Sample records for weather modeling system

  1. Browsing Space Weather Data and Models with the Integrated Space Weather Analysis (iSWA) System

    NASA Technical Reports Server (NTRS)

    Maddox, Marlo M.; Mullinix, Richard E.; Berrios, David H.; Hesse, Michael; Rastaetter, Lutz; Pulkkinen, Antti; Hourcle, Joseph A.; Thompson, Barbara J.

    2011-01-01

    The Integrated Space Weather Analysis (iSWA) System is a comprehensive web-based platform for space weather information that combines data from solar, heliospheric and geospace observatories with forecasts based on the most advanced space weather models. The iSWA system collects, generates, and presents a wide array of space weather resources in an intuitive, user-configurable, and adaptable format - thus enabling users to respond to current and future space weather impacts as well as enabling post-impact analysis. iSWA currently provides over 200 data and modeling products, and features a variety of tools that allow the user to browse, combine, and examine data and models from various sources. This presentation will consist of a summary of the iSWA products and an overview of the customizable user interfaces, and will feature several tutorial demonstrations highlighting the interactive tools and advanced capabilities.

  2. Quality assurance of weather data for agricultural system model input

    USDA-ARS?s Scientific Manuscript database

    It is well known that crop production and hydrologic variation on watersheds is weather related. Rarely, however, is meteorological data quality checks reported for agricultural systems model research. We present quality assurance procedures for agricultural system model weather data input. Problems...

  3. Forecast and virtual weather driven plant disease risk modeling system

    USDA-ARS?s Scientific Manuscript database

    We describe a system in use and development that leverages public weather station data, several spatialized weather forecast types, leaf wetness estimation, generic plant disease models, and online statistical evaluation. Convergent technological developments in all these areas allow, with funding f...

  4. The Ensemble Space Weather Modeling System (eSWMS): Status, Capabilities and Challenges

    NASA Astrophysics Data System (ADS)

    Fry, C. D.; Eccles, J. V.; Reich, J. P.

    2010-12-01

    Marking a milestone in space weather forecasting, the Space Weather Modeling System (SWMS) successfully completed validation testing in advance of operational testing at Air Force Weather Agency’s primary space weather production center. This is the first coupling of stand-alone, physics-based space weather models that are currently in operations at AFWA supporting the warfighter. Significant development effort went into ensuring the component models were portable and scalable while maintaining consistent results across diverse high performance computing platforms. Coupling was accomplished under the Earth System Modeling Framework (ESMF). The coupled space weather models are the Hakamada-Akasofu-Fry version 2 (HAFv2) solar wind model and GAIM1, the ionospheric forecast component of the Global Assimilation of Ionospheric Measurements (GAIM) model. The SWMS was developed by team members from AFWA, Explorations Physics International, Inc. (EXPI) and Space Environment Corporation (SEC). The successful development of the SWMS provides new capabilities beyond enabling extended lead-time, data-driven ionospheric forecasts. These include ingesting diverse data sets at higher resolution, incorporating denser computational grids at finer time steps, and performing probability-based ensemble forecasts. Work of the SWMS development team now focuses on implementing the ensemble-based probability forecast capability by feeding multiple scenarios of 5 days of solar wind forecasts to the GAIM1 model based on the variation of the input fields to the HAFv2 model. The ensemble SWMS (eSWMS) will provide the most-likely space weather scenario with uncertainty estimates for important forecast fields. The eSWMS will allow DoD mission planners to consider the effects of space weather on their systems with more advance warning than is currently possible. The payoff is enhanced, tailored support to the warfighter with improved capabilities, such as point-to-point HF propagation forecasts

  5. Sensor performance and weather effects modeling for intelligent transportation systems (ITS) applications

    NASA Astrophysics Data System (ADS)

    Everson, Jeffrey H.; Kopala, Edward W.; Lazofson, Laurence E.; Choe, Howard C.; Pomerleau, Dean A.

    1995-01-01

    Optical sensors are used for several ITS applications, including lateral control of vehicles, traffic sign recognition, car following, autonomous vehicle navigation, and obstacle detection. This paper treats the performance assessment of a sensor/image processor used as part of an on-board countermeasure system to prevent single vehicle roadway departure crashes. Sufficient image contrast between objects of interest and backgrounds is an essential factor influencing overall system performance. Contrast is determined by material properties affecting reflected/radiated intensities, as well as weather and visibility conditions. This paper discusses the modeling of these parameters and characterizes the contrast performance effects due to reduced visibility. The analysis process first involves generation of inherent road/off- road contrasts, followed by weather effects as a contrast modification. The sensor is modeled as a charge coupled device (CCD), with variable parameters. The results of the sensor/weather modeling are used to predict the performance on an in-vehicle warning system under various levels of adverse weather. Software employed in this effort was previously developed for the U.S. Air Force Wright Laboratory to determine target/background detection and recognition ranges for different sensor systems operating under various mission scenarios.

  6. GFDL's unified regional-global weather-climate modeling system with variable resolution capability for severe weather predictions and regional climate simulations

    NASA Astrophysics Data System (ADS)

    Lin, S. J.

    2015-12-01

    The NOAA/Geophysical Fluid Dynamics Laboratory has been developing a unified regional-global modeling system with variable resolution capabilities that can be used for severe weather predictions (e.g., tornado outbreak events and cat-5 hurricanes) and ultra-high-resolution (1-km) regional climate simulations within a consistent global modeling framework. The fundation of this flexible regional-global modeling system is the non-hydrostatic extension of the vertically Lagrangian dynamical core (Lin 2004, Monthly Weather Review) known in the community as FV3 (finite-volume on the cubed-sphere). Because of its flexability and computational efficiency, the FV3 is one of the final candidates of NOAA's Next Generation Global Prediction System (NGGPS). We have built into the modeling system a stretched (single) grid capability, a two-way (regional-global) multiple nested grid capability, and the combination of the stretched and two-way nests, so as to make convection-resolving regional climate simulation within a consistent global modeling system feasible using today's High Performance Computing System. One of our main scientific goals is to enable simulations of high impact weather phenomena (such as tornadoes, thunderstorms, category-5 hurricanes) within an IPCC-class climate modeling system previously regarded as impossible. In this presentation I will demonstrate that it is computationally feasible to simulate not only super-cell thunderstorms, but also the subsequent genesis of tornadoes using a global model that was originally designed for century long climate simulations. As a unified weather-climate modeling system, we evaluated the performance of the model with horizontal resolution ranging from 1 km to as low as 200 km. In particular, for downscaling studies, we have developed various tests to ensure that the large-scale circulation within the global varaible resolution system is well simulated while at the same time the small-scale can be accurately captured

  7. Weather Information System

    NASA Technical Reports Server (NTRS)

    1995-01-01

    WxLink is an aviation weather system based on advanced airborne sensors, precise positioning available from the satellite-based Global Positioning System, cockpit graphics and a low-cost datalink. It is a two-way system that uplinks weather information to the aircraft and downlinks automatic pilot reports of weather conditions aloft. Manufactured by ARNAV Systems, Inc., the original technology came from Langley Research Center's cockpit weather information system, CWIN (Cockpit Weather INformation). The system creates radar maps of storms, lightning and reports of surface observations, offering improved safety, better weather monitoring and substantial fuel savings.

  8. weather@home 2: validation of an improved global-regional climate modelling system

    NASA Astrophysics Data System (ADS)

    Guillod, Benoit P.; Jones, Richard G.; Bowery, Andy; Haustein, Karsten; Massey, Neil R.; Mitchell, Daniel M.; Otto, Friederike E. L.; Sparrow, Sarah N.; Uhe, Peter; Wallom, David C. H.; Wilson, Simon; Allen, Myles R.

    2017-05-01

    Extreme weather events can have large impacts on society and, in many regions, are expected to change in frequency and intensity with climate change. Owing to the relatively short observational record, climate models are useful tools as they allow for generation of a larger sample of extreme events, to attribute recent events to anthropogenic climate change, and to project changes in such events into the future. The modelling system known as weather@home, consisting of a global climate model (GCM) with a nested regional climate model (RCM) and driven by sea surface temperatures, allows one to generate a very large ensemble with the help of volunteer distributed computing. This is a key tool to understanding many aspects of extreme events. Here, a new version of the weather@home system (weather@home 2) with a higher-resolution RCM over Europe is documented and a broad validation of the climate is performed. The new model includes a more recent land-surface scheme in both GCM and RCM, where subgrid-scale land-surface heterogeneity is newly represented using tiles, and an increase in RCM resolution from 50 to 25 km. The GCM performs similarly to the previous version, with some improvements in the representation of mean climate. The European RCM temperature biases are overall reduced, in particular the warm bias over eastern Europe, but large biases remain. Precipitation is improved over the Alps in summer, with mixed changes in other regions and seasons. The model is shown to represent the main classes of regional extreme events reasonably well and shows a good sensitivity to its drivers. In particular, given the improvements in this version of the weather@home system, it is likely that more reliable statements can be made with regards to impact statements, especially at more localized scales.

  9. User's guide to the weather model: a component of the western spruce budworm modeling system.

    Treesearch

    W. P. Kemp; N. L. Crookston; P. W. Thomas

    1989-01-01

    A stochastic model useful in simulating daily maximum and minimum temperature and precipitation developed by Bruhn and others has been adapted for use in the western spruce budworm modeling system. This document describes how to use the weather model and illustrates some aspects of its behavior.

  10. Towards a unified Global Weather-Climate Prediction System

    NASA Astrophysics Data System (ADS)

    Lin, S. J.

    2016-12-01

    The Geophysical Fluid Dynamics Laboratory has been developing a unified regional-global modeling system with variable resolution capabilities that can be used for severe weather predictions and kilometer scale regional climate simulations within a unified global modeling system. The foundation of this flexible modeling system is the nonhydrostatic Finite-Volume Dynamical Core on the Cubed-Sphere (FV3). A unique aspect of FV3 is that it is "vertically Lagrangian" (Lin 2004), essentially reducing the equation sets to two dimensions, and is the single most important reason why FV3 outperforms other non-hydrostatic cores. Owning to its accuracy, adaptability, and computational efficiency, the FV3 has been selected as the "engine" for NOAA's Next Generation Global Prediction System (NGGPS). We have built into the modeling system a stretched grid, a two-way regional-global nested grid, and an optimal combination of the stretched and two-way nests capability, making kilometer-scale regional simulations within a global modeling system feasible. Our main scientific goal is to enable simulations of high impact weather phenomena (such as tornadoes, thunderstorms, category-5 hurricanes) within an IPCC-class climate modeling system previously regarded as impossible. In this presentation I will demonstrate that, with the FV3, it is computationally feasible to simulate not only super-cell thunderstorms, but also the subsequent genesis of tornado-like vortices using a global model that was originally designed for climate simulations. The development and tuning strategy between traditional weather and climate models are fundamentally different due to different metrics. We were able to adapt and use traditional "climate" metrics or standards, such as angular momentum conservation, energy conservation, and flux balance at top of the atmosphere, and gain insight into problems of traditional weather prediction model for medium-range weather prediction, and vice versa. Therefore, the

  11. Characteristics of Operational Space Weather Forecasting: Observations and Models

    NASA Astrophysics Data System (ADS)

    Berger, Thomas; Viereck, Rodney; Singer, Howard; Onsager, Terry; Biesecker, Doug; Rutledge, Robert; Hill, Steven; Akmaev, Rashid; Milward, George; Fuller-Rowell, Tim

    2015-04-01

    In contrast to research observations, models and ground support systems, operational systems are characterized by real-time data streams and run schedules, with redundant backup systems for most elements of the system. We review the characteristics of operational space weather forecasting, concentrating on the key aspects of ground- and space-based observations that feed models of the coupled Sun-Earth system at the NOAA/Space Weather Prediction Center (SWPC). Building on the infrastructure of the National Weather Service, SWPC is working toward a fully operational system based on the GOES weather satellite system (constant real-time operation with back-up satellites), the newly launched DSCOVR satellite at L1 (constant real-time data network with AFSCN backup), and operational models of the heliosphere, magnetosphere, and ionosphere/thermosphere/mesophere systems run on the Weather and Climate Operational Super-computing System (WCOSS), one of the worlds largest and fastest operational computer systems that will be upgraded to a dual 2.5 Pflop system in 2016. We review plans for further operational space weather observing platforms being developed in the context of the Space Weather Operations Research and Mitigation (SWORM) task force in the Office of Science and Technology Policy (OSTP) at the White House. We also review the current operational model developments at SWPC, concentrating on the differences between the research codes and the modified real-time versions that must run with zero fault tolerance on the WCOSS systems. Understanding the characteristics and needs of the operational forecasting community is key to producing research into the coupled Sun-Earth system with maximal societal benefit.

  12. A Product Development Decision Model for Cockpit Weather Information System

    NASA Technical Reports Server (NTRS)

    Sireli, Yesim; Kauffmann, Paul; Gupta, Surabhi; Kachroo, Pushkin; Johnson, Edward J., Jr. (Technical Monitor)

    2003-01-01

    There is a significant market demand for advanced cockpit weather information products. However, it is unclear how to identify the most promising technological options that provide the desired mix of consumer requirements by employing feasible technical systems at a price that achieves market success. This study develops a unique product development decision model that employs Quality Function Deployment (QFD) and Kano's model of consumer choice. This model is specifically designed for exploration and resolution of this and similar information technology related product development problems.

  13. A Product Development Decision Model for Cockpit Weather Information Systems

    NASA Technical Reports Server (NTRS)

    Sireli, Yesim; Kauffmann, Paul; Gupta, Surabhi; Kachroo, Pushkin

    2003-01-01

    There is a significant market demand for advanced cockpit weather information products. However, it is unclear how to identify the most promising technological options that provide the desired mix of consumer requirements by employing feasible technical systems at a price that achieves market success. This study develops a unique product development decision model that employs Quality Function Deployment (QFD) and Kano's model of consumer choice. This model is specifically designed for exploration and resolution of this and similar information technology related product development problems.

  14. A regressive storm model for extreme space weather

    NASA Astrophysics Data System (ADS)

    Terkildsen, Michael; Steward, Graham; Neudegg, Dave; Marshall, Richard

    2012-07-01

    Extreme space weather events, while rare, pose significant risk to society in the form of impacts on critical infrastructure such as power grids, and the disruption of high end technological systems such as satellites and precision navigation and timing systems. There has been an increased focus on modelling the effects of extreme space weather, as well as improving the ability of space weather forecast centres to identify, with sufficient lead time, solar activity with the potential to produce extreme events. This paper describes the development of a data-based model for predicting the occurrence of extreme space weather events from solar observation. The motivation for this work was to develop a tool to assist space weather forecasters in early identification of solar activity conditions with the potential to produce extreme space weather, and with sufficient lead time to notify relevant customer groups. Data-based modelling techniques were used to construct the model, and an extensive archive of solar observation data used to train, optimise and test the model. The optimisation of the base model aimed to eliminate false negatives (missed events) at the expense of a tolerable increase in false positives, under the assumption of an iterative improvement in forecast accuracy during progression of the solar disturbance, as subsequent data becomes available.

  15. Models Required to Mitigate Impacts of Space Weather on Space Systems

    NASA Technical Reports Server (NTRS)

    Barth, Janet L.

    2003-01-01

    This viewgraph presentation attempts to develop a model of factors which need to be considered in the design and construction of spacecraft to lessen the effects of space weather on these vehicles. Topics considered include: space environments and effects, radiation environments and effects, space weather drivers, space weather models, climate models, solar proton activity and mission design for the GOES mission. The authors conclude that space environment models need to address issues from mission planning through operations and a program to develop and validate authoritative space environment models for application to spacecraft design does not exist at this time.

  16. Models of Weather Impact on Air Traffic

    NASA Technical Reports Server (NTRS)

    Kulkarni, Deepak; Wang, Yao

    2017-01-01

    Flight delays have been a serious problem in the national airspace system costing about $30B per year. About 70 of the delays are attributed to weather and upto two thirds of these are avoidable. Better decision support tools would reduce these delays and improve air traffic management tools. Such tools would benefit from models of weather impacts on the airspace operations. This presentation discusses use of machine learning methods to mine various types of weather and traffic data to develop such models.

  17. WOD - Weather On Demand forecasting system

    NASA Astrophysics Data System (ADS)

    Rognvaldsson, Olafur; Ragnarsson, Logi; Stanislawska, Karolina

    2017-04-01

    The backbone of the Belgingur forecasting system (called WOD - Weather On Demand) is the WRF-Chem atmospheric model, with a number of in-house customisations. Initial and boundary data are taken from the Global Forecasting System, operated by the National Oceanic and Atmospheric Administration (NOAA). Operational forecasts use cycling of a number of parameters, mainly deep soil and surface fields. This is done to minimise spin-up effects and to ensure proper book-keeping of hydrological fields such as snow accumulation and runoff, as well as the constituents of various chemical parameters. The WOD system can be used to create conventional short- to medium-range weather forecasts for any location on the globe. The WOD system can also be used for air quality purposes (e.g. dispersion forecasts from volcanic eruptions) and as a tool to provide input to other modelling systems, such as hydrological models. A wide variety of post-processing options are also available, making WOD an ideal tool for creating highly customised output that can be tailored to the specific needs of individual end-users. The most recent addition to the WOD system is an integrated verification system where forecasts can be compared to surface observations from chosen locations. Forecast visualisation, such as weather charts, meteograms, weather icons and tables, is done via number of web components that can be configured to serve the varying needs of different end-users. The WOD system itself can be installed in an automatic way on hardware running a range of Linux based OS. System upgrades can also be done in semi-automatic fashion, i.e. upgrades and/or bug-fixes can be pushed to the end-user hardware without system downtime. Importantly, the WOD system requires only rudimentary knowledge of the WRF modelling, and the Linux operating systems on behalf of the end-user, making it an ideal NWP tool in locations with limited IT infrastructure.

  18. Space Weather Models at the CCMC And Their Capabilities

    NASA Technical Reports Server (NTRS)

    Hesse, Michael; Rastatter, Lutz; MacNeice, Peter; Kuznetsova, Masha

    2007-01-01

    The Community Coordinated Modeling Center (CCMC) is a US inter-agency activity aiming at research in support of the generation of advanced space weather models. As one of its main functions, the CCMC provides to researchers the use of space science models, even if they are not model owners themselves. The second focus of CCMC activities is on validation and verification of space weather models, and on the transition of appropriate models to space weather forecast centers. As part of the latter activity, the CCMC develops real-time simulation systems that stress models through routine execution. A by-product of these real-time calculations is the ability to derive model products, which may be useful for space weather operators. In this presentation, we will provide an overview of the community-provided, space weather-relevant, model suite, which resides at CCMC. We will discuss current capabilities, and analyze expected future developments of space weather related modeling.

  19. Investigating Surface Bias Errors in the Weather Research and Forecasting (WRF) Model using a Geographic Information System (GIS)

    DTIC Science & Technology

    2015-02-01

    WRF ) Model using a Geographic Information System (GIS) by Jeffrey A Smith, Theresa A Foley, John W Raby, and Brian Reen...ARL-TR-7212 ● FEB 2015 US Army Research Laboratory Investigating Surface Bias Errors in the Weather Research and Forecasting ( WRF ) Model...SUBTITLE Investigating surface bias errors in the Weather Research and Forecasting ( WRF ) Model using a Geographic Information System (GIS) 5a

  20. Weather Observation Systems and Efficiency of Fighting Forest Fires

    NASA Astrophysics Data System (ADS)

    Khabarov, N.; Moltchanova, E.; Obersteiner, M.

    2007-12-01

    Weather observation is an essential component of modern forest fire management systems. Satellite and in-situ based weather observation systems might help to reduce forest loss, human casualties and destruction of economic capital. In this paper, we develop and apply a methodology to assess the benefits of various weather observation systems on reductions of burned area due to early fire detection. In particular, we consider a model where the air patrolling schedule is determined by a fire hazard index. The index is computed from gridded daily weather data for the area covering parts Spain and Portugal. We conduct a number of simulation experiments. First, the resolution of the original data set is artificially reduced. The reduction of the total forest burned area associated with air patrolling based on a finer weather grid indicates the benefit of using higher spatially resolved weather observations. Second, we consider a stochastic model to simulate forest fires and explore the sensitivity of the model with respect to the quality of input data. The analysis of combination of satellite and ground monitoring reveals potential cost saving due to a "system of systems effect" and substantial reduction in burned area. Finally, we estimate the marginal improvement schedule for loss of life and economic capital as a function of the improved fire observing system.

  1. The importance of terrestrial weathering for climate system modelling on extended timescales: a study with the UVic ESCM

    NASA Astrophysics Data System (ADS)

    Brault, Marc-Olivier; Matthews, Damon; Mysak, Lawrence

    2016-04-01

    The chemical erosion of carbonate and silicate rocks is a key process in the global carbon cycle and, through its coupling with calcium carbonate deposition in the ocean, is the primary sink of carbon on geologic timescales. The dynamic interdependence of terrestrial weathering rates with atmospheric temperature and carbon dioxide concentrations is crucial to the regulation of Earth's climate over multi-millennial timescales. However any attempts to develop a modeling context for terrestrial weathering as part of a dynamic climate system are limited, mostly because of the difficulty in adapting the multi-millennial timescales of the implied negative feedback mechanism with those of the atmosphere and ocean. Much of the earlier work on this topic is therefore based on box-model approaches, abandoning spatial variability for the sake of computational efficiency and the possibility to investigate the impact of weathering on climate change over time frames much longer than those allowed by traditional climate system models. As a result we still have but a rudimentary understanding of the chemical weathering feedback mechanism and its effects on ocean biogeochemistry and atmospheric CO2. Here, we introduce a spatially-explicit, rock weathering model into the University of Victoria Earth System Climate Model (UVic ESCM). We use a land map which takes into account a number of different rock lithologies, changes in sea level, as well as an empirical model of the temperature and NPP dependency of weathering rates for the different rock types. We apply this new model to the last deglacial period (c. 21000BP to 13000BP) as well as a future climate change scenario (c. 1800AD to 6000AD+), comparing the results of our 2-D version of the weathering feedback mechanism to simulations using only the box-model parameterizations of Meissner et al. [2012]. These simulations reveal the importance of two-dimensional factors (i.e., changes in sea level and rock type distribution) in the

  2. Pilot Weather Advisor System

    NASA Technical Reports Server (NTRS)

    Lindamood, Glenn; Martzaklis, Konstantinos Gus; Hoffler, Keith; Hill, Damon; Mehrotra, Sudhir C.; White, E. Richard; Fisher, Bruce D.; Crabill, Norman L.; Tucholski, Allen D.

    2006-01-01

    The Pilot Weather Advisor (PWA) system is an automated satellite radio-broadcasting system that provides nearly real-time weather data to pilots of aircraft in flight anywhere in the continental United States. The system was designed to enhance safety in two distinct ways: First, the automated receipt of information would relieve the pilot of the time-consuming and distracting task of obtaining weather information via voice communication with ground stations. Second, the presentation of the information would be centered around a map format, thereby making the spatial and temporal relationships in the surrounding weather situation much easier to understand

  3. A Real-Time Offshore Weather Risk Advisory System

    NASA Astrophysics Data System (ADS)

    Jolivet, Samuel; Zemskyy, Pavlo; Mynampati, Kalyan; Babovic, Vladan

    2015-04-01

    Offshore oil and gas operations in South East Asia periodically face extended downtime due to unpredictable weather conditions, including squalls that are accompanied by strong winds, thunder, and heavy rains. This downtime results in financial losses. Hence, a real time weather risk advisory system is developed to provide the offshore Oil and Gas (O&G) industry specific weather warnings in support of safety and environment security. This system provides safe operating windows based on sensitivity of offshore operations to sea state. Information products for safety and security include area of squall occurrence for the next 24 hours, time before squall strike, and heavy sea state warning for the next 3, 6, 12 & 24 hours. These are predicted using radar now-cast, high resolution Numerical Weather Prediction (NWP) and Data Assimilation (DA). Radar based now-casting leverages the radar data to produce short term (up to 3 hours) predictions of severe weather events including squalls/thunderstorms. A sea state approximation is provided through developing a translational model based on these predictions to risk rank the sensitivity of operations. A high resolution Weather Research and Forecasting (WRF, an open source NWP model) is developed for offshore Brunei, Malaysia and the Philippines. This high resolution model is optimized and validated against the adaptation of temperate to tropical met-ocean parameterization. This locally specific parameters are calibrated against federated data to achieve a 24 hour forecast of high resolution Convective Available Potential Energy (CAPE). CAPE is being used as a proxy for the risk of squall occurrence. Spectral decomposition is used to blend the outputs of the now-cast and the forecast in order to assimilate near real time weather observations as an implementation of the integration of data sources. This system uses the now-cast for the first 3 hours and then the forecast prediction horizons of 3, 6, 12 & 24 hours. The output is

  4. Adaptation of Mesoscale Weather Models to Local Forecasting

    NASA Technical Reports Server (NTRS)

    Manobianco, John T.; Taylor, Gregory E.; Case, Jonathan L.; Dianic, Allan V.; Wheeler, Mark W.; Zack, John W.; Nutter, Paul A.

    2003-01-01

    Methodologies have been developed for (1) configuring mesoscale numerical weather-prediction models for execution on high-performance computer workstations to make short-range weather forecasts for the vicinity of the Kennedy Space Center (KSC) and the Cape Canaveral Air Force Station (CCAFS) and (2) evaluating the performances of the models as configured. These methodologies have been implemented as part of a continuing effort to improve weather forecasting in support of operations of the U.S. space program. The models, methodologies, and results of the evaluations also have potential value for commercial users who could benefit from tailoring their operations and/or marketing strategies based on accurate predictions of local weather. More specifically, the purpose of developing the methodologies for configuring the models to run on computers at KSC and CCAFS is to provide accurate forecasts of winds, temperature, and such specific thunderstorm-related phenomena as lightning and precipitation. The purpose of developing the evaluation methodologies is to maximize the utility of the models by providing users with assessments of the capabilities and limitations of the models. The models used in this effort thus far include the Mesoscale Atmospheric Simulation System (MASS), the Regional Atmospheric Modeling System (RAMS), and the National Centers for Environmental Prediction Eta Model ( Eta for short). The configuration of the MASS and RAMS is designed to run the models at very high spatial resolution and incorporate local data to resolve fine-scale weather features. Model preprocessors were modified to incorporate surface, ship, buoy, and rawinsonde data as well as data from local wind towers, wind profilers, and conventional or Doppler radars. The overall evaluation of the MASS, Eta, and RAMS was designed to assess the utility of these mesoscale models for satisfying the weather-forecasting needs of the U.S. space program. The evaluation methodology includes

  5. Weather Forecaster Understanding of Climate Models

    NASA Astrophysics Data System (ADS)

    Bol, A.; Kiehl, J. T.; Abshire, W. E.

    2013-12-01

    Weather forecasters, particularly those in broadcasting, are the primary conduit to the public for information on climate and climate change. However, many weather forecasters remain skeptical of model-based climate projections. To address this issue, The COMET Program developed an hour-long online lesson of how climate models work, targeting an audience of weather forecasters. The module draws on forecasters' pre-existing knowledge of weather, climate, and numerical weather prediction (NWP) models. In order to measure learning outcomes, quizzes were given before and after the lesson. Preliminary results show large learning gains. For all people that took both pre and post-tests (n=238), scores improved from 48% to 80%. Similar pre/post improvement occurred for National Weather Service employees (51% to 87%, n=22 ) and college faculty (50% to 90%, n=7). We believe these results indicate a fundamental misunderstanding among many weather forecasters of (1) the difference between weather and climate models, (2) how researchers use climate models, and (3) how they interpret model results. The quiz results indicate that efforts to educate the public about climate change need to include weather forecasters, a vital link between the research community and the general public.

  6. Modeling rock weathering in small watersheds

    NASA Astrophysics Data System (ADS)

    Pacheco, Fernando A. L.; Van der Weijden, Cornelis H.

    2014-05-01

    Many mountainous watersheds are conceived as aquifer media where multiple groundwater flow systems have developed (Tóth, 1963), and as bimodal landscapes where differential weathering of bare and soil-mantled rock has occurred (Wahrhaftig, 1965). The results of a weathering algorithm (Pacheco and Van der Weijden, 2012a, 2014), which integrates topographic, hydrologic, rock structure and chemical data to calculate weathering rates at the watershed scale, validated the conceptual models in the River Sordo basin, a small watershed located in the Marão cordillera (North of Portugal). The coupling of weathering, groundwater flow and landscape evolution analyses, as accomplished in this study, is innovative and represents a remarkable achievement towards regionalization of rock weathering at the watershed scale. The River Sordo basin occupies an area of approximately 51.2 km2 and was shaped on granite and metassediment terrains between the altitudes 185-1300 m. The groundwater flow system is composed of recharge areas located at elevations >700 m, identified on the basis of δ18O data. Discharge cells comprehend terminations of local, intermediate and regional flow systems, identified on the basis of spring density patterns, infiltration depth estimates based on 87Sr/86Sr data, and spatial distributions of groundwater pH and natural mineralization. Intermediate and regional flow systems, defined where infiltration depths >125 m, develop solely along the contact zone between granites and metassediments, because fractures in this region are profound and their density is very large. Weathering is accelerated where rocks are covered by thick soils, being five times faster relative to sectors of the basin where rocks are covered by thin soils. Differential weathering of bare and soil-mantled rock is also revealed by the spatial distribution of calculated aquifer hydraulic diffusivities and groundwater travel times.

  7. Large-Scale, Extratropical Weather Systems within Mars' Atmosphere

    NASA Astrophysics Data System (ADS)

    Hollingsworth, Jeffery L.

    2013-04-01

    During late autumn through early spring, extratropical regions on Mars exhibit profound mean zonal equator-to-pole thermal contrasts. The imposition of this strong meridional temperature variation supports intense eastward-traveling, synoptic weather systems (i.e., transient baroclinic/barotropic waves) within Mars' extratropical atmosphere. Such disturbances grow, mature and decay within the east-west varying seasonal-mean midlatitude jet stream (i.e., the polar vortex) on the planet. Near the surface, the weather disturbances indicated large-scale spiraling "comma"-shaped dust cloud structures and scimitar-shaped dust fronts, indicative of processes associated with cyclo-/fronto-genesis. The weather systems occur during specific seasons on Mars, and in both hemispheres. The northern hemisphere (NH) disturbances are significantly more intense than their counterparts in the southern hemisphere (SH). Further, the NH weather systems and accompanying frontal waves appear to have significant impacts on the transport of tracer fields (e.g., particularly dust and to some extent water species (vapor/ice) as well). And regarding dust, frontal waves appear to be key agents in the lifting, lofting, organization and transport of this particular atmospheric aerosol. In this paper, a brief background and supporting observations of Mars' extratropical weather systems is presented. This is followed by a short review of the theory and various modeling studies (i.e., ranging from highly simplified, mechanistic and full global circulation modeling investigations) which have been pursued. Finally, a discussion of outstanding issues and questions regarding the character and nature of Mars' extratropical traveling weather systems is offered.

  8. Large-Scale Extratropical Weather Systems in Mars' Atmosphere

    NASA Technical Reports Server (NTRS)

    Hollingsworth, Jeffery L.

    2013-01-01

    During late autumn through early spring, extratropical regions on Mars exhibit profound mean zonal equator-to-pole thermal contrasts. The imposition of this strong meridional temperature variation supports intense eastward-traveling, synoptic weather systems (i.e., transient baroclinic/barotropic waves) within Mars' extratropical atmosphere. Such disturbances grow, mature and decay within the east-west varying seasonal-mean midlatitude jet stream (i.e., the polar vortex) on the planet. Near the surface, the weather disturbances indicated large-scale spiraling "comma"-shaped dust cloud structures and scimitar-shaped dust fronts, indicative of processes associated with cyclo-/fronto-genesis. The weather systems occur during specific seasons on Mars, and in both hemispheres. The northern hemisphere (NH) disturbances are significantly more intense than their counterparts in the southern hemisphere (SH). Further, the NH weather systems and accompanying frontal waves appear to have significant impacts on the transport of tracer fields (e.g., particularly dust and to some extent water species (vapor/ice) as well). And regarding dust, frontal waves appear to be key agents in the lifting, lofting, organization and transport of this particular atmospheric aerosol. In this paper, a brief background and supporting observations of Mars' extratropical weather systems is presented. This is followed by a short review of the theory and various modeling studies (i.e., ranging from highly simplified, mechanistic and full global circulation modeling investigations) which have been pursued. Finally, a discussion of outstanding issues and questions regarding the character and nature of Mars' extratropical traveling weather systems is offered.

  9. Evaluation of Software Simulation of Road Weather Information System.

    DOT National Transportation Integrated Search

    2016-09-01

    A road weather information system (RWIS) is a combination of technologies that collects, transmits, models, and disseminates weather and road condition information. Sensors measure a range of weatherrelated conditions, including pavement temperatur...

  10. Numerical weather prediction model tuning via ensemble prediction system

    NASA Astrophysics Data System (ADS)

    Jarvinen, H.; Laine, M.; Ollinaho, P.; Solonen, A.; Haario, H.

    2011-12-01

    This paper discusses a novel approach to tune predictive skill of numerical weather prediction (NWP) models. NWP models contain tunable parameters which appear in parameterizations schemes of sub-grid scale physical processes. Currently, numerical values of these parameters are specified manually. In a recent dual manuscript (QJRMS, revised) we developed a new concept and method for on-line estimation of the NWP model parameters. The EPPES ("Ensemble prediction and parameter estimation system") method requires only minimal changes to the existing operational ensemble prediction infra-structure and it seems very cost-effective because practically no new computations are introduced. The approach provides an algorithmic decision making tool for model parameter optimization in operational NWP. In EPPES, statistical inference about the NWP model tunable parameters is made by (i) generating each member of the ensemble of predictions using different model parameter values, drawn from a proposal distribution, and (ii) feeding-back the relative merits of the parameter values to the proposal distribution, based on evaluation of a suitable likelihood function against verifying observations. In the presentation, the method is first illustrated in low-order numerical tests using a stochastic version of the Lorenz-95 model which effectively emulates the principal features of ensemble prediction systems. The EPPES method correctly detects the unknown and wrongly specified parameters values, and leads to an improved forecast skill. Second, results with an atmospheric general circulation model based ensemble prediction system show that the NWP model tuning capacity of EPPES scales up to realistic models and ensemble prediction systems. Finally, a global top-end NWP model tuning exercise with preliminary results is published.

  11. Climate, weather, space weather: model development in an operational context

    NASA Astrophysics Data System (ADS)

    Folini, Doris

    2018-05-01

    Aspects of operational modeling for climate, weather, and space weather forecasts are contrasted, with a particular focus on the somewhat conflicting demands of "operational stability" versus "dynamic development" of the involved models. Some common key elements are identified, indicating potential for fruitful exchange across communities. Operational model development is compelling, driven by factors that broadly fall into four categories: model skill, basic physics, advances in computer architecture, and new aspects to be covered, from costumer needs over physics to observational data. Evaluation of model skill as part of the operational chain goes beyond an automated skill score. Permanent interaction between "pure research" and "operational forecast" people is beneficial to both sides. This includes joint model development projects, although ultimate responsibility for the operational code remains with the forecast provider. The pace of model development reflects operational lead times. The points are illustrated with selected examples, many of which reflect the author's background and personal contacts, notably with the Swiss Weather Service and the Max Planck Institute for Meteorology, Hamburg, Germany. In view of current and future challenges, large collaborations covering a range of expertise are a must - within and across climate, weather, and space weather. To profit from and cope with the rapid progress of computer architectures, supercompute centers must form part of the team.

  12. Creating Weather System Ensembles Through Synergistic Process Modeling and Machine Learning

    NASA Astrophysics Data System (ADS)

    Chen, B.; Posselt, D. J.; Nguyen, H.; Wu, L.; Su, H.; Braverman, A. J.

    2017-12-01

    Earth's weather and climate are sensitive to a variety of control factors (e.g., initial state, forcing functions, etc). Characterizing the response of the atmosphere to a change in initial conditions or model forcing is critical for weather forecasting (ensemble prediction) and climate change assessment. Input - response relationships can be quantified by generating an ensemble of multiple (100s to 1000s) realistic realizations of weather and climate states. Atmospheric numerical models generate simulated data through discretized numerical approximation of the partial differential equations (PDEs) governing the underlying physics. However, the computational expense of running high resolution atmospheric state models makes generation of more than a few simulations infeasible. Here, we discuss an experiment wherein we approximate the numerical PDE solver within the Weather Research and Forecasting (WRF) Model using neural networks trained on a subset of model run outputs. Once trained, these neural nets can produce large number of realization of weather states from a small number of deterministic simulations with speeds that are orders of magnitude faster than the underlying PDE solver. Our neural network architecture is inspired by the governing partial differential equations. These equations are location-invariant, and consist of first and second derivations. As such, we use a 3x3 lon-lat grid of atmospheric profiles as the predictor in the neural net to provide the network the information necessary to compute the first and second moments. Results indicate that the neural network algorithm can approximate the PDE outputs with high degree of accuracy (less than 1% error), and that this error increases as a function of the prediction time lag.

  13. Employing Numerical Weather Models to Enhance Fire Weather and Fire Behavior Predictions

    Treesearch

    Joseph J. Charney; Lesley A. Fusina

    2006-01-01

    This paper presents an assessment of fire weather and fire behavior predictions produced by a numerical weather prediction model similar to those used by operational weather forecasters when preparing their forecasts. The PSU/NCAR MM5 model is used to simulate the weather conditions associated with three fire episodes in June 2005. Extreme fire behavior was reported...

  14. Large-Scale, Synoptic-Period Weather Systems in Mars' Atmosphere

    NASA Astrophysics Data System (ADS)

    Hollingsworth, Jeffery L.; Kahre, M.

    2013-10-01

    During late autumn through early spring, extratropical regions on Mars exhibit profound mean zonal equator-to-pole thermal contrasts associated with its waxing and waning seasonal polar ice caps. The imposition of this strong meridional temperature gradient supports intense eastward-traveling, synoptic-period weather systems (i.e., transient baroclinic/barotropic waves) within Mars' extratropical atmosphere. These disturbances grow, mature and decay within the east-west varying seasonal-mean middle and high-latitude westerly jet stream (i.e., the polar vortex) on the planet. Near the surface, such weather disturbances indicated distinctive, spiraling "comma"-shaped dust cloud structures of large scale, and scimitar-shaped dust fronts, indicative of processes associated with cyclo- and fronto-genesis. The weather systems are most intense during specific seasons on Mars, and in both hemispheres. The northern hemisphere (NH) disturbances appear to be significantly more vigorous than their counterparts in the southern hemisphere (SH). Further, the NH weather systems and accompanying frontal waves appear to have significant impacts on the transport of tracer fields (e.g., particularly dust and to some extent water species (vapor/ice) as well). Regarding dust, frontal waves appear to be key agents in the lifting, lofting, organization and transport of this atmospheric aerosol. A brief background and supporting observations of Mars' extratropical weather systems is presented. This is followed by various modeling studies (i.e., ranging from highly simplified, mechanistic and fully complex global circulation modeling investigations) that we are pursuing. In particular, transport of scalar quantities (e.g., tracers and high-order dynamically revealing diagnostic fields) are investigated. A discussion of outstanding issues and future modeling pursuits is offered related to Mars' extratropical traveling weather systems.

  15. Space weather forecasting with a Multimodel Ensemble Prediction System (MEPS)

    NASA Astrophysics Data System (ADS)

    Schunk, R. W.; Scherliess, L.; Eccles, V.; Gardner, L. C.; Sojka, J. J.; Zhu, L.; Pi, X.; Mannucci, A. J.; Butala, M.; Wilson, B. D.; Komjathy, A.; Wang, C.; Rosen, G.

    2016-07-01

    The goal of the Multimodel Ensemble Prediction System (MEPS) program is to improve space weather specification and forecasting with ensemble modeling. Space weather can have detrimental effects on a variety of civilian and military systems and operations, and many of the applications pertain to the ionosphere and upper atmosphere. Space weather can affect over-the-horizon radars, HF communications, surveying and navigation systems, surveillance, spacecraft charging, power grids, pipelines, and the Federal Aviation Administration (FAA's) Wide Area Augmentation System (WAAS). Because of its importance, numerous space weather forecasting approaches are being pursued, including those involving empirical, physics-based, and data assimilation models. Clearly, if there are sufficient data, the data assimilation modeling approach is expected to be the most reliable, but different data assimilation models can produce different results. Therefore, like the meteorology community, we created a Multimodel Ensemble Prediction System (MEPS) for the Ionosphere-Thermosphere-Electrodynamics (ITE) system that is based on different data assimilation models. The MEPS ensemble is composed of seven physics-based data assimilation models for the ionosphere, ionosphere-plasmasphere, thermosphere, high-latitude ionosphere-electrodynamics, and middle to low latitude ionosphere-electrodynamics. Hence, multiple data assimilation models can be used to describe each region. A selected storm event that was reconstructed with four different data assimilation models covering the middle and low latitude ionosphere is presented and discussed. In addition, the effect of different data types on the reconstructions is shown.

  16. WRF-Fire: coupled weather-wildland fire modeling with the weather research and forecasting model

    Treesearch

    Janice L. Coen; Marques Cameron; John Michalakes; Edward G. Patton; Philip J. Riggan; Kara M. Yedinak

    2012-01-01

    A wildland fire behavior module (WRF-Fire) was integrated into the Weather Research and Forecasting (WRF) public domain numerical weather prediction model. The fire module is a surface fire behavior model that is two-way coupled with the atmospheric model. Near-surface winds from the atmospheric model are interpolated to a finer fire grid and used, with fuel properties...

  17. The Future of Planetary Climate Modeling and Weather Prediction

    NASA Technical Reports Server (NTRS)

    Del Genio, A. D.; Domagal-Goldman, S. D.; Kiang, N. Y.; Kopparapu, R. K.; Schmidt, G. A.; Sohl, L. E.

    2017-01-01

    Modeling of planetary climate and weather has followed the development of tools for studying Earth, with lags of a few years. Early Earth climate studies were performed with 1-dimensionalradiative-convective models, which were soon fol-lowed by similar models for the climates of Mars and Venus and eventually by similar models for exoplan-ets. 3-dimensional general circulation models (GCMs) became common in Earth science soon after and within several years were applied to the meteorology of Mars, but it was several decades before a GCM was used to simulate extrasolar planets. Recent trends in Earth weather and and climate modeling serve as a useful guide to how modeling of Solar System and exoplanet weather and climate will evolve in the coming decade.

  18. Enhanced Weather Radar (EWxR) System

    NASA Technical Reports Server (NTRS)

    Kronfeld, Kevin M. (Technical Monitor)

    2003-01-01

    An airborne weather radar system, the Enhanced Weather Radar (EWxR), with enhanced on-board weather radar data processing was developed and tested. The system features additional weather data that is uplinked from ground-based sources, specialized data processing, and limited automatic radar control to search for hazardous weather. National Weather Service (NWS) ground-based Next Generation Radar (NEXRAD) information is used by the EWxR system to augment the on-board weather radar information. The system will simultaneously display NEXRAD and on-board weather radar information in a split-view format. The on-board weather radar includes an automated or hands-free storm-finding feature that optimizes the radar returns by automatically adjusting the tilt and range settings for the current altitude above the terrain and searches for storm cells near the atmospheric 0-degree isotherm. A rule-based decision aid was developed to automatically characterize cells as hazardous, possibly-hazardous, or non-hazardous based upon attributes of that cell. Cell attributes are determined based on data from the on-board radar and from ground-based radars. A flight path impact prediction algorithm was developed to help pilots to avoid hazardous weather along their flight plan and their mission. During development the system was tested on the NASA B757 aircraft and final tests were conducted on the Rockwell Collins Sabreliner.

  19. Models and applications for space weather forecasting and analysis at the Community Coordinated Modeling Center.

    NASA Astrophysics Data System (ADS)

    Kuznetsova, Maria

    The Community Coordinated Modeling Center (CCMC, http://ccmc.gsfc.nasa.gov) was established at the dawn of the new millennium as a long-term flexible solution to the problem of transition of progress in space environment modeling to operational space weather forecasting. CCMC hosts an expanding collection of state-of-the-art space weather models developed by the international space science community. Over the years the CCMC acquired the unique experience in preparing complex models and model chains for operational environment and developing and maintaining custom displays and powerful web-based systems and tools ready to be used by researchers, space weather service providers and decision makers. In support of space weather needs of NASA users CCMC is developing highly-tailored applications and services that target specific orbits or locations in space and partnering with NASA mission specialists on linking CCMC space environment modeling with impacts on biological and technological systems in space. Confidence assessment of model predictions is an essential element of space environment modeling. CCMC facilitates interaction between model owners and users in defining physical parameters and metrics formats relevant to specific applications and leads community efforts to quantify models ability to simulate and predict space environment events. Interactive on-line model validation systems developed at CCMC make validation a seamless part of model development circle. The talk will showcase innovative solutions for space weather research, validation, anomaly analysis and forecasting and review on-going community-wide model validation initiatives enabled by CCMC applications.

  20. Pilot's Automated Weather Support System (PAWSS) concepts demonstration project. Phase 1: Pilot's weather information requirements and implications for weather data systems design

    NASA Technical Reports Server (NTRS)

    Crabill, Norman L.; Dash, Ernie R.

    1991-01-01

    The weather information requirements for pilots and the deficiencies of the current aviation weather support system in meeting these requirements are defined. As the amount of data available to pilots increases significantly in the near future, expert system technology will be needed to assist pilots in assimilating that information. Some other desirable characteristics of an automation-assisted system for weather data acquisition, dissemination, and assimilation are also described.

  1. Adaptive Numerical Algorithms in Space Weather Modeling

    NASA Technical Reports Server (NTRS)

    Toth, Gabor; vanderHolst, Bart; Sokolov, Igor V.; DeZeeuw, Darren; Gombosi, Tamas I.; Fang, Fang; Manchester, Ward B.; Meng, Xing; Nakib, Dalal; Powell, Kenneth G.; hide

    2010-01-01

    Space weather describes the various processes in the Sun-Earth system that present danger to human health and technology. The goal of space weather forecasting is to provide an opportunity to mitigate these negative effects. Physics-based space weather modeling is characterized by disparate temporal and spatial scales as well as by different physics in different domains. A multi-physics system can be modeled by a software framework comprising of several components. Each component corresponds to a physics domain, and each component is represented by one or more numerical models. The publicly available Space Weather Modeling Framework (SWMF) can execute and couple together several components distributed over a parallel machine in a flexible and efficient manner. The framework also allows resolving disparate spatial and temporal scales with independent spatial and temporal discretizations in the various models. Several of the computationally most expensive domains of the framework are modeled by the Block-Adaptive Tree Solar wind Roe Upwind Scheme (BATS-R-US) code that can solve various forms of the magnetohydrodynamics (MHD) equations, including Hall, semi-relativistic, multi-species and multi-fluid MHD, anisotropic pressure, radiative transport and heat conduction. Modeling disparate scales within BATS-R-US is achieved by a block-adaptive mesh both in Cartesian and generalized coordinates. Most recently we have created a new core for BATS-R-US: the Block-Adaptive Tree Library (BATL) that provides a general toolkit for creating, load balancing and message passing in a 1, 2 or 3 dimensional block-adaptive grid. We describe the algorithms of BATL and demonstrate its efficiency and scaling properties for various problems. BATS-R-US uses several time-integration schemes to address multiple time-scales: explicit time stepping with fixed or local time steps, partially steady-state evolution, point-implicit, semi-implicit, explicit/implicit, and fully implicit numerical

  2. Global Navigation Satellite Systems and Space Weather: Building upon the International Space Weather Initiative

    NASA Astrophysics Data System (ADS)

    Gadimova, S. H.; Haubold, H. J.

    2014-01-01

    Globally there is growing interest in better unders tanding solar-terrestrial interactions, particularly patterns and trends in space weather. This is not only for scientific reasons, but also because the reliable operation of ground-based and space-based assets and infrastructures is increasingly dependent on their robustness against the detrimental effects of space weather. Consequently, in 2009, the United Nations Committee on the Peaceful Uses of Outer Space (COPUOS) proposed the International Space Weather Initiative (ISWI), as a follow-up activity to the International Heliophysical Year 2007 (IHY2007), to be implemented under a three-year workplan from 2010 to 2012 (UNGA Document, A/64/20). All achievements of international cooperation and coordination for ISWI, including instrumentation, data analysis, modelling, education, training and public outreach, are made a vailable through the ISWI Newsletter and the ISWI Website (http://www.iswi-secretariat.org/). Since the last solar maximum in 2000, societal dependence on global navigation satellite system (GNSS) has increased substantially. This situation has brought increasing attention to the subject of space weather and its effects on GNSS systems and users. Results concerning the impact of space weather on GNSS are made available at the Information Portal (www.unoosa.org) of the International Committee on Global Navigati on Satellite Systems (ICG). This paper briefly reviews the curre nt status of ISWI with regard to GNSS.

  3. Weather forecasting expert system study

    NASA Technical Reports Server (NTRS)

    1985-01-01

    Weather forecasting is critical to both the Space Transportation System (STS) ground operations and the launch/landing activities at NASA Kennedy Space Center (KSC). The current launch frequency places significant demands on the USAF weather forecasters at the Cape Canaveral Forecasting Facility (CCFF), who currently provide the weather forecasting for all STS operations. As launch frequency increases, KSC's weather forecasting problems will be great magnified. The single most important problem is the shortage of highly skilled forecasting personnel. The development of forecasting expertise is difficult and requires several years of experience. Frequent personnel changes within the forecasting staff jeopardize the accumulation and retention of experience-based weather forecasting expertise. The primary purpose of this project was to assess the feasibility of using Artificial Intelligence (AI) techniques to ameliorate this shortage of experts by capturing aria incorporating the forecasting knowledge of current expert forecasters into a Weather Forecasting Expert System (WFES) which would then be made available to less experienced duty forecasters.

  4. New Space Weather Systems Under Development and Their Contribution to Space Weather Management

    NASA Astrophysics Data System (ADS)

    Tobiska, W.; Bouwer, D.; Schunk, R.; Garrett, H.; Mertens, C.; Bowman, B.

    2008-12-01

    There have been notable successes during the past decade in the development of operational space environment systems. Examples include the Magnetospheric Specification Model (MSM) of the Earth's magnetosphere, 2000; SOLAR2000 (S2K) solar spectral irradiances, 2001; High Accuracy Satellite Drag Model (HASDM) neutral atmosphere densities, 2004; Global Assimilation of Ionospheric Measurements (GAIM) ionosphere specification, 2006; Hakamada-Akasofu-Fry (HAF) solar wind parameters, 2007; Communication Alert and Prediction System (CAPS) ionosphere, high frequency radio, and scintillation S4 index prediction, 2008; and GEO Alert and Prediction System (GAPS) geosynchronous environment satellite charging specification and forecast, 2008. Operational systems that are in active operational implementation include the Jacchia-Bowman 2006/2008 (JB2006/2008) neutral atmosphere, 2009, and the Nowcast of Atmospheric Ionizing Radiation for Aviation Safety (NAIRAS) aviation radiation model using the Radiation Alert and Prediction System (RAPS), 2010. U.S. national agency and commercial assets will soon reach a state where specification and prediction will become ubiquitous and where coordinated management of the space environment and space weather will become a necessity. We describe the status of the CAPS, GAPS, RAPS, and JB2008 operational development. We additionally discuss the conditions that are laying the groundwork for space weather management and estimate the unfilled needs as we move beyond specification and prediction efforts.

  5. Community Coordinated Modeling Center: Addressing Needs of Operational Space Weather Forecasting

    NASA Technical Reports Server (NTRS)

    Kuznetsova, M.; Maddox, M.; Pulkkinen, A.; Hesse, M.; Rastaetter, L.; Macneice, P.; Taktakishvili, A.; Berrios, D.; Chulaki, A.; Zheng, Y.; hide

    2012-01-01

    Models are key elements of space weather forecasting. The Community Coordinated Modeling Center (CCMC, http://ccmc.gsfc.nasa.gov) hosts a broad range of state-of-the-art space weather models and enables access to complex models through an unmatched automated web-based runs-on-request system. Model output comparisons with observational data carried out by a large number of CCMC users open an unprecedented mechanism for extensive model testing and broad community feedback on model performance. The CCMC also evaluates model's prediction ability as an unbiased broker and supports operational model selections. The CCMC is organizing and leading a series of community-wide projects aiming to evaluate the current state of space weather modeling, to address challenges of model-data comparisons, and to define metrics for various user s needs and requirements. Many of CCMC models are continuously running in real-time. Over the years the CCMC acquired the unique experience in developing and maintaining real-time systems. CCMC staff expertise and trusted relations with model owners enable to keep up to date with rapid advances in model development. The information gleaned from the real-time calculations is tailored to specific mission needs. Model forecasts combined with data streams from NASA and other missions are integrated into an innovative configurable data analysis and dissemination system (http://iswa.gsfc.nasa.gov) that is accessible world-wide. The talk will review the latest progress and discuss opportunities for addressing operational space weather needs in innovative and collaborative ways.

  6. Modeling extreme (Carrington-type) space weather events using three-dimensional MHD code simulations

    NASA Astrophysics Data System (ADS)

    Ngwira, C. M.; Pulkkinen, A. A.; Kuznetsova, M. M.; Glocer, A.

    2013-12-01

    There is growing concern over possible severe societal consequences related to adverse space weather impacts on man-made technological infrastructure and systems. In the last two decades, significant progress has been made towards the modeling of space weather events. Three-dimensional (3-D) global magnetohydrodynamics (MHD) models have been at the forefront of this transition, and have played a critical role in advancing our understanding of space weather. However, the modeling of extreme space weather events is still a major challenge even for existing global MHD models. In this study, we introduce a specially adapted University of Michigan 3-D global MHD model for simulating extreme space weather events that have a ground footprint comparable (or larger) to the Carrington superstorm. Results are presented for an initial simulation run with ``very extreme'' constructed/idealized solar wind boundary conditions driving the magnetosphere. In particular, we describe the reaction of the magnetosphere-ionosphere system and the associated ground induced geoelectric field to such extreme driving conditions. We also discuss the results and what they might mean for the accuracy of the simulations. The model is further tested using input data for an observed space weather event to verify the MHD model consistence and to draw guidance for future work. This extreme space weather MHD model is designed specifically for practical application to the modeling of extreme geomagnetically induced electric fields, which can drive large currents in earth conductors such as power transmission grids.

  7. Weather Augmented Risk Determination (WARD) System

    NASA Astrophysics Data System (ADS)

    Niknejad, M.; Mazdiyasni, O.; Momtaz, F.; AghaKouchak, A.

    2017-12-01

    Extreme climatic events have direct and indirect impacts on society, economy and the environment. Based on the United States Bureau of Economic Analysis (BEA) data, over one third of the U.S. GDP can be considered as weather-sensitive involving some degree of weather risk. This expands from a local scale concrete foundation construction to large scale transportation systems. Extreme and unexpected weather conditions have always been considered as one of the probable risks to human health, productivity and activities. The construction industry is a large sector of the economy, and is also greatly influenced by weather-related risks including work stoppage and low labor productivity. Identification and quantification of these risks, and providing mitigation of their effects are always the concerns of construction project managers. In addition to severe weather conditions' destructive effects, seasonal changes in weather conditions can also have negative impacts on human health. Work stoppage and reduced labor productivity can be caused by precipitation, wind, temperature, relative humidity and other weather conditions. Historical and project-specific weather information can improve better project management and mitigation planning, and ultimately reduce the risk of weather-related conditions. This paper proposes new software for project-specific user-defined data analysis that offers (a) probability of work stoppage and the estimated project length considering weather conditions; (b) information on reduced labor productivity and its impacts on project duration; and (c) probabilistic information on the project timeline based on both weather-related work stoppage and labor productivity. The software (WARD System) is designed such that it can be integrated into the already available project management tools. While the system and presented application focuses on the construction industry, the developed software is general and can be used for any application that involves

  8. The Impact of Different Complexity on Numerical Weather Predictions within the Coupled Global Online Modeling System

    NASA Astrophysics Data System (ADS)

    Zhang, L.; Grell, G. A.; McKeen, S. A.; Ahmadov, R.

    2017-12-01

    The global Flow-following finite-volume Icosahedra Model (FIM), which was developed in the Global Systems Division of NOAA/ESRL and the Finite-volume cubed-sphere dynamical core (FV3) developed by GFDL, have been coupled online with aerosol and gas-phase chemistry schemes (FIM-Chem and FV3-Chem). Within the aerosol and chemistry modules, the models handle wet and dry deposition, chemical reactions, aerosol direct and semi-direct effect, anthropogenic emissions, biogenic emissions, biomass burning, dust and sea-salt emissions. They are able to provide chemical weather predictions at various spatial resolutions and with different levels of complexity. FIM-Chem is also able to quantify the impact of aerosol on numerical weather predictions (NWP). Currently, three different chemical schemes have been coupled with the FIM model. The simplest aerosol modules are from the GOCART model with its simplified parameterization of sulfur/sulfate chemistry. The photochemical gas-phase mechanism RACM was included to determine the impact of additional complexity on the aerosol and gas simulations. We have also implemented a more sophisticated aerosol scheme that includes secondary organic aerosols (SOA) based on the VBS approach. The model performance has been evaluated by comparing with the ATom-1 observations. FIM-Chem is able to reproduce many observed aerosol and gas features very well. A five-day NWP on 120 km horizontal resolution using FIM-Chem has been done for the end of July, 2016 to quantify the impact of the three different chemical schemes on weather forecasts. Compared to a meteorological run that excludes the model chemical schemes, and is driven only by background AODs from the GFS model, the 5-day forecast results shows significant impact on weather predictions when including the prognostic aerosol schemes. This includes convective precipitation, surface temperature, and 700 hPa air temperature. We also use FIM-Chem to investigate the 2012 South American Biomass

  9. Toward a Concept of Operations for Aviation Weather Information Implementation in the Evolving National Airspace System

    NASA Technical Reports Server (NTRS)

    McAdaragh, Raymon M.

    2002-01-01

    The capacity of the National Airspace System is being stressed due to the limits of current technologies. Because of this, the FAA and NASA are working to develop new technologies to increase the system's capacity which enhancing safety. Adverse weather has been determined to be a major factor in aircraft accidents and fatalities and the FAA and NASA have developed programs to improve aviation weather information technologies and communications for system users The Aviation Weather Information Element of the Weather Accident Prevention Project of NASA's Aviation Safety Program is currently working to develop these technologies in coordination with the FAA and industry. This paper sets forth a theoretical approach to implement these new technologies while addressing the National Airspace System (NAS) as an evolving system with Weather Information as one of its subSystems. With this approach in place, system users will be able to acquire the type of weather information that is needed based upon the type of decision-making situation and condition that is encountered. The theoretical approach addressed in this paper takes the form of a model for weather information implementation. This model addresses the use of weather information in three decision-making situations, based upon the system user's operational perspective. The model also addresses two decision-making conditions, which are based upon the need for collaboration due to the level of support offered by the weather information provided by each new product or technology. The model is proposed for use in weather information implementation in order to provide a systems approach to the NAS. Enhancements to the NAS collaborative decision-making capabilities are also suggested.

  10. Investigation and Modeling of Cranberry Weather Stress.

    NASA Astrophysics Data System (ADS)

    Croft, Paul Joseph

    Cranberry bog weather conditions and weather-related stress were investigated for development of crop yield prediction models and models to predict daily weather conditions in the bog. Field investigations and data gathering were completed at the Rutgers University Blueberry/Cranberry Research Center experimental bogs in Chatsworth, New Jersey. Study indicated that although cranberries generally exhibit little or no stomatal response to changing atmospheric conditions, the evaluation of weather-related stress could be accomplished via use of micrometeorological data. Definition of weather -related stress was made by establishing critical thresholds of the frequencies of occurrence, and magnitudes of, temperature and precipitation in the bog based on values determined by a review of the literature and a grower questionnaire. Stress frequencies were correlated with cranberry yield to develop predictive models based on the previous season's yield, prior season data, prior and current season data, current season data; and prior and current season data through July 31 of the current season. The predictive ability of the prior season models was best and could be used in crop planning and production. Further examination of bog micrometeorological data permitted the isolation of those weather conditions conducive to cranberry scald and allowed for the institution of a pilot scald advisory program during the 1991 season. The micrometeorological data from the bog was also used to develop models to predict daily canopy temperature and precipitation, based on upper air data, for grower use. Models were developed for each month for maximum and minimum temperatures and for precipitation and generally performed well. The modeling of bog weather conditions is an important first step toward daily prediction of cranberry weather-related stress.

  11. Analysis of errors introduced by geographic coordinate systems on weather numeric prediction modeling

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

    Cao, Yanni; Cervone, Guido; Barkley, Zachary

    Most atmospheric models, including the Weather Research and Forecasting (WRF) model, use a spherical geographic coordinate system to internally represent input data and perform computations. However, most geographic information system (GIS) input data used by the models are based on a spheroid datum because it better represents the actual geometry of the earth. WRF and other atmospheric models use these GIS input layers as if they were in a spherical coordinate system without accounting for the difference in datum. When GIS layers are not properly reprojected, latitudinal errors of up to 21 km in the midlatitudes are introduced. Recent studiesmore » have suggested that for very high-resolution applications, the difference in datum in the GIS input data (e.g., terrain land use, orography) should be taken into account. However, the magnitude of errors introduced by the difference in coordinate systems remains unclear. This research quantifies the effect of using a spherical vs. a spheroid datum for the input GIS layers used by WRF to study greenhouse gas transport and dispersion in northeast Pennsylvania.« less

  12. Analysis of errors introduced by geographic coordinate systems on weather numeric prediction modeling

    DOE PAGES

    Cao, Yanni; Cervone, Guido; Barkley, Zachary; ...

    2017-09-19

    Most atmospheric models, including the Weather Research and Forecasting (WRF) model, use a spherical geographic coordinate system to internally represent input data and perform computations. However, most geographic information system (GIS) input data used by the models are based on a spheroid datum because it better represents the actual geometry of the earth. WRF and other atmospheric models use these GIS input layers as if they were in a spherical coordinate system without accounting for the difference in datum. When GIS layers are not properly reprojected, latitudinal errors of up to 21 km in the midlatitudes are introduced. Recent studiesmore » have suggested that for very high-resolution applications, the difference in datum in the GIS input data (e.g., terrain land use, orography) should be taken into account. However, the magnitude of errors introduced by the difference in coordinate systems remains unclear. This research quantifies the effect of using a spherical vs. a spheroid datum for the input GIS layers used by WRF to study greenhouse gas transport and dispersion in northeast Pennsylvania.« less

  13. Analysis of errors introduced by geographic coordinate systems on weather numeric prediction modeling

    NASA Astrophysics Data System (ADS)

    Cao, Yanni; Cervone, Guido; Barkley, Zachary; Lauvaux, Thomas; Deng, Aijun; Taylor, Alan

    2017-09-01

    Most atmospheric models, including the Weather Research and Forecasting (WRF) model, use a spherical geographic coordinate system to internally represent input data and perform computations. However, most geographic information system (GIS) input data used by the models are based on a spheroid datum because it better represents the actual geometry of the earth. WRF and other atmospheric models use these GIS input layers as if they were in a spherical coordinate system without accounting for the difference in datum. When GIS layers are not properly reprojected, latitudinal errors of up to 21 km in the midlatitudes are introduced. Recent studies have suggested that for very high-resolution applications, the difference in datum in the GIS input data (e.g., terrain land use, orography) should be taken into account. However, the magnitude of errors introduced by the difference in coordinate systems remains unclear. This research quantifies the effect of using a spherical vs. a spheroid datum for the input GIS layers used by WRF to study greenhouse gas transport and dispersion in northeast Pennsylvania.

  14. Improving aerosol interaction with clouds and precipitation in a regional chemical weather modeling system

    NASA Astrophysics Data System (ADS)

    Zhou, C.; Zhang, X.; Gong, S.; Wang, Y.; Xue, M.

    2016-01-01

    A comprehensive aerosol-cloud-precipitation interaction (ACI) scheme has been developed under a China Meteorological Administration (CMA) chemical weather modeling system, GRAPES/CUACE (Global/Regional Assimilation and PrEdiction System, CMA Unified Atmospheric Chemistry Environment). Calculated by a sectional aerosol activation scheme based on the information of size and mass from CUACE and the thermal-dynamic and humid states from the weather model GRAPES at each time step, the cloud condensation nuclei (CCN) are interactively fed online into a two-moment cloud scheme (WRF Double-Moment 6-class scheme - WDM6) and a convective parameterization to drive cloud physics and precipitation formation processes. The modeling system has been applied to study the ACI for January 2013 when several persistent haze-fog events and eight precipitation events occurred.

    The results show that aerosols that interact with the WDM6 in GRAPES/CUACE obviously increase the total cloud water, liquid water content, and cloud droplet number concentrations, while decreasing the mean diameters of cloud droplets with varying magnitudes of the changes in each case and region. These interactive microphysical properties of clouds improve the calculation of their collection growth rates in some regions and hence the precipitation rate and distributions in the model, showing 24 to 48 % enhancements of threat score for 6 h precipitation in almost all regions. The aerosols that interact with the WDM6 also reduce the regional mean bias of temperature by 3 °C during certain precipitation events, but the monthly means bias is only reduced by about 0.3 °C.

  15. Traffic analysis toolbox volume XI : weather and traffic analysis, modeling and simulation.

    DOT National Transportation Integrated Search

    2010-12-01

    This document presents a weather module for the traffic analysis tools program. It provides traffic engineers, transportation modelers and decisions makers with a guide that can incorporate weather impacts into transportation system analysis and mode...

  16. Modelling Wind Turbine Failures based on Weather Conditions

    NASA Astrophysics Data System (ADS)

    Reder, Maik; Melero, Julio J.

    2017-11-01

    A large proportion of the overall costs of a wind farm is directly related to operation and maintenance (O&M) tasks. By applying predictive O&M strategies rather than corrective approaches these costs can be decreased significantly. Here, especially wind turbine (WT) failure models can help to understand the components’ degradation processes and enable the operators to anticipate upcoming failures. Usually, these models are based on the age of the systems or components. However, latest research shows that the on-site weather conditions also affect the turbine failure behaviour significantly. This study presents a novel approach to model WT failures based on the environmental conditions to which they are exposed to. The results focus on general WT failures, as well as on four main components: gearbox, generator, pitch and yaw system. A penalised likelihood estimation is used in order to avoid problems due to for example highly correlated input covariates. The relative importance of the model covariates is assessed in order to analyse the effect of each weather parameter on the model output.

  17. Space Weather Modeling at the Community Coordinated Modeling Center

    NASA Astrophysics Data System (ADS)

    Hesse, M.; Falasca, A.; Johnson, J.; Keller, K.; Kuznetsova, M.; Rastaetter, L.

    2003-04-01

    The Community Coordinated Modeling Center (CCMC) is a multi-agency partnership aimed at the creation of next generation space weather models. The goal of the CCMC is to support the research and developmental work necessary to substantially increase the present-day modeling capability for space weather purposes, and to provide models for transition to the rapid prototyping centers at the space weather forecast centers. This goal requires close collaborations with and substantial involvement of the research community. The physical regions to be addressed by CCMC-related activities range from the solar atmosphere to the Earth's upper atmosphere. The CCMC is an integral part of NASA's Living With a Star (LWS) initiative, of the National Space Weather Program Implementation Plan, and of the Department of Defense Space Weather Transition Plan. CCMC includes a facility at NASA Goddard Space Flight Center, as well as distributed computing facilities provided by the US Air Force. CCMC also provides, to the research community, access to state-of-the-art space research models. In this paper we will provide updates on CCMC status, on current plans, research and development accomplishments and goals, and on the model testing and validation process undertaken as part of the CCMC mandate. We will demonstrate the capabilities of models resident at CCMC via the analysis of a geomagnetic storm, driven by a shock in the solar wind.

  18. Space Weather Modeling at the Community Coordinated Modeling Center

    NASA Technical Reports Server (NTRS)

    Hesse M.

    2005-01-01

    The Community Coordinated Modeling Center (CCMC) is a multi-agency partnership, which aims at the creation of next generation space weather models. The goal of the CCMC is to support the research and developmental work necessary to substantially increase the present-day modeling capability for space weather purposes, and to provide models for transition to the rapid prototyping centers at the space weather forecast centers. This goal requires dose collaborations with and substantial involvement of the research community. The physical regions to be addressed by CCMC-related activities range from the solar atmosphere to the Earth's upper atmosphere. The CCMC is an integral part of the National Space Weather Program Implementation Plan, of NASA's Living With a Star (LWS) initiative, and of the Department of Defense Space Weather Transition Plan. CCMC includes a facility at NASA Goddard Space Flight Center, as well as distributed computing facilities provided by the US Air Force. CCMC also provides, to the research community, access to state-of-the-art space research models. In this paper we will provide updates on CCMC status, on current plans, research and development accomplishments and goals, and on the model testing and validation process undertaken as part of the CCMC mandate. Special emphasis will be on solar and heliospheric models currently residing at CCMC, and on plans for validation and verification.

  19. Weather Forecasting Systems and Methods

    NASA Technical Reports Server (NTRS)

    Mecikalski, John (Inventor); MacKenzie, Wayne M., Jr. (Inventor); Walker, John Robert (Inventor)

    2014-01-01

    A weather forecasting system has weather forecasting logic that receives raw image data from a satellite. The raw image data has values indicative of light and radiance data from the Earth as measured by the satellite, and the weather forecasting logic processes such data to identify cumulus clouds within the satellite images. For each identified cumulus cloud, the weather forecasting logic applies interest field tests to determine a score indicating the likelihood of the cumulus cloud forming precipitation and/or lightning in the future within a certain time period. Based on such scores, the weather forecasting logic predicts in which geographic regions the identified cumulus clouds will produce precipitation and/or lighting within during the time period. Such predictions may then be used to provide a weather map thereby providing users with a graphical illustration of the areas predicted to be affected by precipitation within the time period.

  20. Space Weather Products at the Community Coordinated Modeling Center

    NASA Technical Reports Server (NTRS)

    Hesse, Michael; Kuznetsova, M.; Pulkkinen, A.; Maddox, M.; Rastaetter, L.; Berrios, D.; MacNeice, P.

    2010-01-01

    The Community Coordinated Modeling Center (CCMC) is a US inter-agency activity aiming at research in support of the generation of advanced space weather models. As one of its main functions, the CCMC provides to researchers the use of space science models, even if they are not model owners themselves. The second CCMC activity is to support Space Weather forecasting at national Space Weather Forecasting Centers. This second activity involves model evaluations, model transitions to operations, and the development of space weather forecasting tools. Owing to the pace of development in the science community, new model capabilities emerge frequently. Consequently, space weather products and tools involve not only increased validity, but often entirely new capabilities. This presentation will review the present state of space weather tools as well as point out emerging future capabilities.

  1. Improving aerosol interaction with clouds and precipitation in a regional chemical weather modeling system

    NASA Astrophysics Data System (ADS)

    Zhou, C.; Zhang, X.; Gong, S.

    2015-12-01

    A comprehensive aerosol-cloud-precipitation interaction (ACI) scheme has been developed under CMA chemical weather modeling system GRAPES/CUACE. Calculated by a sectional aerosol activation scheme based on the information of size and mass from CUACE and the thermal-dynamic and humid states from the weather model GRAPES at each time step, the cloud condensation nuclei (CCN) is fed online interactively into a two-moment cloud scheme (WDM6) and a convective parameterization to drive the cloud physics and precipitation formation processes. The modeling system has been applied to study the ACI for January 2013 when several persistent haze-fog events and eight precipitation events occurred. The results show that interactive aerosols with the WDM6 in GRAPES/CUACE obviously increase the total cloud water, liquid water content and cloud droplet number concentrations while decrease the mean diameter of cloud droplets with varying magnitudes of the changes in each case and region. These interactive micro-physical properties of clouds improve the calculation of their collection growth rates in some regions and hence the precipitation rate and distributions in the model, showing 24% to 48% enhancements of TS scoring for 6-h precipitation in almost all regions. The interactive aerosols with the WDM6 also reduce the regional mean bias of temperature by 3 °C during certain precipitation events, but the monthly means bias is only reduced by about 0.3°C.

  2. An approach to secure weather and climate models against hardware faults

    NASA Astrophysics Data System (ADS)

    Düben, Peter D.; Dawson, Andrew

    2017-03-01

    Enabling Earth System models to run efficiently on future supercomputers is a serious challenge for model development. Many publications study efficient parallelization to allow better scaling of performance on an increasing number of computing cores. However, one of the most alarming threats for weather and climate predictions on future high performance computing architectures is widely ignored: the presence of hardware faults that will frequently hit large applications as we approach exascale supercomputing. Changes in the structure of weather and climate models that would allow them to be resilient against hardware faults are hardly discussed in the model development community. In this paper, we present an approach to secure the dynamical core of weather and climate models against hardware faults using a backup system that stores coarse resolution copies of prognostic variables. Frequent checks of the model fields on the backup grid allow the detection of severe hardware faults, and prognostic variables that are changed by hardware faults on the model grid can be restored from the backup grid to continue model simulations with no significant delay. To justify the approach, we perform model simulations with a C-grid shallow water model in the presence of frequent hardware faults. As long as the backup system is used, simulations do not crash and a high level of model quality can be maintained. The overhead due to the backup system is reasonable and additional storage requirements are small. Runtime is increased by only 13 % for the shallow water model.

  3. An approach to secure weather and climate models against hardware faults

    NASA Astrophysics Data System (ADS)

    Düben, Peter; Dawson, Andrew

    2017-04-01

    Enabling Earth System models to run efficiently on future supercomputers is a serious challenge for model development. Many publications study efficient parallelisation to allow better scaling of performance on an increasing number of computing cores. However, one of the most alarming threats for weather and climate predictions on future high performance computing architectures is widely ignored: the presence of hardware faults that will frequently hit large applications as we approach exascale supercomputing. Changes in the structure of weather and climate models that would allow them to be resilient against hardware faults are hardly discussed in the model development community. We present an approach to secure the dynamical core of weather and climate models against hardware faults using a backup system that stores coarse resolution copies of prognostic variables. Frequent checks of the model fields on the backup grid allow the detection of severe hardware faults, and prognostic variables that are changed by hardware faults on the model grid can be restored from the backup grid to continue model simulations with no significant delay. To justify the approach, we perform simulations with a C-grid shallow water model in the presence of frequent hardware faults. As long as the backup system is used, simulations do not crash and a high level of model quality can be maintained. The overhead due to the backup system is reasonable and additional storage requirements are small. Runtime is increased by only 13% for the shallow water model.

  4. An introduction to Space Weather Integrated Modeling

    NASA Astrophysics Data System (ADS)

    Zhong, D.; Feng, X.

    2012-12-01

    The need for a software toolkit that integrates space weather models and data is one of many challenges we are facing with when applying the models to space weather forecasting. To meet this challenge, we have developed Space Weather Integrated Modeling (SWIM) that is capable of analysis and visualizations of the results from a diverse set of space weather models. SWIM has a modular design and is written in Python, by using NumPy, matplotlib, and the Visualization ToolKit (VTK). SWIM provides data management module to read a variety of spacecraft data products and a specific data format of Solar-Interplanetary Conservation Element/Solution Element MHD model (SIP-CESE MHD model) for the study of solar-terrestrial phenomena. Data analysis, visualization and graphic user interface modules are also presented in a user-friendly way to run the integrated models and visualize the 2-D and 3-D data sets interactively. With these tools we can locally or remotely analysis the model result rapidly, such as extraction of data on specific location in time-sequence data sets, plotting interplanetary magnetic field lines, multi-slicing of solar wind speed, volume rendering of solar wind density, animation of time-sequence data sets, comparing between model result and observational data. To speed-up the analysis, an in-situ visualization interface is used to support visualizing the data 'on-the-fly'. We also modified some critical time-consuming analysis and visualization methods with the aid of GPU and multi-core CPU. We have used this tool to visualize the data of SIP-CESE MHD model in real time, and integrated the Database Model of shock arrival, Shock Propagation Model, Dst forecasting model and SIP-CESE MHD model developed by SIGMA Weather Group at State Key Laboratory of Space Weather/CAS.

  5. NOAA SWPC / NASA CCMC Space Weather Modeling Assessment Project: Toward the Validation of Advancements in Heliospheric Space Weather Prediction Within WSA-Enlil

    NASA Astrophysics Data System (ADS)

    Adamson, E. T.; Pizzo, V. J.; Biesecker, D. A.; Mays, M. L.; MacNeice, P. J.; Taktakishvili, A.; Viereck, R. A.

    2017-12-01

    In 2011, NOAA's Space Weather Prediction Center (SWPC) transitioned the world's first operational space weather model into use at the National Weather Service's Weather and Climate Operational Supercomputing System (WCOSS). This operational forecasting tool is comprised of the Wang-Sheeley-Arge (WSA) solar wind model coupled with the Enlil heliospheric MHD model. Relying on daily-updated photospheric magnetograms produced by the National Solar Observatory's Global Oscillation Network Group (GONG), this tool provides critical predictive knowledge of heliospheric dynamics such as high speed streams and coronal mass ejections. With the goal of advancing this predictive model and quantifying progress, SWPC and NASA's Community Coordinated Modeling Center (CCMC) have initiated a collaborative effort to assess improvements in space weather forecasts at Earth by moving from a single daily-updated magnetogram to a sequence of time-dependent magnetograms to drive the ambient inputs for the WSA-Enlil model as well as incorporating the newly developed Air Force Data Assimilative Photospheric Flux Transport (ADAPT) model. We will provide a detailed overview of the scope of this effort and discuss preliminary results from the first phase focusing on the impact of time-dependent magnetogram inputs to the WSA-Enlil model.

  6. Space Weather Models and Their Validation and Verification at the CCMC

    NASA Technical Reports Server (NTRS)

    Hesse, Michael

    2010-01-01

    The Community Coordinated l\\lodeling Center (CCMC) is a US multi-agency activity with a dual mission. With equal emphasis, CCMC strives to provide science support to the international space research community through the execution of advanced space plasma simulations, and it endeavors to support the space weather needs of the CS and partners. Space weather support involves a broad spectrum, from designing robust forecasting systems and transitioning them to forecasters, to providing space weather updates and forecasts to NASA's robotic mission operators. All of these activities have to rely on validation and verification of models and their products, so users and forecasters have the means to assign confidence levels to the space weather information. In this presentation, we provide an overview of space weather models resident at CCMC, as well as of validation and verification activities undertaken at CCMC or through the use of CCMC services.

  7. Evaluation of weather-based rice yield models in India.

    PubMed

    Sudharsan, D; Adinarayana, J; Reddy, D Raji; Sreenivas, G; Ninomiya, S; Hirafuji, M; Kiura, T; Tanaka, K; Desai, U B; Merchant, S N

    2013-01-01

    The objective of this study was to compare two different rice simulation models--standalone (Decision Support System for Agrotechnology Transfer [DSSAT]) and web based (SImulation Model for RIce-Weather relations [SIMRIW])--with agrometeorological data and agronomic parameters for estimation of rice crop production in southern semi-arid tropics of India. Studies were carried out on the BPT5204 rice variety to evaluate two crop simulation models. Long-term experiments were conducted in a research farm of Acharya N G Ranga Agricultural University (ANGRAU), Hyderabad, India. Initially, the results were obtained using 4 years (1994-1997) of data with weather parameters from a local weather station to evaluate DSSAT simulated results with observed values. Linear regression models used for the purpose showed a close relationship between DSSAT and observed yield. Subsequently, yield comparisons were also carried out with SIMRIW and DSSAT, and validated with actual observed values. Realizing the correlation coefficient values of SIMRIW simulation values in acceptable limits, further rice experiments in monsoon (Kharif) and post-monsoon (Rabi) agricultural seasons (2009, 2010 and 2011) were carried out with a location-specific distributed sensor network system. These proximal systems help to simulate dry weight, leaf area index and potential yield by the Java based SIMRIW on a daily/weekly/monthly/seasonal basis. These dynamic parameters are useful to the farming community for necessary decision making in a ubiquitous manner. However, SIMRIW requires fine tuning for better results/decision making.

  8. Space Weather Modeling Services at the Community Coordinated Modeling Center

    NASA Technical Reports Server (NTRS)

    Hesse, Michael

    2006-01-01

    The Community Coordinated Modeling Center (CCMC) is a multi-agency partnership, which aims at the creation of next generation space weather models. The goal of the CCMC is to support the research and developmental work necessary to substantially increase the present-day modeling capability for space weather purposes, and to provide models for transition to the Rapid Prototyping Centers at the space weather forecast centers. This goal requires close collaborations with and substantial involvement of the research community. The physical regions to be addressed by CCMC-related activities range from the solar atmosphere to the Earth's upper atmosphere. The CCMC is an integral part of the National Space Weather Program Implementation Plan, of NASA's Living With a Star (LWS) initiative, and of the Department of Defense Space Weather Transition Plan. CCMC includes a facility at NASA Goddard Space Flight Center. CCMC also provides, to the research community, access to state-of-the-art space research models. In this paper we will provide a description of the current CCMC status, discuss current plans, research and development accomplishments and goals, and describe the model testing and validation process undertaken as part of the CCMC mandate. Special emphasis will be on solar and heliospheric models currently residing at CCMC, and on plans for validation and verification.

  9. Geodetic Space Weather Monitoring by means of Ionosphere Modelling

    NASA Astrophysics Data System (ADS)

    Schmidt, Michael

    2017-04-01

    The term space weather indicates physical processes and phenomena in space caused by radiation of energy mainly from the Sun. Manifestations of space weather are (1) variations of the Earth's magnetic field, (2) the polar lights in the northern and southern hemisphere, (3) variations within the ionosphere as part of the upper atmosphere characterized by the existence of free electrons and ions, (4) the solar wind, i.e. the permanent emission of electrons and photons, (5) the interplanetary magnetic field, and (6) electric currents, e.g. the van Allen radiation belt. It can be stated that ionosphere disturbances are often caused by so-called solar storms. A solar storm comprises solar events such as solar flares and coronal mass ejections (CMEs) which have different effects on the Earth. Solar flares may cause disturbances in positioning, navigation and communication. CMEs can effect severe disturbances and in extreme cases damages or even destructions of modern infrastructure. Examples are interruptions to satellite services including the global navigation satellite systems (GNSS), communication systems, Earth observation and imaging systems or a potential failure of power networks. Currently the measurements of solar satellite missions such as STEREO and SOHO are used to forecast solar events. Besides these measurements the Earth's ionosphere plays another key role in monitoring the space weather, because it responses to solar storms with an increase of the electron density. Space-geodetic observation techniques, such as terrestrial GNSS, satellite altimetry, space-borne GPS (radio occultation), DORIS and VLBI provide valuable global information about the state of the ionosphere. Additionally geodesy has a long history and large experience in developing and using sophisticated analysis and combination techniques as well as empirical and physical modelling approaches. Consequently, geodesy is predestinated for strongly supporting space weather monitoring via

  10. A weather-driven model of malaria transmission.

    PubMed

    Hoshen, Moshe B; Morse, Andrew P

    2004-09-06

    Climate is a major driving force behind malaria transmission and climate data are often used to account for the spatial, seasonal and interannual variation in malaria transmission. This paper describes a mathematical-biological model of the parasite dynamics, comprising both the weather-dependent within-vector stages and the weather-independent within-host stages. Numerical evaluations of the model in both time and space show that it qualitatively reconstructs the prevalence of infection. A process-based modelling structure has been developed that may be suitable for the simulation of malaria forecasts based on seasonal weather forecasts.

  11. Highlights of Space Weather Services/Capabilities at NASA/GSFC Space Weather Center

    NASA Technical Reports Server (NTRS)

    Fok, Mei-Ching; Zheng, Yihua; Hesse, Michael; Kuznetsova, Maria; Pulkkinen, Antti; Taktakishvili, Aleksandre; Mays, Leila; Chulaki, Anna; Lee, Hyesook

    2012-01-01

    The importance of space weather has been recognized world-wide. Our society depends increasingly on technological infrastructure, including the power grid as well as satellites used for communication and navigation. Such technologies, however, are vulnerable to space weather effects caused by the Sun's variability. NASA GSFC's Space Weather Center (SWC) (http://science.gsfc.nasa.gov//674/swx services/swx services.html) has developed space weather products/capabilities/services that not only respond to NASA's needs but also address broader interests by leveraging the latest scientific research results and state-of-the-art models hosted at the Community Coordinated Modeling Center (CCMC: http://ccmc.gsfc.nasa.gov). By combining forefront space weather science and models, employing an innovative and configurable dissemination system (iSWA.gsfc.nasa.gov), taking advantage of scientific expertise both in-house and from the broader community as well as fostering and actively participating in multilateral collaborations both nationally and internationally, NASA/GSFC space weather Center, as a sibling organization to CCMC, is poised to address NASA's space weather needs (and needs of various partners) and to help enhancing space weather forecasting capabilities collaboratively. With a large number of state-of-the-art physics-based models running in real-time covering the whole space weather domain, it offers predictive capabilities and a comprehensive view of space weather events throughout the solar system. In this paper, we will provide some highlights of our service products/capabilities. In particular, we will take the 23 January and the 27 January space weather events as examples to illustrate how we can use the iSWA system to track them in the interplanetary space and forecast their impacts.

  12. An integrated weather and sea-state forecasting system for the Arabian Peninsula (WASSF)

    NASA Astrophysics Data System (ADS)

    Kallos, George; Galanis, George; Spyrou, Christos; Mitsakou, Christina; Solomos, Stavros; Bartsotas, Nikolaos; Kalogrei, Christina; Athanaselis, Ioannis; Sofianos, Sarantis; Vervatis, Vassios; Axaopoulos, Panagiotis; Papapostolou, Alexandros; Qahtani, Jumaan Al; Alaa, Elyas; Alexiou, Ioannis; Beard, Daniel

    2013-04-01

    Nowadays, large industrial conglomerates such as the Saudi ARAMCO, require a series of weather and sea state forecasting products that cannot be found in state meteorological offices or even commercial data providers. The two major objectives of the system is prevention and mitigation of environmental problems and of course early warning of local conditions associated with extreme weather events. The management and operations part is related to early warning of weather and sea-state events that affect operations of various facilities. The environmental part is related to air quality and especially the desert dust levels in the atmosphere. The components of the integrated system include: (i) a weather and desert dust prediction system with forecasting horizon of 5 days, (ii) a wave analysis and prediction component for Red Sea and Arabian Gulf, (iii) an ocean circulation and tidal analysis and prediction of both Red Sea and Arabian Gulf and (iv) an Aviation part specializing in the vertical structure of the atmosphere and extreme events that affect air transport and other operations. Specialized data sets required for on/offshore operations are provided ate regular basis. State of the art modeling components are integrated to a unique system that distributes the produced analysis and forecasts to each department. The weather and dust prediction system is SKIRON/Dust, the wave analysis and prediction system is based on WAM cycle 4 model from ECMWF, the ocean circulation model is MICOM while the tidal analysis and prediction is a development of the Ocean Physics and Modeling Group of University of Athens, incorporating the Tidal Model Driver. A nowcasting subsystem is included. An interactive system based on Google Maps gives the capability to extract and display the necessary information for any location of the Arabian Peninsula, the Red Sea and Arabian Gulf.

  13. Implementation guidelines for road weather information systems

    DOT National Transportation Integrated Search

    1997-11-01

    The report presents guidelines for implementing road weather information systems (RWIS). These guidelines will assist highway agency personnel with the planning, installation, and maintenance of road weather information systems for either ice or high...

  14. Modeling the weather impact on aviation in a global air traffic model

    NASA Astrophysics Data System (ADS)

    Himmelsbach, S.; Hauf, T.; Rokitansky, C. H.

    2009-09-01

    Weather has a strong impact on aviation safety and efficiency. For a better understanding of that impact, especially of thunderstorms and similar other severe hazards, we pursued a modeling approach. We used the detailed simulation software (NAVSIM) of worldwide air traffic, developed by Rokitansky [Eurocontrol, 2005] and implemented a specific weather module. NAVSIM models each aircraft with its specific performance characteristics separately along preplanned and prescribed routes. The specific weather module in its current version simulates a thunderstorm as an impenetrable 3D object, which forces an aircraft to circumvent the latter. We refer to that object in general terms as a weather object. The Cb-weather object, as a specific weather object, is a heuristic model of a real thunderstorm, with its characteristics based on actually observed satellite and precipitation radar data. It is comprised of an upper volume, mostly the anvil, and a bottom volume, the up- and downdrafts and the lower outflow area [Tafferner and Forster, 2009; Kober and Tafferner 2009; Zinner et al, 2008]. The Cb-weather object is already implemented in NAVSIM, other weather objects like icing and turbulence will follow. This combination of NAVSIM with a weather object allows a detailed investigation of situations where conflicts exist between planned flight routes and adverse weather. The first objective is to simulate the observed circum-navigation in NAVSIM. Real occurring routes will be compared with simulated ones. Once this has successfully completed, NAVSIM offers a platform to assess existing rules and develop more efficient strategies to cope with adverse weather. An overview will be given over the implementation status of weather objects within NAVSIM and first results will be presented. Cb-object data provision by A. Tafferner, C. Forster, T. Zinner, K. Kober, M. Hagen (DLR Oberpfaffenhofen) is greatly acknowledged. References: Eurocontrol, VDL Mode 2 Capacity Analysis through

  15. A graphical weather system design for the NASA transport systems research vehicle B-737

    NASA Technical Reports Server (NTRS)

    Scanlon, Charles H.

    1992-01-01

    A graphical weather system was designed for testing in the NASA Transport Systems Research Vehicle B-737 airplane and simulator. The purpose of these tests was to measure the impact of graphical weather products on aircrew decision processes, weather situation awareness, reroute clearances, workload, and weather monitoring. The flight crew graphical weather interface is described along with integration of the weather system with the flight navigation system, and data link transmission methods for sending weather data to the airplane.

  16. A weather-driven model of malaria transmission

    PubMed Central

    Hoshen, Moshe B; Morse, Andrew P

    2004-01-01

    Background Climate is a major driving force behind malaria transmission and climate data are often used to account for the spatial, seasonal and interannual variation in malaria transmission. Methods This paper describes a mathematical-biological model of the parasite dynamics, comprising both the weather-dependent within-vector stages and the weather-independent within-host stages. Results Numerical evaluations of the model in both time and space show that it qualitatively reconstructs the prevalence of infection. Conclusion A process-based modelling structure has been developed that may be suitable for the simulation of malaria forecasts based on seasonal weather forecasts. PMID:15350206

  17. Weather-based prediction of Plasmodium falciparum malaria in epidemic-prone regions of Ethiopia II. Weather-based prediction systems perform comparably to early detection systems in identifying times for interventions.

    PubMed

    Teklehaimanot, Hailay D; Schwartz, Joel; Teklehaimanot, Awash; Lipsitch, Marc

    2004-11-19

    Timely and accurate information about the onset of malaria epidemics is essential for effective control activities in epidemic-prone regions. Early warning methods that provide earlier alerts (usually by the use of weather variables) may permit control measures to interrupt transmission earlier in the epidemic, perhaps at the expense of some level of accuracy. Expected case numbers were modeled using a Poisson regression with lagged weather factors in a 4th-degree polynomial distributed lag model. For each week, the numbers of malaria cases were predicted using coefficients obtained using all years except that for which the prediction was being made. The effectiveness of alerts generated by the prediction system was compared against that of alerts based on observed cases. The usefulness of the prediction system was evaluated in cold and hot districts. The system predicts the overall pattern of cases well, yet underestimates the height of the largest peaks. Relative to alerts triggered by observed cases, the alerts triggered by the predicted number of cases performed slightly worse, within 5% of the detection system. The prediction-based alerts were able to prevent 10-25% more cases at a given sensitivity in cold districts than in hot ones. The prediction of malaria cases using lagged weather performed well in identifying periods of increased malaria cases. Weather-derived predictions identified epidemics with reasonable accuracy and better timeliness than early detection systems; therefore, the prediction of malarial epidemics using weather is a plausible alternative to early detection systems.

  18. Wildland fire probabilities estimated from weather model-deduced monthly mean fire danger indices

    Treesearch

    Haiganoush K. Preisler; Shyh-Chin Chen; Francis Fujioka; John W. Benoit; Anthony L. Westerling

    2008-01-01

    The National Fire Danger Rating System indices deduced from a regional simulation weather model were used to estimate probabilities and numbers of large fire events on monthly and 1-degree grid scales. The weather model simulations and forecasts are ongoing experimental products from the Experimental Climate Prediction Center at the Scripps Institution of Oceanography...

  19. INNOVATIVE URBAN WET-WEATHER FLOW MANAGEMENT SYSTEMS

    EPA Science Inventory

    This report describes innovative methods to improve wet weather flow (WWF) management systems, that provide drainage services at the same time as decreasing stormwater pollutant discharges, for urban developments of the 21st century. Traditionally, wet-weather collection systems...

  20. Ensemble superparameterization versus stochastic parameterization: A comparison of model uncertainty representation in tropical weather prediction

    NASA Astrophysics Data System (ADS)

    Subramanian, Aneesh C.; Palmer, Tim N.

