resulted in the establishment of standard values of the <span class="hlt">solar</span> constant and extraterrestrial <span class="hlt">solar</span> spectral irradiance. These standard values and other <span class="hlt">solar</span> spectral curves are described. The problem of possible variations of the <span class="hlt">solar</span> constant and <span class="hlt">solar</span> spectrum and their <span class="hlt">influence</span> on the earth-atmosphere system and weather related phenomena is examined. It is shown that the <span class="hlt">solar</span> energy input parameters should be determined with considerably greater accuracy and precision than has been possible. An instrument package designed as a compact, low weight <span class="hlt">solar</span> energy monitor in space (SEMIS) is described.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/28344292','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/28344292"><span><span class="hlt">Influence</span> of Nitrogen Doping on Device Operation for TiO₂-Based Solid-State Dye-Sensitized <span class="hlt">Solar</span> Cells: Photo-Physics from Materials to Devices.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Wang, Jin; Tapio, Kosti; Habert, Aurélie; Sorgues, Sebastien; Colbeau-Justin, Christophe; Ratier, Bernard; Scarisoreanu, Monica; Toppari, Jussi; Herlin-Boime, Nathalie; Bouclé, Johann</p> <p>2016-02-23</p> <p>Solid-state dye-sensitized <span class="hlt">solar</span> cells (ssDSSC) constitute a major approach to photovoltaic energy conversion with efficiencies over 8% reported thanks to the rational design of efficient porous metal oxide electrodes, organic chromophores, and hole transporters. Among the various strategies used to push the performance ahead, doping of the nanocrystalline titanium dioxide (TiO₂) electrode is regularly proposed to extend the photo-<span class="hlt">activity</span> of the materials into the visible range. However, although various beneficial effects for device performance have been observed in the literature, they remain strongly dependent on the method used for the production of the metal oxide, and the <span class="hlt">influence</span> of nitrogen atoms on charge kinetics remains unclear. To shed light on this open question, we synthesized a set of N-doped TiO₂ nanopowders with various nitrogen contents, and exploited them for the fabrication of ssDSSC. Particularly, we carefully analyzed the localization of the dopants using X-ray photo-electron spectroscopy (XPS) and monitored their <span class="hlt">influence</span> on the photo-induced charge kinetics probed both at the material and device levels. We demonstrate a strong correlation between the kinetics of photo-induced charge carriers probed both at the level of the nanopowders and at the level of working <span class="hlt">solar</span> cells, illustrating a direct transposition of the photo-physic properties from materials to devices.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://ntrs.nasa.gov/search.jsp?R=19790069639&hterms=physics&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DTitle%26N%3D0%26No%3D10%26Ntt%3Dphysics','NASA-TRS'); return false;" href="https://ntrs.nasa.gov/search.jsp?R=19790069639&hterms=physics&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DTitle%26N%3D0%26No%3D10%26Ntt%3Dphysics"><span>A broad look at <span class="hlt">solar</span> physics adapted from the <span class="hlt">solar</span> physics study of August 1975</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Parker, E.; Timothy, A.; Beckers, J.; Hundhausen, A.; Kundu, M. R.; Leith, C. E.; Lin, R.; Linsky, J.; Macdonald, F. B.; Noyes, R.</p> <p>1979-01-01</p> <p>The current status of our knowledge of the basic mechanisms involved in fundamental <span class="hlt">solar</span> phenomena is reviewed. These include mechanisms responsible for heating the corona, the generation of the <span class="hlt">solar</span> wind, the particle acceleration in flares, and the dissipation of magnetic energy in field reversal regions, known as current sheets. The discussion covers <span class="hlt">solar</span> flares and high-energy phenomena, <span class="hlt">solar</span> <span class="hlt">active</span> regions; <span class="hlt">solar</span> interior, convection, and <span class="hlt">activity</span>; the structure and energetics of the quiet <span class="hlt">solar</span> atmosphere; the structure of the corona; the <span class="hlt">solar</span> composition; and <span class="hlt">solar</span> terrestrial interactions. It also covers a program of <span class="hlt">solar</span> research, including the special observational requirements for spectral and angular resolution, sensitivity, time resolution, and duration of the techniques employed.</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/2003AGUFMED51C1209A','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2003AGUFMED51C1209A"><span><span class="hlt">Solar</span> Week: Learning from Experience</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Alexander, D.; Hauck, K.</p> <p>2003-12-01</p> <p><span class="hlt">Solar</span> Week is a week-long set of games and <span class="hlt">activities</span> allowing students to interact directly with <span class="hlt">solar</span> science and <span class="hlt">solar</span> scientists. <span class="hlt">Solar</span> Week was developed as a spin-off of the highly successful Yohkoh Public Outreach Project (YPOP). While YPOP provided access to <span class="hlt">solar</span> images, movies and <span class="hlt">activities</span>, the main goal of <span class="hlt">Solar</span> Week was to enhance the participation of women, who are under-represented in the physical sciences. <span class="hlt">Solar</span> Week achieves this by providing young women, primarily in grades 6-8, with access to role models in the sciences. The scientists participating in <span class="hlt">Solar</span> Week are women from a variety of backgrounds and with a variety of scientific expertise. In this paper, our aim is to provide some insight into developing <span class="hlt">activity</span>-based space science for the web and to discuss the lessons-learned from tailoring to a specific group of participants.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/28770995','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/28770995"><span>Short-Term Environmental Effects and Their <span class="hlt">Influence</span> on Spatial Homogeneity of Organic <span class="hlt">Solar</span> Cell Functionality.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Chien, Huei-Ting; Zach, Peter W; Friedel, Bettina</p> <p>2017-08-23</p> <p>In this study, we focus on the induced degradation and spatial inhomogeneity of organic photovoltaic devices under different environmental conditions, uncoupled from the <span class="hlt">influence</span> of any auxiliary hole-transport (HT) layer. During testing of the corresponding devices comprising the standard photoactive layer of poly(3-hexylthiophene) as donor, blended with phenyl-C 61 -butyric acid methyl ester as acceptor, a comparison was made between the nonencapsulated devices upon exposure to argon in the dark, dry air in the dark, dry air with illumination, and humid air in the dark. The impact on the <span class="hlt">active</span> layer's photophysics is discussed, along with the device physics in terms of integral <span class="hlt">solar</span> cell performance and spatially resolved photocurrent distribution with point-to-point analysis of the diode characteristics to determine the origin of the observed integrated organic photovoltaic device behavior. The results show that even without the widely used hygroscopic HT layer, poly(3,4-ethylenedioxythiophene):poly(styrenesulfonate), humidity is still a major factor in the short-term environmental degradation of organic <span class="hlt">solar</span> cells with this architecture, and not only oxygen or light, as is often reported. Different from previous reports where water-induced device degradation was spatially homogeneous and formation of Al 2 O 3 islands was only seen for oxygen permeation through pinholes in aluminum, we observed insulating islands merely after humidity exposure in the present study. Further, we demonstrated with laser beam induced current mapping and point-to-point diode analysis that the water-induced performance losses are a result of the exposed device area comprising regions with entirely unaltered high output and intact diode behavior and those with severe degradation showing detrimentally lowered output and voltage-independent charge blocking, which is essentially insulating behavior. It is suggested that this is caused by transport of water through pinholes to the</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2011A%26A...534A..47C','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2011A%26A...534A..47C"><span>Statistical properties of superactive regions during <span class="hlt">solar</span> cycles 19-23</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Chen, A. Q.; Wang, J. X.; Li, J. W.; Feynman, J.; Zhang, J.</p> <p>2011-10-01</p> <p>Context. Each <span class="hlt">solar</span> <span class="hlt">activity</span> cycle is characterized by a small number of superactive regions (SARs) that produce the most violent of space weather events with the greatest disastrous <span class="hlt">influence</span> on our living environment. Aims: We aim to re-parameterize the SARs and study the latitudinal and longitudinal distributions of SARs. Methods: We select 45 SARs in <span class="hlt">solar</span> cycles 21-23, according to the following four parameters: 1) the maximum area of sunspot group, 2) the soft X-ray flare index, 3) the 10.7 cm radio peak flux, and 4) the variation in the total <span class="hlt">solar</span> irradiance. Another 120 SARs given by previous studies of <span class="hlt">solar</span> cycles 19-23 are also included. The latitudinal and longitudinal distributions of the 165 SARs in both the Carrington frame and the dynamic reference frame during <span class="hlt">solar</span> cycles 19-23 are studied statistically. Results: Our results indicate that these 45 SARs produced 44% of all the X class X-ray flares during <span class="hlt">solar</span> cycles 21-23, and that all the SARs are likely to produce a very fast CME. The latitudinal distributions of SARs display the Maunder butterfly diagrams and SARs occur preferentially in the maximum period of each <span class="hlt">solar</span> cycle. Northern hemisphere SARs dominated in <span class="hlt">solar</span> cycles 19 and 20 and southern hemisphere SARs dominated in <span class="hlt">solar</span> cycles 21 and 22. In <span class="hlt">solar</span> cycle 23, however, SARs occurred about equally in each hemisphere. There are two <span class="hlt">active</span> longitudes in both the northern and southern