    2017-06-01

    Stochastic schemes to represent model uncertainty in the European Centre for Medium-Range Weather Forecasts (ECMWF) ensemble prediction system has helped improve its probabilistic forecast skill over the past decade by both improving its reliability and reducing the ensemble mean error. The largest uncertainties in the model arise from the model physics parameterizations. In the tropics, the parameterization of moist convection presents a major challenge for the accurate prediction of weather and climate. Superparameterization is a promising alternative strategy for including the effects of moist convection through explicit turbulent fluxes calculated from a cloud-resolving model (CRM) embedded within a global climate model (GCM). In this paper, we compare the impact of initial random perturbations in embedded CRMs, within the ECMWF ensemble prediction system, with stochastically perturbed physical tendency (SPPT) scheme as a way to represent model uncertainty in medium-range tropical weather forecasts. We especially focus on forecasts of tropical convection and dynamics during MJO events in October-November 2011. These are well-studied events for MJO dynamics as they were also heavily observed during the DYNAMO field campaign. We show that a multiscale ensemble modeling approach helps improve forecasts of certain aspects of tropical convection during the MJO events, while it also tends to deteriorate certain large-scale dynamic fields with respect to stochastically perturbed physical tendencies approach that is used operationally at ECMWF.Plain Language SummaryProbabilistic <span class="hlt">weather</span> forecasts, especially for tropical <span class="hlt">weather</span>, is still a significant challenge for global <span class="hlt">weather</span> forecasting <span class="hlt">systems</span>. Expressing uncertainty along with <span class="hlt">weather</span> forecasts is important for informed decision making. Hence, we explore the use of a relatively new approach in using super-parameterization, where a cloud resolving <span class="hlt">model</span> is embedded</p> </li> </ol> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_2");'>2</a></li> <li><a href="#" onclick='return showDiv("page_3");'>3</a></li> <li class="active"><span>4</span></li> <li><a href="#" onclick='return showDiv("page_5");'>5</a></li> <li><a href="#" onclick='return showDiv("page_6");'>6</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div><!-- col-sm-12 --> </div><!-- row --> </div><!-- page_4 --> <div id="page_5" class="hiddenDiv"> <div class="row"> <div class="col-sm-12"> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_3");'>3</a></li> <li><a href="#" onclick='return showDiv("page_4");'>4</a></li> <li class="active"><span>5</span></li> <li><a href="#" onclick='return showDiv("page_6");'>6</a></li> <li><a href="#" onclick='return showDiv("page_7");'>7</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div> </div> <div class="row"> <div class="col-sm-12"> <ol class="result-class" start="81"> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/CFR-2010-title14-vol1/pdf/CFR-2010-title14-vol1-sec25-961.pdf','CFR'); return false;" href="https://www.gpo.gov/fdsys/pkg/CFR-2010-title14-vol1/pdf/CFR-2010-title14-vol1-sec25-961.pdf"><span>14 CFR 25.961 - Fuel <span class="hlt">system</span> hot <span class="hlt">weather</span> operation.</span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collectionCfr.action?selectedYearFrom=2010&page.go=Go">Code of Federal Regulations, 2010 CFR</a></p> <p></p> <p>2010-01-01</p> <p>... AIRCRAFT AIRWORTHINESS STANDARDS: TRANSPORT CATEGORY AIRPLANES Powerplant Fuel <span class="hlt">System</span> § 25.961 Fuel <span class="hlt">system</span> hot <span class="hlt">weather</span> operation. (a) The fuel <span class="hlt">system</span> must perform satisfactorily in hot <span class="hlt">weather</span> operation. This... 14 Aeronautics and Space 1 2010-01-01 2010-01-01 false Fuel <span class="hlt">system</span> hot <span class="hlt">weather</span> operation. 25.961...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/CFR-2013-title14-vol1/pdf/CFR-2013-title14-vol1-sec25-961.pdf','CFR2013'); return false;" href="https://www.gpo.gov/fdsys/pkg/CFR-2013-title14-vol1/pdf/CFR-2013-title14-vol1-sec25-961.pdf"><span>14 CFR 25.961 - Fuel <span class="hlt">system</span> hot <span class="hlt">weather</span> operation.</span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collectionCfr.action?selectedYearFrom=2013&page.go=Go">Code of Federal Regulations, 2013 CFR</a></p> <p></p> <p>2013-01-01</p> <p>... AIRCRAFT AIRWORTHINESS STANDARDS: TRANSPORT CATEGORY AIRPLANES Powerplant Fuel <span class="hlt">System</span> § 25.961 Fuel <span class="hlt">system</span> hot <span class="hlt">weather</span> operation. (a) The fuel <span class="hlt">system</span> must perform satisfactorily in hot <span class="hlt">weather</span> operation. This... 14 Aeronautics and Space 1 2013-01-01 2013-01-01 false Fuel <span class="hlt">system</span> hot <span class="hlt">weather</span> operation. 25.961...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/CFR-2012-title14-vol1/pdf/CFR-2012-title14-vol1-sec25-961.pdf','CFR2012'); return false;" href="https://www.gpo.gov/fdsys/pkg/CFR-2012-title14-vol1/pdf/CFR-2012-title14-vol1-sec25-961.pdf"><span>14 CFR 25.961 - Fuel <span class="hlt">system</span> hot <span class="hlt">weather</span> operation.</span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collectionCfr.action?selectedYearFrom=2012&page.go=Go">Code of Federal Regulations, 2012 CFR</a></p> <p></p> <p>2012-01-01</p> <p>... AIRCRAFT AIRWORTHINESS STANDARDS: TRANSPORT CATEGORY AIRPLANES Powerplant Fuel <span class="hlt">System</span> § 25.961 Fuel <span class="hlt">system</span> hot <span class="hlt">weather</span> operation. (a) The fuel <span class="hlt">system</span> must perform satisfactorily in hot <span class="hlt">weather</span> operation. This... 14 Aeronautics and Space 1 2012-01-01 2012-01-01 false Fuel <span class="hlt">system</span> hot <span class="hlt">weather</span> operation. 25.961...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/CFR-2011-title14-vol1/pdf/CFR-2011-title14-vol1-sec25-961.pdf','CFR2011'); return false;" href="https://www.gpo.gov/fdsys/pkg/CFR-2011-title14-vol1/pdf/CFR-2011-title14-vol1-sec25-961.pdf"><span>14 CFR 25.961 - Fuel <span class="hlt">system</span> hot <span class="hlt">weather</span> operation.</span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collectionCfr.action?selectedYearFrom=2011&page.go=Go">Code of Federal Regulations, 2011 CFR</a></p> <p></p> <p>2011-01-01</p> <p>... AIRCRAFT AIRWORTHINESS STANDARDS: TRANSPORT CATEGORY AIRPLANES Powerplant Fuel <span class="hlt">System</span> § 25.961 Fuel <span class="hlt">system</span> hot <span class="hlt">weather</span> operation. (a) The fuel <span class="hlt">system</span> must perform satisfactorily in hot <span class="hlt">weather</span> operation. This... 14 Aeronautics and Space 1 2011-01-01 2011-01-01 false Fuel <span class="hlt">system</span> hot <span class="hlt">weather</span> operation. 25.961...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/CFR-2014-title14-vol1/pdf/CFR-2014-title14-vol1-sec25-961.pdf','CFR2014'); return false;" href="https://www.gpo.gov/fdsys/pkg/CFR-2014-title14-vol1/pdf/CFR-2014-title14-vol1-sec25-961.pdf"><span>14 CFR 25.961 - Fuel <span class="hlt">system</span> hot <span class="hlt">weather</span> operation.</span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collectionCfr.action?selectedYearFrom=2014&page.go=Go">Code of Federal Regulations, 2014 CFR</a></p> <p></p> <p>2014-01-01</p> <p>... AIRCRAFT AIRWORTHINESS STANDARDS: TRANSPORT CATEGORY AIRPLANES Powerplant Fuel <span class="hlt">System</span> § 25.961 Fuel <span class="hlt">system</span> hot <span class="hlt">weather</span> operation. (a) The fuel <span class="hlt">system</span> must perform satisfactorily in hot <span class="hlt">weather</span> operation. This... 14 Aeronautics and Space 1 2014-01-01 2014-01-01 false Fuel <span class="hlt">system</span> hot <span class="hlt">weather</span> operation. 25.961...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2013IJBm...57..107S','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2013IJBm...57..107S"><span>Evaluation of <span class="hlt">weather</span>-based rice yield <span class="hlt">models</span> in India</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Sudharsan, D.; Adinarayana, J.; Reddy, D. Raji; Sreenivas, G.; Ninomiya, S.; Hirafuji, M.; Kiura, T.; Tanaka, K.; Desai, U. B.; Merchant, S. N.</p> <p>2013-01-01</p> <p>The objective of this study was to compare two different rice simulation models—standalone (Decision Support <span class="hlt">System</span> for Agrotechnology Transfer [DSSAT]) and web based (SImulation <span class="hlt">Model</span> for RIce-<span class="hlt">Weather</span> relations [SIMRIW])—with agrometeorological data and agronomic parameters for estimation of rice crop production in southern semi-arid tropics of India. Studies were carried out on the BPT5204 rice variety to evaluate two crop simulation <span class="hlt">models</span>. Long-term experiments were conducted in a research farm of Acharya N G Ranga Agricultural University (ANGRAU), Hyderabad, India. Initially, the results were obtained using 4 years (1994-1997) of data with <span class="hlt">weather</span> parameters from a local <span class="hlt">weather</span> station to evaluate DSSAT simulated results with observed values. Linear regression <span class="hlt">models</span> used for the purpose showed a close relationship between DSSAT and observed yield. Subsequently, yield comparisons were also carried out with SIMRIW and DSSAT, and validated with actual observed values. Realizing the correlation coefficient values of SIMRIW simulation values in acceptable limits, further rice experiments in monsoon (Kharif) and post-monsoon (Rabi) agricultural seasons (2009, 2010 and 2011) were carried out with a location-specific distributed sensor network <span class="hlt">system</span>. These proximal <span class="hlt">systems</span> help to simulate dry weight, leaf area index and potential yield by the Java based SIMRIW on a daily/weekly/monthly/seasonal basis. These dynamic parameters are useful to the farming community for necessary decision making in a ubiquitous manner. However, SIMRIW requires fine tuning for better results/decision making.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/20130012522','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/20130012522"><span>Maintaining a Local Data Integration <span class="hlt">System</span> in Support of <span class="hlt">Weather</span> Forecast Operations</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Watson, Leela R.; Blottman, Peter F.; Sharp, David W.; Hoeth, Brian</p> <p>2010-01-01</p> <p>Since 2000, both the National <span class="hlt">Weather</span> Service in Melbourne, FL (NWS MLB) and the Spaceflight Meteorology Group (SMG) have used a local data integration <span class="hlt">system</span> (LDIS) as part of their forecast and warning operations. Each has benefited from 3-dimensional analyses that are delivered to forecasters every 15 minutes across the peninsula of Florida. The intent is to generate products that enhance short-range <span class="hlt">weather</span> forecasts issued in support of NWS MLB and SMG operational requirements within East Central Florida. The current LDIS uses the Advanced Regional Prediction <span class="hlt">System</span> (ARPS) Data Analysis <span class="hlt">System</span> (ADAS) package as its core, which integrates a wide variety of national, regional, and local observational data sets. It assimilates all available real-time data within its domain and is run at a finer spatial and temporal resolution than current national- or regional-scale analysis packages. As such, it provides local forecasters with a more comprehensive and complete understanding of evolving fine-scale <span class="hlt">weather</span> features. Recent efforts have been undertaken to update the LDIS through the formal tasking process of NASA's Applied Meteorology Unit. The goals include upgrading LDIS with the latest version of ADAS, incorporating new sources of observational data, and making adjustments to shell scripts written to govern the <span class="hlt">system</span>. A series of scripts run a complete <span class="hlt">modeling</span> <span class="hlt">system</span> consisting of the preprocessing step, the main <span class="hlt">model</span> integration, and the post-processing step. The preprocessing step prepares the terrain, surface characteristics data sets, and the objective analysis for <span class="hlt">model</span> initialization. Data ingested through ADAS include (but are not limited to) Level II <span class="hlt">Weather</span> Surveillance Radar- 1988 Doppler (WSR-88D) data from six Florida radars, Geostationary Operational Environmental Satellites (GOES) visible and infrared satellite imagery, surface and upper air observations throughout Florida from NOAA's Earth <span class="hlt">System</span> Research Laboratory/Global <span class="hlt">Systems</span> Division</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/19900002747','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/19900002747"><span>Application of dynamical <span class="hlt">systems</span> theory to global <span class="hlt">weather</span> phenomena revealed by satellite imagery</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Saltzman, Barry; Ebisuzaki, Wesley; Maasch, Kirk A.; Oglesby, Robert; Pandolfo, Lionel; Tang, Chung-Muh</p> <p>1989-01-01</p> <p>Theoretical studies of low frequency and seasonal <span class="hlt">weather</span> variability; dynamical properties of observational and general circulation <span class="hlt">model</span> (GCM)-generated records; effects of the hydrologic cycle and latent heat release on extratropical <span class="hlt">weather</span>; and Earth-<span class="hlt">system</span> science studies are summarized.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2018JOUC...17..219L','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2018JOUC...17..219L"><span>Plausible Effect of <span class="hlt">Weather</span> on Atlantic Meridional Overturning Circulation with a Coupled General Circulation <span class="hlt">Model</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Liu, Zedong; Wan, Xiuquan</p> <p>2018-04-01</p> <p>The Atlantic meridional overturning circulation (AMOC) is a vital component of the global ocean circulation and the heat engine of the climate <span class="hlt">system</span>. Through the use of a coupled general circulation <span class="hlt">model</span>, this study examines the role of synoptic <span class="hlt">systems</span> on the AMOC and presents evidence that internally generated high-frequency, synoptic-scale <span class="hlt">weather</span> variability in the atmosphere could play a significant role in maintaining the overall strength and variability of the AMOC, thereby affecting climate variability and change. Results of a novel coupling technique show that the strength and variability of the AMOC are greatly reduced once the synoptic <span class="hlt">weather</span> variability is suppressed in the coupled <span class="hlt">model</span>. The strength and variability of the AMOC are closely linked to deep convection events at high latitudes, which could be strongly affected by the <span class="hlt">weather</span> variability. Our results imply that synoptic <span class="hlt">weather</span> <span class="hlt">systems</span> are important in driving the AMOC and its variability. Thus, interactions between atmospheric <span class="hlt">weather</span> variability and AMOC may be an important feedback mechanism of the global climate <span class="hlt">system</span> and need to be taken into consideration in future climate change studies.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017ApWS....7.3869S','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017ApWS....7.3869S"><span><span class="hlt">Weather</span> forecasting based on hybrid neural <span class="hlt">model</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Saba, Tanzila; Rehman, Amjad; AlGhamdi, Jarallah S.</p> <p>2017-11-01</p> <p>Making deductions and expectations about climate has been a challenge all through mankind's history. Challenges with exact meteorological directions assist to foresee and handle problems well in time. Different strategies have been investigated using various machine learning techniques in reported forecasting <span class="hlt">systems</span>. Current research investigates climate as a major challenge for machine information mining and deduction. Accordingly, this paper presents a hybrid neural <span class="hlt">model</span> (MLP and RBF) to enhance the accuracy of <span class="hlt">weather</span> forecasting. Proposed hybrid <span class="hlt">model</span> ensure precise forecasting due to the specialty of climate anticipating frameworks. The study concentrates on the data representing Saudi Arabia <span class="hlt">weather</span> forecasting. The main input features employed to train individual and hybrid neural networks that include average dew point, minimum temperature, maximum temperature, mean temperature, average relative moistness, precipitation, normal wind speed, high wind speed and average cloudiness. The output layer composed of two neurons to represent rainy and dry <span class="hlt">weathers</span>. Moreover, trial and error approach is adopted to select an appropriate number of inputs to the hybrid neural network. Correlation coefficient, RMSE and scatter index are the standard yard sticks adopted for forecast accuracy measurement. On individual standing MLP forecasting results are better than RBF, however, the proposed simplified hybrid neural <span class="hlt">model</span> comes out with better forecasting accuracy as compared to both individual networks. Additionally, results are better than reported in the state of art, using a simple neural structure that reduces training time and complexity.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/20130012589','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/20130012589"><span><span class="hlt">Weather</span> Research and Forecasting <span class="hlt">Model</span> Sensitivity Comparisons for Warm Season Convective Initiation</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Watson, Leela R.; Hoeth, Brian; Blottman, Peter F.</p> <p>2007-01-01</p> <p> configuration options are best to address this specific forecast concern, the <span class="hlt">Weather</span> Research and Forecasting (WRF) <span class="hlt">model</span>, which has two dynamical cores - the Advanced Research WRF (ARW) and the Non-hydrostatic Mesoscale <span class="hlt">Model</span> (NMM) was employed. In addition to the two dynamical cores, there are also two options for a "hot-start" initialization of the WRF <span class="hlt">model</span> - the Local Analysis and Prediction <span class="hlt">System</span> (LAPS; McGinley 1995) and the Advanced Regional Prediction <span class="hlt">System</span> (ARPS) Data Analysis <span class="hlt">System</span> (ADAS; Brewster 1996). Both LAPS and ADAS are 3- dimensional <span class="hlt">weather</span> analysis <span class="hlt">systems</span> that integrate multiple meteorological data sources into one consistent analysis over the user's domain of interest. This allows mesoscale <span class="hlt">models</span> to benefit from the addition of highresolution data sources. Having a series of initialization options and WRF cores, as well as many options within each core, provides SMG and MLB with considerable flexibility as well as challenges. It is the goal of this study to assess the different configurations available and to determine which configuration will best predict warm season convective initiation.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/20110000762','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/20110000762"><span><span class="hlt">Systems</span> and methods for supplemental <span class="hlt">weather</span> information presentation on a display</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Bunch, Brian (Inventor)</p> <p>2010-01-01</p> <p>An embodiment of the supplemental <span class="hlt">weather</span> display <span class="hlt">system</span> presents supplemental <span class="hlt">weather</span> information on a display in a craft. An exemplary embodiment receives the supplemental <span class="hlt">weather</span> information from a remote source, determines a location of the supplemental <span class="hlt">weather</span> information relative to the craft, receives <span class="hlt">weather</span> information from an on-board radar <span class="hlt">system</span>, and integrates the supplemental <span class="hlt">weather</span> information with the <span class="hlt">weather</span> information received from the on-board radar <span class="hlt">system</span>.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/23925175','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/23925175"><span>Improved wet <span class="hlt">weather</span> wastewater influent <span class="hlt">modelling</span> at Viikinmäki WWTP by on-line <span class="hlt">weather</span> radar information.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Heinonen, M; Jokelainen, M; Fred, T; Koistinen, J; Hohti, H</p> <p>2013-01-01</p> <p>Municipal wastewater treatment plant (WWTP) influent is typically dependent on diurnal variation of urban production of liquid waste, infiltration of stormwater runoff and groundwater infiltration. During wet <span class="hlt">weather</span> conditions the infiltration phenomenon typically increases the risk of overflows in the sewer <span class="hlt">system</span> as well as the risk of having to bypass the WWTP. Combined sewer infrastructure multiplies the role of rainwater runoff in the total influent. Due to climate change, rain intensity and magnitude is tending to rise as well, which can already be observed in the normal operation of WWTPs. Bypass control can be improved if the WWTP is prepared for the increase of influent, especially if there is some storage capacity prior to the treatment plant. One option for this bypass control is utilisation of on-line <span class="hlt">weather</span>-radar-based forecast data of rainfall as an input for the on-line influent <span class="hlt">model</span>. This paper reports the Viikinmäki WWTP wet <span class="hlt">weather</span> influent <span class="hlt">modelling</span> project results where gridded exceedance probabilities of hourly rainfall accumulations for the next 3 h from the Finnish Meteorological Institute are utilised as on-line input data for the influent <span class="hlt">model</span>.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2018GeCoA.233..159K','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2018GeCoA.233..159K"><span>Effects of atmospheric composition on apparent activation energy of silicate <span class="hlt">weathering</span>: I. <span class="hlt">Model</span> formulation</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Kanzaki, Yoshiki; Murakami, Takashi</p> <p>2018-07-01</p> <p>We have developed a <span class="hlt">weathering</span> <span class="hlt">model</span> to comprehensively understand the determining factors of the apparent activation energy of silicate <span class="hlt">weathering</span> in order to better estimate the silicate-<span class="hlt">weathering</span> flux in the Precambrian. The <span class="hlt">model</span> formulates the reaction rate of a mineral as a basis, then the elemental loss by summing the reaction rates of whole minerals, and finally the <span class="hlt">weathering</span> flux from a given <span class="hlt">weathering</span> profile by integrating the elemental losses along the depth of the profile. The rate expressions are formulated with physicochemical parameters relevant to <span class="hlt">weathering</span>, including solution and atmospheric compositions. The apparent activation energies of silicate <span class="hlt">weathering</span> are then represented by the temperature dependences of the physicochemical parameters based on the rate expressions. It was found that the interactions between individual mineral-reactions and the compositions of solution and atmosphere are necessarily accompanied by those of temperature-dependence counterparts. Indeed, the <span class="hlt">model</span> calculates the apparent activation energy of silicate <span class="hlt">weathering</span> as a function of the temperature dependence of atmospheric CO2 (Δ HCO2‧) . The dependence of the apparent activation energy of silicate <span class="hlt">weathering</span> on Δ HCO2‧ may explain the empirical dependence of silicate <span class="hlt">weathering</span> on the atmospheric composition. We further introduce a compensation law between the apparent activation energy and the pre-exponential factor to obtain the relationship between the silicate-<span class="hlt">weathering</span> flux (FCO2), temperature and the apparent activation energy. The <span class="hlt">model</span> calculation and the compensation law enable us to predict FCO2 as a function of temperature, once Δ HCO2‧ is given. The validity of the <span class="hlt">model</span> is supported by agreements between the <span class="hlt">model</span> prediction and observations of the apparent activation energy and FCO2 in the modern <span class="hlt">weathering</span> <span class="hlt">systems</span>. The present <span class="hlt">weathering</span> <span class="hlt">model</span> will be useful for the estimation of FCO2 in the Precambrian, for which Δ HCO2‧ can be</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2013CSR....63S...2O','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2013CSR....63S...2O"><span>Forecasting near-surface <span class="hlt">weather</span> conditions and precipitation in Alaska's Prince William Sound with the PWS-WRF <span class="hlt">modeling</span> <span class="hlt">system</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Olsson, Peter Q.; Volz, Karl P.; Liu, Haibo</p> <p>2013-07-01</p> <p>In the summer of 2009, several scientific teams engaged in a field program in Prince William Sound (PWS), Alaska to test an end-to-end atmosphere/ocean prediction <span class="hlt">system</span> specially designed for this region. The "Sound Predictions Field Experiment" (FE) was a test of the PWS-Observing <span class="hlt">System</span> (PWS-OS) and the culmination of a five-year program to develop an observational and prediction <span class="hlt">system</span> for the Sound. This manuscript reports on results of an 18-day high-resolution atmospheric forecasting field project using the <span class="hlt">Weather</span> Research and Forecasting (WRF) <span class="hlt">model</span>.Special attention was paid to surface meteorological properties and precipitation. Upon reviewing the results of the real-time forecasts, modifications were incorporated in the PWS-WRF <span class="hlt">modeling</span> <span class="hlt">system</span> in an effort to improve objective forecast skill. Changes were both geometric (<span class="hlt">model</span> grid structure) and physical (different physics parameterizations).The <span class="hlt">weather</span> during the summer-time FE was typical of the PWS in that it was characterized by a number of minor disturbances rotating around an anchored low, but with no major storms in the Gulf of Alaska. The basic PWS-WRF <span class="hlt">modeling</span> <span class="hlt">system</span> as implemented operationally for the FE performed well, especially considering the extremely complex terrain comprising the greater PWS region.Modifications to the initial PWS-WRF <span class="hlt">modeling</span> <span class="hlt">system</span> showed improvement in predicting surface variables, especially where the ambient flow interacted strongly with the terrain. Prediction of precipitation on an accumulated basis was more accurate than prediction on a day-to-day basis. The 18-day period was too short to provide reliable assessment and intercomparison of the quantitative precipitation forecasting (QPF) skill of the PWS-WRF <span class="hlt">model</span> variants.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/20140011813','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/20140011813"><span>Tethered Satellites as an Enabling Platform for Operational Space <span class="hlt">Weather</span> Monitoring <span class="hlt">Systems</span></span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Gilchrist, Brian E.; Krause, Linda Habash; Gallagher, Dennis Lee; Bilen, Sven Gunnar; Fuhrhop, Keith; Hoegy, Walt R.; Inderesan, Rohini; Johnson, Charles; Owens, Jerry Keith; Powers, Joseph; <a style="text-decoration: none; " href="javascript:void(0); " onClick="displayelement('author_20140011813'); toggleEditAbsImage('author_20140011813_show'); toggleEditAbsImage('author_20140011813_hide'); "> <img style="display:inline; width:12px; height:12px; " src="images/arrow-up.gif" width="12" height="12" border="0" alt="hide" id="author_20140011813_show"> <img style="width:12px; height:12px; display:none; " src="images/arrow-down.gif" width="12" height="12" border="0" alt="hide" id="author_20140011813_hide"></p> <p>2013-01-01</p> <p>Tethered satellites offer the potential to be an important enabling technology to support operational space <span class="hlt">weather</span> monitoring <span class="hlt">systems</span>. Space <span class="hlt">weather</span> "nowcasting" and forecasting <span class="hlt">models</span> rely on assimilation of near-real-time (NRT) space environment data to provide warnings for storm events and deleterious effects on the global societal infrastructure. Typically, these <span class="hlt">models</span> are initialized by a climatological <span class="hlt">model</span> to provide "most probable distributions" of environmental parameters as a function of time and space. The process of NRT data assimilation gently pulls the climate <span class="hlt">model</span> closer toward the observed state (e.g., via Kalman smoothing) for nowcasting, and forecasting is achieved through a set of iterative semi-empirical physics-based forward-prediction calculations. Many challenges are associated with the development of an operational <span class="hlt">system</span>, from the top-level architecture (e.g., the required space <span class="hlt">weather</span> observatories to meet the spatial and temporal requirements of these <span class="hlt">models</span>) down to the individual instruments capable of making the NRT measurements. This study focuses on the latter challenge: we present some examples of how tethered satellites (from 100s of m to 20 km) are uniquely suited to address certain shortfalls in our ability to measure critical environmental parameters necessary to drive these space <span class="hlt">weather</span> <span class="hlt">models</span>. Examples include long baseline electric field measurements, magnetized ionospheric conductivity measurements, and the ability to separate temporal from spatial irregularities in environmental parameters. Tethered satellite functional requirements are presented for two examples of space environment observables.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.osti.gov/biblio/21028314-origins-computer-weather-prediction-climate-modeling','SCIGOV-STC'); return false;" href="https://www.osti.gov/biblio/21028314-origins-computer-weather-prediction-climate-modeling"><span>The origins of computer <span class="hlt">weather</span> prediction and climate <span class="hlt">modeling</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>Lynch, Peter</p> <p>2008-03-20</p> <p>Numerical simulation of an ever-increasing range of geophysical phenomena is adding enormously to our understanding of complex processes in the Earth <span class="hlt">system</span>. The consequences for mankind of ongoing climate change will be far-reaching. Earth <span class="hlt">System</span> <span class="hlt">Models</span> are capable of replicating climate regimes of past millennia and are the best means we have of predicting the future of our climate. The basic ideas of numerical forecasting and climate <span class="hlt">modeling</span> were developed about a century ago, long before the first electronic computer was constructed. There were several major practical obstacles to be overcome before numerical prediction could be put into practice. Amore » fuller understanding of atmospheric dynamics allowed the development of simplified <span class="hlt">systems</span> of equations; regular radiosonde observations of the free atmosphere and, later, satellite data, provided the initial conditions; stable finite difference schemes were developed; and powerful electronic computers provided a practical means of carrying out the prodigious calculations required to predict the changes in the <span class="hlt">weather</span>. Progress in <span class="hlt">weather</span> forecasting and in climate <span class="hlt">modeling</span> over the past 50 years has been dramatic. In this presentation, we will trace the history of computer forecasting through the ENIAC integrations to the present day. The useful range of deterministic prediction is increasing by about one day each decade, and our understanding of climate change is growing rapidly as Earth <span class="hlt">System</span> <span class="hlt">Models</span> of ever-increasing sophistication are developed.« less</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2008JCoPh.227.3431L','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2008JCoPh.227.3431L"><span>The origins of computer <span class="hlt">weather</span> prediction and climate <span class="hlt">modeling</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Lynch, Peter</p> <p>2008-03-01</p> <p>Numerical simulation of an ever-increasing range of geophysical phenomena is adding enormously to our understanding of complex processes in the Earth <span class="hlt">system</span>. The consequences for mankind of ongoing climate change will be far-reaching. Earth <span class="hlt">System</span> <span class="hlt">Models</span> are capable of replicating climate regimes of past millennia and are the best means we have of predicting the future of our climate. The basic ideas of numerical forecasting and climate <span class="hlt">modeling</span> were developed about a century ago, long before the first electronic computer was constructed. There were several major practical obstacles to be overcome before numerical prediction could be put into practice. A fuller understanding of atmospheric dynamics allowed the development of simplified <span class="hlt">systems</span> of equations; regular radiosonde observations of the free atmosphere and, later, satellite data, provided the initial conditions; stable finite difference schemes were developed; and powerful electronic computers provided a practical means of carrying out the prodigious calculations required to predict the changes in the <span class="hlt">weather</span>. Progress in <span class="hlt">weather</span> forecasting and in climate <span class="hlt">modeling</span> over the past 50 years has been dramatic. In this presentation, we will trace the history of computer forecasting through the ENIAC integrations to the present day. The useful range of deterministic prediction is increasing by about one day each decade, and our understanding of climate change is growing rapidly as Earth <span class="hlt">System</span> <span class="hlt">Models</span> of ever-increasing sophistication are developed.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.osti.gov/servlets/purl/1182264','SCIGOV-STC'); return false;" href="https://www.osti.gov/servlets/purl/1182264"><span>Application of global <span class="hlt">weather</span> and climate <span class="hlt">model</span> output to the design and operation of wind-energy <span class="hlt">systems</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>Curry, Judith</p> <p></p> <p>This project addressed the challenge of providing <span class="hlt">weather</span> and climate information to support the operation, management and planning for wind-energy <span class="hlt">systems</span>. The need for forecast information is extending to longer projection windows with increasing penetration of wind power into the grid and also with diminishing reserve margins to meet peak loads during significant <span class="hlt">weather</span> events. Maintenance planning and natural gas trading is being influenced increasingly by anticipation of wind generation on timescales of weeks to months. Future scenarios on decadal time scales are needed to support assessment of wind farm siting, government planning, long-term wind purchase agreements and the regulatorymore » environment. The challenge of making wind forecasts on these longer time scales is associated with a wide range of uncertainties in general circulation and regional climate <span class="hlt">models</span> that make them unsuitable for direct use in the design and planning of wind-energy <span class="hlt">systems</span>. To address this challenge, CFAN has developed a hybrid statistical/dynamical forecasting scheme for delivering probabilistic forecasts on time scales from one day to seven months using what is arguably the best forecasting <span class="hlt">system</span> in the world (European Centre for Medium Range <span class="hlt">Weather</span> Forecasting, ECMWF). The project also provided a framework to assess future wind power through developing scenarios of interannual to decadal climate variability and change. The Phase II research has successfully developed an operational wind power forecasting <span class="hlt">system</span> for the U.S., which is being extended to Europe and possibly Asia.« less</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/20140006924','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/20140006924"><span>Development and Implementation of Dynamic Scripts to Support Local <span class="hlt">Model</span> Verification at National <span class="hlt">Weather</span> Service <span class="hlt">Weather</span> Forecast Offices</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Zavordsky, Bradley; Case, Jonathan L.; Gotway, John H.; White, Kristopher; Medlin, Jeffrey; Wood, Lance; Radell, Dave</p> <p>2014-01-01</p> <p>Local <span class="hlt">modeling</span> with a customized configuration is conducted at National <span class="hlt">Weather</span> Service (NWS) <span class="hlt">Weather</span> Forecast Offices (WFOs) to produce high-resolution numerical forecasts that can better simulate local <span class="hlt">weather</span> phenomena and complement larger scale global and regional <span class="hlt">models</span>. The advent of the Environmental <span class="hlt">Modeling</span> <span class="hlt">System</span> (EMS), which provides a pre-compiled version of the <span class="hlt">Weather</span> Research and Forecasting (WRF) <span class="hlt">model</span> and wrapper Perl scripts, has enabled forecasters to easily configure and execute the WRF <span class="hlt">model</span> on local workstations. NWS WFOs often use EMS output to help in forecasting highly localized, mesoscale features such as convective initiation, the timing and inland extent of lake effect snow bands, lake and sea breezes, and topographically-modified winds. However, quantitatively evaluating <span class="hlt">model</span> performance to determine errors and biases still proves to be one of the challenges in running a local <span class="hlt">model</span>. Developed at the National Center for Atmospheric Research (NCAR), the <span class="hlt">Model</span> Evaluation Tools (MET) verification software makes performing these types of quantitative analyses easier, but operational forecasters do not generally have time to familiarize themselves with navigating the sometimes complex configurations associated with the MET tools. To assist forecasters in running a subset of MET programs and capabilities, the Short-term Prediction Research and Transition (SPoRT) Center has developed and transitioned a set of dynamic, easily configurable Perl scripts to collaborating NWS WFOs. The objective of these scripts is to provide SPoRT collaborating partners in the NWS with the ability to evaluate the skill of their local EMS <span class="hlt">model</span> runs in near real time with little prior knowledge of the MET package. The ultimate goal is to make these verification scripts available to the broader NWS community in a future version of the EMS software. This paper provides an overview of the SPoRT MET scripts, instructions for how the scripts are run, and example use</p> </li> </ol> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_3");'>3</a></li> <li><a href="#" onclick='return showDiv("page_4");'>4</a></li> <li class="active"><span>5</span></li> <li><a href="#" onclick='return showDiv("page_6");'>6</a></li> <li><a href="#" onclick='return showDiv("page_7");'>7</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div><!-- col-sm-12 --> </div><!-- row --> </div><!-- page_5 --> <div id="page_6" class="hiddenDiv"> <div class="row"> <div class="col-sm-12"> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_4");'>4</a></li> <li><a href="#" onclick='return showDiv("page_5");'>5</a></li> <li class="active"><span>6</span></li> <li><a href="#" onclick='return showDiv("page_7");'>7</a></li> <li><a href="#" onclick='return showDiv("page_8");'>8</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div> </div> <div class="row"> <div class="col-sm-12"> <ol class="result-class" start="101"> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2018AAS...23115212H','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2018AAS...23115212H"><span>Improved <span class="hlt">Weather</span> Forecasting for the Dynamic Scheduling <span class="hlt">System</span> of the Green Bank Telescope</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Henry, Kari; Maddalena, Ronald</p> <p>2018-01-01</p> <p>The Robert C Byrd Green Bank Telescope (GBT) uses a software <span class="hlt">system</span> that dynamically schedules observations based on <span class="hlt">models</span> of vertical <span class="hlt">weather</span> forecasts produced by the National <span class="hlt">Weather</span> Service (NWS). The NWS provides hourly forecasted values for ~60 layers that extend into the stratosphere over the observatory. We use <span class="hlt">models</span>, recommended by the Radiocommunication Sector of the International Telecommunications Union, to derive the absorption coefficient in each layer for each hour in the NWS forecasts and for all frequencies over which the GBT has receivers, 0.1 to 115 GHz. We apply radiative transfer <span class="hlt">models</span> to derive the opacity and the atmospheric contributions to the <span class="hlt">system</span> temperature, thereby deriving forecasts applicable to scheduling radio observations for up to 10 days into the future. Additionally, the algorithms embedded in the data processing pipeline use historical values of the forecasted opacity to calibrate observations. Until recently, we have concentrated on predictions for high frequency (> 15 GHz) observing, as these need to be scheduled carefully around bad <span class="hlt">weather</span>. We have been using simple <span class="hlt">models</span> for the contribution of rain and clouds since we only schedule low-frequency observations under these conditions. In this project, we wanted to improve the scheduling of the GBT and data calibration at low frequencies by deriving better algorithms for clouds and rain. To address the limitation at low frequency, the observatory acquired a Radiometrics Corporation MP-1500A radiometer, which operates in 27 channels between 22 and 30 GHz. By comparing 16 months of measurements from the radiometer against forecasted <span class="hlt">system</span> temperatures, we have confirmed that forecasted <span class="hlt">system</span> temperatures are indistinguishable from those measured under good <span class="hlt">weather</span> conditions. Small miss-calibrations of the radiometer data dominate the comparison. By using recalibrated radiometer measurements, we looked at bad <span class="hlt">weather</span> days to derive better <span class="hlt">models</span> for forecasting the</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/20110018181','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/20110018181"><span><span class="hlt">Modeling</span> <span class="hlt">Weather</span> Impact on Ground Delay Programs</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Wang, Yao; Kulkarni, Deepak</p> <p>2011-01-01</p> <p>Scheduled arriving aircraft demand may exceed airport arrival capacity when there is abnormal <span class="hlt">weather</span> at an airport. In such situations, Federal Aviation Administration (FAA) institutes ground-delay programs (GDP) to delay flights before they depart from their originating airports. Efficient GDP planning depends on the accuracy of prediction of airport capacity and demand in the presence of uncertainties in <span class="hlt">weather</span> forecast. This paper presents a study of the impact of dynamic airport surface <span class="hlt">weather</span> on GDPs. Using the National Traffic Management Log, effect of <span class="hlt">weather</span> conditions on the characteristics of GDP events at selected busy airports is investigated. Two machine learning methods are used to generate <span class="hlt">models</span> that map the airport operational conditions and <span class="hlt">weather</span> information to issued GDP parameters and results of validation tests are described.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/19750004205','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/19750004205"><span><span class="hlt">Systems</span> Study of an Automated Fire <span class="hlt">Weather</span> Data <span class="hlt">System</span></span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Nishioka, K.</p> <p>1974-01-01</p> <p>A sensor <span class="hlt">system</span> applicable to an automated <span class="hlt">weather</span> station was developed. The sensor provides automated fire <span class="hlt">weather</span> data which correlates with manual readings. The equipment and methods are applied as an aid to the surveillance and protection of wildlands from fire damage. The continuous readings provided by the sensor <span class="hlt">system</span> make it possible to determine the periods of time that the wilderness areas should be closed to the public to minimize the possibilities of fire.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/19880015726','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/19880015726"><span>General-aviation's view of progress in the aviation <span class="hlt">weather</span> <span class="hlt">system</span></span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Lundgren, Douglas J.</p> <p>1988-01-01</p> <p>For all its activity statistics, general-aviation is the most vulnerable to hazardous <span class="hlt">weather</span>. Of concern to the general aviation industry are: (1) the slow pace of getting units of the Automated <span class="hlt">Weather</span> Observation <span class="hlt">System</span> (AWOS) to the field; (2) the efforts of the National <span class="hlt">Weather</span> Service to withdraw from both the observation and dissemination roles of the aviation <span class="hlt">weather</span> <span class="hlt">system</span>; (3) the need for more observation points to improve the accuracy of terminal and area forecasts; (4) the need for improvements in all area forecasts, terminal forecasts, and winds aloft forecasts; (5) slow progress in cockpit <span class="hlt">weather</span> displays; (6) the erosion of transcribed <span class="hlt">weather</span> broadcasts (TWEB) and other deficiencies in <span class="hlt">weather</span> information dissemination; (7) the need to push to make the Direct User Access Terminal (DUAT) a reality; and (7) the need to improve severe <span class="hlt">weather</span> (thunderstorm) warning <span class="hlt">systems</span>.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2014AGUFMGC41H..05C','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2014AGUFMGC41H..05C"><span>Advances in Optimizing <span class="hlt">Weather</span> Driven Electric Power <span class="hlt">Systems</span>.</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Clack, C.; MacDonald, A. E.; Alexander, A.; Dunbar, A. D.; Xie, Y.; Wilczak, J. M.</p> <p>2014-12-01</p> <p>The importance of <span class="hlt">weather</span>-driven renewable energies for the United States (and global) energy portfolio is growing. The main perceived problems with <span class="hlt">weather</span>-driven renewable energies are their intermittent nature, low power density, and high costs. The National Energy with <span class="hlt">Weather</span> <span class="hlt">System</span> Simulator (NEWS) is a mathematical optimization tool that allows the construction of <span class="hlt">weather</span>-driven energy sources that will work in harmony with the needs of the <span class="hlt">system</span>. For example, it will match the electric load, reduce variability, decrease costs, and abate carbon emissions. One important test run included existing US carbon-free power sources, natural gas power when needed, and a High Voltage Direct Current power transmission network. This study shows that the costs and carbon emissions from an optimally designed national <span class="hlt">system</span> decrease with geographic size. It shows that with achievable estimates of wind and solar generation costs, that the US could decrease its carbon emissions by up to 80% by the early 2030s, without an increase in electric costs. The key requirement would be a 48 state network of HVDC transmission, creating a national market for electricity not possible in the current AC grid. These results were found without the need for storage. Further, we tested the effect of changing natural gas fuel prices on the optimal configuration of the national electric power <span class="hlt">system</span>. Another test that was carried out was an extension to global regions. The extension study shows that the same properties found in the US study extend to the most populous regions of the planet. The extra test is a simplified version of the US study, and is where much more research can be carried out. We compare our results to other <span class="hlt">model</span> results.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2013EGUGA..15.7300D','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2013EGUGA..15.7300D"><span>Linking the <span class="hlt">Weather</span> Generator with Regional Climate <span class="hlt">Model</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Dubrovsky, Martin; Farda, Ales; Skalak, Petr; Huth, Radan</p> <p>2013-04-01</p> <p>One of the downscaling approaches, which transform the raw outputs from the climate <span class="hlt">models</span> (GCMs or RCMs) into data with more realistic structure, is based on linking the stochastic <span class="hlt">weather</span> generator with the climate <span class="hlt">model</span> output. The present contribution, in which the parametric daily surface <span class="hlt">weather</span> generator (WG) M&Rfi is linked to the RCM output, follows two aims: (1) Validation of the new simulations of the present climate (1961-1990) made by the ALADIN-Climate Regional Climate <span class="hlt">Model</span> at 25 km resolution. The WG parameters are derived from the RCM-simulated surface <span class="hlt">weather</span> series and compared to those derived from <span class="hlt">weather</span> series observed in 125 Czech meteorological stations. The set of WG parameters will include statistics of the surface temperature and precipitation series (including probability of wet day occurrence). (2) Presenting a methodology for linking the WG with RCM output. This methodology, which is based on merging information from observations and RCM, may be interpreted as a downscaling procedure, whose product is a gridded WG capable of producing realistic synthetic multivariate <span class="hlt">weather</span> series for <span class="hlt">weather</span>-ungauged locations. In this procedure, WG is calibrated with RCM-simulated multi-variate <span class="hlt">weather</span> series in the first step, and the grid specific WG parameters are then de-biased by spatially interpolated correction factors based on comparison of WG parameters calibrated with gridded RCM <span class="hlt">weather</span> series and spatially scarcer observations. The quality of the <span class="hlt">weather</span> series produced by the resultant gridded WG will be assessed in terms of selected climatic characteristics (focusing on characteristics related to variability and extremes of surface temperature and precipitation). Acknowledgements: The present experiment is made within the frame of projects ALARO-Climate (project P209/11/2405 sponsored by the Czech Science Foundation), WG4VALUE (project LD12029 sponsored by the Ministry of Education, Youth and Sports of CR) and VALUE (COST ES 1102</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2018SPIE10710E..1SS','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2018SPIE10710E..1SS"><span>Design of all-<span class="hlt">weather</span> celestial navigation <span class="hlt">system</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Sun, Hongchi; Mu, Rongjun; Du, Huajun; Wu, Peng</p> <p>2018-03-01</p> <p>In order to realize autonomous navigation in the atmosphere, an all-<span class="hlt">weather</span> celestial navigation <span class="hlt">system</span> is designed. The research of celestial navigation <span class="hlt">system</span> include discrimination method of comentropy and the adaptive navigation algorithm based on the P value. The discrimination method of comentropy is studied to realize the independent switching of two celestial navigation modes, starlight and radio. Finally, an adaptive filtering algorithm based on P value is proposed, which can greatly improve the disturbance rejection capability of the <span class="hlt">system</span>. The experimental results show that the accuracy of the three axis attitude is better than 10″, and it can work all <span class="hlt">weather</span>. In perturbation environment, the position accuracy of the integrated navigation <span class="hlt">system</span> can be increased 20% comparing with the traditional method. It basically meets the requirements of the all-<span class="hlt">weather</span> celestial navigation <span class="hlt">system</span>, and it has the ability of stability, reliability, high accuracy and strong anti-interference.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/28530231','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/28530231"><span>Constraining climate sensitivity and continental versus seafloor <span class="hlt">weathering</span> using an inverse geological carbon cycle <span class="hlt">model</span>.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Krissansen-Totton, Joshua; Catling, David C</p> <p>2017-05-22</p> <p>The relative influences of tectonics, continental <span class="hlt">weathering</span> and seafloor <span class="hlt">weathering</span> in controlling the geological carbon cycle are unknown. Here we develop a new carbon cycle <span class="hlt">model</span> that explicitly captures the kinetics of seafloor <span class="hlt">weathering</span> to investigate carbon fluxes and the evolution of atmospheric CO 2 and ocean pH since 100 Myr ago. We compare <span class="hlt">model</span> outputs to proxy data, and rigorously constrain <span class="hlt">model</span> parameters using Bayesian inverse methods. Assuming our forward <span class="hlt">model</span> is an accurate representation of the carbon cycle, to fit proxies the temperature dependence of continental <span class="hlt">weathering</span> must be weaker than commonly assumed. We find that 15-31 °C (1σ) surface warming is required to double the continental <span class="hlt">weathering</span> flux, versus 3-10 °C in previous work. In addition, continental <span class="hlt">weatherability</span> has increased 1.7-3.3 times since 100 Myr ago, demanding explanation by uplift and sea-level changes. The average Earth <span class="hlt">system</span> climate sensitivity is  K (1σ) per CO 2 doubling, which is notably higher than fast-feedback estimates. These conclusions are robust to assumptions about outgassing, modern fluxes and seafloor <span class="hlt">weathering</span> kinetics.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=5458154','PMC'); return false;" href="https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=5458154"><span>Constraining climate sensitivity and continental versus seafloor <span class="hlt">weathering</span> using an inverse geological carbon cycle <span class="hlt">model</span></span></a></p> <p><a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pmc">PubMed Central</a></p> <p>Krissansen-Totton, Joshua; Catling, David C.</p> <p>2017-01-01</p> <p>The relative influences of tectonics, continental <span class="hlt">weathering</span> and seafloor <span class="hlt">weathering</span> in controlling the geological carbon cycle are unknown. Here we develop a new carbon cycle <span class="hlt">model</span> that explicitly captures the kinetics of seafloor <span class="hlt">weathering</span> to investigate carbon fluxes and the evolution of atmospheric CO2 and ocean pH since 100 Myr ago. We compare <span class="hlt">model</span> outputs to proxy data, and rigorously constrain <span class="hlt">model</span> parameters using Bayesian inverse methods. Assuming our forward <span class="hlt">model</span> is an accurate representation of the carbon cycle, to fit proxies the temperature dependence of continental <span class="hlt">weathering</span> must be weaker than commonly assumed. We find that 15–31 °C (1σ) surface warming is required to double the continental <span class="hlt">weathering</span> flux, versus 3–10 °C in previous work. In addition, continental <span class="hlt">weatherability</span> has increased 1.7–3.3 times since 100 Myr ago, demanding explanation by uplift and sea-level changes. The average Earth <span class="hlt">system</span> climate sensitivity is  K (1σ) per CO2 doubling, which is notably higher than fast-feedback estimates. These conclusions are robust to assumptions about outgassing, modern fluxes and seafloor <span class="hlt">weathering</span> kinetics. PMID:28530231</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/20170011239','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/20170011239"><span><span class="hlt">Models</span> of Sector Flows Under Local, Regional and Airport <span class="hlt">Weather</span> Constraints</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Kulkarni, Deepak</p> <p>2017-01-01</p> <p>Recently, the ATM community has made important progress in collaborative trajectory management through the introduction of a new FAA traffic management initiative called a Collaborative Trajectory Options Program (CTOP). FAA can use CTOPs to manage air traffic under multiple constraints (manifested as flow constrained areas or FCAs) in the <span class="hlt">system</span>, and it allows flight operators to indicate their preferences for routing and delay options. CTOPs also permits better management of the overall trajectory of flights by considering both routing and departure delay options simultaneously. However, adoption of CTOPs in airspace has been hampered by many factors that include challenges in how to identify constrained areas and how to set rates for the FCAs. Decision support tools providing assistance would be particularly helpful in effective use of CTOPs. Such DSTs tools would need <span class="hlt">models</span> of demand and capacity in the presence of multiple constraints. This study examines different approaches to using historical data to create and validate <span class="hlt">models</span> of maximum flows in sectors and other airspace regions in the presence of multiple constraints. A challenge in creating an empirical <span class="hlt">model</span> of flows under multiple constraints is a lack of sufficient historical data that captures diverse situations involving combinations of multiple constraints especially those with severe <span class="hlt">weather</span>. The approach taken here to deal with this is two-fold. First, we create a generalized sector <span class="hlt">model</span> encompassing multiple sectors rather than individual sectors in order to increase the amount of data used for creating the <span class="hlt">model</span> by an order of magnitude. Secondly, we decompose the problem so that the amount of data needed is reduced. This involves creating a baseline demand <span class="hlt">model</span> plus a separate <span class="hlt">weather</span> constrained flow reduction <span class="hlt">model</span> and then composing these into a single integrated <span class="hlt">model</span>. A nominal demand <span class="hlt">model</span> is a flow <span class="hlt">model</span> (gdem) in the presence of clear local <span class="hlt">weather</span>. This defines the flow as a</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2010cosp...38.4169J','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2010cosp...38.4169J"><span>Operational Numerical <span class="hlt">Weather</span> Prediction at the Met Office and potential ways forward for operational space <span class="hlt">weather</span> prediction <span class="hlt">systems</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Jackson, David</p> <p></p> <p>NICT (National Institute of Information and Communications Technology) has been in charge of space <span class="hlt">weather</span> forecast service in Japan for more than 20 years. The main target region of the space <span class="hlt">weather</span> is the geo-space in the vicinity of the Earth where human activities are dominant. In the geo-space, serious damages of satellites, international space stations and astronauts take place caused by energetic particles or electromagnetic disturbances: the origin of the causes is dynamically changing of solar activities. Positioning <span class="hlt">systems</span> via GPS satellites are also im-portant recently. Since the most significant effect of positioning error comes from disturbances of the ionosphere, it is crucial to estimate time-dependent modulation of the electron density profiles in the ionosphere. NICT is one of the 13 members of the ISES (International Space Environment Service), which is an international assembly of space <span class="hlt">weather</span> forecast centers under the UNESCO. With help of geo-space environment data exchanging among the member nations, NICT operates daily space <span class="hlt">weather</span> forecast service every day to provide informa-tion on forecasts of solar flare, geomagnetic disturbances, solar proton event, and radio-wave propagation conditions in the ionosphere. The space <span class="hlt">weather</span> forecast at NICT is conducted based on the three methodologies: observations, simulations and informatics (OSI <span class="hlt">model</span>). For real-time or quasi real-time reporting of space <span class="hlt">weather</span>, we conduct our original observations: Hiraiso solar observatory to monitor the solar activity (solar flare, coronal mass ejection, and so on), domestic ionosonde network, magnetometer HF radar observations in far-east Siberia, and south-east Asia low-latitude ionosonde network (SEALION). Real-time observation data to monitor solar and solar-wind activities are obtained through antennae at NICT from ACE and STEREO satellites. We have a middle-class super-computer (NEC SX-8R) to maintain real-time computer simulations for solar and solar</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2014ASPC..485..103B','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2014ASPC..485..103B"><span>Introduction to the Space <span class="hlt">Weather</span> Monitoring <span class="hlt">System</span> at KASI</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Baek, J.; Choi, S.; Kim, Y.; Cho, K.; Bong, S.; Lee, J.; Kwak, Y.; Hwang, J.; Park, Y.; Hwang, E.</p> <p>2014-05-01</p> <p>We have developed the Space <span class="hlt">Weather</span> Monitoring <span class="hlt">System</span> (SWMS) at the Korea Astronomy and Space Science Institute (KASI). Since 2007, the <span class="hlt">system</span> has continuously evolved into a better <span class="hlt">system</span>. The SWMS consists of several subsystems: applications which acquire and process observational data, servers which run the applications, data storage, and display facilities which show the space <span class="hlt">weather</span> information. The applications collect solar and space <span class="hlt">weather</span> data from domestic and oversea sites. The collected data are converted to other format and/or visualized in real time as graphs and illustrations. We manage 3 data acquisition and processing servers, a file service server, a web server, and 3 sets of storage <span class="hlt">systems</span>. We have developed 30 applications for a variety of data, and the volume of data is about 5.5 GB per day. We provide our customers with space <span class="hlt">weather</span> contents displayed at the Space <span class="hlt">Weather</span> Monitoring Lab (SWML) using web services.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/1986PhDT.......138S','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/1986PhDT.......138S"><span>a <span class="hlt">Weather</span> Monitoring <span class="hlt">System</span> for Application to Apple and Corn Production</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Stirm, Walter Leroy</p> <p></p> <p>Many crop management decisions are based on <span class="hlt">weather</span> -crop development relationships. Daily <span class="hlt">weather</span> data is currently used in most crop development research and applied <span class="hlt">models</span>. Present <span class="hlt">weather</span> and computer technology now makes possible monitoring of crop development on a realtime basis. This research tests a method of computing crop sensitive temperatures for corn and apple using standard hourly meteorological data. The method also makes use of detailed plant physiological stage measurements to determine timing of vital cultural operations tied to the observed <span class="hlt">weather</span> conditions. The sensitive temperature method incorporates very short term <span class="hlt">weather</span> variability accounting for changes in the cloud cover, radiation rates, evaporative cooling and other factors involved in the plant's energy balance. The relationship of plant and <span class="hlt">weather</span> measurements are also used to determine corn emergence, corn grain drydown rate and fruit harvest duration. The monitoring <span class="hlt">system</span> also incorporates a crop growth unit forecast technique employing short and medium range temperature forecasts of the National <span class="hlt">Weather</span> Service. The projections of growth units are made for five and ten days into the future. Predicted growth unit accumulations are compared to historical growth unit accumulations to determine the forecast stage. The sensitive temperature crop monitoring <span class="hlt">system</span> removes some of the error involved in evaluation of growth units by average daily temperature. Carry over maximum and minimums, extended duration of warm or cool periods within the day and disruption of diurnal temperature curve by passage of fronts are eliminated.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2002EGSGA..27.4968H','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2002EGSGA..27.4968H"><span>Space <span class="hlt">Weather</span> <span class="hlt">Model</span> Testing And Validation At The Community Coordinated <span class="hlt">Modeling</span> Center</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Hesse, M.; Kuznetsova, M.; Rastaetter, L.; Falasca, A.; Keller, K.; Reitan, P.</p> <p></p> <p>The Community Coordinated <span class="hlt">Modeling</span> Center (CCMC) is a multi-agency partner- ship aimed at the creation of next generation space <span class="hlt">weather</span> <span class="hlt">models</span>. The goal of the CCMC is to undertake the research and developmental work necessary to substantially increase the present-day <span class="hlt">modeling</span> capability for space <span class="hlt">weather</span> purposes, and to pro- vide <span class="hlt">models</span> for transition to the rapid prototyping centers at the space <span class="hlt">weather</span> forecast centers. This goal requires close collaborations with and substantial involvement of the research community. The physical regions to be addressed by CCMC-related activities range from the solar atmosphere to the Earth's upper atmosphere. The CCMC is an integral part of NASA's Living With aStar initiative, of the National Space <span class="hlt">Weather</span> Program Implementation Plan, and of the Department of Defense Space <span class="hlt">Weather</span> Tran- sition Plan. CCMC includes a facility at NASA Goddard Space Flight Center, as well as distributed computing facilities provided by the Air Force. CCMC also provides, to the research community, access to state-of-the-art space research <span class="hlt">models</span>. In this paper we will provide updates on CCMC status, on current plans, research and devel- opment accomplishments and goals, and on the <span class="hlt">model</span> testing and validation process undertaken as part of the CCMC mandate.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/20130009987','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/20130009987"><span><span class="hlt">Weather</span> Research and Forecasting <span class="hlt">Model</span> Sensitivity Comparisons for Warm Season Convective Initiation</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Watson, Leela R.; Hoeth, Brian; Blottman, Peter F.</p> <p>2007-01-01</p> <p>Mesoscale <span class="hlt">weather</span> conditions can significantly affect the space launch and landing operations at Kennedy Space Center (KSC) and Cape Canaveral Air Force Station (CCAFS). During the summer months, land-sea interactions that occur across KSC and CCAFS lead to the formation of a sea breeze, which can then spawn deep convection. These convective processes often last 60 minutes or less and pose a significant challenge to the forecasters at the National <span class="hlt">Weather</span> Service (NWS) Spaceflight Meteorology Group (SMG). The main challenge is that a "GO" forecast for thunderstorms and precipitation is required at the 90 minute deorbit decision for End Of Mission (EOM) and at the 30 minute Return To Launch Site (RTLS) decision at the Shuttle Landing Facility. Convective initiation, timing, and mode also present a forecast challenge for the NWS in Melbourne, FL (MLB). The NWS MLB issues such tactical forecast information as Terminal Aerodrome Forecasts (TAFs), Spot Forecasts for fire <span class="hlt">weather</span> and hazardous materials incident support, and severe/hazardous <span class="hlt">weather</span> Watches, Warnings, and Advisories. Lastly, these forecasting challenges can also affect the 45th <span class="hlt">Weather</span> Squadron (45 WS), which provides comprehensive <span class="hlt">weather</span> forecasts for shuttle launch, as well as ground operations, at KSC and CCAFS. The need for accurate mesoscale <span class="hlt">model</span> forecasts to aid in their decision making is crucial. Both the SMG and the MLB are currently implementing the <span class="hlt">Weather</span> Research and Forecasting Environmental <span class="hlt">Modeling</span> <span class="hlt">System</span> (WRF EMS) software into their operations. The WRF EMS software allows users to employ both dynamical cores - the Advanced Research WRF (ARW) and the Non-hydrostatic Mesoscale <span class="hlt">Model</span> (NMM). There are also data assimilation analysis packages available for the initialization of the WRF <span class="hlt">model</span>- the Local Analysis and Prediction <span class="hlt">System</span> (LAPS) and the Advanced Regional Prediction <span class="hlt">System</span> (ARPS) Data Analysis <span class="hlt">System</span> (ADAS). Having a series of initialization options and WRF cores, as well as many</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/CFR-2010-title14-vol1/pdf/CFR-2010-title14-vol1-sec27-961.pdf','CFR'); return false;" href="https://www.gpo.gov/fdsys/pkg/CFR-2010-title14-vol1/pdf/CFR-2010-title14-vol1-sec27-961.pdf"><span>14 CFR 27.961 - Fuel <span class="hlt">system</span> hot <span class="hlt">weather</span> operation.</span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collectionCfr.action?selectedYearFrom=2010&page.go=Go">Code of Federal Regulations, 2010 CFR</a></p> <p></p> <p>2010-01-01</p> <p>... AIRCRAFT AIRWORTHINESS STANDARDS: NORMAL CATEGORY ROTORCRAFT Powerplant Fuel <span class="hlt">System</span> § 27.961 Fuel <span class="hlt">system</span> hot <span class="hlt">weather</span> operation. Each suction lift fuel <span class="hlt">system</span> and other fuel <span class="hlt">systems</span> with features conducive to... 14 Aeronautics and Space 1 2010-01-01 2010-01-01 false Fuel <span class="hlt">system</span> hot <span class="hlt">weather</span> operation. 27.961...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/CFR-2011-title14-vol1/pdf/CFR-2011-title14-vol1-sec27-961.pdf','CFR2011'); return false;" href="https://www.gpo.gov/fdsys/pkg/CFR-2011-title14-vol1/pdf/CFR-2011-title14-vol1-sec27-961.pdf"><span>14 CFR 27.961 - Fuel <span class="hlt">system</span> hot <span class="hlt">weather</span> operation.</span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collectionCfr.action?selectedYearFrom=2011&page.go=Go">Code of Federal Regulations, 2011 CFR</a></p> <p></p> <p>2011-01-01</p> <p>... AIRCRAFT AIRWORTHINESS STANDARDS: NORMAL CATEGORY ROTORCRAFT Powerplant Fuel <span class="hlt">System</span> § 27.961 Fuel <span class="hlt">system</span> hot <span class="hlt">weather</span> operation. Each suction lift fuel <span class="hlt">system</span> and other fuel <span class="hlt">systems</span> with features conducive to... 14 Aeronautics and Space 1 2011-01-01 2011-01-01 false Fuel <span class="hlt">system</span> hot <span class="hlt">weather</span> operation. 27.961...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/CFR-2013-title14-vol1/pdf/CFR-2013-title14-vol1-sec29-961.pdf','CFR2013'); return false;" href="https://www.gpo.gov/fdsys/pkg/CFR-2013-title14-vol1/pdf/CFR-2013-title14-vol1-sec29-961.pdf"><span>14 CFR 29.961 - Fuel <span class="hlt">system</span> hot <span class="hlt">weather</span> operation.</span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collectionCfr.action?selectedYearFrom=2013&page.go=Go">Code of Federal Regulations, 2013 CFR</a></p> <p></p> <p>2013-01-01</p> <p>... AIRCRAFT AIRWORTHINESS STANDARDS: TRANSPORT CATEGORY ROTORCRAFT Powerplant Fuel <span class="hlt">System</span> § 29.961 Fuel <span class="hlt">system</span> hot <span class="hlt">weather</span> operation. Each suction lift fuel <span class="hlt">system</span> and other fuel <span class="hlt">systems</span> conducive to vapor... 14 Aeronautics and Space 1 2013-01-01 2013-01-01 false Fuel <span class="hlt">system</span> hot <span class="hlt">weather</span> operation. 29.961...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/CFR-2014-title14-vol1/pdf/CFR-2014-title14-vol1-sec27-961.pdf','CFR2014'); return false;" href="https://www.gpo.gov/fdsys/pkg/CFR-2014-title14-vol1/pdf/CFR-2014-title14-vol1-sec27-961.pdf"><span>14 CFR 27.961 - Fuel <span class="hlt">system</span> hot <span class="hlt">weather</span> operation.</span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collectionCfr.action?selectedYearFrom=2014&page.go=Go">Code of Federal Regulations, 2014 CFR</a></p> <p></p> <p>2014-01-01</p> <p>... AIRCRAFT AIRWORTHINESS STANDARDS: NORMAL CATEGORY ROTORCRAFT Powerplant Fuel <span class="hlt">System</span> § 27.961 Fuel <span class="hlt">system</span> hot <span class="hlt">weather</span> operation. Each suction lift fuel <span class="hlt">system</span> and other fuel <span class="hlt">systems</span> with features conducive to... 14 Aeronautics and Space 1 2014-01-01 2014-01-01 false Fuel <span class="hlt">system</span> hot <span class="hlt">weather</span> operation. 27.961...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/CFR-2012-title14-vol1/pdf/CFR-2012-title14-vol1-sec27-961.pdf','CFR2012'); return false;" href="https://www.gpo.gov/fdsys/pkg/CFR-2012-title14-vol1/pdf/CFR-2012-title14-vol1-sec27-961.pdf"><span>14 CFR 27.961 - Fuel <span class="hlt">system</span> hot <span class="hlt">weather</span> operation.</span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collectionCfr.action?selectedYearFrom=2012&page.go=Go">Code of Federal Regulations, 2012 CFR</a></p> <p></p> <p>2012-01-01</p> <p>... AIRCRAFT AIRWORTHINESS STANDARDS: NORMAL CATEGORY ROTORCRAFT Powerplant Fuel <span class="hlt">System</span> § 27.961 Fuel <span class="hlt">system</span> hot <span class="hlt">weather</span> operation. Each suction lift fuel <span class="hlt">system</span> and other fuel <span class="hlt">systems</span> with features conducive to... 14 Aeronautics and Space 1 2012-01-01 2012-01-01 false Fuel <span class="hlt">system</span> hot <span class="hlt">weather</span> operation. 27.961...</p> </li> </ol> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_4");'>4</a></li> <li><a href="#" onclick='return showDiv("page_5");'>5</a></li> <li class="active"><span>6</span></li> <li><a href="#" onclick='return showDiv("page_7");'>7</a></li> <li><a href="#" onclick='return showDiv("page_8");'>8</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div><!-- col-sm-12 --> </div><!-- row --> </div><!-- page_6 --> <div id="page_7" class="hiddenDiv"> <div class="row"> <div class="col-sm-12"> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_5");'>5</a></li> <li><a href="#" onclick='return showDiv("page_6");'>6</a></li> <li class="active"><span>7</span></li> <li><a href="#" onclick='return showDiv("page_8");'>8</a></li> <li><a href="#" onclick='return showDiv("page_9");'>9</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div> </div> <div class="row"> <div class="col-sm-12"> <ol class="result-class" start="121"> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/CFR-2011-title14-vol1/pdf/CFR-2011-title14-vol1-sec29-961.pdf','CFR2011'); return false;" href="https://www.gpo.gov/fdsys/pkg/CFR-2011-title14-vol1/pdf/CFR-2011-title14-vol1-sec29-961.pdf"><span>14 CFR 29.961 - Fuel <span class="hlt">system</span> hot <span class="hlt">weather</span> operation.</span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collectionCfr.action?selectedYearFrom=2011&page.go=Go">Code of Federal Regulations, 2011 CFR</a></p> <p></p> <p>2011-01-01</p> <p>... AIRCRAFT AIRWORTHINESS STANDARDS: TRANSPORT CATEGORY ROTORCRAFT Powerplant Fuel <span class="hlt">System</span> § 29.961 Fuel <span class="hlt">system</span> hot <span class="hlt">weather</span> operation. Each suction lift fuel <span class="hlt">system</span> and other fuel <span class="hlt">systems</span> conducive to vapor... 14 Aeronautics and Space 1 2011-01-01 2011-01-01 false Fuel <span class="hlt">system</span> hot <span class="hlt">weather</span> operation. 29.961...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/CFR-2013-title14-vol1/pdf/CFR-2013-title14-vol1-sec27-961.pdf','CFR2013'); return false;" href="https://www.gpo.gov/fdsys/pkg/CFR-2013-title14-vol1/pdf/CFR-2013-title14-vol1-sec27-961.pdf"><span>14 CFR 27.961 - Fuel <span class="hlt">system</span> hot <span class="hlt">weather</span> operation.</span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collectionCfr.action?selectedYearFrom=2013&page.go=Go">Code of Federal Regulations, 2013 CFR</a></p> <p></p> <p>2013-01-01</p> <p>... AIRCRAFT AIRWORTHINESS STANDARDS: NORMAL CATEGORY ROTORCRAFT Powerplant Fuel <span class="hlt">System</span> § 27.961 Fuel <span class="hlt">system</span> hot <span class="hlt">weather</span> operation. Each suction lift fuel <span class="hlt">system</span> and other fuel <span class="hlt">systems</span> with features conducive to... 14 Aeronautics and Space 1 2013-01-01 2013-01-01 false Fuel <span class="hlt">system</span> hot <span class="hlt">weather</span> operation. 27.961...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/CFR-2014-title14-vol1/pdf/CFR-2014-title14-vol1-sec29-961.pdf','CFR2014'); return false;" href="https://www.gpo.gov/fdsys/pkg/CFR-2014-title14-vol1/pdf/CFR-2014-title14-vol1-sec29-961.pdf"><span>14 CFR 29.961 - Fuel <span class="hlt">system</span> hot <span class="hlt">weather</span> operation.</span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collectionCfr.action?selectedYearFrom=2014&page.go=Go">Code of Federal Regulations, 2014 CFR</a></p> <p></p> <p>2014-01-01</p> <p>... AIRCRAFT AIRWORTHINESS STANDARDS: TRANSPORT CATEGORY ROTORCRAFT Powerplant Fuel <span class="hlt">System</span> § 29.961 Fuel <span class="hlt">system</span> hot <span class="hlt">weather</span> operation. Each suction lift fuel <span class="hlt">system</span> and other fuel <span class="hlt">systems</span> conducive to vapor... 14 Aeronautics and Space 1 2014-01-01 2014-01-01 false Fuel <span class="hlt">system</span> hot <span class="hlt">weather</span> operation. 29.961...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/CFR-2010-title14-vol1/pdf/CFR-2010-title14-vol1-sec29-961.pdf','CFR'); return false;" href="https://www.gpo.gov/fdsys/pkg/CFR-2010-title14-vol1/pdf/CFR-2010-title14-vol1-sec29-961.pdf"><span>14 CFR 29.961 - Fuel <span class="hlt">system</span> hot <span class="hlt">weather</span> operation.</span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collectionCfr.action?selectedYearFrom=2010&page.go=Go">Code of Federal Regulations, 2010 CFR</a></p> <p></p> <p>2010-01-01</p> <p>... AIRCRAFT AIRWORTHINESS STANDARDS: TRANSPORT CATEGORY ROTORCRAFT Powerplant Fuel <span class="hlt">System</span> § 29.961 Fuel <span class="hlt">system</span> hot <span class="hlt">weather</span> operation. Each suction lift fuel <span class="hlt">system</span> and other fuel <span class="hlt">systems</span> conducive to vapor... 14 Aeronautics and Space 1 2010-01-01 2010-01-01 false Fuel <span class="hlt">system</span> hot <span class="hlt">weather</span> operation. 29.961...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/CFR-2012-title14-vol1/pdf/CFR-2012-title14-vol1-sec29-961.pdf','CFR2012'); return false;" href="https://www.gpo.gov/fdsys/pkg/CFR-2012-title14-vol1/pdf/CFR-2012-title14-vol1-sec29-961.pdf"><span>14 CFR 29.961 - Fuel <span class="hlt">system</span> hot <span class="hlt">weather</span> operation.</span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collectionCfr.action?selectedYearFrom=2012&page.go=Go">Code of Federal Regulations, 2012 CFR</a></p> <p></p> <p>2012-01-01</p> <p>... AIRCRAFT AIRWORTHINESS STANDARDS: TRANSPORT CATEGORY ROTORCRAFT Powerplant Fuel <span class="hlt">System</span> § 29.961 Fuel <span class="hlt">system</span> hot <span class="hlt">weather</span> operation. Each suction lift fuel <span class="hlt">system</span> and other fuel <span class="hlt">systems</span> conducive to vapor... 14 Aeronautics and Space 1 2012-01-01 2012-01-01 false Fuel <span class="hlt">system</span> hot <span class="hlt">weather</span> operation. 29.961...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://rosap.ntl.bts.gov/view/dot/32902','DOTNTL'); return false;" href="https://rosap.ntl.bts.gov/view/dot/32902"><span>Assessment of Montana road <span class="hlt">weather</span> information <span class="hlt">system</span> : final report</span></a></p> <p><a target="_blank" href="http://ntlsearch.bts.gov/tris/index.do">DOT National Transportation Integrated Search</a></p> <p></p> <p>2017-01-01</p> <p><span class="hlt">Weather</span> presents considerable challenges to highway agencies both in terms of safety and operations. State transportation agencies have developed road <span class="hlt">weather</span> information <span class="hlt">systems</span> (RWIS) to address such challenges. Road <span class="hlt">weather</span> information has been us...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/20110011476','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/20110011476"><span>Anvil Forecast Tool in the Advanced <span class="hlt">Weather</span> Interactive Processing <span class="hlt">System</span> (AWIPS)</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Barrett, Joe H., III; Hood, Doris</p> <p>2009-01-01</p> <p>Launch <span class="hlt">Weather</span> Officers (LWOs) from the 45th <span class="hlt">Weather</span> Squadron (45 WS) and forecasters from the National <span class="hlt">Weather</span> Service (NWS) Spaceflight Meteorology Group (SMG) have identified anvil forecasting as one of their most challenging tasks when predicting the probability of violating the Lightning Launch Commit Criteria (LLCC) (Krider et al. 2006; Space Shuttle Flight Rules (FR), NASA/JSC 2004)). As a result, the Applied Meteorology Unit (AMU) developed a tool that creates an anvil threat corridor graphic that can be overlaid on satellite imagery using the Meteorological Interactive Data Display <span class="hlt">System</span> (MIDDS, Short and Wheeler, 2002). The tool helps forecasters estimate the locations of thunderstorm anvils at one, two, and three hours into the future. It has been used extensively in launch and landing operations by both the 45 WS and SMG. The Advanced <span class="hlt">Weather</span> Interactive Processing <span class="hlt">System</span> (AWIPS) is now used along with MIDDS for <span class="hlt">weather</span> analysis and display at SMG. In Phase I of this task, SMG tasked the AMU to transition the tool from MIDDS to AWIPS (Barrett et aI., 2007). For Phase II, SMG requested the AMU make the Anvil Forecast Tool in AWIPS more configurable by creating the capability to read <span class="hlt">model</span> gridded data from user-defined <span class="hlt">model</span> files instead of hard-coded files. An NWS local AWIPS application called AGRID was used to accomplish this. In addition, SMG needed to be able to define the pressure levels for the <span class="hlt">model</span> data, instead of hard-coding the bottom level as 300 mb and the top level as 150 mb. This paper describes the initial development of the Anvil Forecast Tool for MIDDS, followed by the migration of the tool to AWIPS in Phase I. It then gives a detailed presentation of the Phase II improvements to the AWIPS tool.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://www.nws.noaa.gov/safety.php','SCIGOVWS'); return false;" href="http://www.nws.noaa.gov/safety.php"><span><span class="hlt">Weather</span> Safety - NOAA's National <span class="hlt">Weather</span> Service</span></a></p> <p><a target="_blank" href="http://www.science.gov/aboutsearch.html">Science.gov Websites</a></p> <p></p> <p></p> <p>Statistical <span class="hlt">Models</span>... MOS Prod GFS-LAMP Prod Climate Past <span class="hlt">Weather</span> Predictions <span class="hlt">Weather</span> <em>Safety</em> <span class="hlt">Weather</span> Radio National <span class="hlt">Weather</span> Service on FaceBook NWS on Facebook NWS Director Home > <em>Safety</em> <span class="hlt">Weather</span> <em>Safety</em> This page <span class="hlt">weather</span> <em>safety</em>. StormReady NOAA <span class="hlt">Weather</span> Radio Emergency Managers Information Network U.S. Hazard Assmt</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/20120015498','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/20120015498"><span>NASA GSFC Space <span class="hlt">Weather</span> Center - Innovative Space <span class="hlt">Weather</span> Dissemination: Web-Interfaces, Mobile Applications, and More</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Maddox, Marlo; Zheng, Yihua; Rastaetter, Lutz; Taktakishvili, A.; Mays, M. L.; Kuznetsova, M.; Lee, Hyesook; Chulaki, Anna; Hesse, Michael; Mullinix, Richard; <a style="text-decoration: none; " href="javascript:void(0); " onClick="displayelement('author_20120015498'); toggleEditAbsImage('author_20120015498_show'); toggleEditAbsImage('author_20120015498_hide'); "> <img style="display:inline; width:12px; height:12px; " src="images/arrow-up.gif" width="12" height="12" border="0" alt="hide" id="author_20120015498_show"> <img style="width:12px; height:12px; display:none; " src="images/arrow-down.gif" width="12" height="12" border="0" alt="hide" id="author_20120015498_hide"></p> <p>2012-01-01</p> <p>The NASA GSFC Space <span class="hlt">Weather</span> Center (http://swc.gsfc.nasa.gov) is committed to providing forecasts, alerts, research, and educational support to address NASA's space <span class="hlt">weather</span> needs - in addition to the needs of the general space <span class="hlt">weather</span> community. We provide a host of services including spacecraft anomaly resolution, historical impact analysis, real-time monitoring and forecasting, custom space <span class="hlt">weather</span> alerts and products, weekly summaries and reports, and most recently - video casts. There are many challenges in providing accurate descriptions of past, present, and expected space <span class="hlt">weather</span> events - and the Space <span class="hlt">Weather</span> Center at NASA GSFC employs several innovative solutions to provide access to a comprehensive collection of both observational data, as well as space <span class="hlt">weather</span> <span class="hlt">model</span>/simulation data. We'll describe the challenges we've faced with managing hundreds of data streams, running <span class="hlt">models</span> in real-time, data storage, and data dissemination. We'll also highlight several <span class="hlt">systems</span> and tools that are utilized by the Space <span class="hlt">Weather</span> Center in our daily operations, all of which are available to the general community as well. These <span class="hlt">systems</span> and services include a web-based application called the Integrated Space <span class="hlt">Weather</span> Analysis <span class="hlt">System</span> (iSWA http://iswa.gsfc.nasa.gov), two mobile space <span class="hlt">weather</span> applications for both IOS and Android devices, an external API for web-service style access to data, google earth compatible data products, and a downloadable client-based visualization tool.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://www.dtic.mil/docs/citations/ADA630138','DTIC-ST'); return false;" href="http://www.dtic.mil/docs/citations/ADA630138"><span>The Analysis, Numerical Simulation, and Diagnosis of Extratropical <span class="hlt">Weather</span> <span class="hlt">Systems</span></span></a></p> <p><a target="_blank" href="http://www.dtic.mil/">DTIC Science & Technology</a></p> <p></p> <p>1999-09-30</p> <p>The Analysis, Numerical Simulation, and Diagnosis of Extratropical <span class="hlt">Weather</span> <span class="hlt">Systems</span> Dr. Melvyn A. Shapiro NOAA/Environmental Technology Laboratory...formulation, and numerical prediction of the life cycles of synoptic-scale and mesoscale extratropical <span class="hlt">weather</span> <span class="hlt">systems</span>, including the influence of planetary...scale inter-annual and intra-seasonal variability on their evolution. These <span class="hlt">weather</span> <span class="hlt">systems</span> include: extratropical oceanic and land-falling cyclones</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/CFR-2011-title14-vol1/pdf/CFR-2011-title14-vol1-sec23-961.pdf','CFR2011'); return false;" href="https://www.gpo.gov/fdsys/pkg/CFR-2011-title14-vol1/pdf/CFR-2011-title14-vol1-sec23-961.pdf"><span>14 CFR 23.961 - Fuel <span class="hlt">system</span> hot <span class="hlt">weather</span> operation.</span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collectionCfr.action?selectedYearFrom=2011&page.go=Go">Code of Federal Regulations, 2011 CFR</a></p> <p></p> <p>2011-01-01</p> <p>... 14 Aeronautics and Space 1 2011-01-01 2011-01-01 false Fuel <span class="hlt">system</span> hot <span class="hlt">weather</span> operation. 23.961... AIRCRAFT AIRWORTHINESS STANDARDS: NORMAL, UTILITY, ACROBATIC, AND COMMUTER CATEGORY AIRPLANES Powerplant Fuel <span class="hlt">System</span> § 23.961 Fuel <span class="hlt">system</span> hot <span class="hlt">weather</span> operation. Each fuel <span class="hlt">system</span> must be free from vapor lock...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/CFR-2012-title14-vol1/pdf/CFR-2012-title14-vol1-sec23-961.pdf','CFR2012'); return false;" href="https://www.gpo.gov/fdsys/pkg/CFR-2012-title14-vol1/pdf/CFR-2012-title14-vol1-sec23-961.pdf"><span>14 CFR 23.961 - Fuel <span class="hlt">system</span> hot <span class="hlt">weather</span> operation.</span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collectionCfr.action?selectedYearFrom=2012&page.go=Go">Code of Federal Regulations, 2012 CFR</a></p> <p></p> <p>2012-01-01</p> <p>... 14 Aeronautics and Space 1 2012-01-01 2012-01-01 false Fuel <span class="hlt">system</span> hot <span class="hlt">weather</span> operation. 23.961... AIRCRAFT AIRWORTHINESS STANDARDS: NORMAL, UTILITY, ACROBATIC, AND COMMUTER CATEGORY AIRPLANES Powerplant Fuel <span class="hlt">System</span> § 23.961 Fuel <span class="hlt">system</span> hot <span class="hlt">weather</span> operation. Each fuel <span class="hlt">system</span> must be free from vapor lock...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/CFR-2010-title14-vol1/pdf/CFR-2010-title14-vol1-sec23-961.pdf','CFR'); return false;" href="https://www.gpo.gov/fdsys/pkg/CFR-2010-title14-vol1/pdf/CFR-2010-title14-vol1-sec23-961.pdf"><span>14 CFR 23.961 - Fuel <span class="hlt">system</span> hot <span class="hlt">weather</span> operation.</span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collectionCfr.action?selectedYearFrom=2010&page.go=Go">Code of Federal Regulations, 2010 CFR</a></p> <p></p> <p>2010-01-01</p> <p>... 14 Aeronautics and Space 1 2010-01-01 2010-01-01 false Fuel <span class="hlt">system</span> hot <span class="hlt">weather</span> operation. 23.961... AIRCRAFT AIRWORTHINESS STANDARDS: NORMAL, UTILITY, ACROBATIC, AND COMMUTER CATEGORY AIRPLANES Powerplant Fuel <span class="hlt">System</span> § 23.961 Fuel <span class="hlt">system</span> hot <span class="hlt">weather</span> operation. Each fuel <span class="hlt">system</span> must be free from vapor lock...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/CFR-2014-title14-vol1/pdf/CFR-2014-title14-vol1-sec23-961.pdf','CFR2014'); return false;" href="https://www.gpo.gov/fdsys/pkg/CFR-2014-title14-vol1/pdf/CFR-2014-title14-vol1-sec23-961.pdf"><span>14 CFR 23.961 - Fuel <span class="hlt">system</span> hot <span class="hlt">weather</span> operation.</span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collectionCfr.action?selectedYearFrom=2014&page.go=Go">Code of Federal Regulations, 2014 CFR</a></p> <p></p> <p>2014-01-01</p> <p>... 14 Aeronautics and Space 1 2014-01-01 2014-01-01 false Fuel <span class="hlt">system</span> hot <span class="hlt">weather</span> operation. 23.961... AIRCRAFT AIRWORTHINESS STANDARDS: NORMAL, UTILITY, ACROBATIC, AND COMMUTER CATEGORY AIRPLANES Powerplant Fuel <span class="hlt">System</span> § 23.961 Fuel <span class="hlt">system</span> hot <span class="hlt">weather</span> operation. Each fuel <span class="hlt">system</span> must be free from vapor lock...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/CFR-2013-title14-vol1/pdf/CFR-2013-title14-vol1-sec23-961.pdf','CFR2013'); return false;" href="https://www.gpo.gov/fdsys/pkg/CFR-2013-title14-vol1/pdf/CFR-2013-title14-vol1-sec23-961.pdf"><span>14 CFR 23.961 - Fuel <span class="hlt">system</span> hot <span class="hlt">weather</span> operation.</span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collectionCfr.action?selectedYearFrom=2013&page.go=Go">Code of Federal Regulations, 2013 CFR</a></p> <p></p> <p>2013-01-01</p> <p>... 14 Aeronautics and Space 1 2013-01-01 2013-01-01 false Fuel <span class="hlt">system</span> hot <span class="hlt">weather</span> operation. 23.961... AIRCRAFT AIRWORTHINESS STANDARDS: NORMAL, UTILITY, ACROBATIC, AND COMMUTER CATEGORY AIRPLANES Powerplant Fuel <span class="hlt">System</span> § 23.961 Fuel <span class="hlt">system</span> hot <span class="hlt">weather</span> operation. Each fuel <span class="hlt">system</span> must be free from vapor lock...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017AGUFMSA23A2538M','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017AGUFMSA23A2538M"><span>Latest Community Coordinated <span class="hlt">Modeling</span> Center (CCMC) services and innovative tools supporting the space <span class="hlt">weather</span> research and operational communities.</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Mendoza, A. M. M.; Rastaetter, L.; Kuznetsova, M. M.; Mays, M. L.; Chulaki, A.; Shim, J. S.; MacNeice, P. J.; Taktakishvili, A.; Collado-Vega, Y. M.; Weigand, C.; Zheng, Y.; Mullinix, R.; Patel, K.; Pembroke, A. D.; Pulkkinen, A. A.; Boblitt, J. M.; Bakshi, S. S.; Tsui, T.</p> <p>2017-12-01</p> <p>The Community Coordinated <span class="hlt">Modeling</span> Center (CCMC), with the fundamental goal of aiding the transition of modern space science <span class="hlt">models</span> into space <span class="hlt">weather</span> forecasting while supporting space science research, has been serving as an integral hub for over 15 years, providing invaluable resources to both space <span class="hlt">weather</span> scientific and operational communities. CCMC has developed and provided innovative web-based point of access tools varying from: Runs-On-Request <span class="hlt">System</span> - providing unprecedented global access to the largest collection of state-of-the-art solar and space physics <span class="hlt">models</span>, Integrated Space <span class="hlt">Weather</span> Analysis (iSWA) - a powerful dissemination <span class="hlt">system</span> for space <span class="hlt">weather</span> information, Advanced Online Visualization and Analysis tools for more accurate interpretation of <span class="hlt">model</span> results, Standard Data formats for Simulation Data downloads, and Mobile apps to view space <span class="hlt">weather</span> data anywhere to the scientific community. In addition to supporting research and performing <span class="hlt">model</span> evaluations, CCMC also supports space science education by hosting summer students through local universities. In this poster, we will showcase CCMC's latest innovative tools and services, and CCMC's tools that revolutionized the way we do research and improve our operational space <span class="hlt">weather</span> capabilities. CCMC's free tools and resources are all publicly available online (http://ccmc.gsfc.nasa.gov).</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/20170000649','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/20170000649"><span>Extratropical <span class="hlt">Weather</span> <span class="hlt">Systems</span> on Mars: Radiatively-Active Water Ice Effects</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Hollingsworth, J. L.; Kahre, M. A.; Haberle, R. M.; Urata, R. A.; Montmessin, F.</p> <p>2017-01-01</p> <p>Extratropical, large-scale <span class="hlt">weather</span> disturbances, namely transient, synoptic-period,baroclinic barotropic eddies - or - low- (high-) pressure cyclones (anticyclones), are components fundamental to global circulation patterns for rapidly rotating, differentially heated, shallow atmospheres such as Earth and Mars. Such "wave-like" disturbances that arise via (geophysical) fluid shear instability develop, mature and decay, and travel west-to-east in the middle and high latitudes within terrestrial-like planetary atmospheres. These disturbances serve as critical agents in the transport of heat and momentum between low and high latitudes of the planet. Moreover, they transport trace species within the atmosphere (e.g., water vapor/ice, other aerosols (dust), chemical species, etc). Between early autumn through early spring, middle and high latitudes on Mars exhibit strong equator-to-pole mean temperature contrasts (i.e., "baroclinicity"). Data collected during the Viking era and observations from both the Mars Global Surveyor (MGS) and Mars Reconnaissance Orbiter (MRO) indicate that such strong baroclinicity supports vigorous, large-scale eastward traveling <span class="hlt">weather</span> <span class="hlt">systems</span> [Banfield et al., 2004; Barnes et al., 1993]. A good example of traveling <span class="hlt">weather</span> <span class="hlt">systems</span>, frontal wave activity and sequestered dust activity from MGS/MOC image analyses is provided in Figure 1 (cf. Wang et al. [2005]). Utilizing an upgraded and evolving version of the NASA Ames Research Center (ARC) Mars global climate <span class="hlt">model</span>, investigated here are key dynamical and physical aspects of simulated northern hemisphere (NH) large-scale extratropica lweather <span class="hlt">systems</span>,with and without radiatively-active water ice clouds. Mars Climate <span class="hlt">Model</span>:</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2014APS..APR.D1019C','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2014APS..APR.D1019C"><span>Infrasonic Influences of Tornados and Cyclonic <span class="hlt">Weather</span> <span class="hlt">Systems</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Cook, Tessa</p> <p>2014-03-01</p> <p>Infrasound waves travel through the air at approximately 340 m/s at sea level, while experiencing low levels of friction, allowing the waves to travel over larger distances. When seismic waves travel through unconsolidated soil, the waves slow down to approximately 340 m/s. Because the speeds of waves in the air and ground are similar, a more effective transfer of energy from the atmosphere to the ground can occur. Large ring lasers can be utilized for detecting sources of infrasound traveling through the ground by measuring anomalies in the frequency difference between their two counter-rotating beams. Sources of infrasound include tornados and other cyclonic <span class="hlt">weather</span> <span class="hlt">systems</span>. The way <span class="hlt">systems</span> create waves that transfer to the ground is unknown and will be continued in further research; this research has focused on attempting to isolate the time that the ring laser detected anomalies in order to investigate if these anomalies may be contributed to isolatable <span class="hlt">weather</span> <span class="hlt">systems</span>. Furthermore, this research analyzed the frequencies detected in each of the anomalies and compared the frequencies with various characteristics of each <span class="hlt">weather</span> <span class="hlt">system</span>, such as tornado width, wind speeds, and <span class="hlt">system</span> development. This research may be beneficial for monitoring gravity waves and <span class="hlt">weather</span> <span class="hlt">systems</span>.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2018MS%26E..336a2024S','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2018MS%26E..336a2024S"><span>Arduino Based <span class="hlt">Weather</span> Monitoring Telemetry <span class="hlt">System</span> Using NRF24L01+</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Sidqi, Rafi; Rio Rynaldo, Bagus; Hadi Suroso, Satya; Firmansyah, Rifqi</p> <p>2018-04-01</p> <p>Abstract-<span class="hlt">Weather</span> is an important part of the natural environment, thus knowing <span class="hlt">weather</span> information is needed before doing activity. The main purpose of this research was to develop a <span class="hlt">weather</span> monitoring <span class="hlt">system</span> which capable to transmit <span class="hlt">weather</span> data via radio frequency by using nRF24L01+ 2,4GHz radio module. This research implement Arduino UNO as the main controller of the <span class="hlt">system</span> which send data wirelessly using the radio module and received by a receiver <span class="hlt">system</span>. Received data then logged and displayed using a Graphical User Interface on a personal computer. Test and experiment result show that the <span class="hlt">system</span> was able to transmit <span class="hlt">weather</span> data via radio wave with maximum transmitting range of 32 meters.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://ntrs.nasa.gov/search.jsp?R=20030065982&hterms=system+web&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D10%26Ntt%3Dsystem%2Bweb','NASA-TRS'); return false;" href="https://ntrs.nasa.gov/search.jsp?R=20030065982&hterms=system+web&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D10%26Ntt%3Dsystem%2Bweb"><span>Web-based <span class="hlt">Weather</span> Expert <span class="hlt">System</span> (WES) for Space Shuttle Launch</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Bardina, Jorge E.; Rajkumar, T.</p> <p>2003-01-01</p> <p>The Web-based <span class="hlt">Weather</span> Expert <span class="hlt">System</span> (WES) is a critical module of the Virtual Test Bed development to support 'go/no go' decisions for Space Shuttle operations in the Intelligent Launch and Range Operations program of NASA. The <span class="hlt">weather</span> rules characterize certain aspects of the environment related to the launching or landing site, the time of the day or night, the pad or runway conditions, the mission durations, the runway equipment and landing type. Expert <span class="hlt">system</span> rules are derived from <span class="hlt">weather</span> contingency rules, which were developed over years by NASA. Backward chaining, a goal-directed inference method is adopted, because a particular consequence or goal clause is evaluated first, and then chained backward through the rules. Once a rule is satisfied or true, then that particular rule is fired and the decision is expressed. The expert <span class="hlt">system</span> is continuously verifying the rules against the past one-hour <span class="hlt">weather</span> conditions and the decisions are made. The normal procedure of operations requires a formal pre-launch <span class="hlt">weather</span> briefing held on Launch minus 1 day, which is a specific <span class="hlt">weather</span> briefing for all areas of Space Shuttle launch operations. In this paper, the Web-based <span class="hlt">Weather</span> Expert <span class="hlt">System</span> of the Intelligent Launch and range Operations program is presented.</p> </li> </ol> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_5");'>5</a></li> <li><a href="#" onclick='return showDiv("page_6");'>6</a></li> <li class="active"><span>7</span></li> <li><a href="#" onclick='return showDiv("page_8");'>8</a></li> <li><a href="#" onclick='return showDiv("page_9");'>9</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div><!-- col-sm-12 --> </div><!-- row --> </div><!-- page_7 --> <div id="page_8" class="hiddenDiv"> <div class="row"> <div class="col-sm-12"> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_6");'>6</a></li> <li><a href="#" onclick='return showDiv("page_7");'>7</a></li> <li class="active"><span>8</span></li> <li><a href="#" onclick='return showDiv("page_9");'>9</a></li> <li><a href="#" onclick='return showDiv("page_10");'>10</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div> </div> <div class="row"> <div class="col-sm-12"> <ol class="result-class" start="141"> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017CoPhC.220..188D','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017CoPhC.220..188D"><span>Atlas : A library for numerical <span class="hlt">weather</span> prediction and climate <span class="hlt">modelling</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Deconinck, Willem; Bauer, Peter; Diamantakis, Michail; Hamrud, Mats; Kühnlein, Christian; Maciel, Pedro; Mengaldo, Gianmarco; Quintino, Tiago; Raoult, Baudouin; Smolarkiewicz, Piotr K.; Wedi, Nils P.</p> <p>2017-11-01</p> <p>The algorithms underlying numerical <span class="hlt">weather</span> prediction (NWP) and climate <span class="hlt">models</span> that have been developed in the past few decades face an increasing challenge caused by the paradigm shift imposed by hardware vendors towards more energy-efficient devices. In order to provide a sustainable path to exascale High Performance Computing (HPC), applications become increasingly restricted by energy consumption. As a result, the emerging diverse and complex hardware solutions have a large impact on the programming <span class="hlt">models</span> traditionally used in NWP software, triggering a rethink of design choices for future massively parallel software frameworks. In this paper, we present Atlas, a new software library that is currently being developed at the European Centre for Medium-Range <span class="hlt">Weather</span> Forecasts (ECMWF), with the scope of handling data structures required for NWP applications in a flexible and massively parallel way. Atlas provides a versatile framework for the future development of efficient NWP and climate applications on emerging HPC architectures. The applications range from full Earth <span class="hlt">system</span> <span class="hlt">models</span>, to specific tools required for post-processing <span class="hlt">weather</span> forecast products. The Atlas library thus constitutes a step towards affordable exascale high-performance simulations by providing the necessary abstractions that facilitate the application in heterogeneous HPC environments by promoting the co-design of NWP algorithms with the underlying hardware.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://eric.ed.gov/?q=mars&id=EJ1087929','ERIC'); return false;" href="https://eric.ed.gov/?q=mars&id=EJ1087929"><span><span class="hlt">Weather</span> Observers: A Manipulative Augmented Reality <span class="hlt">System</span> for <span class="hlt">Weather</span> Simulations at Home, in the Classroom, and at a Museum</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>Hsiao, Hsien-Sheng; Chang, Cheng-Sian; Lin, Chien-Yu; Wang, Yau-Zng</p> <p>2016-01-01</p> <p>This study focused on how to enhance the interactivity and usefulness of augmented reality (AR) by integrating manipulative interactive tools with a real-world environment. A manipulative AR (MAR) <span class="hlt">system</span>, which included 3D interactive <span class="hlt">models</span> and manipulative aids, was designed and developed to teach the unit "Understanding <span class="hlt">Weather</span>" in a…</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://www.dtic.mil/docs/citations/ADA630788','DTIC-ST'); return false;" href="http://www.dtic.mil/docs/citations/ADA630788"><span>The Analysis, Numerical Simulation, and Diagnosis of Extratropical <span class="hlt">Weather</span> <span class="hlt">Systems</span></span></a></p> <p><a target="_blank" href="http://www.dtic.mil/">DTIC Science & Technology</a></p> <p></p> <p>2003-09-30</p> <p>The Analysis, Numerical Simulation, and Diagnosis of Extratropical <span class="hlt">Weather</span> <span class="hlt">Systems</span> Dr. Melvyn A. Shapiro NOAA/Office of <span class="hlt">Weather</span> and Air Quality...predictability of extratropical cyclones. APPROACH My approach toward achieving the above objectives has been to foster national and...TITLE AND SUBTITLE The Analysis, Numerical Simulation, and Diagnosis of Extratropical <span class="hlt">Weather</span> <span class="hlt">Systems</span> 5a. CONTRACT NUMBER 5b. GRANT NUMBER 5c. PROGRAM</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://ntrs.nasa.gov/search.jsp?R=20060054001&hterms=reproduction&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D80%26Ntt%3Dreproduction','NASA-TRS'); return false;" href="https://ntrs.nasa.gov/search.jsp?R=20060054001&hterms=reproduction&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D80%26Ntt%3Dreproduction"><span>Validating the Airspace Concept Evaluation <span class="hlt">System</span> for Different <span class="hlt">Weather</span> Days</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Zelinski, Shannon; Meyn, Larry</p> <p>2006-01-01</p> <p>This paper extends the process for validating the Airspace Concept Evaluation <span class="hlt">System</span> using real-world historical flight operational data. <span class="hlt">System</span> inputs such as flight plans and airport en-route capacities, are generated and processed to create a realistic reproduction of a single day's operations within the National Airspace <span class="hlt">System</span>. <span class="hlt">System</span> outputs such as airport throughput, delays, and en-route sector loads are then compared to real world operational metrics and delay statistics for the reproduced day. The process is repeated for 4 historical days with high and low traffic volume and delay attributed to <span class="hlt">weather</span>. These 4 days are simulated using default en-route capacities and variable en-route capacities used to emulate <span class="hlt">weather</span>. The validation results show that default enroute capacity simulations are closer to real-world data for low <span class="hlt">weather</span> days than high <span class="hlt">weather</span> days. The use of reduced variable enroute capacities adds a large delay bias to ACES but delay trends between <span class="hlt">weather</span> days are better represented.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://rosap.ntl.bts.gov/view/dot/20489','DOTNTL'); return false;" href="https://rosap.ntl.bts.gov/view/dot/20489"><span>Roadway <span class="hlt">weather</span> information <span class="hlt">system</span> and automatic vehicle location (AVL) coordination.</span></a></p> <p><a target="_blank" href="http://ntlsearch.bts.gov/tris/index.do">DOT National Transportation Integrated Search</a></p> <p></p> <p>2011-02-28</p> <p>Roadway <span class="hlt">Weather</span> Information <span class="hlt">System</span> and Automatic Vehicle Location Coordination involves the : development of an Inclement <span class="hlt">Weather</span> Console that provides a new capability for the state of Oklahoma : to monitor <span class="hlt">weather</span>-related roadway conditions. The go...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2013AGUFMSM53D2235K','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2013AGUFMSM53D2235K"><span>Community Coordinated <span class="hlt">Modeling</span> Center: Paving the Way for Progress in Space Science Research to Operational Space <span class="hlt">Weather</span> Forecasting</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Kuznetsova, M. M.; Maddox, M. M.; Mays, M. L.; Mullinix, R.; MacNeice, P. J.; Pulkkinen, A. A.; Rastaetter, L.; Shim, J.; Taktakishvili, A.; Zheng, Y.; Wiegand, C.</p> <p>2013-12-01</p> <p>Community Coordinated <span class="hlt">Modeling</span> Center (CCMC) was established at the dawn of the millennium as an essential element on the National Space <span class="hlt">Weather</span> Program. One of the CCMC goals was to pave the way for progress in space science research to operational space <span class="hlt">weather</span> forecasting. Over the years the CCMC acquired the unique experience in preparing complex <span class="hlt">models</span> and <span class="hlt">model</span> chains for operational environment, in developing and maintaining powerful web-based tools and <span class="hlt">systems</span> ready to be used by space <span class="hlt">weather</span> service providers and decision makers as well as in space <span class="hlt">weather</span> prediction capabilities assessments. The presentation will showcase latest innovative solutions for space <span class="hlt">weather</span> research, analysis, forecasting and validation and review on-going community-wide initiatives enabled by CCMC applications.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2016AGUFMPP23C2346B','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2016AGUFMPP23C2346B"><span><span class="hlt">Modeling</span> Silicate <span class="hlt">Weathering</span> for Elevated CO2 and Temperature</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Bolton, E. W.</p> <p>2016-12-01</p> <p>A reactive transport <span class="hlt">model</span> (RTM) is used to assess CO2 drawdown by silicate <span class="hlt">weathering</span> over a wide range of temperature, pCO2, and infiltration rates for basalts and granites. Although RTM's have been used extensively to <span class="hlt">model</span> <span class="hlt">weathering</span> of basalts and granites for present-day conditions, we extend such <span class="hlt">modeling</span> to higher CO2 that could have existed during the Archean and Proterozoic. We also consider a wide range of surface temperatures and infiltration rates. We consider several <span class="hlt">model</span> basalt and granite compositions. We normally impose CO2 in equilibrium with the various atmospheric ranges <span class="hlt">modeled</span> and CO2 is delivered to the <span class="hlt">weathering</span> zone by aqueous transport. We also consider <span class="hlt">models</span> with fixed CO2 (aq) throughout the <span class="hlt">weathering</span> zone as could occur in soils with partial water saturation or with plant respiration, which can strongly influence pH and mineral dissolution rates. For the <span class="hlt">modeling</span>, we use Kinflow: a <span class="hlt">model</span> developed at Yale that includes mineral dissolution and precipitation under kinetic control, aqueous speciation, surface erosion, dynamic porosity, permeability, and mineral surface areas via sub-grid-scale grain <span class="hlt">models</span>, and exchange of volatiles at the surface. Most of the <span class="hlt">modeling</span> is done in 1D, but some comparisons to 2D domains with heterogeneous permeability are made. We find that when CO2 is fixed only at the surface, the pH tends toward higher values for basalts than granites, in large part due to the presence of more divalent than monovalent cations in the primary minerals, tending to decrease rates of mineral dissolution. <span class="hlt">Weathering</span> rates increase (as expected) with increasing CO2 and temperature. This <span class="hlt">modeling</span> is done with the support of the Virtual Planetary Laboratory.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2016AGUFM.G21C..06F','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2016AGUFM.G21C..06F"><span>Advanced corrections for InSAR using GPS and numerical <span class="hlt">weather</span> <span class="hlt">models</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Foster, J. H.; Cossu, F.; Amelung, F.; Businger, S.; Cherubini, T.