hemispheres, about 160°-200° apart. Applying the improved dynamic reference frame to SARs, we find that SARs rotate faster than the Carrington rate and there is no significant difference between the two hemispheres. The synodic periods are 27.19 days and 27.25 days for the northern and southern hemispheres, respectively. The longitudinal distribution of SARs is significantly non-axisymmetric and about 75% SARs occurred near two <span class="hlt">active</span> longitudes with half widths of 45°. Appendix A is available in electronic form at http://www.aanda.org</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2016AIPC.1720b0005T','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2016AIPC.1720b0005T"><span>Statistical properties of <span class="hlt">solar</span> flares and coronal mass ejections through the <span class="hlt">solar</span> cycle</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Telloni, Daniele; Carbone, Vincenzo; Lepreti, Fabio; Antonucci, Ester</p> <p>2016-03-01</p> <p>Waiting Time Distributions (WTDs) of <span class="hlt">solar</span> flares are investigated all through the <span class="hlt">solar</span> cycle. The same approach applied to Coronal Mass Ejections (CMEs) in a previous work is considered here for flare occurrence. Our analysis reveals that flares and CMEs share some common statistical properties, which result dependent on the level of <span class="hlt">solar</span> <span class="hlt">activity</span>. Both flares and CMEs seem to independently occur during minimum <span class="hlt">solar</span> <span class="hlt">activity</span> phases, whilst their WTDs significantly deviate from a Poisson function at <span class="hlt">solar</span> maximum, thus suggesting that these events are correlated. The characteristics of WTDs are constrained by the physical processes generating those eruptions associated with flares and CMEs. A scenario may be drawn in which different mechanisms are <span class="hlt">actively</span> at work during different phases of the <span class="hlt">solar</span> cycle. Stochastic processes, most likely related to random magnetic reconnections of the field lines, seem to play a key role during <span class="hlt">solar</span> minimum periods. On the other hand, persistent processes, like sympathetic eruptions associated to the variability of the photospheric magnetism, are suggested to dominate during periods of high <span class="hlt">solar</span> <span class="hlt">activity</span>. Moreover, despite the similar statistical properties shown by flares and CMEs, as it was mentioned above, their WTDs appear different in some aspects. During <span class="hlt">solar</span> minimum periods, the flare occurrence randomness seems to be more evident than for CMEs. Those persistent mechanisms generating interdependent events during maximum periods of <span class="hlt">solar</span> <span class="hlt">activity</span> can be suggested to play a more important role for CMEs than for flares, thus mitigating the competitive action of the random processes, which seem instead strong enough to weaken the correlations among flare event occurrence during <span class="hlt">solar</span> minimum periods. However, it cannot be excluded that the physical processes at the basis of the origin of the temporal correlation between <span class="hlt">solar</span> events are different for flares and CMEs, or that, more likely, more sophisticated effects are</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.osti.gov/biblio/22654396-electric-current-neutralization-magnetic-shear-eruptive-activity-solar-active-regions','SCIGOV-STC'); return false;" href="https://www.osti.gov/biblio/22654396-electric-current-neutralization-magnetic-shear-eruptive-activity-solar-active-regions"><span>Electric-current Neutralization, Magnetic Shear, and Eruptive <span class="hlt">Activity</span> in <span class="hlt">Solar</span> <span class="hlt">Active</span> Regions</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>Liu, Yang; Sun, Xudong; Török, Tibor</p> <p></p> <p>The physical conditions that determine whether or not <span class="hlt">solar</span> <span class="hlt">active</span> regions (ARs) produce strong flares and coronal mass ejections (CMEs) are not yet well understood. Here, we investigate the association between electric-current neutralization, magnetic shear along polarity inversion lines (PILs), and eruptive <span class="hlt">activity</span> in four ARs: two emerging and two well-developed ones. We find that the CME-producing ARs are characterized by a strongly non-neutralized total current, while the total current in the ARs that did not produce CMEs is almost perfectly neutralized. The difference in the PIL shear between these two groups is much less pronounced, which suggests that themore » degree of current neutralization may serve as a better proxy for assessing the ability of ARs to produce CMEs.« less</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2012AdSpR..50..211H','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2012AdSpR..50..211H"><span>A nonlinear background removal method for seismo-ionospheric anomaly analysis under a complex <span class="hlt">solar</span> <span class="hlt">activity</span> scenario: A case study of the M9.0 Tohoku earthquake</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>He, Liming; Wu, Lixin; Pulinets, Sergey; Liu, Shanjun; Yang, Fan</p> <p>2012-07-01</p> <p>A precise determination of ionospheric total electron content (TEC) anomaly variations that are likely associated with large earthquakes as observed by global positioning system (GPS) requires the elimination of the ionospheric effect from irregular <span class="hlt">solar</span> electromagnetic radiation. In particular, revealing the seismo-ionospheric anomalies when earthquakes occurred during periods of high <span class="hlt">solar</span> <span class="hlt">activity</span> is of utmost importance. To overcome this constraint, a multiresolution time series processing technique based on wavelet transform applicable to global ionosphere map (GIM) TEC data was used to remove the nonlinear effect from <span class="hlt">solar</span> radiation for the earthquake that struck Tohoku, Japan, on 11 March, 2011. As a result, it was found that the extracted TEC have a good correlation with the measured <span class="hlt">solar</span> extreme ultraviolet flux in 26-34 nm (EUV26-34) and the 10.7 cm <span class="hlt">solar</span> radio flux (F10.7). After removing the <span class="hlt">influence</span> of <span class="hlt">solar</span> radiation origin in GIM TEC, the analysis results show that the TEC around the forthcoming epicenter and its conjugate were significantly enhanced in the afternoon period of 8 March 2011, 3 days before the earthquake. The spatial distributions of the TEC anomalous and extreme enhancements indicate that the earthquake preparation process had brought with a TEC anomaly area of size approximately 1650 and 5700 km in the latitudinal and longitudinal directions, respectively.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017IAUS..328..130D','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017IAUS..328..130D"><span>Deriving the <span class="hlt">solar</span> <span class="hlt">activity</span> cycle modulation on cosmic ray intensity observed by Nagoya muon detector from October 1970 until December 2012</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>de Mendonça, Rafael R. S.; Braga, Carlos. R.; Echer, Ezequiel; Dal Lago, Alisson; Rockenbach, Marlos; Schuch, Nelson J.; Munakata, Kazuoki</p> <p>2017-10-01</p> <p>It is well known that the cosmic ray intensity observed at the Earth's surface presents an 11 and 22-yr variations associated with the <span class="hlt">solar</span> <span class="hlt">activity</span> cycle. However, the observation and analysis of this modulation through ground muon detectors datahave been difficult due to the temperature effect. Furthermore, instrumental changes or temporary problems may difficult the analysis of these variations. In this work, we analyze the cosmic ray intensity observed since October 1970 until December 2012 by the Nagoya muon detector. We show the results obtained after analyzing all discontinuities and gaps present in this data and removing changes not related to natural phenomena. We also show the results found using the mass weighted method for eliminate the <span class="hlt">influence</span> of atmospheric temperature changes on muon intensity observed at ground. As a preliminary result of our analyses, we show the <span class="hlt">solar</span> cycle modulation in the muon intensity observed for more than 40 years.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.osti.gov/servlets/purl/1427606','SCIGOV-STC'); return false;" href="https://www.osti.gov/servlets/purl/1427606"><span>Evaluation of Factors that <span class="hlt">Influence</span> Residential <span class="hlt">Solar</span> Panel Installations</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>Morton, April M.; Omitaomu, Olufemi A.; Kotikot, Susan M.</p> <p></p> <p>Though rooftop photovoltaic (PV) systems are the fastest growing source of distributed generation, detailed information about where they are located and who their owners are is often known only to installers and utility companies. This lack of detailed information is a barrier to policy and financial assessment of <span class="hlt">solar</span> energy generation and use. To bridge the described data gap, Oak Ridge National Laboratory (ORNL) was sponsored by the Department of Energy (DOE) Office of Energy Policy and Systems Analysis (EPSA) to create an automated approach for detecting and characterizing buildings with installed <span class="hlt">solar</span> panels using high-resolution overhead imagery. Additionally, ORNLmore » was tasked with using machine learning techniques to classify parcels on which <span class="hlt">solar</span> panels were automatically detected in the Washington, DC, and Boston areas as commercial or residential, and then providing a list of recommended variables and modeling techniques that could be combined with these results to identify attributes that motivate the installation of residential <span class="hlt">solar</span> panels. This technical report describes the methodology, results, and recommendations in greater detail, including lessons learned and future work.