</p> <p>2016-12-01</p> <p>The complex spatial and temporal changes in the atmospheric propagation delay of the radar signal remain the single biggest factor limiting Interferometric Synthetic Aperture Radar's (InSAR) potential for hazard monitoring and mitigation. A new generation of InSAR <span class="hlt">systems</span> is being built and launched, and optimizing the science and hazard applications of these <span class="hlt">systems</span> requires advanced methodologies to mitigate tropospheric noise. We present preliminary results from an investigation into the application of GPS and numerical <span class="hlt">weather</span> <span class="hlt">models</span> for generating tropospheric correction fields. We use the <span class="hlt">Weather</span> Research and Forecasting (WRF) <span class="hlt">model</span> to generate a 900 m spatial resolution atmospheric <span class="hlt">model</span> covering the Big Island of Hawaii and an even higher, 300 m resolution grid over Mauna Loa and Kilauea volcanoes. By comparing a range of approaches, from the simplest, using reanalyses based on typically available meteorological observations, through to the "kitchen-sink" approach of assimilating all relevant data sets into our custom analyses, we examine the impact of the additional data sets on the atmospheric <span class="hlt">models</span> and their effectiveness in correcting InSAR data. We focus particularly on the assimilation of information from the more than 60 GPS sites in the island. We ingest zenith tropospheric delay estimates from these sites directly into the WRF analyses, and also perform double-difference tomography using the phase residuals from the GPS processing to robustly incorporate information on atmospheric heterogeneity from the GPS data into the <span class="hlt">models</span>. We assess our performance through comparisons of our atmospheric <span class="hlt">models</span> with external observations not ingested into the <span class="hlt">model</span>, and through the effectiveness of the derived phase screens in reducing InSAR variance. This work will produce best-practice recommendations for the use of <span class="hlt">weather</span> <span class="hlt">models</span> for InSAR correction, and inform efforts to design a global strategy for the NISAR mission, for both low-latency and definitive</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2002EGSGA..27.1435B','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2002EGSGA..27.1435B"><span>A Data Assimilation <span class="hlt">System</span> For Operational <span class="hlt">Weather</span> Forecast In Galicia Region (nw Spain)</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Balseiro, C. F.; Souto, M. J.; Pérez-Muñuzuri, V.; Brewster, K.; Xue, M.</p> <p></p> <p>Regional <span class="hlt">weather</span> forecast <span class="hlt">models</span>, such as the Advanced Regional Prediction <span class="hlt">System</span> (ARPS), over complex environments with varying local influences require an accurate meteorological analysis that should include all local meteorological measurements available. In this work, the ARPS Data Analysis <span class="hlt">System</span> (ADAS) (Xue et al. 2001) is applied as a three-dimensional <span class="hlt">weather</span> analysis tool to include surface station and rawinsonde data with the NCEP AVN forecasts as the analysis background. Currently in ADAS, a set of five meteorological variables are considered during the analysis: horizontal grid-relative wind components, pressure, potential temperature and spe- cific humidity. The analysis is used for high resolution numerical <span class="hlt">weather</span> prediction for the Galicia region. The analysis method used in ADAS is based on the successive corrective scheme of Bratseth (1986), which asymptotically approaches the result of a statistical (optimal) interpolation, but at lower computational cost. As in the optimal interpolation scheme, the Bratseth interpolation method can take into account the rel- ative error between background and observational data, therefore they are relatively insensitive to large variations in data density and can integrate data of mixed accuracy. This method can be applied economically in an operational setting, providing signifi- cant improvement over the background <span class="hlt">model</span> forecast as well as any analysis without high-resolution local observations. A one-way nesting is applied for <span class="hlt">weather</span> forecast in Galicia region, and the use of this assimilation <span class="hlt">system</span> in both domains shows better results not only in initial conditions but also in all forecast periods. Bratseth, A.M. (1986): "Statistical interpolation by means of successive corrections." Tellus, 38A, 439-447. Souto, M. J., Balseiro, C. F., Pérez-Muñuzuri, V., Xue, M. Brewster, K., (2001): "Im- pact of cloud analysis on numerical <span class="hlt">weather</span> prediction in the galician region of Spain". Submitted to Journal of</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2014EGUGA..1614940G','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2014EGUGA..1614940G"><span>Network connectivity paradigm for the large data produced by <span class="hlt">weather</span> radar <span class="hlt">systems</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Guenzi, Diego; Bechini, Renzo; Boraso, Rodolfo; Cremonini, Roberto; Fratianni, Simona</p> <p>2014-05-01</p> <p>The traffic over Internet is constantly increasing; this is due in particular to social networks activities but also to the enormous exchange of data caused especially by the so-called "Internet of Things". With this term we refer to every device that has the capability of exchanging information with other devices on the web. In geoscience (and, in particular, in meteorology and climatology) there is a constantly increasing number of sensors that are used to obtain data from different sources (like <span class="hlt">weather</span> radars, digital rain gauges, etc.). This information-gathering activity, frequently, must be followed by a complex data analysis phase, especially when we have large data sets that can be very difficult to analyze (very long historical series of large data sets, for example), like the so called big data. These activities are particularly intensive in resource consumption and they lead to new computational <span class="hlt">models</span> (like cloud computing) and new methods for storing data (like object store, linked open data, NOSQL or NewSQL). The <span class="hlt">weather</span> radar <span class="hlt">systems</span> can be seen as one of the sensors mentioned above: it transmit a large amount of raw data over the network (up to 40 megabytes every five minutes), with 24h/24h continuity and in any <span class="hlt">weather</span> condition. <span class="hlt">Weather</span> radar are often located in peaks and in wild areas where connectivity is poor. For this reason radar measurements are sometimes processed partially on site and reduced in size to adapt them to the limited bandwidth currently available by data transmission <span class="hlt">systems</span>. With the aim to preserve the maximum flow of information, an innovative network connectivity paradigm for the large data produced by <span class="hlt">weather</span> radar <span class="hlt">system</span> is here presented. The study is focused on the Monte Settepani operational <span class="hlt">weather</span> radar <span class="hlt">system</span>, located over a wild peak summit in north-western Italy.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2016cosp...41E.180B','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2016cosp...41E.180B"><span>Operational Space <span class="hlt">Weather</span> Activities in the US</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Berger, Thomas; Singer, Howard; Onsager, Terrance; Viereck, Rodney; Murtagh, William; Rutledge, Robert</p> <p>2016-07-01</p> <p>We review the current activities in the civil operational space <span class="hlt">weather</span> forecasting enterprise of the United States. The NOAA/Space <span class="hlt">Weather</span> Prediction Center is the nation's official source of space <span class="hlt">weather</span> watches, warnings, and alerts, working with partners in the Air Force as well as international operational forecast services to provide predictions, data, and products on a large variety of space <span class="hlt">weather</span> phenomena and impacts. In October 2015, the White House Office of Science and Technology Policy released the National Space <span class="hlt">Weather</span> Strategy (NSWS) and associated Space <span class="hlt">Weather</span> Action Plan (SWAP) that define how the nation will better forecast, mitigate, and respond to an extreme space <span class="hlt">weather</span> event. The SWAP defines actions involving multiple federal agencies and mandates coordination and collaboration with academia, the private sector, and international bodies to, among other things, develop and sustain an operational space <span class="hlt">weather</span> observing <span class="hlt">system</span>; develop and deploy new <span class="hlt">models</span> of space <span class="hlt">weather</span> impacts to critical infrastructure <span class="hlt">systems</span>; define new mechanisms for the transition of research <span class="hlt">models</span> to operations and to ensure that the research community is supported for, and has access to, operational <span class="hlt">model</span> upgrade paths; and to enhance fundamental understanding of space <span class="hlt">weather</span> through support of research <span class="hlt">models</span> and observations. The SWAP will guide significant aspects of space <span class="hlt">weather</span> operational and research activities for the next decade, with opportunities to revisit the strategy in the coming years through the auspices of the National Science and Technology Council.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2015EGUGA..17.1807O','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2015EGUGA..17.1807O"><span>Sensitivity of mineral dissolution rates to physical <span class="hlt">weathering</span> : A <span class="hlt">modeling</span> approach</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Opolot, Emmanuel; Finke, Peter</p> <p>2015-04-01</p> <p>There is continued interest on accurate estimation of natural <span class="hlt">weathering</span> rates owing to their importance in soil formation, nutrient cycling, estimation of acidification in soils, rivers and lakes, and in understanding the role of silicate <span class="hlt">weathering</span> in carbon sequestration. At the same time a challenge does exist to reconcile discrepancies between laboratory-determined <span class="hlt">weathering</span> rates and natural <span class="hlt">weathering</span> rates. Studies have consistently reported laboratory rates to be in orders of magnitude faster than the natural <span class="hlt">weathering</span> rates (White, 2009). These discrepancies have mainly been attributed to (i) changes in fluid composition (ii) changes in primary mineral surfaces (reactive sites) and (iii) the formation of secondary phases; that could slow natural <span class="hlt">weathering</span> rates. It is indeed difficult to measure the interactive effect of the intrinsic factors (e.g. mineral composition, surface area) and extrinsic factors (e.g. solution composition, climate, bioturbation) occurring at the natural setting, in the laboratory experiments. A <span class="hlt">modeling</span> approach could be useful in this case. A number of geochemical <span class="hlt">models</span> (e.g. PHREEQC, EQ3/EQ6) already exist and are capable of estimating mineral dissolution / precipitation rates as a function of time and mineral mass. However most of these approaches assume a constant surface area in a given volume of water (White, 2009). This assumption may become invalid especially at long time scales. One of the widely used <span class="hlt">weathering</span> <span class="hlt">models</span> is the PROFILE <span class="hlt">model</span> (Sverdrup and Warfvinge, 1993). The PROFILE <span class="hlt">model</span> takes into account the mineral composition, solution composition and surface area in determining dissolution / precipitation rates. However there is less coupling with other processes (e.g. physical <span class="hlt">weathering</span>, clay migration, bioturbation) which could directly or indirectly influence dissolution / precipitation rates. We propose in this study a coupling between chemical <span class="hlt">weathering</span> mechanism (defined as a function of reactive area</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://cfpub.epa.gov/si/si_public_record_report.cfm?dirEntryId=308466&Lab=NERL&keyword=dependency&actType=&TIMSType=+&TIMSSubTypeID=&DEID=&epaNumber=&ntisID=&archiveStatus=Both&ombCat=Any&dateBeginCreated=&dateEndCreated=&dateBeginPublishedPresented=&dateEndPublishedPresented=&dateBeginUpdated=&dateEndUpdated=&dateBeginCompleted=&dateEndCompleted=&personID=&role=Any&journalID=&publisherID=&sortBy=revisionDate&count=50','EPA-EIMS'); return false;" href="https://cfpub.epa.gov/si/si_public_record_report.cfm?dirEntryId=308466&Lab=NERL&keyword=dependency&actType=&TIMSType=+&TIMSSubTypeID=&DEID=&epaNumber=&ntisID=&archiveStatus=Both&ombCat=Any&dateBeginCreated=&dateEndCreated=&dateBeginPublishedPresented=&dateEndPublishedPresented=&dateBeginUpdated=&dateEndUpdated=&dateBeginCompleted=&dateEndCompleted=&personID=&role=Any&journalID=&publisherID=&sortBy=revisionDate&count=50"><span>Improving High-resolution <span class="hlt">Weather</span> Forecasts using the <span class="hlt">Weather</span> Research and Forecasting (WRF) <span class="hlt">Model</span> with Upgraded Kain-Fritsch Cumulus Scheme</span></a></p> <p><a target="_blank" href="http://oaspub.epa.gov/eims/query.page">EPA Science Inventory</a></p> <p></p> <p></p> <p>High-resolution <span class="hlt">weather</span> forecasting is affected by many aspects, i.e. <span class="hlt">model</span> initial conditions, subgrid-scale cumulus convection and cloud microphysics schemes. Recent 12km grid studies using the <span class="hlt">Weather</span> Research and Forecasting (WRF) <span class="hlt">model</span> have identified the importance of inco...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/20080004450','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/20080004450"><span>Cockpit <span class="hlt">weather</span> information <span class="hlt">system</span></span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Tu, Jeffrey Chen-Yu (Inventor)</p> <p>2000-01-01</p> <p><span class="hlt">Weather</span> information, periodically collected from throughout a global region, is periodically assimilated and compiled at a central source and sent via a high speed data link to a satellite communication service, such as COMSAT. That communication service converts the compiled <span class="hlt">weather</span> information to GSDB format, and transmits the GSDB encoded information to an orbiting broadcast satellite, INMARSAT, transmitting the information at a data rate of no less than 10.5 kilobits per second. The INMARSAT satellite receives that data over its P-channel and rebroadcasts the GDSB encoded <span class="hlt">weather</span> information, in the microwave L-band, throughout the global region at a rate of no less than 10.5 KB/S. The transmission is received aboard an aircraft by means of an onboard SATCOM receiver and the output is furnished to a <span class="hlt">weather</span> information processor. A touch sensitive liquid crystal panel display allows the pilot to select the <span class="hlt">weather</span> function by touching a predefined icon overlain on the display's surface and in response a color graphic display of the <span class="hlt">weather</span> is displayed for the pilot.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2016AtmRe.178..114A','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2016AtmRe.178..114A"><span>Modern and prospective technologies for <span class="hlt">weather</span> modification activities: A look at integrating unmanned aircraft <span class="hlt">systems</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Axisa, Duncan; DeFelice, Tom P.</p> <p>2016-09-01</p> <p>Present-day <span class="hlt">weather</span> modification technologies are scientifically based and have made controlled technological advances since the late 1990s, early 2000s. The technological advances directly related to <span class="hlt">weather</span> modification have primarily been in the decision support and evaluation based software and <span class="hlt">modeling</span> areas. However, there have been some technological advances in other fields that might now be advanced enough to start considering their usefulness for improving <span class="hlt">weather</span> modification operational efficiency and evaluation accuracy. We consider the programmatic aspects underlying the development of new technologies for use in <span class="hlt">weather</span> modification activities, identifying their potential benefits and limitations. We provide context and initial guidance for operators that might integrate unmanned aircraft <span class="hlt">systems</span> technology in future <span class="hlt">weather</span> modification operations.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017AGUFM.S51B0601M','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017AGUFM.S51B0601M"><span>Improving Estimates of Regional Infrasound Propagation by Incorporating Three-Dimensional <span class="hlt">Weather</span> <span class="hlt">Modeling</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>McKenna, M. H.; Alter, R. E.; Swearingen, M. E.; Wilson, D. K.</p> <p>2017-12-01</p> <p>Many larger sources, such as volcanic eruptions and nuclear detonations, produce infrasound (acoustic waves with a frequency lower than humans can hear, namely 0.1-20 Hz) that can propagate over global scales. But many smaller infrastructure sources, such as bridges, dams, and buildings, also produce infrasound, though with a lower amplitude that tends to propagate only over regional scales (up to 150 km). In order to accurately calculate regional-scale infrasound propagation, we have incorporated high-resolution, three-dimensional forecasts from the <span class="hlt">Weather</span> Research and Forecasting (WRF) meteorological <span class="hlt">model</span> into a signal propagation <span class="hlt">modeling</span> <span class="hlt">system</span> called Environmental Awareness for Sensor and Emitter Employment (EASEE), developed at the US Army Engineer Research and Development Center. To quantify the improvement of infrasound propagation predictions with more realistic <span class="hlt">weather</span> data, we conducted sensitivity studies with different propagation ranges and horizontal resolutions and compared them to default predictions with no <span class="hlt">weather</span> <span class="hlt">model</span> data. We describe the process of incorporating WRF output into EASEE for conducting these acoustic propagation simulations and present the results of the aforementioned sensitivity studies.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.fs.usda.gov/treesearch/pubs/38546','TREESEARCH'); return false;" href="https://www.fs.usda.gov/treesearch/pubs/38546"><span>A simple stochastic <span class="hlt">weather</span> generator for ecological <span class="hlt">modeling</span></span></a></p> <p><a target="_blank" href="http://www.fs.usda.gov/treesearch/">Treesearch</a></p> <p>A.G. Birt; M.R. Valdez-Vivas; R.M. Feldman; C.W. Lafon; D. Cairns; R.N. Coulson; M. Tchakerian; W. Xi; Jim Guldin</p> <p>2010-01-01</p> <p>Stochastic <span class="hlt">weather</span> generators are useful tools for exploring the relationship between organisms and their environment. This paper describes a simple <span class="hlt">weather</span> generator that can be used in ecological <span class="hlt">modeling</span> projects. We provide a detailed description of methodology, and links to full C++ source code (http://weathergen.sourceforge.net) required to implement or modify...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017EGUGA..1914387M','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017EGUGA..1914387M"><span>Towards assimilation of InSAR data in operational <span class="hlt">weather</span> <span class="hlt">models</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Mulder, Gert; van Leijen, Freek; Barkmeijer, Jan; de Haan, Siebren; Hanssen, Ramon</p> <p>2017-04-01</p> <p>InSAR signal delays due to the varying atmospheric refractivity are a potential data source to improve <span class="hlt">weather</span> <span class="hlt">models</span> [1]. Especially with the launch of the new Sentinel-1 satellites, which increases data coverage, latency and accessibility, it may become possible to operationalize the assimilation of differential integrated refractivity (DIR) values in numerical <span class="hlt">weather</span> <span class="hlt">models</span>. Although studies exist on comparison between InSAR data and <span class="hlt">weather</span> <span class="hlt">models</span> [2], the impact of assimilation of DIR values in an operational <span class="hlt">weather</span> <span class="hlt">model</span> has never been assessed. In this study we present different ways to assimilate DIR values in an operational <span class="hlt">weather</span> <span class="hlt">model</span> and show the first forecast results. There are different possibilities to assimilate InSAR-data in a <span class="hlt">weather</span> <span class="hlt">model</span>. For example, (i) absolute DIR values can be derived using additional GNSS zenith or slant delay values, (ii) DIR values can be converted to water vapor pressures, or (iii) water vapor pressures can be derived for different heights by combining GNSS and InSAR data. However, an increasing number of assumptions in these processing steps will increase the uncertainty in the final results. Therefore, we chose to insert the InSAR derived DIR values after minimal additional processing. In this study we use the HARMONIE <span class="hlt">model</span> [3], which is a spectral, non-hydrostatic <span class="hlt">model</span> with a resolution of about 2.5 km. Currently, this is the operational <span class="hlt">model</span> in 11 European countries and based on the AROME <span class="hlt">model</span> [4]. To assimilate the DIR values in the <span class="hlt">weather</span> <span class="hlt">model</span> we use a simple adjustment of the <span class="hlt">weather</span> parameters over the full slant column to match the DIR values. This is a first step towards a more sophisticated approach based on the 3D-VAR or 4D-VAR schemes [5]. Where both assimilation schemes can correct for different <span class="hlt">weather</span> parameters simultaneously, and 4D-VAR allow us to assimilate DIR values at the exact moment of satellite overpass instead of the start of the forecast window. The approach will be demonstrated</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/20140010218','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/20140010218"><span>Flight Deck <span class="hlt">Weather</span> Avoidance Decision Support: Implementation and Evaluation</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Wu, Shu-Chieh; Luna, Rocio; Johnson, Walter W.</p> <p>2013-01-01</p> <p><span class="hlt">Weather</span> related disruptions account for seventy percent of the delays in the National Airspace <span class="hlt">System</span> (NAS). A key component in the <span class="hlt">weather</span> plan of the Next Generation of Air Transportation <span class="hlt">System</span> (NextGen) is to assimilate observed <span class="hlt">weather</span> information and probabilistic forecasts into the decision process of flight crews and air traffic controllers. In this research we explore supporting flight crew <span class="hlt">weather</span> decision making through the development of a flight deck predicted <span class="hlt">weather</span> display <span class="hlt">system</span> that utilizes <span class="hlt">weather</span> predictions generated by ground-based radar. This <span class="hlt">system</span> integrates and presents this <span class="hlt">weather</span> information, together with in-flight trajectory modification tools, within a cockpit display of traffic information (CDTI) prototype. that the CDTI features 2D and perspective 3D visualization <span class="hlt">models</span> of <span class="hlt">weather</span>. The <span class="hlt">weather</span> forecast products that we implemented were the Corridor Integrated <span class="hlt">Weather</span> <span class="hlt">System</span> (CIWS) and the Convective <span class="hlt">Weather</span> Avoidance <span class="hlt">Model</span> (CWAM), both developed by MIT Lincoln Lab. We evaluated the use of CIWS and CWAM for flight deck <span class="hlt">weather</span> avoidance in two part-task experiments. Experiment 1 compared pilots' en route <span class="hlt">weather</span> avoidance performance in four <span class="hlt">weather</span> information conditions that differed in the type and amount of predicted forecast (CIWS current <span class="hlt">weather</span> only, CIWS current and historical <span class="hlt">weather</span>, CIWS current and forecast <span class="hlt">weather</span>, CIWS current and forecast <span class="hlt">weather</span> and CWAM predictions). Experiment 2 compared the use of perspective 3D and 21/2D presentations of <span class="hlt">weather</span> for flight deck <span class="hlt">weather</span> avoidance. Results showed that pilots could take advantage of longer range predicted <span class="hlt">weather</span> forecasts in performing en route <span class="hlt">weather</span> avoidance but more research will be needed to determine what combinations of information are optimal and how best to present them.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2009AGUFM.A42B..08P','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2009AGUFM.A42B..08P"><span>Mesoscale <span class="hlt">weather</span> and climate <span class="hlt">modeling</span> with the global non-hydrostatic Goddard Earth Observing <span class="hlt">System</span> <span class="hlt">Model</span> (GEOS-5) at cloud-permitting resolutions</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Putman, W. M.; Suarez, M.</p> <p>2009-12-01</p> <p>The Goddard Earth Observing <span class="hlt">System</span> <span class="hlt">Model</span> (GEOS-5), an earth <span class="hlt">system</span> <span class="hlt">model</span> developed in the NASA Global <span class="hlt">Modeling</span> and Assimilation Office (GMAO), has integrated the non-hydrostatic finite-volume dynamical core on the cubed-sphere grid. The extension to a non-hydrostatic dynamical framework and the quasi-uniform cubed-sphere geometry permits the efficient exploration of global <span class="hlt">weather</span> and climate <span class="hlt">modeling</span> at cloud permitting resolutions of 10- to 4-km on today's high performance computing platforms. We have explored a series of incremental increases in global resolution with GEOS-5 from it's standard 72-level 27-km resolution (~5.5 million cells covering the globe from the surface to 0.1 hPa) down to 3.5-km (~3.6 billion cells). We will present results from a series of forecast experiments exploring the impact of the non-hydrostatic dynamics at transition resolutions of 14- to 7-km, and the influence of increased horizontal/vertical resolution on convection and physical parameterizations within GEOS-5. Regional and mesoscale features of 5- to 10-day <span class="hlt">weather</span> forecasts will be presented and compared with satellite observations. Our results will highlight the impact of resolution on the structure of cloud features including tropical convection and tropical cyclone predicability, cloud streets, von Karman vortices, and the marine stratocumulus cloud layer. We will also present experiment design and early results from climate impact experiments for global non-hydrostatic <span class="hlt">models</span> using GEOS-5. Our climate experiments will focus on support for the Year of Tropical Convection (YOTC). We will also discuss a seasonal climate time-slice experiment design for downscaling coarse resolution century scale climate simulations to global non-hydrostatic resolutions of 14- to 7-km with GEOS-5.</p> </li> </ol> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_6");'>6</a></li> <li><a href="#" onclick='return showDiv("page_7");'>7</a></li> <li class="active"><span>8</span></li> <li><a href="#" onclick='return showDiv("page_9");'>9</a></li> <li><a href="#" onclick='return showDiv("page_10");'>10</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div><!-- col-sm-12 --> </div><!-- row --> </div><!-- page_8 --> <div id="page_9" class="hiddenDiv"> <div class="row"> <div class="col-sm-12"> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_7");'>7</a></li> <li><a href="#" onclick='return showDiv("page_8");'>8</a></li> <li class="active"><span>9</span></li> <li><a href="#" onclick='return showDiv("page_10");'>10</a></li> <li><a href="#" onclick='return showDiv("page_11");'>11</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div> </div> <div class="row"> <div class="col-sm-12"> <ol class="result-class" start="161"> <li> <p><a target="_blank" onclick="trackOutboundLink('https://rosap.ntl.bts.gov/view/dot/3590','DOTNTL'); return false;" href="https://rosap.ntl.bts.gov/view/dot/3590"><span>Michigan Department of Transportation (MDOT) <span class="hlt">weather</span> responsive traveler information (Wx-TINFO) <span class="hlt">system</span>.</span></a></p> <p><a target="_blank" href="http://ntlsearch.bts.gov/tris/index.do">DOT National Transportation Integrated Search</a></p> <p></p> <p>2016-01-01</p> <p>FHWAs Road <span class="hlt">Weather</span> Management Program partnered with MDOT to develop a <span class="hlt">weather</span> responsive traveler information <span class="hlt">system</span> called Wx-TINFO. The <span class="hlt">system</span>, shown below, integrates multiple <span class="hlt">weather</span> data sources into one program, enabling Transportation Oper...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2015AGUFM.H52C..07P','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2015AGUFM.H52C..07P"><span>Resolving the Multi-scale Behavior of Geochemical <span class="hlt">Weathering</span> in the Critical Zone Using High Resolution Hydro-geochemical <span class="hlt">Models</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Pandey, S.; Rajaram, H.</p> <p>2015-12-01</p> <p>This work investigates hydrologic and geochemical interactions in the Critical Zone (CZ) using high-resolution reactive transport <span class="hlt">modeling</span>. Reactive transport <span class="hlt">models</span> can be used to predict the response of geochemical <span class="hlt">weathering</span> and solute fluxes in the CZ to changes in a dynamic environment, such as those pertaining to human activities and climate change in recent years. The scales of hydrology and geochemistry in the CZ range from days to eons in time and centimeters to kilometers in space. Here, we present results of a multi-dimensional, multi-scale hydro-geochemical <span class="hlt">model</span> to investigate the role of subsurface heterogeneity on the formation of mineral <span class="hlt">weathering</span> fronts in the CZ, which requires consideration of many of these spatio-temporal scales. The <span class="hlt">model</span> is implemented using the reactive transport code PFLOTRAN, an open source subsurface flow and reactive transport code that utilizes parallelization over multiple processing nodes and provides a strong framework for simulating <span class="hlt">weathering</span> in the CZ. The <span class="hlt">model</span> is set up to simulate <span class="hlt">weathering</span> dynamics in the mountainous catchments representative of the Colorado Front Range. <span class="hlt">Model</span> parameters were constrained based on hydrologic, geochemical, and geophysical observations from the Boulder Creek Critical Zone Observatory (BcCZO). Simulations were performed in fractured rock <span class="hlt">systems</span> and compared with <span class="hlt">systems</span> of heterogeneous and homogeneous permeability fields. Tracer simulations revealed that the mean residence time of solutes was drastically accelerated as fracture density increased. In simulations that include mineral reactions, distinct signatures of transport limitations on <span class="hlt">weathering</span> arose when discrete flow paths were included. This transport limitation was related to both advective and diffusive processes in the highly heterogeneous <span class="hlt">systems</span> (i.e. fractured media and correlated random permeability fields with σlnk > 3). The well-known time-dependence of mineral <span class="hlt">weathering</span> rates was found to be the most</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://ntrs.nasa.gov/search.jsp?R=20050182051&hterms=traffic+flow&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D60%26Ntt%3Dtraffic%2Bflow','NASA-TRS'); return false;" href="https://ntrs.nasa.gov/search.jsp?R=20050182051&hterms=traffic+flow&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D60%26Ntt%3Dtraffic%2Bflow"><span>National Airspace <span class="hlt">System</span> Delay Estimation Using <span class="hlt">Weather</span> Weighted Traffic Counts</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Chatterji, Gano B.; Sridhar, Banavar</p> <p>2004-01-01</p> <p>Assessment of National Airspace <span class="hlt">System</span> performance, which is usually measured in terms of delays resulting from the application of traffic flow management initiatives in response to <span class="hlt">weather</span> conditions, volume, equipment outages and runway conditions, is needed both for guiding flow control decisions during the day of operations and for post operations analysis. Comparison of the actual delay, resulting from the traffic flow management initiatives, with the expected delay, based on traffic demand and other conditions, provides the assessment of the National Airspace <span class="hlt">System</span> performance. This paper provides a method for estimating delay using the expected traffic demand and <span class="hlt">weather</span>. In order to identify the cause of delays, 517 days of National Airspace <span class="hlt">System</span> delay data reported by the Federal Aviation Administration s Operations Network were analyzed. This analysis shows that <span class="hlt">weather</span> is the most important causal factor for delays followed by equipment and runway delays. Guided by these results, the concept of <span class="hlt">weather</span> weighted traffic counts as a measure of <span class="hlt">system</span> delay is described. Examples are given to show the variation of these counts as a function of time of the day. The various datasets, consisting of aircraft position data, enroute severe <span class="hlt">weather</span> data, surface wind speed and visibility data, reported delay data and number of aircraft handled by the Centers data, and their sources are described. The procedure for selecting reference days on which traffic was minimally impacted by <span class="hlt">weather</span> is described. Different traffic demand on each reference day of the week, determined by analysis of 42 days of traffic and delay data, was used as the expected traffic demand for each day of the week. Next, the method for computing the <span class="hlt">weather</span> weighted traffic counts using the expected traffic demand, derived from reference days, and the expanded regions around severe <span class="hlt">weather</span> cells is discussed. It is shown via a numerical example that this approach improves the dynamic range</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/20130010528','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/20130010528"><span>Anvil Forecast Tool in the Advanced <span class="hlt">Weather</span> Interactive Processing <span class="hlt">System</span></span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Barrett, Joe H., III; Hood, Doris</p> <p>2009-01-01</p> <p>Meteorologists from the 45th <span class="hlt">Weather</span> Squadron (45 WS) and National <span class="hlt">Weather</span> Service Spaceflight Meteorology Group (SMG) have identified anvil forecasting as one of their most challenging tasks when predicting the probability of violations of the Lightning Launch Commit Criteria and Space Shuttle Flight Rules. As a result, the Applied Meteorology Unit (AMU) was tasked to create a graphical overlay tool for the Meteorological Interactive Data Display <span class="hlt">System</span> (MIDDS) that indicates the threat of thunderstorm anvil clouds, using either observed or <span class="hlt">model</span> forecast winds as input. The tool creates a graphic depicting the potential location of thunderstorm anvils one, two, and three hours into the future. The locations are based on the average of the upper level observed or forecasted winds. The graphic includes 10 and 20 n mi standoff circles centered at the location of interest, as well as one-, two-, and three-hour arcs in the upwind direction. The arcs extend outward across a 30 sector width based on a previous AMU study that determined thunderstorm anvils move in a direction plus or minus 15 of the upper-level wind direction. The AMU was then tasked to transition the tool to the Advanced <span class="hlt">Weather</span> Interactive Processing <span class="hlt">System</span> (AWIPS). SMG later requested the tool be updated to provide more flexibility and quicker access to <span class="hlt">model</span> data. This presentation describes the work performed by the AMU to transition the tool into AWIPS, as well as the subsequent improvements made to the tool.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2015AGUFMSH21B2400B','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2015AGUFMSH21B2400B"><span>Sol-Terra - AN Operational Space <span class="hlt">Weather</span> Forecasting <span class="hlt">Model</span> Framework</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Bisi, M. M.; Lawrence, G.; Pidgeon, A.; Reid, S.; Hapgood, M. A.; Bogdanova, Y.; Byrne, J.; Marsh, M. S.; Jackson, D.; Gibbs, M.</p> <p>2015-12-01</p> <p>The SOL-TERRA project is a collaboration between RHEA Tech, the Met Office, and RAL Space funded by the UK Space Agency. The goal of the SOL-TERRA project is to produce a Roadmap for a future coupled Sun-to-Earth operational space <span class="hlt">weather</span> forecasting <span class="hlt">system</span> covering domains from the Sun down to the magnetosphere-ionosphere-thermosphere and neutral atmosphere. The first stage of SOL-TERRA is underway and involves reviewing current <span class="hlt">models</span> that could potentially contribute to such a <span class="hlt">system</span>. Within a given domain, the various space <span class="hlt">weather</span> <span class="hlt">models</span> will be assessed how they could contribute to such a coupled <span class="hlt">system</span>. This will be done both by reviewing peer reviewed papers, and via direct input from the <span class="hlt">model</span> developers to provide further insight. Once the <span class="hlt">models</span> have been reviewed then the optimal set of <span class="hlt">models</span> for use in support of forecast-based SWE <span class="hlt">modelling</span> will be selected, and a Roadmap for the implementation of an operational forecast-based SWE <span class="hlt">modelling</span> framework will be prepared. The Roadmap will address the current <span class="hlt">modelling</span> capability, knowledge gaps and further work required, and also the implementation and maintenance of the overall architecture and environment that the <span class="hlt">models</span> will operate within. The SOL-TERRA project will engage with external stakeholders in order to ensure independently that the project remains on track to meet its original objectives. A group of key external stakeholders have been invited to provide their domain-specific expertise in reviewing the SOL-TERRA project at critical stages of Roadmap preparation; namely at the Mid-Term Review, and prior to submission of the Final Report. This stakeholder input will ensure that the SOL-TERRA Roadmap will be enhanced directly through the input of <span class="hlt">modellers</span> and end-users. The overall goal of the SOL-TERRA project is to develop a Roadmap for an operational forecast-based SWE <span class="hlt">modelling</span> framework with can be implemented within a larger subsequent activity. The SOL-TERRA project is supported within</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.osti.gov/biblio/982160-evaluating-climate-models-should-we-use-weather-climate-observations','SCIGOV-STC'); return false;" href="https://www.osti.gov/biblio/982160-evaluating-climate-models-should-we-use-weather-climate-observations"><span>Evaluating climate <span class="hlt">models</span>: Should we use <span class="hlt">weather</span> or climate observations?</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>Oglesby, Robert J; Erickson III, David J</p> <p>2009-12-01</p> <p>Calling the numerical <span class="hlt">models</span> that we use for simulations of climate change 'climate <span class="hlt">models</span>' is a bit of a misnomer. These 'general circulation <span class="hlt">models</span>' (GCMs, AKA global climate <span class="hlt">models</span>) and their cousins the 'regional climate <span class="hlt">models</span>' (RCMs) are actually physically-based <span class="hlt">weather</span> simulators. That is, these <span class="hlt">models</span> simulate, either globally or locally, daily <span class="hlt">weather</span> patterns in response to some change in forcing or boundary condition. These simulated <span class="hlt">weather</span> patterns are then aggregated into climate statistics, very much as we aggregate observations into 'real climate statistics'. Traditionally, the output of GCMs has been evaluated using climate statistics, as opposed to their abilitymore » to simulate realistic daily <span class="hlt">weather</span> observations. At the coarse global scale this may be a reasonable approach, however, as RCM's downscale to increasingly higher resolutions, the conjunction between <span class="hlt">weather</span> and climate becomes more problematic. We present results from a series of present-day climate simulations using the WRF ARW for domains that cover North America, much of Latin America, and South Asia. The basic domains are at a 12 km resolution, but several inner domains at 4 km have also been simulated. These include regions of complex topography in Mexico, Colombia, Peru, and Sri Lanka, as well as a region of low topography and fairly homogeneous land surface type (the U.S. Great Plains). <span class="hlt">Model</span> evaluations are performed using standard climate analyses (e.g., reanalyses; NCDC data) but also using time series of daily station observations. Preliminary results suggest little difference in the assessment of long-term mean quantities, but the variability on seasonal and interannual timescales is better described. Furthermore, the value-added by using daily <span class="hlt">weather</span> observations as an evaluation tool increases with the <span class="hlt">model</span> resolution.« less</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://cfpub.epa.gov/si/si_public_record_report.cfm?dirEntryId=129192&keyword=septic+AND+tank&actType=&TIMSType=+&TIMSSubTypeID=&DEID=&epaNumber=&ntisID=&archiveStatus=Both&ombCat=Any&dateBeginCreated=&dateEndCreated=&dateBeginPublishedPresented=&dateEndPublishedPresented=&dateBeginUpdated=&dateEndUpdated=&dateBeginCompleted=&dateEndCompleted=&personID=&role=Any&journalID=&publisherID=&sortBy=revisionDate&count=50','EPA-EIMS'); return false;" href="https://cfpub.epa.gov/si/si_public_record_report.cfm?dirEntryId=129192&keyword=septic+AND+tank&actType=&TIMSType=+&TIMSSubTypeID=&DEID=&epaNumber=&ntisID=&archiveStatus=Both&ombCat=Any&dateBeginCreated=&dateEndCreated=&dateBeginPublishedPresented=&dateEndPublishedPresented=&dateBeginUpdated=&dateEndUpdated=&dateBeginCompleted=&dateEndCompleted=&personID=&role=Any&journalID=&publisherID=&sortBy=revisionDate&count=50"><span>INVESTIGATION OF DRY-<span class="hlt">WEATHER</span> POLLUTANT ENTRIES INTO STORM-DRAINAGE <span class="hlt">SYSTEMS</span></span></a></p> <p><a target="_blank" href="http://oaspub.epa.gov/eims/query.page">EPA Science Inventory</a></p> <p></p> <p></p> <p>This article describes the results of a series of research tasks to develop a procedure to investigate non-stormwater (dry-<span class="hlt">weather</span>) entries into storm drainage <span class="hlt">systems</span>. Dry-<span class="hlt">weather</span> flows discharging from storm drainage <span class="hlt">systems</span> can contribute significant pollutant loadings to rece...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017DPS....4941813H','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017DPS....4941813H"><span>Large-Scale Traveling <span class="hlt">Weather</span> <span class="hlt">Systems</span> in Mars’ Southern Extratropics</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Hollingsworth, Jeffery L.; Kahre, Melinda A.</p> <p>2017-10-01</p> <p>Between late fall and early spring, Mars’ middle- and high-latitude atmosphere supports strong mean equator-to-pole temperature contrasts and an accompanying mean westerly polar vortex. Observations from both the MGS Thermal Emission Spectrometer (TES) and the MRO Mars Climate Sounder (MCS) indicate that a mean baroclinicity-barotropicity supports intense, large-scale eastward traveling <span class="hlt">weather</span> <span class="hlt">systems</span> (i.e., transient synoptic-period waves). Such extratropical <span class="hlt">weather</span> disturbances are critical components of the global circulation as they serve as agents in the transport of heat and momentum, and generalized scalar/tracer quantities (e.g., atmospheric dust, water-vapor and ice clouds). The character of such traveling extratropical synoptic disturbances in Mars' southern hemisphere during late winter through early spring is investigated using a moderately high-resolution Mars global climate <span class="hlt">model</span> (Mars GCM). This Mars GCM imposes interactively-lifted and radiatively-active dust based on a threshold value of the surface stress. The <span class="hlt">model</span> exhibits a reasonable "dust cycle" (i.e., globally averaged, a dustier atmosphere during southern spring and summer occurs). Compared to the northern-hemisphere counterparts, the southern synoptic-period <span class="hlt">weather</span> disturbances and accompanying frontal waves have smaller meridional and zonal scales, and are far less intense. Influences of the zonally asymmetric (i.e., east-west varying) topography on southern large-scale <span class="hlt">weather</span> are investigated, in addition to large-scale up-slope/down-slope flows and the diurnal cycle. A southern storm zone in late winter and early spring presents in the western hemisphere via orographic influences from the Tharsis highlands, and the Argyre and Hellas impact basins. Geographically localized transient-wave activity diagnostics are constructed that illuminate dynamical differences amongst the simulations and these are presented.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/20170010231','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/20170010231"><span>Large-Scale Traveling <span class="hlt">Weather</span> <span class="hlt">Systems</span> in Mars Southern Extratropics</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Hollingsworth, Jeffery L.; Kahre, Melinda A.</p> <p>2017-01-01</p> <p>Between late fall and early spring, Mars' middle- and high-latitude atmosphere supports strong mean equator-to-pole temperature contrasts and an accompanying mean westerly polar vortex. Observations from both the MGS Thermal Emission Spectrometer (TES) and the MRO Mars Climate Sounder (MCS) indicate that a mean baroclinicity-barotropicity supports intense, large-scale eastward traveling <span class="hlt">weather</span> <span class="hlt">systems</span> (i.e., transient synoptic-period waves). Such extratropical <span class="hlt">weather</span> disturbances are critical components of the global circulation as they serve as agents in the transport of heat and momentum, and generalized scalar/tracer quantities (e.g., atmospheric dust, water-vapor and ice clouds). The character of such traveling extratropical synoptic disturbances in Mars' southern hemisphere during late winter through early spring is investigated using a moderately high-resolution Mars global climate <span class="hlt">model</span> (Mars GCM). This Mars GCM imposes interactively-lifted and radiatively-active dust based on a threshold value of the surface stress. The <span class="hlt">model</span> exhibits a reasonable "dust cycle" (i.e., globally averaged, a dustier atmosphere during southern spring and summer occurs). Compared to the northern-hemisphere counterparts, the southern synoptic-period <span class="hlt">weather</span> disturbances and accompanying frontal waves have smaller meridional and zonal scales, and are far less intense. Influences of the zonally asymmetric (i.e., east-west varying) topography on southern large-scale <span class="hlt">weather</span> are investigated, in addition to large-scale up-slope/down-slope flows and the diurnal cycle. A southern storm zone in late winter and early spring presents in the western hemisphere via orographic influences from the Tharsis highlands, and the Argyre and Hellas impact basins. Geographically localized transient-wave activity diagnostics are constructed that illuminate dynamical differences amongst the simulations and these are presented.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2012EGUGA..1410327S','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2012EGUGA..1410327S"><span>Performance of a coupled lagged ensemble <span class="hlt">weather</span> and river runoff prediction <span class="hlt">model</span> <span class="hlt">system</span> for the Alpine Ammer River catchment</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Smiatek, G.; Kunstmann, H.; Werhahn, J.</p> <p>2012-04-01</p> <p>The Ammer River catchment located in the Bavarian Ammergau Alps and alpine forelands, Germany, represents with elevations reaching 2185 m and annual mean precipitation between1100 and 2000 mm a very demanding test ground for a river runoff prediction <span class="hlt">system</span>. Large flooding events in 1999 and 2005 motivated the development of a physically based prediction tool in this area. Such a tool is the coupled high resolution numerical <span class="hlt">weather</span> and river runoff forecasting <span class="hlt">system</span> AM-POE that is being studied in several configurations in various experiments starting from the year 2005. Corner stones of the coupled <span class="hlt">system</span> are the hydrological water balance <span class="hlt">model</span> WaSiM-ETH run at 100 m grid resolution, the numerical <span class="hlt">weather</span> prediction <span class="hlt">model</span> (NWP) MM5 driven at 3.5 km grid cell resolution and the Perl Object Environment (POE) framework. POE implements the input data download from various sources, the input data provision via SOAP based WEB services as well as the runs of the hydrology <span class="hlt">model</span> both with observed and with NWP predicted meteorology input. The one way coupled <span class="hlt">system</span> utilizes a lagged ensemble prediction <span class="hlt">system</span> (EPS) taking into account combination of recent and previous NWP forecasts. Results obtained in the years 2005-2011 reveal that river runoff simulations depict high correlation with observed runoff when driven with monitored observations in hindcast experiments. The ability to runoff forecasts is depending on lead times in the lagged ensemble prediction and shows still limitations resulting from errors in timing and total amount of the predicted precipitation in the complex mountainous area. The presentation describes the <span class="hlt">system</span> implementation, and demonstrates the application of the POE framework in networking, distributed computing and in the setup of various experiments as well as long term results of the <span class="hlt">system</span> application in the years 2005 - 2011.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2012AGUFM.A41I0100D','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2012AGUFM.A41I0100D"><span>Generation of Multivariate Surface <span class="hlt">Weather</span> Series with Use of the Stochastic <span class="hlt">Weather</span> Generator Linked to Regional Climate <span class="hlt">Model</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Dubrovsky, M.; Farda, A.; Huth, R.</p> <p>2012-12-01</p> <p>The regional-scale simulations of <span class="hlt">weather</span>-sensitive processes (e.g. hydrology, agriculture and forestry) for the present and/or future climate often require high resolution meteorological inputs in terms of the time series of selected surface <span class="hlt">weather</span> characteristics (typically temperature, precipitation, solar radiation, humidity, wind) for a set of stations or on a regular grid. As even the latest Global and Regional Climate <span class="hlt">Models</span> (GCMs and RCMs) do not provide realistic representation of statistical structure of the surface <span class="hlt">weather</span>, the <span class="hlt">model</span> outputs must be postprocessed (downscaled) to achieve the desired statistical structure of the <span class="hlt">weather</span> data before being used as an input to the follow-up simulation <span class="hlt">models</span>. One of the downscaling approaches, which is employed also here, is based on a <span class="hlt">weather</span> generator (WG), which is calibrated using the observed <span class="hlt">weather</span> series and then modified (in case of simulations for the future climate) according to the GCM- or RCM-based climate change scenarios. The present contribution uses the parametric daily <span class="hlt">weather</span> generator M&Rfi to follow two aims: (1) Validation of the new simulations of the present climate (1961-1990) made by the ALADIN-Climate/CZ (v.2) Regional Climate <span class="hlt">Model</span> at 25 km resolution. The WG parameters will be derived from the RCM-simulated surface <span class="hlt">weather</span> series and compared to those derived from observational data in the Czech meteorological stations. The set of WG parameters will include selected statistics of the surface temperature and precipitation (characteristics of the mean, variability, interdiurnal variability and extremes). (2) Testing a potential of RCM output for calibration of the WG for the ungauged locations. The methodology being examined will consist in using the WG, whose parameters are interpolated from the surrounding stations and then corrected based on a RCM-simulated spatial variability. The quality of the <span class="hlt">weather</span> series produced by the WG calibrated in this way will be assessed in terms</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/20160003298','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/20160003298"><span>Space <span class="hlt">Weathering</span> on Icy Satellites in the Outer Solar <span class="hlt">System</span></span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Clark, R. N.; Perlman, Z.; Pearson, N.; Cruikshank, D. P.</p> <p>2014-01-01</p> <p>Space <span class="hlt">weathering</span> produces well-known optical effects in silicate minerals in the inner Solar <span class="hlt">System</span>, for example, on the Moon. Space <span class="hlt">weathering</span> from solar wind and UV (ultraviolet radiation) is expected to be significantly weaker in the outer Solar <span class="hlt">System</span> simply because intensities are low. However, cosmic rays and micrometeoroid bombardment would be similar to first order. That, combined with the much higher volatility of icy surfaces means there is the potential for space <span class="hlt">weathering</span> on icy outer Solar <span class="hlt">System</span> surfaces to show optical effects. The Cassini spacecraft orbiting Saturn is providing evidence for space <span class="hlt">weathering</span> on icy bodies. The Cassini Visible and Infrared Mapping Spectrometer (VIMS) instrument has spatially mapped satellite surfaces and the rings from 0.35-5 microns and the Ultraviolet Imaging Spectrograph (UVIS) instrument from 0.1 to 0.2 microns. These data have sampled a complex mixing space between H2O ice and non-ice components and they show some common spectral properties. Similarly, spectra of the icy Galilean satellites and satellites in the Uranian <span class="hlt">system</span> have some commonality in spectral properties with those in the Saturn <span class="hlt">system</span>. The UV absorber is spectrally similar on many surfaces. VIMS has identified CO2, H2 and trace organics in varying abundances on Saturn's satellites. We postulate that through the spatial relationships of some of these compounds that they are created and destroyed through space <span class="hlt">weathering</span> effects. For example, the trapped H2 and CO2 observed by VIMS in regions with high concentrations of dark material may in part be space <span class="hlt">weathering</span> products from the destruction of H2O and organic molecules. The dark material, particularly on Iapetus which has the highest concentration in the Saturn <span class="hlt">system</span>, is well matched by space-<span class="hlt">weathered</span> silicates in the .4 to 2.6 micron range, and the spectral shapes closely match those of the most mature lunar soils, another indicator of space <span class="hlt">weathered</span> material.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017GeCoA.217..421H','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017GeCoA.217..421H"><span>A reactive transport <span class="hlt">model</span> for Marcellus shale <span class="hlt">weathering</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Heidari, Peyman; Li, Li; Jin, Lixin; Williams, Jennifer Z.; Brantley, Susan L.</p> <p>2017-11-01</p> <p>Shale formations account for 25% of the land surface globally and contribute a large proportion of the natural gas used in the United States. One of the most productive shale-gas formations is the Marcellus, a black shale that is rich in organic matter and pyrite. As a first step toward understanding how Marcellus shale interacts with water in the surface or deep subsurface, we developed a reactive transport <span class="hlt">model</span> to simulate shale <span class="hlt">weathering</span> under ambient temperature and pressure conditions, constrained by soil and water chemistry data. The simulation was carried out for 10,000 years since deglaciation, assuming bedrock <span class="hlt">weathering</span> and soil genesis began after the last glacial maximum. Results indicate <span class="hlt">weathering</span> was initiated by pyrite dissolution for the first 1000 years, leading to low pH and enhanced dissolution of chlorite and precipitation of iron hydroxides. After pyrite depletion, chlorite dissolved slowly, primarily facilitated by the presence of CO2 and organic acids, forming vermiculite as a secondary mineral. A sensitivity analysis indicated that the most important controls on <span class="hlt">weathering</span> include the presence of reactive gases (CO2 and O2), specific surface area, and flow velocity of infiltrating meteoric water. The soil chemistry and mineralogy data could not be reproduced without including the reactive gases. For example, pyrite remained in the soil even after 10,000 years if O2 was not continuously present in the soil column; likewise, chlorite remained abundant and porosity remained small if CO2 was not present in the soil gas. The field observations were only simulated successfully when the <span class="hlt">modeled</span> specific surface areas of the reactive minerals were 1-3 orders of magnitude smaller than surface area values measured for powdered minerals. Small surface areas could be consistent with the lack of accessibility of some fluids to mineral surfaces due to surface coatings. In addition, some mineral surface is likely interacting only with equilibrated pore</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2012EGUGA..14.8361G','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2012EGUGA..14.8361G"><span>Numerical <span class="hlt">Weather</span> Prediction <span class="hlt">Models</span> on Linux Boxes as tools in meteorological education in Hungary</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Gyongyosi, A. Z.; Andre, K.; Salavec, P.; Horanyi, A.; Szepszo, G.; Mille, M.; Tasnadi, P.; Weidiger, T.</p> <p>2012-04-01</p> <p>. Numerical <span class="hlt">modeling</span> became a common tool in the daily practice of <span class="hlt">weather</span> experts forecasters due to the i) increasing user demands for <span class="hlt">weather</span> data by the costumers, ii) the growth in computer resources, iii) numerical <span class="hlt">weather</span> prediction <span class="hlt">systems</span> available for integration on affordable, off the shelf computers and iv) available input data (from ECMWF or NCEP) for <span class="hlt">model</span> integrations. Beside learning the theoretical basis, since the last year. Students in their MSc or BSc Thesis Research or in Student's Research ProjectsStudent's Research Projects h have the opportunity to run numerical <span class="hlt">models</span> and to analyze the outputs for different purposes including wind energy estimation, simulation of the dynamics of a polar low, and subtropical cyclones, analysis of the isentropic potential vorticity field, examination of coupled atmospheric dispersion <span class="hlt">models</span>, etc. A special course in the application of numerical <span class="hlt">modeling</span> has been held (is being announced for the upcoming semester) (is being announced for the upcoming semester) for our students in order to improve their skills on this field. Several numerical <span class="hlt">model</span> (NRIPR ETA and WRF) <span class="hlt">systems</span> have been adapted in the University and integrated WRF have been tested and used for the geographical region of the Carpathian Basin (NRIPR, ETA and WRF). Recently ALADIN/CHAPEAU the academic version of the ARPEGE ALADIN cy33t1 meso-scale numerical <span class="hlt">weather</span> prediction <span class="hlt">model</span> <span class="hlt">system</span> (which is the operational forecasting tool of our National <span class="hlt">Weather</span> Service) has been installed at our Institute. ALADIN is the operational forecasting <span class="hlt">model</span> of the Hungarian Meteorological Service and developed in the framework of the international ALADIN co-operation. Our main objectives are i) the analysis of different typical <span class="hlt">weather</span> situations, ii) fine tuning of parameterization schemes and the iii) comparison of the ALADIN/CHAPEAU and WRF <span class="hlt">model</span> outputs based on case studies. The necessary hardware and software innovations has have been done. In the presentation the</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2016AGUFM.H13E1428I','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2016AGUFM.H13E1428I"><span><span class="hlt">Modelling</span> unsaturated/saturated flow in <span class="hlt">weathered</span> profiles</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Ireson, A. M.; Ali, M. A.; Van Der Kamp, G.</p> <p>2016-12-01</p> <p>Vertical <span class="hlt">weathering</span> profiles are a common feature of many geological materials, where the fracture or macropore porosity decreases progressively below the ground surface. The <span class="hlt">weathered</span> near surface zone (WNSZ) has an enhanced storage and permeability. When the water table is deep, the WNSZ can act to buffer recharge. When the water table is shallow, intersecting the WNSZ, transmissivity and lateral saturated flow, increase with increasing water table elevation. Such a situation exists in the glacial till dominated landscapes of the Canadian prairies, effectively resulting in dynamic patterns of subsurface connectivity. Using dual permeability hydraulic properties with vertically scaled macroporosity, we show how the WNSZ can be represented in <span class="hlt">models</span>. The resulting <span class="hlt">model</span> can be more parsimonious than an equivalent <span class="hlt">model</span> with two or more discrete layers, and more physically realistic. We implement our <span class="hlt">model</span> in PARFLOW-CLM, and apply the <span class="hlt">model</span> to a field site in the Canadian prairies. We are able to convincingly simulate shallow groundwater dynamics, and spatio-temporal patterns of groundwater connectivity.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2002iaf..confE.145L','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2002iaf..confE.145L"><span>COSMIC Payload in NCAR-NASPO GPS Satellite <span class="hlt">System</span> for Severe <span class="hlt">Weather</span> Prediction</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Lai-Chen, C.</p> <p></p> <p>Severe <span class="hlt">weather</span>, such as cyclones, heavy rainfall, outburst of cold air, etc., results in great disaster all the world. It is the mission for the scientists to design a warning <span class="hlt">system</span>, to predict the severe <span class="hlt">weather</span> <span class="hlt">systems</span> and to reduce the damage of the society. In Taiwan, National Satellite Project Office (NSPO) initiated ROCSAT-3 program at 1997. She scheduled the Phase I conceptual design to determine the mission for observation <span class="hlt">weather</span> <span class="hlt">system</span>. Cooperating with National Center of Atmospheric Research (NCAR), NSPO involved an international cooperation research and operation program to build a 32 GPS satellites <span class="hlt">system</span>. NCAR will offer 24 GPS satellites. The total expanse will be US 100 millions. NSPO also provide US 80 millions for launching and <span class="hlt">system</span> engineering operation. And NCAR will be responsible for Payload Control Center and Fiducial Network. The cooperative program contract has been signed by Taiwan National Science Council, Taipei Economic Cultural Office of United States and American Institute in Taiwan. One of the payload is COSMIC, Constellation Observation <span class="hlt">System</span> for Meteorology, Ionosphere and Climate. It is a GPS meteorology instrument <span class="hlt">system</span>. The <span class="hlt">system</span> will observe the <span class="hlt">weather</span> information, e. g. electron density profiles, horizontal and vertical TEC and CFT scintillation and communication outage maps. The mission is to obtain the <span class="hlt">weather</span> data such as vertical temperature profiles, water vapor distribution and pressure distribution over the world for global <span class="hlt">weather</span> forecasting, especially during the severe <span class="hlt">weather</span> period. The COSMIC Conference held on November, 1998. The export license was also issued by Department of Commerce of Unites States at November, 1998. Recently, NSPO begun to train their scientists to investigate the <span class="hlt">system</span>. Scientists simulate the observation data to combine the existing routine satellite infrared cloud maps, radar echo and synoptic <span class="hlt">weather</span> analysis for severe <span class="hlt">weather</span> forecasting. It is hopeful to provide more accurate</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2014GeCoA.139..487L','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2014GeCoA.139..487L"><span><span class="hlt">Modeling</span> the influence of organic acids on soil <span class="hlt">weathering</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Lawrence, Corey; Harden, Jennifer; Maher, Kate</p> <p>2014-08-01</p> <p>Biological inputs and organic matter cycling have long been regarded as important factors in the physical and chemical development of soils. In particular, the extent to which low molecular weight organic acids, such as oxalate, influence geochemical reactions has been widely studied. Although the effects of organic acids are diverse, there is strong evidence that organic acids accelerate the dissolution of some minerals. However, the influence of organic acids at the field-scale and over the timescales of soil development has not been evaluated in detail. In this study, a reactive-transport <span class="hlt">model</span> of soil chemical <span class="hlt">weathering</span> and pedogenic development was used to quantify the extent to which organic acid cycling controls mineral dissolution rates and long-term patterns of chemical <span class="hlt">weathering</span>. Specifically, oxalic acid was added to simulations of soil development to investigate a well-studied chronosequence of soils near Santa Cruz, CA. The <span class="hlt">model</span> formulation includes organic acid input, transport, decomposition, organic-metal aqueous complexation and mineral surface complexation in various combinations. Results suggest that although organic acid reactions accelerate mineral dissolution rates near the soil surface, the net response is an overall decrease in chemical <span class="hlt">weathering</span>. <span class="hlt">Model</span> results demonstrate the importance of organic acid input concentrations, fluid flow, decomposition and secondary mineral precipitation rates on the evolution of mineral <span class="hlt">weathering</span> fronts. In particular, <span class="hlt">model</span> soil profile evolution is sensitive to kaolinite precipitation and oxalate decomposition rates. The soil profile-scale <span class="hlt">modeling</span> presented here provides insights into the influence of organic carbon cycling on soil <span class="hlt">weathering</span> and pedogenesis and supports the need for further field-scale measurements of the flux and speciation of reactive organic compounds.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://pubs.er.usgs.gov/publication/70112510','USGSPUBS'); return false;" href="https://pubs.er.usgs.gov/publication/70112510"><span><span class="hlt">Modeling</span> the influence of organic acids on soil <span class="hlt">weathering</span></span></a></p> <p><a target="_blank" href="http://pubs.er.usgs.gov/pubs/index.jsp?view=adv">USGS Publications Warehouse</a></p> <p>Lawrence, Corey R.; Harden, Jennifer W.; Maher, Kate</p> <p>2014-01-01</p> <p>Biological inputs and organic matter cycling have long been regarded as important factors in the physical and chemical development of soils. In particular, the extent to which low molecular weight organic acids, such as oxalate, influence geochemical reactions has been widely studied. Although the effects of organic acids are diverse, there is strong evidence that organic acids accelerate the dissolution of some minerals. However, the influence of organic acids at the field-scale and over the timescales of soil development has not been evaluated in detail. In this study, a reactive-transport <span class="hlt">model</span> of soil chemical <span class="hlt">weathering</span> and pedogenic development was used to quantify the extent to which organic acid cycling controls mineral dissolution rates and long-term patterns of chemical <span class="hlt">weathering</span>. Specifically, oxalic acid was added to simulations of soil development to investigate a well-studied chronosequence of soils near Santa Cruz, CA. The <span class="hlt">model</span> formulation includes organic acid input, transport, decomposition, organic-metal aqueous complexation and mineral surface complexation in various combinations. Results suggest that although organic acid reactions accelerate mineral dissolution rates near the soil surface, the net response is an overall decrease in chemical <span class="hlt">weathering</span>. <span class="hlt">Model</span> results demonstrate the importance of organic acid input concentrations, fluid flow, decomposition and secondary mineral precipitation rates on the evolution of mineral <span class="hlt">weathering</span> fronts. In particular, <span class="hlt">model</span> soil profile evolution is sensitive to kaolinite precipitation and oxalate decomposition rates. The soil profile-scale <span class="hlt">modeling</span> presented here provides insights into the influence of organic carbon cycling on soil <span class="hlt">weathering</span> and pedogenesis and supports the need for further field-scale measurements of the flux and speciation of reactive organic compounds.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2014AGUFMGC43A0679A','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2014AGUFMGC43A0679A"><span>Probabilistic <span class="hlt">Weather</span> Information Tailored to the Needs of Transmission <span class="hlt">System</span> Operators</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Alberts, I.; Stauch, V.; Lee, D.; Hagedorn, R.</p> <p>2014-12-01</p> <p>Reliable and accurate forecasts for wind and photovoltaic (PV) power production are essential for stable transmission <span class="hlt">systems</span>. A high potential for improving the wind and PV power forecasts lies in optimizing the <span class="hlt">weather</span> forecasts, since these energy sources are highly <span class="hlt">weather</span> dependent. For this reason the main objective of the German research project EWeLiNE is to improve the quality the underlying numerical <span class="hlt">weather</span> predictions towards energy operations. In this project, the German Meteorological Service (DWD), the Fraunhofer Institute for Wind Energy and Energy <span class="hlt">System</span> Technology, and three of the German transmission <span class="hlt">system</span> operators (TSOs) are working together to improve the <span class="hlt">weather</span> and power forecasts. Probabilistic predictions are of particular interest, as the quantification of uncertainties provides an important tool for risk management. Theoretical considerations suggest that it can be advantageous to use probabilistic information to represent and respond to the remaining uncertainties in the forecasts. However, it remains a challenge to integrate this information into the decision making processes related to market participation and power <span class="hlt">systems</span> operations. The project is planned and carried out in close cooperation with the involved TSOs in order to ensure the usability of the products developed. It will conclude with a demonstration phase, in which the improved <span class="hlt">models</span> and newly developed products are combined into a process chain and used to provide information to TSOs in a real-time decision support tool. The use of a web-based development platform enables short development cycles and agile adaptation to evolving user needs. This contribution will present the EWeLiNE project and discuss ideas on how to incorporate probabilistic information into the users' current decision making processes.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2015TESS....120004Z','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2015TESS....120004Z"><span>CCMC: Serving research and space <span class="hlt">weather</span> communities with unique space <span class="hlt">weather</span> services, innovative tools and resources</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Zheng, Yihua; Kuznetsova, Maria M.; Pulkkinen, Antti; Maddox, Marlo</p> <p>2015-04-01</p> <p>With the addition of Space <span class="hlt">Weather</span> Research Center (a sub-team within CCMC) in 2010 to address NASA’s own space <span class="hlt">weather</span> needs, CCMC has become a unique entity that not only facilitates research through providing access to the state-of-the-art space science and space <span class="hlt">weather</span> <span class="hlt">models</span>, but also plays a critical role in providing unique space <span class="hlt">weather</span> services to NASA robotic missions, developing innovative tools and transitioning research to operations via user feedback. With scientists, forecasters and software developers working together within one team, through close and direct connection with space <span class="hlt">weather</span> customers and trusted relationship with <span class="hlt">model</span> developers, CCMC is flexible, nimble and effective to meet customer needs. In this presentation, we highlight a few unique aspects of CCMC/SWRC’s space <span class="hlt">weather</span> services, such as addressing space <span class="hlt">weather</span> throughout the solar <span class="hlt">system</span>, pushing the frontier of space <span class="hlt">weather</span> forecasting via the ensemble approach, providing direct personnel and tool support for spacecraft anomaly resolution, prompting development of multi-purpose tools and knowledge bases, and educating and engaging the next generation of space <span class="hlt">weather</span> scientists.</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://rosap.ntl.bts.gov/view/dot/2643','DOTNTL'); return false;" href="https://rosap.ntl.bts.gov/view/dot/2643"><span>Improving the Wyoming Road <span class="hlt">Weather</span> Information <span class="hlt">System</span></span></a></p> <p><a target="_blank" href="http://ntlsearch.bts.gov/tris/index.do">DOT National Transportation Integrated Search</a></p> <p></p> <p>1998-11-01</p> <p>A two-year study of the Wyoming Road <span class="hlt">Weather</span> Information <span class="hlt">System</span> (RWIS) indicated that the <span class="hlt">system</span> will facilitate and improve maintenance operations and enhance the safety and convenience of highway travel if certain critical improvements are made. Wi...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/25581272','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/25581272"><span>Public Health <span class="hlt">System</span> Response to Extreme <span class="hlt">Weather</span> Events.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Hunter, Mark D; Hunter, Jennifer C; Yang, Jane E; Crawley, Adam W; Aragón, Tomás J</p> <p>2016-01-01</p> <p>Extreme <span class="hlt">weather</span> events, unpredictable and often far-reaching, constitute a persistent challenge for public health preparedness. The goal of this research is to inform public health <span class="hlt">systems</span> improvement through examination of extreme <span class="hlt">weather</span> events, comparing across cases to identify recurring patterns in event and response characteristics. Structured telephone-based interviews were conducted with representatives from health departments to assess characteristics of recent extreme <span class="hlt">weather</span> events and agencies' responses. Response activities were assessed using the Centers for Disease Control and Prevention Public Health Emergency Preparedness Capabilities framework. Challenges that are typical of this response environment are reported. Forty-five local health departments in 20 US states. Respondents described public health <span class="hlt">system</span> responses to 45 events involving tornadoes, flooding, wildfires, winter <span class="hlt">weather</span>, hurricanes, and other storms. Events of similar scale were infrequent for a majority (62%) of the communities involved; disruption to critical infrastructure was universal. Public Health Emergency Preparedness Capabilities considered most essential involved environmental health investigations, mass care and sheltering, surveillance and epidemiology, information sharing, and public information and warning. Unanticipated response activities or operational constraints were common. We characterize extreme <span class="hlt">weather</span> events as a "quadruple threat" because (1) direct threats to population health are accompanied by damage to public health protective and community infrastructure, (2) event characteristics often impose novel and pervasive burdens on communities, (3) responses rely on critical infrastructures whose failure both creates new burdens and diminishes response capacity, and (4) their infrequency and scale further compromise response capacity. Given the challenges associated with extreme <span class="hlt">weather</span> events, we suggest opportunities for organizational learning and</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/17604645','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/17604645"><span><span class="hlt">Weather</span> variability and the incidence of cryptosporidiosis: comparison of time series poisson regression and SARIMA <span class="hlt">models</span>.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Hu, Wenbiao; Tong, Shilu; Mengersen, Kerrie; Connell, Des</p> <p>2007-09-01</p> <p>Few studies have examined the relationship between <span class="hlt">weather</span> variables and cryptosporidiosis in Australia. This paper examines the potential impact of <span class="hlt">weather</span> variability on the transmission of cryptosporidiosis and explores the possibility of developing an empirical forecast <span class="hlt">system</span>. Data on <span class="hlt">weather</span> variables, notified cryptosporidiosis cases, and population size in Brisbane were supplied by the Australian Bureau of Meteorology, Queensland Department of Health, and Australian Bureau of Statistics for the period of January 1, 1996-December 31, 2004, respectively. Time series Poisson regression and seasonal auto-regression integrated moving average (SARIMA) <span class="hlt">models</span> were performed to examine the potential impact of <span class="hlt">weather</span> variability on the transmission of cryptosporidiosis. Both the time series Poisson regression and SARIMA <span class="hlt">models</span> show that seasonal and monthly maximum temperature at a prior moving average of 1 and 3 months were significantly associated with cryptosporidiosis disease. It suggests that there may be 50 more cases a year for an increase of 1 degrees C maximum temperature on average in Brisbane. <span class="hlt">Model</span> assessments indicated that the SARIMA <span class="hlt">model</span> had better predictive ability than the Poisson regression <span class="hlt">model</span> (SARIMA: root mean square error (RMSE): 0.40, Akaike information criterion (AIC): -12.53; Poisson regression: RMSE: 0.54, AIC: -2.84). Furthermore, the analysis of residuals shows that the time series Poisson regression appeared to violate a <span class="hlt">modeling</span> assumption, in that residual autocorrelation persisted. The results of this study suggest that <span class="hlt">weather</span> variability (particularly maximum temperature) may have played a significant role in the transmission of cryptosporidiosis. A SARIMA <span class="hlt">model</span> may be a better predictive <span class="hlt">model</span> than a Poisson regression <span class="hlt">model</span> in the assessment of the relationship between <span class="hlt">weather</span> variability and the incidence of cryptosporidiosis.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/20110020261','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/20110020261"><span>Integration of <span class="hlt">Weather</span> Avoidance and Traffic Separation</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Consiglio, Maria C.; Chamberlain, James P.; Wilson, Sara R.</p> <p>2011-01-01</p> <p>This paper describes a dynamic convective <span class="hlt">weather</span> avoidance concept that compensates for <span class="hlt">weather</span> motion uncertainties; the integration of this <span class="hlt">weather</span> avoidance concept into a prototype 4-D trajectory-based Airborne Separation Assurance <span class="hlt">System</span> (ASAS) application; and test results from a batch (non-piloted) simulation of the integrated application with high traffic densities and a dynamic convective <span class="hlt">weather</span> <span class="hlt">model</span>. The <span class="hlt">weather</span> <span class="hlt">model</span> can simulate a number of pseudo-random hazardous <span class="hlt">weather</span> patterns, such as slow- or fast-moving cells and opening or closing <span class="hlt">weather</span> gaps, and also allows for <span class="hlt">modeling</span> of onboard <span class="hlt">weather</span> radar limitations in range and azimuth. The <span class="hlt">weather</span> avoidance concept employs nested "core" and "avoid" polygons around convective <span class="hlt">weather</span> cells, and the simulations assess the effectiveness of various avoid polygon sizes in the presence of different <span class="hlt">weather</span> patterns, using traffic scenarios representing approximately two times the current traffic density in en-route airspace. Results from the simulation experiment show that the <span class="hlt">weather</span> avoidance concept is effective over a wide range of <span class="hlt">weather</span> patterns and cell speeds. Avoid polygons that are only 2-3 miles larger than their core polygons are sufficient to account for <span class="hlt">weather</span> uncertainties in almost all cases, and traffic separation performance does not appear to degrade with the addition of <span class="hlt">weather</span> polygon avoidance. Additional "lessons learned" from the batch simulation study are discussed in the paper, along with insights for improving the <span class="hlt">weather</span> avoidance concept. Introduction</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2018OcDyn..68...91G','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2018OcDyn..68...91G"><span>Evaluation of <span class="hlt">weather</span> forecast <span class="hlt">systems</span> for storm surge <span class="hlt">modeling</span> in the Chesapeake Bay</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Garzon, Juan L.; Ferreira, Celso M.; Padilla-Hernandez, Roberto</p> <p>2018-01-01</p> <p>Accurate forecast of sea-level heights in coastal areas depends, among other factors, upon a reliable coupling of a meteorological forecast <span class="hlt">system</span> to a hydrodynamic and wave <span class="hlt">system</span>. This study evaluates the predictive skills of the coupled circulation and wind-wave <span class="hlt">model</span> <span class="hlt">system</span> (ADCIRC+SWAN) for simulating storm tides in the Chesapeake Bay, forced by six different products: (1) Global Forecast <span class="hlt">System</span> (GFS), (2) Climate Forecast <span class="hlt">System</span> (CFS) version 2, (3) North American Mesoscale Forecast <span class="hlt">System</span> (NAM), (4) Rapid Refresh (RAP), (5) European Center for Medium-Range <span class="hlt">Weather</span> Forecasts (ECMWF), and (6) the Atlantic hurricane database (HURDAT2). This evaluation is based on the hindcasting of four events: Irene (2011), Sandy (2012), Joaquin (2015), and Jonas (2016). By comparing the simulated water levels to observations at 13 monitoring stations, we have found that the ADCIR+SWAN <span class="hlt">System</span> forced by the following: (1) the HURDAT2-based <span class="hlt">system</span> exhibited the weakest statistical skills owing to a noteworthy overprediction of the simulated wind speed; (2) the ECMWF, RAP, and NAM products captured the moment of the peak and moderately its magnitude during all storms, with a correlation coefficient ranging between 0.98 and 0.77; (3) the CFS <span class="hlt">system</span> exhibited the worst averaged root-mean-square difference (excepting HURDAT2); (4) the GFS <span class="hlt">system</span> (the lowest horizontal resolution product tested) resulted in a clear underprediction of the maximum water elevation. Overall, the simulations forced by NAM and ECMWF <span class="hlt">systems</span> induced the most accurate results best accuracy to support water level forecasting in the Chesapeake Bay during both tropical and extra-tropical storms.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2016HESS...20.4707Z','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2016HESS...20.4707Z"><span>Coupled hydro-meteorological <span class="hlt">modelling</span> on a HPC platform for high-resolution extreme <span class="hlt">weather</span> impact study</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Zhu, Dehua; Echendu, Shirley; Xuan, Yunqing; Webster, Mike; Cluckie, Ian</p> <p>2016-11-01</p> <p>Impact-focused studies of extreme <span class="hlt">weather</span> require coupling of accurate simulations of <span class="hlt">weather</span> and climate <span class="hlt">systems</span> and impact-measuring hydrological <span class="hlt">models</span> which themselves demand larger computer resources. In this paper, we present a preliminary analysis of a high-performance computing (HPC)-based hydrological <span class="hlt">modelling</span> approach, which is aimed at utilizing and maximizing HPC power resources, to support the study on extreme <span class="hlt">weather</span> impact due to climate change. Here, four case studies are presented through implementation on the HPC Wales platform of the UK mesoscale meteorological Unified <span class="hlt">Model</span> (UM) with high-resolution simulation suite UKV, alongside a Linux-based hydrological <span class="hlt">model</span>, Hydrological Predictions for the Environment (HYPE). The results of this study suggest that the coupled hydro-meteorological <span class="hlt">model</span> was still able to capture the major flood peaks, compared with the conventional gauge- or radar-driving forecast, but with the added value of much extended forecast lead time. The high-resolution rainfall estimation produced by the UKV performs similarly to that of radar rainfall products in the first 2-3 days of tested flood events, but the uncertainties particularly increased as the forecast horizon goes beyond 3 days. This study takes a step forward to identify how the online mode approach can be used, where both numerical <span class="hlt">weather</span> prediction and the hydrological <span class="hlt">model</span> are executed, either simultaneously or on the same hardware infrastructures, so that more effective interaction and communication can be achieved and maintained between the <span class="hlt">models</span>. But the concluding comments are that running the entire <span class="hlt">system</span> on a reasonably powerful HPC platform does not yet allow for real-time simulations, even without the most complex and demanding data simulation part.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/20030102266','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/20030102266"><span>Prevention of Spacecraft Anomalies: The Role of Space Climate and Space <span class="hlt">Weather</span> <span class="hlt">Models</span></span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Barth, Janet L.</p> <p>2003-01-01</p> <p>Space-based <span class="hlt">systems</span> are developing into critical infrastructure to support the quality of life on Earth. Mission requirements along with rapidly evolving technologies have outpaced efforts to accommodate detrimental space environment impacts on <span class="hlt">systems</span>. This chapter describes approaches to accommodate space climate and space <span class="hlt">weather</span> impacts on <span class="hlt">systems</span> and notes areas where gaps in <span class="hlt">model</span> development limit our ability to prevent spacecraft anomalies.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/28932771','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/28932771"><span>Urban <span class="hlt">weather</span> data and building <span class="hlt">models</span> for the inclusion of the urban heat island effect in building performance simulation.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Palme, M; Inostroza, L; Villacreses, G; Lobato, A; Carrasco, C</p> <p>2017-10-01</p> <p>This data article presents files supporting calculation for urban heat island (UHI) inclusion in building performance simulation (BPS). Methodology is used in the research article "From urban climate to energy consumption. Enhancing building performance simulation by including the urban heat island effect" (Palme et al., 2017) [1]. In this research, a Geographical Information <span class="hlt">System</span> (GIS) study is done in order to statistically represent the most important urban scenarios of four South-American cities (Guayaquil, Lima, Antofagasta and Valparaíso). Then, a Principal Component Analysis (PCA) is done to obtain reference Urban Tissues Categories (UTC) to be used in urban <span class="hlt">weather</span> simulation. The urban <span class="hlt">weather</span> files are generated by using the Urban <span class="hlt">Weather</span> Generator (UWG) software (version 4.1 beta). Finally, BPS is run out with the Transient <span class="hlt">System</span> Simulation (TRNSYS) software (version 17). In this data paper, four sets of data are presented: 1) PCA data (excel) to explain how to group different urban samples in representative UTC; 2) UWG data (text) to reproduce the Urban <span class="hlt">Weather</span> Generation for the UTC used in the four cities (4 UTC in Lima, Guayaquil, Antofagasta and 5 UTC in Valparaíso); 3) <span class="hlt">weather</span> data (text) with the resulting rural and urban <span class="hlt">weather</span>; 4) BPS <span class="hlt">models</span> (text) data containing the TRNSYS <span class="hlt">models</span> (four building <span class="hlt">models</span>).</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2015AGUFMEP33D..01W','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2015AGUFMEP33D..01W"><span>A Physically Based Coupled Chemical and Physical <span class="hlt">Weathering</span> <span class="hlt">Model</span> for Simulating Soilscape Evolution</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Willgoose, G. R.; Welivitiya, D.; Hancock, G. R.</p> <p>2015-12-01</p> <p>A critical missing link in existing landscape evolution <span class="hlt">models</span> is a dynamic soil evolution <span class="hlt">models</span> where soils co-evolve with the landform. Work by the authors over the last decade has demonstrated a computationally manageable <span class="hlt">model</span> for soil profile evolution (soilscape evolution) based on physical <span class="hlt">weathering</span>. For chemical <span class="hlt">weathering</span> it is clear that full geochemistry <span class="hlt">models</span> such as CrunchFlow and PHREEQC are too computationally intensive to be couplable to existing soilscape and landscape evolution <span class="hlt">models</span>. This paper presents a simplification of CrunchFlow chemistry and physics that makes the task feasible, and generalises it for hillslope geomorphology applications. Results from this simplified <span class="hlt">model</span> will be compared with field data for soil pedogenesis. Other researchers have previously proposed a number of very simple <span class="hlt">weathering</span> functions (e.g. exponential, humped, reverse exponential) as conceptual <span class="hlt">models</span> of the in-profile <span class="hlt">weathering</span> process. The paper will show that all of these functions are possible for specific combinations of in-soil environmental, geochemical and geologic conditions, and the presentation will outline the key variables controlling which of these conceptual <span class="hlt">models</span> can be realistic <span class="hlt">models</span> of in-profile processes and under what conditions. The presentation will finish by discussing the coupling of this <span class="hlt">model</span> with a physical <span class="hlt">weathering</span> <span class="hlt">model</span>, and will show sample results from our SSSPAM soilscape evolution <span class="hlt">model</span> to illustrate the implications of including chemical <span class="hlt">weathering</span> in the soilscape evolution <span class="hlt">model</span>.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/20080017381','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/20080017381"><span>Step 1: Human <span class="hlt">System</span> Integration Pilot-Technology Interface Requirements for <span class="hlt">Weather</span> Management</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p></p> <p>2005-01-01</p> <p>This document involves definition of technology interface requirements for Hazardous <span class="hlt">Weather</span> Avoidance. Technology concepts in use by the Access 5 <span class="hlt">Weather</span> Management Work Package were considered. Beginning with the Human <span class="hlt">System</span> Integration (HIS) high-level functional requirement for Hazardous <span class="hlt">Weather</span> Avoidance, and Hazardous <span class="hlt">Weather</span> Avoidance technology elements, HSI requirements for the interface to the pilot were identified. Results of the analysis describe (1) the information required by the pilot to have knowledge of hazardous <span class="hlt">weather</span>, and (2) the control capability needed by the pilot to obtain hazardous <span class="hlt">weather</span> information. Fundamentally, these requirements provide the candidate Hazardous <span class="hlt">Weather</span> Avoidance technology concepts with the necessary human-related elements to make them compatible with human capabilities and limitations. The results of the analysis describe how Hazardous <span class="hlt">Weather</span> Avoidance operations and functions should interface with the pilot to provide the necessary <span class="hlt">Weather</span> Management functionality to the UA-pilot <span class="hlt">system</span>. Requirements and guidelines for Hazardous <span class="hlt">Weather</span> Avoidance are partitioned into four categories: (1) Planning En Route (2) Encountering Hazardous <span class="hlt">Weather</span> En Route, (3) Planning to Destination, and (4) Diversion Planning Alternate Airport. Each requirement is stated and is supported with a rationale and associated reference(s).</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/20070006538','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/20070006538"><span>Aircraft <span class="hlt">Weather</span> Mitigation for the Next Generation Air Transportation <span class="hlt">System</span></span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Stough, H. Paul, III</p> <p>2007-01-01</p> <p>Atmospheric effects on aviation are described by Mahapatra (1999) as including (1) atmospheric phenomena involving air motion - wind shear and turbulence; (2) hydrometeorological phenomena - rain, snow and hail; (3) aircraft icing; (4) low visibility; and (5) atmospheric electrical phenomena. Aircraft <span class="hlt">Weather</span> Mitigation includes aircraft <span class="hlt">systems</span> (e.g. airframe, propulsion, avionics, controls) that can be enacted (by a pilot, automation or hybrid <span class="hlt">systems</span>) to suppress and/or prepare for the effects of encountered or unavoidable <span class="hlt">weather</span> or to facilitate a crew operational decision-making process relative to <span class="hlt">weather</span>. Aircraft <span class="hlt">weather</span> mitigation can be thought of as a continuum (Figure 1) with the need to avoid all adverse <span class="hlt">weather</span> at one extreme and the ability to safely operate in all <span class="hlt">weather</span> conditions at the other extreme. Realistic aircraft capabilities fall somewhere between these two extremes. The capabilities of small general aviation aircraft would be expected to fall closer to the "Avoid All Adverse <span class="hlt">Weather</span>" point, and the capabilities of large commercial jet transports would fall closer to the "Operate in All <span class="hlt">Weather</span> Conditions" point. The ability to safely operate in adverse <span class="hlt">weather</span> conditions is dependent upon the pilot s capabilities (training, total experience and recent experience), the airspace in which the operation is taking place (terrain, navigational aids, traffic separation), the capabilities of the airport (approach guidance, runway and taxiway lighting, availability of air traffic control), as well as the capabilities of the airplane. The level of mitigation may vary depending upon the type of adverse <span class="hlt">weather</span>. For example, a small general aviation airplane may be equipped to operate "in the clouds" without outside visual references, but not be equipped to prevent airframe ice that could be accreted in those clouds.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/19930016427','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/19930016427"><span>Interactive Forecasting with the National <span class="hlt">Weather</span> Service River Forecast <span class="hlt">System</span></span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Smith, George F.; Page, Donna</p> <p>1993-01-01</p> <p>The National <span class="hlt">Weather</span> Service River Forecast <span class="hlt">System</span> (NWSRFS) consists of several major hydrometeorologic subcomponents to <span class="hlt">model</span> the physics of the flow of water through the hydrologic cycle. The entire NWSRFS currently runs in both mainframe and minicomputer environments, using command oriented text input to control the <span class="hlt">system</span> computations. As computationally powerful and graphically sophisticated scientific workstations became available, the National <span class="hlt">Weather</span> Service (NWS) recognized that a graphically based, interactive environment would enhance the accuracy and timeliness of NWS river and flood forecasts. Consequently, the operational forecasting portion of the NWSRFS has been ported to run under a UNIX operating <span class="hlt">system</span>, with X windows as the display environment on a <span class="hlt">system</span> of networked scientific workstations. In addition, the NWSRFS Interactive Forecast Program was developed to provide a graphical user interface to allow the forecaster to control NWSRFS program flow and to make adjustments to forecasts as necessary. The potential market for water resources forecasting is immense and largely untapped. Any private company able to market the river forecasting technologies currently developed by the NWS Office of Hydrology could provide benefits to many information users and profit from providing these services.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2004JGRD..10919S24U','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2004JGRD..10919S24U"><span>Numerical study of Asian dust transport during the springtime of 2001 simulated with the Chemical <span class="hlt">Weather</span> Forecasting <span class="hlt">System</span> (CFORS) <span class="hlt">model</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Uno, Itsushi; Satake, Shinsuke; Carmichael, Gregory R.; Tang, Youhua; Wang, Zifa; Takemura, Toshihiko; Sugimoto, Nobuo; Shimizu, Atsushi; Murayama, Toshiyuki; Cahill, Thomas A.; Cliff, Steven; Uematsu, Mitsuo; Ohta, Sachio; Quinn, Patricia K.; Bates, Timothy S.</p> <p>2004-10-01</p> <p>The regional-scale aerosol transport <span class="hlt">model</span> Chemical <span class="hlt">Weather</span> Forecasting <span class="hlt">System</span> (CFORS) is used for analysis of large-scale dust phenomena during the Asian Pacific Regional Characterization Experiment (ACE-Asia) intensive observation. Dust <span class="hlt">modeling</span> results are examined with the surface <span class="hlt">weather</span> reports, satellite-derived dust index (Total Ozone Mapping Spectrometer (TOMS) Aerosol Index (AI)), Mie-scattering lidar observation, and surface aerosol observations. The CFORS dust results are shown to accurately reproduce many of the important observed features. <span class="hlt">Model</span> analysis shows that the simulated dust vertical loading correlates well with TOMS AI and that the dust loading is transported with the meandering of the synoptic-scale temperature field at the 500-hPa level. Quantitative examination of aerosol optical depth shows that <span class="hlt">model</span> predictions are within 20% difference of the lidar observations for the major dust episodes. The structure of the ACE-Asia Perfect Dust Storm, which occurred in early April, is clarified with the help of the CFORS <span class="hlt">model</span> analysis. This storm consisted of two boundary layer components and one elevated dust (>6-km height) feature (resulting from the movement of two large low-pressure <span class="hlt">systems</span>). Time variation of the CFORS dust fields shows the correct onset timing of the elevated dust for each observation site, but the <span class="hlt">model</span> results tend to overpredict dust concentrations at lower latitude sites. The horizontal transport flux at 130°E longitude is examined, and the overall dust transport flux at 130°E during March-April is evaluated to be 55 Tg.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://ntrs.nasa.gov/search.jsp?R=20090012452&hterms=leadership+experience&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D70%26Ntt%3Dleadership%2Bexperience','NASA-TRS'); return false;" href="https://ntrs.nasa.gov/search.jsp?R=20090012452&hterms=leadership+experience&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D70%26Ntt%3Dleadership%2Bexperience"><span>Community <span class="hlt">Modeling</span> Program for Space <span class="hlt">Weather</span>: A CCMC Perspective</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Hesse, Michael</p> <p>2009-01-01</p> <p>A community <span class="hlt">modeling</span> program, which provides a forum for exchange and integration between <span class="hlt">modelers</span>, has excellent potential for furthering our Space <span class="hlt">Weather</span> <span class="hlt">modeling</span> and forecasting capabilities. The design of such a program is of great importance to its success. In this presentation, we will argue that the most effective community <span class="hlt">modeling</span> program should be focused on Space <span class="hlt">Weather</span>-related objectives, and that it should be open and inclusive. The tremendous successes of prior community research activities further suggest that the most effective implementation of a new community <span class="hlt">modeling</span> program should be based on community leadership, rather than on domination by individual institutions or centers. This presentation will provide an experience-based justification for these conclusions.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://www.noaanews.noaa.gov/stories2014/20140930_hrrr.html','SCIGOVWS'); return false;" href="http://www.noaanews.noaa.gov/stories2014/20140930_hrrr.html"><span>NOAA's <span class="hlt">weather</span> forecasts go hyper-local with next-generation <span class="hlt">weather</span></span></a></p> <p><a target="_blank" href="http://www.science.gov/aboutsearch.html">Science.gov Websites</a></p> <p></p> <p></p> <p><em><span class="hlt">model</span></em></A> NOAA HOME <span class="hlt">WEATHER</span> OCEANS FISHERIES CHARTING SATELLITES CLIMATE RESEARCH COASTS CAREERS with next-generation <span class="hlt">weather</span> <em><span class="hlt">model</span></em> New <em><span class="hlt">model</span></em> will help forecasters predict a storm's path, timing and intensity better than ever September 30, 2014 This is a <em>comparison</em> of two <span class="hlt">weather</span> forecast <span class="hlt">models</span> looking</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.osti.gov/pages/biblio/1422964-integration-ram-scb-space-weather-modeling-framework','SCIGOV-DOEP'); return false;" href="https://www.osti.gov/pages/biblio/1422964-integration-ram-scb-space-weather-modeling-framework"><span>Integration of RAM-SCB into the Space <span class="hlt">Weather</span> <span class="hlt">Modeling</span> Framework</span></a></p> <p><a target="_blank" href="http://www.osti.gov/pages">DOE PAGES</a></p> <p>Welling, Daniel; Toth, Gabor; Jordanova, Vania Koleva; ...</p> <p>2018-02-07</p> <p>We present that numerical simulations of the ring current are a challenging endeavor. They require a large set of inputs, including electric and magnetic fields and plasma sheet fluxes. Because the ring current broadly affects the magnetosphere-ionosphere <span class="hlt">system</span>, the input set is dependent on the ring current region itself. This makes obtaining a set of inputs that are self-consistent with the ring current difficult. To overcome this challenge, researchers have begun coupling ring current <span class="hlt">models</span> to global <span class="hlt">models</span> of the magnetosphere-ionosphere <span class="hlt">system</span>. This paper describes the coupling between the Ring current Atmosphere interaction <span class="hlt">Model</span> with Self-Consistent Magnetic field (RAM-SCB) tomore » the <span class="hlt">models</span> within the Space <span class="hlt">Weather</span> <span class="hlt">Modeling</span> Framework. Full details on both previously introduced and new coupling mechanisms are defined. Finally, the impact of self-consistently including the ring current on the magnetosphere-ionosphere <span class="hlt">system</span> is illustrated via a set of example simulations.« less</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.osti.gov/biblio/1422964-integration-ram-scb-space-weather-modeling-framework','SCIGOV-STC'); return false;" href="https://www.osti.gov/biblio/1422964-integration-ram-scb-space-weather-modeling-framework"><span>Integration of RAM-SCB into the Space <span class="hlt">Weather</span> <span class="hlt">Modeling</span> Framework</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>Welling, Daniel; Toth, Gabor; Jordanova, Vania Koleva</p> <p></p> <p>We present that numerical simulations of the ring current are a challenging endeavor. They require a large set of inputs, including electric and magnetic fields and plasma sheet fluxes. Because the ring current broadly affects the magnetosphere-ionosphere <span class="hlt">system</span>, the input set is dependent on the ring current region itself. This makes obtaining a set of inputs that are self-consistent with the ring current difficult. To overcome this challenge, researchers have begun coupling ring current <span class="hlt">models</span> to global <span class="hlt">models</span> of the magnetosphere-ionosphere <span class="hlt">system</span>. This paper describes the coupling between the Ring current Atmosphere interaction <span class="hlt">Model</span> with Self-Consistent Magnetic field (RAM-SCB) tomore » the <span class="hlt">models</span> within the Space <span class="hlt">Weather</span> <span class="hlt">Modeling</span> Framework. Full details on both previously introduced and new coupling mechanisms are defined. Finally, the impact of self-consistently including the ring current on the magnetosphere-ionosphere <span class="hlt">system</span> is illustrated via a set of example simulations.« less</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2006AGUSMIN41A..04F','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2006AGUSMIN41A..04F"><span>A <span class="hlt">Weather</span> Analysis and Forecasting <span class="hlt">System</span> for Baja California, Mexico</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Farfan, L. M.</p> <p>2006-05-01</p> <p>The <span class="hlt">weather</span> of the Baja California Peninsula, part of northwestern Mexico, is mild and dry most of the year. However, during the summer, humid air masses associated with tropical cyclones move northward in the eastern Pacific Ocean. Added features that create a unique meteorological situation include mountain ranges along the spine of the peninsula, warm water in the Gulf of California, and the cold California Current in the Pacific. These features interact with the environmental flow to induce conditions that play a role in the occurrence of localized, convective <span class="hlt">systems</span> during the approach of tropical cyclones. Most of these events occur late in the summer, generating heavy precipitation, strong winds, lightning, and are associated with significant property damage to the local populations. Our goal is to provide information on the characteristics of these <span class="hlt">weather</span> <span class="hlt">systems</span> by performing an analysis of observations derived from a regional network. This includes imagery from radar and geostationary satellite, and data from surface stations. A set of real-time products are generated in our research center and are made available to a broad audience (researchers, students, and business employees) by using an internet site. Graphical products are updated anywhere from one to 24 hours and includes predictions from numerical <span class="hlt">models</span>. Forecasts are derived from an operational <span class="hlt">model</span> (GFS) and locally generated simulations based on a mesoscale <span class="hlt">model</span> (MM5). Our analysis and forecasting <span class="hlt">system</span> has been in operation since the summer of 2005 and was used as a reference for a set of discussions during the development of eastern Pacific tropical cyclones. This basin had 15 named storms and none of them made landfall on the west coast of Mexico; however, four <span class="hlt">systems</span> were within 800 km from the area of interest, resulting in some convective activity. During the whole season, a group of 30 users from our institution, government offices, and local businesses received daily information</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://www.dtic.mil/docs/citations/AD1016607','DTIC-ST'); return false;" href="http://www.dtic.mil/docs/citations/AD1016607"><span>Change in <span class="hlt">Weather</span> Research and Forecasting (WRF) <span class="hlt">Model</span> Accuracy with Age of Input Data from the Global Forecast <span class="hlt">System</span> (GFS)</span></a></p> <p><a target="_blank" href="http://www.dtic.mil/">DTIC Science & Technology</a></p> <p></p> <p>2016-09-01</p> <p>Laboratory Change in <span class="hlt">Weather</span> Research and Forecasting (WRF) <span class="hlt">Model</span> Accuracy with Age of Input Data from the Global Forecast <span class="hlt">System</span> (GFS) by JL Cogan...analysis. As expected, accuracy generally tended to decline as the large-scale data aged , but appeared to improve slightly as the age of the large...19 Table 7 Minimum and maximum mean RMDs for each WRF time (or GFS data age ) category. Minimum and</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/20140001451','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/20140001451"><span>Software for Generating Troposphere Corrections for InSAR Using GPS and <span class="hlt">Weather</span> <span class="hlt">Model</span> Data</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Moore, Angelyn W.; Webb, Frank H.; Fishbein, Evan F.; Fielding, Eric J.; Owen, Susan E.; Granger, Stephanie L.; Bjoerndahl, Fredrik; Loefgren, Johan; Fang, Peng; Means, James D.; <a style="text-decoration: none; " href="javascript:void(0); " onClick="displayelement('author_20140001451'); toggleEditAbsImage('author_20140001451_show'); toggleEditAbsImage('author_20140001451_hide'); "> <img style="display:inline; width:12px; height:12px; " src="images/arrow-up.gif" width="12" height="12" border="0" alt="hide" id="author_20140001451_show"> <img style="width:12px; height:12px; display:none; " src="images/arrow-down.gif" width="12" height="12" border="0" alt="hide" id="author_20140001451_hide"></p> <p>2013-01-01</p> <p>Atmospheric errors due to the troposphere are a limiting error source for spaceborne interferometric synthetic aperture radar (InSAR) imaging. This software generates tropospheric delay maps that can be used to correct atmospheric artifacts in InSAR data. The software automatically acquires all needed GPS (Global Positioning <span class="hlt">System</span>), <span class="hlt">weather</span>, and Digital Elevation Map data, and generates a tropospheric correction map using a novel algorithm for combining GPS and <span class="hlt">weather</span> information while accounting for terrain. Existing JPL software was prototypical in nature, required a MATLAB license, required additional steps to acquire and ingest needed GPS and <span class="hlt">weather</span> data, and did not account for topography in interpolation. Previous software did not achieve a level of automation suitable for integration in a Web portal. This software overcomes these issues. GPS estimates of tropospheric delay are a source of corrections that can be used to form correction maps to be applied to InSAR data, but the spacing of GPS stations is insufficient to remove short-wavelength tropospheric artifacts. This software combines interpolated GPS delay with <span class="hlt">weather</span> <span class="hlt">model</span> precipitable water vapor (PWV) and a digital elevation <span class="hlt">model</span> to account for terrain, increasing the spatial resolution of the tropospheric correction maps and thus removing short wavelength tropospheric artifacts to a greater extent. It will be integrated into a Web portal request <span class="hlt">system</span>, allowing use in a future L-band SAR Earth radar mission data <span class="hlt">system</span>. This will be a significant contribution to its technology readiness, building on existing investments in in situ space geodetic networks, and improving timeliness, quality, and science value of the collected 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_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('http://adsabs.harvard.edu/abs/2017AGUFMEP21H..04L','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017AGUFMEP21H..04L"><span>A Reactive Transport <span class="hlt">Model</span> for Marcellus Shale <span class="hlt">Weathering</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Li, L.; Heidari, P.; Jin, L.; Williams, J.; Brantley, S.</p> <p>2017-12-01</p> <p>Shale formations account for 25% of the land surface globally. One of the most productive shale-gas formations is the Marcellus, a black shale that is rich in organic matter and pyrite. As a first step toward understanding how Marcellus shale interacts with water, we developed a reactive transport <span class="hlt">model</span> to simulate shale <span class="hlt">weathering</span> under ambient temperature and pressure conditions, constrained by soil chemistry and water data. The simulation was carried out for 10,000 years, assuming bedrock <span class="hlt">weathering</span> and soil genesis began right after the last glacial maximum. Results indicate <span class="hlt">weathering</span> was initiated by pyrite dissolution for the first 1,000 years, leading to low pH and enhanced dissolution of chlorite and precipitation of iron hydroxides. After pyrite depletion, chlorite dissolved slowly, primarily facilitated by the presence of CO2 and organic acids, forming vermiculite as a secondary mineral. A sensitivity analysis indicated that the most important controls on <span class="hlt">weathering</span> include the presence of reactive gases (CO2 and O2), specific surface area, and flow velocity of infiltrating meteoric water. The soil chemistry and mineralogy data could not be reproduced without including the reactive gases. For example, pyrite remained in the soil even after 10,000 years if O2 was not continuously present in the soil column; likewise, chlorite remained abundant and porosity remained small with the presence of soil CO2. The field observations were only simulated successfully when the specific surface areas of the reactive minerals were 1-3 orders of magnitude smaller than surface area values measured for powdered minerals, reflecting the lack of accessibility of fluids to mineral surfaces and potential surface coating. An increase in the water infiltration rate enhanced <span class="hlt">weathering</span> by removing dissolution products and maintaining far-from-equilibrium conditions. We conclude that availability of reactive surface area and transport of H2O and gases are the most important</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/28803960','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/28803960"><span>Evaluating impacts of different longitudinal driver assistance <span class="hlt">systems</span> on reducing multi-vehicle rear-end crashes during small-scale inclement <span class="hlt">weather</span>.