« less</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017PhDT.......111K','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017PhDT.......111K"><span>P3HT:PCBM-based organic <span class="hlt">solar</span> cells : Optimisation of <span class="hlt">active</span> layer nanostructure and interface properties</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Kadem, Burak Yahya</p> <p></p> <p>[61]BM, PC[70]BM and PC[71]BM) and the <span class="hlt">active</span> layers were processed using the optimum solvent as well as optimum film's thickness.These PCBM derivatives have different lower unoccupied molecular level (LUMO) and different higher occupied molecular level (HOMO) positions, which subsequently <span class="hlt">influence</span> the PV parameters of the OSCs such as the device open circuit voltage (V[oc]) and its built-in potential (V[bi]). P3HT:PC61BM-based blend has exhibited the highest device performance with PCE reaching 4.2%. Using the above mentioned optimum parameters, the P3HT:PCBM-based devices have been subjected to post-deposition annealing at different temperatures in the range 100-180°C. Efficient device performance was ascribed to P3HT:PCBM layers being subjected to post-deposition heat treatment at 140°C with PCE=5.5%. Device stability as a result of post-deposition heat treatment has also been shown to improve with PCE degrading by about 38% after 55 days.The use of interfacial layer is found to play a key part in modifying the <span class="hlt">solar</span> cell performance; using electron transport layer (ETL) such as aluminium tris(8-hydroxyquinoline) (Alq3) as a solution processable layer has contributed in increasing PCE to 4.25%, while, using PEDOT:PSS as a hole transport layer (HTL) doped with metal salts has significantly contributed in increasing PCE to reach 6.82% in device when PEDOT:PSS was doped with LiCl aqueous solution. Stability study for the device based on HTL has shown degradation in the PCE from 6.82% to around 1% over 96 days. Using ETL and HTL simultaneously in a complete device has shown a further enhanced PCE reaching 7%. In a further study, doping the P3HT:PCBM with the novel ZnPc hybrids (SWCNTs and reduced graphene oxide (rGO) are covalently and non-covalently functionalised to ZnPc) with the weight ratio of (1:0.01) has significantly altered the <span class="hlt">solar</span> cell device properties. The best performance is based on P3HT:PCBM blended with ZnPc-SWCNTs-co bonded as a ternary <span class="hlt">active</span></p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.osti.gov/biblio/22357182-magnetic-helicity-emerging-solar-active-regions','SCIGOV-STC'); return false;" href="https://www.osti.gov/biblio/22357182-magnetic-helicity-emerging-solar-active-regions"><span>Magnetic helicity in emerging <span class="hlt">solar</span> <span class="hlt">active</span> regions</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>Liu, Y.; Hoeksema, J. T.; Bobra, M.</p> <p></p> <p>Using vector magnetic field data from the Helioseismic and Magnetic Imager instrument aboard the <span class="hlt">Solar</span> Dynamics Observatory, we study magnetic helicity injection into the corona in emerging <span class="hlt">active</span> regions (ARs) and examine the hemispheric helicity rule. In every region studied, photospheric shearing motion contributes most of the helicity accumulated in the corona. In a sample of 28 emerging ARs, 17 follow the hemisphere rule (61% ± 18% at a 95% confidence interval). Magnetic helicity and twist in 25 ARs (89% ± 11%) have the same sign. The maximum magnetic twist, which depends on the size of an AR, is inferredmore » in a sample of 23 emerging ARs with a bipolar magnetic field configuration.« less</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2015TESS....130902W','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2015TESS....130902W"><span>Description and primary results of Total <span class="hlt">Solar</span> Irradiance Monitor, a <span class="hlt">solar</span>-pointing instrument on an Earth observing satellite</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Wang, Hongrui; Fang, Wei; Li, Huiduan</p> <p>2015-04-01</p> <p><span class="hlt">Solar</span> driving mechanism for Earth climate has been a controversial problem for centuries. Long-time data of <span class="hlt">solar</span> <span class="hlt">activity</span> is required by the investigations of the <span class="hlt">solar</span> driving mechanism, such as Total <span class="hlt">Solar</span> Irradiance (TSI) record. Three Total <span class="hlt">Solar</span> Irradiance Monitors (TSIM) have been developed by Changchun Institute of Optics, Fine Mechanics and Physics for China Meteorological Administration to maintain continuities of TSI data series which lasted for nearly 4 decades.The newest TSIM has recorded TSI daily with accurate <span class="hlt">solar</span> pointing on the FY-3C meteorological satellite since Oct 2013. TSIM/FY-3C has a pointing system for automatic <span class="hlt">solar</span> tracking, onboard the satellite designed mainly for Earth observing. Most payloads of FY-3C are developed for observation of land, ocean and atmosphere. Consequently, the FY-3C satellite is a nadir-pointing spacecraft with its z axis to be pointed at the center of the Earth. Previous TSIMs onboard the FY-3A and FY-3B satellites had no pointing system, <span class="hlt">solar</span> observations were only performed when the sun swept through field-of-view of the instruments. And TSI measurements are <span class="hlt">influenced</span> inevitably by the <span class="hlt">solar</span> pointing errors. Corrections of the <span class="hlt">solar</span> pointing errors were complex. The problem is now removed by TSIM/FY-3C.TSIM/FY-3C follows the sun accurately by itself using its pointing system based on scheme of visual servo control. The pointing system is consisted of a radiometer package, two motors for <span class="hlt">solar</span> tracking, a sun sensor and etc. TSIM/FY-3C has made daily observations of TSI for more than one year, with nearly zero <span class="hlt">solar</span> pointing errors. Short time-scale variations in TSI detected by TSIM/FY-3C are nearly the same with VIRGO/SOHO and TIM/SORCE.Instrument details, primary results of <span class="hlt">solar</span> pointing control, <span class="hlt">solar</span> observations and etc will be given in the presentation.