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Li, Ye; Xing, Lu; Wang, Wei; Wang, Hao; Dong, Changyin; Liu, Shanwen</p> <p>2017-10-01</p> <p>Multi-vehicle rear-end (MVRE) crashes during small-scale inclement (SSI) <span class="hlt">weather</span> cause high fatality rates on freeways, which cannot be solved by traditional speed limit strategies. This study aimed to reduce MVRE crash risks during SSI <span class="hlt">weather</span> using different longitudinal driver assistance <span class="hlt">systems</span> (LDAS). The impact factors on MVRE crashes during SSI <span class="hlt">weather</span> were firstly analyzed. Then, four LDAS, including Forward collision warning (FCW), Autonomous emergency braking (AEB), Adaptive cruise control (ACC) and Cooperative ACC (CACC), were <span class="hlt">modeled</span> based on a unified platform, the Intelligent Driver <span class="hlt">Model</span> (IDM). Simulation experiments were designed and a large number of simulations were then conducted to evaluate safety effects of different LDAS. Results indicate that the FCW and ACC <span class="hlt">system</span> have poor performance on reducing MVRE crashes during SSI <span class="hlt">weather</span>. The slight improvement of sight distance of FCW and the limitation of perception-reaction time of ACC lead the failure of avoiding MVRE crashes in most scenarios. The AEB <span class="hlt">system</span> has the better effect due to automatic perception and reaction, as well as performing the full brake when encountering SSI <span class="hlt">weather</span>. The CACC <span class="hlt">system</span> has the best performance because wireless communication provides a larger sight distance and a shorter time delay at the sub-second level. Sensitivity analyses also indicated that the larger number of vehicles and speed changes after encountering SSI <span class="hlt">weather</span> have negative impacts on safety performances. Results of this study provide useful information for accident prevention during SSI <span class="hlt">weather</span>. Copyright © 2017 Elsevier Ltd. All rights reserved.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2015AGUFMGC11H1110M','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2015AGUFMGC11H1110M"><span><span class="hlt">Modeled</span> Forecasts of Dengue Fever in San Juan, Puerto Rico Using NASA Satellite Enhanced <span class="hlt">Weather</span> Forecasts</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Morin, C.; Quattrochi, D. A.; Zavodsky, B.; Case, J.</p> <p>2015-12-01</p> <p>Dengue fever (DF) is an important mosquito transmitted disease that is strongly influenced by meteorological and environmental conditions. Recent research has focused on forecasting DF case numbers based on meteorological data. However, these forecasting tools have generally relied on empirical <span class="hlt">models</span> that require long DF time series to train. Additionally, their accuracy has been tested retrospectively, using past meteorological data. Consequently, the operational utility of the forecasts are still in question because the error associated with <span class="hlt">weather</span> and climate forecasts are not reflected in the results. Using up-to-date weekly dengue case numbers for <span class="hlt">model</span> parameterization and <span class="hlt">weather</span> forecast data as meteorological input, we produced weekly forecasts of DF cases in San Juan, Puerto Rico. Each week, the past weeks' case counts were used to re-parameterize a process-based DF <span class="hlt">model</span> driven with updated <span class="hlt">weather</span> forecast data to generate forecasts of DF case numbers. Real-time <span class="hlt">weather</span> forecast data was produced using the <span class="hlt">Weather</span> Research and Forecasting (WRF) numerical <span class="hlt">weather</span> prediction (NWP) <span class="hlt">system</span> enhanced using additional high-resolution NASA satellite data. This methodology was conducted in a weekly iterative process with each DF forecast being evaluated using county-level DF cases reported by the Puerto Rico Department of Health. The one week DF forecasts were accurate especially considering the two sources of <span class="hlt">model</span> error. First, <span class="hlt">weather</span> forecasts were sometimes inaccurate and generally produced lower than observed temperatures. Second, the DF <span class="hlt">model</span> was often overly influenced by the previous weeks DF case numbers, though this phenomenon could be lessened by increasing the number of simulations included in the forecast. Although these results are promising, we would like to develop a methodology to produce longer range forecasts so that public health workers can better prepare for dengue epidemics.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.osti.gov/biblio/1126355-simulation-based-weather-normalization-approach-study-impact-weather-energy-use-buildings','SCIGOV-STC'); return false;" href="https://www.osti.gov/biblio/1126355-simulation-based-weather-normalization-approach-study-impact-weather-energy-use-buildings"><span>SIMULATION-BASED <span class="hlt">WEATHER</span> NORMALIZATION APPROACH TO STUDY THE IMPACT OF <span class="hlt">WEATHER</span> ON ENERGY USE OF BUILDINGS IN THE U.S.</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>Makhmalbaf, Atefe; Srivastava, Viraj; Wang, Na</p> <p></p> <p><span class="hlt">Weather</span> normalization is a crucial task in several applications related to building energy conservation such as retrofit measurements and energy rating. This paper documents preliminary results found from an effort to determine a set of <span class="hlt">weather</span> adjustment coefficients that can be used to smooth out impacts of <span class="hlt">weather</span> on energy use of buildings in 1020 <span class="hlt">weather</span> location sites available in the U.S. The U.S. Department of Energy (DOE) commercial reference building <span class="hlt">models</span> are adopted as hypothetical <span class="hlt">models</span> with standard operations to deliver consistency in <span class="hlt">modeling</span>. The correlation between building envelop design, HVAC <span class="hlt">system</span> design and properties for different building typesmore » and the change in heating and cooling energy consumption caused by variations in <span class="hlt">weather</span> is examined.« less</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://ntrs.nasa.gov/search.jsp?R=20000110530&hterms=information+technology&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D30%26Ntt%3Dinformation%2Btechnology','NASA-TRS'); return false;" href="https://ntrs.nasa.gov/search.jsp?R=20000110530&hterms=information+technology&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D30%26Ntt%3Dinformation%2Btechnology"><span>Estimating The Rate of Technology Adoption for Cockpit <span class="hlt">Weather</span> Information <span class="hlt">Systems</span></span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Kauffmann, Paul; Stough, H. P.</p> <p>2000-01-01</p> <p>In February 1997, President Clinton announced a national goal to reduce the <span class="hlt">weather</span> related fatal accident rate for aviation by 80% in ten years. To support that goal, NASA established an Aviation <span class="hlt">Weather</span> Information Distribution and Presentation Project to develop technologies that will provide timely and intuitive information to pilots, dispatchers, and air traffic controllers. This information should enable the detection and avoidance of atmospheric hazards and support an improvement in the fatal accident rate related to <span class="hlt">weather</span>. A critical issue in the success of NASA's <span class="hlt">weather</span> information program is the rate at which the market place will adopt this new <span class="hlt">weather</span> information technology. This paper examines that question by developing estimated adoption curves for <span class="hlt">weather</span> information <span class="hlt">systems</span> in five critical aviation segments: commercial, commuter, business, general aviation, and rotorcraft. The paper begins with development of general product descriptions. Using this data, key adopters are surveyed and estimates of adoption rates are obtained. These estimates are regressed to develop adoption curves and equations for <span class="hlt">weather</span> related information <span class="hlt">systems</span>. The paper demonstrates the use of adoption rate curves in product development and research planning to improve managerial decision processes and resource allocation.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2013EGUGA..1512511C','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2013EGUGA..1512511C"><span><span class="hlt">Weather</span> <span class="hlt">models</span> as virtual sensors to data-driven rainfall predictions in urban watersheds</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Cozzi, Lorenzo; Galelli, Stefano; Pascal, Samuel Jolivet De Marc; Castelletti, Andrea</p> <p>2013-04-01</p> <p><span class="hlt">Weather</span> and climate predictions are a key element of urban hydrology where they are used to inform water management and assist in flood warning delivering. Indeed, the <span class="hlt">modelling</span> of the very fast dynamics of urbanized catchments can be substantially improved by the use of <span class="hlt">weather</span>/rainfall predictions. For example, in Singapore Marina Reservoir catchment runoff processes have a very short time of concentration (roughly one hour) and observational data are thus nearly useless for runoff predictions and <span class="hlt">weather</span> prediction are required. Unfortunately, radar nowcasting methods do not allow to carrying out long - term <span class="hlt">weather</span> predictions, whereas numerical <span class="hlt">models</span> are limited by their coarse spatial scale. Moreover, numerical <span class="hlt">models</span> are usually poorly reliable because of the fast motion and limited spatial extension of rainfall events. In this study we investigate the combined use of data-driven <span class="hlt">modelling</span> techniques and <span class="hlt">weather</span> variables observed/simulated with a numerical <span class="hlt">model</span> as a way to improve rainfall prediction accuracy and lead time in the Singapore metropolitan area. To explore the feasibility of the approach, we use a <span class="hlt">Weather</span> Research and Forecast (WRF) <span class="hlt">model</span> as a virtual sensor network for the input variables (the states of the WRF <span class="hlt">model</span>) to a machine learning rainfall prediction <span class="hlt">model</span>. More precisely, we combine an input variable selection method and a non-parametric tree-based <span class="hlt">model</span> to characterize the empirical relation between the rainfall measured at the catchment level and all possible <span class="hlt">weather</span> input variables provided by WRF <span class="hlt">model</span>. We explore different lead time to evaluate the <span class="hlt">model</span> reliability for different long - term predictions, as well as different time lags to see how past information could improve results. Results show that the proposed approach allow a significant improvement of the prediction accuracy of the WRF <span class="hlt">model</span> on the Singapore urban area.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/20110012892','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/20110012892"><span>Convective <span class="hlt">Weather</span> Avoidance with Uncertain <span class="hlt">Weather</span> Forecasts</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Karahan, Sinan; Windhorst, Robert D.</p> <p>2009-01-01</p> <p>Convective <span class="hlt">weather</span> events have a disruptive impact on air traffic both in terminal area and in en-route airspaces. In order to make sure that the national air transportation <span class="hlt">system</span> is safe and efficient, it is essential to respond to convective <span class="hlt">weather</span> events effectively. Traffic flow control initiatives in response to convective <span class="hlt">weather</span> include ground delay, airborne delay, miles-in-trail restrictions as well as tactical and strategic rerouting. The rerouting initiatives can potentially increase traffic density and complexity in regions neighboring the convective <span class="hlt">weather</span> activity. There is a need to perform rerouting in an intelligent and efficient way such that the disruptive effects of rerouting are minimized. An important area of research is to study the interaction of in-flight rerouting with traffic congestion or complexity and developing methods that quantitatively measure this interaction. Furthermore, it is necessary to find rerouting solutions that account for uncertainties in <span class="hlt">weather</span> forecasts. These are important steps toward managing complexity during rerouting operations, and the paper is motivated by these research questions. An automated <span class="hlt">system</span> is developed for rerouting air traffic in order to avoid convective <span class="hlt">weather</span> regions during the 20- minute - 2-hour time horizon. Such a <span class="hlt">system</span> is envisioned to work in concert with separation assurance (0 - 20-minute time horizon), and longer term air traffic management (2-hours and beyond) to provide a more comprehensive solution to complexity and safety management. In this study, <span class="hlt">weather</span> is dynamic and uncertain; it is represented as regions of airspace that pilots are likely to avoid. Algorithms are implemented in an air traffic simulation environment to support the research study. The algorithms used are deterministic but periodically revise reroutes to account for <span class="hlt">weather</span> forecast updates. In contrast to previous studies, in this study convective <span class="hlt">weather</span> is represented as regions of airspace that pilots</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.osti.gov/pages/biblio/1376542-stochastic-parameterization-toward-new-view-weather-climate-models','SCIGOV-DOEP'); return false;" href="https://www.osti.gov/pages/biblio/1376542-stochastic-parameterization-toward-new-view-weather-climate-models"><span>Stochastic Parameterization: Toward a New View of <span class="hlt">Weather</span> and Climate <span class="hlt">Models</span></span></a></p> <p><a target="_blank" href="http://www.osti.gov/pages">DOE PAGES</a></p> <p>Berner, Judith; Achatz, Ulrich; Batté, Lauriane; ...</p> <p>2017-03-31</p> <p>The last decade has seen the success of stochastic parameterizations in short-term, medium-range, and seasonal forecasts: operational <span class="hlt">weather</span> centers now routinely use stochastic parameterization schemes to represent <span class="hlt">model</span> inadequacy better and to improve the quantification of forecast uncertainty. Developed initially for numerical <span class="hlt">weather</span> prediction, the inclusion of stochastic parameterizations not only provides better estimates of uncertainty, but it is also extremely promising for reducing long-standing climate biases and is relevant for determining the climate response to external forcing. This article highlights recent developments from different research groups that show that the stochastic representation of unresolved processes in the atmosphere, oceans,more » land surface, and cryosphere of comprehensive <span class="hlt">weather</span> and climate <span class="hlt">models</span> 1) gives rise to more reliable probabilistic forecasts of <span class="hlt">weather</span> and climate and 2) reduces systematic <span class="hlt">model</span> bias. We make a case that the use of mathematically stringent methods for the derivation of stochastic dynamic equations will lead to substantial improvements in our ability to accurately simulate <span class="hlt">weather</span> and climate at all scales. Recent work in mathematics, statistical mechanics, and turbulence is reviewed; its relevance for the climate problem is demonstrated; and future research directions are outlined« less</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.osti.gov/servlets/purl/1376542','SCIGOV-STC'); return false;" href="https://www.osti.gov/servlets/purl/1376542"><span>Stochastic Parameterization: Toward a New View of <span class="hlt">Weather</span> and Climate <span class="hlt">Models</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>Berner, Judith; Achatz, Ulrich; Batté, Lauriane</p> <p></p> <p>The last decade has seen the success of stochastic parameterizations in short-term, medium-range, and seasonal forecasts: operational <span class="hlt">weather</span> centers now routinely use stochastic parameterization schemes to represent <span class="hlt">model</span> inadequacy better and to improve the quantification of forecast uncertainty. Developed initially for numerical <span class="hlt">weather</span> prediction, the inclusion of stochastic parameterizations not only provides better estimates of uncertainty, but it is also extremely promising for reducing long-standing climate biases and is relevant for determining the climate response to external forcing. This article highlights recent developments from different research groups that show that the stochastic representation of unresolved processes in the atmosphere, oceans,more » land surface, and cryosphere of comprehensive <span class="hlt">weather</span> and climate <span class="hlt">models</span> 1) gives rise to more reliable probabilistic forecasts of <span class="hlt">weather</span> and climate and 2) reduces systematic <span class="hlt">model</span> bias. We make a case that the use of mathematically stringent methods for the derivation of stochastic dynamic equations will lead to substantial improvements in our ability to accurately simulate <span class="hlt">weather</span> and climate at all scales. Recent work in mathematics, statistical mechanics, and turbulence is reviewed; its relevance for the climate problem is demonstrated; and future research directions are outlined« less</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017AGUFM.B23B2070C','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017AGUFM.B23B2070C"><span>Advanced Corrections for InSAR Using GPS and Numerical <span class="hlt">Weather</span> <span class="hlt">Models</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Cossu, F.; Foster, J. H.; Amelung, F.; Varugu, B. K.; Businger, S.; Cherubini, T.</p> <p>2017-12-01</p> <p>We present results from an investigation into the application of numerical <span class="hlt">weather</span> <span class="hlt">models</span> for generating tropospheric correction fields for Interferometric Synthetic Aperture Radar (InSAR). We apply the technique to data acquired from a UAVSAR campaign as well as from the CosmoSkyMed satellites. The complex spatial and temporal changes in the atmospheric propagation delay of the radar signal remain the single biggest factor limiting InSAR's potential for hazard monitoring and mitigation. A new generation of InSAR <span class="hlt">systems</span> is being built and launched, and optimizing the science and hazard applications of these <span class="hlt">systems</span> requires advanced methodologies to mitigate tropospheric noise. We use the <span class="hlt">Weather</span> Research and Forecasting (WRF) <span class="hlt">model</span> to generate a 900 m spatial resolution atmospheric <span class="hlt">models</span> covering the Big Island of Hawaii and an even higher, 300 m resolution grid over the Mauna Loa and Kilauea volcanoes. By comparing a range of approaches, from the simplest, using reanalyses based on typically available meteorological observations, through to the "kitchen-sink" approach of assimilating all relevant data sets into our custom analyses, we examine the impact of the additional data sets on the atmospheric <span class="hlt">models</span> and their effectiveness in correcting InSAR data. We focus particularly on the assimilation of information from the more than 60 GPS sites in the island. We ingest zenith tropospheric delay estimates from these sites directly into the WRF analyses, and also perform double-difference tomography using the phase residuals from the GPS processing to robustly incorporate heterogeneous information from the GPS data into the atmospheric <span class="hlt">models</span>. We assess our performance through comparisons of our atmospheric <span class="hlt">models</span> with external observations not ingested into the <span class="hlt">model</span>, and through the effectiveness of the derived phase screens in reducing InSAR variance. Comparison of the InSAR data, our atmospheric analyses, and assessments of the active local and mesoscale</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2012AGUFMED53C0930M','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2012AGUFMED53C0930M"><span>Community Coordinated <span class="hlt">Modeling</span> Center (CCMC): Using innovative tools and services to support worldwide space <span class="hlt">weather</span> scientific communities and networks</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Mendoza, A. M.; Bakshi, S.; Berrios, D.; Chulaki, A.; Evans, R. M.; Kuznetsova, M. M.; Lee, H.; MacNeice, P. J.; Maddox, M. M.; Mays, M. L.; Mullinix, R. E.; Ngwira, C. M.; Patel, K.; Pulkkinen, A.; Rastaetter, L.; Shim, J.; Taktakishvili, A.; Zheng, Y.</p> <p>2012-12-01</p> <p>Community Coordinated <span class="hlt">Modeling</span> Center (CCMC) was established to enhance basic solar terrestrial research and to aid in the development of <span class="hlt">models</span> for specifying and forecasting conditions in the space environment. In achieving this goal, CCMC has developed and provides a set of innovative tools varying from: Integrated Space <span class="hlt">Weather</span> Analysis (iSWA) web -based dissemination <span class="hlt">system</span> for space <span class="hlt">weather</span> information, Runs-On-Request <span class="hlt">System</span> providing access to unique collection of state-of-the-art solar and space physics <span class="hlt">models</span> (unmatched anywhere in the world), Advanced Online Visualization and Analysis tools for more accurate interpretation of <span class="hlt">model</span> results, Standard Data formats for Simulation Data downloads, and recently Mobile apps (iPhone/Android) to view space <span class="hlt">weather</span> data anywhere to the scientific community. The number of runs requested and the number of resulting scientific publications and presentations from the research community has not only been an indication of the broad scientific usage of the CCMC and effective participation by space scientists and researchers, but also guarantees active collaboration and coordination amongst the space <span class="hlt">weather</span> research community. Arising from the course of CCMC activities, CCMC also supports community-wide <span class="hlt">model</span> validation challenges and research focus group projects for a broad range of programs such as the multi-agency National Space <span class="hlt">Weather</span> Program, NSF's CEDAR (Coupling, Energetics and Dynamics of Atmospheric Regions), GEM (Geospace Environment <span class="hlt">Modeling</span>) and Shine (Solar Heliospheric and INterplanetary Environment) programs. In addition to performing research and <span class="hlt">model</span> development, CCMC also supports space science education by hosting summer students through local universities; through the provision of simulations in support of classroom programs such as Heliophysics Summer School (with student research contest) and CCMC Workshops; training next generation of junior scientists in space <span class="hlt">weather</span> forecasting; and educating</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/19930007503','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/19930007503"><span>Pilot <span class="hlt">weather</span> advisor</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Kilgore, W. A.; Seth, S.; Crabill, N. L.; Shipley, S. T.; Graffman, I.; Oneill, J.</p> <p>1992-01-01</p> <p>The results of the work performed by ViGYAN, Inc., to demonstrate the Pilot <span class="hlt">Weather</span> Advisor cockpit <span class="hlt">weather</span> data <span class="hlt">system</span> using a broadcast satellite communication <span class="hlt">system</span> are presented. The Pilot <span class="hlt">Weather</span> Advisor demonstrated that the technical problems involved with transmitting significant amount of <span class="hlt">weather</span> data to an aircraft in-flight or on-the-ground via satellite are solvable with today's technology. The Pilot <span class="hlt">Weather</span> Advisor appears to be a viable solution for providing accurate and timely <span class="hlt">weather</span> information for general aviation aircraft.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2016WRR....52.4801P','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2016WRR....52.4801P"><span>Ensemble forecasting of short-term <span class="hlt">system</span> scale irrigation demands using real-time flow data and numerical <span class="hlt">weather</span> predictions</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Perera, Kushan C.; Western, Andrew W.; Robertson, David E.; George, Biju; Nawarathna, Bandara</p> <p>2016-06-01</p> <p>Irrigation demands fluctuate in response to <span class="hlt">weather</span> variations and a range of irrigation management decisions, which creates challenges for water supply <span class="hlt">system</span> operators. This paper develops a method for real-time ensemble forecasting of irrigation demand and applies it to irrigation command areas of various sizes for lead times of 1 to 5 days. The ensemble forecasts are based on a deterministic time series <span class="hlt">model</span> coupled with ensemble representations of the various inputs to that <span class="hlt">model</span>. Forecast inputs include past flow, precipitation, and potential evapotranspiration. These inputs are variously derived from flow observations from a modernized irrigation delivery <span class="hlt">system</span>; short-term <span class="hlt">weather</span> forecasts derived from numerical <span class="hlt">weather</span> prediction <span class="hlt">models</span> and observed <span class="hlt">weather</span> data available from automatic <span class="hlt">weather</span> stations. The predictive performance for the ensemble spread of irrigation demand was quantified using rank histograms, the mean continuous rank probability score (CRPS), the mean CRPS reliability and the temporal mean of the ensemble root mean squared error (MRMSE). The mean forecast was evaluated using root mean squared error (RMSE), Nash-Sutcliffe <span class="hlt">model</span> efficiency (NSE) and bias. The NSE values for evaluation periods ranged between 0.96 (1 day lead time, whole study area) and 0.42 (5 days lead time, smallest command area). Rank histograms and comparison of MRMSE, mean CRPS, mean CRPS reliability and RMSE indicated that the ensemble spread is generally a reliable representation of the forecast uncertainty for short lead times but underestimates the uncertainty for long lead times.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017AGUFM.A14C..04C','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017AGUFM.A14C..04C"><span>Atmosphere-Wave-Ocean Coupling from Regional to Global Earth <span class="hlt">System</span> <span class="hlt">Models</span> for High-Impact Extreme <span class="hlt">Weather</span> Prediction</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Chen, S. S.; Curcic, M.</p> <p>2017-12-01</p> <p>The need for acurrate and integrated impact forecasts of extreme wind, rain, waves, and storm surge is growing as coastal population and built environment expand worldwide. A key limiting factor in forecasting impacts of extreme <span class="hlt">weather</span> events associated with tropical cycle and winter storms is fully coupled atmosphere-wave-ocean <span class="hlt">model</span> interface with explicit momentum and energy exchange. It is not only critical for accurate prediction of storm intensity, but also provides coherent wind, rian, ocean waves and currents forecasts for forcing for storm surge. The Unified Wave INterface (UWIN) has been developed for coupling of the atmosphere-wave-ocean <span class="hlt">models</span>. UWIN couples the atmosphere, wave, and ocean <span class="hlt">models</span> using the Earth <span class="hlt">System</span> <span class="hlt">Modeling</span> Framework (ESMF). It is a physically based and computationally efficient coupling sytem that is flexible to use in a multi-<span class="hlt">model</span> <span class="hlt">system</span> and portable for transition to the next generation global Earth <span class="hlt">system</span> prediction mdoels. This standardized coupling framework allows researchers to develop and test air-sea coupling parameterizations and coupled data assimilation, and to better facilitate research-to-operation activities. It has been used and extensively tested and verified in regional coupled <span class="hlt">model</span> forecasts of tropical cycles and winter storms (Chen and Curcic 2016, Curcic et al. 2016, and Judt et al. 2016). We will present 1) an overview of UWIN and its applications in fully coupled atmosphere-wave-ocean <span class="hlt">model</span> predictions of hurricanes and coastal winter storms, and 2) implenmentation of UWIN in the NASA GMAO GEOS-5.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2018MS%26E..309a2054R','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2018MS%26E..309a2054R"><span>Implementation of bayesian <span class="hlt">model</span> averaging on the <span class="hlt">weather</span> data forecasting applications utilizing open <span class="hlt">weather</span> map</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Rahmat, R. F.; Nasution, F. R.; Seniman; Syahputra, M. F.; Sitompul, O. S.</p> <p>2018-02-01</p> <p><span class="hlt">Weather</span> is condition of air in a certain region at a relatively short period of time, measured with various parameters such as; temperature, air preasure, wind velocity, humidity and another phenomenons in the atmosphere. In fact, extreme <span class="hlt">weather</span> due to global warming would lead to drought, flood, hurricane and other forms of <span class="hlt">weather</span> occasion, which directly affects social andeconomic activities. Hence, a forecasting technique is to predict <span class="hlt">weather</span> with distinctive output, particullary mapping process based on GIS with information about current <span class="hlt">weather</span> status in certain cordinates of each region with capability to forecast for seven days afterward. Data used in this research are retrieved in real time from the server openweathermap and BMKG. In order to obtain a low error rate and high accuracy of forecasting, the authors use Bayesian <span class="hlt">Model</span> Averaging (BMA) method. The result shows that the BMA method has good accuracy. Forecasting error value is calculated by mean square error shows (MSE). The error value emerges at minumum temperature rated at 0.28 and maximum temperature rated at 0.15. Meanwhile, the error value of minimum humidity rates at 0.38 and the error value of maximum humidity rates at 0.04. Afterall, the forecasting error rate of wind speed is at 0.076. The lower the forecasting error rate, the more optimized the accuracy is.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2003BAMS...84..187W','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2003BAMS...84..187W"><span>A Hole in the <span class="hlt">Weather</span> Warning <span class="hlt">System</span>.</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Wood, Vincent T.; Weisman, Robert A.</p> <p>2003-02-01</p> <p>lack of text information. These problems had forced deaf and hard of hearing people to rely on looking at the sky or having hearing people alert them as their primary methods of receiving emergency information. These problems are documented through the use of a survey of 277 deaf and hard of hearing people in Minnesota and Oklahoma as well as specific examples.During the last two years, some progress has been made to "close this hole" in the <span class="hlt">weather</span> warning <span class="hlt">system</span>. The Federal Communications Commission has approved new rules, requiring that all audio emergency information provided by television stations, satellite, and cable operators must also be provided visually. In addition, the use of new technology such as pager <span class="hlt">systems</span>, <span class="hlt">weather</span> radios adapted for use by those with special needs, the Internet, and satellite warning <span class="hlt">systems</span> have allowed deaf and hard of hearing people to have more access to emergency information.In this article, these improvements are documented but continuing problems and possible solutions are also listed.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2015AGUFMGC51H..02P','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2015AGUFMGC51H..02P"><span><span class="hlt">Weather</span> Driven Renewable Energy Analysis, <span class="hlt">Modeling</span> New Technologies</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Paine, J.; Clack, C.; Picciano, P.; Terry, L.</p> <p>2015-12-01</p> <p>Carbon emission reduction is essential to hampering anthropogenic climate change. While there are several methods to broach carbon reductions, the National Energy with <span class="hlt">Weather</span> <span class="hlt">System</span> (NEWS) <span class="hlt">model</span> focuses on limiting electrical generation emissions by way of a national high-voltage direct-current transmission that takes advantage of the strengths of different regions in terms of variable sources of energy. Specifically, we focus upon <span class="hlt">modeling</span> concentrating solar power (CSP) as another source to contribute to the electric grid. Power tower solar fields are optimized taking into account high spatial and temporal resolution, 13km and hourly, numerical <span class="hlt">weather</span> prediction <span class="hlt">model</span> data gathered by NOAA from the years of 2006-2008. Importantly, the optimization of these CSP power plants takes into consideration factors that decrease the optical efficiency of the heliostats reflecting solar irradiance. For example, cosine efficiency, atmospheric attenuation, and shadowing are shown here; however, it should be noted that they are not the only limiting factors. While solar photovoltaic plants can be combined for similar efficiency to the power tower and currently at a lower cost, they do not have a cost-effective capability to provide electricity when there are interruptions in solar irradiance. Power towers rely on a heat transfer fluid, which can be used for thermal storage changing the cost efficiency of this energy source. Thermal storage increases the electric stability that many other renewable energy sources lack, and thus, the ability to choose between direct electric conversion and thermal storage is discussed. The figure shown is a test <span class="hlt">model</span> of a CSP plant made up of heliostats. The colors show the optical efficiency of each heliostat at a single time of the day.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://rosap.ntl.bts.gov/view/dot/4133','DOTNTL'); return false;" href="https://rosap.ntl.bts.gov/view/dot/4133"><span>Road <span class="hlt">weather</span> information <span class="hlt">systems</span> : enabling proactive maintenance practices in Washington state</span></a></p> <p><a target="_blank" href="http://ntlsearch.bts.gov/tris/index.do">DOT National Transportation Integrated Search</a></p> <p></p> <p>2002-03-01</p> <p>Washington State Department of Transportation's (WSDOT) r<span class="hlt">Weather</span> program has significantly integrated and expanded the capabilities of road <span class="hlt">weather</span> information <span class="hlt">systems</span> (RWIS) in the state, enabling proactive winter maintenance practices and better-in...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2013JASTP.102..329G','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2013JASTP.102..329G"><span>GIM-TEC adaptive ionospheric <span class="hlt">weather</span> assessment and forecast <span class="hlt">system</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Gulyaeva, T. L.; Arikan, F.; Hernandez-Pajares, M.; Stanislawska, I.</p> <p>2013-09-01</p> <p>The Ionospheric <span class="hlt">Weather</span> Assessment and Forecast (IWAF) <span class="hlt">system</span> is a computer software package designed to assess and predict the world-wide representation of 3-D electron density profiles from the Global Ionospheric Maps of Total Electron Content (GIM-TEC). The unique <span class="hlt">system</span> products include daily-hourly numerical global maps of the F2 layer critical frequency (foF2) and the peak height (hmF2) generated with the International Reference Ionosphere extended to the plasmasphere, IRI-Plas, upgraded by importing the daily-hourly GIM-TEC as a new <span class="hlt">model</span> driving parameter. Since GIM-TEC maps are provided with 1- or 2-days latency, the global maps forecast for 1 day and 2 days ahead are derived using an harmonic analysis applied to the temporal changes of TEC, foF2 and hmF2 at 5112 grid points of a map encapsulated in IONEX format (-87.5°:2.5°:87.5°N in latitude, -180°:5°:180°E in longitude). The <span class="hlt">system</span> provides online the ionospheric disturbance warnings in the global W-index map establishing categories of the ionospheric <span class="hlt">weather</span> from the quiet state (W=±1) to intense storm (W=±4) according to the thresholds set for instant TEC perturbations regarding quiet reference median for the preceding 7 days. The accuracy of IWAF <span class="hlt">system</span> predictions of TEC, foF2 and hmF2 maps is superior to the standard persistence <span class="hlt">model</span> with prediction equal to the most recent ‘true’ map. The paper presents outcomes of the new service expressed by the global ionospheric foF2, hmF2 and W-index maps demonstrating the process of origin and propagation of positive and negative ionosphere disturbances in space and time and their forecast under different scenarios.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2012PApGe.169..321M','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2012PApGe.169..321M"><span>The Local Ensemble Transform Kalman Filter with the <span class="hlt">Weather</span> Research and Forecasting <span class="hlt">Model</span>: Experiments with Real Observations</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Miyoshi, Takemasa; Kunii, Masaru</p> <p>2012-03-01</p> <p>The local ensemble transform Kalman filter (LETKF) is implemented with the <span class="hlt">Weather</span> Research and Forecasting (WRF) <span class="hlt">model</span>, and real observations are assimilated to assess the newly-developed WRF-LETKF <span class="hlt">system</span>. The WRF <span class="hlt">model</span> is a widely-used mesoscale numerical <span class="hlt">weather</span> prediction <span class="hlt">model</span>, and the LETKF is an ensemble Kalman filter (EnKF) algorithm particularly efficient in parallel computer architecture. This study aims to provide the basis of future research on mesoscale data assimilation using the WRF-LETKF <span class="hlt">system</span>, an additional testbed to the existing EnKF <span class="hlt">systems</span> with the WRF <span class="hlt">model</span> used in the previous studies. The particular LETKF <span class="hlt">system</span> adopted in this study is based on the <span class="hlt">system</span> initially developed in 2004 and has been continuously improved through theoretical studies and wide applications to many kinds of dynamical <span class="hlt">models</span> including realistic geophysical <span class="hlt">models</span>. Most recent and important improvements include an adaptive covariance inflation scheme which considers the spatial and temporal inhomogeneity of inflation parameters. Experiments show that the LETKF successfully assimilates real observations and that adaptive inflation is advantageous. Additional experiments with various ensemble sizes show that using more ensemble members improves the analyses consistently.</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://rosap.ntl.bts.gov/view/dot/2124','DOTNTL'); return false;" href="https://rosap.ntl.bts.gov/view/dot/2124"><span>Improving the Wyoming road <span class="hlt">weather</span> information <span class="hlt">system</span></span></a></p> <p><a target="_blank" href="http://ntlsearch.bts.gov/tris/index.do">DOT National Transportation Integrated Search</a></p> <p></p> <p>1998-11-01</p> <p>Studies in other states and countries have shown that Road <span class="hlt">Weather</span> Information <span class="hlt">Systems</span> (RWIS) can improve the efficiency of snow and ice control operations and reduce accidents. The RWIS network in Wyoming is presently comprised of 27 roadside weathe...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2015EGUGA..17.4205D','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2015EGUGA..17.4205D"><span>Linking the M&Rfi <span class="hlt">Weather</span> Generator with Agrometeorological <span class="hlt">Models</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Dubrovsky, Martin; Trnka, Miroslav</p> <p>2015-04-01</p> <p>Realistic meteorological inputs (representing the present and/or future climates) for the agrometeorological <span class="hlt">model</span> simulations are often produced by stochastic <span class="hlt">weather</span> generators (WGs). This contribution presents some methodological issues and results obtained in our recent experiments. We also address selected questions raised in the synopsis of this session. The input meteorological time series for our experiments are produced by the parametric single site <span class="hlt">weather</span> generator (WG) Marfi, which is calibrated from the available observational data (or interpolated from surrounding stations). To produce meteorological series representing the future climate, the WG parameters are modified by climate change scenarios, which are prepared by the pattern scaling method: the standardised scenarios derived from Global or Regional Climate <span class="hlt">Models</span> are multiplied by the change in global mean temperature (ΔTG) determined by the simple climate <span class="hlt">model</span> MAGICC. The presentation will address following questions: (i) The dependence of the quality of the synthetic <span class="hlt">weather</span> series and impact results on the WG settings. An emphasis will be put on an effect of conditioning the daily WG on monthly WG (presently being one of our hot topics), which aims at improvement of the reproduction of the low-frequency <span class="hlt">weather</span> variability. Comparison of results obtained with various WG settings is made in terms of climatic and agroclimatic indices (including extreme temperature and precipitation characteristics and drought indices). (ii) Our methodology accounts for the uncertainties coming from various sources. We will show how the climate change impact results are affected by 1. uncertainty in climate <span class="hlt">modelling</span>, 2. uncertainty in ΔTG, and 3. uncertainty related to the complexity of the climate change scenario (focusing on an effect of inclusion of changes in variability into the climate change scenarios). Acknowledgements: This study was funded by project "Building up a multidisciplinary scientific</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2016AGUFMSH11C2259S','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2016AGUFMSH11C2259S"><span>New Space <span class="hlt">Weather</span> Forecasting at NOAA with Michigan's Geospace <span class="hlt">Model</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Singer, H. J.; Millward, G. H.; Balch, C. C.; Cash, M. D.; Onsager, T. G.; Toth, G.; Welling, D. T.; Gombosi, T. I.</p> <p>2016-12-01</p> <p>We will present first results from the University of Michigan's Geospace <span class="hlt">model</span> that is transitioning, during 2016, from a research capability into operations at the NOAA Space <span class="hlt">Weather</span> Prediction Center. The first generation of space <span class="hlt">weather</span> products from this <span class="hlt">model</span> will be described. These initial products will support power grid operators, as well as other users, with both global and regional, short-term predictions of geomagnetic activity. The Geospace <span class="hlt">model</span> is a coupled <span class="hlt">system</span> including three components: the BATS-R-US magnetohydrodynamic (MHD) <span class="hlt">model</span> of the magnetosphere; the Ridley ionosphere electrodynamics <span class="hlt">model</span> (RIM); and the Rice Convection <span class="hlt">Model</span> (RCM), an inner magnetosphere ring-current <span class="hlt">model</span> developed at Rice University. The <span class="hlt">model</span> is driven by solar wind data from a satellite at L1 (now NOAA's DSCOVR satellite) and F10.7, a proxy for solar extreme ultra-violet radiation. The Geospace <span class="hlt">model</span> runs continuously, driven by the 1-minute cadence real-time L1 data that is propagated to the inflow boundary of the MHD code. The <span class="hlt">model</span> steps back to an earlier time and then continues forward if high-speed solar wind overtakes slower solar wind. This mode of operation is unique among the <span class="hlt">models</span> at NOAA's National Center for Environment Prediction's Central Operations (NCO), and it is also different from the typical scientific simulation mode. All of this work has involved 3D graphical <span class="hlt">model</span> displays and validation tools that are being developed to support forecasters and web-based external users. Lessons learned during the transition process will be described, as well as the iterative process that occurs between Research and Operations and the scientific challenges for future <span class="hlt">model</span> and product improvements.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://www.dtic.mil/docs/citations/ADA101342','DTIC-ST'); return false;" href="http://www.dtic.mil/docs/citations/ADA101342"><span>The Design Implementation of an Operational, Computer Based <span class="hlt">Weather</span> Radar <span class="hlt">System</span>,</span></a></p> <p><a target="_blank" href="http://www.dtic.mil/">DTIC Science & Technology</a></p> <p></p> <p>1979-01-01</p> <p>AN OPERATIONAL, COMPUTER-BASED <span class="hlt">WEATHER</span> RADAR <span class="hlt">SYSTEM</span> Authors: A P Ball, J L Clarke, M J O’Brien A H Shaw , S E Trigg and T A Voller ’Original contains...A ’Ball, J L/Clarke, MJ/O’Brien A H , Shaw , S E Trigg and T A Voller SUMMARY Inis memorand,,m describes the work of the RSRE <span class="hlt">Weather</span> Radar Division in...IMPLEMENTATION OF AN OPERATIONAL, COMPUTER BASED <span class="hlt">WEATHER</span> RADAR <span class="hlt">SYSTEM</span> A P Ball, J L Clarke, M J O’Brien, A H Shaw , S E Trigg and T A Voller CONTENTS 1</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2014cosp...40E3359T','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2014cosp...40E3359T"><span>Concept for an International Standard related to Space <span class="hlt">Weather</span> Effects on Space <span class="hlt">Systems</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Tobiska, W. Kent; Tomky, Alyssa</p> <p></p> <p>There is great interest in developing an international standard related to space <span class="hlt">weather</span> in order to specify the tools and parameters needed for space <span class="hlt">systems</span> operations. In particular, a standard is important for satellite operators who may not be familiar with space <span class="hlt">weather</span>. In addition, there are others who participate in space <span class="hlt">systems</span> operations that would also benefit from such a document. For example, the developers of software <span class="hlt">systems</span> that provide LEO satellite orbit determination, radio communication availability for scintillation events (GEO-to-ground L and UHF bands), GPS uncertainties, and the radiation environment from ground-to-space for commercial space tourism. These groups require recent historical data, current epoch specification, and forecast of space <span class="hlt">weather</span> events into their automated or manual <span class="hlt">systems</span>. Other examples are national government agencies that rely on space <span class="hlt">weather</span> data provided by their organizations such as those represented in the International Space Environment Service (ISES) group of 14 national agencies. Designers, manufacturers, and launchers of space <span class="hlt">systems</span> require real-time, operational space <span class="hlt">weather</span> parameters that can be measured, monitored, or built into automated <span class="hlt">systems</span>. Thus, a broad scope for the document will provide a useful international standard product to a variety of engineering and science domains. The structure of the document should contain a well-defined scope, consensus space <span class="hlt">weather</span> terms and definitions, and internationally accepted descriptions of the main elements of space <span class="hlt">weather</span>, its sources, and its effects upon space <span class="hlt">systems</span>. Appendices will be useful for describing expanded material such as guidelines on how to use the standard, how to obtain specific space <span class="hlt">weather</span> parameters, and short but detailed descriptions such as when best to use some parameters and not others; appendices provide a path for easily updating the standard since the domain of space <span class="hlt">weather</span> is rapidly changing with new advances</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2007AGUFM.H43C1514B','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2007AGUFM.H43C1514B"><span>Biologically-Mediated <span class="hlt">Weathering</span> of Minerals From Nanometre Scale to Environmental <span class="hlt">Systems</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Brown, D. J.; Banwart, S. A.; Smits, M. M.; Leake, J. R.; Bonneville, S.; Benning, L. G.; Haward, S. J.; Ragnarsdottir, K.</p> <p>2007-12-01</p> <p>The <span class="hlt">Weathering</span> Science Consortium is a multi-disciplinary project that aims to create a step change in understanding how biota control mineral <span class="hlt">weathering</span> and soil formation (http://www.wun.ac.uk/wsc). Our hypothesis is that rates of biotic <span class="hlt">weathering</span> are driven by the energy supply from plants to the organisms, controlling their biomass, surface area of contact with minerals and their capacity to interact chemically with minerals. Symbiotic fungal mycorrhiza of 90% of plant species are empowered with an available carbohydrate supply from plants that is unparalleled amongst soil microbes. They develop extensive mycelial networks that intimately contact minerals, which they <span class="hlt">weather</span> aggressively. We hypothesise that mycorrhiza play a critical role through their focussing of photosynthate energy from plants into sub-surface <span class="hlt">weathering</span> environments. Our work identifies how these fungal cells, and their secretions, interact with mineral surfaces and affect the rates of nutrient transfer from minerals to the organism. Investigating these living <span class="hlt">systems</span> allows us to create new concepts and mathematical <span class="hlt">models</span> that can describe biological <span class="hlt">weathering</span> and be used in computer simulations of soil <span class="hlt">weathering</span> dynamics. We are studying these biochemical interactions at 3 levels of observation: 1. At the molecular scale to understand interactions between living cells and minerals and to quantify the chemistry that breaks down the mineral structure; 2. At the soil grain scale to quantify the activity and spatial distribution of the fungi, roots and other organisms (e.g. bacteria) and their effects on the rates at which minerals are dissolved to release nutrients; 3. At soil profile scale to test <span class="hlt">models</span> for the spatial distribution of active fungi and carbon energy and their seasonal variability and impact on mineral dissolution rates. Here we present early results from molecular and soil grain scale experiments. We have grown pure culture (Suillus bovinus, Paxillus involutus</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2016AGUFMED43B0862C','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2016AGUFMED43B0862C"><span>The New Space <span class="hlt">Weather</span> Action Center; the Next Level on Space <span class="hlt">Weather</span> Education</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Collado-Vega, Y. M.; Lewis, E. M.; Cline, T. D.; MacDonald, E.</p> <p>2016-12-01</p> <p>The Space <span class="hlt">Weather</span> Action Center (SWAC) provides access for students to near real-time space <span class="hlt">weather</span> data, and a set of easy instructions and well-defined protocols that allow them to correctly interpret such data. It is a student centered approach to teaching science and technology in classrooms, as students are encouraged to act like real scientists by accessing, collecting, analyzing, recording, and communicating space <span class="hlt">weather</span> forecasts. Integration and implementation of several programs will enhance and provide a rich education experience for students' grades 5-16. We will enhance the existing data and tutorials available using the Integrated Space <span class="hlt">Weather</span> Analysis (iSWA) tool created by the Community Coordinated <span class="hlt">Modeling</span> Center (CCMC) at NASA GSFC. iSWA is a flexible, turn-key, customer-configurable, Web-based dissemination <span class="hlt">system</span> for NASA-relevant space <span class="hlt">weather</span> information that combines data based on the most advanced space <span class="hlt">weather</span> <span class="hlt">models</span> available through the CCMC with concurrent space environment information. This tool provides an additional component by the use of videos and still imagery from different sources as a tool for educators to effectively show what happens during an eruption from the surface of the Sun. We will also update content on the net result of space <span class="hlt">weather</span> forecasting that the public can experience by including Aurorasaurus, a well established, growing, modern, innovative, interdisciplinary citizen science project centered around the public's visibility of the northern lights with mobile applications via the use of social media connections.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/20030013637','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/20030013637"><span>Graphical <span class="hlt">Weather</span> Information <span class="hlt">System</span> Evaluation: Usability, Perceived Utility, and Preferences from General Aviation Pilots</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Latorella, Kara A.; Chamberlain, James P.</p> <p>2002-01-01</p> <p><span class="hlt">Weather</span> is a significant factor in General Aviation (GA) accidents and fatality rates. Graphical <span class="hlt">Weather</span> Information <span class="hlt">Systems</span> (GWISs) for the flight deck are appropriate technologies for mitigating the difficulties GA pilots have with current aviation <span class="hlt">weather</span> information sources. This paper describes usability evaluations of a prototype GWIS by 12 GA pilots after using the <span class="hlt">system</span> in flights towards convective <span class="hlt">weather</span>. We provide design guidance for GWISs and discuss further research required to support <span class="hlt">weather</span> situation awareness and in-flight decision making for GA pilots.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2016AGUFM.H42B..05C','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2016AGUFM.H42B..05C"><span>An Overview of the National <span class="hlt">Weather</span> Service National Water <span class="hlt">Model</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Cosgrove, B.; Gochis, D.; Clark, E. P.; Cui, Z.; Dugger, A. L.; Feng, X.; Karsten, L. R.; Khan, S.; Kitzmiller, D.; Lee, H. S.; Liu, Y.; McCreight, J. L.; Newman, A. J.; Oubeidillah, A.; Pan, L.; Pham, C.; Salas, F.; Sampson, K. M.; Sood, G.; Wood, A.; Yates, D. N.; Yu, W.</p> <p>2016-12-01</p> <p>The National <span class="hlt">Weather</span> Service (NWS) Office of Water Prediction (OWP), in conjunction with the National Center for Atmospheric Research (NCAR) and the NWS National Centers for Environmental Prediction (NCEP) recently implemented version 1.0 of the National Water <span class="hlt">Model</span> (NWM) into operations. This <span class="hlt">model</span> is an hourly cycling uncoupled analysis and forecast <span class="hlt">system</span> that provides streamflow for 2.7 million river reaches and other hydrologic information on 1km and 250m grids. It will provide complementary hydrologic guidance at current NWS river forecast locations and significantly expand guidance coverage and type in underserved locations. The core of this <span class="hlt">system</span> is the NCAR-supported community <span class="hlt">Weather</span> Research and Forecasting (WRF)-Hydro hydrologic <span class="hlt">model</span>. It ingests forcing from a variety of sources including Multi-Sensor Multi-Radar (MRMS) radar-gauge observed precipitation data and High Resolution Rapid Refresh (HRRR), Rapid Refresh (RAP), Global Forecast <span class="hlt">System</span> (GFS) and Climate Forecast <span class="hlt">System</span> (CFS) forecast data. WRF-Hydro is configured to use the Noah-Multi Parameterization (Noah-MP) Land Surface <span class="hlt">Model</span> (LSM) to simulate land surface processes. Separate water routing modules perform diffusive wave surface routing and saturated subsurface flow routing on a 250m grid, and Muskingum-Cunge channel routing down National Hydrogaphy Dataset Plus V2 (NHDPlusV2) stream reaches. River analyses and forecasts are provided across a domain encompassing the Continental United States (CONUS) and hydrologically contributing areas, while land surface output is available on a larger domain that extends beyond the CONUS into Canada and Mexico (roughly from latitude 19N to 58N). The <span class="hlt">system</span> includes an analysis and assimilation configuration along with three forecast configurations. These include a short-range 15 hour deterministic forecast, a medium-Range 10 day deterministic forecast and a long-range 30 day 16-member ensemble forecast. United Sates Geologic Survey (USGS) streamflow</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2014AGUFMSM31A4184C','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2014AGUFMSM31A4184C"><span>Operational Space <span class="hlt">Weather</span> Needs - Perspectives from SEASONS 2014</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Comberiate, J.; Kelly, M. A.; Paxton, L. J.; Schaefer, R. K.; Bust, G. S.; Sotirelis, T.; Fox, N. J.</p> <p>2014-12-01</p> <p>A key challenge for the operational space <span class="hlt">weather</span> community is the gap between the latest scientific data, <span class="hlt">models</span>, methods, and indices and those that are currently used in operational <span class="hlt">systems</span>. The November 2014 SEASONS (Space Environment Applications, <span class="hlt">Systems</span>, and Operations for National Security) Workshop at JHU/APL in Laurel, Maryland, brings together representatives from the operational and scientific communities. The theme of SEASONS 2014 is "Beyond Climatology," with a focus on how space <span class="hlt">weather</span> events threaten operational assets and disrupt missions. Here we present perspectives from SEASONS 2014 on new observations, <span class="hlt">models</span> in development, and forecasting methods that are of interest to the operational space <span class="hlt">weather</span> community. Highlighted topics include ionospheric data assimilation and forecasting <span class="hlt">models</span>, HF propagation <span class="hlt">models</span>, radiation belt observations, and energetic particle <span class="hlt">modeling</span>. The SEASONS 2014 web site can be found at https://secwww.jhuapl.edu/SEASONS/</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://rosap.ntl.bts.gov/view/dot/3350','DOTNTL'); return false;" href="https://rosap.ntl.bts.gov/view/dot/3350"><span>Integrating Clarus data in traffic signal <span class="hlt">system</span> operation : a survivable real-time <span class="hlt">weather</span>-responsive <span class="hlt">system</span>.</span></a></p> <p><a target="_blank" href="http://ntlsearch.bts.gov/tris/index.do">DOT National Transportation Integrated Search</a></p> <p></p> <p>2011-07-11</p> <p>This report presents a prototype of a secure, dependable, real-time <span class="hlt">weather</span>-responsive traffic signal <span class="hlt">system</span>. The prototype executes two tasks: 1) accesses <span class="hlt">weather</span> information that provides near real-time atmospheric and pavement surface condition ob...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=3563012','PMC'); return false;" href="https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=3563012"><span>A Bayesian hierarchical <span class="hlt">model</span> with spatial variable selection: the effect of <span class="hlt">weather</span> on insurance claims</span></a></p> <p><a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pmc">PubMed Central</a></p> <p>Scheel, Ida; Ferkingstad, Egil; Frigessi, Arnoldo; Haug, Ola; Hinnerichsen, Mikkel; Meze-Hausken, Elisabeth</p> <p>2013-01-01</p> <p>Climate change will affect the insurance industry. We develop a Bayesian hierarchical statistical approach to explain and predict insurance losses due to <span class="hlt">weather</span> events at a local geographic scale. The number of <span class="hlt">weather</span>-related insurance claims is <span class="hlt">modelled</span> by combining generalized linear <span class="hlt">models</span> with spatially smoothed variable selection. Using Gibbs sampling and reversible jump Markov chain Monte Carlo methods, this <span class="hlt">model</span> is fitted on daily <span class="hlt">weather</span> and insurance data from each of the 319 municipalities which constitute southern and central Norway for the period 1997–2006. Precise out-of-sample predictions validate the <span class="hlt">model</span>. Our results show interesting regional patterns in the effect of different <span class="hlt">weather</span> covariates. In addition to being useful for insurance pricing, our <span class="hlt">model</span> can be used for short-term predictions based on <span class="hlt">weather</span> forecasts and for long-term predictions based on downscaled climate <span class="hlt">models</span>. PMID:23396890</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2009IJBm...53..101K','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2009IJBm...53..101K"><span>Psychological mechanisms in outdoor place and <span class="hlt">weather</span> assessment: towards a conceptual <span class="hlt">model</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Knez, Igor; Thorsson, Sofia; Eliasson, Ingegärd; Lindberg, Fredrik</p> <p>2009-01-01</p> <p>The general aim has been to illuminate the psychological mechanisms involved in outdoor place and <span class="hlt">weather</span> assessment. This reasoning was conceptualized in a <span class="hlt">model</span>, tentatively proposing direct and indirect links of influence in an outdoor place-human relationship. The <span class="hlt">model</span> was subsequently tested by an empirical study, performed in a Nordic city, on the impact of <span class="hlt">weather</span> and personal factors on participants’ perceptual and emotional estimations of outdoor urban places. In line with our predictions, we report significant influences of <span class="hlt">weather</span> parameters (air temperature, wind, and cloudlessness) and personal factors (environmental attitude and age) on participants’ perceptual and emotional estimations of outdoor urban places. All this is a modest, yet significant, step towards an understanding of the psychology of outdoor place and <span class="hlt">weather</span> assessment.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.osti.gov/servlets/purl/1079638','SCIGOV-STC'); return false;" href="https://www.osti.gov/servlets/purl/1079638"><span>Using <span class="hlt">Weather</span> Data and Climate <span class="hlt">Model</span> Output in Economic Analyses of Climate Change</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>Auffhammer, M.; Hsiang, S. M.; Schlenker, W.</p> <p>2013-06-28</p> <p>Economists are increasingly using <span class="hlt">weather</span> data and climate <span class="hlt">model</span> output in analyses of the economic impacts of climate change. This article introduces a set of <span class="hlt">weather</span> data sets and climate <span class="hlt">models</span> that are frequently used, discusses the most common mistakes economists make in using these products, and identifies ways to avoid these pitfalls. We first provide an introduction to <span class="hlt">weather</span> data, including a summary of the types of datasets available, and then discuss five common pitfalls that empirical researchers should be aware of when using historical <span class="hlt">weather</span> data as explanatory variables in econometric applications. We then provide a brief overviewmore » of climate <span class="hlt">models</span> and discuss two common and significant errors often made by economists when climate <span class="hlt">model</span> output is used to simulate the future impacts of climate change on an economic outcome of interest.« less</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017AGUFMIN43C0089M','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017AGUFMIN43C0089M"><span>Using Space <span class="hlt">Weather</span> for Enhanced, Extreme Terrestrial <span class="hlt">Weather</span> Predictions.</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>McKenna, M. H.; Lee, T. A., III</p> <p>2017-12-01</p> <p>Considering the complexities of the Sun-Earth <span class="hlt">system</span>, the impacts of space <span class="hlt">weather</span> to <span class="hlt">weather</span> here on Earth are not fully understood. This study attempts to analyze this interrelationship by providing a theoretical framework for studying the varied modalities of solar inclination and explores the extent to which they contribute, both in formation and intensity, to extreme terrestrial <span class="hlt">weather</span>. Using basic topologic and ontology engineering concepts (TOEC), the transdisciplinary syntaxes of space physics, geophysics, and meteorology are analyzed as a seamless interrelated <span class="hlt">system</span>. This paper reports this investigation's initial findings and examines the validity of the question "Does space <span class="hlt">weather</span> contribute to extreme <span class="hlt">weather</span> on Earth, and if so, to what degree?"</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/20140006421','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/20140006421"><span>Tethered Satellites as Enabling Platforms for an Operational Space <span class="hlt">Weather</span> Monitoring <span class="hlt">System</span></span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Krause, L. Habash; Gilchrist, B. E.; Bilen, S.; Owens, J.; Voronka, N.; Furhop, K.</p> <p>2013-01-01</p> <p>Space <span class="hlt">weather</span> nowcasting and forecasting <span class="hlt">models</span> require assimilation of near-real time (NRT) space environment data to improve the precision and accuracy of operational products. Typically, these <span class="hlt">models</span> begin with a climatological <span class="hlt">model</span> to provide "most probable distributions" of environmental parameters as a function of time and space. The process of NRT data assimilation gently pulls the climate <span class="hlt">model</span> closer toward the observed state (e.g. via Kalman smoothing) for nowcasting, and forecasting is achieved through a set of iterative physics-based forward-prediction calculations. The issue of required space <span class="hlt">weather</span> observatories to meet the spatial and temporal requirements of these <span class="hlt">models</span> is a complex one, and we do not address that with this poster. Instead, we present some examples of how tethered satellites can be used to address the shortfalls in our ability to measure critical environmental parameters necessary to drive these space <span class="hlt">weather</span> <span class="hlt">models</span>. Examples include very long baseline electric field measurements, magnetized ionospheric conductivity measurements, and the ability to separate temporal from spatial irregularities in environmental parameters. Tethered satellite functional requirements will be presented for each space <span class="hlt">weather</span> parameter considered in this study.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://rosap.ntl.bts.gov/view/dot/3685','DOTNTL'); return false;" href="https://rosap.ntl.bts.gov/view/dot/3685"><span>Final report of the operation and demonstration test of short-range <span class="hlt">weather</span> forecasting decision support within an advanced transportation <span class="hlt">weather</span> information <span class="hlt">system</span> (#Safe)</span></a></p> <p><a target="_blank" href="http://ntlsearch.bts.gov/tris/index.do">DOT National Transportation Integrated Search</a></p> <p></p> <p>2006-04-01</p> <p>The purpose of the Advanced Transportation <span class="hlt">Weather</span> Information <span class="hlt">System</span> (ATWIS) was to provide en-route <span class="hlt">weather</span> forecasts and road condition information to the traveling public across North Dakota and South Dakota. ATWIS was the first <span class="hlt">system</span> to develop...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2012AGUFMAE11A..06M','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2012AGUFMAE11A..06M"><span>Lightning Forecasts and Data Assimilation into Numerical <span class="hlt">Weather</span> Prediction <span class="hlt">Models</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>MacGorman, D. R.; Mansell, E. R.; Fierro, A.; Ziegler, C.</p> <p>2012-12-01</p> <p>This presentation reviews two aspects of lightning in numerical <span class="hlt">weather</span> prediction (NWP) <span class="hlt">models</span>: forecasting lightning and assimilating lightning data into NWP <span class="hlt">models</span> to improve <span class="hlt">weather</span> forecasts. One of the earliest routine forecasts of lightning was developed for fire <span class="hlt">weather</span> operations. This approach used a multi-parameter regression analysis of archived cloud-to-ground (CG) lightning data and archived NWP data to optimize the combination of <span class="hlt">model</span> state variables to use in forecast equations for various CG rates. Since then, understanding of how storms produce lightning has improved greatly. As the treatment of ice in microphysics packages used by NWP <span class="hlt">models</span> has improved and the horizontal resolution of <span class="hlt">models</span> has begun approaching convection-permitting scales (with convection-resolving scales on the horizon), it is becoming possible to use this improved understanding in NWP <span class="hlt">models</span> to predict lightning more directly. An important role for data assimilation in NWP <span class="hlt">models</span> is to depict the location, timing, and spatial extent of thunderstorms during <span class="hlt">model</span> spin-up so that the effects of prior convection that can strongly influence future thunderstorm activity, such as updrafts and outflow boundaries, can be included in the initial state of a NWP <span class="hlt">model</span> run. Radar data have traditionally been used, but <span class="hlt">systems</span> that map lightning activity with varying degrees of coverage, detail, and detection efficiency are now available routinely over large regions and reveal information about storms that is complementary to the information provided by radar. Because data from lightning mapping <span class="hlt">systems</span> are compact, easily handled, and reliably indicate the location and timing of thunderstorms, even in regions with little or no radar coverage, several groups have investigated techniques for assimilating these data into NWP <span class="hlt">models</span>. This application will become even more valuable with the launch of the Geostationary Lightning Mapper on the GOES-R satellite, which will extend routine</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=4063030','PMC'); return false;" href="https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=4063030"><span>A Space <span class="hlt">Weather</span> Forecasting <span class="hlt">System</span> with Multiple Satellites Based on a Self-Recognizing Network</span></a></p> <p><a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pmc">PubMed Central</a></p> <p>Tokumitsu, Masahiro; Ishida, Yoshiteru</p> <p>2014-01-01</p> <p>This paper proposes a space <span class="hlt">weather</span> forecasting <span class="hlt">system</span> at geostationary orbit for high-energy electron flux (>2 MeV). The forecasting <span class="hlt">model</span> involves multiple sensors on multiple satellites. The sensors interconnect and evaluate each other to predict future conditions at geostationary orbit. The proposed forecasting <span class="hlt">model</span> is constructed using a dynamic relational network for sensor diagnosis and event monitoring. The sensors of the proposed <span class="hlt">model</span> are located at different positions in space. The satellites for solar monitoring equip with monitoring devices for the interplanetary magnetic field and solar wind speed. The satellites orbit near the Earth monitoring high-energy electron flux. We investigate forecasting for typical two examples by comparing the performance of two <span class="hlt">models</span> with different numbers of sensors. We demonstrate the prediction by the proposed <span class="hlt">model</span> against coronal mass ejections and a coronal hole. This paper aims to investigate a possibility of space <span class="hlt">weather</span> forecasting based on the satellite network with in-situ sensing. PMID:24803190</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/24803190','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/24803190"><span>A space <span class="hlt">weather</span> forecasting <span class="hlt">system</span> with multiple satellites based on a self-recognizing network.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Tokumitsu, Masahiro; Ishida, Yoshiteru</p> <p>2014-05-05</p> <p>This paper proposes a space <span class="hlt">weather</span> forecasting <span class="hlt">system</span> at geostationary orbit for high-energy electron flux (>2 MeV). The forecasting <span class="hlt">model</span> involves multiple sensors on multiple satellites. The sensors interconnect and evaluate each other to predict future conditions at geostationary orbit. The proposed forecasting <span class="hlt">model</span> is constructed using a dynamic relational network for sensor diagnosis and event monitoring. The sensors of the proposed <span class="hlt">model</span> are located at different positions in space. The satellites for solar monitoring equip with monitoring devices for the interplanetary magnetic field and solar wind speed. The satellites orbit near the Earth monitoring high-energy electron flux. We investigate forecasting for typical two examples by comparing the performance of two <span class="hlt">models</span> with different numbers of sensors. We demonstrate the prediction by the proposed <span class="hlt">model</span> against coronal mass ejections and a coronal hole. This paper aims to investigate a possibility of space <span class="hlt">weather</span> forecasting based on the satellite network with in-situ sensing.</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/2060/19870010632','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/19870010632"><span>Predicting the magnetospheric plasma of <span class="hlt">weather</span></span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Dawson, John M.</p> <p>1986-01-01</p> <p>The prediction of the plasma environment in time, the plasma <span class="hlt">weather</span>, is discussed. It is important to be able to predict when large magnetic storms will produce auroras, which will affect the space station operating in low orbit, and what precautions to take both for personnel and sensitive control (computer) equipment onboard. It is also important to start to establish a set of plasma <span class="hlt">weather</span> records and a record of the ability to predict this <span class="hlt">weather</span>. A successful forecasting <span class="hlt">system</span> requires a set of satellite <span class="hlt">weather</span> stations to provide data from which predictions can be made and a set of plasma <span class="hlt">weather</span> codes capable of accurately forecasting the status of the Earth's magnetosphere. A numerical magnetohydrodynamic fluid <span class="hlt">model</span> which is used to <span class="hlt">model</span> the flow in the magnetosphere, the currents flowing into and out of the auroral regions, the magnetopause, the bow shock location and the magnetotail of the Earth is discussed.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2006AGUFM.H23E1559D','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2006AGUFM.H23E1559D"><span>On the assimilation of satellite derived soil moisture in numerical <span class="hlt">weather</span> prediction <span class="hlt">models</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Drusch, M.</p> <p>2006-12-01</p> <p>Satellite derived surface soil moisture data sets are readily available and have been used successfully in hydrological applications. In many operational numerical <span class="hlt">weather</span> prediction <span class="hlt">systems</span> the initial soil moisture conditions are analysed from the <span class="hlt">modelled</span> background and 2 m temperature and relative humidity. This approach has proven its efficiency to improve surface latent and sensible heat fluxes and consequently the forecast on large geographical domains. However, since soil moisture is not always related to screen level variables, <span class="hlt">model</span> errors and uncertainties in the forcing data can accumulate in root zone soil moisture. Remotely sensed surface soil moisture is directly linked to the <span class="hlt">model</span>'s uppermost soil layer and therefore is a stronger constraint for the soil moisture analysis. Three data assimilation experiments with the Integrated Forecast <span class="hlt">System</span> (IFS) of the European Centre for Medium-range <span class="hlt">Weather</span> Forecasts (ECMWF) have been performed for the two months period of June and July 2002: A control run based on the operational soil moisture analysis, an open loop run with freely evolving soil moisture, and an experimental run incorporating bias corrected TMI (TRMM Microwave Imager) derived soil moisture over the southern United States through a nudging scheme using 6-hourly departures. Apart from the soil moisture analysis, the <span class="hlt">system</span> setup reflects the operational forecast configuration including the atmospheric 4D-Var analysis. Soil moisture analysed in the nudging experiment is the most accurate estimate when compared against in-situ observations from the Oklahoma Mesonet. The corresponding forecast for 2 m temperature and relative humidity is almost as accurate as in the control experiment. Furthermore, it is shown that the soil moisture analysis influences local <span class="hlt">weather</span> parameters including the planetary boundary layer height and cloud coverage. The transferability of the results to other satellite derived soil moisture data sets will be discussed.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/20020086343','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/20020086343"><span><span class="hlt">Weather</span> Information Processing</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p></p> <p>1991-01-01</p> <p>Science Communications International (SCI), formerly General Science Corporation, has developed several commercial products based upon experience acquired as a NASA Contractor. Among them are METPRO, a meteorological data acquisition and processing <span class="hlt">system</span>, which has been widely used, RISKPRO, an environmental assessment <span class="hlt">system</span>, and MAPPRO, a geographic information <span class="hlt">system</span>. METPRO software is used to collect <span class="hlt">weather</span> data from satellites, ground-based observation <span class="hlt">systems</span> and radio <span class="hlt">weather</span> broadcasts to generate <span class="hlt">weather</span> maps, enabling potential disaster areas to receive advance warning. GSC's initial work for NASA Goddard Space Flight Center resulted in METPAK, a <span class="hlt">weather</span> satellite data analysis <span class="hlt">system</span>. METPAK led to the commercial METPRO <span class="hlt">system</span>. The company also provides data to other government agencies, U.S. embassies and foreign countries.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/20110023352','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/20110023352"><span>Updates on CCMC Activities and GSFC Space <span class="hlt">Weather</span> Services</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Zhengm Y.; Hesse, M.; Kuznetsova, M.; Pulkkinen, A.; Rastaetter, L.; Maddox, M.; Taktakishvili, A.; Berrios, D.; Chulaki, A.; Lee, H.; <a style="text-decoration: none; " href="javascript:void(0); " onClick="displayelement('author_20110023352'); toggleEditAbsImage('author_20110023352_show'); toggleEditAbsImage('author_20110023352_hide'); "> <img style="display:inline; width:12px; height:12px; " src="images/arrow-up.gif" width="12" height="12" border="0" alt="hide" id="author_20110023352_show"> <img style="width:12px; height:12px; display:none; " src="images/arrow-down.gif" width="12" height="12" border="0" alt="hide" id="author_20110023352_hide"></p> <p>2011-01-01</p> <p>In this presentation, we provide updates on CCMC <span class="hlt">modeling</span> activities, CCMC metrics and validation studies, and other CCMC efforts. In addition, an overview of GSFC Space <span class="hlt">Weather</span> Services (a sibling organization to the Community Coordinated <span class="hlt">Modeling</span> Center) and its products/capabilities will be given. We show how some of the research grade <span class="hlt">models</span>, if running in an operational mode, can help address NASA's space <span class="hlt">weather</span> needs by providing forecasting/now casting capabilities of significant space <span class="hlt">weather</span> events throughout the solar <span class="hlt">system</span>.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2016AGUFMGC53E1338C','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2016AGUFMGC53E1338C"><span>Next generation of <span class="hlt">weather</span> generators on web service framework</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Chinnachodteeranun, R.; Hung, N. D.; Honda, K.; Ines, A. V. M.</p> <p>2016-12-01</p> <p><span class="hlt">Weather</span> generator is a statistical <span class="hlt">model</span> that synthesizes possible realization of long-term historical <span class="hlt">weather</span> in future. It generates several tens to hundreds of realizations stochastically based on statistical analysis. Realization is essential information as a crop <span class="hlt">modeling</span>'s input for simulating crop growth and yield. Moreover, they can be contributed to analyzing uncertainty of <span class="hlt">weather</span> to crop development stage and to decision support <span class="hlt">system</span> on e.g. water management and fertilizer management. Performing crop <span class="hlt">modeling</span> requires multidisciplinary skills which limit the usage of <span class="hlt">weather</span> generator only in a research group who developed it as well as a barrier for newcomers. To improve the procedures of performing <span class="hlt">weather</span> generators as well as the methodology to acquire the realization in a standard way, we implemented a framework for providing <span class="hlt">weather</span> generators as web services, which support service interoperability. Legacy <span class="hlt">weather</span> generator programs were wrapped in the web service framework. The service interfaces were implemented based on an international standard that was Sensor Observation Service (SOS) defined by Open Geospatial Consortium (OGC). Clients can request realizations generated by the <span class="hlt">model</span> through SOS Web service. Hierarchical data preparation processes required for <span class="hlt">weather</span> generator are also implemented as web services and seamlessly wired. Analysts and applications can invoke services over a network easily. The services facilitate the development of agricultural applications and also reduce the workload of analysts on iterative data preparation and handle legacy <span class="hlt">weather</span> generator program. This architectural design and implementation can be a prototype for constructing further services on top of interoperable sensor network <span class="hlt">system</span>. This framework opens an opportunity for other sectors such as application developers and scientists in other fields to utilize <span class="hlt">weather</span> generators.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2005IJCli..25.1881C','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2005IJCli..25.1881C"><span><span class="hlt">Weather</span> and seasonal climate prediction for South America using a multi-<span class="hlt">model</span> superensemble</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Chaves, Rosane R.; Ross, Robert S.; Krishnamurti, T. N.</p> <p>2005-11-01</p> <p>This work examines the feasibility of <span class="hlt">weather</span> and seasonal climate predictions for South America using the multi-<span class="hlt">model</span> synthetic superensemble approach for climate, and the multi-<span class="hlt">model</span> conventional superensemble approach for numerical <span class="hlt">weather</span> prediction, both developed at Florida State University (FSU). The effect on seasonal climate forecasts of the number of <span class="hlt">models</span> used in the synthetic superensemble is investigated. It is shown that the synthetic superensemble approach for climate and the conventional superensemble approach for numerical <span class="hlt">weather</span> prediction can reduce the errors over South America in seasonal climate prediction and numerical <span class="hlt">weather</span> prediction.For climate prediction, a suite of 13 <span class="hlt">models</span> is used. The forecast lead-time is 1 month for the climate forecasts, which consist of precipitation and surface temperature forecasts. The multi-<span class="hlt">model</span> ensemble is comprised of four versions of the FSU-Coupled Ocean-Atmosphere <span class="hlt">Model</span>, seven <span class="hlt">models</span> from the Development of a European Multi-<span class="hlt">model</span> Ensemble <span class="hlt">System</span> for Seasonal to Interannual Prediction (DEMETER), a version of the Community Climate <span class="hlt">Model</span> (CCM3), and a version of the predictive Ocean Atmosphere <span class="hlt">Model</span> for Australia (POAMA). The results show that conditions over South America are appropriately simulated by the Florida State University Synthetic Superensemble (FSUSSE) in comparison to observations and that the skill of this approach increases with the use of additional <span class="hlt">models</span> in the ensemble. When compared to observations, the forecasts are generally better than those from both a single climate <span class="hlt">model</span> and the multi-<span class="hlt">model</span> ensemble mean, for the variables tested in this study.For numerical <span class="hlt">weather</span> prediction, the conventional Florida State University Superensemble (FSUSE) is used to predict the mass and motion fields over South America. Predictions of mean sea level pressure, 500 hPa geopotential height, and 850 hPa wind are made with a multi-<span class="hlt">model</span> superensemble comprised of six global <span class="hlt">models</span> for the period</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2011AGUFM.G23A0852F','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2011AGUFM.G23A0852F"><span>Application of Numerical <span class="hlt">Weather</span> <span class="hlt">Models</span> to Mitigating Atmospheric Artifacts in InSAR</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Foster, J. H.; Kealy, J.; Businger, S.; Cherubini, T.; Brooks, B. A.; Albers, S. C.; Lu, Z.; Poland, M. P.; Chen, S.; Mass, C.</p> <p>2011-12-01</p> <p>A high-resolution <span class="hlt">weather</span> "hindcasting" <span class="hlt">system</span> to <span class="hlt">model</span> the atmosphere at the time of SAR scene acquisitions has been established to investigate and mitigate the impact of atmospheric water vapor on InSAR deformation maps. Variations in the distributions of water vapor in the atmosphere between SAR acquisitions lead to artifacts in interferograms that can mask real ground motion signals. A database of regional numerical <span class="hlt">weather</span> prediction <span class="hlt">model</span> outputs generated by the University of Washington and U.C. Davis for times matching SAR acquisitions was used as "background" for higher resolution analyses of the atmosphere for Mount St Helens volcano in Washington, and Los Angeles in southern California. Using this background, we use LAPS to incrementally incorporate all other available meteorological data sets, including GPS, to explore the impact of additional observations on <span class="hlt">model</span> accuracy. Our results suggest that, even with significant quantities of contemporaneously measured data, high-resolution atmospheric analyses are unable to <span class="hlt">model</span> the timing and location of water vapor perturbations accurately enough to produce robust and reliable phase screens that can be directly subtracted from interferograms. Despite this, the analyses are able to reproduce the statistical character of the atmosphere with some confidence, suggesting that, in the absence of unusually dense in-situ measurements (such as is the case with GPS data for Los Angeles), <span class="hlt">weather</span> analysis can play a valuable role in constraining the power-spectrum expected in an interferogram due to the troposphere. This could be used to provide objective weights to scenes during traditional stacking or to tune the filter parameters in time-series analyses.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2012AGUFMIN33C1562M','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2012AGUFMIN33C1562M"><span>Innovative Near Real-Time Data Dissemination Tools Developed by the Space <span class="hlt">Weather</span> Research Center</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Mullinix, R.; Maddox, M. M.; Berrios, D.; Kuznetsova, M.; Pulkkinen, A.; Rastaetter, L.; Zheng, Y.</p> <p>2012-12-01</p> <p>Space <span class="hlt">weather</span> affects virtually all of NASA's endeavors, from robotic missions to human exploration. Knowledge and prediction of space <span class="hlt">weather</span> conditions are therefore essential to NASA operations. The diverse nature of currently available space environment measurements and <span class="hlt">modeling</span> products compels the need for a single access point to such information. The Integrated Space <span class="hlt">Weather</span> Analysis (iSWA) <span class="hlt">System</span> provides this single point access along with the capability to collect and catalog a vast range of sources including both observational and <span class="hlt">model</span> data. NASA Goddard Space <span class="hlt">Weather</span> Research Center heavily utilizes the iSWA <span class="hlt">System</span> daily for research, space <span class="hlt">weather</span> <span class="hlt">model</span> validation, and forecasting for NASA missions. iSWA provides the capabilities to view and analyze near real-time space <span class="hlt">weather</span> data from any where in the world. This presentation will describe the technology behind the iSWA <span class="hlt">system</span> and describe how to use the <span class="hlt">system</span> for space <span class="hlt">weather</span> research, forecasting, training, education, and sharing.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2018JSWSC...8A...3P','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2018JSWSC...8A...3P"><span>North Europe power transmission <span class="hlt">system</span> vulnerability during extreme space <span class="hlt">weather</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Piccinelli, Roberta; Krausmann, Elisabeth</p> <p>2018-01-01</p> <p>Space <span class="hlt">weather</span> driven by solar activity can induce geomagnetic disturbances at the Earth's surface that can affect power transmission <span class="hlt">systems</span>. Variations in the geomagnetic field result in geomagnetically induced currents that can enter the <span class="hlt">system</span> through its grounding connections, saturate transformers and lead to <span class="hlt">system</span> instability and possibly collapse. This study analyzes the impact of extreme space <span class="hlt">weather</span> on the northern part of the European power transmission grid for different transformer designs to understand its vulnerability in case of an extreme event. The behavior of the <span class="hlt">system</span> was analyzed in its operational mode during a severe geomagnetic storm, and mitigation measures, like line compensation, were also considered. These measures change the topology of the <span class="hlt">system</span>, thus varying the path of geomagnetically induced currents and inducing a local imbalance in the voltage stability superimposed on the grid operational flow. Our analysis shows that the North European power transmission <span class="hlt">system</span> is fairly robust against extreme space <span class="hlt">weather</span> events. When considering transformers more vulnerable to geomagnetic storms, only few episodes of instability were found in correspondence with an existing voltage instability due to the underlying <span class="hlt">system</span> load. The presence of mitigation measures limited the areas of the network in which bus voltage instabilities arise with respect to the <span class="hlt">system</span> in which mitigation measures are absent.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2015EGUGA..1712788H','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2015EGUGA..1712788H"><span>Climate Central World <span class="hlt">Weather</span> Attribution (WWA) project: Real-time extreme <span class="hlt">weather</span> event attribution analysis</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Haustein, Karsten; Otto, Friederike; Uhe, Peter; Allen, Myles; Cullen, Heidi</p> <p>2015-04-01</p> <p>Extreme <span class="hlt">weather</span> detection and attribution analysis has emerged as a core theme in climate science over the last decade or so. By using a combination of observational data and climate <span class="hlt">models</span> it is possible to identify the role of climate change in certain types of extreme <span class="hlt">weather</span> events such as sea level rise and its contribution to storm surges, extreme heat events and droughts or heavy rainfall and flood events. These analyses are usually carried out after an extreme event has occurred when reanalysis and observational data become available. The Climate Central WWA project will exploit the increasing forecast skill of seasonal forecast prediction <span class="hlt">systems</span> such as the UK MetOffice GloSea5 (Global seasonal forecasting <span class="hlt">system</span>) ensemble forecasting method. This way, the current <span class="hlt">weather</span> can be fed into climate <span class="hlt">models</span> to simulate large ensembles of possible <span class="hlt">weather</span> scenarios before an event has fully emerged yet. This effort runs along parallel and intersecting tracks of science and communications that involve research, message development and testing, staged socialization of attribution science with key audiences, and dissemination. The method we employ uses a very large ensemble of simulations of regional climate <span class="hlt">models</span> to run two different analyses: one to represent the current climate as it was observed, and one to represent the same events in the world that might have been without human-induced climate change. For the <span class="hlt">weather</span> "as observed" experiment, the atmospheric <span class="hlt">model</span> uses observed sea surface temperature (SST) data from GloSea5 (currently) and present-day atmospheric gas concentrations to simulate <span class="hlt">weather</span> events that are possible given the observed climate conditions. The <span class="hlt">weather</span> in the "world that might have been" experiments is obtained by removing the anthropogenic forcing from the observed SSTs, thereby simulating a counterfactual world without human activity. The anthropogenic forcing is obtained by comparing the CMIP5 historical and natural simulations</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/20140008304','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/20140008304"><span>Prediction of <span class="hlt">Weather</span> Impacted Airport Capacity using Ensemble Learning</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Wang, Yao Xun</p> <p>2011-01-01</p> <p>Ensemble learning with the Bagging Decision Tree (BDT) <span class="hlt">model</span> was used to assess the impact of <span class="hlt">weather</span> on airport capacities at selected high-demand airports in the United States. The ensemble bagging decision tree <span class="hlt">models</span> were developed and validated using the Federal Aviation Administration (FAA) Aviation <span class="hlt">System</span> Performance Metrics (ASPM) data and <span class="hlt">weather</span> forecast at these airports. The study examines the performance of BDT, along with traditional single Support Vector Machines (SVM), for airport runway configuration selection and airport arrival rates (AAR) prediction during <span class="hlt">weather</span> impacts. Testing of these <span class="hlt">models</span> was accomplished using observed <span class="hlt">weather</span>, <span class="hlt">weather</span> forecast, and airport operation information at the chosen airports. The experimental results show that ensemble methods are more accurate than a single SVM classifier. The airport capacity ensemble method presented here can be used as a decision support <span class="hlt">model</span> that supports air traffic flow management to meet the <span class="hlt">weather</span> impacted airport capacity in order to reduce costs and increase safety.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2009GBioC..23.4013B','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2009GBioC..23.4013B"><span>Process-based <span class="hlt">modeling</span> of silicate mineral <span class="hlt">weathering</span> responses to increasing atmospheric CO2 and climate change</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Banwart, Steven A.; Berg, Astrid; Beerling, David J.</p> <p>2009-12-01</p> <p>A mathematical <span class="hlt">model</span> describes silicate mineral <span class="hlt">weathering</span> processes in modern soils located in the boreal coniferous region of northern Europe. The process <span class="hlt">model</span> results demonstrate a stabilizing biological feedback mechanism between atmospheric CO2 levels and silicate <span class="hlt">weathering</span> rates as is generally postulated for atmospheric evolution. The process <span class="hlt">model</span> feedback response agrees within a factor of 2 of that calculated by a <span class="hlt">weathering</span> feedback function of the type generally employed in global geochemical carbon cycle <span class="hlt">models</span> of the Earth's Phanerozoic CO2 history. Sensitivity analysis of parameter values in the process <span class="hlt">model</span> provides insight into the key mechanisms that influence the strength of the biological feedback to <span class="hlt">weathering</span>. First, the process <span class="hlt">model</span> accounts for the alkalinity released by <span class="hlt">weathering</span>, whereby its acceleration stabilizes pH at values that are higher than expected. Although the process <span class="hlt">model</span> yields faster <span class="hlt">weathering</span> with increasing temperature, because of activation energy effects on mineral dissolution kinetics at warmer temperature, the mineral dissolution rate laws utilized in the process <span class="hlt">model</span> also result in lower dissolution rates at higher pH values. Hence, as dissolution rates increase under warmer conditions, more alkalinity is released by the <span class="hlt">weathering</span> reaction, helping maintain higher pH values thus stabilizing the <span class="hlt">weathering</span> rate. Second, the process <span class="hlt">model</span> yields a relatively low sensitivity of soil pH to increasing plant productivity. This is due to more rapid decomposition of dissolved organic carbon (DOC) under warmer conditions. Because DOC fluxes strongly influence the soil water proton balance and pH, this increased decomposition rate dampens the feedback between productivity and <span class="hlt">weathering</span>. The process <span class="hlt">model</span> is most sensitive to parameters reflecting soil structure; depth, porosity, and water content. This suggests that the role of biota to influence these characteristics of the <span class="hlt">weathering</span> profile is as important, if not</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://www.dtic.mil/docs/citations/ADA535963','DTIC-ST'); return false;" href="http://www.dtic.mil/docs/citations/ADA535963"><span>Cold <span class="hlt">Weather</span> Admixture <span class="hlt">Systems</span> Demonstration at Fort Wainwright, Alaska</span></a></p> <p><a target="_blank" href="http://www.dtic.mil/">DTIC Science & Technology</a></p> <p></p> <p>2010-08-01</p> <p>3, and 5, the remaining two test sec- tions (Test Sections 2 and 4) were readied for concrete . The interior formwork was removed, and the rebar was...Washington, DC 20314-1000 ERDC/CRREL TR-10-6 ii Abstract: Cold <span class="hlt">Weather</span> Admixture <span class="hlt">Systems</span> (CWAS) is a new approach to cold <span class="hlt">weather</span> concreting that...incorporates suites of commercially avail- able chemical admixtures in concrete mixes. When used in combination, these admixtures depress the freezing</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://www.dtic.mil/docs/citations/ADA626666','DTIC-ST'); return false;" href="http://www.dtic.mil/docs/citations/ADA626666"><span>Toward Seamless <span class="hlt">Weather</span>-Climate Prediction with a Global Cloud Resolving <span class="hlt">Model</span></span></a></p> <p><a target="_blank" href="http://www.dtic.mil/">DTIC Science & Technology</a></p> <p></p> <p>2016-01-14</p> <p>distribution is unlimited. TOWARD SEAMLESS <span class="hlt">WEATHER</span>- CLIMATE PREDICTION WITH A GLOBAL CLOUD RESOLVING <span class="hlt">MODEL</span> PI: Tim Li IPRC/SOEST, University of Hawaii at...Project Final Report 3. DATES COVERED (From - To) 1 May 2012 - 30 September 2015 4. TITLE AND SUBTITLE TOWARD SEAMLESS <span class="hlt">WEATHER</span>- CLIMATE PREDICTION WITH...A GLOBAL CLOUD RESOLVING <span class="hlt">MODEL</span> 5a. CONTRACT NUMBER 5b. GRANT NUMBER N000141210450 5c. PROGRAM ELEMENT NUMBER ONR Marine Meteorology Program 6</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://rosap.ntl.bts.gov/view/dot/17126','DOTNTL'); return false;" href="https://rosap.ntl.bts.gov/view/dot/17126"><span>Road <span class="hlt">Weather</span> <span class="hlt">Systems</span> [SD .WMV (720x480/29fps/25.2 MB)</span></a></p> <p><a target="_blank" href="http://ntlsearch.bts.gov/tris/index.do">DOT National Transportation Integrated Search</a></p> <p></p> <p>2009-01-01</p> <p>Iowas road <span class="hlt">weather</span> information <span class="hlt">system</span> at work. The Iowa DOT will install new sensors and upgrades to most road <span class="hlt">weather</span> information <span class="hlt">system</span> (RWIS) sites. These include: : color cameras, new precipitation sensors, new speed sensors, revised weathervi...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/20170009791','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/20170009791"><span>UTM <span class="hlt">Weather</span> Presentation</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Chan, William N.; Kopardekar, Parimal H.; Carmichael, Bruce; Cornman, Larry</p> <p>2017-01-01</p> <p>Presentation highlighting how <span class="hlt">weather</span> affected UAS operations during the UTM field tests. Research to develop UAS <span class="hlt">weather</span> translation <span class="hlt">models</span> with a description of current and future work for UTM <span class="hlt">weather</span>.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://pubs.er.usgs.gov/publication/28633','USGSPUBS'); return false;" href="https://pubs.er.usgs.gov/publication/28633"><span>A conceptual <span class="hlt">weather</span>-type classification procedure for the Philadelphia, Pennsylvania, area</span></a></p> <p><a target="_blank" href="http://pubs.er.usgs.gov/pubs/index.jsp?view=adv">USGS Publications Warehouse</a></p> <p>McCabe, Gregory J.</p> <p>1990-01-01</p> <p>A simple method of <span class="hlt">weather</span>-type classification, based on a conceptual <span class="hlt">model</span> of pressure <span class="hlt">systems</span> that pass through the Philadelphia, Pennsylvania, area, has been developed. The only inputs required for the procedure are daily mean wind direction and cloud cover, which are used to index the relative position of pressure <span class="hlt">systems</span> and fronts to Philadelphia.Daily mean wind-direction and cloud-cover data recorded at Philadelphia, Pennsylvania, from January 1954 through August 1988 were used to categorize daily <span class="hlt">weather</span> conditions. The conceptual <span class="hlt">weather</span> types reflect changes in daily air and dew-point temperatures, and changes in monthly mean temperature and monthly and annual precipitation. The <span class="hlt">weather</span>-type classification produced by using the conceptual <span class="hlt">model</span> was similar to a classification produced by using a multivariate statistical classification procedure. Even though the conceptual <span class="hlt">weather</span> types are derived from a small amount of data, they appear to account for the variability of daily <span class="hlt">weather</span> patterns sufficiently to describe distinct <span class="hlt">weather</span> conditions for use in environmental analyses of <span class="hlt">weather</span>-sensitive processes.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2016AGUFMSM23C..06W','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2016AGUFMSM23C..06W"><span>Operationalizing the Space <span class="hlt">Weather</span> <span class="hlt">Modeling</span> Framework: Challenges and Resolutions</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Welling, D. T.; Gombosi, T. I.; Toth, G.; Singer, H. J.; Millward, G. H.; Balch, C. C.; Cash, M. D.</p> <p>2016-12-01</p> <p>Predicting ground-based magnetic perturbations is a critical step towards specifying and predicting geomagnetically induced currents (GICs) in high voltage transmission lines. Currently, the Space <span class="hlt">Weather</span> <span class="hlt">Modeling</span> Framework (SWMF), a flexible <span class="hlt">modeling</span> framework for simulating the multi-scale space environment, is being transitioned from research to operational use (R2O) by NOAA's Space <span class="hlt">Weather</span> Prediction Center. Upon completion of this transition, the SWMF will provide localized time-varying magnetic field (dB/dt) predictions using real-time solar wind observations from L1 and the F10.7 proxy for EUV as <span class="hlt">model</span> input. This presentation chronicles the challenges encountered during the R2O transition of the SWMF. Because operations relies on frequent calculations of global surface dB/dt, new optimizations were required to keep the <span class="hlt">model</span> running faster than real time. Additionally, several singular situations arose during the 30-day robustness test that required immediate attention. Solutions and strategies for overcoming these issues will be presented. This includes new failsafe options for code execution, new physics and coupling parameters, and the development of an automated validation suite that allows us to monitor performance with code evolution. Finally, the operations-to-research (O2R) impact on SWMF-related research is presented. The lessons learned from this work are valuable and instructive for the space <span class="hlt">weather</span> community as further R2O progress is made.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/FR-2011-10-28/pdf/2011-26791.pdf','FEDREG'); return false;" href="https://www.gpo.gov/fdsys/pkg/FR-2011-10-28/pdf/2011-26791.pdf"><span>76 FR 67018 - Notice to Manufacturers of Airport In-Pavement Stationary Runway <span class="hlt">Weather</span> Information <span class="hlt">Systems</span></span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collection.action?collectionCode=FR">Federal Register 2010, 2011, 2012, 2013, 2014</a></p> <p></p> <p>2011-10-28</p> <p>...-Pavement Stationary Runway <span class="hlt">Weather</span> Information <span class="hlt">Systems</span> AGENCY: Federal Aviation Administration (FAA), U.S. DOT. ACTION: Notice to Manufacturers of In-Pavement Stationary Runway <span class="hlt">Weather</span> Information <span class="hlt">Systems</span>... waivers to foreign manufacturers of Active or Passive In- Pavement Stationary Runway <span class="hlt">Weather</span> Information...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/20110023415','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/20110023415"><span>Space <span class="hlt">Weather</span>, Geomagnetic Disturbances and Impact on the High-Voltage Transmission <span class="hlt">Systems</span></span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Pullkkinen, A.</p> <p>2011-01-01</p> <p>Geomagnetically induced currents (GIC) affecting the performance of high-voltage power transmission <span class="hlt">systems</span> are one of the most significant hazards space <span class="hlt">weather</span> poses on the operability of critical US infrastructure. The severity of the threat was emphasized, for example, in two recent reports: the National Research Council (NRC) report "Severe Space <span class="hlt">Weather</span> Events--Understanding Societal and Economic Impacts: A Workshop Report" and the North American Electric Reliability Corporation (NERC) report "HighImpact, Low-Frequency Event Risk to the North American Bulk Power <span class="hlt">System</span>." The NRC and NERC reports demonstrated the important national security dimension of space <span class="hlt">weather</span> and GIC and called for comprehensive actions to forecast and mitigate the hazard. In this paper we will give a brief overview of space <span class="hlt">weather</span> storms and accompanying geomagnetic storm events that lead to GIC. We will also review the fundamental principles of how GIC can impact the power transmission <span class="hlt">systems</span>. Space <span class="hlt">weather</span> has been a subject of great scientific advances that have changed the wonder of the past to a quantitative field of physics with true predictive power of today. NASA's Solar Shield <span class="hlt">system</span> aimed at forecasting of GIC in the North American high-voltage power transmission <span class="hlt">system</span> can be considered as one of the ultimate fruits of those advances. We will review the fundamental principles of the Solar Shield <span class="hlt">system</span> and provide our view of the way forward in the science of GIC.</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://rosap.ntl.bts.gov/view/dot/6457','DOTNTL'); return false;" href="https://rosap.ntl.bts.gov/view/dot/6457"><span>Road <span class="hlt">Weather</span> Information <span class="hlt">Systems</span> (RWIS) data integration guidelines</span></a></p> <p><a target="_blank" href="http://ntlsearch.bts.gov/tris/index.do">DOT National Transportation Integrated Search</a></p> <p></p> <p>2002-01-01</p> <p>In an effort to reduce winter road maintenance costs, agencies are using Road <span class="hlt">Weather</span> : Information <span class="hlt">Systems</span> (RWIS) to gain more information for application to surface transportation. : RWIS technologies consist of roadside Environmental Sensor Statio...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://pubs.usgs.gov/of/1989/0415/report.pdf','USGSPUBS'); return false;" href="https://pubs.usgs.gov/of/1989/0415/report.pdf"><span>A primer on clothing <span class="hlt">systems</span> for cold-<span class="hlt">weather</span> field work</span></a></p> <p><a target="_blank" href="http://pubs.er.usgs.gov/pubs/index.jsp?view=adv">USGS Publications Warehouse</a></p> <p>Denner, J.C.</p> <p>1993-01-01</p> <p>Hypothermia in cold environments can be prevented by physiological adaptation and by the proper use of cold <span class="hlt">weather</span> clothing. The human body adjusts to cold temperature by increasing the rates of basal metabolism, specific dynamic action, and physical exercise. Heat loss is reduced by vasoconstriction. Clothing <span class="hlt">systems</span> for cold <span class="hlt">weather</span> reduce loss by providing insulation and protection from the elements. Satisfactory cold- <span class="hlt">weather</span> clothing is constructed of wool fabrics or the synthetic fibers polypropylene and polyester. Outerwear suitable for cold climates is insulated with down, high-loft polyester fiberfills, or the new synthetic thin insulators. (USGS)</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2015AGUFMSM13F..01B','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2015AGUFMSM13F..01B"><span>Fifty Years of Space <span class="hlt">Weather</span> Forecasting from Boulder</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Berger, T. E.</p> <p>2015-12-01</p> <p>The first official space <span class="hlt">weather</span> forecast was issued by the Space Disturbances Laboratory in Boulder, Colorado, in 1965, ushering in an era of operational prediction that continues to this day. Today, the National Oceanic and Atmospheric Administration (NOAA) charters the Space <span class="hlt">Weather</span> Prediction Center (SWPC) as one of the nine National Centers for Environmental Prediction (NCEP) to provide the nation's official watches, warnings, and alerts of space <span class="hlt">weather</span> phenomena. SWPC is now integral to national and international efforts to predict space <span class="hlt">weather</span> events, from the common and mild, to the rare and extreme, that can impact critical technological infrastructure. In 2012, the Strategic National Risk Assessment included extreme space <span class="hlt">weather</span> events as low-to-medium probability phenomena that could, unlike any other meteorogical phenomena, have an impact on the government's ability to function. Recognizing this, the White House chartered the Office of Science and Technology Policy (OSTP) to produce the first comprehensive national strategy for the prediction, mitigation, and response to an extreme space <span class="hlt">weather</span> event. The implementation of the National Strategy is ongoing with NOAA, its partners, and stakeholders concentrating on the goal of improving our ability to observe, <span class="hlt">model</span>, and predict the onset and severity of space <span class="hlt">weather</span> events. In addition, work continues with the research community to improve our understanding of the physical mechanisms - on the Sun, in the heliosphere, and in the Earth's magnetic field and upper atmosphere - of space <span class="hlt">weather</span> as well as the effects on critical infrastructure such as electrical power transmission <span class="hlt">systems</span>. In fifty years, people will hopefully look back at the history of operational space <span class="hlt">weather</span> prediction and credit our efforts today with solidifying the necessary developments in observational <span class="hlt">systems</span>, full-physics <span class="hlt">models</span> of the entire Sun-Earth <span class="hlt">system</span>, and tools for predicting the impacts to infrastructure to protect</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2012AGUFMSM22D..02L','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2012AGUFMSM22D..02L"><span>Space <span class="hlt">weather</span> forecasting: Past, Present, Future</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Lanzerotti, L. J.</p> <p>2012-12-01</p> <p>There have been revolutionary advances in electrical technologies over the last 160 years. The historical record demonstrates that space <span class="hlt">weather</span> processes have often provided surprises in the implementation and operation of many of these technologies. The historical record also demonstrates that as the complexity of <span class="hlt">systems</span> increase, including their interconnectedness and interoperability, they can become more susceptible to space <span class="hlt">weather</span> effects. An engineering goal, beginning during the decades following the 1859 Carrington event, has been to attempt to forecast solar-produced disturbances that could affect technical <span class="hlt">systems</span>, be they long grounded conductor-based or radio-based or required for exploration, or the increasingly complex <span class="hlt">systems</span> immersed in the space environment itself. Forecasting of space <span class="hlt">weather</span> events involves both frontier measurements and <span class="hlt">models</span> to address engineering requirements, and industrial and governmental policies that encourage and permit creativity and entrepreneurship. While analogies of space <span class="hlt">weather</span> forecasting to terrestrial <span class="hlt">weather</span> forecasting are frequently made, and while many of the analogies are valid, there are also important differences. This presentation will provide some historical perspectives on the forecast problem, a personal assessment of current status of several areas including important policy issues, and a look into the not-too-distant future.