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/25804610','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/25804610"><span>Nrf2 <span class="hlt">Activation</span> Protects against <span class="hlt">Solar</span>-Simulated Ultraviolet Radiation in Mice and Humans.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Knatko, Elena V; Ibbotson, Sally H; Zhang, Ying; Higgins, Maureen; Fahey, Jed W; Talalay, Paul; Dawe, Robert S; Ferguson, James; Huang, Jeffrey T-J; Clarke, Rosemary; Zheng, Suqing; Saito, Akira; Kalra, Sukirti; Benedict, Andrea L; Honda, Tadashi; Proby, Charlotte M; Dinkova-Kostova, Albena T</p> <p>2015-06-01</p> <p>The transcription factor Nrf2 determines the ability to adapt and survive under conditions of electrophilic, oxidative, and inflammatory stress by regulating the expression of elaborate networks comprising nearly 500 genes encoding proteins with versatile cytoprotective functions. In mice, disruption of Nrf2 increases susceptibility to carcinogens and accelerates disease pathogenesis. Paradoxically, Nrf2 is upregulated in established human tumors, but whether this upregulation drives carcinogenesis is not known. Here we show that the incidence, multiplicity, and burden of <span class="hlt">solar</span>-simulated UV radiation-mediated cutaneous tumors that form in SKH-1 hairless mice in which Nrf2 is genetically constitutively <span class="hlt">activated</span> are lower than those that arise in their wild-type counterparts. Pharmacologic Nrf2 <span class="hlt">activation</span> by topical biweekly applications of small (40 nmol) quantities of the potent bis(cyano enone) inducer TBE-31 has a similar protective effect against <span class="hlt">solar</span>-simulated UV radiation in animals receiving long-term treatment with the immunosuppressive agent azathioprine. Genetic or pharmacologic Nrf2 <span class="hlt">activation</span> lowers the expression of the pro-inflammatory factors IL6 and IL1β, and COX2 after acute exposure of mice to UV radiation. In healthy human subjects, topical applications of extracts delivering the Nrf2 <span class="hlt">activator</span> sulforaphane reduced the degree of <span class="hlt">solar</span>-simulated UV radiation-induced skin erythema, a quantifiable surrogate endpoint for cutaneous damage and skin cancer risk. Collectively, these data show that Nrf2 is not a driver for tumorigenesis even upon exposure to a very potent and complete carcinogen and strongly suggest that the frequent <span class="hlt">activation</span> of Nrf2 in established human tumors is a marker of metabolic adaptation. ©2015 American Association for Cancer Research.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=4454593','PMC'); return false;" href="https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=4454593"><span>Nrf2 <span class="hlt">activation</span> protects against <span class="hlt">solar</span>-simulated ultraviolet radiation in mice and humans</span></a></p> <p><a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pmc">PubMed Central</a></p> <p>Knatko, Elena V.; Ibbotson, Sally H.; Zhang, Ying; Higgins, Maureen; Fahey, Jed W.; Talalay, Paul; Dawe, Robert S.; Ferguson, James; Huang, Jeffrey T.-J.; Clarke, Rosemary; Zheng, Suqing; Saito, Akira; Kalra, Sukirti; Benedict, Andrea L.; Honda, Tadashi; Proby, Charlotte M.; Dinkova-Kostova, Albena T.</p> <p>2015-01-01</p> <p>The transcription factor Nrf2 determines the ability to adapt and survive under conditions of electrophilic, oxidative and inflammatory stress by regulating the expression of elaborate networks comprising nearly 500 genes encoding proteins with versatile cytoprotective functions. In mice, disruption of Nrf2 increases susceptibility to carcinogens and accelerates disease pathogenesis. Paradoxically, Nrf2 is upregulated in established human tumors, but whether this upregulation drives carcinogenesis is not known. Here we show that the incidence, multiplicity and burden of <span class="hlt">solar</span>-simulated UV radiation-mediated cutaneous tumors that form in SKH-1 hairless mice in which Nrf2 is genetically constitutively <span class="hlt">activated</span>, are lower than those that arise in their wild-type counterparts. Pharmacological Nrf2 <span class="hlt">activation</span> by topical bi-weekly applications of small (40 nmol) quantities of the potent bis(cyano enone) inducer TBE-31 has a similar protective effect against <span class="hlt">solar</span>-simulated UV radiation in animals receiving long-term treatment with the immunosuppressive agent azathioprine. Genetic or pharmacological Nrf2 <span class="hlt">activation</span> lowers the expression of the pro-inflammatory factors interleukin (IL)-6 and IL-1β, and cyclooxygenase (COX)-2 after acute exposure of mice to UV radiation. In healthy human subjects, topical applications of extracts delivering the Nrf2 <span class="hlt">activator</span> sulforaphane, reduced the degree of <span class="hlt">solar</span>-simulated UV radiation-induced skin erythema, a quantifiable surrogate end-point for cutaneous damage and skin cancer risk. Collectively, these data show that Nrf2 is not a driver for tumorigenesis even upon exposure to a very potent and complete carcinogen, and strongly suggest that the frequent <span class="hlt">activation</span> of Nrf2 in established human tumors is a marker of metabolic adaptation. PMID:25804610</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.osti.gov/biblio/21460075-changes-solar-meridional-velocity-profile-during-cycle-explained-flows-toward-activity-belts','SCIGOV-STC'); return false;" href="https://www.osti.gov/biblio/21460075-changes-solar-meridional-velocity-profile-during-cycle-explained-flows-toward-activity-belts"><span>CHANGES OF THE <span class="hlt">SOLAR</span> MERIDIONAL VELOCITY PROFILE DURING CYCLE 23 EXPLAINED BY FLOWS TOWARD THE <span class="hlt">ACTIVITY</span> BELTS</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>Cameron, R. H.; Schuessler, M., E-mail: cameron@mps.mpg.d</p> <p></p> <p>The <span class="hlt">solar</span> meridional flow is an important ingredient in Babcock-Leighton type models of the <span class="hlt">solar</span> dynamo. Global variations of this flow have been suggested to explain the variations in the amplitudes and lengths of the <span class="hlt">activity</span> cycles. Recently, cycle-related variations in the amplitude of the P{sup 1}{sub 2} term in the Legendre decomposition of the observed meridional flow have been reported. The result is often interpreted in terms of an overall variation in the flow amplitude during the <span class="hlt">activity</span> cycle. Using a semi-empirical model based upon the observed distribution of magnetic flux on the <span class="hlt">solar</span> surface, we show that themore » reported variations of the P{sup 1}{sub 2} term can be explained by the observed localized inflows into the <span class="hlt">active</span> region belts. No variation of the overall meridional flow amplitude is required.« less</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/26290974','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/26290974"><span>Understanding the Thickness-Dependent Performance of Organic Bulk Heterojunction <span class="hlt">Solar</span> Cells: The <span class="hlt">Influence</span> of Mobility, Lifetime, and Space Charge.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Kirchartz, Thomas; Agostinelli, Tiziano; Campoy-Quiles, Mariano; Gong, Wei; Nelson, Jenny</p> <p>2012-12-06</p> <p>We investigate the reasons for the dependence of photovoltaic performance on the absorber thickness of organic <span class="hlt">solar</span> cells using experiments and drift-diffusion simulations. The main trend in photocurrent and fill factor versus thickness is determined by mobility and lifetime of the charge carriers. In addition, space charge becomes more and more important the thicker the device is because it creates field free regions with low collection efficiency. The two main sources of space-charge effects are doping and asymmetric mobilities. We show that for our experimental results on Si-PCPDTBT:PC71BM (poly[(4,40-bis(2-ethylhexyl)dithieno[3,2-b:20,30-d]silole)-2,6-diyl-alt-(4,7-bis(2-thienyl)-2,1,3-benzothiadiazole)-5,50-diyl]:[6,6]-phenyl C71-butyric acid methyl ester) <span class="hlt">solar</span> cells, the <span class="hlt">influence</span> of doping is most likely the dominant <span class="hlt">influence</span> on the space charge and has an important effect on the thickness dependence of performance.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/19900010714','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/19900010714"><span>MAX 1991. The <span class="hlt">active</span> sun: A plan for pursuing the study of the <span class="hlt">active</span> sun at the time of the next maximum in <span class="hlt">solar</span> <span class="hlt">activity</span>, January 1985</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Acton, L.</p> <p>1989-01-01</p> <p>The results of the discusions of a working group for the definition of a program for the forthcoming crest of <span class="hlt">solar</span> <span class="hlt">activity</span>, 1990 to 1993 are presented. The MAX '91 program described are intended to achieve important scientific goals within the context of the natural <span class="hlt">solar</span> variability. The heart of the MAX '91 program is a series of campaigns oriented towards specific scientific problems, and taking place in the <span class="hlt">solar</span> maximum period 1990 to 1993. These campaigns will take advantage of the load-carrying capability of the Space Shuttle to fly instruments with observational capabilities very different from those of the <span class="hlt">Solar</span> Maximum Mission. Various combinations of instruments appropriate to the specific scientific problem of a given campaign would be flown on a Shuttle sortie mission.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2011PhDT.......138T','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2011PhDT.......138T"><span>Radio-derived three-dimensional structure of a <span class="hlt">solar</span> <span class="hlt">active</span> region</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Tun, Samuel D.