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2005AdSpR..36.2516L','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2005AdSpR..36.2516L"><span>Progress in space <span class="hlt">weather</span> predictions and applications</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Lundstedt, H.</p> <p></p> <p>The methods of today's predictions of space <span class="hlt">weather</span> and effects are so much more advanced and yesterday's statistical methods are now replaced by integrated knowledge-based neuro-computing <span class="hlt">models</span> and MHD methods. Within the ESA Space <span class="hlt">Weather</span> Programme Study a real-time forecast service has been developed for space <span class="hlt">weather</span> and effects. This prototype is now being implemented for specific users. Today's applications are not only so many more but also so much more advanced and user-oriented. A scientist needs real-time predictions of a global index as input for an MHD <span class="hlt">model</span> calculating the radiation dose for EVAs. A power company <span class="hlt">system</span> operator needs a prediction of the local value of a geomagnetically induced current. A science tourist needs to know whether or not aurora will occur. Soon we might even be able to predict the tropospheric climate changes and <span class="hlt">weather</span> caused by the space <span class="hlt">weather</span>.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://pubs.er.usgs.gov/publication/70026139','USGSPUBS'); return false;" href="https://pubs.er.usgs.gov/publication/70026139"><span>Uranium adsorption on <span class="hlt">weathered</span> schist - Intercomparison of <span class="hlt">modeling</span> approaches</span></a></p> <p><a target="_blank" href="http://pubs.er.usgs.gov/pubs/index.jsp?view=adv">USGS Publications Warehouse</a></p> <p>Payne, T.E.; Davis, J.A.; Ochs, M.; Olin, M.; Tweed, C.J.</p> <p>2004-01-01</p> <p>Experimental data for uranium adsorption on a complex <span class="hlt">weathered</span> rock were simulated by twelve <span class="hlt">modelling</span> teams from eight countries using surface complexation (SC) <span class="hlt">models</span>. This intercomparison was part of an international project to evaluate the present capabilities and limitations of SC <span class="hlt">models</span> in representing sorption by geologic materials. The <span class="hlt">models</span> were assessed in terms of their predictive ability, data requirements, number of optimised parameters, ability to simulate diverse chemical conditions and transferability to other substrates. A particular aim was to compare the generalised composite (GC) and component additivity (CA) approaches for <span class="hlt">modelling</span> sorption by complex substrates. Both types of SC <span class="hlt">models</span> showed a promising capability to simulate sorption data obtained across a range of chemical conditions. However, the <span class="hlt">models</span> incorporated a wide variety of assumptions, particularly in terms of input parameters such as site densities and surface site types. Furthermore, the methods used to extrapolate the <span class="hlt">model</span> simulations to different <span class="hlt">weathered</span> rock samples collected at the same field site tended to be unsatisfactory. The outcome of this <span class="hlt">modelling</span> exercise provides an overview of the present status of adsorption <span class="hlt">modelling</span> in the context of radionuclide migration as practised in a number of countries worldwide.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2012Icar..221...12K','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2012Icar..221...12K"><span>Space <span class="hlt">weathering</span> and the color indexes of minor bodies in the outer Solar <span class="hlt">System</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Kaňuchová, Zuzana; Brunetto, Rosario; Melita, Mario; Strazzulla, Giovanni</p> <p>2012-09-01</p> <p>The surfaces of small bodies in the outer Solar <span class="hlt">System</span> are rich in organic compounds and carbonaceous refractories mixed with ices and silicates. As made clear by dedicated laboratory experiments space <span class="hlt">weathering</span> (e.g. energetic ion bombardment) can produce red colored materials starting from bright and spectrally flat ices. In a classical scenario, the space <span class="hlt">weathering</span> processes “nurture” alter the small bodies surface spectra but are in competition with resurfacing agents that restore the original colors, and the result of these competing processes continuously modifying the surfaces is supposed to be responsible for the observed spectral variety of those small bodies. However an alternative point of view is that the different colors are due to “nature” i.e. to the different primordial composition of different objects. In this paper we present a <span class="hlt">model</span>, based on laboratory results, that gives an original contribution to the “nature” vs. “nurture” debate by addressing the case of surfaces showing different fractions of rejuvenated vs. space <span class="hlt">weathered</span> surface, and calculating the corresponding color variations. We will show how a combination of increasing dose coupled to different resurfacing can reproduce the whole range of observations of small outer Solar <span class="hlt">System</span> bodies. Here we demonstrate, for the first time that objects having a fully <span class="hlt">weathered</span> material turn back in the color-color diagrams. At the same time, object with the different ratio of pristine and <span class="hlt">weathered</span> surface areas lay on specific lines in color-color diagrams, if exposed to the same amount of irradiation.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/20160005686','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/20160005686"><span>Overview of NASA MSFC and UAH Space <span class="hlt">Weather</span> <span class="hlt">Modeling</span> and Data Efforts</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Parker, Linda Neergaard</p> <p>2016-01-01</p> <p>Marshall Space Flight Center, along with its industry and academia neighbors, has a long history of space environment <span class="hlt">model</span> development and testing. Space <span class="hlt">weather</span> efforts include research, testing, <span class="hlt">model</span> development, environment definition, anomaly investigation, and operational support. This presentation will highlight a few of the current space <span class="hlt">weather</span> activities being performed at Marshall and through collaborative efforts with University of Alabama in Huntsville scientists.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2018NHESS..18.1617P','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2018NHESS..18.1617P"><span>A statistical <span class="hlt">model</span> to estimate the local vulnerability to severe <span class="hlt">weather</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Pardowitz, Tobias</p> <p>2018-06-01</p> <p>We present a spatial analysis of <span class="hlt">weather</span>-related fire brigade operations in Berlin. By comparing operation occurrences to insured losses for a set of severe <span class="hlt">weather</span> events we demonstrate the representativeness and usefulness of such data in the analysis of <span class="hlt">weather</span> impacts on local scales. We investigate factors influencing the local rate of operation occurrence. While depending on multiple factors - which are often not available - we focus on publicly available quantities. These include topographic features, land use information based on satellite data and information on urban structure based on data from the OpenStreetMap project. After identifying suitable predictors such as housing coverage or local density of the road network we set up a statistical <span class="hlt">model</span> to be able to predict the average occurrence frequency of local fire brigade operations. Such <span class="hlt">model</span> can be used to determine potential <q>hotspots</q> for <span class="hlt">weather</span> impacts even in areas or cities where no systematic records are available and can thus serve as a basis for a broad range of tools or applications in emergency management and planning.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2015AGUFMSH43C..02J','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2015AGUFMSH43C..02J"><span><span class="hlt">Modeling</span> AWSoM CMEs with EEGGL: A New Approach for Space <span class="hlt">Weather</span> Forecasting</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Jin, M.; Manchester, W.; van der Holst, B.; Sokolov, I.; Toth, G.; Vourlidas, A.; de Koning, C. A.; Gombosi, T. I.</p> <p>2015-12-01</p> <p>The major source of destructive space <span class="hlt">weather</span> is coronal mass ejections (CMEs). However, our understanding of CMEs and their propagation in the heliosphere is limited by the insufficient observations. Therefore, the development of first-principals numerical <span class="hlt">models</span> plays a vital role in both theoretical investigation and providing space <span class="hlt">weather</span> forecasts. Here, we present results of the simulation of CME propagation from the Sun to 1AU by combining the analytical Gibson & Low (GL) flux rope <span class="hlt">model</span> with the state-of-art solar wind <span class="hlt">model</span> AWSoM. We also provide an approach for transferring this research <span class="hlt">model</span> to a space <span class="hlt">weather</span> forecasting tool by demonstrating how the free parameters of the GL flux rope can be prescribed based on remote observations via the new Eruptive Event Generator by Gibson-Low (EEGGL) toolkit. This capability allows us to predict the long-term evolution of the CME in interplanetary space. We perform proof-of-concept case studies to show the capability of the <span class="hlt">model</span> to capture physical processes that determine CME evolution while also reproducing many observed features both in the corona and at 1 AU. We discuss the potential and limitations of this <span class="hlt">model</span> as a future space <span class="hlt">weather</span> forecasting tool.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/20120016447','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/20120016447"><span>Evaluating the Impacts of NASA/SPoRT Daily Greenness Vegetation Fraction on Land Surface <span class="hlt">Model</span> and Numerical <span class="hlt">Weather</span> Forecasts</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Bell, Jordan R.; Case, Jonathan L.; Molthan, Andrew L.</p> <p>2011-01-01</p> <p>The NASA Short-term Prediction Research and Transition (SPoRT) Center develops new products and techniques that can be used in operational meteorology. The majority of these products are derived from NASA polar-orbiting satellite imagery from the Earth Observing <span class="hlt">System</span> (EOS) platforms. One such product is a Greenness Vegetation Fraction (GVF) dataset, which is produced from Moderate Resolution Imaging Spectroradiometer (MODIS) data aboard the NASA EOS Aqua and Terra satellites. NASA SPoRT began generating daily real-time GVF composites at 1-km resolution over the Continental United States (CONUS) on 1 June 2010. The purpose of this study is to compare the National Centers for Environmental Prediction (NCEP) climatology GVF product (currently used in operational <span class="hlt">weather</span> <span class="hlt">models</span>) to the SPoRT-MODIS GVF during June to October 2010. The NASA Land Information <span class="hlt">System</span> (LIS) was employed to study the impacts of the new SPoRT-MODIS GVF dataset on land surface <span class="hlt">models</span> apart from a full numerical <span class="hlt">weather</span> prediction (NWP) <span class="hlt">model</span>. For the 2010 warm season, the SPoRT GVF in the western portion of the CONUS was generally higher than the NCEP climatology. The eastern CONUS GVF had variations both above and below the climatology during the period of study. These variations in GVF led to direct impacts on the rates of heating and evaporation from the land surface. The second phase of the project is to examine the impacts of the SPoRT GVF dataset on NWP using the <span class="hlt">Weather</span> Research and Forecasting (WRF) <span class="hlt">model</span>. Two separate WRF <span class="hlt">model</span> simulations were made for individual severe <span class="hlt">weather</span> case days using the NCEP GVF (control) and SPoRT GVF (experimental), with all other <span class="hlt">model</span> parameters remaining the same. Based on the sensitivity results in these case studies, regions with higher GVF in the SPoRT <span class="hlt">model</span> runs had higher evapotranspiration and lower direct surface heating, which typically resulted in lower (higher) predicted 2-m temperatures (2-m dewpoint temperatures). The opposite was true</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://rosap.ntl.bts.gov/view/dot/3799','DOTNTL'); return false;" href="https://rosap.ntl.bts.gov/view/dot/3799"><span>Project report : road <span class="hlt">weather</span> information <span class="hlt">system</span> phase I</span></a></p> <p><a target="_blank" href="http://ntlsearch.bts.gov/tris/index.do">DOT National Transportation Integrated Search</a></p> <p></p> <p>2004-11-01</p> <p>The Alaska Department of Transportation & Public Facilities (ADOT&PF) initiated the first eight environmental sensor stations (ESS) in the Anchorage area, called the Road <span class="hlt">Weather</span> Information <span class="hlt">System</span> (RWIS) Phase I. The ESS are used to detect road weat...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/29219105','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/29219105"><span>Impact of extreme <span class="hlt">weather</span> events and climate change for health and social care <span class="hlt">systems</span>.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Curtis, Sarah; Fair, Alistair; Wistow, Jonathan; Val, Dimitri V; Oven, Katie</p> <p>2017-12-05</p> <p>This review, commissioned by the Research Councils UK Living With Environmental Change (LWEC) programme, concerns research on the impacts on health and social care <span class="hlt">systems</span> in the United Kingdom of extreme <span class="hlt">weather</span> events, under conditions of climate change. Extreme <span class="hlt">weather</span> events considered include heatwaves, coldwaves and flooding. Using a structured review method, we consider evidence regarding the currently observed and anticipated future impacts of extreme <span class="hlt">weather</span> on health and social care <span class="hlt">systems</span> and the potential of preparedness and adaptation measures that may enhance resilience. We highlight a number of general conclusions which are likely to be of international relevance, although the review focussed on the situation in the UK. Extreme <span class="hlt">weather</span> events impact the operation of health services through the effects on built, social and institutional infrastructures which support health and health care, and also because of changes in service demand as extreme <span class="hlt">weather</span> impacts on human health. Strategic planning for extreme <span class="hlt">weather</span> and impacts on the care <span class="hlt">system</span> should be sensitive to within country variations. Adaptation will require changes to built infrastructure <span class="hlt">systems</span> (including transport and utilities as well as individual care facilities) and also to institutional and social infrastructure supporting the health care <span class="hlt">system</span>. Care sector organisations, communities and individuals need to adapt their practices to improve resilience of health and health care to extreme <span class="hlt">weather</span>. Preparedness and emergency response strategies call for action extending beyond the emergency response services, to include health and social care providers more generally.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2015AGUFM.H53A1649C','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2015AGUFM.H53A1649C"><span>Hydrologic <span class="hlt">Modeling</span> at the National Water Center: Operational Implementation of the WRF-Hydro <span class="hlt">Model</span> to support National <span class="hlt">Weather</span> Service Hydrology</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Cosgrove, B.; Gochis, D.; Clark, E. P.; Cui, Z.; Dugger, A. L.; Fall, G. M.; Feng, X.; Fresch, M. A.; Gourley, J. J.; Khan, S.; Kitzmiller, D.; Lee, H. S.; Liu, Y.; McCreight, J. L.; Newman, A. J.; Oubeidillah, A.; Pan, L.; Pham, C.; Salas, F.; Sampson, K. M.; Smith, M.; Sood, G.; Wood, A.; Yates, D. N.; Yu, W.; Zhang, Y.</p> <p>2015-12-01</p> <p>The National <span class="hlt">Weather</span> Service (NWS) National Water Center(NWC) is collaborating with the NWS National Centers for Environmental Prediction (NCEP) and the National Center for Atmospheric Research (NCAR) to implement a first-of-its-kind operational instance of the <span class="hlt">Weather</span> Research and Forecasting (WRF)-Hydro <span class="hlt">model</span> over the Continental United States (CONUS) and contributing drainage areas on the NWS <span class="hlt">Weather</span> and Climate Operational Supercomputing <span class="hlt">System</span> (WCOSS) supercomputer. The <span class="hlt">system</span> will provide seamless, high-resolution, continuously cycling forecasts of streamflow and other hydrologic outputs of value from both deterministic- and ensemble-type runs. WRF-Hydro will form the core of the NWC national water <span class="hlt">modeling</span> strategy, supporting NWS hydrologic forecast operations along with emergency response and water management efforts of partner agencies. Input and output from the <span class="hlt">system</span> will be comprehensively verified via the NWC Water Resource Evaluation Service. Hydrologic events occur on a wide range of temporal scales, from fast acting flash floods, to long-term flow events impacting water supply. In order to capture this range of events, the initial operational WRF-Hydro configuration will feature 1) hourly analysis runs, 2) short-and medium-range deterministic forecasts out to two day and ten day horizons and 3) long-range ensemble forecasts out to 30 days. All three of these configurations are underpinned by a 1km execution of the NoahMP land surface <span class="hlt">model</span>, with channel routing taking place on 2.67 million NHDPlusV2 catchments covering the CONUS and contributing areas. Additionally, the short- and medium-range forecasts runs will feature surface and sub-surface routing on a 250m grid, while the hourly analyses will feature this same 250m routing in addition to nudging-based assimilation of US Geological Survey (USGS) streamflow observations. A limited number of major reservoirs will be configured within the <span class="hlt">model</span> to begin to represent the first-order impacts of</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/26188633','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/26188633"><span>Time series regression <span class="hlt">model</span> for infectious disease and <span class="hlt">weather</span>.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Imai, Chisato; Armstrong, Ben; Chalabi, Zaid; Mangtani, Punam; Hashizume, Masahiro</p> <p>2015-10-01</p> <p>Time series regression has been developed and long used to evaluate the short-term associations of air pollution and <span class="hlt">weather</span> with mortality or morbidity of non-infectious diseases. The application of the regression approaches from this tradition to infectious diseases, however, is less well explored and raises some new issues. We discuss and present potential solutions for five issues often arising in such analyses: changes in immune population, strong autocorrelations, a wide range of plausible lag structures and association patterns, seasonality adjustments, and large overdispersion. The potential approaches are illustrated with datasets of cholera cases and rainfall from Bangladesh and influenza and temperature in Tokyo. Though this article focuses on the application of the traditional time series regression to infectious diseases and <span class="hlt">weather</span> factors, we also briefly introduce alternative approaches, including mathematical <span class="hlt">modeling</span>, wavelet analysis, and autoregressive integrated moving average (ARIMA) <span class="hlt">models</span>. Modifications proposed to standard time series regression practice include using sums of past cases as proxies for the immune population, and using the logarithm of lagged disease counts to control autocorrelation due to true contagion, both of which are motivated from "susceptible-infectious-recovered" (SIR) <span class="hlt">models</span>. The complexity of lag structures and association patterns can often be informed by biological mechanisms and explored by using distributed lag non-linear <span class="hlt">models</span>. For overdispersed <span class="hlt">models</span>, alternative distribution <span class="hlt">models</span> such as quasi-Poisson and negative binomial should be considered. Time series regression can be used to investigate dependence of infectious diseases on <span class="hlt">weather</span>, but may need modifying to allow for features specific to this context. Copyright © 2015 The Authors. Published by Elsevier Inc. All rights reserved.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/20130010086','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/20130010086"><span>Creating a Realistic <span class="hlt">Weather</span> Environment for Motion-Based Piloted Flight Simulation</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Daniels, Taumi S.; Schaffner, Philip R.; Evans, Emory T.; Neece, Robert T.; Young, Steve D.</p> <p>2012-01-01</p> <p>A flight simulation environment is being enhanced to facilitate experiments that evaluate research prototypes of advanced onboard <span class="hlt">weather</span> radar, hazard/integrity monitoring (HIM), and integrated alerting and notification (IAN) concepts in adverse <span class="hlt">weather</span> conditions. The simulation environment uses <span class="hlt">weather</span> data based on real <span class="hlt">weather</span> events to support operational scenarios in a terminal area. A simulated atmospheric environment was realized by using numerical <span class="hlt">weather</span> data sets. These were produced from the High-Resolution Rapid Refresh (HRRR) <span class="hlt">model</span> hosted and run by the National Oceanic and Atmospheric Administration (NOAA). To align with the planned flight simulation experiment requirements, several HRRR data sets were acquired courtesy of NOAA. These data sets coincided with severe <span class="hlt">weather</span> events at the Memphis International Airport (MEM) in Memphis, TN. In addition, representative flight tracks for approaches and departures at MEM were generated and used to develop and test simulations of (1) what onboard sensors such as the <span class="hlt">weather</span> radar would observe; (2) what datalinks of <span class="hlt">weather</span> information would provide; and (3) what atmospheric conditions the aircraft would experience (e.g. turbulence, winds, and icing). The simulation includes a <span class="hlt">weather</span> radar display that provides <span class="hlt">weather</span> and turbulence modes, derived from the <span class="hlt">modeled</span> <span class="hlt">weather</span> along the flight track. The radar capabilities and the pilots controls simulate current-generation commercial <span class="hlt">weather</span> radar <span class="hlt">systems</span>. Appropriate data-linked <span class="hlt">weather</span> advisories (e.g., SIGMET) were derived from the HRRR <span class="hlt">weather</span> <span class="hlt">models</span> and provided to the pilot consistent with NextGen concepts of use for Aeronautical Information Service (AIS) and Meteorological (MET) data link products. The net result of this simulation development was the creation of an environment that supports investigations of new flight deck information <span class="hlt">systems</span>, methods for incorporation of better <span class="hlt">weather</span> information, and pilot interface and operational improvements</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017AtmEn.170...33S','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017AtmEn.170...33S"><span>Impact of bacterial ice nucleating particles on <span class="hlt">weather</span> predicted by a numerical <span class="hlt">weather</span> prediction <span class="hlt">model</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Sahyoun, Maher; Korsholm, Ulrik S.; Sørensen, Jens H.; Šantl-Temkiv, Tina; Finster, Kai; Gosewinkel, Ulrich; Nielsen, Niels W.</p> <p>2017-12-01</p> <p>Bacterial ice-nucleating particles (INP) have the ability to facilitate ice nucleation from super-cooled cloud droplets at temperatures just below the melting point. Bacterial INP have been detected in cloud water, precipitation, and dry air, hence they may have an impact on <span class="hlt">weather</span> and climate. In <span class="hlt">modeling</span> studies, the potential impact of bacteria on ice nucleation and precipitation formation on global scale is still uncertain due to their small concentration compared to other types of INP, i.e. dust. Those earlier studies did not account for the yet undetected high concentration of nanoscale fragments of bacterial INP, which may be found free or attached to soil dust in the atmosphere. In this study, we investigate the sensitivity of <span class="hlt">modeled</span> cloud ice, precipitation and global solar radiation in different <span class="hlt">weather</span> scenarios to changes in the fraction of cloud droplets containing bacterial INP, regardless of their size. For this purpose, a module that calculates the probability of ice nucleation as a function of ice nucleation rate and bacterial INP fraction was developed and implemented in a numerical <span class="hlt">weather</span> prediction <span class="hlt">model</span>. The threshold value for the fraction of cloud droplets containing bacterial INP needed to produce a 1% increase in cloud ice was determined at 10-5 to 10-4. We also found that increasing this fraction causes a perturbation in the forecast, leading to significant differences in cloud ice and smaller differences in convective and total precipitation and in net solar radiation reaching the surface. These effects were most pronounced in local convective events. Our results show that bacterial INP can be considered as a trigger factor for precipitation, but not an enhancement factor.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2015AGUFMOS23E..02F','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2015AGUFMOS23E..02F"><span>Assessing the Role of Seafloor <span class="hlt">Weathering</span> in Global Geochemical Cycling</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Farahat, N. X.; Abbot, D. S.; Archer, D. E.</p> <p>2015-12-01</p> <p>Low-temperature alteration of the basaltic upper oceanic crust, known as seafloor <span class="hlt">weathering</span>, has been proposed as a mechanism for long-term climate regulation similar to the continental climate-<span class="hlt">weathering</span> negative feedback. Despite this potentially far-reaching impact of seafloor <span class="hlt">weathering</span> on habitable planet evolution, existing <span class="hlt">modeling</span> frameworks do not include the full scope of alteration reactions or recent findings of convective flow dynamics. We present a coupled fluid dynamic and geochemical numerical <span class="hlt">model</span> of low-temperature, off-axis hydrothermal activity. This <span class="hlt">model</span> is designed to explore the the seafloor <span class="hlt">weathering</span> flux of carbon to the oceanic crust and its responsiveness to climate fluctuations. The <span class="hlt">model</span>'s ability to reproduce the seafloor <span class="hlt">weathering</span> environment is evaluated by constructing numerical simulations for comparison with two low-temperature hydrothermal <span class="hlt">systems</span>: A transect east of the Juan de Fuca Ridge and the southern Costa Rica Rift flank. We explore the sensitivity of carbon uptake by seafloor <span class="hlt">weathering</span> on climate and geology by varying deep ocean temperature, seawater dissolved inorganic carbon, continental <span class="hlt">weathering</span> inputs, and basaltic host rock in a suite of numerical experiments.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2013OAP....26..300S','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2013OAP....26..300S"><span>Space <span class="hlt">Weather</span> and the State of Cardiovascular <span class="hlt">System</span> of a Healthy Human Being</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Samsonov, S. N.; Manykina, V. I.; Krymsky, G. F.; Petrova, P. G.; Palshina, A. M.; Vishnevsky, V. V.</p> <p></p> <p>The term "space <span class="hlt">weather</span>" characterizes a state of the near-Earth environmental space. An organism of human being represents an open <span class="hlt">system</span> so the change of conditions in the environment including the near-Earth environmental space influences the health state of a human being.In recent years many works devoted to the effect of space <span class="hlt">weather</span> on the life on the Earth, and the degree of such effect has been represented from a zero-order up to apocalypse. To reveal a real effect of space <span class="hlt">weather</span> on the health of human being the international Russian- Ukrainian experiment "Geliomed" is carried out since 2005 (http://geliomed.immsp.kiev.ua) [Vishnevsky et al., 2009]. The analysis of observational set of data has allowed to show a synchronism and globality of such effect (simultaneous manifestation of space <span class="hlt">weather</span> parameters in a state of cardiovascular <span class="hlt">system</span> of volunteer groups removed from each other at a distance over 6000 km). The response of volunteer' cardiovascular <span class="hlt">system</span> to the changes of space <span class="hlt">weather</span> parameters were observed even at insignificant values of the Earth's geomagnetic field. But even at very considerable disturbances of space <span class="hlt">weather</span> parameters a human being healthy did not feel painful symptoms though measurements of objective physiological indices showed their changes.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2007PhDT.......198H','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2007PhDT.......198H"><span>Explicit simulation of ice particle habits in a Numerical <span class="hlt">Weather</span> Prediction <span class="hlt">Model</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Hashino, Tempei</p> <p>2007-05-01</p> <p>This study developed a scheme for explicit simulation of ice particle habits in Numerical <span class="hlt">Weather</span> Prediction (NWP) <span class="hlt">Models</span>. The scheme is called Spectral Ice Habit Prediction <span class="hlt">System</span> (SHIPS), and the goal is to retain growth history of ice particles in the Eulerian dynamics framework. It diagnoses characteristics of ice particles based on a series of particle property variables (PPVs) that reflect history of microphysieal processes and the transport between mass bins and air parcels in space. Therefore, categorization of ice particles typically used in bulk microphysical parameterization and traditional bin <span class="hlt">models</span> is not necessary, so that errors that stem from the categorization can be avoided. SHIPS predicts polycrystals as well as hexagonal monocrystals based on empirically derived habit frequency and growth rate, and simulates the habit-dependent aggregation and riming processes by use of the stochastic collection equation with predicted PPVs. Idealized two dimensional simulations were performed with SHIPS in a NWP <span class="hlt">model</span>. The predicted spatial distribution of ice particle habits and types, and evolution of particle size distributions showed good quantitative agreement with observation This comprehensive <span class="hlt">model</span> of ice particle properties, distributions, and evolution in clouds can be used to better understand problems facing wide range of research disciplines, including microphysics processes, radiative transfer in a cloudy atmosphere, data assimilation, and <span class="hlt">weather</span> modification.</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/2060/20140002291','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/20140002291"><span>GPS Estimates of Integrated Precipitable Water Aid <span class="hlt">Weather</span> Forecasters</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Moore, Angelyn W.; Gutman, Seth I.; Holub, Kirk; Bock, Yehuda; Danielson, David; Laber, Jayme; Small, Ivory</p> <p>2013-01-01</p> <p>Global Positioning <span class="hlt">System</span> (GPS) meteorology provides enhanced density, low-latency (30-min resolution), integrated precipitable water (IPW) estimates to NOAA NWS (National Oceanic and Atmospheric Adminis tration Nat ional <span class="hlt">Weather</span> Service) <span class="hlt">Weather</span> Forecast Offices (WFOs) to provide improved <span class="hlt">model</span> and satellite data verification capability and more accurate forecasts of extreme <span class="hlt">weather</span> such as flooding. An early activity of this project was to increase the number of stations contributing to the NOAA Earth <span class="hlt">System</span> Research Laboratory (ESRL) GPS meteorology observing network in Southern California by about 27 stations. Following this, the Los Angeles/Oxnard and San Diego WFOs began using the enhanced GPS-based IPW measurements provided by ESRL in the 2012 and 2013 monsoon seasons. Forecasters found GPS IPW to be an effective tool in evaluating <span class="hlt">model</span> performance, and in monitoring monsoon development between <span class="hlt">weather</span> <span class="hlt">model</span> runs for improved flood forecasting. GPS stations are multi-purpose, and routine processing for position solutions also yields estimates of tropospheric zenith delays, which can be converted into mm-accuracy PWV (precipitable water vapor) using in situ pressure and temperature measurements, the basis for GPS meteorology. NOAA ESRL has implemented this concept with a nationwide distribution of more than 300 "GPSMet" stations providing IPW estimates at sub-hourly resolution currently used in operational <span class="hlt">weather</span> <span class="hlt">models</span> in the U.S.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/20120003374','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/20120003374"><span><span class="hlt">Weather</span> Research and Forecasting <span class="hlt">Model</span> Sensitivity Comparisons for Warm Season Convective Initiation</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Watson, Leela R.</p> <p>2007-01-01</p> <p>This report describes the work done by the Applied Meteorology Unit (AMU) in assessing the success of different <span class="hlt">model</span> configurations in predicting warm season convection over East-Central Florida. The <span class="hlt">Weather</span> Research and Forecasting Environmental <span class="hlt">Modeling</span> <span class="hlt">System</span> (WRF EMS) software allows users to choose among two dynamical cores - the Advanced Research WRF (ARW) and the Non-hydrostatic Mesoscale <span class="hlt">Model</span> (NMM). There are also data assimilation analysis packages available for the initialization of the WRF <span class="hlt">model</span> - the Local Analysis and Prediction <span class="hlt">System</span> (LAPS) and the Advanced Regional Prediction <span class="hlt">System</span> (ARPS) Data Analysis <span class="hlt">System</span> (ADAS). Besides <span class="hlt">model</span> core and initialization options, the WRF <span class="hlt">model</span> can be run with one- or two-way nesting. Having a series of initialization options and WRF cores, as well as many options within each core, creates challenges for local forecasters, such as determining which configuration options are best to address specific forecast concerns. This project assessed three different <span class="hlt">model</span> intializations available to determine which configuration best predicts warm season convective initiation in East-Central Florida. The project also examined the use of one- and two-way nesting in predicting warm season convection.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/20150002983','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/20150002983"><span>Don Quixote Pond: A Small Scale <span class="hlt">Model</span> of <span class="hlt">Weathering</span> and Salt Accumulation</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Englert, P.; Bishop, J. L.; Patel, S. N.; Gibson, E. K.; Koeberl, C.</p> <p>2015-01-01</p> <p>The formation of Don Quixote Pond in the North Fork of Wright Valley, Antarctica, is a <span class="hlt">model</span> for unique terrestrial calcium, chlorine, and sulfate <span class="hlt">weathering</span>, accumulation, and distribution processes. The formation of Don Quixote Pond by simple shallow and deep groundwater contrasts more complex <span class="hlt">models</span> for Don Juan Pond in the South Fork of Wright Valley. Our study intends to understand the formation of Don Quixote Pond as unique terrestrial processes and as a <span class="hlt">model</span> for Ca, C1, and S <span class="hlt">weathering</span> and distribution on Mars.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017EGUGA..1910859P','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017EGUGA..1910859P"><span>Development of GNSS PWV information management <span class="hlt">system</span> for very short-term <span class="hlt">weather</span> forecast in the Korean Peninsula</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Park, Han-Earl; Yoon, Ha Su; Yoo, Sung-Moon; Cho, Jungho</p> <p>2017-04-01</p> <p>Over the past decade, Global Navigation Satellite <span class="hlt">System</span> (GNSS) was in the spotlight as a meteorological research tool. The Korea Astronomy and Space Science Institute (KASI) developed a GNSS precipitable water vapor (PWV) information management <span class="hlt">system</span> to apply PWV to practical applications, such as very short-term <span class="hlt">weather</span> forecast. The <span class="hlt">system</span> consists of a DPR, DRS, and TEV, which are divided functionally. The DPR processes GNSS data using the Bernese GNSS software and then retrieves PWV from zenith total delay (ZTD) with the optimized mean temperature equation for the Korean Peninsula. The DRS collects data from eighty permanent GNSS stations in the southern part of the Korean Peninsula and provides the PWV retrieved from GNSS data to a user. The TEV is in charge of redundancy of the DPR. The whole process is performed in near real-time where the delay is ten minutes. The validity of the GNSS PWV was proved by means of a comparison with radiosonde data. In the experiment of numerical <span class="hlt">weather</span> prediction <span class="hlt">model</span>, the GNSS PWV was utilized as the initial value of the <span class="hlt">Weather</span> Research & Forecasting (WRF) <span class="hlt">model</span> for heavy rainfall event. As a result, we found that the forecasting capability of the WRF is improved by data assimilation of GNSS PWV.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/20150020518','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/20150020518"><span>Method and <span class="hlt">System</span> for Dynamic Automated Corrections to <span class="hlt">Weather</span> Avoidance Routes for Aircraft in En Route Airspace</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>McNally, B. David (Inventor); Erzberger, Heinz (Inventor); Sheth, Kapil (Inventor)</p> <p>2015-01-01</p> <p>A dynamic <span class="hlt">weather</span> route <span class="hlt">system</span> automatically analyzes routes for in-flight aircraft flying in convective <span class="hlt">weather</span> regions and attempts to find more time and fuel efficient reroutes around current and predicted <span class="hlt">weather</span> cells. The dynamic <span class="hlt">weather</span> route <span class="hlt">system</span> continuously analyzes all flights and provides reroute advisories that are dynamically updated in real time while the aircraft are in flight. The dynamic <span class="hlt">weather</span> route <span class="hlt">system</span> includes a graphical user interface that allows users to visualize, evaluate, modify if necessary, and implement proposed reroutes.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://www.dtic.mil/docs/citations/ADA589390','DTIC-ST'); return false;" href="http://www.dtic.mil/docs/citations/ADA589390"><span>An Automated <span class="hlt">Weather</span> Research and Forecasting (WRF)-Based Nowcasting <span class="hlt">System</span>: Software Description</span></a></p> <p><a target="_blank" href="http://www.dtic.mil/">DTIC Science & Technology</a></p> <p></p> <p>2013-10-01</p> <p>14. ABSTRACT A Web service /Web interface software package has been engineered to address the need for an automated means to run the <span class="hlt">Weather</span> Research...An Automated <span class="hlt">Weather</span> Research and Forecasting (WRF)- Based Nowcasting <span class="hlt">System</span>: Software Description by Stephen F. Kirby, Brian P. Reen, and...Based Nowcasting <span class="hlt">System</span>: Software Description Stephen F. Kirby, Brian P. Reen, and Robert E. Dumais Jr. Computational and Information Sciences</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2014EGUGA..16.3058C','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2014EGUGA..16.3058C"><span>Training the next generation of scientists in <span class="hlt">Weather</span> Forecasting: new approaches with real <span class="hlt">models</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Carver, Glenn; Váňa, Filip; Siemen, Stephan; Kertesz, Sandor; Keeley, Sarah</p> <p>2014-05-01</p> <p>The European Centre for Medium Range <span class="hlt">Weather</span> Forecasts operationally produce medium range forecasts using what is internationally acknowledged as the world leading global <span class="hlt">weather</span> forecast <span class="hlt">model</span>. Future development of this scientifically advanced <span class="hlt">model</span> relies on a continued availability of experts in the field of meteorological science and with high-level software skills. ECMWF therefore has a vested interest in young scientists and University graduates developing the necessary skills in numerical <span class="hlt">weather</span> prediction including both scientific and technical aspects. The OpenIFS project at ECMWF maintains a portable version of the ECMWF forecast <span class="hlt">model</span> (known as IFS) for use in education and research at Universities, National Meteorological Services and other research and education organisations. OpenIFS <span class="hlt">models</span> can be run on desktop or high performance computers to produce <span class="hlt">weather</span> forecasts in a similar way to the operational forecasts at ECMWF. ECMWF also provide the Metview desktop application, a modern, graphical, and easy to use tool for analysing and visualising forecasts that is routinely used by scientists and forecasters at ECMWF and other institutions. The combination of Metview with the OpenIFS <span class="hlt">models</span> has the potential to deliver classroom-friendly tools allowing students to apply their theoretical knowledge to real-world examples using a world-leading <span class="hlt">weather</span> forecasting <span class="hlt">model</span>. In this paper we will describe how the OpenIFS <span class="hlt">model</span> has been used for teaching. We describe the use of Linux based 'virtual machines' pre-packaged on USB sticks that support a technically easy and safe way of providing 'classroom-on-a-stick' learning environments for advanced training in numerical <span class="hlt">weather</span> prediction. We welcome discussions with interested parties.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://rosap.ntl.bts.gov/view/dot/16091','DOTNTL'); return false;" href="https://rosap.ntl.bts.gov/view/dot/16091"><span>Arizona Road <span class="hlt">Weather</span> Information <span class="hlt">System</span> (RWIS) communications plan</span></a></p> <p><a target="_blank" href="http://ntlsearch.bts.gov/tris/index.do">DOT National Transportation Integrated Search</a></p> <p></p> <p>2003-04-01</p> <p>There have been two implementations of Roadway <span class="hlt">Weather</span> Information <span class="hlt">Systems</span> in Arizona, known as RWIS Phase 0 and Phase 1. Each Phase has met with limited success and has on-going issues that need to be addressed before new RWIS sites are implemented....</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2015EGUGA..1712542D','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2015EGUGA..1712542D"><span>Fire danger assessment using ECMWF <span class="hlt">weather</span> prediction <span class="hlt">system</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Di Giuseppe, Francesca; Pappemberger, Florian; Wetterhall, Fredrik</p> <p>2015-04-01</p> <p><span class="hlt">Weather</span> plays a major role in the birth, growth and death of a wildfire wherever there is availability of combustible vegetation and suitable terrain topography. Prolonged dry periods creates favourable conditions for ignitions, wind can then increase the fire spread, while higher relative humidity, and precipitation (rain or snow) may decrease or extinguish it altogether. The European Forest Fire Information <span class="hlt">System</span> (EFFIS), started in 2011 under the lead of the European Joint Research Centre (JRC) to monitor and forecast fire danger and fire behaviour in Europe. In 2012 a collaboration with the European Centre for Medium range <span class="hlt">Weather</span> Forecast (ECMWF) was established to explore the potential of using state of the art <span class="hlt">weather</span> forecast <span class="hlt">systems</span> as driving forcing for the calculations of fire risk indices. From this collaboration in 2013 the EC-fire <span class="hlt">system</span> was born. It implements the three most commonly used fire danger rating <span class="hlt">systems</span> (NFDRS, FWI and MARK-5) and it is both initialised and forced by gridded atmospheric fields provided either by ECMWF re-analysis or ECMWF ensemble prediction <span class="hlt">systems</span>. For consistency invariant fields (i.e fuel maps, vegetation cover, topogarphy) and real-time <span class="hlt">weather</span> information are all provided on the same grid. Similarly global climatological vegetation stage conditions for each day of the year are provided by remote satellite observations. These climatological static maps substitute the traditional man judgement in an effort to create an automated procedure that can work in places where local observations are not available. The <span class="hlt">system</span> has been in operation for the last year providing an ensemble of daily forecasts for fire indices with lead-times up to 10 days over Europe and Globally. An important part of the <span class="hlt">system</span> is provided by its (re)-analysis dataset obtained by using the (re)-analysis forcings as drivers to calculate the fire risk indices. This is a crucial part of the whole chain since these fields are used to establish the</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2015AGUFMED23A0856C','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2015AGUFMED23A0856C"><span>Community Coordinated <span class="hlt">Modeling</span> Center: A Powerful Resource in Space Science and Space <span class="hlt">Weather</span> Education</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Chulaki, A.; Kuznetsova, M. M.; Rastaetter, L.; MacNeice, P. J.; Shim, J. S.; Pulkkinen, A. A.; Taktakishvili, A.; Mays, M. L.; Mendoza, A. M. M.; Zheng, Y.; Mullinix, R.; Collado-Vega, Y. M.; Maddox, M. M.; Pembroke, A. D.; Wiegand, C.</p> <p>2015-12-01</p> <p>Community Coordinated <span class="hlt">Modeling</span> Center (CCMC) is a NASA affiliated interagency partnership with the primary goal of aiding the transition of modern space science <span class="hlt">models</span> into space <span class="hlt">weather</span> forecasting while supporting space science research. Additionally, over the past ten years it has established itself as a global space science education resource supporting undergraduate and graduate education and research, and spreading space <span class="hlt">weather</span> awareness worldwide. A unique combination of assets, capabilities and close ties to the scientific and educational communities enable this small group to serve as a hub for raising generations of young space scientists and engineers. CCMC resources are publicly available online, providing unprecedented global access to the largest collection of modern space science <span class="hlt">models</span> (developed by the international research community). CCMC has revolutionized the way simulations are utilized in classrooms settings, student projects, and scientific labs and serves hundreds of educators, students and researchers every year. Another major CCMC asset is an expert space <span class="hlt">weather</span> prototyping team primarily serving NASA's interplanetary space <span class="hlt">weather</span> needs. Capitalizing on its unrivaled capabilities and experiences, the team provides in-depth space <span class="hlt">weather</span> training to students and professionals worldwide, and offers an amazing opportunity for undergraduates to engage in real-time space <span class="hlt">weather</span> monitoring, analysis, forecasting and research. In-house development of state-of-the-art space <span class="hlt">weather</span> tools and applications provides exciting opportunities to students majoring in computer science and computer engineering fields to intern with the software engineers at the CCMC while also learning about the space <span class="hlt">weather</span> from the NASA scientists.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2006AGUFMSA53A1349S','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2006AGUFMSA53A1349S"><span>Operational Space <span class="hlt">Weather</span> in USAF Education</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Smithtro, C.; Quigley, S.</p> <p>2006-12-01</p> <p>Most education programs offering space <span class="hlt">weather</span> courses are understandably and traditionally heavily weighted with theoretical space physics that is the basis for most of what is researched and <span class="hlt">modeled</span>. While understanding the theory is a good and necessary grounding for anyone working the field of space <span class="hlt">weather</span>, few military or commercial jobs employ such theory in real-time operations. The operations sites/centers are much more geared toward use of applied theory-resultant <span class="hlt">models</span>, tools and products. To ensure its operations centers personnel, commanders, real-time <span class="hlt">system</span> operators and other customers affected by the space environment are educated on available and soon-to-be operational space <span class="hlt">weather</span> <span class="hlt">models</span> and products, the USAF has developed applicable course/lecture material taught at various institutions to include the Air Force Institute of Technology (AFIT) and the Joint <span class="hlt">Weather</span> Training Complex (335th/TRS/OUA). Less frequent training of operational space <span class="hlt">weather</span> is available via other venues that will be discussed, and associated course material is also being developed for potential use at the National Security Space Institute (NSSI). This presentation provides an overview of the programs, locations, courses and material developed and/or taught by or for USAF personnel dealing with operational space <span class="hlt">weather</span>. It also provides general information on student research project results that may be used in operational support, along with observations regarding logistical and professional benefits of teaching such non-theoretical/non-traditional material.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017AGUFM.A44F..03B','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017AGUFM.A44F..03B"><span>Evaluation of Unmanned Aircraft <span class="hlt">Systems</span> (UAS) for <span class="hlt">Weather</span> and Climate using the Multi-testbed approach</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Baker, B.; Lee, T.; Buban, M.; Dumas, E. J.</p> <p>2017-12-01</p> <p>Evaluation of Unmanned Aircraft <span class="hlt">Systems</span> (UAS) for <span class="hlt">Weather</span> and Climate using the Multi-testbed approachC. Bruce Baker1, Ed Dumas1,2, Temple Lee1,2, Michael Buban1,21NOAA ARL, Atmospheric Turbulence and Diffusion Division, Oak Ridge, TN2Oak Ridge Associated Universities, Oak Ridge, TN The development of a small Unmanned Aerial <span class="hlt">System</span> (sUAS) testbeds that can be used to validate, integrate, calibrate and evaluate new technology and sensors for routine boundary layer research, validation of operational <span class="hlt">weather</span> <span class="hlt">models</span>, improvement of <span class="hlt">model</span> parameterizations, and recording observations within high-impact storms is important for understanding the importance and impact of using sUAS's routinely as a new observing platform. The goal of the multi-testbed approach is to build a robust set of protocols to assess the cost and operational feasibility of unmanned observations for routine applications using various combinations of sUAS aircraft and sensors in different locations and field experiments. All of these observational testbeds serve different community needs, but they also use a diverse suite of methodologies for calibration and evaluation of different sensors and platforms for severe <span class="hlt">weather</span> and boundary layer research. The primary focus will be to evaluate meteorological sensor payloads to measure thermodynamic parameters and define surface characteristics with visible, IR, and multi-spectral cameras. This evaluation will lead to recommendations for sensor payloads for VTOL and fixed-wing sUAS.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://eric.ed.gov/?q=meteorology&pg=6&id=EJ301864','ERIC'); return false;" href="https://eric.ed.gov/?q=meteorology&pg=6&id=EJ301864"><span><span class="hlt">Weather</span> or Not To Teach Junior High Meteorology.</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>Knorr, Thomas P.</p> <p>1984-01-01</p> <p>Presents a technique for teaching meteorology allowing students to observe and analyze consecutive <span class="hlt">weather</span> maps and relate local conditions; a <span class="hlt">model</span> illustrating the three-dimensional nature of the atmosphere is employed. Instructional methods based on studies of daily <span class="hlt">weather</span> maps to trace <span class="hlt">systems</span> sweeping across the United States are discussed.…</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://ntrs.nasa.gov/search.jsp?R=20040034245&hterms=time+series+forecasting&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D10%26Ntt%3Dtime%2Bseries%2Bforecasting','NASA-TRS'); return false;" href="https://ntrs.nasa.gov/search.jsp?R=20040034245&hterms=time+series+forecasting&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D10%26Ntt%3Dtime%2Bseries%2Bforecasting"><span>Use of EOS Data in AWIPS for <span class="hlt">Weather</span> Forecasting</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Jedlovec, Gary J.; Haines, Stephanie L.; Suggs, Ron J.; Bradshaw, Tom; Darden, Chris; Burks, Jason</p> <p>2003-01-01</p> <p>Operational <span class="hlt">weather</span> forecasting relies heavily on real time data and <span class="hlt">modeling</span> products for forecast preparation and dissemination of significant <span class="hlt">weather</span> information to the public. The synthesis of this information (observations and <span class="hlt">model</span> products) by the meteorologist is facilitated by a decision support <span class="hlt">system</span> to display and integrate the information in a useful fashion. For the NWS this <span class="hlt">system</span> is called Advanced <span class="hlt">Weather</span> Interactive Processing <span class="hlt">System</span> (AWIPS). Over the last few years NASA has launched a series of new Earth Observation Satellites (EOS) for climate monitoring that include several instruments that provide high-resolution measurements of atmospheric and surface features important for <span class="hlt">weather</span> forecasting and analysis. The key to the utilization of these unique new measurements by the NWS is the real time integration of the EOS data into the AWIPS <span class="hlt">system</span>. This is currently being done in the Huntsville and Birmingham NWS Forecast Offices under the NASA Short-term Prediction Research and Transition (SPORT) Program. This paper describes the use of near real time MODIS and AIRS data in AWIPS to improve the detection of clouds, moisture variations, atmospheric stability, and thermal signatures that can lead to significant <span class="hlt">weather</span> development. The paper and the conference presentation will focus on several examples where MODIS and AIRS data have made a positive impact on forecast accuracy. The results of an assessment of the utility of these products for <span class="hlt">weather</span> forecast improvement made at the Huntsville NWS Forecast Office will be presented.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2007JGRD..112.3102D','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2007JGRD..112.3102D"><span>Initializing numerical <span class="hlt">weather</span> prediction <span class="hlt">models</span> with satellite-derived surface soil moisture: Data assimilation experiments with ECMWF's Integrated Forecast <span class="hlt">System</span> and the TMI soil moisture 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>Drusch, M.</p> <p>2007-02-01</p> <p>Satellite-derived surface soil moisture data sets are readily available and have been used successfully in hydrological applications. In many operational numerical <span class="hlt">weather</span> prediction <span class="hlt">systems</span> the initial soil moisture conditions are analyzed from the <span class="hlt">modeled</span> background and 2 m temperature and relative humidity. This approach has proven its efficiency to improve surface latent and sensible heat fluxes and consequently the forecast on large geographical domains. However, since soil moisture is not always related to screen level variables, <span class="hlt">model</span> errors and uncertainties in the forcing data can accumulate in root zone soil moisture. Remotely sensed surface soil moisture is directly linked to the <span class="hlt">model</span>'s uppermost soil layer and therefore is a stronger constraint for the soil moisture analysis. For this study, three data assimilation experiments with the Integrated Forecast <span class="hlt">System</span> (IFS) of the European Centre for Medium-Range <span class="hlt">Weather</span> Forecasts (ECMWF) have been performed for the 2-month period of June and July 2002: a control run based on the operational soil moisture analysis, an open loop run with freely evolving soil moisture, and an experimental run incorporating TMI (TRMM Microwave Imager) derived soil moisture over the southern United States. In this experimental run the satellite-derived soil moisture product is introduced through a nudging scheme using 6-hourly increments. Apart from the soil moisture analysis, the <span class="hlt">system</span> setup reflects the operational forecast configuration including the atmospheric 4D-Var analysis. Soil moisture analyzed in the nudging experiment is the most accurate estimate when compared against in situ observations from the Oklahoma Mesonet. The corresponding forecast for 2 m temperature and relative humidity is almost as accurate as in the control experiment. Furthermore, it is shown that the soil moisture analysis influences local <span class="hlt">weather</span> parameters including the planetary boundary layer height and cloud coverage.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/20120003999','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/20120003999"><span>Effects of Real-Time NASA Vegetation Data on <span class="hlt">Model</span> Forecasts of Severe <span class="hlt">Weather</span></span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Case, Jonathan L.; Bell, Jordan R.; LaFontaine, Frank J.; Peters-Lidard, Christa D.</p> <p>2012-01-01</p> <p>The NASA Short-term Prediction Research and Transition (SPoRT) Center has developed a Greenness Vegetation Fraction (GVF) dataset, which is updated daily using swaths of Normalized Difference Vegetation Index data from the Moderate Resolution Imaging Spectroradiometer (MODIS) data aboard the NASA-EOS Aqua and Terra satellites. NASA SPoRT started generating daily real-time GVF composites at 1-km resolution over the Continental United States beginning 1 June 2010. A companion poster presentation (Bell et al.) primarily focuses on impact results in an offline configuration of the Noah land surface <span class="hlt">model</span> (LSM) for the 2010 warm season, comparing the SPoRT/MODIS GVF dataset to the current operational monthly climatology GVF available within the National Centers for Environmental Prediction (NCEP) and <span class="hlt">Weather</span> Research and Forecasting (WRF) <span class="hlt">models</span>. This paper/presentation primarily focuses on individual case studies of severe <span class="hlt">weather</span> events to determine the impacts and possible improvements by using the real-time, high-resolution SPoRT-MODIS GVFs in place of the coarser-resolution NCEP climatological GVFs in <span class="hlt">model</span> simulations. The NASA-Unified WRF (NU-WRF) <span class="hlt">modeling</span> <span class="hlt">system</span> is employed to conduct the sensitivity simulations of individual events. The NU-WRF is an integrated <span class="hlt">modeling</span> <span class="hlt">system</span> based on the Advanced Research WRF dynamical core that is designed to represents aerosol, cloud, precipitation, and land processes at satellite-resolved scales in a coupled simulation environment. For this experiment, the coupling between the NASA Land Information <span class="hlt">System</span> (LIS) and the WRF <span class="hlt">model</span> is utilized to measure the impacts of the daily SPoRT/MODIS versus the monthly NCEP climatology GVFs. First, a spin-up run of the LIS is integrated for two years using the Noah LSM to ensure that the land surface fields reach an equilibrium state on the 4-km grid mesh used. Next, the spin-up LIS is run in two separate modes beginning on 1 June 2010, one continuing with the climatology GVFs while the</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/20140008764','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/20140008764"><span>Expansion of the Real-Time SPoRT-Land Information <span class="hlt">System</span> for NOAA/National <span class="hlt">Weather</span> Service Situational Awareness and Local <span class="hlt">Modeling</span> Applications</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Case, Jonathan L; White, Kristopher D.</p> <p>2014-01-01</p> <p>The NASA Short-term Prediction Research and Transition (SPoRT) Center in Huntsville, AL is running a real-time configuration of the Noah land surface <span class="hlt">model</span> (LSM) within the NASA Land Information <span class="hlt">System</span> (LIS) framework (hereafter referred to as the "SPoRT-LIS"). Output from the real-time SPoRT-LIS is used for (1) initializing land surface variables for local <span class="hlt">modeling</span> applications, and (2) displaying in decision support <span class="hlt">systems</span> for situational awareness and drought monitoring at select NOAA/National <span class="hlt">Weather</span> Service (NWS) partner offices. The experimental CONUS run incorporates hourly quantitative precipitation estimation (QPE) from the National Severe Storms Laboratory Multi- Radar Multi-Sensor (MRMS) which will be transitioned into operations at the National Centers for Environmental Prediction (NCEP) in Fall 2014.This paper describes the current and experimental SPoRT-LIS configurations, and documents some of the limitations still remaining through the advent of MRMS precipitation analyses in the SPoRT-LIS land surface <span class="hlt">model</span> (LSM) simulations.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/20080042406','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/20080042406"><span>Anvil Forecast Tool in the Advanced <span class="hlt">Weather</span> Interactive Processing <span class="hlt">System</span>, Phase II</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Barrett, Joe H., III</p> <p>2008-01-01</p> <p>Meteorologists from the 45th <span class="hlt">Weather</span> Squadron (45 WS) and Spaceflight Meteorology Group have identified anvil forecasting as one of their most challenging tasks when predicting the probability of violations of the Lightning Launch Commit Criteria and Space Light Rules. As a result, the Applied Meteorology Unit (AMU) created a graphical overlay tool for the Meteorological Interactive Data Display <span class="hlt">Systems</span> (MIDDS) to indicate the threat of thunderstorm anvil clouds, using either observed or <span class="hlt">model</span> forecast winds as input.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/19760011661','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/19760011661"><span><span class="hlt">Weather</span> and climate</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>Recommendations for using space observations of <span class="hlt">weather</span> and climate to aid in solving earth based problems are given. Special attention was given to: (1) extending useful forecasting capability of space <span class="hlt">systems</span>, (2) reducing social, economic, and human losses caused by <span class="hlt">weather</span>, (3) development of space <span class="hlt">system</span> capability to manage and control air pollutant concentrations, and (4) establish mechanisms for the national examination of deliberate and inadvertent means for modifying <span class="hlt">weather</span> and climate.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017EGUGA..1916128K','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017EGUGA..1916128K"><span>The DACCIWA <span class="hlt">model</span> evaluation project: representation of the meteorology of southern West Africa in state-of-the-art <span class="hlt">weather</span>, seasonal and climate prediction <span class="hlt">models</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Kniffka, Anke; Benedetti, Angela; Knippertz, Peter; Stanelle, Tanja; Brooks, Malcolm; Deetz, Konrad; Maranan, Marlon; Rosenberg, Philip; Pante, Gregor; Allan, Richard; Hill, Peter; Adler, Bianca; Fink, Andreas; Kalthoff, Norbert; Chiu, Christine; Vogel, Bernhard; Field, Paul; Marsham, John</p> <p>2017-04-01</p> <p>DACCIWA (Dynamics-Aerosol-Chemistry-Cloud Interactions in West Africa) is an EU-funded project that aims to determine the influence of anthropogenic and natural emissions on the atmospheric composition, air quality, <span class="hlt">weather</span> and climate over southern West Africa. DACCIWA organised a major international field campaign in June-July 2016 and involves a wide range of <span class="hlt">modelling</span> activities. Here we report about the coordinated <span class="hlt">model</span> evaluation performed in the framework of DACCIWA focusing on meteorological fields. This activity consists of two elements: (a) the quality of numerical <span class="hlt">weather</span> prediction during the field campaign, (b) the ability of seasonal and climate <span class="hlt">models</span> to represent the mean state and its variability. For the first element, the extensive observations from the main field campaign in West Africa in June-July 2016 (ground supersites, radiosondes, aircraft measurements) will be combined with conventional data (synoptic stations, satellites data from various sensors) to evaluate <span class="hlt">models</span> against. The forecasts include operational products from centres such as the ECMWF, UK MetOffice and the German <span class="hlt">Weather</span> Service and runs specifically conducted for the planning and the post-analysis of the field campaign using higher resolutions (e.g., WRF, COSMO). The forecast and the observations are analysed in a concerted way to assess the ability of the <span class="hlt">models</span> to represent the southern West African <span class="hlt">weather</span> <span class="hlt">systems</span> and secondly to provide a comprehensive synoptic overview of the state of the atmosphere. In a second step the process will be extended to long-term <span class="hlt">modelling</span> periods. This includes both seasonal and climate <span class="hlt">models</span>, respectively. In this case, the observational dataset contains long-term satellite observations and station data, some of which were digitised from written records in the framework of DACCIWA. Parameter choice and spatial averaging will build directly on the <span class="hlt">weather</span> forecasting evaluation to allow an assessment of the impact of short-term errors on</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://adsabs.harvard.edu/abs/2009AGUFMIN11E..07K','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2009AGUFMIN11E..07K"><span>A Portable Regional <span class="hlt">Weather</span> and Climate Downscaling <span class="hlt">System</span> Using GEOS-5, LIS-6, WRF, and the NASA Workflow Tool</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Kemp, E. M.; Putman, W. M.; Gurganus, J.; Burns, R. W.; Damon, M. R.; McConaughy, G. R.; Seablom, M. S.; Wojcik, G. S.</p> <p>2009-12-01</p> <p>We present a regional downscaling <span class="hlt">system</span> (RDS) suitable for high-resolution <span class="hlt">weather</span> and climate simulations in multiple supercomputing environments. The RDS is built on the NASA Workflow Tool, a software framework for configuring, running, and managing computer <span class="hlt">models</span> on multiple platforms with a graphical user interface. The Workflow Tool is used to run the NASA Goddard Earth Observing <span class="hlt">System</span> <span class="hlt">Model</span> Version 5 (GEOS-5), a global atmospheric-ocean <span class="hlt">model</span> for <span class="hlt">weather</span> and climate simulations down to 1/4 degree resolution; the NASA Land Information <span class="hlt">System</span> Version 6 (LIS-6), a land surface <span class="hlt">modeling</span> <span class="hlt">system</span> that can simulate soil temperature and moisture profiles; and the <span class="hlt">Weather</span> Research and Forecasting (WRF) community <span class="hlt">model</span>, a limited-area atmospheric <span class="hlt">model</span> for <span class="hlt">weather</span> and climate simulations down to 1-km resolution. The Workflow Tool allows users to customize <span class="hlt">model</span> settings to user needs; saves and organizes simulation experiments; distributes <span class="hlt">model</span> runs across different computer clusters (e.g., the DISCOVER cluster at Goddard Space Flight Center, the Cray CX-1 Desktop Supercomputer, etc.); and handles all file transfers and network communications (e.g., scp connections). Together, the RDS is intended to aid researchers by making simulations as easy as possible to generate on the computer resources available. Initial conditions for LIS-6 and GEOS-5 are provided by Modern Era Retrospective-Analysis for Research and Applications (MERRA) reanalysis data stored on DISCOVER. The LIS-6 is first run for 2-4 years forced by MERRA atmospheric analyses, generating initial conditions for the WRF soil physics. GEOS-5 is then initialized from MERRA data and run for the period of interest. Large-scale atmospheric data, sea-surface temperatures, and sea ice coverage from GEOS-5 are used as boundary conditions for WRF, which is run for the same period of interest. Multiply nested grids are used for both LIS-6 and WRF, with the innermost grid run at a resolution sufficient for typical</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/20020090699','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/20020090699"><span>NASA Aviation Safety Program <span class="hlt">Weather</span> Accident Prevention/<span class="hlt">weather</span> Information Communications (WINCOMM)</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Feinberg, Arthur; Tauss, James; Chomos, Gerald (Technical Monitor)</p> <p>2002-01-01</p> <p><span class="hlt">Weather</span> is a contributing factor in approximately 25-30 percent of general aviation accidents. The lack of timely, accurate and usable <span class="hlt">weather</span> information to the general aviation pilot in the cockpit to enhance pilot situational awareness and improve pilot judgment remains a major impediment to improving aviation safety. NASA Glenn Research Center commissioned this 120 day <span class="hlt">weather</span> datalink market survey to assess the technologies, infrastructure, products, and services of commercial avionics <span class="hlt">systems</span> being marketed to the general aviation community to address these longstanding safety concerns. A market survey of companies providing or proposing to provide graphical <span class="hlt">weather</span> information to the general aviation cockpit was conducted. Fifteen commercial companies were surveyed. These <span class="hlt">systems</span> are characterized and evaluated in this report by availability, end-user pricing/cost, <span class="hlt">system</span> constraints/limits and technical specifications. An analysis of market survey results and an evaluation of product offerings were made. In addition, recommendations to NASA for additional research and technology development investment have been made as a result of this survey to accelerate deployment of cockpit <span class="hlt">weather</span> information <span class="hlt">systems</span> for enhancing aviation safety.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2014AGUFMED21B3449S','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2014AGUFMED21B3449S"><span>Capturing the WUnder: Using <span class="hlt">weather</span> stations and <span class="hlt">Weather</span>Underground to increase middle school students' understanding and interest in science</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Schild, K. M.; Dunne, P.</p> <p>2014-12-01</p> <p>New <span class="hlt">models</span> of elementary- and middle-school level science education are emerging in response to the need for science literacy and the development of the Next Generation Science Standards. One of these <span class="hlt">models</span> is fostered through the NSF's Graduate Teaching Fellows in K-12 Education (GK-12) program, which pairs a graduate fellow with a science teacher at a local school for an entire school year. In our project, a PhD Earth Sciences student was paired with a local middle school science teacher with the goal of installing a <span class="hlt">weather</span> station, and incorporating the station data into the 8th grade science curriculum. Here we discuss how we were able to use a school <span class="hlt">weather</span> station to introduce <span class="hlt">weather</span> and climate material, engage and involve students in the creative process of science, and motivate students through inquiry-based lessons. In using a <span class="hlt">weather</span> station as the starting point for material, we were able to make science tangible for students and provide an opportunity for each student to experience the entire process of scientific inquiry. This hands-on approach resulted in a more thorough understanding the <span class="hlt">system</span> beyond a knowledge of the components, and was particularly effective in challenging prior <span class="hlt">weather</span> and climate misconceptions. We were also able to expand the reach of the lessons by connecting with other <span class="hlt">weather</span> stations in our region and even globally, enabling the students to become members of a larger <span class="hlt">system</span>.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.fs.usda.gov/treesearch/pubs/31208','TREESEARCH'); return false;" href="https://www.fs.usda.gov/treesearch/pubs/31208"><span>Managing wildland fires: integrating <span class="hlt">weather</span> <span class="hlt">models</span> into fire projections</span></a></p> <p><a target="_blank" href="http://www.fs.usda.gov/treesearch/">Treesearch</a></p> <p>Anne M. Rosenthal; Francis Fujioka</p> <p>2004-01-01</p> <p>Flames from the Old Fire sweep through lands north of San Bernardino during late fall of 2003. Like many Southern California fires, the Old Fire consumed susceptible forests at the urban-wildland interface and spread to nearby city neighborhoods. By incorporating <span class="hlt">weather</span> <span class="hlt">models</span> into fire perimeter projections, scientist Francis Fujioka is improving fire <span class="hlt">modeling</span> as a...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2011AGUFM.A51A0250Y','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2011AGUFM.A51A0250Y"><span>Strategies for Effective Implementation of Science <span class="hlt">Models</span> into 6-9 Grade Classrooms on Climate, <span class="hlt">Weather</span>, and Energy Topics</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Yarker, M. B.; Stanier, C. O.; Forbes, C.; Park, S.</p> <p>2011-12-01</p> <p>As atmospheric scientists, we depend on Numerical <span class="hlt">Weather</span> Prediction (NWP) <span class="hlt">models</span>. We use them to predict <span class="hlt">weather</span> patterns, to understand external forcing on the atmosphere, and as evidence to make claims about atmospheric phenomenon. Therefore, it is important that we adequately prepare atmospheric science students to use computer <span class="hlt">models</span>. However, the public should also be aware of what <span class="hlt">models</span> are in order to understand scientific claims about atmospheric issues, such as climate change. Although familiar with <span class="hlt">weather</span> forecasts on television and the Internet, the general public does not understand the process of using computer <span class="hlt">models</span> to generate a <span class="hlt">weather</span> and climate forecasts. As a result, the public often misunderstands claims scientists make about their daily <span class="hlt">weather</span> as well as the state of climate change. Since computer <span class="hlt">models</span> are the best method we have to forecast the future of our climate, scientific <span class="hlt">models</span> and <span class="hlt">modeling</span> should be a topic covered in K-12 classrooms as part of a comprehensive science curriculum. According to the National Science Education Standards, teachers are encouraged to science <span class="hlt">models</span> into the classroom as a way to aid in the understanding of the nature of science. However, there is very little description of what constitutes a science <span class="hlt">model</span>, so the term is often associated with scale <span class="hlt">models</span>. Therefore, teachers often use drawings or scale representations of physical entities, such as DNA, the solar <span class="hlt">system</span>, or bacteria. In other words, <span class="hlt">models</span> used in classrooms are often used as visual representations, but the purpose of science <span class="hlt">models</span> is often overlooked. The implementation of a <span class="hlt">model</span>-based curriculum in the science classroom can be an effective way to prepare students to think critically, problem solve, and make informed decisions as a contributing member of society. However, there are few resources available to help teachers implement science <span class="hlt">models</span> into the science curriculum effectively. Therefore, this research project looks at</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://rosap.ntl.bts.gov/view/dot/17402','DOTNTL'); return false;" href="https://rosap.ntl.bts.gov/view/dot/17402"><span>Aviation <span class="hlt">weather</span> : FAA and the National <span class="hlt">Weather</span> Service are considering plans to consolidate <span class="hlt">weather</span> service offices, but face significant challenges.</span></a></p> <p><a target="_blank" href="http://ntlsearch.bts.gov/tris/index.do">DOT National Transportation Integrated Search</a></p> <p></p> <p>2009-07-01</p> <p>The National <span class="hlt">Weather</span> Services (NWS) <span class="hlt">weather</span> products are a vital component of the Federal Aviation Administrations (FAA) air traffic control <span class="hlt">system</span>. In addition to providing aviation <span class="hlt">weather</span> products developed at its own facilities, NWS also pr...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2006AGUSM.A53C..04H','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2006AGUSM.A53C..04H"><span><span class="hlt">Weather</span> <span class="hlt">modeling</span> for hazard and consequence assessment operations during the 2006 Winter Olympic Games</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Hayes, P.; Trigg, J. L.; Stauffer, D.; Hunter, G.; McQueen, J.</p> <p>2006-05-01</p> <p>Consequence assessment (CA) operations are those processes that attempt to mitigate negative impacts of incidents involving hazardous materials such as chemical, biological, radiological, nuclear, and high explosive (CBRNE) agents, facilities, weapons, or transportation. Incident types range from accidental spillage of chemicals at/en route to/from a manufacturing plant, to the deliberate use of radiological or chemical material as a weapon in a crowded city. The impacts of these incidents are highly variable, from little or no impact to catastrophic loss of life and property. Local and regional scale atmospheric conditions strongly influence atmospheric transport and dispersion processes in the boundary layer, and the extent and scope of the spread of dangerous materials in the lower levels of the atmosphere. Therefore, CA personnel charged with managing the consequences of CBRNE incidents must have detailed knowledge of current and future <span class="hlt">weather</span> conditions to accurately <span class="hlt">model</span> potential effects. A meteorology team was established at the U.S. Defense Threat Reduction Agency (DTRA) to provide <span class="hlt">weather</span> support to CA personnel operating DTRA's CA tools, such as the Hazard Prediction and Assessment Capability (HPAC) tool. The meteorology team performs three main functions: 1) regular provision of meteorological data for use by personnel using HPAC, 2) determination of the best performing medium-range <span class="hlt">model</span> forecast for the 12 - 48 hour timeframe and 3) provision of real-time help-desk support to users regarding acquisition and use of <span class="hlt">weather</span> in HPAC CA applications. The normal meteorology team operations were expanded during a recent <span class="hlt">modeling</span> project which took place during the 2006 Winter Olympic Games. The meteorology team took advantage of special <span class="hlt">weather</span> observation datasets available in the domain of the Winter Olympic venues and undertook a project to improve <span class="hlt">weather</span> <span class="hlt">modeling</span> at high resolution. The varied and complex terrain provided a special challenge to the</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.osti.gov/servlets/purl/1376465','SCIGOV-STC'); return false;" href="https://www.osti.gov/servlets/purl/1376465"><span>Comparison of Microclimate Simulated <span class="hlt">weather</span> data to ASHRAE Clear Sky <span class="hlt">Model</span> and Measured Data</span></a></p> <p><a target="_blank" href="http://www.osti.gov/search">DOE Office of Scientific and Technical Information (OSTI.GOV)</a></p> <p>Bhandari, Mahabir S.</p> <p></p> <p>In anticipation of emerging global urbanization and its impact on microclimate, a need exists to better understand and quantify microclimate effects on building energy use. Satisfaction of this need will require coordinated research of microclimate impacts on and from “human <span class="hlt">systems</span>.” The Urban Microclimate and Energy Tool (Urban-MET) project seeks to address this need by quantifying and analyzing the relationships among climatic conditions, urban morphology, land cover, and energy use; and using these relationships to inform energy-efficient urban development and planning. Initial research will focus on analysis of measured and <span class="hlt">modeled</span> energy efficiency of various building types in selected urbanmore » areas and temporal variations in energy use for different urban morphologies under different microclimatic conditions. In this report, we analyze the differences between microclimate <span class="hlt">weather</span> data sets for the Oak Ridge National Laboratory campus produced by ENVI-met and <span class="hlt">Weather</span> Research Forecast (WRF) <span class="hlt">models</span>, the ASHRAE clear sky which defines the maximum amounts of solar radiation that can be expected, and measured data from a <span class="hlt">weather</span> station on campus. Errors with climate variables and their impact on building energy consumption will be shown for the microclimate simulations to help prioritize future improvement for use in microclimate simulation impacts to energy use of buildings.« less</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017GeoRL..44.3346M','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017GeoRL..44.3346M"><span>A dynamical <span class="hlt">systems</span> approach to studying midlatitude <span class="hlt">weather</span> extremes</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Messori, Gabriele; Caballero, Rodrigo; Faranda, Davide</p> <p>2017-04-01</p> <p>Extreme <span class="hlt">weather</span> occurrences carry enormous social and economic costs and routinely garner widespread scientific and media coverage. The ability to predict these events is therefore a topic of crucial importance. Here we propose a novel predictability pathway for extreme events, by building upon recent advances in dynamical <span class="hlt">systems</span> theory. We show that simple dynamical <span class="hlt">systems</span> metrics can be used to identify sets of large-scale atmospheric flow patterns with similar spatial structure and temporal evolution on time scales of several days to a week. In regions where these patterns favor extreme <span class="hlt">weather</span>, they afford a particularly good predictability of the extremes. We specifically test this technique on the atmospheric circulation in the North Atlantic region, where it provides predictability of large-scale wintertime surface temperature extremes in Europe up to 1 week in advance.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2015AdWR...85...14G','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2015AdWR...85...14G"><span>A transient stochastic <span class="hlt">weather</span> generator incorporating climate <span class="hlt">model</span> uncertainty</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Glenis, Vassilis; Pinamonti, Valentina; Hall, Jim W.; Kilsby, Chris G.</p> <p>2015-11-01</p> <p>Stochastic <span class="hlt">weather</span> generators (WGs), which provide long synthetic time series of <span class="hlt">weather</span> variables such as rainfall and potential evapotranspiration (PET), have found widespread use in water resources <span class="hlt">modelling</span>. When conditioned upon the changes in climatic statistics (change factors, CFs) predicted by climate <span class="hlt">models</span>, WGs provide a useful tool for climate impacts assessment and adaption planning. The latest climate <span class="hlt">modelling</span> exercises have involved large numbers of global and regional climate <span class="hlt">models</span> integrations, designed to explore the implications of uncertainties in the climate <span class="hlt">model</span> formulation and parameter settings: so called 'perturbed physics ensembles' (PPEs). In this paper we show how these climate <span class="hlt">model</span> uncertainties can be propagated through to impact studies by testing multiple vectors of CFs, each vector derived from a different sample from a PPE. We combine this with a new methodology to parameterise the projected time-evolution of CFs. We demonstrate how, when conditioned upon these time-dependent CFs, an existing, well validated and widely used WG can be used to generate non-stationary simulations of future climate that are consistent with probabilistic outputs from the Met Office Hadley Centre's Perturbed Physics Ensemble. The WG enables extensive sampling of natural variability and climate <span class="hlt">model</span> uncertainty, providing the basis for development of robust water resources management strategies in the context of a non-stationary climate.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://ntrs.nasa.gov/search.jsp?R=19800025990&hterms=physical+dependence&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D20%26Ntt%3Dphysical%2Bdependence','NASA-TRS'); return false;" href="https://ntrs.nasa.gov/search.jsp?R=19800025990&hterms=physical+dependence&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D20%26Ntt%3Dphysical%2Bdependence"><span>Effects of sounding temperature assimilation on <span class="hlt">weather</span> forecasting - <span class="hlt">Model</span> dependence studies</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Ghil, M.; Halem, M.; Atlas, R.</p> <p>1979-01-01</p> <p>In comparing various methods for the assimilation of remote sounding information into numerical <span class="hlt">weather</span> prediction (NWP) <span class="hlt">models</span>, the problem of <span class="hlt">model</span> dependence for the different results obtained becomes important. The paper investigates two aspects of the <span class="hlt">model</span> dependence question: (1) the effect of increasing horizontal resolution within a given <span class="hlt">model</span> on the assimilation of sounding data, and (2) the effect of using two entirely different <span class="hlt">models</span> with the same assimilation method and sounding data. Tentative conclusions reached are: first, that <span class="hlt">model</span> improvement as exemplified by increased resolution, can act in the same direction as judicious 4-D assimilation of remote sounding information, to improve 2-3 day numerical <span class="hlt">weather</span> forecasts. Second, that the time continuous 4-D methods developed at GLAS have similar beneficial effects when used in the assimilation of remote sounding information into NWP <span class="hlt">models</span> with very different numerical and physical characteristics.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2016EGUGA..1810225G','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2016EGUGA..1810225G"><span>Adverse <span class="hlt">weather</span> impacts on arable cropping <span class="hlt">systems</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Gobin, Anne</p> <p>2016-04-01</p> <p>Damages due to extreme or adverse <span class="hlt">weather</span> strongly depend on crop type, crop stage, soil conditions and management. The impact is largest during the sensitive periods of the farming calendar, and requires a <span class="hlt">modelling</span> approach to capture the interactions between the crop, its environment and the occurrence of the meteorological event. The hypothesis is that extreme and adverse <span class="hlt">weather</span> events can be quantified and subsequently incorporated in current crop <span class="hlt">models</span>. Since crop development is driven by thermal time and photoperiod, a regional crop <span class="hlt">model</span> was used to examine the likely frequency, magnitude and impacts of frost, drought, heat stress and waterlogging in relation to the cropping season and crop sensitive stages. Risk profiles and associated return levels were obtained by fitting generalized extreme value distributions to block maxima for air humidity, water balance and temperature variables. The risk profiles were subsequently confronted with yields and yield losses for the major arable crops in Belgium, notably winter wheat, winter barley, winter oilseed rape, sugar beet, potato and maize at the field (farm records) to regional scale (statistics). The average daily vapour pressure deficit (VPD) and reference evapotranspiration (ET0) during the growing season is significantly lower (p < 0.001) and has a higher variability before 1988 than after 1988. Distribution patterns of VPD and ET0 have relevant impacts on crop yields. The response to rising temperatures depends on the crop's capability to condition its microenvironment. Crops short of water close their stomata, lose their evaporative cooling potential and ultimately become susceptible to heat stress. Effects of heat stress therefore have to be combined with moisture availability such as the precipitation deficit or the soil water balance. Risks of combined heat and moisture deficit stress appear during the summer. These risks are subsequently related to crop damage. The methodology of defining</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://ntrs.nasa.gov/search.jsp?R=20150014258&hterms=databases&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D40%26Ntt%3Ddatabases','NASA-TRS'); return false;" href="https://ntrs.nasa.gov/search.jsp?R=20150014258&hterms=databases&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D40%26Ntt%3Ddatabases"><span>Development of a Global Fire <span class="hlt">Weather</span> Database</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Field, R. D.; Spessa, A. C.; Aziz, N. A.; Camia, A.; Cantin, A.; Carr, R.; de Groot, W. J.; Dowdy, A. J.; Flannigan, M. D.; Manomaiphiboon, K.; <a style="text-decoration: none; " href="javascript:void(0); " onClick="displayelement('author_20150014258'); toggleEditAbsImage('author_20150014258_show'); toggleEditAbsImage('author_20150014258_hide'); "> <img style="display:inline; width:12px; height:12px; " src="images/arrow-up.gif" width="12" height="12" border="0" alt="hide" id="author_20150014258_show"> <img style="width:12px; height:12px; display:none; " src="images/arrow-down.gif" width="12" height="12" border="0" alt="hide" id="author_20150014258_hide"></p> <p>2015-01-01</p> <p>The Canadian Forest Fire <span class="hlt">Weather</span> Index (FWI) <span class="hlt">System</span> is the mostly widely used fire danger rating <span class="hlt">system</span> in the world. We have developed a global database of daily FWI <span class="hlt">System</span> calculations, beginning in 1980, called the Global Fire <span class="hlt">WEather</span> Database (GFWED) gridded to a spatial resolution of 0.5 latitude by 2/3 longitude. Input <span class="hlt">weather</span> data were obtained from the NASA Modern Era Retrospective- Analysis for Research and Applications (MERRA), and two different estimates of daily precipitation from rain gauges over land. FWI <span class="hlt">System</span> Drought Code calculations from the gridded data sets were compared to calculations from individual <span class="hlt">weather</span> station data for a representative set of 48 stations in North, Central and South America, Europe, Russia, Southeast Asia and Australia. Agreement between gridded calculations and the station-based calculations tended to be most different at low latitudes for strictly MERRA based calculations. Strong biases could be seen in either direction: MERRA DC over the Mato Grosso in Brazil reached unrealistically high values exceeding DCD1500 during the dry season but was too low over Southeast Asia during the dry season. These biases are consistent with those previously identified in MERRA's precipitation, and they reinforce the need to consider alternative sources of precipitation data. GFWED can be used for analyzing historical relationships between fire <span class="hlt">weather</span> and fire activity at continental and global scales, in identifying large-scale atmosphere-ocean controls on fire <span class="hlt">weather</span>, and calibration of FWI-based fire prediction <span class="hlt">models</span>.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/20160000451','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/20160000451"><span>Introducing GFWED: The Global Fire <span class="hlt">Weather</span> Database</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Field, R. D.; Spessa, A. C.; Aziz, N. A.; Camia, A.; Cantin, A.; Carr, R.; de Groot, W. J.; Dowdy, A. J.; Flannigan, M. D.; Manomaiphiboon, K.; <a style="text-decoration: none; " href="javascript:void(0); " onClick="displayelement('author_20160000451'); toggleEditAbsImage('author_20160000451_show'); toggleEditAbsImage('author_20160000451_hide'); "> <img style="display:inline; width:12px; height:12px; " src="images/arrow-up.gif" width="12" height="12" border="0" alt="hide" id="author_20160000451_show"> <img style="width:12px; height:12px; display:none; " src="images/arrow-down.gif" width="12" height="12" border="0" alt="hide" id="author_20160000451_hide"></p> <p>2015-01-01</p> <p>The Canadian Forest Fire <span class="hlt">Weather</span> Index (FWI) <span class="hlt">System</span> is the mostly widely used fire danger rating <span class="hlt">system</span> in the world. We have developed a global database of daily FWI <span class="hlt">System</span> calculations, beginning in 1980, called the Global Fire <span class="hlt">WEather</span> Database (GFWED) gridded to a spatial resolution of 0.5 latitude by 2-3 longitude. Input <span class="hlt">weather</span> data were obtained from the NASA Modern Era Retrospective-Analysis for Research and Applications (MERRA), and two different estimates of daily precipitation from rain gauges over land. FWI <span class="hlt">System</span> Drought Code calculations from the gridded data sets were compared to calculations from individual <span class="hlt">weather</span> station data for a representative set of 48 stations in North, Central and South America, Europe, Russia,Southeast Asia and Australia. Agreement between gridded calculations and the station-based calculations tended to be most different at low latitudes for strictly MERRA based calculations. Strong biases could be seen in either direction: MERRA DC over the Mato Grosso in Brazil reached unrealistically high values exceeding DCD1500 during the dry season but was too low over Southeast Asia during the dry season. These biases are consistent with those previously identified in MERRAs precipitation, and they reinforce the need to consider alternative sources of precipitation data. GFWED can be used for analyzing historical relationships between fire <span class="hlt">weather</span> and fire activity at continental and global scales, in identifying large-scale atmosphereocean controls on fire <span class="hlt">weather</span>, and calibration of FWI-based fire prediction <span class="hlt">models</span>.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017AGUFMPP13E..05P','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017AGUFMPP13E..05P"><span>Interactions between tectonics, silicate <span class="hlt">weathering</span>, and climate explored with carbon cycle <span class="hlt">modeling</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Penman, D. E.; Caves Rugenstein, J. K.; Ibarra, D. E.; Winnick, M.</p> <p>2017-12-01</p> <p>Earth's long-term carbon cycle is thought to benefit from a stabilizing negative feedback in the form of CO2 consumption by the chemical <span class="hlt">weathering</span> of silicate minerals: during periods of elevated atmospheric pCO2, chemical <span class="hlt">weathering</span> rates increase, thus consuming more atmospheric CO2 and cooling global climate, whereas during periods of low pCO2, <span class="hlt">weathering</span> rates decrease, allowing buildup of CO2 in the atmosphere and warming. At equilibrium, CO2 consumption by silicate <span class="hlt">weathering</span> balances volcanic CO2 degassing at a specific atmospheric pCO2 dictated by the relationship between total silicate <span class="hlt">weathering</span> rate and pCO2: Earth's "<span class="hlt">weathering</span> curve." We use numerical carbon cycle <span class="hlt">modeling</span> to demonstrate that the shape and slope of the <span class="hlt">weathering</span> curve is crucial to understanding proposed tectonic controls on pCO2 and climate. First, the shape of the <span class="hlt">weathering</span> curve dictates the equilibrium response of the carbon cycle to changes in the rate of background volcanic/solid Earth CO2 degassing, which has been suggested to vary significantly with plate tectonic reorganizations over geologic timescales. Second, we demonstrate that if tectonic events can significantly change the <span class="hlt">weathering</span> curve, this can act as an effective driver of pCO2 and climate on tectonic timescales by changing the atmospheric pCO2 at which silicate <span class="hlt">weathering</span> balances a constant volcanic/solid Earth degassing rate. Finally, we review the complex interplay of environmental factors that affect modern <span class="hlt">weathering</span> rates in the field and highlight how the resulting uncertainty surrounding the shape of Earth's <span class="hlt">weathering</span> curve significantly hampers our ability to quantitatively predict the response of pCO2 and climate to tectonic forcing, and thus represents a substantial knowledge gap in Earth science. We conclude with strategies for closing this knowledge gap by using precise paleoclimatic reconstructions of intervals with known tectonic forcings.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2006AdAtS..23..442W','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2006AdAtS..23..442W"><span>Framework of distributed coupled atmosphere-ocean-wave <span class="hlt">modeling</span> <span class="hlt">system</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Wen, Yuanqiao; Huang, Liwen; Deng, Jian; Zhang, Jinfeng; Wang, Sisi; Wang, Lijun</p> <p>2006-05-01</p> <p>In order to research the interactions between the atmosphere and ocean as well as their important role in the intensive <span class="hlt">weather</span> <span class="hlt">systems</span> of coastal areas, and to improve the forecasting ability of the hazardous <span class="hlt">weather</span> processes of coastal areas, a coupled atmosphere-ocean-wave <span class="hlt">modeling</span> <span class="hlt">system</span> has been developed. The agent-based environment framework for linking <span class="hlt">models</span> allows flexible and dynamic information exchange between <span class="hlt">models</span>. For the purpose of flexibility, portability and scalability, the framework of the whole <span class="hlt">system</span> takes a multi-layer architecture that includes a user interface layer, computational layer and service-enabling layer. The numerical experiment presented in this paper demonstrates the performance of the distributed coupled <span class="hlt">modeling</span> <span class="hlt">system</span>.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2016EGUGA..18..563D','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2016EGUGA..18..563D"><span>A combined road <span class="hlt">weather</span> forecast <span class="hlt">system</span> to prevent road ice formation in the Adige Valley (Italy)</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Di Napoli, Claudia; Piazza, Andrea; Antonacci, Gianluca; Todeschini, Ilaria; Apolloni, Roberto; Pretto, Ilaria</p> <p>2016-04-01</p> <p>Road ice is a dangerous meteorological hazard to a nation's transportation <span class="hlt">system</span> and economy. By reducing the pavement friction with vehicle tyres, ice formation on pavements increases accident risk and delays travelling times thus posing a serious threat to road users' safety and the running of economic activities. Keeping roads clear and open is therefore essential, especially in mountainous areas where ice is likely to form during the winter period. Winter road maintenance helps to restore road efficiency and security, and its benefits are up to 8 times the costs sustained for anti-icing strategies [1]. However, the optimization of maintenance costs and the reduction of the environmental damage from over-salting demand further improvements. These can be achieved by reliable road <span class="hlt">weather</span> forecasts, and in particular by the prediction of road surface temperatures (RSTs). RST is one of the most important parameters in determining road surface conditions. It is well known from literature that ice forms on pavements in high-humidity conditions when RSTs are below 0°C. We have therefore implemented an automatic forecast <span class="hlt">system</span> to predict critical RSTs on a test route along the Adige Valley complex terrain, in the Italian Alps. The <span class="hlt">system</span> considers two physical <span class="hlt">models</span>, each computing heat and energy fluxes between the road and the atmosphere. One is Reuter's radiative cooling <span class="hlt">model</span>, which predicts RSTs at sunrise as a function of surface temperatures at sunset and the time passed since then [2]. One is METRo (<span class="hlt">Model</span> of the Environment and Temperature of Roads), a road <span class="hlt">weather</span> forecast software which also considers heat conduction through road material [3]. We have applied the forecast <span class="hlt">system</span> to a network of road <span class="hlt">weather</span> stations (road <span class="hlt">weather</span> information <span class="hlt">system</span>, RWIS) installed on the test route [4]. Road and atmospheric observations from RWIS have been used as initial conditions for both METRo and Reuter's <span class="hlt">model</span>. In METRo observations have also been coupled to</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2009AGUFMSA43A1613T','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2009AGUFMSA43A1613T"><span>A Milestone in Commercial Space <span class="hlt">Weather</span>: USTAR Center for Space <span class="hlt">Weather</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Tobiska, W.; Schunk, R. W.; Sojka, J. J.; Thompson, D. C.; Scherliess, L.; Zhu, L.; Gardner, L. C.</p> <p>2009-12-01</p> <p>As of 2009, Utah State University (USU) hosts a new organization to develop commercial space <span class="hlt">weather</span> applications using funding that has been provided by the State of Utah’s Utah Science Technology and Research (USTAR) initiative. The USTAR Center for Space <span class="hlt">Weather</span> (UCSW) is located on the USU campus in Logan, Utah and is developing innovative applications for mitigating adverse space <span class="hlt">weather</span> effects in technological <span class="hlt">systems</span>. Space weather’s effects upon the near-Earth environment are due to dynamic changes in the Sun’s photons, particles, and fields. Of the space environment domains that are affected by space <span class="hlt">weather</span>, the ionosphere is the key region that affects communication and navigation <span class="hlt">systems</span>. The UCSW has developed products for users of <span class="hlt">systems</span> that are affected by space <span class="hlt">weather</span>-driven ionospheric changes. For example, on September 1, 2009 USCW released, in conjunction with Space Environment Technologies, the world’s first real-time space <span class="hlt">weather</span> via an iPhone app. Space WX displays the real-time, current global ionosphere total electron content along with its space <span class="hlt">weather</span> drivers; it is available through the Apple iTunes store and is used around the planet. The Global Assimilation of Ionospheric Measurements (GAIM) <span class="hlt">system</span> is now being run operationally in real-time at UCSW with the continuous ingestion of hundreds of global data streams to dramatically improve the ionosphere’s characterization. We discuss not only funding and technical advances that have led to current products but also describe the direction for UCSW that includes partnering opportunities for moving commercial space <span class="hlt">weather</span> into fully automated specification and forecasting over the next half decade.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/20140013010','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/20140013010"><span>The Role of <span class="hlt">Model</span> and Initial Condition Error in Numerical <span class="hlt">Weather</span> Forecasting Investigated with an Observing <span class="hlt">System</span> Simulation Experiment</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Prive, Nikki C.; Errico, Ronald M.</p> <p>2013-01-01</p> <p>A series of experiments that explore the roles of <span class="hlt">model</span> and initial condition error in numerical <span class="hlt">weather</span> prediction are performed using an observing <span class="hlt">system</span> simulation experiment (OSSE) framework developed at the National Aeronautics and Space Administration Global <span class="hlt">Modeling</span> and Assimilation Office (NASA/GMAO). The use of an OSSE allows the analysis and forecast errors to be explicitly calculated, and different hypothetical observing networks can be tested with ease. In these experiments, both a full global OSSE framework and an 'identical twin' OSSE setup are utilized to compare the behavior of the data assimilation <span class="hlt">system</span> and evolution of forecast skill with and without <span class="hlt">model</span> error. The initial condition error is manipulated by varying the distribution and quality of the observing network and the magnitude of observation errors. The results show that <span class="hlt">model</span> error has a strong impact on both the quality of the analysis field and the evolution of forecast skill, including both systematic and unsystematic <span class="hlt">model</span> error components. With a realistic observing network, the analysis state retains a significant quantity of error due to systematic <span class="hlt">model</span> error. If errors of the analysis state are minimized, <span class="hlt">model</span> error acts to rapidly degrade forecast skill during the first 24-48 hours of forward integration. In the presence of <span class="hlt">model</span> error, the impact of observation errors on forecast skill is small, but in the absence of <span class="hlt">model</span> error, observation errors cause a substantial degradation of the skill of medium range forecasts.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2015AGUFMSH21B2412H','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2015AGUFMSH21B2412H"><span>Verification of Space <span class="hlt">Weather</span> Forecasts using Terrestrial <span class="hlt">Weather</span> Approaches</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Henley, E.; Murray, S.; Pope, E.; Stephenson, D.; Sharpe, M.; Bingham, S.; Jackson, D.</p> <p>2015-12-01</p> <p>The Met Office Space <span class="hlt">Weather</span> Operations Centre (MOSWOC) provides a range of 24/7 operational space <span class="hlt">weather</span> forecasts, alerts, and warnings, which provide valuable information on space <span class="hlt">weather</span> that can degrade electricity grids, radio communications, and satellite electronics. Forecasts issued include arrival times of coronal mass ejections (CMEs), and probabilistic forecasts for flares, geomagnetic storm indices, and energetic particle fluxes and fluences. These forecasts are produced twice daily using a combination of output from <span class="hlt">models</span> such as Enlil, near-real-time observations, and forecaster experience. Verification of forecasts is crucial for users, researchers, and forecasters to understand the strengths and limitations of forecasters, and to assess forecaster added value. To this end, the Met Office (in collaboration with Exeter University) has been adapting verification techniques from terrestrial <span class="hlt">weather</span>, and has been working closely with the International Space Environment Service (ISES) to standardise verification procedures. We will present the results of part of this work, analysing forecast and observed CME arrival times, assessing skill using 2x2 contingency tables. These MOSWOC forecasts can be objectively compared to those produced by the NASA Community Coordinated <span class="hlt">Modelling</span> Center - a useful benchmark. This approach cannot be taken for the other forecasts, as they are probabilistic and categorical (e.g., geomagnetic storm forecasts give probabilities of exceeding levels from minor to extreme). We will present appropriate verification techniques being developed to address these forecasts, such as rank probability skill score, and comparing forecasts against climatology and persistence benchmarks. As part of this, we will outline the use of discrete time Markov chains to assess and improve the performance of our geomagnetic storm forecasts. We will also discuss work to adapt a terrestrial verification visualisation <span class="hlt">system</span> to space <span class="hlt">weather</span>, to help</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://www.dtic.mil/docs/citations/AD1019130','DTIC-ST'); return false;" href="http://www.dtic.mil/docs/citations/AD1019130"><span>Assimilating Thor: How Airmen Integrate <span class="hlt">Weather</span> Prediction</span></a></p> <p><a target="_blank" href="http://www.dtic.mil/">DTIC Science & Technology</a></p> <p></p> <p>2010-06-01</p> <p>atmosphere and the earth from the air and from space widened the aperture of data so as to overexpose humans to the panoply of information coming...endurance record flights circled the earth without stopping; aircraft climbed through the atmosphere into space. <span class="hlt">Weather</span> surveillance radar...advances found congruence in the meteorological advance of ensemble <span class="hlt">weather</span> <span class="hlt">modeling</span>. Complex, adaptive <span class="hlt">systems</span> like the atmosphere lend themselves to</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017JGRF..122.2016C','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017JGRF..122.2016C"><span>Hydrologic Transport of Dissolved Inorganic Carbon and Its Control on Chemical <span class="hlt">Weathering</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Calabrese, Salvatore; Parolari, Anthony J.; Porporato, Amilcare</p> <p>2017-10-01</p> <p>Chemical <span class="hlt">weathering</span> is one of the major processes interacting with climate and tectonics to form clays, supply nutrients to soil microorganisms and plants, and sequester atmospheric CO2. Hydrology and dissolution kinetics have been emphasized as factors controlling chemical <span class="hlt">weathering</span> rates. However, the interaction between hydrology and transport of dissolved inorganic carbon (DIC) in controlling <span class="hlt">weathering</span> has received less attention. In this paper, we present an analytical <span class="hlt">model</span> that couples subsurface water and chemical molar balance equations to analyze the roles of hydrology and DIC transport on chemical <span class="hlt">weathering</span>. The balance equations form a dynamical <span class="hlt">system</span> that fully determines the dynamics of the <span class="hlt">weathering</span> zone chemistry as forced by the transport of DIC. The <span class="hlt">model</span> is formulated specifically for the silicate mineral albite, but it can be extended to other minerals, and is studied as a function of percolation rate and water transit time. Three <span class="hlt">weathering</span> regimes are elucidated. For very small or large values of transit time, the <span class="hlt">weathering</span> is limited by reaction kinetics or transport, respectively. For intermediate values, the <span class="hlt">system</span> is transport controlled and is sensitive to transit time. We apply the <span class="hlt">model</span> to a series of watersheds for which we estimate transit times and identify the type of <span class="hlt">weathering</span> regime. The results suggest that hydrologic transport of DIC may be as important as reaction kinetics and dilution in determining chemical <span class="hlt">weathering</span> rates.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://ntrs.nasa.gov/search.jsp?R=20060040988&hterms=marine&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D90%26Ntt%3Dmarine','NASA-TRS'); return false;" href="https://ntrs.nasa.gov/search.jsp?R=20060040988&hterms=marine&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D90%26Ntt%3Dmarine"><span>Monitoring Marine <span class="hlt">Weather</span> <span class="hlt">Systems</span> Using Quikscat and TRMM Data</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Liu, W.; Tang, W.; Datta, A.; Hsu, C.</p> <p>1999-01-01</p> <p>We do not understand nor are able to predict marine storms, particularly tropical cyclones, sufficiently well because ground-based measurements are sparse and operational numerical <span class="hlt">weather</span> prediction <span class="hlt">models</span> do not have sufficient spatial resolution nor accurate parameterization of the physics.