</p> <p></p> <p><span class="hlt">Solar</span> <span class="hlt">active</span> regions are the source of the most violent events observed on the Sun, some of which have a direct impact to modern civilization. Efforts to understand and predict such events require determination of the three-dimensional distributions of density, temperature, and magnetic fields above such <span class="hlt">active</span> regions. This thesis presents the structure of the <span class="hlt">solar</span> atmosphere above <span class="hlt">active</span> region AR 10923, observed on 2006 Nov 10, as deduced from multi-wavelength studies including combined microwave observations from the Very Large Array (VLA) and the Owens Valley <span class="hlt">Solar</span> Array (OVSA). The VLA observations provide excellent image quality at a few widely spaced frequencies while the OVSA data provide information at many intermediate frequencies to fill in the spectral coverage. In order to optimize the OVSA data for spectroscopic studies, the L1 method of self-calibration was implemented at this observatory, producing the best single frequency maps produced to date. Images at the 25 distinct, available frequencies are used to provide spatially resolved spectra along many lines of sight in the <span class="hlt">active</span> region, from which microwave spectral diagnostics are obtained for deducing two-dimensional maps of temperature, magnetic field strength, and column density. The derived quantities are compared with multi-wavelength observations from SoHO and Hinode spacecraft, and with a standard potential magnetic field extrapolation. It is found that a two component temperature model is required to fit the data, in which a hot (> 2 MK) lower corona above the strong-field plage and sunspot regions (emitting via the gyroresonance process) is overlaid with somewhat cooler (˜ 1 MK) coronal loops that partially absorb the gyroresonance emission through the free-free (Bremsstrahlung) process. It is also found that the potential magnetic field extrapolation model can quantitatively account for the observed gyroresonance emission over most of the <span class="hlt">active</span> region, but in a few areas a higher</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/19850026826','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/19850026826"><span>Sporadic radio emission connected with a definite manifestation of <span class="hlt">solar</span> <span class="hlt">activity</span> in the near Earth space</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Dudnic, A. V.; Zaljubovski, I. I.; Kartashev, V. M.; Shmatko, E. S.</p> <p>1985-01-01</p> <p>Sporadic radio emission of near Earth space at the frequency of 38 MHz is shown to appear in the event of a rapid development of instabilities in the ionospheric plasma. The instabilities are generated due to primary ionospheric disturbances occurring under the <span class="hlt">influence</span> of <span class="hlt">solar</span> chromospheric flares.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://eric.ed.gov/?q=solar+AND+two&pg=7&id=ED222362','ERIC'); return false;" href="https://eric.ed.gov/?q=solar+AND+two&pg=7&id=ED222362"><span><span class="hlt">Solar</span> Energy in the Home. Revised.</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>Roeder, Allen A.; Woodland, James A.</p> <p></p> <p>Recommended for grades 10-12 physical, earth, or general science classes, this 5-7 day unit is designed to give students a general understanding of <span class="hlt">solar</span> energy and its use as a viable alternative to present energy sources. Along with this technology, students examine several factors of <span class="hlt">solar</span> energy which <span class="hlt">influence</span> the choice of <span class="hlt">solar</span> home site…</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2012APh....36...18S','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2012APh....36...18S"><span>Analysis of gamma radiation from a radon source: Indications of a <span class="hlt">solar</span> <span class="hlt">influence</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Sturrock, P. A.; Steinitz, G.; Fischbach, E.; Javorsek, D.; Jenkins, J. H.</p> <p>2012-08-01</p> <p>This article presents an analysis of about 29,000 measurements of gamma radiation associated with the decay of radon in a sealed container at the Geological Survey of Israel (GSI) Laboratory in Jerusalem between 28 January 2007 and 10 May 2010. These measurements exhibit strong variations in time of year and time of day, which may be due in part to environmental <span class="hlt">influences</span>. However, time-series analysis reveals a number of periodicities, including two at approximately 11.2 year-1 and 12.5 year-1. We have previously found these oscillations in nuclear-decay data acquired at the Brookhaven National Laboratory and at the Physiklisch-Technische Bundesanstalt, and we have suggested that these oscillations are attributable to some form of <span class="hlt">solar</span> radiation that has its origin in the deep <span class="hlt">solar</span> interior. A curious property of the GSI data is that the annual oscillation is much stronger in daytime data than in nighttime data, but the opposite is true for all other oscillations. This may be a systematic effect but, if it is not, this property should help narrow the theoretical options for the mechanism responsible for decay-rate variability.</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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