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2018NatEn...3..395Z','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2018NatEn...3..395Z"><span>Designing low-carbon power <span class="hlt">systems</span> for Great Britain in 2050 that are robust to the spatiotemporal and inter-annual variability of <span class="hlt">weather</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Zeyringer, Marianne; Price, James; Fais, Birgit; Li, Pei-Hao; Sharp, Ed</p> <p>2018-05-01</p> <p>The design of cost-effective power <span class="hlt">systems</span> with high shares of variable renewable energy (VRE) technologies requires a <span class="hlt">modelling</span> approach that simultaneously represents the whole energy <span class="hlt">system</span> combined with the spatiotemporal and inter-annual variability of VRE. Here, we soft-link a long-term energy <span class="hlt">system</span> <span class="hlt">model</span>, which explores new energy <span class="hlt">system</span> configurations from years to decades, with a high spatial and temporal resolution power <span class="hlt">system</span> <span class="hlt">model</span> that captures VRE variability from hours to years. Applying this methodology to Great Britain for 2050, we find that VRE-focused power <span class="hlt">system</span> design is highly sensitive to the inter-annual variability of <span class="hlt">weather</span> and that planning based on a single year can lead to operational inadequacy and failure to meet long-term decarbonization objectives. However, some insights do emerge that are relatively stable to <span class="hlt">weather</span>-year. Reinforcement of the transmission <span class="hlt">system</span> consistently leads to a decrease in <span class="hlt">system</span> costs while electricity storage and flexible generation, needed to integrate VRE into the <span class="hlt">system</span>, are generally deployed close to demand centres.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/20110023242','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/20110023242"><span>Dynamic <span class="hlt">Weather</span> Routes: A <span class="hlt">Weather</span> Avoidance Concept for Trajectory-Based Operations</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>McNally, B. David; Love, John</p> <p>2011-01-01</p> <p>The integration of convective <span class="hlt">weather</span> <span class="hlt">modeling</span> with trajectory automation for conflict detection, trial planning, direct routing, and auto resolution has uncovered a concept that could help controllers, dispatchers, and pilots identify improved <span class="hlt">weather</span> routes that result in significant savings in flying time and fuel burn. Trajectory automation continuously and automatically monitors aircraft in flight to find those that could potentially benefit from improved <span class="hlt">weather</span> reroutes. Controllers, dispatchers, and pilots then evaluate reroute options to assess their suitability given current <span class="hlt">weather</span> and traffic. In today's operations aircraft fly convective <span class="hlt">weather</span> avoidance routes that were implemented often hours before aircraft approach the <span class="hlt">weather</span> and automation does not exist to automatically monitor traffic to find improved <span class="hlt">weather</span> routes that open up due to changing <span class="hlt">weather</span> conditions. The automation concept runs in real-time and employs two keysteps. First, a direct routing algorithm automatically identifies flights with large dog legs in their routes and therefore potentially large savings in flying time. These are common - and usually necessary - during convective <span class="hlt">weather</span> operations and analysis of Fort Worth Center traffic shows many aircraft with short cuts that indicate savings on the order of 10 flying minutes. The second and most critical step is to apply trajectory automation with <span class="hlt">weather</span> <span class="hlt">modeling</span> to determine what savings could be achieved by modifying the direct route such that it avoids <span class="hlt">weather</span> and traffic and is acceptable to controllers and flight crews. Initial analysis of Fort Worth Center traffic suggests a savings of roughly 50% of the direct route savings could be achievable.The core concept is to apply trajectory automation with convective <span class="hlt">weather</span> <span class="hlt">modeling</span> in real time to identify a reroute that is free of <span class="hlt">weather</span> and traffic conflicts and indicates enough time and fuel savings to be considered. The concept is interoperable with today</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/20040040165','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/20040040165"><span>An Integrated Decision-Making <span class="hlt">Model</span> for Categorizing <span class="hlt">Weather</span> Products and Decision Aids</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Elgin, Peter D.; Thomas, Rickey P.</p> <p>2004-01-01</p> <p>The National Airspace <span class="hlt">System</span> s capacity will experience considerable growth in the next few decades. <span class="hlt">Weather</span> adversely affects safe air travel. The FAA and NASA are working to develop new technologies that display <span class="hlt">weather</span> information to support situation awareness and optimize pilot decision-making in avoiding hazardous <span class="hlt">weather</span>. Understanding situation awareness and naturalistic decision-making is an important step in achieving this goal. Information representation and situation time stress greatly influence attentional resource allocation and working memory capacity, potentially obstructing accurate situation awareness assessments. Three naturalistic decision-making theories were integrated to provide an understanding of the levels of decision making incorporated in three operational situations and two conditions. The task characteristics associated with each phase of flight govern the level of situation awareness attained and the decision making processes utilized. <span class="hlt">Weather</span> product s attributes and situation task characteristics combine to classify <span class="hlt">weather</span> products according to the decision-making processes best supported. In addition, a graphical interface is described that affords intuitive selection of the appropriate <span class="hlt">weather</span> product relative to the pilot s current flight situation.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/20150002900','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/20150002900"><span>Cloud-Based Numerical <span class="hlt">Weather</span> Prediction for Near Real-Time Forecasting and Disaster Response</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Molthan, Andrew; Case, Jonathan; Venners, Jason; Schroeder, Richard; Checchi, Milton; Zavodsky, Bradley; Limaye, Ashutosh; O'Brien, Raymond</p> <p>2015-01-01</p> <p>The use of cloud computing resources continues to grow within the public and private sector components of the <span class="hlt">weather</span> enterprise as users become more familiar with cloud-computing concepts, and competition among service providers continues to reduce costs and other barriers to entry. Cloud resources can also provide capabilities similar to high-performance computing environments, supporting multi-node <span class="hlt">systems</span> required for near real-time, regional <span class="hlt">weather</span> predictions. Referred to as "Infrastructure as a Service", or IaaS, the use of cloud-based computing hardware in an on-demand payment <span class="hlt">system</span> allows for rapid deployment of a <span class="hlt">modeling</span> <span class="hlt">system</span> in environments lacking access to a large, supercomputing infrastructure. Use of IaaS capabilities to support regional <span class="hlt">weather</span> prediction may be of particular interest to developing countries that have not yet established large supercomputing resources, but would otherwise benefit from a regional <span class="hlt">weather</span> forecasting capability. Recently, collaborators from NASA Marshall Space Flight Center and Ames Research Center have developed a scripted, on-demand capability for launching the NOAA/NWS Science and Training Resource Center (STRC) Environmental <span class="hlt">Modeling</span> <span class="hlt">System</span> (EMS), which includes pre-compiled binaries of the latest version of the <span class="hlt">Weather</span> Research and Forecasting (WRF) <span class="hlt">model</span>. The WRF-EMS provides scripting for downloading appropriate initial and boundary conditions from global <span class="hlt">models</span>, along with higher-resolution vegetation, land surface, and sea surface temperature data sets provided by the NASA Short-term Prediction Research and Transition (SPoRT) Center. This presentation will provide an overview of the <span class="hlt">modeling</span> <span class="hlt">system</span> capabilities and benchmarks performed on the Amazon Elastic Compute Cloud (EC2) environment. In addition, the presentation will discuss future opportunities to deploy the <span class="hlt">system</span> in support of <span class="hlt">weather</span> prediction in developing countries supported by NASA's SERVIR Project, which provides capacity building</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2014AGUFMGC23D0662D','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2014AGUFMGC23D0662D"><span>Stochastic Hourly <span class="hlt">Weather</span> Generator HOWGH: Validation and its Use in Pest <span class="hlt">Modelling</span> under Present and Future Climates</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Dubrovsky, M.; Hirschi, M.; Spirig, C.</p> <p>2014-12-01</p> <p>To quantify impact of the climate change on a specific pest (or any <span class="hlt">weather</span>-dependent process) in a specific site, we may use a site-calibrated pest (or other) <span class="hlt">model</span> and compare its outputs obtained with site-specific <span class="hlt">weather</span> data representing present vs. perturbed climates. The input <span class="hlt">weather</span> data may be produced by the stochastic <span class="hlt">weather</span> generator. Apart from the quality of the pest <span class="hlt">model</span>, the reliability of the results obtained in such experiment depend on an ability of the generator to represent the statistical structure of the real world <span class="hlt">weather</span> series, and on the sensitivity of the pest <span class="hlt">model</span> to possible imperfections of the generator. This contribution deals with the multivariate HOWGH <span class="hlt">weather</span> generator, which is based on a combination of parametric and non-parametric statistical methods. Here, HOWGH is used to generate synthetic hourly series of three <span class="hlt">weather</span> variables (solar radiation, temperature and precipitation) required by a dynamic pest <span class="hlt">model</span> SOPRA to simulate the development of codling moth. The contribution presents results of the direct and indirect validation of HOWGH. In the direct validation, the synthetic series generated by HOWGH (various settings of its underlying <span class="hlt">model</span> are assumed) are validated in terms of multiple climatic characteristics, focusing on the subdaily wet/dry and hot/cold spells. In the indirect validation, we assess the generator in terms of characteristics derived from the outputs of SOPRA <span class="hlt">model</span> fed by the observed vs. synthetic series. The <span class="hlt">weather</span> generator may be used to produce <span class="hlt">weather</span> series representing present and future climates. In the latter case, the parameters of the generator may be modified by the climate change scenarios based on Global or Regional Climate <span class="hlt">Models</span>. To demonstrate this feature, the results of codling moth simulations for future climate will be shown. Acknowledgements: The <span class="hlt">weather</span> generator is developed and validated within the frame of projects WG4VALUE (project LD12029 sponsored by the Ministry</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2010AGUFMSM51A1735C','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2010AGUFMSM51A1735C"><span>Realtime Space <span class="hlt">Weather</span> Forecasts Via Android Phone App</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Crowley, G.; Haacke, B.; Reynolds, A.</p> <p>2010-12-01</p> <p>For the past several years, ASTRA has run a first-principles global 3-D fully coupled thermosphere-ionosphere <span class="hlt">model</span> in real-time for space <span class="hlt">weather</span> applications. The <span class="hlt">model</span> is the Thermosphere-Ionosphere Mesosphere Electrodynamics General Circulation <span class="hlt">Model</span> (TIMEGCM). ASTRA also runs the Assimilative Mapping of Ionospheric Electrodynamics (AMIE) in real-time. Using AMIE to drive the high latitude inputs to the TIMEGCM produces high fidelity simulations of the global thermosphere and ionosphere. These simulations can be viewed on the Android Phone App developed by ASTRA. The Space<span class="hlt">Weather</span> app for the Android operating <span class="hlt">system</span> is free and can be downloaded from the Google Marketplace. We present the current status of realtime thermosphere-ionosphere space-<span class="hlt">weather</span> forcasting and discuss the way forward. We explore some of the issues in maintaining real-time simulations with assimilative data feeds in a quasi-operational setting. We also discuss some of the challenges of presenting large amounts of data on a smartphone. The ASTRA Space<span class="hlt">Weather</span> app includes the broadest and most unique range of space <span class="hlt">weather</span> data yet to be found on a single smartphone app. This is a one-stop-shop for space <span class="hlt">weather</span> and the only app where you can get access to ASTRA’s real-time predictions of the global thermosphere and ionosphere, high latitude convection and geomagnetic activity. Because of the phone's GPS capability, users can obtain location specific vertical profiles of electron density, temperature, and time-histories of various parameters from the <span class="hlt">models</span>. The Space<span class="hlt">Weather</span> app has over 9000 downloads, 30 reviews, and a following of active users. It is clear that real-time space <span class="hlt">weather</span> on smartphones is here to stay, and must be included in planning for any transition to operational space-<span class="hlt">weather</span> use.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/19970023066','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/19970023066"><span>Workstation-Based Real-Time Mesoscale <span class="hlt">Modeling</span> Designed for <span class="hlt">Weather</span> Support to Operations at the Kennedy Space Center and Cape Canaveral Air Station</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Manobianco, John; Zack, John W.; Taylor, Gregory E.</p> <p>1996-01-01</p> <p>This paper describes the capabilities and operational utility of a version of the Mesoscale Atmospheric Simulation <span class="hlt">System</span> (MASS) that has been developed to support operational <span class="hlt">weather</span> forecasting at the Kennedy Space Center (KSC) and Cape Canaveral Air Station (CCAS). The implementation of local, mesoscale <span class="hlt">modeling</span> <span class="hlt">systems</span> at KSC/CCAS is designed to provide detailed short-range (less than 24 h) forecasts of winds, clouds, and hazardous <span class="hlt">weather</span> such as thunderstorms. Short-range forecasting is a challenge for daily operations, and manned and unmanned launches since KSC/CCAS is located in central Florida where the <span class="hlt">weather</span> during the warm season is dominated by mesoscale circulations like the sea breeze. For this application, MASS has been modified to run on a Stardent 3000 workstation. Workstation-based, real-time numerical <span class="hlt">modeling</span> requires a compromise between the requirement to run the <span class="hlt">system</span> fast enough so that the output can be used before expiration balanced against the desire to improve the simulations by increasing resolution and using more detailed physical parameterizations. It is now feasible to run high-resolution mesoscale <span class="hlt">models</span> such as MASS on local workstations to provide timely forecasts at a fraction of the cost required to run these <span class="hlt">models</span> on mainframe supercomputers. MASS has been running in the Applied Meteorology Unit (AMU) at KSC/CCAS since January 1994 for the purpose of <span class="hlt">system</span> evaluation. In March 1995, the AMU began sending real-time MASS output to the forecasters and meteorologists at CCAS, Spaceflight Meteorology Group (Johnson Space Center, Houston, Texas), and the National <span class="hlt">Weather</span> Service (Melbourne, Florida). However, MASS is not yet an operational <span class="hlt">system</span>. The final decision whether to transition MASS for operational use will depend on a combination of forecaster feedback, the AMU's final evaluation results, and the life-cycle costs of the operational <span class="hlt">system</span>.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2015AGUFMIN31D..01F','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2015AGUFMIN31D..01F"><span>Towards a National Space <span class="hlt">Weather</span> Predictive Capability</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Fox, N. J.; Ryschkewitsch, M. G.; Merkin, V. G.; Stephens, G. K.; Gjerloev, J. W.; Barnes, R. J.; Anderson, B. J.; Paxton, L. J.; Ukhorskiy, A. Y.; Kelly, M. A.; Berger, T. E.; Bonadonna, L. C. M. F.; Hesse, M.; Sharma, S.</p> <p>2015-12-01</p> <p>National needs in the area of space <span class="hlt">weather</span> informational and predictive tools are growing rapidly. Adverse conditions in the space environment can cause disruption of satellite operations, communications, navigation, and electric power distribution grids, leading to a variety of socio-economic losses and impacts on our security. Future space exploration and most modern human endeavors will require major advances in physical understanding and improved transition of space research to operations. At present, only a small fraction of the latest research and development results from NASA, NOAA, NSF and DoD investments are being used to improve space <span class="hlt">weather</span> forecasting and to develop operational tools. The power of modern research and space <span class="hlt">weather</span> <span class="hlt">model</span> development needs to be better utilized to enable comprehensive, timely, and accurate operational space <span class="hlt">weather</span> tools. The mere production of space <span class="hlt">weather</span> information is not sufficient to address the needs of those who are affected by space <span class="hlt">weather</span>. A coordinated effort is required to support research-to-applications transition efforts and to develop the tools required those who rely on this information. In this presentation we will review the space <span class="hlt">weather</span> <span class="hlt">system</span> developed for the Van Allen Probes mission, together with other datasets, tools and <span class="hlt">models</span> that have resulted from research by scientists at JHU/APL. We will look at how these, and results from future missions such as Solar Probe Plus, could be applied to support space <span class="hlt">weather</span> applications in coordination with other community assets and capabilities.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2009EGUGA..11.3658T','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2009EGUGA..11.3658T"><span>Data Driven Ionospheric <span class="hlt">Modeling</span> in Relation to Space <span class="hlt">Weather</span>: Percent Cloud Coverage</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Tulunay, Y.; Senalp, E. T.; Tulunay, E.</p> <p>2009-04-01</p> <p>Since 1990, a small group at METU has been developing data driven <span class="hlt">models</span> in order to forecast some critical <span class="hlt">system</span> parameters related with the near-Earth space processes. The background on the subject supports new achievements, which contributed the COST 724 activities, which will contribute to the new ES0803 activities. This work mentions one of the outstanding contributions, namely forecasting of meteorological parameters by considering the probable influence of cosmic rays (CR) and sunspot numbers (SSN). The data-driven method is generic and applicable to many Near-Earth Space processes including ionospheric/plasmaspheric interactions. It is believed that the EURIPOS initiative would be useful in supplying wide range reliable data to the <span class="hlt">models</span> developed. Quantification of physical mechanisms, which causally link Space <span class="hlt">Weather</span> to the Earth's <span class="hlt">Weather</span>, has been a challenging task. In this basis, the percent cloud coverage (%CC) and cloud top temperatures (CTT) were forecast one month ahead of time between geographic coordinates of (22.5˚N; 57.5˚N); and (7.5˚W; 47.5˚E) at 96 grid locations and covering the years of 1983 to 2000 using the Middle East Technical University Fuzzy Neural Network <span class="hlt">Model</span> (METU-FNN-M) [Tulunay, 2008]. The Near Earth Space variability at several different time scales arises from a number of separate factors and the physics of the variations cannot be <span class="hlt">modeled</span> due to the lack of current information about the parameters of several natural processes. CR are shielded by the magnetosphere to a certain extent, but they can modulate the low level cloud cover. METU-FNN-M was developed, trained and applied for forecasting the %CC and CTT, by considering the history of those meteorological variables; Cloud Optical Depth (COD); the Ionization (I) value that is formulized and computed by using CR data and CTT; SSN; temporal variables; and defuzified cloudiness. The temporal and spatial variables and the cut off rigidity are used to compute the</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/20090023414','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/20090023414"><span>Configuring the HYSPLIT <span class="hlt">Model</span> for National <span class="hlt">Weather</span> Service Forecast Office and Spaceflight Meteorology Group Applications</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Dreher, Joseph G.</p> <p>2009-01-01</p> <p>For expedience in delivering dispersion guidance in the diversity of operational situations, National <span class="hlt">Weather</span> Service Melbourne (MLB) and Spaceflight Meteorology Group (SMG) are becoming increasingly reliant on the PC-based version of the HYSPLIT <span class="hlt">model</span> run through a graphical user interface (GUI). While the GUI offers unique advantages when compared to traditional methods, it is difficult for forecasters to run and manage in an operational environment. To alleviate the difficulty in providing scheduled real-time trajectory and concentration guidance, the Applied Meteorology Unit (AMU) configured a Linux version of the Hybrid Single-Particle Lagrangian Integrated Trajectory (HYSPLIT) (HYSPLIT) <span class="hlt">model</span> that ingests the National Centers for Environmental Prediction (NCEP) guidance, such as the North American Mesoscale (NAM) and the Rapid Update Cycle (RUC) <span class="hlt">models</span>. The AMU configured the HYSPLIT <span class="hlt">system</span> to automatically download the NCEP <span class="hlt">model</span> products, convert the meteorological grids into HYSPLIT binary format, run the <span class="hlt">model</span> from several pre-selected latitude/longitude sites, and post-process the data to create output graphics. In addition, the AMU configured several software programs to convert local <span class="hlt">Weather</span> Research and Forecast (WRF) <span class="hlt">model</span> output into HYSPLIT format.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/20120007669','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/20120007669"><span>Using Science Data and <span class="hlt">Models</span> for Space <span class="hlt">Weather</span> Forecasting - Challenges and Opportunities</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Hesse, Michael; Pulkkinen, Antti; Zheng, Yihua; Maddox, Marlo; Berrios, David; Taktakishvili, Sandro; Kuznetsova, Masha; Chulaki, Anna; Lee, Hyesook; Mullinix, Rick; <a style="text-decoration: none; " href="javascript:void(0); " onClick="displayelement('author_20120007669'); toggleEditAbsImage('author_20120007669_show'); toggleEditAbsImage('author_20120007669_hide'); "> <img style="display:inline; width:12px; height:12px; " src="images/arrow-up.gif" width="12" height="12" border="0" alt="hide" id="author_20120007669_show"> <img style="width:12px; height:12px; display:none; " src="images/arrow-down.gif" width="12" height="12" border="0" alt="hide" id="author_20120007669_hide"></p> <p>2012-01-01</p> <p>Space research, and, consequently, space <span class="hlt">weather</span> forecasting are immature disciplines. Scientific knowledge is accumulated frequently, which changes our understanding or how solar eruptions occur, and of how they impact targets near or on the Earth, or targets throughout the heliosphere. Along with continuous progress in understanding, space research and forecasting <span class="hlt">models</span> are advancing rapidly in capability, often providing substantially increases in space <span class="hlt">weather</span> value over time scales of less than a year. Furthermore, the majority of space environment information available today is, particularly in the solar and heliospheric domains, derived from research missions. An optimal forecasting environment needs to be flexible enough to benefit from this rapid development, and flexible enough to adapt to evolving data sources, many of which may also stem from non-US entities. This presentation will analyze the experiences obtained by developing and operating both a forecasting service for NASA, and an experimental forecasting <span class="hlt">system</span> for Geomagnetically Induced Currents.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2010cosp...38.4177S','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2010cosp...38.4177S"><span>Particle radiation transport and effects <span class="hlt">models</span> from research to space <span class="hlt">weather</span> operations</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Santin, Giovanni; Nieminen, Petteri; Rivera, Angela; Ibarmia, Sergio; Truscott, Pete; Lei, Fan; Desorgher, Laurent; Ivanchenko, Vladimir; Kruglanski, Michel; Messios, Neophytos</p> <p></p> <p>Assessment of risk from potential radiation-induced effects to space <span class="hlt">systems</span> requires knowledge of both the conditions of the radiation environment and of the impact of radiation on sensi-tive spacecraft elements. During sensitivity analyses, test data are complemented by <span class="hlt">models</span> to predict how external radiation fields are transported and modified in spacecraft materials. Radiation transport is still itself a subject of research and <span class="hlt">models</span> are continuously improved to describe the physical interactions that take place when particles pass through shielding materi-als or hit electronic <span class="hlt">systems</span> or astronauts, sometimes down to nanometre-scale interactions of single particles with deep sub-micron technologies or DNA structures. In recent years, though, such radiation transport <span class="hlt">models</span> are transitioning from being a research subject by itself, to being widely used in the space engineering domain and finally being directly applied in the context of operation of space <span class="hlt">weather</span> services. A significant "research to operations" (R2O) case is offered by Geant4, an open source toolkit initially developed and used in the context of fundamental research in high energy physics. Geant4 is also being used in the space domain, e.g. for <span class="hlt">modelling</span> detector responses in science payloads, but also for studying the radiation environment itself, with subjects ranging from cosmic rays, to solar energetic particles in the heliosphere, to geomagnetic shielding. Geant4-based tools are now becoming more and more integrated in spacecraft design procedures, also through user friendly interfaces such as SPEN-VIS. Some examples are given by MULASSIS, offering multi-layered shielding analysis capa-bilities in realistic spacecraft materials, or GEMAT, focused on micro-dosimetry in electronics, or PLANETOCOSMICS, describing the interaction of the space environment with planetary magneto-and atmospheres, or GRAS, providing a modular and easy to use interface to various analysis types in simple or</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/1986JApMe..25.1333F','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/1986JApMe..25.1333F"><span>The Contribution of Mesoscale Convective <span class="hlt">Weather</span> <span class="hlt">Systems</span> to the Warm-Season Precipitation in the United States.</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Fritsch, J. M.; Kane, R. J.; Chelius, C. R.</p> <p>1986-10-01</p> <p>The contribution of precipitation from mesoscale convective <span class="hlt">weather</span> <span class="hlt">systems</span> to the warm-season (April-September) rainfall in the United States is evaluated. Both Mesoscale Convective Complexes (MCC's) and other large, long-lived mesoscale convective <span class="hlt">systems</span> that do not quite meet Maddox's criteria for being termed an MCC are included in the evaluation. The distribution and geographical limits of the precipitation from the convective <span class="hlt">weather</span> <span class="hlt">systems</span> are constructed for the warm seasons of 1982, a `normal' year, and 1983, a drought year. Precipitation characteristics of the <span class="hlt">systems</span> are compared for the 2 years to determine how large-scale drought patterns affect their precipitation production.The frequency, precipitation characteristics and hydrologic ramifications of multiple occurrences, or series, of convective <span class="hlt">weather</span> <span class="hlt">systems</span> are presented and discussed. The temporal and spatial characteristics of the accumulated precipitation from a series of convective complexes is investigated and compared to that of Hurricane Alicia.It is found that mesoscale convective <span class="hlt">weather</span> <span class="hlt">systems</span> account for approximately 30% to 70% of the warm-season (April-September) precipitation over much of the region between the Rocky Mountains and the Mississippi River. During the June through August period, their contribution is even larger. Moreover, series of convective <span class="hlt">weather</span> <span class="hlt">systems</span> are very likely the most prolific precipitation producer in the United States, rivaling and even exceeding that of hurricanes.Changes in the large-scale circulation patterns affected the seasonal precipitation from mesoscale convective <span class="hlt">weather</span> <span class="hlt">systems</span> by altering the precipitation characteristics of individual <span class="hlt">systems</span>. In particular, for the drought period of 1983, the frequency of the convective <span class="hlt">systems</span> remained nearly the same as in the `normal' year (1982); however, the average precipitation area and the average volumetric production significantly decreased. Nevertheless, the rainfall that was produced by</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://ntrs.nasa.gov/search.jsp?R=20040035530&hterms=cognitive+task+analysis&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D10%26Ntt%3Dcognitive%2Btask%2Banalysis','NASA-TRS'); return false;" href="https://ntrs.nasa.gov/search.jsp?R=20040035530&hterms=cognitive+task+analysis&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D10%26Ntt%3Dcognitive%2Btask%2Banalysis"><span>Human-Centered <span class="hlt">Systems</span> Analysis of Aircraft Separation from Adverse <span class="hlt">Weather</span>: Implications for Icing Remote Sensing</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Vigeant-Langlois, Laurence; Hansman, R. John, Jr.</p> <p>2003-01-01</p> <p>The objective of this project was to propose a means to improve aviation <span class="hlt">weather</span> information, training procedures based on a human-centered <span class="hlt">systems</span> approach. Methodology: cognitive analysis of pilot's tasks; trajectory-based approach to <span class="hlt">weather</span> information; contingency planning support; and implications for improving <span class="hlt">weather</span> information.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2018E%26PSL.493..174M','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2018E%26PSL.493..174M"><span>Mountain ranges, climate and <span class="hlt">weathering</span>. Do orogens strengthen or weaken the silicate <span class="hlt">weathering</span> carbon sink?</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Maffre, Pierre; Ladant, Jean-Baptiste; Moquet, Jean-Sébastien; Carretier, Sébastien; Labat, David; Goddéris, Yves</p> <p>2018-07-01</p> <p>The role of mountains in the geological evolution of the carbon cycle has been intensively debated for the last decades. Mountains are thought to increase the local physical erosion, which in turns promotes silicate <span class="hlt">weathering</span>, organic carbon transport and burial, and release of sulfuric acid by dissolution of sulfides. In this contribution, we explore the impact of mountain ranges on silicate <span class="hlt">weathering</span>. Mountains modify the global pattern of atmospheric circulation as well as the local erosion conditions. Using an IPCC-class climate <span class="hlt">model</span>, we first estimate the climatic impact of mountains by comparing the present day climate with the climate when all the continents are assumed to be flat. We then use these climate output to calculate <span class="hlt">weathering</span> changes when mountains are present or absent, using standard expression for physical erosion and a 1D vertical <span class="hlt">model</span> for rock <span class="hlt">weathering</span>. We found that large-scale climate changes and enhanced rock supply by erosion due to mountain uplift have opposite effect, with similar orders of magnitude. A thorough testing of the <span class="hlt">weathering</span> <span class="hlt">model</span> parameters by data-<span class="hlt">model</span> comparison shows that best-fit parameterizations lead to a decrease of <span class="hlt">weathering</span> rate in the absence of mountain by about 20%. However, we demonstrate that solutions predicting an increase in <span class="hlt">weathering</span> in the absence of mountain cannot be excluded. A clear discrimination between the solutions predicting an increase or a decrease in global <span class="hlt">weathering</span> is pending on the improvement of the existing global databases for silicate <span class="hlt">weathering</span>. Nevertheless, imposing a constant and homogeneous erosion rate for <span class="hlt">models</span> without relief, we found that <span class="hlt">weathering</span> decrease becomes unequivocal for very low erosion rates (below 10 t/km2/yr). We conclude that further monitoring of continental silicate <span class="hlt">weathering</span> should be performed with a spatial distribution allowing to discriminate between the various continental landscapes (mountains, plains …).</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017AGUFMSH32B..01B','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017AGUFMSH32B..01B"><span>NSF's Perspective on Space <span class="hlt">Weather</span> Research for Building Forecasting Capabilities</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Bisi, M. M.; Pulkkinen, A. A.; Bisi, M. M.; Pulkkinen, A. A.; Webb, D. F.; Oughton, E. J.; Azeem, S. I.</p> <p>2017-12-01</p> <p>Space <span class="hlt">weather</span> research at the National Science Foundation (NSF) is focused on scientific discovery and on deepening knowledge of the Sun-Geospace <span class="hlt">system</span>. The process of maturation of knowledge base is a requirement for the development of improved space <span class="hlt">weather</span> forecast <span class="hlt">models</span> and for the accurate assessment of potential mitigation strategies. Progress in space <span class="hlt">weather</span> forecasting requires advancing in-depth understanding of the underlying physical processes, developing better instrumentation and measurement techniques, and capturing the advancements in understanding in large-scale physics based <span class="hlt">models</span> that span the entire chain of events from the Sun to the Earth. This presentation will provide an overview of current and planned programs pertaining to space <span class="hlt">weather</span> research at NSF and discuss the recommendations of the Geospace Section portfolio review panel within the context of space <span class="hlt">weather</span> forecasting capabilities.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017AGUFMSH32B..04T','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017AGUFMSH32B..04T"><span>Overview of NASA Heliophysics and the Science of Space <span class="hlt">Weather</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Talaat, E. R.</p> <p>2017-12-01</p> <p>In this paper, an overview is presented on the various activities within NASA that address space <span class="hlt">weather</span>-related observations, <span class="hlt">model</span> development, and research to operations. Specific to space <span class="hlt">weather</span>, NASA formulates and implements, through the Heliophysics division, a national research program for understanding the Sun and its interactions with the Earth and the Solar <span class="hlt">System</span> and how these phenomena impact life and society. NASA researches and prototypes new mission and instrument capabilities in this area, providing new physics-based algorithms to advance the state of solar, space physics, and space <span class="hlt">weather</span> <span class="hlt">modeling</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_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/2060/19810007126','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/19810007126"><span>World <span class="hlt">weather</span> program</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p></p> <p>1980-01-01</p> <p>A brief description of the Global <span class="hlt">Weather</span> Experiment is presented. The world <span class="hlt">weather</span> watch program plan is described and includes a global observing <span class="hlt">system</span>, a global data processing <span class="hlt">system</span>, a global telecommunication <span class="hlt">system</span>, and a voluntary cooperation program. A summary of Federal Agency plans and programs to meet the challenges of international meteorology for the two year period, FY 1980-1981, is presented.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/28336017','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/28336017"><span><span class="hlt">Weather</span> Webcam <span class="hlt">System</span> for the Safety of Helicopter Emergency Medical Services in Miyazaki, Japan.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Kanemaru, Katsuhiro; Katzer, Robert; Hanato, Syu; Nakamura, Koji; Matsuoka, Hiroshi; Ochiai, Hidenobu</p> <p></p> <p>In Japan, the helicopter emergency medical services (HEMS) <span class="hlt">system</span> was initiated in 2001 and introduced to Miyazaki Prefecture in 2012. Mountainous areas occupy 88% of Miyazaki's land area, and HEMS flights can be subject to the effects of <span class="hlt">weather</span>. Therefore, ensuring safety in changing <span class="hlt">weather</span> conditions is a necessity for HEMS. The <span class="hlt">weather</span> webcam <span class="hlt">system</span> (WWS) was established to observe the meteorological conditions in 29 locations. Assessments of the probability of a flight based on conventional data including a <span class="hlt">weather</span> chart provided by the Japan Meteorological Agency and meteorological reports provided by the Miyazaki Airport were compared with the assessment based on the combination of the information obtained from the WWS and the conventional data. The results showed that the probability of a flight by HEMS increased when using the WSS, leading to an increased transportation opportunity for patients in the mountains who rely on HEMS. In addition, the results indicate that the WWS may prevent flights in unfavorable <span class="hlt">weather</span> conditions. The WWS used in conjunction with conventional <span class="hlt">weather</span> data within Miyazaki HEMS increased the pilot's awareness of current <span class="hlt">weather</span> conditions throughout the Prefecture, increasing the probability of accepting a flight. Copyright © 2017 Air Medical Journal Associates. Published by Elsevier Inc. All rights reserved.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/20110020754','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/20110020754"><span>SCOSTEP: Understanding the Climate and <span class="hlt">Weather</span> of the Sun-Earth <span class="hlt">System</span></span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Gopalswamy, Natchimuthuk</p> <p>2011-01-01</p> <p>The international solar-terrestrial physics community had recognized the importance of space <span class="hlt">weather</span> more than a decade ago, which resulted in a number of international collaborative activities such as the Climate and <span class="hlt">Weather</span> of the Sun Earth <span class="hlt">System</span> (CAWSES) by the Scientific Committee on Solar Terrestrial Physics (SCOSTEP). The CAWSES program is the current major scientific program of SCOSTEP that will continue until the end of the year 2013. The CAWSES program has brought scientists from all over the world together to tackle the scientific issues behind the Sun-Earth connected <span class="hlt">system</span> and explore ways of helping the human society. In addition to the vast array of space instruments, ground based instruments have been deployed, which not only filled voids in data coverage, but also inducted young scientists from developing countries into the scientific community. This paper presents a summary of CAWSES and other SCOSTEP activities that promote space <span class="hlt">weather</span> science via complementary approaches in international scientific collaborations, capacity building, and public outreach.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/20140006646','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/20140006646"><span>Accelerating Climate and <span class="hlt">Weather</span> Simulations through Hybrid Computing</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Zhou, Shujia; Cruz, Carlos; Duffy, Daniel; Tucker, Robert; Purcell, Mark</p> <p>2011-01-01</p> <p>Unconventional multi- and many-core processors (e.g. IBM (R) Cell B.E.(TM) and NVIDIA (R) GPU) have emerged as effective accelerators in trial climate and <span class="hlt">weather</span> simulations. Yet these climate and <span class="hlt">weather</span> <span class="hlt">models</span> typically run on parallel computers with conventional processors (e.g. Intel, AMD, and IBM) using Message Passing Interface. To address challenges involved in efficiently and easily connecting accelerators to parallel computers, we investigated using IBM's Dynamic Application Virtualization (TM) (IBM DAV) software in a prototype hybrid computing <span class="hlt">system</span> with representative climate and <span class="hlt">weather</span> <span class="hlt">model</span> components. The hybrid <span class="hlt">system</span> comprises two Intel blades and two IBM QS22 Cell B.E. blades, connected with both InfiniBand(R) (IB) and 1-Gigabit Ethernet. The <span class="hlt">system</span> significantly accelerates a solar radiation <span class="hlt">model</span> component by offloading compute-intensive calculations to the Cell blades. Systematic tests show that IBM DAV can seamlessly offload compute-intensive calculations from Intel blades to Cell B.E. blades in a scalable, load-balanced manner. However, noticeable communication overhead was observed, mainly due to IP over the IB protocol. Full utilization of IB Sockets Direct Protocol and the lower latency production version of IBM DAV will reduce this overhead.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2015AGUFMGC43H..05F','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2015AGUFMGC43H..05F"><span>Introducing the Global Fire <span class="hlt">WEather</span> Database (GFWED)</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Field, R. D.</p> <p>2015-12-01</p> <p>The Canadian Fire <span class="hlt">Weather</span> Index (FWI) <span class="hlt">System</span> is the mostly widely used fire danger rating <span class="hlt">system</span> in the world. We have developed a global database of daily FWI <span class="hlt">System</span> calculations beginning in 1980 called the Global Fire <span class="hlt">WEather</span> Database (GFWED) gridded to a spatial resolution of 0.5° latitude by 2/3° longitude. Input <span class="hlt">weather</span> data were obtained from the NASA Modern Era Retrospective-Analysis for Research (MERRA), and two different estimates of daily precipitation from rain gauges over land. FWI <span class="hlt">System</span> Drought Code calculations from the gridded datasets were compared to calculations from individual <span class="hlt">weather</span> station data for a representative set of 48 stations in North, Central and South America, Europe, Russia, Southeast Asia and Australia. Agreement between gridded calculations and the station-based calculations tended to be most different at low latitudes for strictly MERRA-based calculations. Strong biases could be seen in either direction: MERRA DC over the Mato Grosso in Brazil reached unrealistically high values exceeding DC=1500 during the dry season but was too low over Southeast Asia during the dry season. These biases are consistent with those previously-identified in MERRA's precipitation and reinforce the need to consider alternative sources of precipitation data. GFWED is being used by researchers around the world for analyzing historical relationships between fire <span class="hlt">weather</span> and fire activity at large scales, in identifying large-scale atmosphere-ocean controls on fire <span class="hlt">weather</span>, and calibration of FWI-based fire prediction <span class="hlt">models</span>. These applications will be discussed. More information on GFWED can be found at http://data.giss.nasa.gov/impacts/gfwed/</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/19920012260','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/19920012260"><span>Cockpit <span class="hlt">weather</span> information needs</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Scanlon, Charles H.</p> <p>1992-01-01</p> <p>The primary objective is to develop an advanced pilot <span class="hlt">weather</span> interface for the flight deck and to measure its utilization and effectiveness in pilot reroute decision processes, <span class="hlt">weather</span> situation awareness, and <span class="hlt">weather</span> monitoring. Identical graphical <span class="hlt">weather</span> displays for the dispatcher, air traffic control (ATC), and pilot crew should also enhance the dialogue capabilities for reroute decisions. By utilizing a broadcast data link for surface observations, forecasts, radar summaries, lightning strikes, and <span class="hlt">weather</span> alerts, onboard <span class="hlt">weather</span> computing facilities construct graphical displays, historical <span class="hlt">weather</span> displays, color textual displays, and other tools to assist the pilot crew. Since the <span class="hlt">weather</span> data is continually being received and stored by the airborne <span class="hlt">system</span>, the pilot crew has instantaneous access to the latest information. This information is color coded to distinguish degrees of category for surface observations, ceiling and visibilities, and ground radar summaries. Automatic <span class="hlt">weather</span> monitoring and pilot crew alerting is accomplished by the airborne computing facilities. When a new <span class="hlt">weather</span> information is received, the displays are instantaneously changed to reflect the new information. Also, when a new surface or special observation for the intended destination is received, the pilot crew is informed so that information can be studied at the pilot's discretion. The pilot crew is also immediately alerted when a severe <span class="hlt">weather</span> notice, AIRMET or SIGMET, is received. The cockpit <span class="hlt">weather</span> display shares a multicolor eight inch cathode ray tube and overlaid touch panel with a pilot crew data link interface. Touch sensitive buttons and areas are used for pilot selection of graphical and data link displays. Time critical ATC messages are presented in a small window that overlays other displays so that immediate pilot alerting and action can be taken. Predeparture and reroute clearances are displayed on the graphical <span class="hlt">weather</span> <span class="hlt">system</span> so pilot review of <span class="hlt">weather</span> along</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/20160008033','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/20160008033"><span>Magnetogram Forecast: An All-Clear Space <span class="hlt">Weather</span> Forecasting <span class="hlt">System</span></span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Barghouty, Nasser; Falconer, David</p> <p>2015-01-01</p> <p>Solar flares and coronal mass ejections (CMEs) are the drivers of severe space <span class="hlt">weather</span>. Forecasting the probability of their occurrence is critical in improving space <span class="hlt">weather</span> forecasts. The National Oceanic and Atmospheric Administration (NOAA) currently uses the McIntosh active region category <span class="hlt">system</span>, in which each active region on the disk is assigned to one of 60 categories, and uses the historical flare rates of that category to make an initial forecast that can then be adjusted by the NOAA forecaster. Flares and CMEs are caused by the sudden release of energy from the coronal magnetic field by magnetic reconnection. It is believed that the rate of flare and CME occurrence in an active region is correlated with the free energy of an active region. While the free energy cannot be measured directly with present observations, proxies of the free energy can instead be used to characterize the relative free energy of an active region. The Magnetogram Forecast (MAG4) (output is available at the Community Coordinated <span class="hlt">Modeling</span> Center) was conceived and designed to be a databased, all-clear forecasting <span class="hlt">system</span> to support the operational goals of NASA's Space Radiation Analysis Group. The MAG4 <span class="hlt">system</span> automatically downloads nearreal- time line-of-sight Helioseismic and Magnetic Imager (HMI) magnetograms on the Solar Dynamics Observatory (SDO) satellite, identifies active regions on the solar disk, measures a free-energy proxy, and then applies forecasting curves to convert the free-energy proxy into predicted event rates for X-class flares, M- and X-class flares, CMEs, fast CMEs, and solar energetic particle events (SPEs). The forecast curves themselves are derived from a sample of 40,000 magnetograms from 1,300 active region samples, observed by the Solar and Heliospheric Observatory Michelson Doppler Imager. Figure 1 is an example of MAG4 visual output</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/19920010186','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/19920010186"><span>JPL's Real-Time <span class="hlt">Weather</span> Processor project (RWP) metrics and observations at <span class="hlt">system</span> completion</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Loesh, Robert E.; Conover, Robert A.; Malhotra, Shan</p> <p>1990-01-01</p> <p>As an integral part of the overall upgraded National Airspace <span class="hlt">System</span> (NAS), the objective of the Real-Time <span class="hlt">Weather</span> Processor (RWP) project is to improve the quality of <span class="hlt">weather</span> information and the timeliness of its dissemination to <span class="hlt">system</span> users. To accomplish this, an RWP will be installed in each of the Center <span class="hlt">Weather</span> Service Units (CWSUs), located in 21 of the 23 Air Route Traffic Control Centers (ARTCCs). The RWP <span class="hlt">System</span> is a prototype <span class="hlt">system</span>. It is planned that the software will be GFE and that production hardware will be acquired via industry competitive procurement. The ARTCC is a facility established to provide air traffic control service to aircraft operating on Instrument Flight Rules (IFR) flight plans within controlled airspace, principally during the en route phase of the flight. Covered here are requirement metrics, Software Problem Failure Reports (SPFRs), and Ada portability metrics and observations.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://ntrs.nasa.gov/search.jsp?R=20030020320&hterms=Information+Systems&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D90%26Ntt%3DInformation%2BSystems','NASA-TRS'); return false;" href="https://ntrs.nasa.gov/search.jsp?R=20030020320&hterms=Information+Systems&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D90%26Ntt%3DInformation%2BSystems"><span>General Aviation Cockpit <span class="hlt">Weather</span> Information <span class="hlt">System</span> Simulation Studies</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>McAdaragh, Ray; Novacek, Paul</p> <p>2003-01-01</p> <p>This viewgraph presentation provides information on two experiments on the effectiveness of a cockpit <span class="hlt">weather</span> information <span class="hlt">system</span> on a simulated general aviation flight. The presentation covers the simulation hardware configuration, the display device screen layout, a mission scenario, conclusions, and recommendations. The second experiment, with its own scenario and conclusions, is a follow-on experiment.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://ntrs.nasa.gov/search.jsp?R=19820040851&hterms=Flight+planning&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D50%26Ntt%3DFlight%2Bplanning','NASA-TRS'); return false;" href="https://ntrs.nasa.gov/search.jsp?R=19820040851&hterms=Flight+planning&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D50%26Ntt%3DFlight%2Bplanning"><span>Airline flight planning - The <span class="hlt">weather</span> connection</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Steinberg, R.</p> <p>1981-01-01</p> <p>The history of airline flight planning is briefly reviewed. Over half a century ago, when scheduled airline services began, <span class="hlt">weather</span> data were almost nonexistent. By the early 1950's a reliable synoptic network provided upper air reports. The next 15 years saw a rapid growth in commercial aviation, and airlines introduced computer techniques to flight planning. The 1970's saw the development of <span class="hlt">weather</span> satellites. The current state of flight planning activities is analyzed. It is found that accurate flight planning will require meteorological information on a finer scale than can be provided by a synoptic forecast. Opportunities for a new approach are examined, giving attention to the available options, a mesoscale numerical <span class="hlt">weather</span> prediction <span class="hlt">model</span>, limited area fine mesh <span class="hlt">models</span>, man-computer interactive display <span class="hlt">systems</span>, the use of interactive techniques with the present upper air data base, and the implementation of interactive techniques.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2004AGUFMED31D..02B','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2004AGUFMED31D..02B"><span><span class="hlt">Weather</span> it's Climate Change?</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Bostrom, A.; Lashof, D.</p> <p>2004-12-01</p> <p>For almost two decades both national polls and in-depth studies of global warming perceptions have shown that people commonly conflate <span class="hlt">weather</span> and global climate change. Not only are current <span class="hlt">weather</span> events such as anecdotal heat waves, droughts or cold spells treated as evidence for or against global warming, but <span class="hlt">weather</span> changes such as warmer <span class="hlt">weather</span> and increased storm intensity and frequency are the consequences most likely to come to mind. Distinguishing <span class="hlt">weather</span> from climate remains a challenge for many. This <span class="hlt">weather</span> 'framing' of global warming may inhibit behavioral and policy change in several ways. <span class="hlt">Weather</span> is understood as natural, on an immense scale that makes controlling it difficult to conceive. Further, these attributes contribute to perceptions that global warming, like <span class="hlt">weather</span>, is uncontrollable. This talk presents an analysis of data from public opinion polls, focus groups, and cognitive studies regarding people's mental <span class="hlt">models</span> of and 'frames' for global warming and climate change, and the role <span class="hlt">weather</span> plays in these. This research suggests that priming people with a <span class="hlt">model</span> of global warming as being caused by a "thickening blanket of carbon dioxide" that "traps heat" in the atmosphere solves some of these communications problems and makes it more likely that people will support policies to address global warming.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://eric.ed.gov/?q=solar+AND+radiation&pg=6&id=ED087622','ERIC'); return false;" href="https://eric.ed.gov/?q=solar+AND+radiation&pg=6&id=ED087622"><span>Winds and <span class="hlt">Weather</span>, Teacher's Edition. Probing the Natural World/3.</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>Florida State Univ., Tallahassee. Dept. of Science Education.</p> <p></p> <p>The teacher's edtion for the Intermediate Science Curriculum Study Level III unit entitled "Winds and <span class="hlt">Weather</span>" provides instructions for teachers for examining some principles underlying thermal convention, <span class="hlt">weather</span> observation, closed <span class="hlt">systems</span>, moisture and cloud formation, the heated-air <span class="hlt">model</span>, and fronts. A brief introduction dealing…</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2010SPIE.7692E..02C','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2010SPIE.7692E..02C"><span>All <span class="hlt">weather</span> collision avoidance for unmanned aircraft <span class="hlt">systems</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Contarino, Mark</p> <p>2010-04-01</p> <p>For decades, military and other national security agencies have been denied unfettered access to the National Air Space (NAS) because their unmanned aircraft lack a highly reliable and effective collision avoidance capability. The controlling agency, the Federal Aviation Administration, justifiably demands "no harm" to the safety of the NAS. To overcome the constraints imposed on Unmanned Aircraft <span class="hlt">Systems</span> (UAS) use of the NAS, a new, complex, conformable collision avoidance <span class="hlt">system</span> has been developed - one that will be effective in all flyable <span class="hlt">weather</span> conditions, overcoming the shortfalls of other sensing <span class="hlt">systems</span>, including radar, lidar, acoustic, EO/IR, etc., while meeting form factor and cost criteria suitable for Tier II UAS operations. The <span class="hlt">system</span> also targets Tier I as an ultimate goal, understanding the operational limitations of the smallest UASs may require modification of the design that is suitable for Tier II and higher. The All <span class="hlt">Weather</span> Sense and Avoid <span class="hlt">System</span> (AWSAS) takes into account the FAA's plan to incorporate ADS-B (out) for all aircraft by 2020, and it is intended to make collision avoidance capability available for UAS entry into the NAS as early as 2013. When approved, UASs can fly mission or training flights in the NAS free of the constraints presently in place. Upon implementation this <span class="hlt">system</span> will achieve collision avoidance capability for UASs deployed for national security purposes and will allow expansion of UAS usage for commercial or other civil purposes.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2010cosp...38.4166G','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2010cosp...38.4166G"><span>The Space <span class="hlt">Weather</span> <span class="hlt">Modeling</span> Framework (SWMF): <span class="hlt">Models</span> and Validation</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Gombosi, Tamas; Toth, Gabor; Sokolov, Igor; de Zeeuw, Darren; van der Holst, Bart; Ridley, Aaron; Manchester, Ward, IV</p> <p></p> <p>In the last decade our group at the Center for Space Environment <span class="hlt">Modeling</span> (CSEM) has developed the Space <span class="hlt">Weather</span> <span class="hlt">Modeling</span> Framework (SWMF) that efficiently couples together different <span class="hlt">models</span> describing the interacting regions of the space environment. Many of these domain <span class="hlt">models</span> (such as the global solar corona, the inner heliosphere or the global magneto-sphere) are based on MHD and are represented by our multiphysics code, BATS-R-US. SWMF is a powerful tool for coupling regional <span class="hlt">models</span> describing the space environment from the solar photosphere to the bottom of the ionosphere. Presently, SWMF contains over a dozen components: the solar corona (SC), eruptive event generator (EE), inner heliosphere (IE), outer heliosphere (OH), solar energetic particles (SE), global magnetosphere (GM), inner magnetosphere (IM), radiation belts (RB), plasmasphere (PS), ionospheric electrodynamics (IE), polar wind (PW), upper atmosphere (UA) and lower atmosphere (LA). This talk will present an overview of SWMF, new results obtained with improved physics as well as some validation studies.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/19850009758','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/19850009758"><span>The Altitude Wind Tunnel (AWT): A unique facility for propulsion <span class="hlt">system</span> and adverse <span class="hlt">weather</span> testing</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Chamberlin, R.</p> <p>1985-01-01</p> <p>A need has arisen for a new wind tunnel facility with unique capabilities for testing propulsion <span class="hlt">systems</span> and for conducting research in adverse <span class="hlt">weather</span> conditions. New propulsion <span class="hlt">system</span> concepts, new aircraft configurations with an unprecedented degree of propulsion <span class="hlt">system</span>/aircraft integration, and requirements for aircraft operation in adverse <span class="hlt">weather</span> dictate the need for a new test facility. Required capabilities include simulation of both altitude pressure and temperature, large size, full subsonic speed range, propulsion <span class="hlt">system</span> operation, and <span class="hlt">weather</span> simulation (i.e., icing, heavy rain). A cost effective rehabilitation of the NASA Lewis Research Center's Altitude Wind Tunnel (AWT) will provide a facility with all these capabilities.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017AGUFM.A13L..01C','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017AGUFM.A13L..01C"><span>Improving Air Quality (and <span class="hlt">Weather</span>) Predictions using Advanced Data Assimilation Techniques Applied to Coupled <span class="hlt">Models</span> during KORUS-AQ</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Carmichael, G. R.; Saide, P. E.; Gao, M.; Streets, D. G.; Kim, J.; Woo, J. H.</p> <p>2017-12-01</p> <p>Ambient aerosols are important air pollutants with direct impacts on human health and on the Earth's <span class="hlt">weather</span> and climate <span class="hlt">systems</span> through their interactions with radiation and clouds. Their role is dependent on their distributions of size, number, phase and composition, which vary significantly in space and time. There remain large uncertainties in simulated aerosol distributions due to uncertainties in emission estimates and in chemical and physical processes associated with their formation and removal. These uncertainties lead to large uncertainties in <span class="hlt">weather</span> and air quality predictions and in estimates of health and climate change impacts. Despite these uncertainties and challenges, regional-scale coupled chemistry-meteorological <span class="hlt">models</span> such as WRF-Chem have significant capabilities in predicting aerosol distributions and explaining aerosol-<span class="hlt">weather</span> interactions. We explore the hypothesis that new advances in on-line, coupled atmospheric chemistry/meteorological <span class="hlt">models</span>, and new emission inversion and data assimilation techniques applicable to such coupled <span class="hlt">models</span>, can be applied in innovative ways using current and evolving observation <span class="hlt">systems</span> to improve predictions of aerosol distributions at regional scales. We investigate the impacts of assimilating AOD from geostationary satellite (GOCI) and surface PM2.5 measurements on predictions of AOD and PM in Korea during KORUS-AQ through a series of experiments. The results suggest assimilating datasets from multiple platforms can improve the predictions of aerosol temporal and spatial distributions.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2013enss.confE.130M','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2013enss.confE.130M"><span>Innovative Near Real-Time Data Dissemination Tools Developed by the Space <span class="hlt">Weather</span> Research Center</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Maddox, Marlo M.; Mullinix, Richard; Mays, M. Leila; Kuznetsova, Maria; Zheng, Yihua; Pulkkinen, Antti; Rastaetter, Lutz</p> <p>2013-03-01</p> <p>Access to near real-time and real-time space <span class="hlt">weather</span> data is essential to accurately specifying and forecasting the space environment. The Space <span class="hlt">Weather</span> Research Center at NASA Goddard Space Flight Center's Space <span class="hlt">Weather</span> Laboratory provides vital space <span class="hlt">weather</span> forecasting services primarily to NASA robotic mission operators, as well as external space <span class="hlt">weather</span> stakeholders including the Air Force <span class="hlt">Weather</span> Agency. A key component in this activity is the iNtegrated Space <span class="hlt">Weather</span> Analysis <span class="hlt">System</span> which is a joint development project at NASA GSFC between the Space <span class="hlt">Weather</span> Laboratory, Community Coordinated <span class="hlt">Modeling</span> Center, Applied Engineering & Technology Directorate, and NASA HQ Office Of Chief Engineer. The iSWA <span class="hlt">system</span> was developed to address technical challenges in acquiring and disseminating space <span class="hlt">weather</span> environment information. A key design driver for the iSWA <span class="hlt">system</span> was to generate and present vast amounts of space <span class="hlt">weather</span> resources in an intuitive, user-configurable, and adaptable format - thus enabling users to respond to current and future space <span class="hlt">weather</span> impacts as well as enabling post-impact analysis. Having access to near real-time and real-time data is essential to not only ensuring that relevant observational data is available for analysis - but also in ensuring that <span class="hlt">models</span> can be driven with the requisite input parameters at proper and efficient temporal and spacial resolutions. The iSWA <span class="hlt">system</span> currently manages over 300 unique near-real and real-time data feeds from various sources consisting of both observational and simulation data. A comprehensive suite of actionable space <span class="hlt">weather</span> analysis tools and products are generated and provided utilizing a mixture of the ingested data - enabling new capabilities in quickly assessing past, present, and expected space <span class="hlt">weather</span> effects. This paper will highlight current and future iSWA <span class="hlt">system</span> capabilities including the utilization of data from the Solar Dynamics Observatory mission. http://iswa.gsfc.nasa.gov/</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://ntrs.nasa.gov/search.jsp?R=20080013606&hterms=seasonal+forecast&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D30%26Ntt%3Dseasonal%2Bforecast','NASA-TRS'); return false;" href="https://ntrs.nasa.gov/search.jsp?R=20080013606&hterms=seasonal+forecast&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D30%26Ntt%3Dseasonal%2Bforecast"><span>Application of the NASA A-Train to Evaluate Clouds Simulated by the <span class="hlt">Weather</span> Research and Forecast <span class="hlt">Model</span></span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Molthan, Andrew L.; Jedlovec, Gary J.; Lapenta, William M.</p> <p>2008-01-01</p> <p>The CloudSat Mission, part of the NASA A-Train, is providing the first global survey of cloud profiles and cloud physical properties, observing seasonal and geographical variations that are pertinent to evaluating the way clouds are parameterized in <span class="hlt">weather</span> and climate forecast <span class="hlt">models</span>. CloudSat measures the vertical structure of clouds and precipitation from space through the Cloud Profiling Radar (CPR), a 94 GHz nadir-looking radar measuring the power backscattered by clouds as a function of distance from the radar. One of the goals of the CloudSat mission is to evaluate the representation of clouds in forecast <span class="hlt">models</span>, thereby contributing to improved predictions of <span class="hlt">weather</span>, climate and the cloud-climate feedback problem. This paper highlights potential limitations in cloud microphysical schemes currently employed in the <span class="hlt">Weather</span> Research and Forecast (WRF) <span class="hlt">modeling</span> <span class="hlt">system</span>. The horizontal and vertical structure of explicitly simulated cloud fields produced by the WRF <span class="hlt">model</span> at 4-km resolution are being evaluated using CloudSat observations in concert with products derived from MODIS and AIRS. A radiative transfer <span class="hlt">model</span> is used to produce simulated profiles of radar reflectivity given WRF input profiles of hydrometeor mixing ratios and ambient atmospheric conditions. The preliminary results presented in the paper will compare simulated and observed reflectivity fields corresponding to horizontal and vertical cloud structures associated with midlatitude cyclone events.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2013EGUGA..1513747M','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2013EGUGA..1513747M"><span><span class="hlt">Modelling</span> two-way interactions between atmospheric pollution and <span class="hlt">weather</span> using high-resolution GEM-MACH</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Makar, Paul; Gong, Wanmin; Pabla, Balbir; Cheung, Philip; Milbrandt, Jason; Gravel, Sylvie; Moran, Michael; Gilbert, Samuel; Zhang, Junhua; Zheng, Qiong</p> <p>2013-04-01</p> <p>The Global Environmental Multiscale (GEM) <span class="hlt">model</span> is the source of the Canadian government's operational numerical <span class="hlt">weather</span> forecast guidance, and GEM-MACH is the Canadian operational air-quality forecast <span class="hlt">model</span>. GEM-MACH comprises GEM and the '<span class="hlt">Modelling</span> Air-quality and Chemistry' module, a gas-phase, aqueous-phase and aerosol chemistry and microphysics subroutine package called from within GEM's physics module. The present operational GEM-MACH <span class="hlt">model</span> is "on-line" (both chemistry and meteorology are part of the same <span class="hlt">modelling</span> structure) but is not fully coupled (<span class="hlt">weather</span> variables are provided as inputs to the chemistry, but the chemical variables are not used to modify the <span class="hlt">weather</span>). In this work, we describe modifications made to GEM-MACH as part of the 2nd phase of the Air Quality <span class="hlt">Model</span> Evaluation International Initiative, in order to bring the <span class="hlt">model</span> to a fully coupled status and present the results of initial tests comparing uncoupled and coupled versions of the <span class="hlt">model</span> to observations for a high-resolution forecasting <span class="hlt">system</span>. Changes to GEM's cloud microphysics and radiative transfer packages were carried out to allow two-way coupling. The cloud microphysics package used here is the Milbrandt-Yau 2-moment (MY2) bulk microphysics scheme, which solves prognostic equations for the total droplet number concentration and the mass mixing ratios of six hydrometeor categories. Here, we have replaced the original cloud condensation nucleation parameterization of MY2 (empirically relating supersaturation and CCN number) with the aerosol activation scheme of Abdul-Razzak and Ghan (2002). The latter scheme makes use of the particle size and speciation distribution of GEM-MACH's chemistry code as well as meteorological inputs to predict the number of aerosol particles activated to form cloud droplets, which is then used in the MY2 microphysics. The radiative transfer routines of GEM assume a default constant concentration aerosol profile between the surface and 1500m, and a single</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/18460387','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/18460387"><span>Studying the effect of <span class="hlt">weather</span> conditions on daily crash counts using a discrete time-series <span class="hlt">model</span>.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Brijs, Tom; Karlis, Dimitris; Wets, Geert</p> <p>2008-05-01</p> <p>In previous research, significant effects of <span class="hlt">weather</span> conditions on car crashes have been found. However, most studies use monthly or yearly data and only few studies are available analyzing the impact of <span class="hlt">weather</span> conditions on daily car crash counts. Furthermore, the studies that are available on a daily level do not explicitly <span class="hlt">model</span> the data in a time-series context, hereby ignoring the temporal serial correlation that may be present in the data. In this paper, we introduce an integer autoregressive <span class="hlt">model</span> for <span class="hlt">modelling</span> count data with time interdependencies. The <span class="hlt">model</span> is applied to daily car crash data, metereological data and traffic exposure data from the Netherlands aiming at examining the risk impact of <span class="hlt">weather</span> conditions on the observed counts. The results show that several assumptions related to the effect of <span class="hlt">weather</span> conditions on crash counts are found to be significant in the data and that if serial temporal correlation is not accounted for in the <span class="hlt">model</span>, this may produce biased 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_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('http://adsabs.harvard.edu/abs/2017AGUFMPP31A1264N','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017AGUFMPP31A1264N"><span>Reconstruction of Historical <span class="hlt">Weather</span> by Assimilating Old <span class="hlt">Weather</span> Diary Data</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Neluwala, P.; Yoshimura, K.; Toride, K.; Hirano, J.; Ichino, M.; Okazaki, A.</p> <p>2017-12-01</p> <p>Climate can control not only human life style but also other living beings. It is important to investigate historical climate to understand the current and future climates. Information about daily <span class="hlt">weather</span> can give a better understanding of past life on earth. Long-term <span class="hlt">weather</span> influences crop calendar as well as the development of civilizations. Unfortunately, existing reconstructed daily <span class="hlt">weather</span> data are limited to 1850s due to the availability of instrumental data. The climate data prior to that are derived from proxy materials (e.g., tree-ring width, ice core isotopes, etc.) which are either in annual or decadal scale. However, there are many historical documents which contain information about <span class="hlt">weather</span> such as personal diaries. In Japan, around 20 diaries in average during the 16th - 19th centuries have been collected and converted into a digitized form. As such, diary data exist in many other countries. This study aims to reconstruct historical daily <span class="hlt">weather</span> during the 18th and 19th centuries using personal daily diaries which have analogue <span class="hlt">weather</span> descriptions such as `cloudy' or `sunny'. A recent study has shown the possibility of assimilating coarse <span class="hlt">weather</span> data using idealized experiments. We further extend this study by assimilating modern <span class="hlt">weather</span> descriptions similar to diary data in recent periods. The Global Spectral <span class="hlt">model</span> (GSM) of National Centers for Environmental Prediction (NCEP) is used to reconstruct <span class="hlt">weather</span> with the Local Ensemble Kalman filter (LETKF). Descriptive data are first converted to <span class="hlt">model</span> variables such as total cloud cover (TCC), solar radiation and precipitation using empirical relationships. Those variables are then assimilated on a daily basis after adding random errors to consider the uncertainty of actual diary data. The assimilation of downward short wave solar radiation using <span class="hlt">weather</span> descriptions improves RMSE from 64.3 w/m2 to 33.0 w/m2 and correlation coefficient (R) from 0.5 to 0.8 compared with the case without any</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2015AGUFM.H42D..01P','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2015AGUFM.H42D..01P"><span>Integrated Information <span class="hlt">Systems</span> Across the <span class="hlt">Weather</span>-Climate Continuum</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Pulwarty, R. S.; Higgins, W.; Nierenberg, C.; Trtanj, J.</p> <p>2015-12-01</p> <p>The increasing demand for well-organized (integrated) end-to-end research-based information has been highlighted in several National Academy studies, in IPCC Reports (such as the SREX and Fifth Assessment) and by public and private constituents. Such information constitutes a significant component of the "environmental intelligence" needed to address myriad societal needs for early warning and resilience across the <span class="hlt">weather</span>-climate continuum. The next generation of climate research in service to the nation requires an even more visible, authoritative and robust commitment to scientific integration in support of adaptive information <span class="hlt">systems</span> that address emergent risks and inform longer-term resilience strategies. A proven mechanism for resourcing such requirements is to demonstrate vision, purpose, support, connection to constituencies, and prototypes of desired capabilities. In this presentation we will discuss efforts at NOAA, and elsewhere, that: Improve information on how changes in extremes in key phenomena such as drought, floods, and heat stress impact management decisions for resource planning and disaster risk reduction Develop regional integrated information <span class="hlt">systems</span> to address these emergent challenges, that integrate observations, monitoring and prediction, impacts assessments and scenarios, preparedness and adaptation, and coordination and capacity-building. Such <span class="hlt">systems</span>, as illustrated through efforts such as NIDIS, have strengthened the integration across the foundational research enterprise (through for instance, RISAs, <span class="hlt">Modeling</span> Analysis Predictions and Projections) by increasing agility for responding to emergent risks. The recently- initiated Climate Services Information <span class="hlt">System</span>, in support of the WMO Global Framework for Climate Services draws on the above <span class="hlt">models</span> and will be introduced during the presentation.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2015AGUFMSM13F..07W','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2015AGUFMSM13F..07W"><span>Nowcasting Ground Magnetic Perturbations with the Space <span class="hlt">Weather</span> <span class="hlt">Modeling</span> Framework</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Welling, D. T.; Toth, G.; Singer, H. J.; Millward, G. H.; Gombosi, T. I.</p> <p>2015-12-01</p> <p>Predicting ground-based magnetic perturbations is a critical step towards specifying and predicting geomagnetically induced currents (GICs) in high voltage transmission lines. Currently, the Space <span class="hlt">Weather</span> <span class="hlt">Modeling</span> Framework (SWMF), a flexible <span class="hlt">modeling</span> framework for simulating the multi-scale space environment, is being transitioned from research to operational use (R2O) by NOAA's Space <span class="hlt">Weather</span> Prediction Center. Upon completion of this transition, the SWMF will provide localized B/t predictions using real-time solar wind observations from L1 and the F10.7 proxy for EUV as <span class="hlt">model</span> input. This presentation describes the operational SWMF setup and summarizes the changes made to the code to enable R2O progress. The framework's algorithm for calculating ground-based magnetometer observations will be reviewed. Metrics from data-<span class="hlt">model</span> comparisons will be reviewed to illustrate predictive capabilities. Early data products, such as regional-K index and grids of virtual magnetometer stations, will be presented. Finally, early successes will be shared, including the code's ability to reproduce the recent March 2015 St. Patrick's Day Storm.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017AGUFMIN51D0044N','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017AGUFMIN51D0044N"><span>Preparing for Operational Use of High Priority Products from the Joint Polar Satellite <span class="hlt">System</span> (JPSS) in Numerical <span class="hlt">Weather</span> Prediction</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Nandi, S.; Layns, A. L.; Goldberg, M.; Gambacorta, A.; Ling, Y.; Collard, A.; Grumbine, R. W.; Sapper, J.; Ignatov, A.; Yoe, J. G.</p> <p>2017-12-01</p> <p>This work describes end to end operational implementation of high priority products from National Oceanic and Atmospheric Administration's (NOAA) operational polar-orbiting satellite constellation, to include Suomi National Polar-orbiting Partnership (S-NPP) and the Joint Polar Satellite <span class="hlt">System</span> series initial satellite (JPSS-1), into numerical <span class="hlt">weather</span> prediction and earth <span class="hlt">systems</span> <span class="hlt">models</span>. Development and evaluation needed for the initial implementations of VIIRS Environmental Data Records (EDR) for Sea Surface Temperature ingestion in the Real-Time Global Sea Surface Temperature Analysis (RTG) and Polar Winds assimilated in the National <span class="hlt">Weather</span> Service (NWS) Global Forecast <span class="hlt">System</span> (GFS) is presented. These implementations ensure continuity of data in these <span class="hlt">models</span> in the event of loss of legacy sensor data. Also discussed is accelerated operational implementation of Advanced Technology Microwave Sounder (ATMS) Temperature Data Records (TDR) and Cross-track Infrared Sounder (CrIS) Sensor Data Records, identified as Key Performance Parameters by the National <span class="hlt">Weather</span> Service. Operational use of SNPP after 28 October, 2011 launch took more than one year due to the learning curve and development needed for full exploitation of new remote sensing capabilities. Today, ATMS and CrIS data positively impact <span class="hlt">weather</span> forecast accuracy. For NOAA's JPSS initial satellite (JPSS-1), scheduled for launch in late 2017, we identify scope and timelines for pre-launch and post-launch activities needed to efficiently transition these capabilities into operations. As part of these alignment efforts, operational readiness for KPPs will be possible as soon as 90 days after launch. The schedule acceleration is possible because of the experience with S-NPP. NOAA operational polar-orbiting satellite constellation provides continuity and enhancement of earth <span class="hlt">systems</span> observations out to 2036. Program best practices and lessons learned will inform future implementation for follow-on JPSS-3 and -4</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2011Icar..211..504W','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2011Icar..211..504W"><span>Asteroid age distributions determined by space <span class="hlt">weathering</span> and collisional evolution <span class="hlt">models</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Willman, Mark; Jedicke, Robert</p> <p>2011-01-01</p> <p>We provide evidence of consistency between the dynamical evolution of main belt asteroids and their color evolution due to space <span class="hlt">weathering</span>. The dynamical age of an asteroid's surface (Bottke, W.F., Durda, D.D., Nesvorný, D., Jedicke, R., Morbidelli, A., Vokrouhlický, D., Levison, H. [2005]. Icarus 175 (1), 111-140; Nesvorný, D., Jedicke, R., Whiteley, R.J., Ivezić, Ž. [2005]. Icarus 173, 132-152) is the time since its last catastrophic disruption event which is a function of the object's diameter. The age of an S-complex asteroid's surface may also be determined from its color using a space <span class="hlt">weathering</span> <span class="hlt">model</span> (e.g. Willman, M., Jedicke, R., Moskovitz, N., Nesvorný, D., Vokrouhlický, D., Mothé-Diniz, T. [2010]. Icarus 208, 758-772; Jedicke, R., Nesvorný, D., Whiteley, R.J., Ivezić, Ž., Jurić, M. [2004]. Nature 429, 275-277; Willman, M., Jedicke, R., Nesvorny, D., Moskovitz, N., Ivezić, Ž., Fevig, R. [2008]. Icarus 195, 663-673. We used a sample of 95 S-complex asteroids from SMASS and obtained their absolute magnitudes and u, g, r, i, z filter magnitudes from SDSS. The absolute magnitudes yield a size-derived age distribution. The u, g, r, i, z filter magnitudes lead to the principal component color which yields a color-derived age distribution by inverting our color-age relationship, an enhanced version of the 'dual τ' space <span class="hlt">weathering</span> <span class="hlt">model</span> of Willman et al. (2010). We fit the size-age distribution to the enhanced dual τ <span class="hlt">model</span> and found characteristic <span class="hlt">weathering</span> and gardening times of τw = 2050 ± 80 Myr and τg=4400-500+700Myr respectively. The fit also suggests an initial principal component color of -0.05 ± 0.01 for fresh asteroid surface with a maximum possible change of the probable color due to <span class="hlt">weathering</span> of Δ PC = 1.34 ± 0.04. Our predicted color of fresh asteroid surface matches the color of fresh ordinary chondritic surface of PC1 = 0.17 ± 0.39.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2016EGUGA..18.4525B','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2016EGUGA..18.4525B"><span>Toward seamless <span class="hlt">weather</span>-climate and environmental prediction</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Brunet, Gilbert</p> <p>2016-04-01</p> <p>Over the last decade or so, predicting the <span class="hlt">weather</span>, climate and atmospheric composition has emerged as one of the most important areas of scientific endeavor. This is partly because the remarkable increase in skill of current <span class="hlt">weather</span> forecasts has made society more and more dependent on them day to day for a whole range of decision making. And it is partly because climate change is now widely accepted and the realization is growing rapidly that it will affect every person in the world profoundly, either directly or indirectly. One of the important endeavors of our societies is to remain at the cutting-edge of <span class="hlt">modelling</span> and predicting the evolution of the fully coupled environmental <span class="hlt">system</span>: atmosphere (<span class="hlt">weather</span> and composition), oceans, land surface (physical and biological), and cryosphere. This effort will provide an increasingly accurate and reliable service across all the socio-economic sectors that are vulnerable to the effects of adverse <span class="hlt">weather</span> and climatic conditions, whether now or in the future. This emerging challenge was at the center of the World <span class="hlt">Weather</span> Open Science Conference (Montreal, 2014).The outcomes of the conference are described in the World Meteorological Organization (WMO) book: Seamless Prediction of the Earth <span class="hlt">System</span>: from Minutes to Months, (G. Brunet, S. Jones, P. Ruti Eds., WMO-No. 1156, 2015). It is freely available on line at the WMO website. We will discuss some of the outcomes of the conference for the WMO World <span class="hlt">Weather</span> Research Programme (WWRP) and Global Atmospheric Watch (GAW) long term goals and provide examples of seamless <span class="hlt">modelling</span> and prediction across a range of timescales at convective and sub-kilometer scales for regional coupled forecasting applications at Environment and Climate Change Canada (ECCC).</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2014EGUGA..16.1741A','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2014EGUGA..16.1741A"><span>Employing Tropospheric Numerical <span class="hlt">Weather</span> Prediction <span class="hlt">Model</span> for High-Precision GNSS Positioning</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Alves, Daniele; Gouveia, Tayna; Abreu, Pedro; Magário, Jackes</p> <p>2014-05-01</p> <p>In the past few years is increasing the necessity of realizing high accuracy positioning. In this sense, the spatial technologies have being widely used. The GNSS (Global Navigation Satellite <span class="hlt">System</span>) has revolutionized the geodetic positioning activities. Among the existent methods one can emphasize the Precise Point Positioning (PPP) and network-based positioning. But, to get high accuracy employing these methods, mainly in real time, is indispensable to realize the atmospheric <span class="hlt">modeling</span> (ionosphere and troposphere) accordingly. Related to troposphere, there are the empirical <span class="hlt">models</span> (for example Saastamoinen and Hopfield). But when highly accuracy results (error of few centimeters) are desired, maybe these <span class="hlt">models</span> are not appropriated to the Brazilian reality. In order to minimize this limitation arises the NWP (Numerical <span class="hlt">Weather</span> Prediction) <span class="hlt">models</span>. In Brazil the CPTEC/INPE (Center for <span class="hlt">Weather</span> Prediction and Climate Studies / Brazilian Institute for Spatial Researches) provides a regional NWP <span class="hlt">model</span>, currently used to produce Zenithal Tropospheric Delay (ZTD) predictions (http://satelite.cptec.inpe.br/zenital/). The actual version, called eta15km <span class="hlt">model</span>, has a spatial resolution of 15 km and temporal resolution of 3 hours. In this paper the main goal is to accomplish experiments and analysis concerning the use of troposphere NWP <span class="hlt">model</span> (eta15km <span class="hlt">model</span>) in PPP and network-based positioning. Concerning PPP it was used data from dozens of stations over the Brazilian territory, including Amazon forest. The results obtained with NWP <span class="hlt">model</span> were compared with Hopfield one. NWP <span class="hlt">model</span> presented the best results in all experiments. Related to network-based positioning it was used data from GNSS/SP Network in São Paulo State, Brazil. This network presents the best configuration in the country to realize this kind of positioning. Actually the network is composed by twenty stations (http://www.fct.unesp.br/#!/pesquisa/grupos-de-estudo-e-pesquisa/gege//gnss-sp-network2789/). The</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2014AGUFM.B53D0213M','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2014AGUFM.B53D0213M"><span>Reproducibility of Carbon and Water Cycle by an Ecosystem Process Based <span class="hlt">Model</span> Using a <span class="hlt">Weather</span> Generator and Effect of Temporal Concentration of Precipitation on <span class="hlt">Model</span> Outputs</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Miyauchi, T.; Machimura, T.</p> <p>2014-12-01</p> <p>GCM is generally used to produce input <span class="hlt">weather</span> data for the simulation of carbon and water cycle by ecosystem process based <span class="hlt">models</span> under climate change however its temporal resolution is sometimes incompatible to requirement. A <span class="hlt">weather</span> generator (WG) is used for temporal downscaling of input <span class="hlt">weather</span> data for <span class="hlt">models</span>, where the effect of WG algorithms on reproducibility of ecosystem <span class="hlt">model</span> outputs must be assessed. In this study simulated carbon and water cycle by Biome-BGC <span class="hlt">model</span> using <span class="hlt">weather</span> data measured and generated by CLIMGEN <span class="hlt">weather</span> generator were compared. The measured <span class="hlt">weather</span> data (daily precipitation, maximum, minimum air temperature) at a few sites for 30 years was collected from NNDC Online <span class="hlt">weather</span> data. The generated <span class="hlt">weather</span> data was produced by CLIMGEN parameterized using the measured <span class="hlt">weather</span> data. NPP, heterotrophic respiration (HR), NEE and water outflow were simulated by Biome-BGC using measured and generated <span class="hlt">weather</span> data. In the case of deciduous broad leaf forest in Lushi, Henan Province, China, 30 years average monthly NPP by WG was 10% larger than that by measured <span class="hlt">weather</span> in the growing season. HR by WG was larger than that by measured <span class="hlt">weather</span> in all months by 15% in average. NEE by WG was more negative in winter and was close to that by measured <span class="hlt">weather</span> in summer. These differences in carbon cycle were because the soil water content by WG was larger than that by measured <span class="hlt">weather</span>. The difference between monthly water outflow by WG and by measured <span class="hlt">weather</span> was large and variable, and annual outflow by WG was 50% of that by measured <span class="hlt">weather</span>. The inconsistency in carbon and water cycle by WG and measured <span class="hlt">weather</span> was suggested be affected by the difference in temporal concentration of precipitation, which was assessed.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2014AGUFMGC41B0559C','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2014AGUFMGC41B0559C"><span>National Energy with <span class="hlt">Weather</span> <span class="hlt">System</span> Simultator (NEWS) Sets Bounds on Cost Effective Wind and Solar PV Deployment in the USA without the Use of Storage.</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Clack, C.; MacDonald, A. E.; Alexander, A.; Dunbar, A. D.; Xie, Y.; Wilczak, J. M.</p> <p>2014-12-01</p> <p>The importance of <span class="hlt">weather</span>-driven renewable energies for the United States energy portfolio is growing. The main perceived problems with <span class="hlt">weather</span>-driven renewable energies are their intermittent nature, low power density, and high costs. In 2009, we began a large-scale investigation into the characteristics of <span class="hlt">weather</span>-driven renewables. The project utilized the best available <span class="hlt">weather</span> data assimilation <span class="hlt">model</span> to compute high spatial and temporal resolution power datasets for the renewable resources of wind and solar PV. The <span class="hlt">weather</span> <span class="hlt">model</span> used is the Rapid Update Cycle for the years of 2006-2008. The team also collated a detailed electrical load dataset for the contiguous USA from the Federal Energy Regulatory Commission for the same three-year period. The coincident time series of electrical load and <span class="hlt">weather</span> data allows the possibility of temporally correlated computations for optimal design over large geographic areas. The past two years have seen the development of a cost optimization mathematic <span class="hlt">model</span> that designs electric power <span class="hlt">systems</span>. The <span class="hlt">model</span> plans the <span class="hlt">system</span> and dispatches it on an hourly timescale. The <span class="hlt">system</span> is designed to be reliable, reduce carbon, reduce variability of renewable resources and move the electricity about the whole domain. The <span class="hlt">system</span> built would create the infrastructure needed to reduce carbon emissions to 0 by 2050. The advantages of the <span class="hlt">system</span> is reduced water demain, dual incomes for farmers, jobs for construction of the infrastructure, and price stability for energy. One important simplified test that was run included existing US carbon free power sources, natural gas power when needed, and a High Voltage Direct Current power transmission network. This study shows that the costs and carbon emissions from an optimally designed national <span class="hlt">system</span> decrease with geographic size. It shows that with achievable estimates of wind and solar generation costs, that the US could decrease its carbon emissions by up to 80% by the early 2030s, without an</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2009AGUSMIN32A..01P','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2009AGUSMIN32A..01P"><span>It's All About the Data: Workflow <span class="hlt">Systems</span> and <span class="hlt">Weather</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Plale, B.</p> <p>2009-05-01</p> <p>Digital data is fueling new advances in the computational sciences, particularly geospatial research as environmental sensing grows more practical through reduced technology costs, broader network coverage, and better instruments. e-Science research (i.e., cyberinfrastructure research) has responded to data intensive computing with tools, <span class="hlt">systems</span>, and frameworks that support computationally oriented activities such as <span class="hlt">modeling</span>, analysis, and data mining. Workflow <span class="hlt">systems</span> support execution of sequences of tasks on behalf of a scientist. These <span class="hlt">systems</span>, such as Taverna, Apache ODE, and Kepler, when built as part of a larger cyberinfrastructure framework, give the scientist tools to construct task graphs of execution sequences, often through a visual interface for connecting task boxes together with arcs representing control flow or data flow. Unlike business processing workflows, scientific workflows expose a high degree of detail and control during configuration and execution. Data-driven science imposes unique needs on workflow frameworks. Our research is focused on two issues. The first is the support for workflow-driven analysis over all kinds of data sets, including real time streaming data and locally owned and hosted data. The second is the essential role metadata/provenance collection plays in data driven science, for discovery, determining quality, for science reproducibility, and for long-term preservation. The research has been conducted over the last 6 years in the context of cyberinfrastructure for mesoscale <span class="hlt">weather</span> research carried out as part of the Linked Environments for Atmospheric Discovery (LEAD) project. LEAD has pioneered new approaches for integrating complex <span class="hlt">weather</span> data, assimilation, <span class="hlt">modeling</span>, mining, and cyberinfrastructure <span class="hlt">systems</span>. Workflow <span class="hlt">systems</span> have the potential to generate huge volumes of data. Without some form of automated metadata capture, either metadata description becomes largely a manual task that is difficult if not impossible</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/20120013459','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/20120013459"><span>NASA Space <span class="hlt">Weather</span> Center Services: Potential for Space <span class="hlt">Weather</span> Research</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Zheng, Yihua; Kuznetsova, Masha; Pulkkinen, Antti; Taktakishvili, A.; Mays, M. L.; Chulaki, A.; Lee, H.; Hesse, M.</p> <p>2012-01-01</p> <p>The NASA Space <span class="hlt">Weather</span> Center's primary objective is to provide the latest space <span class="hlt">weather</span> information and forecasting for NASA's robotic missions and its partners and to bring space <span class="hlt">weather</span> knowledge to the public. At the same time, the tools and services it possesses can be invaluable for research purposes. Here we show how our archive and real-time <span class="hlt">modeling</span> of space <span class="hlt">weather</span> events can aid research in a variety of ways, with different classification criteria. We will list and discuss major CME events, major geomagnetic storms, and major SEP events that occurred during the years 2010 - 2012. Highlights of major tools/resources will be provided.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/25350507','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/25350507"><span><span class="hlt">Modeling</span> apple surface temperature dynamics based on <span class="hlt">weather</span> data.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Li, Lei; Peters, Troy; Zhang, Qin; Zhang, Jingjin; Huang, Danfeng</p> <p>2014-10-27</p> <p>The exposure of fruit surfaces to direct sunlight during the summer months can result in sunburn damage. Losses due to sunburn damage are a major economic problem when marketing fresh apples. The objective of this study was to develop and validate a <span class="hlt">model</span> for simulating fruit surface temperature (FST) dynamics based on energy balance and measured <span class="hlt">weather</span> data. A series of <span class="hlt">weather</span> data (air temperature, humidity, solar radiation, and wind speed) was recorded for seven hours between 11:00-18:00 for two months at fifteen minute intervals. To validate the <span class="hlt">model</span>, the FSTs of "Fuji" apples were monitored using an infrared camera in a natural orchard environment. The FST dynamics were measured using a series of thermal images. For the apples that were completely exposed to the sun, the RMSE of the <span class="hlt">model</span> for estimating FST was less than 2.0 °C. A sensitivity analysis of the emissivity of the apple surface and the conductance of the fruit surface to water vapour showed that accurate estimations of the apple surface emissivity were important for the <span class="hlt">model</span>. The validation results showed that the <span class="hlt">model</span> was capable of accurately describing the thermal performances of apples under different solar radiation intensities. Thus, this <span class="hlt">model</span> could be used to more accurately estimate the FST relative to estimates that only consider the air temperature. In addition, this <span class="hlt">model</span> provides useful information for sunburn protection management.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=4279478','PMC'); return false;" href="https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=4279478"><span><span class="hlt">Modeling</span> Apple Surface Temperature Dynamics Based on <span class="hlt">Weather</span> Data</span></a></p> <p><a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pmc">PubMed Central</a></p> <p>Li, Lei; Peters, Troy; Zhang, Qin; Zhang, Jingjin; Huang, Danfeng</p> <p>2014-01-01</p> <p>The exposure of fruit surfaces to direct sunlight during the summer months can result in sunburn damage. Losses due to sunburn damage are a major economic problem when marketing fresh apples. The objective of this study was to develop and validate a <span class="hlt">model</span> for simulating fruit surface temperature (FST) dynamics based on energy balance and measured <span class="hlt">weather</span> data. A series of <span class="hlt">weather</span> data (air temperature, humidity, solar radiation, and wind speed) was recorded for seven hours between 11:00–18:00 for two months at fifteen minute intervals. To validate the <span class="hlt">model</span>, the FSTs of “Fuji” apples were monitored using an infrared camera in a natural orchard environment. The FST dynamics were measured using a series of thermal images. For the apples that were completely exposed to the sun, the RMSE of the <span class="hlt">model</span> for estimating FST was less than 2.0 °C. A sensitivity analysis of the emissivity of the apple surface and the conductance of the fruit surface to water vapour showed that accurate estimations of the apple surface emissivity were important for the <span class="hlt">model</span>. The validation results showed that the <span class="hlt">model</span> was capable of accurately describing the thermal performances of apples under different solar radiation intensities. Thus, this <span class="hlt">model</span> could be used to more accurately estimate the FST relative to estimates that only consider the air temperature. In addition, this <span class="hlt">model</span> provides useful information for sunburn protection management. PMID:25350507</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2012AGUFMED51A0880D','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2012AGUFMED51A0880D"><span>Using Virtualization to Integrate <span class="hlt">Weather</span>, Climate, and Coastal Science Education</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Davis, J. R.; Paramygin, V. A.; Figueiredo, R.; Sheng, Y.</p> <p>2012-12-01</p> <p>To better understand and communicate the important roles of <span class="hlt">weather</span> and climate on the coastal environment, a unique publically available tool is being developed to support research, education, and outreach activities. This tool uses virtualization technologies to facilitate an interactive, hands-on environment in which students, researchers, and general public can perform their own numerical <span class="hlt">modeling</span> experiments. While prior efforts have focused solely on the study of the coastal and estuary environments, this effort incorporates the community supported <span class="hlt">weather</span> and climate <span class="hlt">model</span> (WRF-ARW) into the Coastal Science Educational Virtual Appliance (CSEVA), an education tool used to assist in the learning of coastal transport processes; storm surge and inundation; and evacuation <span class="hlt">modeling</span>. The <span class="hlt">Weather</span> Research and Forecasting (WRF) <span class="hlt">Model</span> is a next-generation, community developed and supported, mesoscale numerical <span class="hlt">weather</span> prediction <span class="hlt">system</span> designed to be used internationally for research, operations, and teaching. It includes two dynamical solvers (ARW - Advanced Research WRF and NMM - Nonhydrostatic Mesoscale <span class="hlt">Model</span>) as well as a data assimilation <span class="hlt">system</span>. WRF-ARW is the ARW dynamics solver combined with other components of the WRF <span class="hlt">system</span> which was developed primarily at NCAR, community support provided by the Mesoscale and Microscale Meteorology (MMM) division of National Center for Atmospheric Research (NCAR). Included with WRF is the WRF Pre-processing <span class="hlt">System</span> (WPS) which is a set of programs to prepare input for real-data simulations. The CSEVA is based on the Grid Appliance (GA) framework and is built using virtual machine (VM) and virtual networking technologies. Virtualization supports integration of an operating <span class="hlt">system</span>, libraries (e.g. Fortran, C, Perl, NetCDF, etc. necessary to build WRF), web server, numerical <span class="hlt">models</span>/grids/inputs, pre-/post-processing tools (e.g. WPS / RIP4 or UPS), graphical user interfaces, "Cloud"-computing infrastructure and other tools into a</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017E%26PSL.457..191H','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017E%26PSL.457..191H"><span>A <span class="hlt">model</span> for late Archean chemical <span class="hlt">weathering</span> and world average river water</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Hao, Jihua; Sverjensky, Dimitri A.; Hazen, Robert M.</p> <p>2017-01-01</p> <p>Interpretations of the geologic record of late Archean near-surface environments depend very strongly on an understanding of <span class="hlt">weathering</span> and resultant riverine transport to the oceans. The late Archean atmosphere is widely recognized to be anoxic (pO2,g =10-5 to 10-13 bars; pH2,g =10-3 to 10-5 bars). Detrital siderite (FeCO3), pyrite (FeS2), and uraninite (UO2) in late Archean sedimentary rocks also suggest anoxic conditions. However, whether the observed detrital minerals could have been thermodynamically stable during <span class="hlt">weathering</span> and riverine transport under such an atmosphere remains untested. Similarly, interpretations of fluctuations recorded by trace metals and isotopes are hampered by a lack of knowledge of the chemical linkages between the atmosphere, <span class="hlt">weathering</span>, riverine transport, and the mineralogical record. In this study, we used theoretical reaction path <span class="hlt">models</span> to simulate the chemistry involved in rainwater and <span class="hlt">weathering</span> processes under present-day and hypothetical Archean atmospheric boundary conditions. We included new estimates of the thermodynamic properties of Fe(II)-smectites as well as smectite and calcite solid solutions. Simulation of present-day <span class="hlt">weathering</span> of basalt + calcite by world-average rainwater produced hematite, kaolinite, Na-Mg-saponite, and chalcedony after 10-4 moles of reactant minerals kg-1 H2O were destroyed. Combination of the resultant water chemistry with results for granitic <span class="hlt">weathering</span> produced a water composition comparable to present-day world average river water (WARW). In contrast, under late Archean atmospheric conditions (pCO2,g =10-1.5 and pH2,g =10-5.0 bars), <span class="hlt">weathering</span> of olivine basalt + calcite to the same degree of reaction produced kaolinite, chalcedony, and Na-Fe(II)-rich-saponite. Late Archean <span class="hlt">weathering</span> of tonalite-trondhjemite-granodiorite (TTG) formed Fe(II)-rich beidellite and chalcedony. Combining the waters from olivine basalt and TTG <span class="hlt">weathering</span> resulted in a <span class="hlt">model</span> for late Archean WARW with the</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.osti.gov/servlets/purl/1127267','SCIGOV-STC'); return false;" href="https://www.osti.gov/servlets/purl/1127267"><span>Using Mesoscale <span class="hlt">Weather</span> <span class="hlt">Model</span> Output as Boundary Conditions for Atmospheric Large-Eddy Simulations and Wind-Plant Aerodynamic Simulations (Presentation)</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>Churchfield, M. J.; Michalakes, J.; Vanderwende, B.</p> <p></p> <p>Wind plant aerodynamics are directly affected by the microscale <span class="hlt">weather</span>, which is directly influenced by the mesoscale <span class="hlt">weather</span>. Microscale <span class="hlt">weather</span> refers to processes that occur within the atmospheric boundary layer with the largest scales being a few hundred meters to a few kilometers depending on the atmospheric stability of the boundary layer. Mesoscale <span class="hlt">weather</span> refers to large <span class="hlt">weather</span> patterns, such as <span class="hlt">weather</span> fronts, with the largest scales being hundreds of kilometers wide. Sometimes microscale simulations that capture mesoscale-driven variations (changes in wind speed and direction over time or across the spatial extent of a wind plant) are important in windmore » plant analysis. In this paper, we present our preliminary work in coupling a mesoscale <span class="hlt">weather</span> <span class="hlt">model</span> with a microscale atmospheric large-eddy simulation <span class="hlt">model</span>. The coupling is one-way beginning with the <span class="hlt">weather</span> <span class="hlt">model</span> and ending with a computational fluid dynamics solver using the <span class="hlt">weather</span> <span class="hlt">model</span> in coarse large-eddy simulation mode as an intermediary. We simulate one hour of daytime moderately convective microscale development driven by the mesoscale data, which are applied as initial and boundary conditions to the microscale domain, at a site in Iowa. We analyze the time and distance necessary for the smallest resolvable microscales to develop.« less</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2010cosp...38.4180W','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2010cosp...38.4180W"><span>The RMI Space <span class="hlt">Weather</span> and Navigation <span class="hlt">Systems</span> (SWANS) Project</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Warnant, Rene; Lejeune, Sandrine; Wautelet, Gilles; Spits, Justine; Stegen, Koen; Stankov, Stan</p> <p></p> <p>The SWANS (Space <span class="hlt">Weather</span> and Navigation <span class="hlt">Systems</span>) research and development project (http://swans.meteo.be) is an initiative of the Royal Meteorological Institute (RMI) under the auspices of the Belgian Solar-Terrestrial Centre of Excellence (STCE). The RMI SWANS objectives are: research on space <span class="hlt">weather</span> and its effects on GNSS applications; permanent mon-itoring of the local/regional geomagnetic and ionospheric activity; and development/operation of relevant nowcast, forecast, and alert services to help professional GNSS/GALILEO users in mitigating space <span class="hlt">weather</span> effects. Several SWANS developments have already been implemented and available for use. The K-LOGIC (Local Operational Geomagnetic Index K Calculation) <span class="hlt">system</span> is a nowcast <span class="hlt">system</span> based on a fully automated computer procedure for real-time digital magnetogram data acquisition, data screening, and calculating the local geomagnetic K index. Simultaneously, the planetary Kp index is estimated from solar wind measurements, thus adding to the service reliability and providing forecast capabilities as well. A novel hybrid empirical <span class="hlt">model</span>, based on these ground-and space-based observations, has been implemented for nowcasting and forecasting the geomagnetic index, issuing also alerts whenever storm-level activity is indicated. A very important feature of the nowcast/forecast <span class="hlt">system</span> is the strict control on the data input and processing, allowing for an immediate assessment of the output quality. The purpose of the LIEDR (Local Ionospheric Electron Density Reconstruction) <span class="hlt">system</span> is to acquire and process data from simultaneous ground-based GNSS TEC and digital ionosonde measurements, and subsequently to deduce the vertical electron density distribution. A key module is the real-time estimation of the ionospheric slab thickness, offering additional infor-mation on the local ionospheric dynamics. The RTK (Real Time Kinematic) status mapping provides a quick look at the small-scale ionospheric effects on the RTK</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017AGUFMPA41A0287P','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017AGUFMPA41A0287P"><span>Using <span class="hlt">Weather</span> Types to Understand and Communicate <span class="hlt">Weather</span> and Climate Impacts</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Prein, A. F.; Hale, B.; Holland, G. J.; Bruyere, C. L.; Done, J.; Mearns, L.</p> <p>2017-12-01</p> <p>A common challenge in atmospheric research is the translation of scientific advancements and breakthroughs to decision relevant and actionable information. This challenge is central to the mission of NCAR's Capacity Center for Climate and <span class="hlt">Weather</span> Extremes (C3WE, www.c3we.ucar.edu). C3WE advances our understanding of <span class="hlt">weather</span> and climate impacts and integrates these advances with distributed information technology to create tools that promote a global culture of resilience to <span class="hlt">weather</span> and climate extremes. Here we will present an interactive web-based tool that connects historic U.S. losses and fatalities from extreme <span class="hlt">weather</span> and climate events to 12 large-scale <span class="hlt">weather</span> types. <span class="hlt">Weather</span> types are dominant <span class="hlt">weather</span> situations such as winter high-pressure <span class="hlt">systems</span> over the U.S. leading to very cold temperatures or summertime moist humid air masses over the central U.S. leading to severe thunderstorms. Each <span class="hlt">weather</span> type has a specific fingerprint of economic losses and fatalities in a region that is quantified. Therefore, <span class="hlt">weather</span> types enable a direct connection of observed or forecasted <span class="hlt">weather</span> situation to loss of life and property. The presented tool allows the user to explore these connections, raise awareness of existing vulnerabilities, and build resilience to <span class="hlt">weather</span> and climate extremes.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/29156311','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/29156311"><span>Impacts from urban water <span class="hlt">systems</span> on receiving waters - How to account for severe wet-<span class="hlt">weather</span> events in LCA?</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Risch, Eva; Gasperi, Johnny; Gromaire, Marie-Christine; Chebbo, Ghassan; Azimi, Sam; Rocher, Vincent; Roux, Philippe; Rosenbaum, Ralph K; Sinfort, Carole</p> <p>2018-01-01</p> <p>Sewage <span class="hlt">systems</span> are a vital part of the urban infrastructure in most cities. They provide drainage, which protects public health, prevents the flooding of property and protects the water environment around urban areas. On some occasions sewers will overflow into the water environment during heavy rain potentially causing unacceptable impacts from releases of untreated sewage into the environment. In typical Life Cycle Assessment (LCA) studies of urban wastewater <span class="hlt">systems</span> (UWS), average dry-<span class="hlt">weather</span> conditions are <span class="hlt">modelled</span> while wet-<span class="hlt">weather</span> flows from UWS, presenting a high temporal variability, are not currently accounted for. In this context, the loads from several storm events could be important contributors to the impact categories freshwater eutrophication and ecotoxicity. In this study we investigated the contributions of these wet-<span class="hlt">weather</span>-induced discharges relative to average dry-<span class="hlt">weather</span> conditions in the life cycle inventory for UWS. In collaboration with the Paris public sanitation service (SIAAP) and Observatory of Urban Pollutants (OPUR) program researchers, this work aimed at identifying and comparing contributing flows from the UWS in the Paris area by a selection of routine wastewater parameters and priority pollutants. This collected data is organized according to archetypal <span class="hlt">weather</span> days during a reference year. Then, for each archetypal <span class="hlt">weather</span> day and its associated flows to the receiving river waters (Seine), the parameters of pollutant loads (statistical distribution of concentrations and volumes) were determined. The resulting inventory flows (i.e. the potential loads from the UWS) were used as LCA input data to assess the associated impacts. This allowed investigating the relative importance of episodic wet-<span class="hlt">weather</span> versus "continuous" dry-<span class="hlt">weather</span> loads with a probabilistic approach to account for pollutant variability within the urban flows. The analysis at the scale of one year showed that storm events are significant contributors to the impacts</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2016Icar..265..161B','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2016Icar..265..161B"><span>Optical space <span class="hlt">weathering</span> on Vesta: Radiative-transfer <span class="hlt">models</span> and Dawn observations</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Blewett, David T.; Denevi, Brett W.; Le Corre, Lucille; Reddy, Vishnu; Schröder, Stefan E.; Pieters, Carle M.; Tosi, Federico; Zambon, Francesca; De Sanctis, Maria Cristina; Ammannito, Eleonora; Roatsch, Thomas; Raymond, Carol A.; Russell, Christopher T.</p> <p>2016-02-01</p> <p>Exposure to ion and micrometeoroid bombardment in the space environment causes physical and chemical changes in the surface of an airless planetary body. These changes, called space <span class="hlt">weathering</span>, can strongly influence a surface's optical characteristics, and hence complicate interpretation of composition from reflectance spectroscopy. Prior work using data from the Dawn spacecraft (Pieters, C.M. et al. [2012]. Nature 491, 79-82) found that accumulation of nanophase metallic iron (npFe0), which is a key space-<span class="hlt">weathering</span> product on the Moon, does not appear to be important on Vesta, and instead regolith evolution is dominated by mixing with carbonaceous chondrite (CC) material delivered by impacts. In order to gain further insight into the nature of space <span class="hlt">weathering</span> on Vesta, we constructed <span class="hlt">model</span> reflectance spectra using Hapke's radiative-transfer theory and used them as an aid to understanding multispectral observations obtained by Dawn's Framing Cameras (FC). The <span class="hlt">model</span> spectra, for a howardite mineral assemblage, include both the effects of npFe0 and that of a mixed CC component. We found that a plot of the 438-nm/555-nm ratio vs. the 555-nm reflectance for the <span class="hlt">model</span> spectra helps to separate the effects of lunar-style space <span class="hlt">weathering</span> (LSSW) from those of CC-mixing. We then constructed ratio-reflectance pixel scatterplots using FC images for four areas of contrasting composition: a eucritic area at Vibidia crater, a diogenitic area near Antonia crater, olivine-bearing material within Bellicia crater, and a light mantle unit (referred to as an ;orange patch; in some previous studies, based on steep spectral slope in the visible) northeast of Oppia crater. In these four cases the observed spectral trends are those expected from CC-mixing, with no evidence for <span class="hlt">weathering</span> dominated by production of npFe0. In order to survey a wider range of surfaces, we also defined a spectral parameter that is a function of the change in 438-nm/555-nm ratio and the 555-nm reflectance</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('https://rosap.ntl.bts.gov/view/dot/8596','DOTNTL'); return false;" href="https://rosap.ntl.bts.gov/view/dot/8596"><span>Establishment and discontinuance criteria for automated <span class="hlt">weather</span> observing <span class="hlt">systems</span> (AWOS)</span></a></p> <p><a target="_blank" href="http://ntlsearch.bts.gov/tris/index.do">DOT National Transportation Integrated Search</a></p> <p></p> <p>1983-05-01</p> <p>This report develops establishment and discontinuance criteria for automated : <span class="hlt">weather</span> observing <span class="hlt">systems</span> (AWOS) for publication in FAA Order 703l.2B, Airway : Planning Standard Number One. Airway Planning Standard Number One contains : the policy and...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://ntrs.nasa.gov/search.jsp?R=19830025560&hterms=aviation+safety&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D60%26Ntt%3Daviation%2Bsafety','NASA-TRS'); return false;" href="https://ntrs.nasa.gov/search.jsp?R=19830025560&hterms=aviation+safety&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D60%26Ntt%3Daviation%2Bsafety"><span>Federal Aviation Administration <span class="hlt">weather</span> program to improve aviation safety</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Wedan, R. W.</p> <p>1983-01-01</p> <p>The implementation of the National Airspace <span class="hlt">System</span> (NAS) will improve safety services to aviation. These services include collision avoidance, improved landing <span class="hlt">systems</span> and better <span class="hlt">weather</span> data acquisition and dissemination. The program to improve the quality of <span class="hlt">weather</span> information includes the following: Radar Remote <span class="hlt">Weather</span> Display <span class="hlt">System</span>; Flight Service Automation <span class="hlt">System</span>; Automatic <span class="hlt">Weather</span> Observation <span class="hlt">System</span>; Center <span class="hlt">Weather</span> Processor, and Next Generation <span class="hlt">Weather</span> Radar Development.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2013AGUFM.A22B..01S','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2013AGUFM.A22B..01S"><span>Probability for <span class="hlt">Weather</span> and Climate</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Smith, L. A.</p> <p>2013-12-01</p> <p>Over the last 60 years, the availability of large-scale electronic computers has stimulated rapid and significant advances both in meteorology and in our understanding of the Earth <span class="hlt">System</span> as a whole. The speed of these advances was due, in large part, to the sudden ability to explore nonlinear <span class="hlt">systems</span> of equations. The computer allows the meteorologist to carry a physical argument to its conclusion; the time scales of <span class="hlt">weather</span> phenomena then allow the refinement of physical theory, numerical approximation or both in light of new observations. Prior to this extension, as Charney noted, the practicing meteorologist could ignore the results of theory with good conscience. Today, neither the practicing meteorologist nor the practicing climatologist can do so, but to what extent, and in what contexts, should they place the insights of theory above quantitative simulation? And in what circumstances can one confidently estimate the probability of events in the world from <span class="hlt">model</span>-based simulations? Despite solid advances of theory and insight made possible by the computer, the fidelity of our <span class="hlt">models</span> of climate differs in kind from the fidelity of <span class="hlt">models</span> of <span class="hlt">weather</span>. While all prediction is extrapolation in time, <span class="hlt">weather</span> resembles interpolation in state space, while climate change is fundamentally an extrapolation. The trichotomy of simulation, observation and theory which has proven essential in meteorology will remain incomplete in climate science. Operationally, the roles of probability, indeed the kinds of probability one has access too, are different in operational <span class="hlt">weather</span> forecasting and climate services. Significant barriers to forming probability forecasts (which can be used rationally as probabilities) are identified. Monte Carlo ensembles can explore sensitivity, diversity, and (sometimes) the likely impact of measurement uncertainty and structural <span class="hlt">model</span> error. The aims of different ensemble strategies, and fundamental differences in ensemble design to support of</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2015APS..APR.L1049D','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2015APS..APR.L1049D"><span>Investigating Anomalies in the Output Generated by the <span class="hlt">Weather</span> Research and Forecasting (WRF) <span class="hlt">Model</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Decicco, Nicholas; Trout, Joseph; Manson, J. Russell; Rios, Manny; King, David</p> <p>2015-04-01</p> <p>The <span class="hlt">Weather</span> Research and Forecasting (WRF) <span class="hlt">model</span> is an advanced mesoscale numerical <span class="hlt">weather</span> prediction (NWP) <span class="hlt">model</span> comprised of two numerical cores, the Numerical Mesoscale <span class="hlt">Modeling</span> (NMM) core, and the Advanced Research WRF (ARW) core. An investigation was done to determine the source of erroneous output generated by the NMM core. In particular were the appearance of zero values at regularly spaced grid cells in output fields and the NMM core's evident (mis)use of static geographic information at a resolution lower than the nesting level for which the core is performing computation. A brief discussion of the high-level modular architecture of the <span class="hlt">model</span> is presented as well as methods utilized to identify the cause of these problems. Presented here are the initial results from a research grant, ``A Pilot Project to Investigate Wake Vortex Patterns and <span class="hlt">Weather</span> Patterns at the Atlantic City Airport by the Richard Stockton College of NJ and the FAA''.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2015AMTD....810179L','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2015AMTD....810179L"><span><span class="hlt">Modeling</span> the Zeeman effect in high altitude SSMIS channels for numerical <span class="hlt">weather</span> prediction profiles: comparing a fast <span class="hlt">model</span> and a line-by-line <span class="hlt">model</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Larsson, R.; Milz, M.; Rayer, P.; Saunders, R.; Bell, W.; Booton, A.; Buehler, S. A.; Eriksson, P.; John, V.</p> <p>2015-10-01</p> <p>We present a comparison of a reference and a fast radiative transfer <span class="hlt">model</span> using numerical <span class="hlt">weather</span> prediction profiles for the Zeeman-affected high altitude Special Sensor Microwave Imager/Sounder channels 19-22. We find that the <span class="hlt">models</span> agree well for channels 21 and 22 compared to the channels' <span class="hlt">system</span> noise temperatures (1.9 and 1.3 K, respectively) and the expected profile errors at the affected altitudes (estimated to be around 5 K). For channel 22 there is a 0.5 K average difference between the <span class="hlt">models</span>, with a standard deviation of 0.24 K for the full set of atmospheric profiles. Same channel, there is 1.2 K in average between the fast <span class="hlt">model</span> and the sensor measurement, with 1.4 K standard deviation. For channel 21 there is a 0.9 K average difference between the <span class="hlt">models</span>, with a standard deviation of 0.56 K. Same channel, there is 1.3 K in average between the fast <span class="hlt">model</span> and the sensor measurement, with 2.4 K standard deviation. We consider the relatively small <span class="hlt">model</span> differences as a validation of the fast Zeeman effect scheme for these channels. Both channels 19 and 20 have smaller average differences between the <span class="hlt">models</span> (at below 0.2 K) and smaller standard deviations (at below 0.4 K) when both <span class="hlt">models</span> use a two-dimensional magnetic field profile. However, when the reference <span class="hlt">model</span> is switched to using a full three-dimensional magnetic field profile, the standard deviation to the fast <span class="hlt">model</span> is increased to almost 2 K due to viewing geometry dependencies causing up to ± 7 K differences near the equator. The average differences between the two <span class="hlt">models</span> remain small despite changing magnetic field configurations. We are unable to compare channels 19 and 20 to sensor measurements due to limited altitude range of the numerical <span class="hlt">weather</span> prediction profiles. We recommended that numerical <span class="hlt">weather</span> prediction software using the fast <span class="hlt">model</span> takes the available fast Zeeman scheme into account for data assimilation of the affected sensor channels to better constrain the upper</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2005AdSpR..36.2231P','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2005AdSpR..36.2231P"><span>Effects of space <span class="hlt">weather</span> on high-latitude ground <span class="hlt">systems</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Pirjola, Risto</p> <p></p> <p>Geomagnetically induced currents (GIC) in technological <span class="hlt">systems</span>, such as power grids, pipelines, cables and railways, are a ground manifestation of space <span class="hlt">weather</span>. The first GIC observations were already made in early telegraph equipment more than 150 years ago. In power networks, GIC may saturate transformers with possible harmful consequences extending even to a collapse of the whole <span class="hlt">system</span> or to permanent damage of transformers. In pipelines, GIC and the associated pipe-to-soil voltages may enhance corrosion or disturb surveys associated with corrosion control. GIC are driven by the geoelectric field induced by a geomagnetic variation at the Earth’s surface. The electric and magnetic fields are primarily produced by ionospheric currents and secondarily affected by the ground conductivity. Of great importance is the auroral electrojet with other rapidly varying currents indicating that GIC are a particular high-latitude problem. In this paper, we summarize the GIC research done in Finland during about 25 years, and discuss the calculation of GIC in a given network. Special attention is paid to <span class="hlt">modelling</span> a power <span class="hlt">system</span>. It is shown that, when considering GIC at a site, it is usually sufficient to take account for a smaller grid in the vicinity of the particular site. <span class="hlt">Modelling</span> GIC also provides a basis for developing forecasting and warning methods of GIC.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2016cosp...41E2121Y','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2016cosp...41E2121Y"><span>Space <span class="hlt">Weather</span> Services of Korea</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Yoon, KiChang; Kim, Jae-Hun; Kim, Young Yun; Kwon, Yongki; Wi, Gwan-sik</p> <p>2016-07-01</p> <p>The Korean Space <span class="hlt">Weather</span> Center (KSWC) of the National Radio Research Agency (RRA) is a government agency which is the official source of space <span class="hlt">weather</span> information for Korean Government and the primary action agency of emergency measure to severe space <span class="hlt">weather</span> condition. KSWC's main role is providing alerts, watches, and forecasts in order to minimize the space <span class="hlt">weather</span> impacts on both of public and commercial sectors of satellites, aviation, communications, navigations, power grids, and etc. KSWC is also in charge of monitoring the space <span class="hlt">weather</span> condition and conducting research and development for its main role of space <span class="hlt">weather</span> operation in Korea. In this study, we will present KSWC's recent efforts on development of application-oriented space <span class="hlt">weather</span> research products and services on user needs, and introduce new international collaborative projects, such as IPS-Driven Enlil <span class="hlt">model</span>, DREAM <span class="hlt">model</span> estimating electron in satellite orbit, global network of DSCOVR and STEREO satellites tracking, and ARMAS (Automated Radiation Measurement for Aviation Safety).</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2016AGUFMSH22B..08Y','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2016AGUFMSH22B..08Y"><span>Space <span class="hlt">Weather</span> Services of Korea</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Yoon, K.; Hong, S.; Jangsuk, C.; Dong Kyu, K.; Jinyee, C.; Yeongoh, C.</p> <p>2016-12-01</p> <p>The Korean Space <span class="hlt">Weather</span> Center (KSWC) of the National Radio Research Agency (RRA) is a government agency which is the official source of space <span class="hlt">weather</span> information for Korean Government and the primary action agency of emergency measure to severe space <span class="hlt">weather</span> condition. KSWC's main role is providing alerts, watches, and forecasts in order to minimize the space <span class="hlt">weather</span> impacts on both of public and commercial sectors of satellites, aviation, communications, navigations, power grids, and etc. KSWC is also in charge of monitoring the space <span class="hlt">weather</span> condition and conducting research and development for its main role of space <span class="hlt">weather</span> operation in Korea. In this study, we will present KSWC's recent efforts on development of application-oriented space <span class="hlt">weather</span> research products and services on user needs, and introduce new international collaborative projects, such as IPS-Driven Enlil <span class="hlt">model</span>, DREAM <span class="hlt">model</span> estimating electron in satellite orbit, global network of DSCOVR and STEREO satellites tracking, and ARMAS (Automated Radiation Measurement for Aviation Safety).</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017AGUFM.H11O..01R','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017AGUFM.H11O..01R"><span>A new precipitation and meteorological drought climatology based on <span class="hlt">weather</span> patterns</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Richardson, D.; Fowler, H. J.; Kilsby, C. G.; Neal, R.</p> <p>2017-12-01</p> <p><span class="hlt">Weather</span>-pattern, or <span class="hlt">weather</span>-type, classifications are a valuable tool in many applications as they characterise the broad-scale atmospheric circulation over a given region. An analysis of regional UK precipitation and meteorological drought climatology with respect to a set of objectively defined <span class="hlt">weather</span> patterns is presented. This classification <span class="hlt">system</span>, introduced last year, is currently being used by the Met Office in several probabilistic forecasting applications driven by ensemble forecasting <span class="hlt">systems</span>. The classification consists of 30 daily patterns derived from North Atlantic Ocean and European mean sea level pressure data. Clustering these 30 patterns yields another set of eight patterns that are intended for use in longer-range applications. <span class="hlt">Weather</span> pattern definitions and daily occurrences are mapped to the commonly-used Lamb <span class="hlt">Weather</span> Types (LWTs), and parallels between the two classifications are drawn. Daily precipitation distributions are associated with each <span class="hlt">weather</span> pattern and LWT. Drought index series are calculated for a range of aggregation periods and seasons. Monthly <span class="hlt">weather</span>-pattern frequency anomalies are calculated for different drought index thresholds, representing dry, wet and drought conditions. The set of 30 <span class="hlt">weather</span> patterns is shown to be adequate for precipitation-based analyses in the UK, although the smaller set of clustered patterns is not. Furthermore, intra-pattern precipitation variability is lower in the new classification compared to the LWTs, which is an advantage in the context of precipitation studies. <span class="hlt">Weather</span> patterns associated with drought over the different UK regions are identified. This has potential forecasting application - if a <span class="hlt">model</span> (e.g. a global seasonal forecast <span class="hlt">model</span>) can predict <span class="hlt">weather</span> pattern occurrences then regional drought outlooks may be derived from the forecasted <span class="hlt">weather</span> patterns.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/19980137407','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/19980137407"><span>The Aviation <span class="hlt">System</span> Analysis Capability Airport Capacity and Delay <span class="hlt">Models</span></span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Lee, David A.; Nelson, Caroline; Shapiro, Gerald</p> <p>1998-01-01</p> <p>The ASAC Airport Capacity <span class="hlt">Model</span> and the ASAC Airport Delay <span class="hlt">Model</span> support analyses of technologies addressing airport capacity. NASA's Aviation <span class="hlt">System</span> Analysis Capability (ASAC) Airport Capacity <span class="hlt">Model</span> estimates the capacity of an airport as a function of <span class="hlt">weather</span>, Federal Aviation Administration (FAA) procedures, traffic characteristics, and the level of technology available. Airport capacity is presented as a Pareto frontier of arrivals per hour versus departures per hour. The ASAC Airport Delay <span class="hlt">Model</span> allows the user to estimate the minutes of arrival delay for an airport, given its (<span class="hlt">weather</span> dependent) capacity. Historical <span class="hlt">weather</span> observations and demand patterns are provided by ASAC as inputs to the delay <span class="hlt">model</span>. The ASAC economic <span class="hlt">models</span> can translate a reduction in delay minutes into benefit dollars.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/20120002541','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/20120002541"><span>Understanding Space <span class="hlt">Weather</span>: The Sun as a Variable Star</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Strong, Keith; Saba, Julia; Kucera, Therese</p> <p>2011-01-01</p> <p>The Sun is a complex <span class="hlt">system</span> of <span class="hlt">systems</span> and until recently, less than half of its surface was observable at any given time and then only from afar. New observational techniques and <span class="hlt">modeling</span> capabilities are giving us a fresh perspective of the solar interior and how our Sun works as a variable star. This revolution in solar observations and <span class="hlt">modeling</span> provides us with the exciting prospect of being able to use a vastly increased stream of solar data taken simultaneously from several different vantage points to produce more reliable and prompt space <span class="hlt">weather</span> forecasts. Solar variations that cause identifiable space <span class="hlt">weather</span> effects do not happen only on solar-cycle timescales from decades to centuries; there are also many shorter-term events that have their own unique space <span class="hlt">weather</span> effects and a different set of challenges to understand and predict, such as flares, coronal mass ejections, and solar wind variations</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/20140006649','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/20140006649"><span>Understanding Space <span class="hlt">Weather</span>: The Sun as a Variable Star</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Strong, Keith; Saba, Julia; Kucera, Therese</p> <p>2012-01-01</p> <p>The Sun is a complex <span class="hlt">system</span> of <span class="hlt">systems</span> and until recently, less than half of its surface was observable at any given time and then only from afar. New observational techniques and <span class="hlt">modeling</span> capabilities are giving us a fresh perspective of the solar interior and how our Sun works as a variable star. This revolution in solar observations and <span class="hlt">modeling</span> provides us with the exciting prospect of being able to use a vastly increased stream of solar data taken simultaneously from several different vantage points to produce more reliable and prompt space <span class="hlt">weather</span> forecasts. Solar variations that cause identifiable space <span class="hlt">weather</span> effects do not happen only on solar-cycle timescales from decades to centuries; there are also many shorter-term events that have their own unique space <span class="hlt">weather</span> effects and a different set of challenges to understand and predict, such as flares, coronal mass ejections, and solar wind variations.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://rosap.ntl.bts.gov/view/dot/14180','DOTNTL'); return false;" href="https://rosap.ntl.bts.gov/view/dot/14180"><span>The Advanced Transportation <span class="hlt">Weather</span> Information <span class="hlt">System</span> (ATWIS)</span></a></p> <p><a target="_blank" href="http://ntlsearch.bts.gov/tris/index.do">DOT National Transportation Integrated Search</a></p> <p></p> <p>2000-01-01</p> <p>Understanding and interpreting <span class="hlt">weather</span> information can be critical to the success of any winter snow and ice removal operation. Knowing when, where and what type of deicing material to use for a particular winter <span class="hlt">weather</span> event can be a challenge to e...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017AGUFMGC13C0798S','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017AGUFMGC13C0798S"><span>Assessing Individual <span class="hlt">Weather</span> Risk-Taking and Its Role in <span class="hlt">Modeling</span> Likelihood of Hurricane Evacuation</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Stewart, A. E.</p> <p>2017-12-01</p> <p>This research focuses upon measuring an individual's level of perceived risk of different severe and extreme <span class="hlt">weather</span> conditions using a new self-report measure, the <span class="hlt">Weather</span> Risk-Taking Scale (WRTS). For 32 severe and extreme situations in which people could perform an unsafe behavior (e. g., remaining outside with lightning striking close by, driving over roadways covered with water, not evacuating ahead of an approaching hurricane, etc.), people rated: 1.their likelihood of performing the behavior, 2. The perceived risk of performing the behavior, 3. the expected benefits of performing the behavior, and 4. whether the behavior has actually been performed in the past. Initial development research with the measure using 246 undergraduate students examined its psychometric properties and found that it was internally consistent (Cronbach's a ranged from .87 to .93 for the four scales) and that the scales possessed good temporal (test-retest) reliability (r's ranged from .84 to .91). A second regression study involving 86 undergraduate students found that taking <span class="hlt">weather</span> risks was associated with having taken similar risks in one's past and with the personality trait of sensation-seeking. Being more attentive to the <span class="hlt">weather</span> and perceiving its risks when it became extreme was associated with lower likelihoods of taking <span class="hlt">weather</span> risks (overall regression <span class="hlt">model</span>, R2adj = 0.60). A third study involving 334 people examined the contributions of <span class="hlt">weather</span> risk perceptions and risk-taking in <span class="hlt">modeling</span> the self-reported likelihood of complying with a recommended evacuation ahead of a hurricane. Here, higher perceptions of hurricane risks and lower perceived benefits of risk-taking along with fear of severe <span class="hlt">weather</span> and hurricane personal self-efficacy ratings were all statistically significant contributors to the likelihood of evacuating ahead of a hurricane. Psychological rootedness and attachment to one's home also tend to predict lack of evacuation. This research highlights the</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/20120004024','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/20120004024"><span>Evaluating the Impacts of NASA/SPoRT Daily Greenness Vegetation Fraction on Land Surface <span class="hlt">Model</span> and Numerical <span class="hlt">Weather</span> Forecasts</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Bell, Jordan R.; Case, Jonathan L.; LaFontaine, Frank J.; Kumar, Sujay V.</p> <p>2012-01-01</p> <p>The NASA Short-term Prediction Research and Transition (SPoRT) Center has developed a Greenness Vegetation Fraction (GVF) dataset, which is updated daily using swaths of Normalized Difference Vegetation Index data from the Moderate Resolution Imaging Spectroradiometer (MODIS) data aboard the NASA EOS Aqua and Terra satellites. NASA SPoRT began generating daily real-time GVF composites at 1-km resolution over the Continental United States (CONUS) on 1 June 2010. The purpose of this study is to compare the National Centers for Environmental Prediction (NCEP) climatology GVF product (currently used in operational <span class="hlt">weather</span> <span class="hlt">models</span>) to the SPoRT-MODIS GVF during June to October 2010. The NASA Land Information <span class="hlt">System</span> (LIS) was employed to study the impacts of the SPoRT-MODIS GVF dataset on a land surface <span class="hlt">model</span> (LSM) apart from a full numerical <span class="hlt">weather</span> prediction (NWP) <span class="hlt">model</span>. For the 2010 warm season, the SPoRT GVF in the western portion of the CONUS was generally higher than the NCEP climatology. The eastern CONUS GVF had variations both above and below the climatology during the period of study. These variations in GVF led to direct impacts on the rates of heating and evaporation from the land surface. In the West, higher latent heat fluxes prevailed, which enhanced the rates of evapotranspiration and soil moisture depletion in the LSM. By late Summer and Autumn, both the average sensible and latent heat fluxes increased in the West as a result of the more rapid soil drying and higher coverage of GVF. The impacts of the SPoRT GVF dataset on NWP was also examined for a single severe <span class="hlt">weather</span> case study using the <span class="hlt">Weather</span> Research and Forecasting (WRF) <span class="hlt">model</span>. Two separate coupled LIS/WRF <span class="hlt">model</span> simulations were made for the 17 July 2010 severe <span class="hlt">weather</span> event in the Upper Midwest using the NCEP and SPoRT GVFs, with all other <span class="hlt">model</span> parameters remaining the same. Based on the sensitivity results, regions with higher GVF in the SPoRT <span class="hlt">model</span> runs had higher evapotranspiration and</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017JOC....38..287N','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017JOC....38..287N"><span>An Analytical Approach for Performance Enhancement of FSO Communication <span class="hlt">System</span> Using Array of Receivers in Adverse <span class="hlt">Weather</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>Nagpal, Shaina; Gupta, Amit</p> <p>2017-08-01</p> <p>Free Space Optics (FSO) link exploits the tremendous network capacity and is capable of offering wireless communications similar to communications through optical fibres. However, FSO link is extremely <span class="hlt">weather</span> dependent and the major effect on FSO links is due to adverse <span class="hlt">weather</span> conditions like fog and snow. In this paper, an FSO link is designed using an array of receivers. The disparity of the link for very high attenuation conditions due to fog and snow is analysed using aperture averaging technique. Further effect of aperture averaging technique is investigated by comparing the <span class="hlt">systems</span> using aperture averaging technique with <span class="hlt">systems</span> not using aperture averaging technique. The performance of proposed <span class="hlt">model</span> of FSO link has been evaluated in terms of Q factor, bit error rate (BER) and eye diagram.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://rosap.ntl.bts.gov/view/dot/34408','DOTNTL'); return false;" href="https://rosap.ntl.bts.gov/view/dot/34408"><span>Caltrans <span class="hlt">Weather</span>Share Phase II <span class="hlt">System</span>: An Application of <span class="hlt">Systems</span> and Software Engineering Process to Project Development</span></a></p> <p><a target="_blank" href="http://ntlsearch.bts.gov/tris/index.do">DOT National Transportation Integrated Search</a></p> <p></p> <p>2009-08-25</p> <p>In cooperation with the California Department of Transportation, Montana State University's Western Transportation Institute has developed the <span class="hlt">Weather</span>Share Phase II <span class="hlt">system</span> by applying <span class="hlt">Systems</span> Engineering and Software Engineering processes. The <span class="hlt">system</span>...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2016AGUFMNH33A1910P','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2016AGUFMNH33A1910P"><span>Effects of <span class="hlt">Weather</span> on Tourism and its Moderation</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Park, J. H.; Kim, S.; Lee, D. K.</p> <p>2016-12-01</p> <p>Tourism is <span class="hlt">weather</span> sensitive industry (Gómez Martín, 2005). As climate change has been intensifying, the concerns about negative effects of <span class="hlt">weather</span> on tourism also have been increasing. This study attempted to find ways that mitigate the negative effects from <span class="hlt">weather</span> on tourism, by analyzing a path of the effects of <span class="hlt">weather</span> on intention to revisit and its moderation. The data of the study were collected by a self-recording online questionnaire survey of South Korean domestic tourists during August 2015, and 2,412 samples were gathered. A path <span class="hlt">model</span> of effects of <span class="hlt">weather</span> on intention to revisit that including moderating effects from physical attraction satisfaction and service satisfaction was ran. Season was controlled in the path <span class="hlt">model</span>. The <span class="hlt">model</span> fit was adequate (CMIN/DF=2.372(p=.000), CFI=.974, RMSEA=.024, SRMR=0.040), and the <span class="hlt">Model</span> Comparison, which assumes that the base <span class="hlt">model</span> to be correct with season constrained <span class="hlt">model</span>, showed that there was a seasonal differences in the <span class="hlt">model</span> ( DF=24, CMIN=32.430, P=.117). By the analysis, it was figured out that <span class="hlt">weather</span> and <span class="hlt">weather</span> expectation affected <span class="hlt">weather</span> satisfaction, and the <span class="hlt">weather</span> satisfaction affected intention to revisit (spring/fall: .167**, summer: .104**, and winter: .114**). Meanwhile physical attraction satisfaction (.200**), and service satisfaction (.210**) of tourism positively moderated <span class="hlt">weather</span> satisfaction in summer, and <span class="hlt">weather</span> satisfaction positively moderated physical attraction (.238**) satisfaction and service satisfaction (.339**). In other words, in summer, dissatisfaction from hot <span class="hlt">weather</span> was moderated by satisfaction from physical attractions and services, and in spring/fall, comfort <span class="hlt">weather</span> conditions promoted tourists to accept tourism experience and be satisfied from attractions and services positively. Based on the result, it was expected that if industries focus on offering the good attractions and services based on <span class="hlt">weather</span> conditions, there would be positive effects to alleviate tourists</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2014AGUFMIN13C3646L','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2014AGUFMIN13C3646L"><span>A near real time regional JPSS and GOES-R data assimilation <span class="hlt">system</span> for high impact <span class="hlt">weather</span> research and applications</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Li, J.; Wang, P.; Han, H.; Schmit, T. J.</p> <p>2014-12-01</p> <p>JPSS and GOES-R observations play important role in numerical <span class="hlt">weather</span> prediction (NWP). However, how to best represent the information from satellite observations and how to get value added information from these satellite data into regional NWP <span class="hlt">models</span>, including both radiance and derived products, still need investigations. In order to enhance the applications of JPSS and GOES-R data in regional NWP for high impact <span class="hlt">weather</span> forecasts, scientists from Cooperative Institute of Meteorological Satellite Studies (CIMSS) at University of Wisconsin-Madison have recently developed a near realtime regional Satellite Data Assimilation <span class="hlt">system</span> for Tropical storm forecasts (SDAT) (http://cimss.ssec.wisc.edu/sdat). The <span class="hlt">system</span> consists of the community Gridpoint Statistical Interpolation (GSI) assimilation <span class="hlt">system</span> and the advanced <span class="hlt">Weather</span> Research Forecast (WRF) <span class="hlt">model</span>. In addition to assimilate GOES, AMSUA/AMSUB, HIRS, MHS, ATMS (Suomi-NPP), AIRS and IASI radiances, the SDAT is also able to assimilate satellite-derived products such as hyperspectral IR retrieved temperature and moisture profiles, total precipitable water (TPW), GOES Sounder (and future GOES-R) layer precipitable water (LPW) and GOES Imager atmospheric motion vector (AMV) products into the <span class="hlt">system</span>. Real time forecasted GOES infrared (IR) images simulated from SDAT output have also been part of the SDAT <span class="hlt">system</span> for applications and forecast evaluations. To set up the <span class="hlt">system</span> parameters, a series of experiments have been carried out to test the impacts of different initialization schemes, including different background error matrix, different NCEP global <span class="hlt">model</span> date sets, and different WRF <span class="hlt">model</span> horizontal resolutions. Using SDAT as a research testbed, researches have been conducted for different satellite data impacts study, as well as different techniques for handling clouds in radiance assimilation. Since the fall of 2013, the SDAT <span class="hlt">system</span> has been running in near real time. The results from historical cases and 2014</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://rosap.ntl.bts.gov/view/dot/12115','DOTNTL'); return false;" href="https://rosap.ntl.bts.gov/view/dot/12115"><span>Transportation <span class="hlt">system</span> resilience, extreme <span class="hlt">weather</span> and climate change : a thought leadership series</span></a></p> <p><a target="_blank" href="http://ntlsearch.bts.gov/tris/index.do">DOT National Transportation Integrated Search</a></p> <p></p> <p>2014-09-01</p> <p>This report summarizes key findings from the Transportation <span class="hlt">System</span> Resilience, Extreme <span class="hlt">Weather</span> and Climate Change thought leadership series held at Volpe, the National Transportation <span class="hlt">Systems</span> Center from fall 2013 to spring 2014.</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://hdl.handle.net/2060/20000074058','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/20000074058"><span>Aviation <span class="hlt">Weather</span> Information Requirements Study</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Keel, Byron M.; Stancil, Charles E.; Eckert, Clifford A.; Brown, Susan M.; Gimmestad, Gary G.; Richards, Mark A.; Schaffner, Philip R. (Technical Monitor)</p> <p>2000-01-01</p> <p>The Aviation Safety Program (AvSP) has as its goal an improvement in aviation safety by a factor of 5 over the next 10 years and a factor of 10 over the next 20 years. Since <span class="hlt">weather</span> has a big impact on aviation safety and is associated with 30% of all aviation accidents, <span class="hlt">Weather</span> Accident Prevention (WxAP) is a major element under this program. The Aviation <span class="hlt">Weather</span> Information (AWIN) Distribution and Presentation project is one of three projects under this element. This report contains the findings of a study conducted by the Georgia Tech Research Institute (GTRI) under the Enhanced <span class="hlt">Weather</span> Products effort, which is a task under AWIN. The study examines current aviation <span class="hlt">weather</span> products and there application. The study goes on to identify deficiencies in the current <span class="hlt">system</span> and to define requirements for aviation <span class="hlt">weather</span> products that would lead to an increase in safety. The study also provides an overview the current set of sensors applied to the collection of aviation <span class="hlt">weather</span> information. New, modified, or fused sensor <span class="hlt">systems</span> are identified which could be applied in improving the current set of <span class="hlt">weather</span> products and in addressing the deficiencies defined in the report. In addition, the study addresses and recommends possible sensors for inclusion in an electronic pilot reporting (EPIREP) <span class="hlt">system</span>.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017AGUFMSH21A2635C','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017AGUFMSH21A2635C"><span>CCMC: bringing space <span class="hlt">weather</span> awareness to the next generation</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Chulaki, A.; Muglach, K.; Zheng, Y.; Mays, M. L.; Kuznetsova, M. M.; Taktakishvili, A.; Collado-Vega, Y. M.; Rastaetter, L.; Mendoza, A. M. M.; Thompson, B. J.; Pulkkinen, A. A.; Pembroke, A. D.</p> <p>2017-12-01</p> <p>Making space <span class="hlt">weather</span> an element of core education is critical for the future of the young field of space <span class="hlt">weather</span>. Community Coordinated <span class="hlt">Modeling</span> Center (CCMC) is an interagency partnership established to aid the transition of modern space science <span class="hlt">models</span> into space <span class="hlt">weather</span> forecasting while supporting space science research. Additionally, over the past ten years it has established itself as a global space science education resource supporting undergraduate and graduate education and research, and spreading space <span class="hlt">weather</span> awareness worldwide. A unique combination of assets, capabilities and close ties to the scientific and educational communities enable our small group to serve as a hub for rising generations of young space scientists and engineers. CCMC offers a variety of educational tools and resources publicly available online and providing access to the largest collection of modern space science <span class="hlt">models</span> developed by the international research community. CCMC has revolutionized the way these simulations are utilized in classrooms settings, student projects, and scientific labs. Every year, this online <span class="hlt">system</span> serves hundreds of students, educators and researchers worldwide. Another major CCMC asset is an expert space <span class="hlt">weather</span> prototyping team primarily serving NASA's interplanetary space <span class="hlt">weather</span> needs. Capitalizing on its unique capabilities and experiences, the team also provides in-depth space <span class="hlt">weather</span> training to hundreds of students and professionals. One training module offers undergraduates an opportunity to actively engage in real-time space <span class="hlt">weather</span> monitoring, analysis, forecasting, tools development and research, eventually serving remotely as NASA space <span class="hlt">weather</span> forecasters. In yet another project, CCMC is collaborating with Hayden Planetarium and Linkoping University on creating a visualization platform for planetariums (and classrooms) to provide simulations of dynamic processes in the large domain stretching from the solar corona to the Earth's upper</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2015AGUFM.A11F0101C','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2015AGUFM.A11F0101C"><span>Evaluating Changes in Extreme <span class="hlt">Weather</span> During the North American Monsoon in the Southwest U.S. Using High Resolution, Convective-Permitting Regional Atmospheric <span class="hlt">Modeling</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Castro, C. L.; Chang, H. I.; Luong, T. M.; Lahmers, T.; Jares, M.; Mazon, J.; Carrillo, C. M.; Adams, D. K.</p> <p>2015-12-01</p> <p>The North American monsoon (NAM) is the principal driver of summer severe <span class="hlt">weather</span> in the Southwest U.S. Monsoon convection typically initiates during daytime over the mountains and may organize into mesoscale convective <span class="hlt">systems</span> (MCSs). Most monsoon-related severe <span class="hlt">weather</span> occurs in association with organized convection, including microbursts, dust storms, flash flooding and lightning. A convective resolving grid spacing (on the kilometer scale) <span class="hlt">model</span> is required to explicitly represent the physical characteristics of organized convection, for example the presence of leading convective lines and trailing stratiform precipitation regions. Our objective is to analyze how monsoon severe <span class="hlt">weather</span> is changing in relation to anthropogenic climate change. We first consider a dynamically downscaled reanalysis during a historical period 1948-2010. Individual severe <span class="hlt">weather</span> event days, identified by favorable thermodynamic conditions, are then simulated for short-term, numerical <span class="hlt">weather</span> prediction-type simulations of 30h at a convective-permitting scale. Changes in <span class="hlt">modeled</span> severe <span class="hlt">weather</span> events indicate increases in precipitation intensity in association with long-term increases in atmospheric instability and moisture, particularly with organized convection downwind of mountain ranges. However, because the frequency of synoptic transients is decreasing during the monsoon, organized convection is less frequent and convective precipitation tends to be more phased locked to terrain. These types of <span class="hlt">modeled</span> changes also similarly appear in observed CPC precipitation, when the severe <span class="hlt">weather</span> event days are selected using historical radiosonde data. Next, we apply the identical <span class="hlt">model</span> simulation and analysis procedures to several dynamically downscaled CMIP3 and CMIP5 <span class="hlt">models</span> for the period 1950-2100, to assess how monsoon severe <span class="hlt">weather</span> may change in the future with respect to occurrence and intensity and if these changes correspond with what is already occurring in the historical</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2016AGUFM.A21F0140H','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2016AGUFM.A21F0140H"><span>A Prototype Nonhydrostatic Regional-to-Global Nested-Grid Atmosphere <span class="hlt">Model</span> for Medium-range <span class="hlt">Weather</span> Forecasting</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Harris, L.; Lin, S. J.; Zhou, L.; Chen, J. H.; Benson, R.; Rees, S.</p> <p>2016-12-01</p> <p>Limited-area convection-permitting <span class="hlt">models</span> have proven useful for short-range NWP, but are unable to interact with the larger scales needed for longer lead-time skill. A new global forecast <span class="hlt">model</span>, fvGFS, has been designed combining a modern nonhydrostatic dynamical core, the GFDL Finite-Volume Cubed-Sphere dynamical core (FV3) with operational GFS physics and initial conditions, and has been shown to provide excellent global skill while improving representation of small-scale phenomena. The nested-grid capability of FV3 allows us to build a regional-to-global variable-resolution <span class="hlt">model</span> to efficiently refine to 3-km grid spacing over the Continental US. The use of two-way grid nesting allows us to reach these resolutions very efficiently, with the operational requirement easily attainable on current supercomputing <span class="hlt">systems</span>.Even without a boundary-layer or advanced microphysical scheme appropriate for convection-perrmitting resolutions, the effectiveness of fvGFS can be demonstrated for a variety of <span class="hlt">weather</span> events. We demonstrate successful proof-of-concept simulations of a variety of phenomena. We show the capability to develop intense hurricanes with realistic fine-scale eyewalls and rainbands. The new <span class="hlt">model</span> also produces skillful predictions of severe <span class="hlt">weather</span> outbreaks and of organized mesoscale convective <span class="hlt">systems</span>. Fine-scale orographic and boundary-layer phenomena are also simulated with excellent fidelity by fvGFS. Further expected improvements are discussed, including the introduction of more sophisticated microphysics and of scale-aware convection schemes.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017EGUGA..19..543H','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017EGUGA..19..543H"><span>Improving <span class="hlt">Weather</span> Forecasts Through Reduced Precision Data Assimilation</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Hatfield, Samuel; Düben, Peter; Palmer, Tim</p> <p>2017-04-01</p> <p>We present a new approach for improving the efficiency of data assimilation, by trading numerical precision for computational speed. Future supercomputers will allow a greater choice of precision, so that <span class="hlt">models</span> can use a level of precision that is commensurate with the <span class="hlt">model</span> uncertainty. Previous studies have already indicated that the quality of climate and <span class="hlt">weather</span> forecasts is not significantly degraded when using a precision less than double precision [1,2], but so far these studies have not considered data assimilation. Data assimilation is inherently uncertain due to the use of relatively long assimilation windows, noisy observations and imperfect <span class="hlt">models</span>. Thus, the larger rounding errors incurred from reducing precision may be within the tolerance of the <span class="hlt">system</span>. Lower precision arithmetic is cheaper, and so by reducing precision in ensemble data assimilation, we can redistribute computational resources towards, for example, a larger ensemble size. Because larger ensembles provide a better estimate of the underlying distribution and are less reliant on covariance inflation and localisation, lowering precision could actually allow us to improve the accuracy of <span class="hlt">weather</span> forecasts. We will present results on how lowering numerical precision affects the performance of an ensemble data assimilation <span class="hlt">system</span>, consisting of the Lorenz '96 toy atmospheric <span class="hlt">model</span> and the ensemble square root filter. We run the <span class="hlt">system</span> at half precision (using an emulation tool), and compare the results with simulations at single and double precision. We estimate that half precision assimilation with a larger ensemble can reduce assimilation error by 30%, with respect to double precision assimilation with a smaller ensemble, for no extra computational cost. This results in around half a day extra of skillful <span class="hlt">weather</span> forecasts, if the error-doubling characteristics of the Lorenz '96 <span class="hlt">model</span> are mapped to those of the real atmosphere. Additionally, we investigate the sensitivity of these results</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2003EAEJA.....2019N','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2003EAEJA.....2019N"><span>A climatological study of the associated <span class="hlt">weather</span> events to Cut-off low <span class="hlt">systems</span> in the Southwestern Europe and Northern Africa</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Nieto, R.; Gimeno, L.; de La Torre, L.; Tesouro, M.; Añel, J.; Ribera, P.</p> <p>2003-04-01</p> <p>Cut-off low-pressure <span class="hlt">systems</span>-COLS- are usually closed circulations at middle and upper troposphere developed from a deep trough in the westerlies. As general rule troposphere below COLs is unstable and convective severe events can occur as a function of the surface conditions. COLs can bring moderate to heavy rainfall over large areas. In particular they are among the most important <span class="hlt">weather</span> <span class="hlt">systems</span> that affect Southern Europe and Northern Africa and responsible for some of the most catastrophic <span class="hlt">weather</span> events in terms of precipitation rate. In this study we identify COLs <span class="hlt">systems</span> in Southwestern Europe and Northern Africa for a 41-year period (1958 to 1998) using an approach based in imposing the three main physical characteristics of the conceptual <span class="hlt">model</span> of COL (a. closed circulation and minimum of geopotential, minimum of equivalent thickness, and two two baroclinic zones, one in front of the low and the other behind the low). Data from NCAR-NCEP reanalysis were used. The objective was to check the expected <span class="hlt">weather</span> events according to the conceptual <span class="hlt">model</span> of COL in an area where precipitation due to COL is relevant. In general terms results confirm expected <span class="hlt">weather</span> events: a frontal cloud band on the leading edge of an upper level low that is usually thick enough to produce precipitation. Over cold surface there is no convection, and therefore no showers occur. Over Sea, moderate to heavy showery precipitation is frequent. The heaviest precipitation occur when convective cells are observed in the centre and over warm ocean, fall flash flood is frequent.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://rosap.ntl.bts.gov/view/dot/30953','DOTNTL'); return false;" href="https://rosap.ntl.bts.gov/view/dot/30953"><span>Thermoelectric generator installation at Divide Road <span class="hlt">Weather</span> Information <span class="hlt">Systems</span> (RWIS).</span></a></p> <p><a target="_blank" href="http://ntlsearch.bts.gov/tris/index.do">DOT National Transportation Integrated Search</a></p> <p></p> <p>2016-04-13</p> <p>The Department of Transportation and Public Facilities (DOT&PF) has a network of Road <span class="hlt">Weather</span> Information <span class="hlt">System</span> (RWIS) environmental sensor stations (ESS) deployed along the road network. Six of the stations do not have access to commercial power an...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2013EGUGA..1513709R','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2013EGUGA..1513709R"><span>GEOSS interoperability for <span class="hlt">Weather</span>, Ocean and Water</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Richardson, David; Nyenhuis, Michael; Zsoter, Ervin; Pappenberger, Florian</p> <p>2013-04-01</p> <p>"Understanding the Earth <span class="hlt">system</span> — its <span class="hlt">weather</span>, climate, oceans, atmosphere, water, land, geodynamics, natural resources, ecosystems, and natural and human-induced hazards — is crucial to enhancing human health, safety and welfare, alleviating human suffering including poverty, protecting the global environment, reducing disaster losses, and achieving sustainable development. Observations of the Earth <span class="hlt">system</span> constitute critical input for advancing this understanding." With this in mind, the Group on Earth Observations (GEO) started implementing the Global Earth Observation <span class="hlt">System</span> of <span class="hlt">Systems</span> (GEOSS). GEOWOW, short for "GEOSS interoperability for <span class="hlt">Weather</span>, Ocean and Water", is supporting this objective. GEOWOW's main challenge is to improve Earth observation data discovery, accessibility and exploitability, and to evolve GEOSS in terms of interoperability, standardization and functionality. One of the main goals behind the GEOWOW project is to demonstrate the value of the TIGGE archive in interdisciplinary applications, providing a vast amount of useful and easily accessible information to the users through the GEO Common Infrastructure (GCI). GEOWOW aims at developing funcionalities that will allow easy discovery, access and use of TIGGE archive data and of in-situ observations, e.g. from the Global Runoff Data Centre (GRDC), to support applications such as river discharge forecasting.TIGGE (THORPEX Interactive Grand Global Ensemble) is a key component of THORPEX: a World <span class="hlt">Weather</span> Research Programme to accelerate the improvements in the accuracy of 1-day to 2 week high-impact <span class="hlt">weather</span> forecasts for the benefit of humanity. The TIGGE archive consists of ensemble <span class="hlt">weather</span> forecast data from ten global NWP centres, starting from October 2006, which has been made available for scientific research. The TIGGE archive has been used to analyse hydro-meteorological forecasts of flooding in Europe as well as in China. In general the analysis has been favourable in terms of</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://rosap.ntl.bts.gov/view/dot/3851','DOTNTL'); return false;" href="https://rosap.ntl.bts.gov/view/dot/3851"><span>Phase II (baseline) report for the Greater Yellowstone Regional Traveler and <span class="hlt">Weather</span> Information <span class="hlt">System</span> (GYRTWIS)</span></a></p> <p><a target="_blank" href="http://ntlsearch.bts.gov/tris/index.do">DOT National Transportation Integrated Search</a></p> <p></p> <p>2002-09-11</p> <p>In an effort to make road and <span class="hlt">weather</span> information more readily available to travelers and maintenance personnel, Montana is implementing the Greater Yellowstone Regional Traveler and <span class="hlt">Weather</span> Information <span class="hlt">System</span> (GYRTWIS). GYRTWIS replaces the existing...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2014AGUFMED31E3460B','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2014AGUFMED31E3460B"><span>Studying <span class="hlt">Weather</span> and Climate Using Atmospheric Retrospective Analyses</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Bosilovich, M. G.</p> <p>2014-12-01</p> <p>Over the last 35 years, tremendous amounts of satellite observations of the Earth's atmosphere have been collected along side the much longer and diverse record of in situ measurements. The satellite data records have disparate qualities, structure and uncertainty which make comparing <span class="hlt">weather</span> from the 80s and 2000s a challenging prospect. Likewise, in-situ data records lack complete coverage of the earth in both space and time. Atmospheric reanalyses use the observations with numerical <span class="hlt">models</span> and data assimilation to produce continuous and consistent <span class="hlt">weather</span> data records for periods longer than decades. The result is a simplified data format with a relatively straightforward learning curve that includes many more variables available (through the <span class="hlt">modeling</span> component of the <span class="hlt">system</span>), but driven by a full suite of observational data. The simplified data format allows introduction into <span class="hlt">weather</span> and climate data analysis. Some examples are provided from undergraduate meteorology program internship projects. We will present the students progression through the projects from their initial understanding and competencies to some final results and the skills learned along the way. Reanalyses are a leading research tool in <span class="hlt">weather</span> and climate, but can also provide an introductory experience as well, allowing students to develop an understanding of the physical <span class="hlt">system</span> while learning basic programming and analysis skills.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2009AGUFMSA34A..02S','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2009AGUFMSA34A..02S"><span>Operational Space <span class="hlt">Weather</span> <span class="hlt">Models</span>: Trials, Tribulations and Rewards</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Schunk, R. W.; Scherliess, L.; Sojka, J. J.; Thompson, D. C.; Zhu, L.</p> <p>2009-12-01</p> <p>There are many empirical, physics-based, and data assimilation <span class="hlt">models</span> that can probably be used for space <span class="hlt">weather</span> applications and the <span class="hlt">models</span> cover the entire domain from the surface of the Sun to the Earth’s surface. At Utah State University we developed two physics-based data assimilation <span class="hlt">models</span> of the terrestrial ionosphere as part of a program called Global Assimilation of Ionospheric Measurements (GAIM). One of the data assimilation <span class="hlt">models</span> is now in operational use at the Air Force <span class="hlt">Weather</span> Agency (AFWA) in Omaha, Nebraska. This <span class="hlt">model</span> is a Gauss-Markov Kalman Filter (GAIM-GM) <span class="hlt">model</span>, and it uses a physics-based <span class="hlt">model</span> of the ionosphere and a Kalman filter as a basis for assimilating a diverse set of real-time (or near real-time) measurements. The physics-based <span class="hlt">model</span> is the Ionosphere Forecast <span class="hlt">Model</span> (IFM), which is global and covers the E-region, F-region, and topside ionosphere from 90 to 1400 km. It takes account of five ion species (NO+, O2+, N2+, O+, H+), but the main output of the <span class="hlt">model</span> is a 3-dimensional electron density distribution at user specified times. The second data assimilation <span class="hlt">model</span> uses a physics-based Ionosphere-Plasmasphere <span class="hlt">Model</span> (IPM) and an ensemble Kalman filter technique as a basis for assimilating a diverse set of real-time (or near real-time) measurements. This Full Physics <span class="hlt">model</span> (GAIM-FP) is global, covers the altitude range from 90 to 30,000 km, includes six ions (NO+, O2+, N2+, O+, H+, He+), and calculates the self-consistent ionospheric drivers (electric fields and neutral winds). The GAIM-FP <span class="hlt">model</span> is scheduled for delivery in 2012. Both of these GAIM <span class="hlt">models</span> assimilate bottom-side Ne profiles from a variable number of ionosondes, slant TEC from a variable number of ground GPS/TEC stations, in situ Ne from four DMSP satellites, line-of-sight UV emissions measured by satellites, and occultation data. Quality control algorithms for all of the data types are provided as an integral part of the GAIM <span class="hlt">models</span> and these <span class="hlt">models</span> take account of</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/19900011618','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/19900011618"><span><span class="hlt">Weather</span> data dissemination to aircraft</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Mcfarland, Richard H.; Parker, Craig B.</p> <p>1990-01-01</p> <p>Documentation exists that shows <span class="hlt">weather</span> to be responsible for approximately 40 percent of all general aviation accidents with fatalities. <span class="hlt">Weather</span> data products available on the ground are becoming more sophisticated and greater in number. Although many of these data are critical to aircraft safety, they currently must be transmitted verbally to the aircraft. This process is labor intensive and provides a low rate of information transfer. Consequently, the pilot is often forced to make life-critical decisions based on incomplete and outdated information. Automated transmission of <span class="hlt">weather</span> data from the ground to the aircraft can provide the aircrew with accurate data in near-real time. The current National Airspace <span class="hlt">System</span> Plan calls for such an uplink capability to be provided by the Mode S Beacon <span class="hlt">System</span> data link. Although this <span class="hlt">system</span> has a very advanced data link capability, it will not be capable of providing adequate <span class="hlt">weather</span> data to all airspace users in its planned configuration. This paper delineates some of the important <span class="hlt">weather</span> data uplink <span class="hlt">system</span> requirements, and describes a <span class="hlt">system</span> which is capable of meeting these requirements. The proposed <span class="hlt">system</span> utilizes a run-length coding technique for image data compression and a hybrid phase and amplitude modulation technique for the transmission of both voice and <span class="hlt">weather</span> data on existing aeronautical Very High Frequency (VHF) voice communication channels.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2014AGUFMIN42A..06B','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2014AGUFMIN42A..06B"><span>Near Real Time Data for Operational Space <span class="hlt">Weather</span> Forecasting</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Berger, T. E.</p> <p>2014-12-01</p> <p>Space <span class="hlt">weather</span> operations presents unique challenges for data <span class="hlt">systems</span> and providers. Space <span class="hlt">weather</span> events evolve more quickly than terrestrial <span class="hlt">weather</span> events. While terrestrial <span class="hlt">weather</span> occurs on timescales of minutes to hours, space <span class="hlt">weather</span> storms evolve on timescales of seconds to minutes. For example, the degradation of the High Frequency Radio communications between the ground and commercial airlines is nearly instantaneous when a solar flare occurs. Thus the customer is observing impacts at the same time that the operational forecast center is seeing the event unfold. The diversity and spatial scale of the space <span class="hlt">weather</span> <span class="hlt">system</span> is such that no single observation can capture the salient features. The vast space that encompasses space <span class="hlt">weather</span> and the scarcity of observations further exacerbates the situation and make each observation even more valuable. The physics of interplanetary space, through which many major storms propagate, is very different from the physics of the ionosphere where most of the impacts are felt. And while some observations can be made from ground-based observatories, many of the most critical data comes from satellites, often in unique orbits far from Earth. In this presentation, I will describe some of the more important sources and types of data that feed into the operational alerts, watches, and warnings of space <span class="hlt">weather</span> storms. Included will be a discussion of some of the new space <span class="hlt">weather</span> forecast <span class="hlt">models</span> and the data challenges that they bring forward.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.osti.gov/servlets/purl/1414656','SCIGOV-STC'); return false;" href="https://www.osti.gov/servlets/purl/1414656"><span>Coding a <span class="hlt">Weather</span> <span class="hlt">Model</span>: DOE-FIU Science & Technology Workforce Development Program.</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>Bradley, Jon David</p> <p></p> <p>DOE Fellow, Andres Cremisini, completed a 10-week internship with Sandia National Laboratories (SNL) in Albuquerque, New Mexico. Under the management of Kristopher Klingler and the mentorship of Jon Bradley, he was tasked with conceiving and coding a realistic <span class="hlt">weather</span> <span class="hlt">model</span> for use in physical security applications. The objective was to make a <span class="hlt">weather</span> <span class="hlt">model</span> that could use real data to accurately predict wind and precipitation conditions at any location of interest on the globe at any user-determined time. The intern received guidance on software design, the C++ programming language and clear communication of project goals and ongoing progress. In addition,more » Mr. Cremisini was given license to structure the program however he best saw fit, an experience that will benefit ongoing research endeavors.« less</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2010cosp...38.4168M','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2010cosp...38.4168M"><span>Activities of NICT space <span class="hlt">weather</span> project</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Murata, Ken T.; Nagatsuma, Tsutomu; Watari, Shinichi; Shinagawa, Hiroyuki; Ishii, Mamoru</p> <p></p> <p>NICT (National Institute of Information and Communications Technology) has been in charge of space <span class="hlt">weather</span> forecast service in Japan for more than 20 years. The main target region of the space <span class="hlt">weather</span> is the geo-space in the vicinity of the Earth where human activities are dominant. In the geo-space, serious damages of satellites, international space stations and astronauts take place caused by energetic particles or electromagnetic disturbances: the origin of the causes is dynamically changing of solar activities. Positioning <span class="hlt">systems</span> via GPS satellites are also im-portant recently. Since the most significant effect of positioning error comes from disturbances of the ionosphere, it is crucial to estimate time-dependent modulation of the electron density profiles in the ionosphere. NICT is one of the 13 members of the ISES (International Space Environment Service), which is an international assembly of space <span class="hlt">weather</span> forecast centers under the UNESCO. With help of geo-space environment data exchanging among the member nations, NICT operates daily space <span class="hlt">weather</span> forecast service every day to provide informa-tion on forecasts of solar flare, geomagnetic disturbances, solar proton event, and radio-wave propagation conditions in the ionosphere. The space <span class="hlt">weather</span> forecast at NICT is conducted based on the three methodologies: observations, simulations and informatics (OSI <span class="hlt">model</span>). For real-time or quasi real-time reporting of space <span class="hlt">weather</span>, we conduct our original observations: Hiraiso solar observatory to monitor the solar activity (solar flare, coronal mass ejection, and so on), domestic ionosonde network, magnetometer HF radar observations in far-east Siberia, and south-east Asia low-latitude ionosonde network (SEALION). Real-time observation data to monitor solar and solar-wind activities are obtained through antennae at NICT from ACE and STEREO satellites. We have a middle-class super-computer (NEC SX-8R) to maintain real-time computer simulations for solar and solar</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017E3SWC..2001008N','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017E3SWC..2001008N"><span>Geospace monitoring for space <span class="hlt">weather</span> research and operation</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Nagatsuma, Tsutomu</p> <p>2017-10-01</p> <p>Geospace, a space surrounding the Earth, is one of the key area for space <span class="hlt">weather</span>. Because geospace environment dynamically varies depending on the solar wind conditions. Many kinds of space assets are operating in geospace for practical purposes. Anomalies of space assets are sometimes happened because of space <span class="hlt">weather</span> disturbances in geospace. Therefore, monitoring and forecasting of geospace environment is very important tasks for NICT's space <span class="hlt">weather</span> research and development. To monitor and to improve forecasting <span class="hlt">model</span>, fluxgate magnetometers and HF radars are operated by our laboratory, and its data are used for our research work, too. We also operate real-time data acquisition <span class="hlt">system</span> for satellite data, such as DSCOVR, STEREO, and routinely received high energy particle data from Himawari-8. Based on these data, we are monitoring current condition of geomagnetic disturbances, and that of radiation belt. Using these data, we have developed empirical <span class="hlt">models</span> for relativistic electron flux at GEO and inner magnetosphere. To provide userfriendly information , we are trying to develop individual spacecraft anomaly risk estimation tool based on combining <span class="hlt">models</span> of space <span class="hlt">weather</span> and those of spacecraft charging, Current status of geospace monitoring, forecasting, and research activities are introduced.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/28683431','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/28683431"><span><span class="hlt">Modeling</span> and projection of dengue fever cases in Guangzhou based on variation of <span class="hlt">weather</span> factors.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Li, Chenlu; Wang, Xiaofeng; Wu, Xiaoxu; Liu, Jianing; Ji, Duoying; Du, Juan</p> <p>2017-12-15</p> <p>Dengue fever is one of the most serious vector-borne infectious diseases, especially in Guangzhou, China. Dengue viruses and their vectors Aedes albopictus are sensitive to climate change primarily in relation to <span class="hlt">weather</span> factors. Previous research has mainly focused on identifying the relationship between climate factors and dengue cases, or developing dengue case <span class="hlt">models</span> with some non-climate factors. However, there has been little research addressing the <span class="hlt">modeling</span> and projection of dengue cases only from the perspective of climate change. This study considered this topic using long time series data (1998-2014). First, sensitive <span class="hlt">weather</span> factors were identified through meta-analysis that included literature review screening, lagged analysis, and collinear analysis. Then, key factors that included monthly average temperature at a lag of two months, and monthly average relative humidity and monthly average precipitation at lags of three months were determined. Second, time series Poisson analysis was used with the generalized additive <span class="hlt">model</span> approach to develop a dengue <span class="hlt">model</span> based on key <span class="hlt">weather</span> factors for January 1998 to December 2012. Data from January 2013 to July 2014 were used to validate that the <span class="hlt">model</span> was reliable and reasonable. Finally, future <span class="hlt">weather</span> data (January 2020 to December 2070) were input into the <span class="hlt">model</span> to project the occurrence of dengue cases under different climate scenarios (RCP 2.6 and RCP 8.5). Longer time series analysis and scientifically selected <span class="hlt">weather</span> variables were used to develop a dengue <span class="hlt">model</span> to ensure reliability. The projections suggested that seasonal disease control (especially in summer and fall) and mitigation of greenhouse gas emissions could help reduce the incidence of dengue fever. The results of this study hope to provide a scientifically theoretical basis for the prevention and control of dengue fever in Guangzhou. Copyright © 2017 Elsevier B.V. All rights reserved.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/20020081040','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/20020081040"><span>Aircraft Icing <span class="hlt">Weather</span> Data Reporting and Dissemination <span class="hlt">System</span></span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Bass, Ellen J.; Minsk, Brian; Lindholm, Tenny; Politovich, Marcia; Reehorst, Andrew (Technical Monitor)</p> <p>2002-01-01</p> <p>The long-term operational concept of this research is to develop an onboard aircraft <span class="hlt">system</span> that assesses and reports atmospheric icing conditions automatically and in a timely manner in order to improve aviation safety and the efficiency of aircraft operations via improved real-time and forecast <span class="hlt">weather</span> products. The idea is to use current measurement capabilities on aircraft equipped with icing sensors and in-flight data communication technologies as a reporting source. Without requiring expensive avionics upgrades, aircraft data must be processed and available for downlink. Ideally, the data from multiple aircraft can then be integrated (along with other real-time and <span class="hlt">modeled</span> data) on the ground such that aviation-centered icing hazard metrics for volumes of airspace can be assessed. As the effect of icing on different aircraft types can vary, the information should be displayed in meaningful ways such that multiple types of users can understand the information. That is, information must be presented in a manner to allow users to understand the icing conditions with respect to individual concerns and aircraft capabilities. This research provides progress toward this operational concept by: identifying an aircraft platform capable of digitally capturing, processing, and downlinking icing data; identifying the required in situ icing data processing; investigating the requirements for routing the icing data for use by <span class="hlt">weather</span> products; developing an icing case study in order to gain insight into major air carrier needs; developing and prototyping icing display concepts based on the National Center for Atmospheric Research's existing diagnostic and forecast experimental icing products; and conducting a usability study for the prototyped icing display concepts.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017EGUGA..19.6579B','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017EGUGA..19.6579B"><span>Silicon isotopes fractionation in meteoric chemical <span class="hlt">weathering</span> and hydrothermal alteration <span class="hlt">systems</span> of volcanic rocks (Mayotte)</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Basile-Doelsch, Isabelle; Puyraveau, Romain-Arnaud; Guihou, Abel; Haurine, Frederic; Deschamps, Pierre; rad, Setareh; Nehlig, Pierre</p> <p>2017-04-01</p> <p>Low temperature chemical <span class="hlt">weathering</span> fractionates silicon (Si) isotopes while forming secondary silicates. The Si fractionation ranges of high temperature secondary phyllosilicates formed in hydrothermal alteration environments have not been investigated to date. Several parameters, including temperature, reaction rates, pH, ionic concentrations in solution, precipitation/dissolution series or kinetic versus equilibrium regime are not the same in hydrothermal alteration and surface <span class="hlt">weathering</span> <span class="hlt">systems</span> and may lead to different fractionation factors. In this work, we analyzed Si isotopes in these two types of alteration conditions in two profiles sampled on the volcanic island of Mayotte. In both profiles, Si-bearing secondary mineral was kaolinite. Both profiles showed 30Si depletion as a function of the degree of alteration but each with a distinct pattern. In the meteoric <span class="hlt">weathering</span> profile, from the bottom to the top, a gradual decrease of the δ30Si from parent rock (-0.29 ± 0.13 ‰) towards the most <span class="hlt">weathered</span> product (-2.05 ± 0.13 ‰) was observed. In the hydrothermal alteration profile, in which meteoric <span class="hlt">weathering</span> was also superimposed at the top of the profile, an abrupt transition of the δ30Si was measured at the interface between parent-rock (-0.21 ± 0.11 ‰) and the altered products, with a minimum value of -3.06 ± 0.16 ‰˙ At the scale of Si-bearing secondary minerals, in the chemical <span class="hlt">weathering</span> <span class="hlt">system</span>, a Δ30Sikaol-parentrock of -1.9 ‰ was observed, in agreement with results in the literature. A low temperature kinetic fractionation 30ɛ of -2.29 ‰ was calculated using a simple steady state <span class="hlt">model</span>. However, an unexpected Δ30Sikaol-parentrock of -2.85 ‰ was measured in the hydrothermal alteration site, pointing to possible mechanisms linked to dissolution/precipitation series and/or to ionic composition of the solution as the main controlling factors of fractionation in hydrothermal conditions. At the scale of the profiles, both δ30Si</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017APS..DFDD17001S','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017APS..DFDD17001S"><span><span class="hlt">Weather</span> Research and Forecasting <span class="hlt">model</span> simulation of an onshore wind farm: assessment against LiDAR and SCADA data</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Santoni, Christian; Garcia-Cartagena, Edgardo J.; Zhan, Lu; Iungo, Giacomo Valerio; Leonardi, Stefano</p> <p>2017-11-01</p> <p>The integration of wind farm parameterizations into numerical <span class="hlt">weather</span> prediction <span class="hlt">models</span> is essential to study power production under realistic conditions. Nevertheless, recent <span class="hlt">models</span> are unable to capture turbine wake interactions and, consequently, the mean kinetic energy entrainment, which are essential for the development of power optimization <span class="hlt">models</span>. To address the study of wind turbine wake interaction, one-way nested mesoscale to large-eddy simulation (LES) were performed using the <span class="hlt">Weather</span> Research and Forecasting <span class="hlt">model</span> (WRF). The simulation contains five nested domains <span class="hlt">modeling</span> the mesoscale wind on the entire North Texas Panhandle region to the microscale wind fluctuations and turbine wakes of a wind farm located at Panhandle, Texas. The wind speed, direction and boundary layer profile obtained from WRF were compared against measurements obtained with a sonic anemometer and light detection and ranging <span class="hlt">system</span> located within the wind farm. Additionally, the power production were assessed against measurements obtained from the supervisory control and data acquisition <span class="hlt">system</span> located in each turbine. Furthermore, to incorporate the turbines into very coarse LES, a modification to the implementation of the wind farm parameterization by Fitch et al. (2012) is proposed. This work was supported by the NSF, Grants No. 1243482 (WINDINSPIRE) and IIP 1362033 (WindSTAR), and TACC.</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://hdl.handle.net/2060/19840026819','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/19840026819"><span>Development of the Centralized Storm Information <span class="hlt">System</span> (CSIS) for use in severe <span class="hlt">weather</span> prediction</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Mosher, F. R.</p> <p>1984-01-01</p> <p>The centralized storm information <span class="hlt">system</span> is now capable of ingesting and remapping radar scope presentations on a satellite projection. This can be color enhanced and superposed on other data types. Presentations from more than one radar can be composited on a single image. As with most other data sources, a simple macro establishes the loops and scheduling of the radar ingestions as well as the autodialing. There are approximately 60 NWS network 10 cm radars that can be interrogated. NSSFC forecasters have found this data source to be extremely helpful in severe <span class="hlt">weather</span> situations. The capability to access lightning frequency data stored in a National <span class="hlt">Weather</span> Service computer was added. Plans call for an interface with the National Meteorological Center to receive and display prognostic fields from operational computer forecast <span class="hlt">models</span>. Programs are to be developed to plot and display locations of reported severe local storm events.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.osti.gov/biblio/1177297-modeling-high-impact-weather-climate-lessons-from-tropical-cyclone-perspective','SCIGOV-STC'); return false;" href="https://www.osti.gov/biblio/1177297-modeling-high-impact-weather-climate-lessons-from-tropical-cyclone-perspective"><span><span class="hlt">Modeling</span> High-Impact <span class="hlt">Weather</span> and Climate: Lessons From a Tropical Cyclone Perspective</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>Done, James; Holland, Greg; Bruyere, Cindy</p> <p>2013-10-19</p> <p>Although the societal impact of a <span class="hlt">weather</span> event increases with the rarity of the event, our current ability to assess extreme events and their impacts is limited by not only rarity but also by current <span class="hlt">model</span> fidelity and a lack of understanding of the underlying physical processes. This challenge is driving fresh approaches to assess high-impact <span class="hlt">weather</span> and climate. Recent lessons learned in <span class="hlt">modeling</span> high-impact <span class="hlt">weather</span> and climate are presented using the case of tropical cyclones as an illustrative example. Through examples using the Nested Regional Climate <span class="hlt">Model</span> to dynamically downscale large-scale climate data the need to treat bias inmore » the driving data is illustrated. Domain size, location, and resolution are also shown to be critical and should be guided by the need to: include relevant regional climate physical processes; resolve key impact parameters; and to accurately simulate the response to changes in external forcing. The notion of sufficient <span class="hlt">model</span> resolution is introduced together with the added value in combining dynamical and statistical assessments to fill out the parent distribution of high-impact parameters. Finally, through the example of a tropical cyclone damage index, direct impact assessments are resented as powerful tools that distill complex datasets into concise statements on likely impact, and as highly effective communication devices.« less</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017AGUFMNH51B0128X','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017AGUFMNH51B0128X"><span>Monitoring Space <span class="hlt">Weather</span> Hazards caused by geomagnetic disturbances with Space Hazard Monitor (SHM) <span class="hlt">systems</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Xu, Z.; Gannon, J. L.; Peek, T. A.; Lin, D.</p> <p>2017-12-01</p> <p>One space <span class="hlt">weather</span> hazard is the Geomagnetically Induced Currents (GICs) in the electric power transmission <span class="hlt">systems</span>, which is naturally induced geoelectric field during the geomagnetic disturbances (GMDs). GICs are a potentially catastrophic threat to bulk power <span class="hlt">systems</span>. For instance, the Blackout in Quebec in March 1989 was caused by GMDs during a significant magnetic storm. To monitor the GMDs, the autonomous Space Hazard Monitor (SHM) <span class="hlt">system</span> is developed recently. The <span class="hlt">system</span> includes magnetic field measurement from magnetometers and geomagnetic field measurement from electrodes. In this presentation, we introduce the six sites of SHMs which have been deployed in the US continental regions. The data from the magnetometers are processed with the Multiple Observatory Geomagnetic Data Analysis Software (MOGDAS). And the statistical results are presented here. It reveals not only the impacts of space <span class="hlt">weather</span> over US continental region but also the potential of improving instrumentation development to provide better space <span class="hlt">weather</span> monitor.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/26894570','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/26894570"><span>Developing a Time Series Predictive <span class="hlt">Model</span> for Dengue in Zhongshan, China Based on <span class="hlt">Weather</span> and Guangzhou Dengue Surveillance Data.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Zhang, Yingtao; Wang, Tao; Liu, Kangkang; Xia, Yao; Lu, Yi; Jing, Qinlong; Yang, Zhicong; Hu, Wenbiao; Lu, Jiahai</p> <p>2016-02-01</p> <p>Dengue is a re-emerging infectious disease of humans, rapidly growing from endemic areas to dengue-free regions due to favorable conditions. In recent decades, Guangzhou has again suffered from several big outbreaks of dengue; as have its neighboring cities. This study aims to examine the impact of dengue epidemics in Guangzhou, China, and to develop a predictive <span class="hlt">model</span> for Zhongshan based on local <span class="hlt">weather</span> conditions and Guangzhou dengue surveillance information. We obtained weekly dengue case data from 1st January, 2005 to 31st December, 2014 for Guangzhou and Zhongshan city from the Chinese National Disease Surveillance Reporting <span class="hlt">System</span>. Meteorological data was collected from the Zhongshan <span class="hlt">Weather</span> Bureau and demographic data was collected from the Zhongshan Statistical Bureau. A negative binomial regression <span class="hlt">model</span> with a log link function was used to analyze the relationship between weekly dengue cases in Guangzhou and Zhongshan, controlling for meteorological factors. Cross-correlation functions were applied to identify the time lags of the effect of each <span class="hlt">weather</span> factor on weekly dengue cases. <span class="hlt">Models</span> were validated using receiver operating characteristic (ROC) curves and k-fold cross-validation. Our results showed that weekly dengue cases in Zhongshan were significantly associated with dengue cases in Guangzhou after the treatment of a 5 weeks prior moving average (Relative Risk (RR) = 2.016, 95% Confidence Interval (CI): 1.845-2.203), controlling for <span class="hlt">weather</span> factors including minimum temperature, relative humidity, and rainfall. ROC curve analysis indicated our forecasting <span class="hlt">model</span> performed well at different prediction thresholds, with 0.969 area under the receiver operating characteristic curve (AUC) for a threshold of 3 cases per week, 0.957 AUC for a threshold of 2 cases per week, and 0.938 AUC for a threshold of 1 case per week. <span class="hlt">Models</span> established during k-fold cross-validation also had considerable AUC (average 0.938-0.967). The sensitivity and specificity</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/20100036254','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/20100036254"><span>Maintaining a Local Data Integration <span class="hlt">System</span> in Support of <span class="hlt">Weather</span> Forecast Operations</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Watson, Leela R.; Blottman, Peter F.; Sharp, David W.; Hoeth, Brian</p> <p>2010-01-01</p> <p>Since 2000, both the National <span class="hlt">Weather</span> Service in Melbourne, FL (NWS MLB) and the Spaceflight Meteorology Group (SMG) at Johnson Space Center in Houston, TX have used a local data integration <span class="hlt">system</span> (LDIS) as part of their forecast and warning operations. The original LDIS was developed by NASA's Applied Meteorology Unit (AMU; Bauman et ai, 2004) in 1998 (Manobianco and Case 1998) and has undergone subsequent improvements. Each has benefited from three-dimensional (3-D) analyses that are delivered to forecasters every 15 minutes across the peninsula of Florida. The intent is to generate products that enhance short-range <span class="hlt">weather</span> forecasts issued in support of NWS MLB and SMG operational requirements within East Central Florida. The current LDIS uses the Advanced Regional Prediction <span class="hlt">System</span> (ARPS) Data Analysis <span class="hlt">System</span> (ADAS) package as its core, which integrates a wide variety of national, regional, and local observational data sets. It assimilates all available real-time data within its domain and is run at a finer spatial and temporal resolution than current national- or regional-scale analysis packages. As such, it provides local forecasters with a more comprehensive understanding of evolving fine-scale <span class="hlt">weather</span> features</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2012AGUFMED43A0710Y','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2012AGUFMED43A0710Y"><span>Preparing Middle School Teachers to Use Science <span class="hlt">Models</span> Effectively when Teaching about <span class="hlt">Weather</span> and Climate Topics</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Yarker, M. B.; Stanier, C. O.; Forbes, C.; Park, S.</p> <p>2012-12-01</p> <p>According to the National Science Education Standards (NSES), teachers are encouraged to use science <span class="hlt">models</span> in the classroom as a way to aid in the understanding of the nature of the scientific process. This is of particular importance to the atmospheric science community because climate and <span class="hlt">weather</span> <span class="hlt">models</span> are very important when it comes to understanding current and future behaviors of our atmosphere. Although familiar with <span class="hlt">weather</span> forecasts on television and the Internet, most people do not understand the process of using computer <span class="hlt">models</span> to generate <span class="hlt">weather</span> and climate forecasts. As a result, the public often misunderstands claims scientists make about their daily <span class="hlt">weather</span> as well as the state of climate change. Therefore, it makes sense that recent research in science education indicates that scientific <span class="hlt">models</span> and <span class="hlt">modeling</span> should be a topic covered in K-12 classrooms as part of a comprehensive science curriculum. The purpose of this research study is to describe how three middle school teachers use science <span class="hlt">models</span> to teach about topics in climate and <span class="hlt">weather</span>, as well as the challenges they face incorporating <span class="hlt">models</span> effectively into the classroom. Participants in this study took part in a week long professional development designed to orient them towards appropriate use of science <span class="hlt">models</span> for a unit on <span class="hlt">weather</span>, climate, and energy concepts. The course design was based on empirically tested features of effective professional development for science teachers and was aimed at teaching content to the teachers while simultaneously orienting them towards effective use of science <span class="hlt">models</span> in the classroom in a way that both aids in learning about the content knowledge as well as how <span class="hlt">models</span> are used in scientific inquiry. Results indicate that teachers perceive <span class="hlt">models</span> to be physical representations that can be used as evidence to convince students that the teacher's conception of the concept is correct. Additionally, teachers tended to use them as ways to explain an idea to</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2013AGUFMPA23A..04V','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2013AGUFMPA23A..04V"><span>Presenting Critical Space <span class="hlt">Weather</span> Information to Customers and Stakeholders (Invited)</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Viereck, R. A.; Singer, H. J.; Murtagh, W. J.; Rutledge, B.</p> <p>2013-12-01</p> <p>Space <span class="hlt">weather</span> involves changes in the near-Earth space environment that impact technological <span class="hlt">systems</span> such as electric power, radio communication, satellite navigation (GPS), and satellite opeartions. As with terrestrial <span class="hlt">weather</span>, there are several different kinds of space <span class="hlt">weather</span> and each presents unique challenges to the impacted technologies and industries. But unlike terrestrial <span class="hlt">weather</span>, many customers are not fully aware of space <span class="hlt">weather</span> or how it impacts their <span class="hlt">systems</span>. This issue is further complicated by the fact that the largest space <span class="hlt">weather</span> events occur very infrequently with years going by without severe storms. Recent reports have estimated very large potential costs to the economy and to society if a geomagnetic storm were to cause major damage to the electric power transmission <span class="hlt">system</span>. This issue has come to the attention of emergency managers and federal agencies including the office of the president. However, when considering space <span class="hlt">weather</span> impacts, it is essential to also consider uncertainties in the frequency of events and the predicted impacts. The unique nature of space <span class="hlt">weather</span> storms, the specialized technologies that are impacted by them, and the disparate groups and agencies that respond to space <span class="hlt">weather</span> forecasts and alerts create many challenges to the task of communicating space <span class="hlt">weather</span> information to the public. Many customers that receive forecasts and alerts are highly technical and knowledgeable about the subtleties of the space environment. Others know very little and require ongoing education and explanation about how a space <span class="hlt">weather</span> storm will affect their <span class="hlt">systems</span>. In addition, the current knowledge and understanding of the space environment that goes into forecasting storms is quite immature. It has only been within the last five years that physics-based <span class="hlt">models</span> of the space environment have played important roles in predictions. Thus, the uncertainties in the forecasts are quite large. There is much that we don't know about space</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2018PApGe.tmp.1252R','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2018PApGe.tmp.1252R"><span>Waterspout Forecasting Method Over the Eastern Adriatic Using a High-Resolution Numerical <span class="hlt">Weather</span> <span class="hlt">Model</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Renko, Tanja; Ivušić, Sarah; Telišman Prtenjak, Maja; Šoljan, Vinko; Horvat, Igor</p> <p>2018-03-01</p> <p>In this study, a synoptic and mesoscale analysis was performed and Szilagyi's waterspout forecasting method was tested on ten waterspout events in the period of 2013-2016. Data regarding waterspout occurrences were collected from <span class="hlt">weather</span> stations, an online survey at the official website of the National Meteorological and Hydrological Service of Croatia and eyewitness reports from newspapers and the internet. Synoptic <span class="hlt">weather</span> conditions were analyzed using surface pressure fields, 500 hPa level synoptic charts, SYNOP reports and atmospheric soundings. For all observed waterspout events, a synoptic type was determined using the 500 hPa geopotential height chart. The occurrence of lightning activity was determined from the LINET lightning database, and waterspouts were divided into thunderstorm-related and "fair <span class="hlt">weather</span>" ones. Mesoscale characteristics (with a focus on thermodynamic instability indices) were determined using the high-resolution (500 m grid length) mesoscale numerical <span class="hlt">weather</span> <span class="hlt">model</span> and <span class="hlt">model</span> results were compared with the available observations. Because thermodynamic instability indices are usually insufficient for forecasting waterspout activity, the performance of the Szilagyi Waterspout Index (SWI) was tested using vertical atmospheric profiles provided by the mesoscale numerical <span class="hlt">model</span>. The SWI successfully forecasted all waterspout events, even the winter events. This indicates that the Szilagyi's waterspout prognostic method could be used as a valid prognostic tool for the eastern Adriatic.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/20110012914','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/20110012914"><span>Using Satellite Data in <span class="hlt">Weather</span> Forecasting: I</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Jedlovec, Gary J.; Suggs, Ronnie J.; Lecue, Juan M.</p> <p>2006-01-01</p> <p>The GOES Product Generation <span class="hlt">System</span> (GPGS) is a set of computer codes and scripts that enable the assimilation of real-time Geostationary Operational Environmental Satellite (GOES) data into regional-<span class="hlt">weather</span>-forecasting mathematical <span class="hlt">models</span>. The GPGS can be used to derive such geophysical parameters as land surface temperature, the amount of precipitable water, the degree of cloud cover, the surface albedo, and the amount of insolation from satellite measurements of radiant energy emitted by the Earth and its atmosphere. GPGS incorporates a priori information (initial guesses of thermodynamic parameters of the atmosphere) and radiometric measurements from the geostationary operational environmental satellites along with mathematical <span class="hlt">models</span> of physical principles that govern the transfer of energy in the atmosphere. GPGS solves the radiative-transfer equation and provides the resulting data products in formats suitable for use by <span class="hlt">weather</span>-forecasting computer programs. The data-assimilation capability afforded by GPGS offers the potential to improve local <span class="hlt">weather</span> forecasts ranging from 3 hours to 2 days - especially with respect to temperature, humidity, cloud cover, and the probability of precipitation. The improvements afforded by GPGS could be of interest to news media, utility companies, and other organizations that utilize regional <span class="hlt">weather</span> forecasts.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2007SPIE.6557E..0CF','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2007SPIE.6557E..0CF"><span>New <span class="hlt">weather</span> depiction technology for night vision goggle (NVG) training: 3D virtual/augmented reality scene-<span class="hlt">weather</span>-atmosphere-target simulation</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Folaron, Michelle; Deacutis, Martin; Hegarty, Jennifer; Vollmerhausen, Richard; Schroeder, John; Colby, Frank P.</p> <p>2007-04-01</p> <p>US Navy and Marine Corps pilots receive Night Vision Goggle (NVG) training as part of their overall training to maintain the superiority of our forces. This training must incorporate realistic targets; backgrounds; and representative atmospheric and <span class="hlt">weather</span> effects they may encounter under operational conditions. An approach for pilot NVG training is to use the Night Imaging and Threat Evaluation Laboratory (NITE Lab) concept. The NITE Labs utilize a 10' by 10' static terrain <span class="hlt">model</span> equipped with both natural and cultural lighting that are used to demonstrate various illumination conditions, and visual phenomena which might be experienced when utilizing night vision goggles. With this technology, the military can safely, systematically, and reliably expose pilots to the large number of potentially dangerous environmental conditions that will be experienced in their NVG training flights. A previous SPIE presentation described our work for NAVAIR to add realistic atmospheric and <span class="hlt">weather</span> effects to the NVG NITE Lab training facility using the NVG - WDT(<span class="hlt">Weather</span> Depiction Technology) <span class="hlt">system</span> (Colby, et al.). NVG -WDT consist of a high end multiprocessor server with <span class="hlt">weather</span> simulation software, and several fixed and goggle mounted Heads Up Displays (HUDs). Atmospheric and <span class="hlt">weather</span> effects are simulated using state-of-the-art computer codes such as the WRF (<span class="hlt">Weather</span> Research μ Forecasting) <span class="hlt">model</span>; and the US Air Force Research Laboratory MODTRAN radiative transport <span class="hlt">model</span>. Imagery for a variety of natural and man-made obscurations (e.g. rain, clouds, snow, dust, smoke, chemical releases) are being calculated and injected into the scene observed through the NVG via the fixed and goggle mounted HUDs. This paper expands on the work described in the previous presentation and will describe the 3D Virtual/Augmented Reality Scene - <span class="hlt">Weather</span> - Atmosphere - Target Simulation part of the NVG - WDT. The 3D virtual reality software is a complete simulation <span class="hlt">system</span> to generate realistic</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2011AGUFMED43D..01G','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2011AGUFMED43D..01G"><span>Training Early Career Space <span class="hlt">Weather</span> Researchers and other Space <span class="hlt">Weather</span> Professionals at the CISM Space <span class="hlt">Weather</span> Summer School</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Gross, N. A.; Hughes, W.</p> <p>2011-12-01</p> <p>This talk will outline the organization of a summer school designed to introduce young professions to a sub-discipline of geophysics. Through out the 10 year life time of the Center for Integrated Space <span class="hlt">Weather</span> <span class="hlt">Modeling</span> (CISM) the CISM Team has offered a two week summer school that introduces new graduate students and other interested professional to the fundamentals of space <span class="hlt">weather</span>. The curriculum covers basic concepts in space physics, the hazards of space <span class="hlt">weather</span>, and the utility of computer <span class="hlt">models</span> of the space environment. Graduate students attend from both inside and outside CISM, from all the sub-disciplines involved in space <span class="hlt">weather</span> (solar, heliosphere, geomagnetic, and aeronomy), and from across the nation and around the world. In addition, between 1/4 and 1/3 of the participants each year are professionals involved in space <span class="hlt">weather</span> in some way, such as: forecasters from NOAA and the Air Force, Air Force satellite program directors, NASA specialists involved in astronaut radiation safety, and representatives from industries affected by space <span class="hlt">weather</span>. The summer school has adopted modern pedagogy that has been used successfully at the undergraduate level. A typical daily schedule involves three morning lectures followed by an afternoon lab session. During the morning lectures, student interaction is encouraged using "Timeout to Think" questions and peer instruction, along with question cards for students to ask follow up questions. During the afternoon labs students, working in groups of four, answer thought provoking questions using results from simulations and observation data from a variety of source. Through the interactions with each other and the instructors, as well as social interactions during the two weeks, students network and form bonds that will last them through out their careers. We believe that this summer school can be used as a <span class="hlt">model</span> for summer schools in a wide variety of disciplines.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/20010008274','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/20010008274"><span>AWE: Aviation <span class="hlt">Weather</span> Data Visualization Environment</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Spirkovska, Lilly; Lodha, Suresh K.</p> <p>2000-01-01</p> <p>The two official sources for aviation <span class="hlt">weather</span> reports both provide <span class="hlt">weather</span> information to a pilot in a textual format. A number of <span class="hlt">systems</span> have recently become available to help pilots with the visualization task by providing much of the data graphically. However, two types of aviation <span class="hlt">weather</span> data are still not being presented graphically. These are airport-specific current <span class="hlt">weather</span> reports (known as meteorological observations, or METARs) and forecast <span class="hlt">weather</span> reports (known as terminal area forecasts, or TAFs). Our <span class="hlt">system</span>, Aviation <span class="hlt">Weather</span> Environment (AWE), presents intuitive graphical displays for both METARs and TAFs, as well as winds aloft forecasts. We start with a computer-generated textual aviation <span class="hlt">weather</span> briefing. We map this briefing onto a cartographic grid specific to the pilot's area of interest. The pilot is able to obtain aviation-specific <span class="hlt">weather</span> for the entire area or for his specific route. The route, altitude, true airspeed, and proposed departure time can each be modified in AWE. Integral visual display of these three elements of <span class="hlt">weather</span> reports makes AWE a useful planning tool, as well as a <span class="hlt">weather</span> briefing tool.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/20000025078','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/20000025078"><span>An Initial Study of the Sensitivity of Aircraft Vortex Spacing <span class="hlt">System</span> (AVOSS) Spacing Sensitivity to <span class="hlt">Weather</span> and Configuration Input Parameters</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Riddick, Stephen E.; Hinton, David A.</p> <p>2000-01-01</p> <p>A study has been performed on a computer code <span class="hlt">modeling</span> an aircraft wake vortex spacing <span class="hlt">system</span> during final approach. This code represents an initial engineering <span class="hlt">model</span> of a <span class="hlt">system</span> to calculate reduced approach separation criteria needed to increase airport productivity. This report evaluates <span class="hlt">model</span> sensitivity toward various <span class="hlt">weather</span> conditions (crosswind, crosswind variance, turbulent kinetic energy, and thermal gradient), code configurations (approach corridor option, and wake demise definition), and post-processing techniques (rounding of provided spacing values, and controller time variance).</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://rosap.ntl.bts.gov/view/dot/25652','DOTNTL'); return false;" href="https://rosap.ntl.bts.gov/view/dot/25652"><span>Guidelines for disseminating road <span class="hlt">weather</span> messages.</span></a></p> <p><a target="_blank" href="http://ntlsearch.bts.gov/tris/index.do">DOT National Transportation Integrated Search</a></p> <p></p> <p>2010-06-01</p> <p>The tremendous growth in the amount of available <span class="hlt">weather</span> and road condition informationincluding devices that gather <span class="hlt">weather</span> information, <span class="hlt">models</span> and forecasting tools for predicting <span class="hlt">weather</span> conditions, and electronic devices used by travelersha...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2016EGUGA..1817203Q','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2016EGUGA..1817203Q"><span>Experimental geobiology links evolutionary intensification of rooting <span class="hlt">systems</span> and <span class="hlt">weathering</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Quirk, Joe; Beerling, David; Leake, Jonathan</p> <p>2016-04-01</p> <p>The evolution of mycorrhizal fungi in partnership with early land plants over 440 million years ago led to the greening of the continents by plants of increasing biomass, rooting depth, nutrient demand and capacity to alter soil minerals, culminating in modern forested ecosystems. The later co-evolution of trees and rooting <span class="hlt">systems</span> with arbuscular mycorrhizal (AM) fungi, together driving the biogeochemical cycling of elements and <span class="hlt">weathering</span> of minerals in soil to meet subsequent increased phosphorus demands is thought to constitute one the most important biotic feedbacks on the geochemical carbon cycle to emerge during the Phanerozoic, and fundamentally rests on the intensifying effect of trees and their root-associating mycorrhizal fungal partners on mineral <span class="hlt">weathering</span>. Here I present experimental and field evidence linking these evolutionary events to a mechanistic framework whereby: (1) as plants evolved in stature, biomass, and rooting depth, their mycorrhizal fungal partnerships received increasing amounts of plant photosynthate; (2) this enabled intensification of plant-driven fungal <span class="hlt">weathering</span> of rocks to release growth-limiting nutrients; (3) in turn, this increased land-to-ocean export of Ca and P and enhanced ocean carbonate precipitation impacting the global carbon cycle and biosphere-geosphere-ocean-atmosphere interactions over the past 410 Ma. Our findings support an over-arching hypothesis that evolution has selected plant and mycorrhizal partnerships that have intensified mineral <span class="hlt">weathering</span> and altered global biogeochemical cycles.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/20100036761','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/20100036761"><span><span class="hlt">Weather</span> Research and Forecasting <span class="hlt">Model</span> Wind Sensitivity Study at Edwards Air Force Base, CA</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Watson, Leela R.; Bauman, William H., III</p> <p>2008-01-01</p> <p>NASA prefers to land the space shuttle at Kennedy Space Center (KSC). When <span class="hlt">weather</span> conditions violate Flight Rules at KSC, NASA will usually divert the shuttle landing to Edwards Air Force Base (EAFB) in Southern California. But forecasting surface winds at EAFB is a challenge for the Spaceflight Meteorology Group (SMG) forecasters due to the complex terrain that surrounds EAFB, One particular phenomena identified by SMG is that makes it difficult to forecast the EAFB surface winds is called "wind cycling". This occurs when wind speeds and directions oscillate among towers near the EAFB runway leading to a challenging deorbit bum forecast for shuttle landings. The large-scale numerical <span class="hlt">weather</span> prediction <span class="hlt">models</span> cannot properly resolve the wind field due to their coarse horizontal resolutions, so a properly tuned high-resolution mesoscale <span class="hlt">model</span> is needed. The <span class="hlt">Weather</span> Research and Forecasting (WRF) <span class="hlt">model</span> meets this requirement. The AMU assessed the different WRF <span class="hlt">model</span> options to determine which configuration best predicted surface wind speed and direction at EAFB, To do so, the AMU compared the WRF <span class="hlt">model</span> performance using two hot start initializations with the Advanced Research WRF and Non-hydrostatic Mesoscale <span class="hlt">Model</span> dynamical cores and compared <span class="hlt">model</span> performance while varying the physics options.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/20110011477','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/20110011477"><span><span class="hlt">Weather</span> Research and Forecasting <span class="hlt">Model</span> Wind Sensitivity Study at Edwards Air Force Base, CA</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Watson, Leela R.; Bauman, William H., III; Hoeth, Brian</p> <p>2009-01-01</p> <p>This abstract describes work that will be done by the Applied Meteorology Unit (AMU) in assessing the success of different <span class="hlt">model</span> configurations in predicting "wind cycling" cases at Edwards Air Force Base, CA (EAFB), in which the wind speeds and directions oscillate among towers near the EAFB runway. The <span class="hlt">Weather</span> Research and Forecasting (WRF) <span class="hlt">model</span> allows users to choose among two dynamical cores - the Advanced Research WRF (ARW) and the Non-hydrostatic Mesoscale <span class="hlt">Model</span> (NMM). There are also data assimilation analysis packages available for the initialization of the WRF <span class="hlt">model</span> - the Local Analysis and Prediction <span class="hlt">System</span> (LAPS) and the Advanced Regional Prediction <span class="hlt">System</span> (ARPS) Data Analysis <span class="hlt">System</span> (ADAS). Having a series of initialization options and WRF cores, as well as many options within each core, creates challenges for local forecasters, such as determining which configuration options are best to address specific forecast concerns. The goal of this project is to assess the different configurations available and determine which configuration will best predict surface wind speed and direction at EAFB.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2010ems..confE.483N','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2010ems..confE.483N"><span>Graphical tools for TV <span class="hlt">weather</span> presentation</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Najman, M.</p> <p>2010-09-01</p> <p>Contemporary meteorology and its media presentation faces in my opinion following key tasks: - Delivering the meteorological information to the end user/spectator in understandable and modern fashion, which follows industry standard of video output (HD, 16:9) - Besides <span class="hlt">weather</span> icons show also the outputs of numerical <span class="hlt">weather</span> prediction <span class="hlt">models</span>, climatological data, satellite and radar images, observed <span class="hlt">weather</span> as actual as possible. - Does not compromise the accuracy of presented data. - Ability to prepare and adjust the <span class="hlt">weather</span> show according to actual synoptic situtation. - Ability to refocus and completely adjust the <span class="hlt">weather</span> show to actual extreme <span class="hlt">weather</span> events. - Ground map resolution <span class="hlt">weather</span> data presentation need to be at least 20 m/pixel to be able to follow the numerical <span class="hlt">weather</span> prediction <span class="hlt">model</span> resolution. - Ability to switch between different numerical <span class="hlt">weather</span> prediction <span class="hlt">models</span> each day, each show or even in the middle of one <span class="hlt">weather</span> show. - The graphical <span class="hlt">weather</span> software need to be flexible and fast. The graphical changes nee to be implementable and airable within minutes before the show or even live. These tasks are so demanding and the usual original approach of custom graphics could not deal with it. It was not able to change the show every day, the shows were static and identical day after day. To change the content of the <span class="hlt">weather</span> show daily was costly and most of the time impossible with the usual approach. The development in this area is fast though and there are several different options for <span class="hlt">weather</span> predicting organisations such as national meteorological offices and private meteorological companies to solve this problem. What are the ways to solve it? What are the limitations and advantages of contemporary graphical tools for meteorologists? All these questions will be answered.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.osti.gov/servlets/purl/1078057','SCIGOV-STC'); return false;" href="https://www.osti.gov/servlets/purl/1078057"><span><span class="hlt">Weather</span>-Corrected Performance Ratio</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>Dierauf, T.; Growitz, A.; Kurtz, S.</p> <p></p> <p>Photovoltaic (PV) <span class="hlt">system</span> performance depends on both the quality of the <span class="hlt">system</span> and the <span class="hlt">weather</span>. One simple way to communicate the <span class="hlt">system</span> performance is to use the performance ratio (PR): the ratio of the electricity generated to the electricity that would have been generated if the plant consistently converted sunlight to electricity at the level expected from the DC nameplate rating. The annual <span class="hlt">system</span> yield for flat-plate PV <span class="hlt">systems</span> is estimated by the product of the annual insolation in the plane of the array, the nameplate rating of the <span class="hlt">system</span>, and the PR, which provides an attractive way to estimatemore » expected annual <span class="hlt">system</span> yield. Unfortunately, the PR is, again, a function of both the PV <span class="hlt">system</span> efficiency and the <span class="hlt">weather</span>. If the PR is measured during the winter or during the summer, substantially different values may be obtained, making this metric insufficient to use as the basis for a performance guarantee when precise confidence intervals are required. This technical report defines a way to modify the PR calculation to neutralize biases that may be introduced by variations in the <span class="hlt">weather</span>, while still reporting a PR that reflects the annual PR at that site given the project design and the project <span class="hlt">weather</span> file. This resulting <span class="hlt">weather</span>-corrected PR gives more consistent results throughout the year, enabling its use as a metric for performance guarantees while still retaining the familiarity this metric brings to the industry and the value of its use in predicting actual annual <span class="hlt">system</span> yield. A testing protocol is also presented to illustrate the use of this new metric with the intent of providing a reference starting point for contractual content.« less</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/20080039447','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/20080039447"><span>A Goddard Multi-Scale <span class="hlt">Modeling</span> <span class="hlt">System</span> with Unified Physics</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Tao, W.K.; Anderson, D.; Atlas, R.; Chern, J.; Houser, P.; Hou, A.; Lang, S.; Lau, W.; Peters-Lidard, C.; Kakar, R.; <a style="text-decoration: none; " href="javascript:void(0); " onClick="displayelement('author_20080039447'); toggleEditAbsImage('author_20080039447_show'); toggleEditAbsImage('author_20080039447_hide'); "> <img style="display:inline; width:12px; height:12px; " src="images/arrow-up.gif" width="12" height="12" border="0" alt="hide" id="author_20080039447_show"> <img style="width:12px; height:12px; display:none; " src="images/arrow-down.gif" width="12" height="12" border="0" alt="hide" id="author_20080039447_hide"></p> <p>2008-01-01</p> <p>Numerical cloud resolving <span class="hlt">models</span> (CRMs), which are based the non-hydrostatic equations of motion, have been extensively applied to cloud-scale and mesoscale processes during the past four decades. Recent GEWEX Cloud <span class="hlt">System</span> Study (GCSS) <span class="hlt">model</span> comparison projects have indicated that CRMs agree with observations in simulating various types of clouds and cloud <span class="hlt">systems</span> from different geographic locations. Cloud resolving <span class="hlt">models</span> now provide statistical information useful for developing more realistic physically based parameterizations for climate <span class="hlt">models</span> and numerical <span class="hlt">weather</span> prediction <span class="hlt">models</span>. It is also expected that Numerical <span class="hlt">Weather</span> Prediction (NWP) and regional scale <span class="hlt">model</span> can be run in grid size similar to cloud resolving <span class="hlt">model</span> through nesting technique. Current and future NASA satellite programs can provide cloud, precipitation, aerosol and other data at very fine spatial and temporal scales. It requires a coupled global circulation <span class="hlt">model</span> (GCM) and cloud-scale <span class="hlt">model</span> (termed a szrper-parameterization or multi-scale <span class="hlt">modeling</span> -framework, MMF) to use these satellite data to improve the understanding of the physical processes that are responsible for the variation in global and regional climate and hydrological <span class="hlt">systems</span>. The use of a GCM will enable global coverage, and the use of a CRM will allow for better and more sophisticated physical parameterization. NASA satellite and field campaign can provide initial conditions as well as validation through utilizing the Earth Satellite simulators. At Goddard, we have developed a multi-scale <span class="hlt">modeling</span> <span class="hlt">system</span> with unified physics. The <span class="hlt">modeling</span> <span class="hlt">system</span> consists a coupled GCM-CRM (or MMF); a state-of-the-art <span class="hlt">weather</span> research forecast <span class="hlt">model</span> (WRF) and a cloud-resolving <span class="hlt">model</span> (Goddard Cumulus Ensemble <span class="hlt">model</span>). In these <span class="hlt">models</span>, the same microphysical schemes (2ICE, several 3ICE), radiation (including explicitly calculated cloud optical properties), and surface <span class="hlt">models</span> are applied. In addition, a comprehensive unified Earth Satellite</p> </li> </ol> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_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://hdl.handle.net/2060/20160005026','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/20160005026"><span>Initial Analysis of and Predictive <span class="hlt">Model</span> Development for <span class="hlt">Weather</span> Reroute Advisory Use</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Arneson, Heather M.</p> <p>2016-01-01</p> <p>In response to severe <span class="hlt">weather</span> conditions, traffic management coordinators specify reroutes to route air traffic around affected regions of airspace. Providing analysis and recommendations of available reroute options would assist the traffic management coordinators in making more efficient rerouting decisions. These recommendations can be developed by examining historical data to determine which previous reroute options were used in similar <span class="hlt">weather</span> and traffic conditions. Essentially, using previous information to inform future decisions. This paper describes the initial steps and methodology used towards this goal. A method to extract relevant features from the large volume of <span class="hlt">weather</span> data to quantify the convective <span class="hlt">weather</span> scenario during a particular time range is presented. Similar routes are clustered. A description of the algorithm to identify which cluster of reroute advisories were actually followed by pilots is described. <span class="hlt">Models</span> built for fifteen of the top twenty most frequently used reroute clusters correctly predict the use of the cluster for over 60 of the test examples. Results are preliminary but indicate that the methodology is worth pursuing with modifications based on insight gained from this analysis.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/23932695','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/23932695"><span>Identifying crash-prone traffic conditions under different <span class="hlt">weather</span> on freeways.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Xu, Chengcheng; Wang, Wei; Liu, Pan</p> <p>2013-09-01</p> <p>Understanding the relationships between traffic flow characteristics and crash risk under adverse <span class="hlt">weather</span> conditions will help highway agencies develop proactive safety management strategies to improve traffic safety in adverse <span class="hlt">weather</span> conditions. The primary objective is to develop separate crash risk prediction <span class="hlt">models</span> for different <span class="hlt">weather</span> conditions. The crash data, <span class="hlt">weather</span> data, and traffic data used in this study were collected on the I-880N freeway in California in 2008 and 2010. This study considered three different <span class="hlt">weather</span> conditions: clear <span class="hlt">weather</span>, rainy <span class="hlt">weather</span>, and reduced visibility <span class="hlt">weather</span>. The preliminary analysis showed that there was some heterogeneity in the risk estimates for traffic flow characteristics by <span class="hlt">weather</span> conditions, and that the crash risk prediction <span class="hlt">model</span> for all <span class="hlt">weather</span> conditions cannot capture the impacts of the traffic flow variables on crash risk under adverse <span class="hlt">weather</span> conditions. The Bayesian random intercept logistic regression <span class="hlt">models</span> were applied to link the likelihood of crash occurrence with various traffic flow characteristics under different <span class="hlt">weather</span> conditions. The crash risk prediction <span class="hlt">models</span> were compared to their corresponding logistic regression <span class="hlt">model</span>. It was found that the random intercept <span class="hlt">model</span> improved the goodness-of-fit of the crash risk prediction <span class="hlt">models</span>. The <span class="hlt">model</span> estimation results showed that the traffic flow characteristics contributing to crash risk were different across different <span class="hlt">weather</span> conditions. The speed difference between upstream and downstream stations was found to be significant in each crash risk prediction <span class="hlt">model</span>. Speed difference between upstream and downstream stations had the largest impact on crash risk in reduced visibility <span class="hlt">weather</span>, followed by that in rainy <span class="hlt">weather</span>. The ROC curves were further developed to evaluate the predictive performance of the crash risk prediction <span class="hlt">models</span> under different <span class="hlt">weather</span> conditions. The predictive performance of the crash risk <span class="hlt">model</span> for clear <span class="hlt">weather</span> was better</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/20010092181','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/20010092181"><span>AWE: Aviation <span class="hlt">Weather</span> Data Visualization Environment</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Spirkovska, Lilly; Lodha, Suresh K.; Norvig, Peter (Technical Monitor)</p> <p>2000-01-01</p> <p><span class="hlt">Weather</span> is one of the major causes of aviation accidents. General aviation (GA) flights account for 92% of all the aviation accidents, In spite of all the official and unofficial sources of <span class="hlt">weather</span> visualization tools available to pilots, there is an urgent need for visualizing several <span class="hlt">weather</span> related data tailored for general aviation pilots. Our <span class="hlt">system</span>, Aviation <span class="hlt">Weather</span> Data Visualization Environment AWE), presents graphical displays of meteorological observations, terminal area forecasts, and winds aloft forecasts onto a cartographic grid specific to the pilot's area of interest. Decisions regarding the graphical display and design are made based on careful consideration of user needs. Integral visual display of these elements of <span class="hlt">weather</span> reports is designed for the use of GA pilots as a <span class="hlt">weather</span> briefing and route selection tool. AWE provides linking of the <span class="hlt">weather</span> information to the flight's path and schedule. The pilot can interact with the <span class="hlt">system</span> to obtain aviation-specific <span class="hlt">weather</span> for the entire area or for his specific route to explore what-if scenarios and make "go/no-go" decisions. The <span class="hlt">system</span>, as evaluated by some pilots at NASA Ames Research Center, was found to be useful.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017AGUFMIN43C0091F','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017AGUFMIN43C0091F"><span>Forecasting Space <span class="hlt">Weather</span>-Induced GPS Performance Degradation Using Random Forest</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Filjar, R.; Filic, M.; Milinkovic, F.</p> <p>2017-12-01</p> <p>Space <span class="hlt">weather</span> and ionospheric dynamics have a profound effect on positioning performance of the Global Satellite Navigation <span class="hlt">System</span> (GNSS). However, the quantification of that effect is still the subject of scientific activities around the world. In the latest contribution to the understanding of the space <span class="hlt">weather</span> and ionospheric effects on satellite-based positioning performance, we conducted a study of several candidates for forecasting method for space <span class="hlt">weather</span>-induced GPS positioning performance deterioration. First, a 5-days set of experimentally collected data was established, encompassing the space <span class="hlt">weather</span> and ionospheric activity indices (including: the readings of the Sudden Ionospheric Disturbance (SID) monitors, components of geomagnetic field strength, global Kp index, Dst index, GPS-derived Total Electron Content (TEC) samples, standard deviation of TEC samples, and sunspot number) and observations of GPS positioning error components (northing, easting, and height positioning error) derived from the Adriatic Sea IGS reference stations' RINEX raw pseudorange files in quiet space <span class="hlt">weather</span> periods. This data set was split into the training and test sub-sets. Then, a selected set of supervised machine learning methods based on Random Forest was applied to the experimentally collected data set in order to establish the appropriate regional (the Adriatic Sea) forecasting <span class="hlt">models</span> for space <span class="hlt">weather</span>-induced GPS positioning performance deterioration. The forecasting <span class="hlt">models</span> were developed in the R/rattle statistical programming environment. The forecasting quality of the regional forecasting <span class="hlt">models</span> developed was assessed, and the conclusions drawn on the advantages and shortcomings of the regional forecasting <span class="hlt">models</span> for space <span class="hlt">weather</span>-caused GNSS positioning performance deterioration.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/20020038769','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/20020038769"><span>Implications of Automotive and Trucking On-Board Information <span class="hlt">Systems</span> for General Aviation Cockpit <span class="hlt">Weather</span> <span class="hlt">Systems</span></span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Sireli, Yesim; Kauffmann, Paul; Gupta, Surabhi; Kachroo, Pushkin</p> <p>2002-01-01</p> <p>In this study, current characteristics and future developments of Intelligent Transportation <span class="hlt">Systems</span> (ITS) in the automobile and trucking industry are investigated to identify the possible implications of such <span class="hlt">systems</span> for General Aviation (GA) cockpit <span class="hlt">weather</span> <span class="hlt">systems</span>. First, ITS are explained based on tracing their historical development in various countries. Then, current <span class="hlt">systems</span> and the enabling communication technologies are discussed. Finally, a market analysis for GA is included.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2010ems..confE.616A','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2010ems..confE.616A"><span>Utilization of Live Localized <span class="hlt">Weather</span> Information for Sustainable Agriculture</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Anderson, J.; Usher, J.</p> <p>2010-09-01</p> <p>Authors: Jim Anderson VP, Global Network and Business Development <span class="hlt">Weather</span>Bug® Professional Jeremy Usher Managing Director, Europe <span class="hlt">Weather</span>Bug® Professional Localized, real-time <span class="hlt">weather</span> information is vital for day-to-day agronomic management of all crops. The challenge for agriculture is twofold in that local and timely <span class="hlt">weather</span> data is not often available for producers and farmers, and it is not integrated into decision-support tools they require. Many of the traditional sources of <span class="hlt">weather</span> information are not sufficient for agricultural applications because of the long distances between <span class="hlt">weather</span> stations, meaning the data is not always applicable for on-farm decision making processes. The second constraint with traditional <span class="hlt">weather</span> information is the timeliness of the data. Most delivery <span class="hlt">systems</span> are designed on a one-hour time step, whereas many decisions in agriculture are based on minute-by-minute <span class="hlt">weather</span> conditions. This is especially true for decisions surrounding chemical and fertilizer application and frost events. This presentation will outline how the creation of an agricultural mesonet (<span class="hlt">weather</span> network) can enable producers and farmers with live, local <span class="hlt">weather</span> information from <span class="hlt">weather</span> stations installed in farm/field locations. The live <span class="hlt">weather</span> information collected from each <span class="hlt">weather</span> station is integrated into a web-enabled decision support tool, supporting numerous on-farm agronomic activities such as pest management, or dealing with heavy rainfall and frost events. Agronomic <span class="hlt">models</span> can be used to assess the potential of disease pressure, enhance the farmer's abilities to time pesticide applications, or assess conditions contributing to yield and quality fluctuations. Farmers and industry stakeholders may also view quality-assured historical <span class="hlt">weather</span> variables at any location. This serves as a record-management tool for viewing previously uncharted agronomic <span class="hlt">weather</span> events in graph or table form. This set of <span class="hlt">weather</span> tools is unique and provides a</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.osti.gov/servlets/purl/1184931','SCIGOV-STC'); return false;" href="https://www.osti.gov/servlets/purl/1184931"><span>HESFIRE: a global fire <span class="hlt">model</span> to explore the role of anthropogenic and <span class="hlt">weather</span> drivers</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>Le Page, Yannick LB; Morton, Douglas; Bond-Lamberty, Benjamin</p> <p></p> <p>Vegetation fires are a major driver of ecosystem dynamics and greenhouse gas emissions. Anticipating potential changes in fire activity and their impacts relies first on a realistic <span class="hlt">model</span> of fire activity (e.g., fire incidence and interannual variability) and second on a <span class="hlt">model</span> accounting for fire impacts (e.g., mortality and emissions). In this paper, we focus on our understanding of fire activity and describe a new fire <span class="hlt">model</span>, HESFIRE (Human–Earth <span class="hlt">System</span> FIRE), which integrates the influence of <span class="hlt">weather</span>, vegetation characteristics, and human activities on fires in a stand-alone framework. It was developed with a particular emphasis on allowing fires to spreadmore » over consecutive days given their major contribution to burned areas in many ecosystems. A subset of the <span class="hlt">model</span> parameters was calibrated through an optimization procedure using observation data to enhance our knowledge of regional drivers of fire activity and improve the performance of the <span class="hlt">model</span> on a global scale. <span class="hlt">Modeled</span> fire activity showed reasonable agreement with observations of burned area, fire seasonality, and interannual variability in many regions, including for spatial and temporal domains not included in the optimization procedure. Significant discrepancies are investigated, most notably regarding fires in boreal regions and in xeric ecosystems and also fire size distribution. The sensitivity of fire activity to <span class="hlt">model</span> parameters is analyzed to explore the dominance of specific drivers across regions and ecosystems. The characteristics of HESFIRE and the outcome of its evaluation provide insights into the influence of anthropogenic activities and <span class="hlt">weather</span>, and their interactions, on fire activity.« less</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.osti.gov/pages/biblio/1184931-hesfire-global-fire-model-explore-role-anthropogenic-weather-drivers','SCIGOV-DOEP'); return false;" href="https://www.osti.gov/pages/biblio/1184931-hesfire-global-fire-model-explore-role-anthropogenic-weather-drivers"><span>HESFIRE: a global fire <span class="hlt">model</span> to explore the role of anthropogenic and <span class="hlt">weather</span> drivers</span></a></p> <p><a target="_blank" href="http://www.osti.gov/pages">DOE PAGES</a></p> <p>Le Page, Yannick LB; Morton, Douglas; Bond-Lamberty, Benjamin; ...</p> <p>2015-02-13</p> <p>Vegetation fires are a major driver of ecosystem dynamics and greenhouse gas emissions. Anticipating potential changes in fire activity and their impacts relies first on a realistic <span class="hlt">model</span> of fire activity (e.g., fire incidence and interannual variability) and second on a <span class="hlt">model</span> accounting for fire impacts (e.g., mortality and emissions). In this paper, we focus on our understanding of fire activity and describe a new fire <span class="hlt">model</span>, HESFIRE (Human–Earth <span class="hlt">System</span> FIRE), which integrates the influence of <span class="hlt">weather</span>, vegetation characteristics, and human activities on fires in a stand-alone framework. It was developed with a particular emphasis on allowing fires to spreadmore » over consecutive days given their major contribution to burned areas in many ecosystems. A subset of the <span class="hlt">model</span> parameters was calibrated through an optimization procedure using observation data to enhance our knowledge of regional drivers of fire activity and improve the performance of the <span class="hlt">model</span> on a global scale. <span class="hlt">Modeled</span> fire activity showed reasonable agreement with observations of burned area, fire seasonality, and interannual variability in many regions, including for spatial and temporal domains not included in the optimization procedure. Significant discrepancies are investigated, most notably regarding fires in boreal regions and in xeric ecosystems and also fire size distribution. The sensitivity of fire activity to <span class="hlt">model</span> parameters is analyzed to explore the dominance of specific drivers across regions and ecosystems. The characteristics of HESFIRE and the outcome of its evaluation provide insights into the influence of anthropogenic activities and <span class="hlt">weather</span>, and their interactions, on fire activity.« less</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2006cosp...36.2522P','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2006cosp...36.2522P"><span>CAWSES (Climate and <span class="hlt">Weather</span> of the Sun-Earth <span class="hlt">System</span>) Science: Progress thus far and the next steps</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Pallamraju, D.; Kozyra, J.; Basu, S.</p> <p></p> <p>Climate and <span class="hlt">Weather</span> of the Sun Earth <span class="hlt">System</span> CAWSES is the current program of Scientific Committee for Solar Terrestrial Physics SCOSTEP for 2004 - 2008 The main aim of CAWSES is to bring together scientists from various nations to address the coupled and global nature of the Sun-Earth <span class="hlt">System</span> phenomena Towards that end CAWSES provides a platform for international cooperation in observations data analysis theory and <span class="hlt">modeling</span> There has been active international participation thus far with endorsement of the national CAWSES programs in some countries and many scientists around the globe actively volunteering their time in this effort The CAWSES Science Steering Group has organized the CAWSES program into five Themes for better execution of its science Solar Influence on Climate Space <span class="hlt">Weather</span> Science and Applications Atmospheric Coupling Processes Space Climatology and Capacity Building and Education CAWSES will cooperate with International programs that focus on the Sun-Earth <span class="hlt">system</span> science and at the same time compliment the work of programs whose scope is beyond the realm of CAWSES This talk will briefly review the science goals of CAWSES provide salient results from different Themes with emphasis on those from the Space <span class="hlt">Weather</span> Theme This talk will also indicate the next steps that are being planned in this program and solicit inputs from the community for the science efforts to be carried out in the future</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/20010069502','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/20010069502"><span>Satellite Delivery of Aviation <span class="hlt">Weather</span> Data</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Kerczewski, Robert J.; Haendel, Richard</p> <p>2001-01-01</p> <p>With aviation traffic continuing to increase worldwide, reducing the aviation accident rate and aviation schedule delays is of critical importance. In the United States, the National Aeronautics and Space Administration (NASA) has established the Aviation Safety Program and the Aviation <span class="hlt">System</span> Capacity Program to develop and test new technologies to increase aviation safety and <span class="hlt">system</span> capacity. <span class="hlt">Weather</span> is a significant contributor to aviation accidents and schedule delays. The timely dissemination of <span class="hlt">weather</span> information to decision makers in the aviation <span class="hlt">system</span>, particularly to pilots, is essential in reducing <span class="hlt">system</span> delays and <span class="hlt">weather</span> related aviation accidents. The NASA Glenn Research Center is investigating improved methods of <span class="hlt">weather</span> information dissemination through satellite broadcasting directly to aircraft. This paper describes an on-going cooperative research program with NASA, Rockwell Collins, WorldSpace, Jeppesen and American Airlines to evaluate the use of satellite digital audio radio service (SDARS) for low cost broadcast of aviation <span class="hlt">weather</span> information, called Satellite <span class="hlt">Weather</span> Information Service (SWIS). The description and results of the completed SWIS Phase 1 are presented, and the description of the on-going SWIS Phase 2 is given.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2006AGUFMSA53A1348F','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2006AGUFMSA53A1348F"><span>Aviation & Space <span class="hlt">Weather</span> Policy Research: Integrating Space <span class="hlt">Weather</span> Observations & Forecasts into Operations</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Fisher, G.; Jones, B.</p> <p>2006-12-01</p> <p>The American Meteorological Society and SolarMetrics Limited are conducting a policy research project leading to recommendations that will increase the safety, reliability, and efficiency of the nation's airline operations through more effective use of space <span class="hlt">weather</span> forecasts and information. This study, which is funded by a 3-year National Science Foundation grant, also has the support of the Federal Aviation Administration and the Joint Planning and Development Office (JPDO) who is planning the Next Generation Air Transportation <span class="hlt">System</span>. A major component involves interviewing and bringing together key people in the aviation industry who deal with space <span class="hlt">weather</span> information. This research also examines public and industrial strategies and plans to respond to space <span class="hlt">weather</span> information. The focus is to examine policy issues in implementing effective application of space <span class="hlt">weather</span> services to the management of the nation's aviation <span class="hlt">system</span>. The results from this project will provide government and industry leaders with additional tools and information to make effective decisions with respect to investments in space <span class="hlt">weather</span> research and services. While space <span class="hlt">weather</span> can impact the entire aviation industry, and this project will address national and international issues, the primary focus will be on developing a U.S. perspective for the airlines.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017spwe.book.....H','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017spwe.book.....H"><span>Space <span class="hlt">Weather</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Hapgood, Mike</p> <p>2017-01-01</p> <p>Space <span class="hlt">weather</span>-changes in the Earth's environment that can often be traced to physical processes in the Sun-can have a profound impact on critical Earth-based infrastructures such as power grids and civil aviation. Violent eruptions on the solar surface can eject huge clouds of magnetized plasma and particle radiation, which then propagate across interplanetary space and envelop the Earth. These space <span class="hlt">weather</span> events can drive major changes in a variety of terrestrial environments, which can disrupt, or even damage, many of the technological <span class="hlt">systems</span> that underpin modern societies. The aim of this book is to offer an insight into our current scientific understanding of space <span class="hlt">weather</span>, and how we can use that knowledge to mitigate the risks it poses for Earth-based technologies. It also identifies some key challenges for future space-<span class="hlt">weather</span> research, and considers how emerging technological developments may introduce new risks that will drive continuing investigation.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/19980107900','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/19980107900"><span>The <span class="hlt">Weathering</span> of Antarctic Meteorites: Climatic Controls on <span class="hlt">Weathering</span> Rates and Implications for Meteorite Accumulation</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Benoit, P. H.; Akridge, J. M. C.; Sears, D. W. G.; Bland, P. A.</p> <p>1995-01-01</p> <p><span class="hlt">Weathering</span> of meteorites includes a variety of chemical and mineralogical changes, including conversion of metal to iron oxides, or rust. Other changes include the devitrification of glass, especially in fusion crust. On a longer time scale, major minerals such as olivine, pyroxene, and feldspar are partially or wholly converted to various phyllosilicates. The degree of <span class="hlt">weathering</span> of meteorite finds is often noted using a qualitative <span class="hlt">system</span> based on visual inspection of hand specimens. Several quantitative <span class="hlt">weathering</span> classification <span class="hlt">systems</span> have been proposed or are currently under development. Wlotzka has proposed a classification <span class="hlt">system</span> based on mineralogical changes observed in polished sections and Mossbauer properties of meteorite powders have also been used. In the current paper, we discuss induced thermoluminescence (TL) as an indicator of degree of <span class="hlt">weathering</span> of individual meteorites. The quantitative measures of <span class="hlt">weathering</span>, including induced TL, suffer from one major flaw, namely that their results only apply to small portions of the meteorite.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2016AGUFM.A21D0101H','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2016AGUFM.A21D0101H"><span>Assimilation of Cloud Information in Numerical <span class="hlt">Weather</span> Prediction <span class="hlt">Model</span> in Southwest China</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>HENG, Z.</p> <p>2016-12-01</p> <p>Based on the ARPS Data Analysis <span class="hlt">System</span> (ADAS), <span class="hlt">Weather</span> Research and Forecasting (WRF) <span class="hlt">model</span>, simulation experiments from July 1st 2015 to August 1st 2015 are conducted in the region of Southwest China. In the assimilation experiment (EXP), datasets from surface observations are assimilated, cloud information from <span class="hlt">weather</span> Doppler radar, Fengyun-2E (FY-2E) geostationary satellite are retrieved by using the complex cloud analysis scheme in the ADAS, to insert microphysical variables and adjust the humility structure in the initial condition. As a control run (CTL), datasets from surface observations are assimilated, but no cloud information is used in the ADAS. The simulation result of a rainstorm caused by the Southwest Vortex during 14-15 July 2015 shows that, the EXP run has a better capability in representing the shape and intensity of precipitation, especially the center of rainstorm. The one-month inter-comparison of the initial and prediction results between the EXP and CTL runs reveled that, EXP runs can present a more reasonable phenomenon of rain and get a higher score in the rain prediction. Keywords: NWP, rainstorm, Data assimilation</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017AtmRe.198..194K','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017AtmRe.198..194K"><span>Prediction skill of rainstorm events over India in the TIGGE <span class="hlt">weather</span> prediction <span class="hlt">models</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Karuna Sagar, S.; Rajeevan, M.; Vijaya Bhaskara Rao, S.; Mitra, A. K.</p> <p>2017-12-01</p> <p>Extreme rainfall events pose a serious threat of leading to severe floods in many countries worldwide. Therefore, advance prediction of its occurrence and spatial distribution is very essential. In this paper, an analysis has been made to assess the skill of numerical <span class="hlt">weather</span> prediction <span class="hlt">models</span> in predicting rainstorms over India. Using gridded daily rainfall data set and objective criteria, 15 rainstorms were identified during the monsoon season (June to September). The analysis was made using three TIGGE (THe Observing <span class="hlt">System</span> Research and Predictability Experiment (THORPEX) Interactive Grand Global Ensemble) <span class="hlt">models</span>. The <span class="hlt">models</span> considered are the European Centre for Medium-Range <span class="hlt">Weather</span> Forecasts (ECMWF), National Centre for Environmental Prediction (NCEP) and the UK Met Office (UKMO). Verification of the TIGGE <span class="hlt">models</span> for 43 observed rainstorm days from 15 rainstorm events has been made for the period 2007-2015. The comparison reveals that rainstorm events are predictable up to 5 days in advance, however with a bias in spatial distribution and intensity. The statistical parameters like mean error (ME) or Bias, root mean square error (RMSE) and correlation coefficient (CC) have been computed over the rainstorm region using the multi-<span class="hlt">model</span> ensemble (MME) mean. The study reveals that the spread is large in ECMWF and UKMO followed by the NCEP <span class="hlt">model</span>. Though the ensemble spread is quite small in NCEP, the ensemble member averages are not well predicted. The rank histograms suggest that the forecasts are under prediction. The modified Contiguous Rain Area (CRA) technique was used to verify the spatial as well as the quantitative skill of the TIGGE <span class="hlt">models</span>. Overall, the contribution from the displacement and pattern errors to the total RMSE is found to be more in magnitude. The volume error increases from 24 hr forecast to 48 hr forecast in all the three <span class="hlt">models</span>.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2016AMT.....9..841L','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2016AMT.....9..841L"><span><span class="hlt">Modeling</span> the Zeeman effect in high-altitude SSMIS channels for numerical <span class="hlt">weather</span> prediction profiles: comparing a fast <span class="hlt">model</span> and a line-by-line <span class="hlt">model</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Larsson, Richard; Milz, Mathias; Rayer, Peter; Saunders, Roger; Bell, William; Booton, Anna; Buehler, Stefan A.; Eriksson, Patrick; John, Viju O.</p> <p>2016-03-01</p> <p>We present a comparison of a reference and a fast radiative transfer <span class="hlt">model</span> using numerical <span class="hlt">weather</span> prediction profiles for the Zeeman-affected high-altitude Special Sensor Microwave Imager/Sounder channels 19-22. We find that the <span class="hlt">models</span> agree well for channels 21 and 22 compared to the channels' <span class="hlt">system</span> noise temperatures (1.9 and 1.3 K, respectively) and the expected profile errors at the affected altitudes (estimated to be around 5 K). For channel 22 there is a 0.5 K average difference between the <span class="hlt">models</span>, with a standard deviation of 0.24 K for the full set of atmospheric profiles. Concerning the same channel, there is 1.2 K on average between the fast <span class="hlt">model</span> and the sensor measurement, with 1.4 K standard deviation. For channel 21 there is a 0.9 K average difference between the <span class="hlt">models</span>, with a standard deviation of 0.56 K. Regarding the same channel, there is 1.3 K on average between the fast <span class="hlt">model</span> and the sensor measurement, with 2.4 K standard deviation. We consider the relatively small <span class="hlt">model</span> differences as a validation of the fast Zeeman effect scheme for these channels. Both channels 19 and 20 have smaller average differences between the <span class="hlt">models</span> (at below 0.2 K) and smaller standard deviations (at below 0.4 K) when both <span class="hlt">models</span> use a two-dimensional magnetic field profile. However, when the reference <span class="hlt">model</span> is switched to using a full three-dimensional magnetic field profile, the standard deviation to the fast <span class="hlt">model</span> is increased to almost 2 K due to viewing geometry dependencies, causing up to ±7 K differences near the equator. The average differences between the two <span class="hlt">models</span> remain small despite changing magnetic field configurations. We are unable to compare channels 19 and 20 to sensor measurements due to limited altitude range of the numerical <span class="hlt">weather</span> prediction profiles. We recommended that numerical <span class="hlt">weather</span> prediction software using the fast <span class="hlt">model</span> takes the available fast Zeeman scheme into account for data assimilation of the affected sensor channels to</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2013AGUFM.B13B0461F','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2013AGUFM.B13B0461F"><span>Seafloor <span class="hlt">weathering</span> buffering climate: numerical experiments</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Farahat, N. X.; Archer, D. E.; Abbot, D. S.</p> <p>2013-12-01</p> <p>Continental silicate <span class="hlt">weathering</span> is widely held to consume atmospheric CO2 at a rate controlled in part by temperature, resulting in a climate-<span class="hlt">weathering</span> feedback [Walker et al., 1981]. It has been suggested that <span class="hlt">weathering</span> of oceanic crust of warm mid-ocean ridge flanks also has a CO2 uptake rate that is controlled by climate [Sleep and Zahnle, 2001; Brady and Gislason, 1997]. Although this effect might not be significant on present-day Earth [Caldeira, 1995], seafloor <span class="hlt">weathering</span> may be more pronounced during snowball states [Le Hir et al., 2008], during the Archean when seafloor spreading rates were faster [Sleep and Zahnle, 2001], and on waterworld planets [Abbot et al., 2012]. Previous studies of seafloor <span class="hlt">weathering</span> have made significant contributions using qualitative, generally one-box, <span class="hlt">models</span>, and the logical next step is to extend this work using a spatially resolved <span class="hlt">model</span>. For example, experiments demonstrate that seafloor <span class="hlt">weathering</span> reactions are temperature dependent, but it is not clear whether the deep ocean temperature affects the temperature at which the reactions occur, or if instead this temperature is set only by geothermal processes. Our goal is to develop a 2-D numerical <span class="hlt">model</span> that can simulate hydrothermal circulation and resulting alteration of oceanic basalts, and can therefore address such questions. A <span class="hlt">model</span> of diffusive and convective heat transfer in fluid-saturated porous media simulates hydrothermal circulation through porous oceanic basalt. Unsteady natural convection is solved for using a Darcy <span class="hlt">model</span> of porous media flow that has been extensively benchmarked. Background hydrothermal circulation is coupled to mineral reaction kinetics of basaltic alteration and hydrothermal mineral precipitation. In order to quantify seafloor <span class="hlt">weathering</span> as a climate-<span class="hlt">weathering</span> feedback process, this <span class="hlt">model</span> focuses on hydrothermal reactions that influence carbon uptake as well as ocean alkalinity: silicate rock dissolution, calcium and magnesium leaching</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2012EGUGA..1413219L','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2012EGUGA..1413219L"><span>Do GCM's predict the climate.... Or the low frequency <span class="hlt">weather</span>?</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Lovejoy, S.; Schertzer, D.; Varon, D.</p> <p>2012-04-01</p> <p> control runs (i.e. without climate forcing) of GCM based climate forecasting <span class="hlt">systems</span> including those of the Institut Pierre Simon Laplace (Paris) and the Earth Forecasting <span class="hlt">System</span> (Hamburg). In order for these <span class="hlt">systems</span> to go beyond simply predicting low frequency <span class="hlt">weather</span> i.e. in order for them to predict the climate, they need appropriate climate forcings and/ or new internal mechanisms of variability. Using statistical scaling techniques we examine the scale dependence of fluctuations from forced and unforced GCM outputs, including from the ECHO-G and EFS simulations in the Millenium climate reconstruction project and compare this with data, multiproxies and paleo data. Our general conclusion is that the <span class="hlt">models</span> systematically underestimate the multidecadal, multicentennial scale variability.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://rosap.ntl.bts.gov/view/dot/3369','DOTNTL'); return false;" href="https://rosap.ntl.bts.gov/view/dot/3369"><span>Implementation and Evaluation of <span class="hlt">Weather</span> Responsive Traffic Estimation and Prediction <span class="hlt">System</span></span></a></p> <p><a target="_blank" href="http://ntlsearch.bts.gov/tris/index.do">DOT National Transportation Integrated Search</a></p> <p></p> <p>2012-06-01</p> <p>The objective of the project is to develop a framework and procedures for implementing and evaluating <span class="hlt">weather</span>-responsive traffic management (WRTM) strategies using Traffic Estimation and Prediction <span class="hlt">System</span> (TrEPS) methodologies. In a previous FHWA-fun...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://rosap.ntl.bts.gov/view/dot/3769','DOTNTL'); return false;" href="https://rosap.ntl.bts.gov/view/dot/3769"><span>Evaluation of the Idaho Transportation Department integrated road-<span class="hlt">weather</span> information <span class="hlt">system</span></span></a></p> <p><a target="_blank" href="http://ntlsearch.bts.gov/tris/index.do">DOT National Transportation Integrated Search</a></p> <p></p> <p>2005-02-02</p> <p>This report presents the results of FHWA's evaluation of the Idaho Transportation Department's (ITD) integration of its Road-<span class="hlt">Weather</span> Information <span class="hlt">System</span> (RWIS). The ITD RWIS project was selected for evaluation because it held significant potential to ...</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://www.nws.noaa.gov/predictions.php','SCIGOVWS'); return false;" href="http://www.nws.noaa.gov/predictions.php"><span>Climate Prediction - NOAA's National <span class="hlt">Weather</span> Service</span></a></p> <p><a target="_blank" href="http://www.science.gov/aboutsearch.html">Science.gov Websites</a></p> <p></p> <p></p> <p>Statistical <span class="hlt">Models</span>... MOS Prod GFS-LAMP Prod <em>Climate</em> Past <span class="hlt">Weather</span> Predictions <span class="hlt">Weather</span> Safety <span class="hlt">Weather</span> Radio National <span class="hlt">Weather</span> Service on FaceBook NWS on Facebook NWS Director Home > <em>Climate</em> > Predictions <em>Climate</em> Prediction Long range forecasts across the U.S. <em>Climate</em> Prediction Web Sites <em>Climate</em> Prediction</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://www.nws.noaa.gov/om/marine/wxsat.htm','SCIGOVWS'); return false;" href="http://www.nws.noaa.gov/om/marine/wxsat.htm"><span>NOAA <span class="hlt">WEATHER</span> SATELLITES</span></a></p> <p><a target="_blank" href="http://www.science.gov/aboutsearch.html">Science.gov Websites</a></p> <p></p> <p></p> <p>extent of snow cover. In addition, <em>satellite</em> <em>sensors</em> detect ice fields and map the movement of sea and greater danger near shore or any shallow waters? NATIONAL <span class="hlt">WEATHER</span> SERVICE <em>SATELLITE</em> PRODUCTS NOAA's operational <span class="hlt">weather</span> <em>satellite</em> <span class="hlt">system</span> is composed of two types of satellites: geostationary operational</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2010nspm.conf..162V','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2010nspm.conf..162V"><span>Space <span class="hlt">weather</span> <span class="hlt">modeling</span> using artificial neural network. (Slovak Title: Modelovanie kozmického počasia umelou neurónovou sietou)</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Valach, F.; Revallo, M.; Hejda, P.; Bochníček, J.</p> <p>2010-12-01</p> <p>Our modern society with its advanced technology is becoming increasingly vulnerable to the Earth's <span class="hlt">system</span> disorders originating in explosive processes on the Sun. Coronal mass ejections (CMEs) blasted into interplanetary space as gigantic clouds of ionized gas can hit Earth within a few hours or days and cause, among other effects, geomagnetic storms - perhaps the best known manifestation of solar wind interaction with Earth's magnetosphere. Solar energetic particles (SEP), accelerated to near relativistic energy during large solar storms, arrive at the Earth's orbit even in few minutes and pose serious risk to astronauts traveling through the interplanetary space. These and many other threats are the reason why experts pay increasing attention to space <span class="hlt">weather</span> and its predictability. For research on space <span class="hlt">weather</span>, it is typically necessary to examine a large number of parameters which are interrelated in a complex non-linear way. One way to cope with such a task is to use an artificial neural network for space <span class="hlt">weather</span> <span class="hlt">modeling</span>, a tool originally developed for artificial intelligence. In our contribution, we focus on practical aspects of the neural networks application to <span class="hlt">modeling</span> and forecasting selected space <span class="hlt">weather</span> parameters.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2015AGUFMIN23C1737W','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2015AGUFMIN23C1737W"><span>Using Predictive Analytics to Predict Power Outages from Severe <span class="hlt">Weather</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Wanik, D. W.; Anagnostou, E. N.; Hartman, B.; Frediani, M. E.; Astitha, M.</p> <p>2015-12-01</p> <p>The distribution of reliable power is essential to businesses, public services, and our daily lives. With the growing abundance of data being collected and created by industry (i.e. outage data), government agencies (i.e. land cover), and academia (i.e. <span class="hlt">weather</span> forecasts), we can begin to tackle problems that previously seemed too complex to solve. In this session, we will present newly developed tools to aid decision-support challenges at electric distribution utilities that must mitigate, prepare for, respond to and recover from severe <span class="hlt">weather</span>. We will show a performance evaluation of outage predictive <span class="hlt">models</span> built for Eversource Energy (formerly Connecticut Light & Power) for storms of all types (i.e. blizzards, thunderstorms and hurricanes) and magnitudes (from 20 to >15,000 outages). High resolution <span class="hlt">weather</span> simulations (simulated with the <span class="hlt">Weather</span> and Research Forecast <span class="hlt">Model</span>) were joined with utility outage data to calibrate four types of <span class="hlt">models</span>: a decision tree (DT), random forest (RF), boosted gradient tree (BT) and an ensemble (ENS) decision tree regression that combined predictions from DT, RF and BT. The study shows that the ENS <span class="hlt">model</span> forced with <span class="hlt">weather</span>, infrastructure and land cover data was superior to the other <span class="hlt">models</span> we evaluated, especially in terms of predicting the spatial distribution of outages. This research has the potential to be used for other critical infrastructure <span class="hlt">systems</span> (such as telecommunications, drinking water and gas distribution networks), and can be readily expanded to the entire New England region to facilitate better planning and coordination among decision-makers when severe <span class="hlt">weather</span> strikes.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2018BoLMe.166..503J','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2018BoLMe.166..503J"><span>Evaluating <span class="hlt">Weather</span> Research and Forecasting <span class="hlt">Model</span> Sensitivity to Land and Soil Conditions Representative of Karst Landscapes</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Johnson, Christopher M.; Fan, Xingang; Mahmood, Rezaul; Groves, Chris; Polk, Jason S.; Yan, Jun</p> <p>2018-03-01</p> <p>Due to their particular physiographic, geomorphic, soil cover, and complex surface-subsurface hydrologic conditions, karst regions produce distinct land-atmosphere interactions. It has been found that floods and droughts over karst regions can be more pronounced than those in non-karst regions following a given rainfall event. Five convective <span class="hlt">weather</span> events are simulated using the <span class="hlt">Weather</span> Research and Forecasting <span class="hlt">model</span> to explore the potential impacts of land-surface conditions on <span class="hlt">weather</span> simulations over karst regions. Since no existing <span class="hlt">weather</span> or climate <span class="hlt">model</span> has the ability to represent karst landscapes, simulation experiments in this exploratory study consist of a control (default land-cover/soil types) and three land-surface conditions, including barren ground, forest, and sandy soils over the karst areas, which mimic certain karst characteristics. Results from sensitivity experiments are compared with the control simulation, as well as with the National Centers for Environmental Prediction multi-sensor precipitation analysis Stage-IV data, and near-surface atmospheric observations. Mesoscale features of surface energy partition, surface water and energy exchange, the resulting surface-air temperature and humidity, and low-level instability and convective energy are analyzed to investigate the potential land-surface impact on <span class="hlt">weather</span> over karst regions. We conclude that: (1) barren ground used over karst regions has a pronounced effect on the overall simulation of precipitation. Barren ground provides the overall lowest root-mean-square errors and bias scores in precipitation over the peak-rain periods. Contingency table-based equitable threat and frequency bias scores suggest that the barren and forest experiments are more successful in simulating light to moderate rainfall. Variables dependent on local surface conditions show stronger contrasts between karst and non-karst regions than variables dominated by large-scale synoptic <span class="hlt">systems</span>; (2) significant</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017AGUFM.U22B..04H','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017AGUFM.U22B..04H"><span>Alexander Hegedus Lightning Talk: Integrating Measurements to Optimize Space <span class="hlt">Weather</span> Strategies</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Hegedus, A. M.</p> <p>2017-12-01</p> <p>Alexander Hegedus is a PhD Candidate at the University of Michigan, and won an Outstanding Student Paper Award at the AGU 2016 Fall Meeting for his poster "Simulating 3D Spacecraft Constellations for Low Frequency Radio Imaging." In this short talk, Alex outlines his current research of analyzing data from both real and simulated instruments to answer Heliophysical questions. He then sketches out future plans to simulate science pipelines in a real-time data assimilation <span class="hlt">model</span> that uses a Bayesian framework to integrate information from different instruments to determine the efficacy of future Space <span class="hlt">Weather</span> Alert <span class="hlt">systems</span>. MHD simulations made with Michigan's own Space <span class="hlt">Weather</span> <span class="hlt">Model</span> Framework will provide input to simulated instruments, acting as an Observing <span class="hlt">System</span> Simulation Experiment to verify that a certain set of measurements can accurately predict different classes of Space <span class="hlt">Weather</span> events.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://www.ars.usda.gov/research/publications/publication/?seqNo115=254511','TEKTRAN'); return false;" href="http://www.ars.usda.gov/research/publications/publication/?seqNo115=254511"><span>Comparisons of Historical versus Synthetic <span class="hlt">Weather</span> Inputs to Watershed <span class="hlt">Models</span> and their Effect on Pollutant Loads</span></a></p> <p><a target="_blank" href="https://www.ars.usda.gov/research/publications/find-a-publication/">USDA-ARS?s Scientific Manuscript database</a></p> <p></p> <p></p> <p>Synthetic <span class="hlt">weather</span> generators are important for continuous-simulation of agricultural watersheds for risk analyses of downstream water quality. Many watersheds are sparsely or totally ungauged and daily <span class="hlt">weather</span> must either be transposed or augmented. Since water quality <span class="hlt">models</span> must recognize runoff...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/20170003345','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/20170003345"><span>Seasonal Forecasting of Fire <span class="hlt">Weather</span> Based on a New Global Fire <span class="hlt">Weather</span> Database</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Dowdy, Andrew J.; Field, Robert D.; Spessa, Allan C.</p> <p>2016-01-01</p> <p>Seasonal forecasting of fire <span class="hlt">weather</span> is examined based on a recently produced global database of the Fire <span class="hlt">Weather</span> Index (FWI) <span class="hlt">system</span> beginning in 1980. Seasonal average values of the FWI are examined in relation to measures of the El Nino-Southern Oscillation (ENSO) and the Indian Ocean Dipole (IOD). The results are used to examine seasonal forecasts of fire <span class="hlt">weather</span> conditions throughout the world.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.osti.gov/biblio/1231936-weather-research-forecasting-model-vertical-nesting-capability','SCIGOV-STC'); return false;" href="https://www.osti.gov/biblio/1231936-weather-research-forecasting-model-vertical-nesting-capability"><span><span class="hlt">Weather</span> Research and Forecasting <span class="hlt">Model</span> with Vertical Nesting Capability</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></p> <p>2014-08-01</p> <p>The <span class="hlt">Weather</span> Research and Forecasting (WRF) <span class="hlt">model</span> with vertical nesting capability is an extension of the WRF <span class="hlt">model</span>, which is available in the public domain, from www.wrf-<span class="hlt">model</span>.org. The new code modifies the nesting procedure, which passes lateral boundary conditions between computational domains in the WRF <span class="hlt">model</span>. Previously, the same vertical grid was required on all domains, while the new code allows different vertical grids to be used on concurrently run domains. This new functionality improves WRF's ability to produce high-resolution simulations of the atmosphere by allowing a wider range of scales to be efficiently resolved and more accurate lateral boundarymore » conditions to be provided through the nesting procedure.« less</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017AGUFM.A31J2310L','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017AGUFM.A31J2310L"><span>Hazardous Convective <span class="hlt">Weather</span> in the Central United States: Present and Future</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Liu, C.; Ikeda, K.; Rasmussen, R.</p> <p>2017-12-01</p> <p>Two sets of 13-year continental-scale convection-permitting simulations were performed using the 4-km-resolution WRF <span class="hlt">model</span>. They consist of a retrospective simulation, which downscales the ERA-Interim reanalysis during the period October 2000 - September 2013, and a future climate sensitivity simulation for the same period based on the perturbed reanalysis-derived boundary conditions with the CMIP5 ensemble-mean high-end emission scenario climate change. The evaluation of the retrospective simulation indicates that the <span class="hlt">model</span> is able to realistically reproduce the main characteristics of deep precipitating convection observed in the current climate such as the spectra of convective population and propagating mesoscale convective <span class="hlt">systems</span> (MCSs). It is also shown that severe convection and associated MCS will increase in frequency and intensity, implying a potential increase in high impact convective <span class="hlt">weather</span> in a future warmer climate. In this study, the warm-season hazardous convective <span class="hlt">weather</span> (i.e., tonadoes, hails and damaging gusty wind) in the central United states is examined using these 4-km downscaling simulations. First, a <span class="hlt">model</span>-based proxy for hazardous convective <span class="hlt">weather</span> is derived on the basis of a set of characteristic meteorological variables such as the <span class="hlt">model</span> composite radar reflectivity, updraft helicity, vertical wind shear, and low-level wind. Second, the developed proxy is applied to the retrospective simulation for estimate of the <span class="hlt">model</span> hazardous <span class="hlt">weather</span> events during the historical period. Third, the simulated hazardous <span class="hlt">weather</span> statistics are evaluated against the NOAA severe <span class="hlt">weather</span> reports. Lastly, the proxy is applied to the future climate simulation for the projected change of hazardous convective <span class="hlt">weather</span> in response to global warming. Preliminary results will be reported at the 2017 AGU session "High Resolution Climate <span class="hlt">Modeling</span>".</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/20140006910','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/20140006910"><span>Integration of <span class="hlt">Weather</span> Data into Airspace and Traffic Operations Simulation (ATOS) for Trajectory- Based Operations Research</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Peters, Mark; Boisvert, Ben; Escala, Diego</p> <p>2009-01-01</p> <p>Explicit integration of aviation <span class="hlt">weather</span> forecasts with the National Airspace <span class="hlt">System</span> (NAS) structure is needed to improve the development and execution of operationally effective <span class="hlt">weather</span> impact mitigation plans and has become increasingly important due to NAS congestion and associated increases in delay. This article considers several contemporary <span class="hlt">weather</span>-air traffic management (ATM) integration applications: the use of probabilistic forecasts of visibility at San Francisco, the Route Availability Planning Tool to facilitate departures from the New York airports during thunderstorms, the estimation of en route capacity in convective <span class="hlt">weather</span>, and the application of mixed-integer optimization techniques to air traffic management when the en route and terminal capacities are varying with time because of convective <span class="hlt">weather</span> impacts. Our operational experience at San Francisco and New York coupled with very promising initial results of traffic flow optimizations suggests that <span class="hlt">weather</span>-ATM integrated <span class="hlt">systems</span> warrant significant research and development investment. However, they will need to be refined through rapid prototyping at facilities with supportive operational users We have discussed key elements of an emerging aviation <span class="hlt">weather</span> research area: the explicit integration of aviation <span class="hlt">weather</span> forecasts with NAS structure to improve the effectiveness and timeliness of <span class="hlt">weather</span> impact mitigation plans. Our insights are based on operational experiences with Lincoln Laboratory-developed integrated <span class="hlt">weather</span> sensing and processing <span class="hlt">systems</span>, and derivative early prototypes of explicit ATM decision support tools such as the RAPT in New York City. The technical components of this effort involve improving meteorological forecast skill, tailoring the forecast outputs to the problem of estimating airspace impacts, developing <span class="hlt">models</span> to quantify airspace impacts, and prototyping automated tools that assist in the development of objective broad-area ATM strategies, given probabilistic</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017AGUFMNG51B..07S','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017AGUFMNG51B..07S"><span>A Simple Exploration of Complexity at the Climate-<span class="hlt">Weather</span>-Social-Conflict Nexus</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Shaw, M.</p> <p>2017-12-01</p> <p>The conceptualization, exploration, and prediction of interplay between climate, <span class="hlt">weather</span>, important resources, and social and economic - so political - human behavior is cast, and analyzed, in terms familiar from statistical physics and nonlinear dynamics. A simple threshold toy <span class="hlt">model</span> is presented which emulates human tendencies to either actively engage in responses deriving, in part, from environmental circumstances or to maintain some semblance of status quo, formulated based on efforts drawn from the sociophysics literature - more specifically vis a vis a <span class="hlt">model</span> akin to spin glass depictions of human behavior - with threshold/switching of individual and collective dynamics influenced by relatively more detailed <span class="hlt">weather</span> and land surface <span class="hlt">model</span> (hydrological) analyses via a land data assimilation <span class="hlt">system</span> (a custom rendition of the NASA GSFC Land Information <span class="hlt">System</span>). Parameters relevant to human <span class="hlt">systems</span>' - e.g., individual and collective switching - sensitivity to hydroclimatology are explored towards investigation of overall <span class="hlt">system</span> behavior; i.e., fixed points/equilibria, oscillations, and bifurcations of <span class="hlt">systems</span> composed of human interactions and responses to climate and <span class="hlt">weather</span> through, e.g., agriculture. We discuss implications in terms of conceivable impacts of climate change and associated natural disasters on socioeconomics, politics, and power transfer, drawing from relatively recent literature concerning human conflict.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/20070021329','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/20070021329"><span>Anvil Tool in the Advanced <span class="hlt">Weather</span> Interactive Processing <span class="hlt">System</span></span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Barrett, Joe, III; Bauman, William, III; Keen, Jeremy</p> <p>2007-01-01</p> <p>Meteorologists from the 45th <span class="hlt">Weather</span> Squadron (45 WS) and Spaceflight Meteorology Group (SMG) have identified anvil forecasting as one of their most challenging tasks when predicting the probability of violations of the lightning Launch Commit Criteria and Space Shuttle Flight Rules. As a result, the Applied Meteorology Unit (AMU) created a graphical overlay tool for the Meteorological Interactive Data Display <span class="hlt">Systems</span> (MIDDS) to indicate the threat of thunderstorm anvil clouds, using either observed or <span class="hlt">model</span> forecast winds as input. In order for the Anvil Tool to remain available to the meteorologists, the AMU was tasked to transition the tool to the Advanced <span class="hlt">Weather</span> interactive Processing <span class="hlt">System</span> (AWIPS). This report describes the work done by the AMU to develop the Anvil Tool for AWIPS to create a graphical overlay depicting the threat from thunderstorm anvil clouds. The AWIPS Anvil Tool is based on the previously deployed AMU MIDDS Anvil Tool. SMG and 45 WS forecasters have used the MIDDS Anvil Tool during launch and landing operations. SMG's primary <span class="hlt">weather</span> analysis and display <span class="hlt">system</span> is now AWIPS and the 45 WS has plans to replace MIDDS with AWIPS. The Anvil Tool creates a graphic that users can overlay on satellite or radar imagery to depict the potential location of thunderstorm anvils one, two, and three hours into the future. The locations are based on an average of the upper-level observed or forecasted winds. The graphic includes 10 and 20 nm standoff circles centered at the location of interest, in addition to one-, two-, and three-hour arcs in the upwind direction. The arcs extend outward across a 30 degree sector width based on a previous AMU study which determined thunderstorm anvils move in a direction plus or minus 15 degrees of the upper-level (300- to 150-mb) wind direction. This report briefly describes the history of the MIDDS Anvil Tool and then explains how the initial development of the AWIPS Anvil Tool was carried out. After testing was</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2016E%26PSL.450..381T','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2016E%26PSL.450..381T"><span>The acid and alkalinity budgets of <span class="hlt">weathering</span> in the Andes-Amazon <span class="hlt">system</span>: Insights into the erosional control of global biogeochemical cycles</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Torres, Mark A.; West, A. Joshua; Clark, Kathryn E.; Paris, Guillaume; Bouchez, Julien; Ponton, Camilo; Feakins, Sarah J.; Galy, Valier; Adkins, Jess F.</p> <p>2016-09-01</p> <p>The correlation between chemical <span class="hlt">weathering</span> fluxes and denudation rates suggests that tectonic activity can force variations in atmospheric pCO2 by modulating <span class="hlt">weathering</span> fluxes. However, the effect of <span class="hlt">weathering</span> on pCO2 is not solely determined by the total mass flux. Instead, the effect of <span class="hlt">weathering</span> on pCO2 also depends upon the balance between 1) alkalinity generation by carbonate and silicate mineral dissolution and 2) sulfuric acid generation by the oxidation of sulfide minerals. In this study, we explore how the balance between acid and alkalinity generation varies with tectonic uplift to better understand the links between tectonics and the long-term carbon cycle. To trace <span class="hlt">weathering</span> reactions across the transition from the Peruvian Andes to the Amazonian foreland basin, we measured a suite of elemental concentrations (Na, K, Ca, Mg, Sr, Si, Li, SO4, and Cl) and isotopic ratios (87Sr/86Sr and δ34S) on both dissolved and solid phase samples. Using an inverse <span class="hlt">model</span>, we quantitatively link systematic changes in solute geochemistry with elevation to downstream declines in sulfuric acid <span class="hlt">weathering</span> as well as the proportion of cations sourced from silicates. With a new carbonate-<span class="hlt">system</span> framework, we show that <span class="hlt">weathering</span> in the Andes Mountains is a CO2 source whereas foreland <span class="hlt">weathering</span> is a CO2 sink. These results are consistent with the theoretical expectation that the ratio of sulfide oxidation to silicate <span class="hlt">weathering</span> increases with increasing erosion. Altogether, our results suggest that the effect of tectonically-enhanced <span class="hlt">weathering</span> on atmospheric pCO2 is strongly modulated by sulfide mineral oxidation.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/20130003167','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/20130003167"><span>Development of a High Resolution <span class="hlt">Weather</span> Forecast <span class="hlt">Model</span> for Mesoamerica Using the NASA Nebula Cloud Computing Environment</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Molthan, Andrew L.; Case, Jonathan L.; Venner, Jason; Moreno-Madrinan, Max. J.; Delgado, Francisco</p> <p>2012-01-01</p> <p>Over the past two years, scientists in the Earth Science Office at NASA fs Marshall Space Flight Center (MSFC) have explored opportunities to apply cloud computing concepts to support near real ]time <span class="hlt">weather</span> forecast <span class="hlt">modeling</span> via the <span class="hlt">Weather</span> Research and Forecasting (WRF) <span class="hlt">model</span>. Collaborators at NASA fs Short ]term Prediction Research and Transition (SPoRT) Center and the SERVIR project at Marshall Space Flight Center have established a framework that provides high resolution, daily <span class="hlt">weather</span> forecasts over Mesoamerica through use of the NASA Nebula Cloud Computing Platform at Ames Research Center. Supported by experts at Ames, staff at SPoRT and SERVIR have established daily forecasts complete with web graphics and a user interface that allows SERVIR partners access to high resolution depictions of <span class="hlt">weather</span> in the next 48 hours, useful for monitoring and mitigating meteorological hazards such as thunderstorms, heavy precipitation, and tropical <span class="hlt">weather</span> that can lead to other disasters such as flooding and landslides. This presentation will describe the framework for establishing and providing WRF forecasts, example applications of output provided via the SERVIR web portal, and early results of forecast <span class="hlt">model</span> verification against available surface ] and satellite ]based observations.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2012AGUFMIN43C1526M','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2012AGUFMIN43C1526M"><span>Development of a High Resolution <span class="hlt">Weather</span> Forecast <span class="hlt">Model</span> for Mesoamerica Using the NASA Nebula Cloud Computing Environment</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Molthan, A.; Case, J.; Venner, J.; Moreno-Madriñán, M. J.; Delgado, F.</p> <p>2012-12-01</p> <p>Over the past two years, scientists in the Earth Science Office at NASA's Marshall Space Flight Center (MSFC) have explored opportunities to apply cloud computing concepts to support near real-time <span class="hlt">weather</span> forecast <span class="hlt">modeling</span> via the <span class="hlt">Weather</span> Research and Forecasting (WRF) <span class="hlt">model</span>. Collaborators at NASA's Short-term Prediction Research and Transition (SPoRT) Center and the SERVIR project at Marshall Space Flight Center have established a framework that provides high resolution, daily <span class="hlt">weather</span> forecasts over Mesoamerica through use of the NASA Nebula Cloud Computing Platform at Ames Research Center. Supported by experts at Ames, staff at SPoRT and SERVIR have established daily forecasts complete with web graphics and a user interface that allows SERVIR partners access to high resolution depictions of <span class="hlt">weather</span> in the next 48 hours, useful for monitoring and mitigating meteorological hazards such as thunderstorms, heavy precipitation, and tropical <span class="hlt">weather</span> that can lead to other disasters such as flooding and landslides. This presentation will describe the framework for establishing and providing WRF forecasts, example applications of output provided via the SERVIR web portal, and early results of forecast <span class="hlt">model</span> verification against available surface- and satellite-based observations.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://pubs.usgs.gov/of/1989/0415_1990/report.pdf','USGSPUBS'); return false;" href="https://pubs.usgs.gov/of/1989/0415_1990/report.pdf"><span>A primer on clothing <span class="hlt">systems</span> for cold-<span class="hlt">weather</span> field work</span></a></p> <p><a target="_blank" href="http://pubs.er.usgs.gov/pubs/index.jsp?view=adv">USGS Publications Warehouse</a></p> <p>Denner, Jon</p> <p>1990-01-01</p> <p>Conducting field work in cold <span class="hlt">weather</span> is a demanding task. The most important safety consideration for field personnel is to maintain normal body temperature and avoid hypothermia.The human body adjusts to cold temperatures through different physiological processes. Heat production is enhanced by increases in the rates of basal metabolism, specific dynamic action, and physical exercise, and heat loss is reduced by vasoconstriction.Physiological adaptations alone are inadequate to stop rapid heat loss in cold temperatures. Additional insulation in the form of cold-<span class="hlt">weather</span> clothing is necessary to retain heat.The most practical method of dressing for winter conditions is the layering <span class="hlt">system</span>. Wearing multiple thin layers allows one to fine tune the insulation needed for different temperatures and activity levels.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2012aogs...30..117H','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2012aogs...30..117H"><span>Recent Progress of Solar <span class="hlt">Weather</span> Forecasting at Naoc</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>He, Han; Wang, Huaning; Du, Zhanle; Zhang, Liyun; Huang, Xin; Yan, Yan; Fan, Yuliang; Zhu, Xiaoshuai; Guo, Xiaobo; Dai, Xinghua</p> <p></p> <p>The history of solar <span class="hlt">weather</span> forecasting services at National Astronomical Observatories, Chinese Academy of Sciences (NAOC) can be traced back to 1960s. Nowadays, NAOC is the headquarters of the Regional Warning Center of China (RWC-China), which is one of the members of the International Space Environment Service (ISES). NAOC is responsible for exchanging data, information and space <span class="hlt">weather</span> forecasts of RWC-China with other RWCs. The solar <span class="hlt">weather</span> forecasting services at NAOC cover short-term prediction (within two or three days), medium-term prediction (within several weeks), and long-term prediction (in time scale of solar cycle) of solar activities. Most efforts of the short-term prediction research are concentrated on the solar eruptive phenomena, such as flares, coronal mass ejections (CMEs) and solar proton events, which are the key driving sources of strong space <span class="hlt">weather</span> disturbances. Based on the high quality observation data of the latest space-based and ground-based solar telescopes and with the help of artificial intelligence techniques, new numerical <span class="hlt">models</span> with quantitative analyses and physical consideration are being developed for the predictions of solar eruptive events. The 3-D computer simulation technology is being introduced for the operational solar <span class="hlt">weather</span> service platform to visualize the monitoring of solar activities, the running of the prediction <span class="hlt">models</span>, as well as the presenting of the forecasting results. A new generation operational solar <span class="hlt">weather</span> monitoring and forecasting <span class="hlt">system</span> is expected to be constructed in the near future at NAOC.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2009EGUGA..11.7056W','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2009EGUGA..11.7056W"><span>Detection of mesoscale zones of atmospheric instabilities using remote sensing and <span class="hlt">weather</span> forecasting <span class="hlt">model</span> data</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Winnicki, I.; Jasinski, J.; Kroszczynski, K.; Pietrek, S.</p> <p>2009-04-01</p> <p>The paper presents elements of research conducted in the Faculty of Civil Engineering and Geodesy of the Military University of Technology, Warsaw, Poland, concerning application of mesoscale <span class="hlt">models</span> and remote sensing data to determining meteorological conditions of aircraft flight directly related with atmospheric instabilities. The quality of meteorological support of aviation depends on prompt and effective forecasting of <span class="hlt">weather</span> conditions changes. The paper presents a computer module for detecting and monitoring zones of cloud cover, precipitation and turbulence along the aircraft flight route. It consists of programs and scripts for managing, processing and visualizing meteorological and remote sensing databases. The application was developed in Matlab® for Windows®. The module uses products of COAMPS (Coupled Ocean/Atmosphere Mesoscale Prediction <span class="hlt">System</span>) mesoscale non-hydrostatic <span class="hlt">model</span> of the atmosphere developed by the US Naval Research Laboratory, satellite images acquisition <span class="hlt">system</span> from the MSG-2 (Meteosat Second Generation) of the European Organization for the Exploitation of Meteorological Satellites (EUMETSAT) and meteorological radars data acquired from the Institute of Meteorology and Water Management (IMGW), Warsaw, Poland. The satellite images acquisition <span class="hlt">system</span> and the COAMPS <span class="hlt">model</span> are run operationally in the Faculty of Civil Engineering and Geodesy. The mesoscale <span class="hlt">model</span> is run on an IA64 Feniks multiprocessor 64-bit computer cluster. The basic task of the module is to enable a complex analysis of data sets of miscellaneous information structure and to verify COAMPS results using satellite and radar data. The research is conducted using uniform cartographic projection of all elements of the database. Satellite and radar images are transformed into the Lambert Conformal projection of COAMPS. This facilitates simultaneous interpretation and supports decision making process for safe execution of flights. Forecasts are based on horizontal</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/19657150','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/19657150"><span>Separate and combined sewer <span class="hlt">systems</span>: a long-term <span class="hlt">modelling</span> approach.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Mannina, Giorgio; Viviani, Gaspare</p> <p>2009-01-01</p> <p>Sewer <span class="hlt">systems</span> convey mostly dry <span class="hlt">weather</span> flow, coming from domestic and industrial sanitary sewage as well as infiltration flow, and stormwater due to meteoric precipitations. Traditionally, in urban drainage two types of sewer <span class="hlt">systems</span> are adopted: separate and combined sewers. The former convey dry and wet <span class="hlt">weather</span> flow separately into two different networks, while the latter convey dry and wet <span class="hlt">weather</span> flow together. Which is the best solution in terms of cost-benefit analysis still remains a controversial subject. The present study was aimed at comparing the pollution loads discharged to receiving bodies by Wastewater Treatment Plant (WWTP) and Combined Sewer Overflow (CSO) for different kinds of sewer <span class="hlt">systems</span> (combined and separate). To accomplish this objective, a comparison between the two <span class="hlt">systems</span> was carried out using results from simulations of catchments characterised by different dimensions, population densities and water supply rate. The analysis was based on a parsimonious mathematical <span class="hlt">model</span> able to simulate the sewer <span class="hlt">system</span> as well as the WWTP during both dry and wet <span class="hlt">weather</span>. The rain series employed for the simulations was six years long. Several pollutants, both dissolved and particulate, were <span class="hlt">modelled</span>. The results confirmed the uncertainties in the choice of one <span class="hlt">system</span> versus the other, emphasising the concept that case-by-case solutions have to be undertaken. Further, the compared <span class="hlt">systems</span> showed different responses in terms of effectiveness in reducing the discharged mass to the RWB in relation to the particular pollutant taken into account.</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://hdl.handle.net/2060/19780006813','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/19780006813"><span><span class="hlt">Weather</span> assessment and forecasting</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p></p> <p>1977-01-01</p> <p>Data management program activities centered around the analyses of selected far-term Office of Applications (OA) objectives, with the intent of determining if significant data-related problems would be encountered and if so what alternative solutions would be possible. Three far-term (1985 and beyond) OA objectives selected for analyses as having potential significant data problems were large-scale <span class="hlt">weather</span> forecasting, local <span class="hlt">weather</span> and severe storms forecasting, and global marine <span class="hlt">weather</span> forecasting. An overview of general <span class="hlt">weather</span> forecasting activities and their implications upon the ground based data <span class="hlt">system</span> is provided. Selected topics were specifically oriented to the use of satellites.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017AGUFM.B31E2035N','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017AGUFM.B31E2035N"><span>A subsurface Fe-silicate <span class="hlt">weathering</span> microbiome</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Napieralski, S. A.; Buss, H. L.; Roden, E. E.</p> <p>2017-12-01</p> <p>Traditional <span class="hlt">models</span> of microbially mediated <span class="hlt">weathering</span> of primary Fe-bearing minerals often invoke organic ligands (e.g. siderophores) used for nutrient acquisition. However, it is well known that the oxidation of Fe(II) governs the overall rate of Fe-silicate mineral dissolution. Recent work has demonstrated the ability of lithtrophic iron oxidizing bacteria (FeOB) to grow via the oxidation of structural Fe(II) in biotite as a source of metabolic energy with evidence suggesting a direct enzymatic attack on the mineral surface. This process necessitates the involvement of dedicated outer membrane proteins that interact with insoluble mineral phases in a process known as extracellular electron transfer (EET). To investigate the potential role FeOB in a terrestrial subsurface <span class="hlt">weathering</span> <span class="hlt">system</span>, samples were obtained from the bedrock-saprolite interface (785 cm depth) within the Rio Icacos Watershed of the Luquillo Mountains in Puerto Rico. Prior geochemical evidence suggests the flux of Fe(II) from the <span class="hlt">weathering</span> bedrock supports a robust lithotrophic microbial community at depth. Current work confirms the activity of microorganism in situ, with a marked increase in ATP near the bedrock-saprolite interface. Regolith recovered from the interface was used as inoculum to establish enrichment cultures with powderized Fe(II)-bearing minerals serving as the sole energy source. Monitoring of the Fe(II)/Fe(total) ratio and ATP generation suggests growth of microorganisms coupled to the oxidation of mineral bound Fe(II). Analysis of 16S rRNA gene and shotgun metagenomic libraries from in situ and enrichment culture samples lends further support to FeOB involvement in the <span class="hlt">weathering</span> process. Multiple metagenomic bins related to known FeOB, including Betaproteobacteria genera, contain homologs to <span class="hlt">model</span> EET <span class="hlt">systems</span>, including Cyc2 and MtoAB. Our approach combining geochemistry and metagenomics with ongoing microbiological and genomic characterization of novel isolates obtained</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://rosap.ntl.bts.gov/view/dot/24648','DOTNTL'); return false;" href="https://rosap.ntl.bts.gov/view/dot/24648"><span><span class="hlt">Weather</span> in the cockpit : priorities, sources, delivery, and needs in the next generation air transportation <span class="hlt">system</span>.</span></a></p> <p><a target="_blank" href="http://ntlsearch.bts.gov/tris/index.do">DOT National Transportation Integrated Search</a></p> <p></p> <p>2012-07-01</p> <p>A study was conducted to identify/verify <span class="hlt">weather</span> factors important to the conduct of aviation activities and : that would be important to consider in <span class="hlt">systems</span> intended to operate within the NextGen environment. The : study reviewed <span class="hlt">weather</span>-information...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://www.ars.usda.gov/research/publications/publication/?seqNo115=259527','TEKTRAN'); return false;" href="http://www.ars.usda.gov/research/publications/publication/?seqNo115=259527"><span>Decision Aids for Multiple-Decision Disease Management as Affected by <span class="hlt">Weather</span> Input Errors</span></a></p> <p><a target="_blank" href="https://www.ars.usda.gov/research/publications/find-a-publication/">USDA-ARS?s Scientific Manuscript database</a></p> <p></p> <p></p> <p>Many disease management decision support <span class="hlt">systems</span> (DSS) rely, exclusively or in part, on <span class="hlt">weather</span> inputs to calculate an indicator for disease hazard. Error in the <span class="hlt">weather</span> inputs, typically due to forecasting, interpolation or estimation from off-site sources, may affect <span class="hlt">model</span> calculations and manage...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2016AGUFMGC51G..01E','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2016AGUFMGC51G..01E"><span>Past and future <span class="hlt">weather</span>-induced risk in crop production</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Elliott, J. W.; Glotter, M.; Russo, T. A.; Sahoo, S.; Foster, I.; Benton, T.; Mueller, C.</p> <p>2016-12-01</p> <p>Drought-induced agricultural loss is one of the most costly impacts of extreme <span class="hlt">weather</span> and may harm more people than any other consequence of climate change. Improvements in farming practices have dramatically increased crop productivity, but yields today are still tightly linked to climate variation. We report here on a number of recent studies evaluating extreme event risk and impacts under historical and near future conditions, including studies conducted as part of the Agricultural <span class="hlt">Modeling</span> Intercomparison and Improvement Project (AgMIP), the Inter-Sectoral Impacts <span class="hlt">Model</span> Intercomparison Project (ISI-MIP) and the UK-US Taskforce on Extreme <span class="hlt">Weather</span> and Global Food <span class="hlt">System</span> Resilience.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/20130003214','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/20130003214"><span>Development of a High Resolution <span class="hlt">Weather</span> Forecast <span class="hlt">Model</span> for Mesoamerica Using the NASA Ames Code I Private Cloud Computing Environment</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Molthan, Andrew; Case, Jonathan; Venner, Jason; Moreno-Madrinan, Max J.; Delgado, Francisco</p> <p>2012-01-01</p> <p>Two projects at NASA Marshall Space Flight Center have collaborated to develop a high resolution <span class="hlt">weather</span> forecast <span class="hlt">model</span> for Mesoamerica: The NASA Short-term Prediction Research and Transition (SPoRT) Center, which integrates unique NASA satellite and <span class="hlt">weather</span> forecast <span class="hlt">modeling</span> capabilities into the operational <span class="hlt">weather</span> forecasting community. NASA's SERVIR Program, which integrates satellite observations, ground-based data, and forecast <span class="hlt">models</span> to improve disaster response in Central America, the Caribbean, Africa, and the Himalayas.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/20110012969','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/20110012969"><span>Using Artificial Intelligence to Inform Pilots of <span class="hlt">Weather</span></span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Spirkovska, Lilly; Lodha, Suresh K.</p> <p>2006-01-01</p> <p>An automated <span class="hlt">system</span> to assist a General Aviation (GA) pilot in improving situational awareness of <span class="hlt">weather</span> in flight is now undergoing development. This development is prompted by the observation that most fatal GA accidents are attributable to loss of <span class="hlt">weather</span> awareness. Loss of <span class="hlt">weather</span> awareness, in turn, has been attributed to the difficulty of interpreting traditional preflight <span class="hlt">weather</span> briefings and the difficulty of both obtaining and interpreting traditional in-flight <span class="hlt">weather</span> briefings. The developmental automated <span class="hlt">system</span> not only improves <span class="hlt">weather</span> awareness but also substantially reduces the time a pilot must spend in acquiring and maintaining <span class="hlt">weather</span> awareness.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://rosap.ntl.bts.gov/view/dot/24673','DOTNTL'); return false;" href="https://rosap.ntl.bts.gov/view/dot/24673"><span>Evaluation of a variable speed limit <span class="hlt">system</span> for wet and extreme <span class="hlt">weather</span> conditions : phase 1 report.</span></a></p> <p><a target="_blank" href="http://ntlsearch.bts.gov/tris/index.do">DOT National Transportation Integrated Search</a></p> <p></p> <p>2012-06-01</p> <p><span class="hlt">Weather</span> presents considerable challenges to the highway <span class="hlt">system</span>, both in terms of safety and operations. From a safety standpoint, <span class="hlt">weather</span> (i.e. precipitation in the form of rain, snow or ice) reduces pavement friction, thus increasing the potential f...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2014cosp...40E1096G','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2014cosp...40E1096G"><span>Challenges in Heliophysics and Space <span class="hlt">Weather</span>: What Instrumentation for the Future?</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Guhathakurta, Madhulika</p> <p></p> <p>A hundred years ago, the sun-Earth connection (the field of heliophysics research and space <span class="hlt">weather</span> impacts) was of interest to only a small number of scientists. Solar activity had little effect on daily life. Today, a single strong solar flare could bring civilization to its knees. Modern society has come to depend on technologies sensitive to solar radiation and geomagnetic storms. Particularly vulnerable are intercontinental power grids, interplanetary robotic and human exploration, satellite operations and communications, and GPS navigation. These technologies are woven into the fabric of daily life, from health care and finance to basic utilities. Both short- and long-term forecasting <span class="hlt">models</span> are urgently needed to mitigate the effects of solar storms and to anticipate their collective impact on aviation, astronaut safety, terrestrial climate and others. Even during a relatively weak solar maximum, the potential consequences that such events can have on society are too important to ignore. The challenges associated with space <span class="hlt">weather</span> affect all developed and developing countries. Work on space <span class="hlt">weather</span> specification, <span class="hlt">modeling</span>, and forecasting has great societal benefit: It is basic research with a high public purpose. At present, we have a fleet “Heliophysics <span class="hlt">System</span> Observatory” of dedicated spacecraft titled (e.g. SOHO, STEREO, SDO, ACE), and serendipitous resources contributing data for space <span class="hlt">weather</span> <span class="hlt">modeling</span> from both remote observations of the sun and in-situ measurements to provide sparse space <span class="hlt">weather</span> situational awareness which were mostly built for a 2-3 year lifetime and are wearing out and won’t be around for very long. Missions currently in formulation will significantly enhance the capability of physics-based <span class="hlt">models</span> that are used to understand and predict the impact of the variable sun. To enhance current <span class="hlt">models</span>, and make them effective in predicting space <span class="hlt">weather</span> throughout the solar <span class="hlt">system</span>, we need a distributed network of spacecraft</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/20160009527','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/20160009527"><span>Traffic Management Coordinator Evaluation of the Dynamic <span class="hlt">Weather</span> Routes Concept and <span class="hlt">System</span></span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Gong, Chester</p> <p>2014-01-01</p> <p>Dynamic <span class="hlt">Weather</span> Routes (DWR) is a <span class="hlt">weather</span>-avoidance <span class="hlt">system</span> for airline dispatchers and FAA traffic managers that continually searches for and advises the user of more efficient routes around convective <span class="hlt">weather</span>. NASA and American Airlines (AA) have been conducting an operational trial of DWR since July 17, 2012. The objective of this evaluation is to assess DWR from a traffic management coordinator (TMC) perspective, using recently retired TMCs and actual DWR reroutes advisories that were rated acceptable by AA during the operational trial. Results from the evaluation showed that the primary reasons for a TMC to modify or reject airline reroute requests were related to airspace configuration. Approximately 80 percent of the reroutes evaluated required some coordination before implementation. Analysis showed TMCs approved 62 percent of the requested DWR reroutes, resulting in 57 percent of the total requested DWR time savings.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://pubs.er.usgs.gov/publication/70032849','USGSPUBS'); return false;" href="https://pubs.er.usgs.gov/publication/70032849"><span>Geochemical investigation of <span class="hlt">weathering</span> processes in a forested headwater catchment: Mass-balance <span class="hlt">weathering</span> fluxes</span></a></p> <p><a target="_blank" href="http://pubs.er.usgs.gov/pubs/index.jsp?view=adv">USGS Publications Warehouse</a></p> <p>Jones, B.F.; Herman, J.S.</p> <p>2008-01-01</p> <p>Geochemical research on natural <span class="hlt">weathering</span> has often been directed towards explanations of the chemical composition of surface water and ground water resulting from subsurface water-rock interactions. These interactions are often defined as the incongruent dissolution of primary silicates, such as feldspar, producing secondary <span class="hlt">weathering</span> products, such as clay minerals and oxyhydroxides, and solute fluxes (Meunier and Velde, 1979). The chemical composition of the clay-mineral product is often ignored. However, in earlier investigations, the saprolitic <span class="hlt">weathering</span> profile at the South Fork Brokenback Run (SFBR) watershed, Shenandoah National Park, Virginia, was characterized extensively in terms of its mineralogical and chemical composition (Piccoli, 1987; Pochatila et al., 2006; Jones et al., 2007) and its basic hydrology. O'Brien et al. (1997) attempted to determine the contribution of primary mineral <span class="hlt">weathering</span> to observed stream chemistry at SFBR. Mass-balance <span class="hlt">model</span> results, however, could provide only a rough estimate of the <span class="hlt">weathering</span> reactions because idealized mineral compositions were utilized in the calculations. Making use of detailed information on the mineral occurrence in the regolith, the objective of the present study was to evaluate the effects of compositional variation on mineral-solute mass-balance <span class="hlt">modelling</span> and to generate plausible quantitative <span class="hlt">weathering</span> reactions that support both the chemical evolution of the surface water and ground water in the catchment, as well as the mineralogical evolution of the <span class="hlt">weathering</span> profile. ?? 2008 The Mineralogical Society.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/19910663','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/19910663"><span>Directable <span class="hlt">weathering</span> of concave rock using curvature estimation.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Jones, Michael D; Farley, McKay; Butler, Joseph; Beardall, Matthew</p> <p>2010-01-01</p> <p>We address the problem of directable <span class="hlt">weathering</span> of exposed concave rock for use in computer-generated animation or games. Previous <span class="hlt">weathering</span> <span class="hlt">models</span> that admit concave surfaces are computationally inefficient and difficult to control. In nature, the spheroidal and cavernous <span class="hlt">weathering</span> rates depend on the surface curvature. Spheroidal <span class="hlt">weathering</span> is fastest in areas with large positive mean curvature and cavernous <span class="hlt">weathering</span> is fastest in areas with large negative mean curvature. We simulate both processes using an approximation of mean curvature on a voxel grid. Both <span class="hlt">weathering</span> rates are also influenced by rock durability. The user controls rock durability by editing a durability graph before and during <span class="hlt">weathering</span> simulation. Simulations of rockfall and colluvium deposition further improve realism. The profile of the final <span class="hlt">weathered</span> rock matches the shape of the durability graph up to the effects of <span class="hlt">weathering</span> and colluvium deposition. We demonstrate the top-down directability and visual plausibility of the resulting <span class="hlt">model</span> through a series of screenshots and rendered images. The results include the <span class="hlt">weathering</span> of a cube into a sphere and of a sheltered inside corner into a cavern as predicted by the underlying geomorphological <span class="hlt">models</span>.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/1997BAMS...78.2851V','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/1997BAMS...78.2851V"><span>Performance of an Advanced MOS <span class="hlt">System</span> in the 1996-97 National Collegiate <span class="hlt">Weather</span> Forecasting Contest.</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Vislocky, Robert L.; Fritsch, J. Michael</p> <p>1997-12-01</p> <p>A prototype advanced <span class="hlt">model</span> output statistics (MOS) forecast <span class="hlt">system</span> that was entered in the 1996-97 National Collegiate <span class="hlt">Weather</span> Forecast Contest is described and its performance compared to that of widely available objective guidance and to contest participants. The prototype <span class="hlt">system</span> uses an optimal blend of aviation (AVN) and nested grid <span class="hlt">model</span> (NGM) MOS forecasts, explicit output from the NGM and Eta guidance, and the latest surface <span class="hlt">weather</span> observations from the forecast site. The forecasts are totally objective and can be generated quickly on a personal computer. Other "objective" forms of guidance tracked in the contest are 1) the consensus forecast (i.e., the average of the forecasts from all of the human participants), 2) the combination of NGM raw output (for precipitation forecasts) and NGM MOS guidance (for temperature forecasts), and 3) the combination of Eta <span class="hlt">Model</span> raw output (for precipitation forecasts) and AVN MOS guidance (for temperature forecasts).Results show that the advanced MOS <span class="hlt">system</span> finished in 20th place out of 737 original entrants, or better than approximately 97% of the human forecasters who entered the contest. Moreover, the advanced MOS <span class="hlt">system</span> was slightly better than consensus (23d place). The fact that an objective forecast <span class="hlt">system</span> finished ahead of consensus is a significant accomplishment since consensus is traditionally a very formidable "opponent" in forecast competitions. Equally significant is that the advanced MOS <span class="hlt">system</span> was superior to the traditional guidance products available from the National Centers for Environmental Prediction (NCEP). Specifically, the combination of NGM raw output and NGM MOS guidance finished in 175th place, and the combination of Eta <span class="hlt">Model</span> raw output and AVN MOS guidance finished in 266th place. The latter result is most intriguing since the proposed elimination of all NGM products would likely result in a serious degradation of objective products disseminated by NCEP, unless they are replaced with equal</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2016GeCoA.195...29E','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2016GeCoA.195...29E"><span>Quantifying chemical <span class="hlt">weathering</span> rates along a precipitation gradient on Basse-Terre Island, French Guadeloupe: New insight from U-series isotopes in <span class="hlt">weathering</span> rinds</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Engel, Jacqueline M.; Ma, Lin; Sak, Peter B.; Gaillardet, Jerome; Ren, Minghua; Engle, Mark A.; Brantley, Susan L.</p> <p>2016-12-01</p> <p> that multiple <span class="hlt">weathering</span> clasts from the same watershed were analyzed for U-series isotope disequlibrian and show consistent results. The U-series disequilibria allowed for the determination of rind formation ages and <span class="hlt">weathering</span> advance rates with a U-series mass balance <span class="hlt">model</span>. The <span class="hlt">weathering</span> advance rates generally decreased with decreasing curvature: ∼0.17 ± 0.10 mm/kyr for high curvature, ∼0.12 ± 0.05 mm/kyr for medium curvature, and ∼0.11 ± 0.04, 0.08 ± 0.03, 0.06 ± 0.03 mm/kyr for low curvature locations. The observed positive correlation between the curvature and the <span class="hlt">weathering</span> rates is well supported by predictions of <span class="hlt">weathering</span> <span class="hlt">models</span>, i.e., that the curvature of the rind-core boundary controls the porosity creation and <span class="hlt">weathering</span> advance rates at the clast scale. At the watershed scale, the new <span class="hlt">weathering</span> advance rates derived on the low curvature transects for the relatively dry Deshaies watershed (average rate of 0.08 mm/kyr; MAP = 1800 mm and MAT = 23 °C) are ∼60% slower than the rind formation rates previously determined in the much wetter Bras David watershed (∼0.18 mm/kyr, low curvature transect; MAP = 3400 mm and MAT = 23 °C) also on Basse-Terre Island. Thus, a doubling of MAP roughly correlates with a doubling of <span class="hlt">weathering</span> advance rate. The new rind study highlights the effect of precipitation on <span class="hlt">weathering</span> rates over a time scale of ∼100 kyr. <span class="hlt">Weathering</span> rinds are thus a suitable <span class="hlt">system</span> for investigating long-term chemical <span class="hlt">weathering</span> across environmental gradients, complementing short-term riverine solute fluxes.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://www.ars.usda.gov/research/publications/publication/?seqNo115=249303','TEKTRAN'); return false;" href="http://www.ars.usda.gov/research/publications/publication/?seqNo115=249303"><span>Evaluating the accuracy of VEMAP daily <span class="hlt">weather</span> data for application in crop simulations on a regional scale</span></a></p> <p><a target="_blank" href="https://www.ars.usda.gov/research/publications/find-a-publication/">USDA-ARS?s Scientific Manuscript database</a></p> <p></p> <p></p> <p><span class="hlt">Weather</span> plays a critical role in eco-environmental and agricultural <span class="hlt">systems</span>. Limited availability of meteorological records often constrains the applications of simulation <span class="hlt">models</span> and related decision support tools. The Vegetation/Ecosystem <span class="hlt">Modeling</span> and Analysis Project (VEMAP) provides daily <span class="hlt">weather</span>...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2012EGUGA..14.1916G','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2012EGUGA..14.1916G"><span>How accurate are the <span class="hlt">weather</span> forecasts for Bierun (southern Poland)?</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Gawor, J.</p> <p>2012-04-01</p> <p><span class="hlt">Weather</span> forecast accuracy has increased in recent times mainly thanks to significant development of numerical <span class="hlt">weather</span> prediction <span class="hlt">models</span>. Despite the improvements, the forecasts should be verified to control their quality. The evaluation of forecast accuracy can also be an interesting learning activity for students. It joins natural curiosity about everyday <span class="hlt">weather</span> and scientific process skills: problem solving, database technologies, graph construction and graphical analysis. The examination of the <span class="hlt">weather</span> forecasts has been taken by a group of 14-year-old students from Bierun (southern Poland). They participate in the GLOBE program to develop inquiry-based investigations of the local environment. For the atmospheric research the automatic <span class="hlt">weather</span> station is used. The observed data were compared with corresponding forecasts produced by two numerical <span class="hlt">weather</span> prediction <span class="hlt">models</span>, i.e. COAMPS (Coupled Ocean/Atmosphere Mesoscale Prediction <span class="hlt">System</span>) developed by Naval Research Laboratory Monterey, USA; it runs operationally at the Interdisciplinary Centre for Mathematical and Computational <span class="hlt">Modelling</span> in Warsaw, Poland and COSMO (The Consortium for Small-scale <span class="hlt">Modelling</span>) used by the Polish Institute of Meteorology and Water Management. The analysed data included air temperature, precipitation, wind speed, wind chill and sea level pressure. The prediction periods from 0 to 24 hours (Day 1) and from 24 to 48 hours (Day 2) were considered. The verification statistics that are commonly used in meteorology have been applied: mean error, also known as bias, for continuous data and a 2x2 contingency table to get the hit rate and false alarm ratio for a few precipitation thresholds. The results of the aforementioned activity became an interesting basis for discussion. The most important topics are: 1) to what extent can we rely on the <span class="hlt">weather</span> forecasts? 2) How accurate are the forecasts for two considered time ranges? 3) Which precipitation threshold is the most predictable? 4) Why</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/19790015713','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/19790015713"><span>Atmospheric and oceanographic research review, 1978. [global <span class="hlt">weather</span>, ocean/air interactions, and climate</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>Research activities related to global <span class="hlt">weather</span>, ocean/air interactions, and climate are reported. The global <span class="hlt">weather</span> research is aimed at improving the assimilation of satellite-derived data in <span class="hlt">weather</span> forecast <span class="hlt">models</span>, developing analysis/forecast <span class="hlt">models</span> that can more fully utilize satellite data, and developing new measures of forecast skill to properly assess the impact of satellite data on <span class="hlt">weather</span> forecasting. The oceanographic research goal is to understand and <span class="hlt">model</span> the processes that determine the general circulation of the oceans, focusing on those processes that affect sea surface temperature and oceanic heat storage, which are the oceanographic variables with the greatest influence on climate. The climate research objective is to support the development and effective utilization of space-acquired data <span class="hlt">systems</span> in climate forecast <span class="hlt">models</span> and to conduct sensitivity studies to determine the affect of lower boundary conditions on climate and predictability studies to determine which global climate features can be <span class="hlt">modeled</span> either deterministically or statistically.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/20140007294','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/20140007294"><span>Expansion of the Real-time Sport-land Information <span class="hlt">System</span> for NOAA/National <span class="hlt">Weather</span> Service Situational Awareness and Local <span class="hlt">Modeling</span> Applications</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Case, Jonathan L.</p> <p>2014-01-01</p> <p>The NASA Short-term Prediction Research and Transition (SPoRT) Center has been running a real-time version of the Land Information <span class="hlt">System</span> (LIS) since summer 2010 (hereafter, SPoRTLIS). The real-time SPoRT-LIS runs the Noah land surface <span class="hlt">model</span> (LSM) in an offline capacity apart from a numerical <span class="hlt">weather</span> prediction <span class="hlt">model</span>, using input atmospheric and precipitation analyses (i.e., "forcings") to drive the Noah LSM integration at 3-km resolution. Its objectives are to (1) produce local-scale information about the soil state for NOAA/National <span class="hlt">Weather</span> Service (NWS) situational awareness applications such as drought monitoring and assessing flood potential, and (2) provide land surface initialization fields for local <span class="hlt">modeling</span> initiatives. The current domain extent has been limited by the input atmospheric analyses that drive the Noah LSM integration within SPoRT-LIS, specifically the National Centers for Environmental Prediction (NCEP) Stage IV precipitation analyses. Due to the nature of the geographical edges of the Stage IV precipitation grid and its limitations in the western U.S., the SPoRT-LIS was originally confined to a domain fully nested within the Stage IV grid, over the southeastern half of the Conterminous United States (CONUS). In order to expand the real-time SPoRT-LIS to a full CONUS domain, alternative precipitation forcing datasets were explored in year-long, offline comparison runs of the Noah LSM. Based on results of these comparison simulations, we chose to implement the radar/gauge-based precipitation analyses from the National Severe Storms Laboratory as a replacement to the Stage IV product. The Multi-Radar Multi-Sensor (MRMS; formerly known as the National Mosaic and multi-sensor Quantitative precipitation estimate) product has full CONUS coverage at higher-resolution, thereby providing better coverage and greater detail than that of the Stage IV product. This paper will describe the expanded/upgraded SPoRT-LIS, present comparisons between the</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017AGUFMSH34B..05W','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017AGUFMSH34B..05W"><span>Solar Atmosphere to Earth's Surface: Long Lead Time dB/dt Predictions with the Space <span class="hlt">Weather</span> <span class="hlt">Modeling</span> Framework</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Welling, D. T.; Manchester, W.; Savani, N.; Sokolov, I.; van der Holst, B.; Jin, M.; Toth, G.; Liemohn, M. W.; Gombosi, T. I.</p> <p>2017-12-01</p> <p>The future of space <span class="hlt">weather</span> prediction depends on the community's ability to predict L1 values from observations of the solar atmosphere, which can yield hours of lead time. While both empirical and physics-based L1 forecast methods exist, it is not yet known if this nascent capability can translate to skilled dB/dt forecasts at the Earth's surface. This paper shows results for the first forecast-quality, solar-atmosphere-to-Earth's-surface dB/dt predictions. Two methods are used to predict solar wind and IMF conditions at L1 for several real-world coronal mass ejection events. The first method is an empirical and observationally based <span class="hlt">system</span> to estimate the plasma characteristics. The magnetic field predictions are based on the Bz4Cast <span class="hlt">system</span> which assumes that the CME has a cylindrical flux rope geometry locally around Earth's trajectory. The remaining plasma parameters of density, temperature and velocity are estimated from white-light coronagraphs via a variety of triangulation methods and forward based <span class="hlt">modelling</span>. The second is a first-principles-based approach that combines the Eruptive Event Generator using Gibson-Low configuration (EEGGL) <span class="hlt">model</span> with the Alfven Wave Solar <span class="hlt">Model</span> (AWSoM). EEGGL specifies parameters for the Gibson-Low flux rope such that it erupts, driving a CME in the coronal <span class="hlt">model</span> that reproduces coronagraph observations and propagates to 1AU. The resulting solar wind predictions are used to drive the operational Space <span class="hlt">Weather</span> <span class="hlt">Modeling</span> Framework (SWMF) for geospace. Following the configuration used by NOAA's Space <span class="hlt">Weather</span> Prediction Center, this setup couples the BATS-R-US global magnetohydromagnetic <span class="hlt">model</span> to the Rice Convection <span class="hlt">Model</span> (RCM) ring current <span class="hlt">model</span> and a height-integrated ionosphere electrodynamics <span class="hlt">model</span>. The long lead time predictions of dB/dt are compared to <span class="hlt">model</span> results that are driven by L1 solar wind observations. Both are compared to real-world observations from surface magnetometers at a variety of geomagnetic latitudes</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2011SPIE.8186E..0HR','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2011SPIE.8186E..0HR"><span>Active imaging <span class="hlt">systems</span> to perform the strategic surveillance of an aircraft environment in bad <span class="hlt">weather</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>Riviere, Nicolas; Hespel, Laurent; Ceolato, Romain; Drouet, Florence</p> <p>2011-11-01</p> <p>Onera, the French Aerospace Lab, develops and <span class="hlt">models</span> active imaging <span class="hlt">systems</span> to understand the relevant physical phenomena impacting on their performances. As a consequence, efforts have been done both on the propagation of a pulse through the atmosphere (scintillation and turbulence effects) and, on target geometries and their surface properties (radiometric and speckle effects). But these imaging <span class="hlt">systems</span> must operate at night in all ambient illuminations and <span class="hlt">weather</span> conditions in order to perform the strategic surveillance of the environment for various worldwide operations or to perform the enhanced navigation of an aircraft. Onera has implemented codes for 2D and 3D laser imaging <span class="hlt">systems</span>. As we aim to image a scene even in the presence of rain, snow, fog or haze, Onera introduces such meteorological effects in these numerical <span class="hlt">models</span> and compares simulated images with measurements provided by commercial imaging <span class="hlt">systems</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_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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