Search results for "solar"

showing 10 items of 2301 documents

Multi-point galactic cosmic ray measurements between 1 and 4.5 AU over a full solar cycle

2019

The radiation data collected by the Standard Radiation Environment Monitor (SREM) aboard ESA missions INTEGRAL (INTErnational Gamma-Ray Astrophysics Laboratory), Rosetta, Herschel, Planck and Proba-1, and by the high-energy neutron detector (HEND) instrument aboard Mars Odyssey, are analysed with an emphasis on characterising galactic cosmic rays (GCRs) in the inner heliosphere. A cross calibration between all sensors was performed for this study, which can also be used in subsequent works. We investigate the stability of the SREM detectors over long-term periods. The radiation data are compared qualitatively and quantitatively with the corresponding solar activity. Based on INTEGRAL and Ro…

Atmospheric Science010504 meteorology & atmospheric sciencesCometFluxCosmic rayRadiation01 natural sciencessymbols.namesake0103 physical sciencesEarth and Planetary Sciences (miscellaneous)Neutron detectionPlancklcsh:Science010303 astronomy & astrophysics0105 earth and related environmental sciencesPhysicslcsh:QC801-809AstronomyGeologyAstronomy and Astrophysicslcsh:QC1-999Solar cyclelcsh:Geophysics. Cosmic physics13. Climate actionSpace and Planetary Sciencesymbolslcsh:QHeliospherelcsh:PhysicsAnnales Geophysicae
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Exploring the Validity of the Long-Term Data Record V4 Database for Land Surface Monitoring

2016

A new version of the long-term data record (LTDR)—Version 4—has been released recently by NASA. This database includes daily information for all advanced very high resolution radiometer channels, as well as ancillary data, from July 1981 up to present. This dataset is the longest available record of remotely sensed data useful for land surface monitoring, since it allows the daily estimation of vegetation indices, as well as the estimation of land surface temperature (LST). Here, we analyze the fitness of this database for land surface monitoring, especially as regards long-term trends and their validity. To that end, we estimated normalized difference vegetation index (NDVI), LST, as well …

Atmospheric Science010504 meteorology & atmospheric sciencesDatabaseAdvanced very-high-resolution radiometer0211 other engineering and technologiesSolar zenith angle02 engineering and technologyEnhanced vegetation indexVegetationcomputer.software_genre01 natural sciencesNormalized Difference Vegetation IndexAncillary dataEnvironmental scienceComputers in Earth SciencesTime seriescomputer021101 geological & geomatics engineering0105 earth and related environmental sciencesRemote sensingInterpolationIEEE Journal of Selected Topics in Applied Earth Observations and Remote Sensing
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Heating rate profiles and radiative forcing due to a dust storm in the Western Mediterranean using satellite observations

2017

Abstract We analyze the vertically-resolved radiative impact due to a dust storm in the Western Mediterranean. The dust plume travels around 3–5 km altitude and the aerosol optical depth derived by MODIS at 550 nm ranges from 0.33 to 0.52 at the overpass time (13:05 UT). The aerosol radiative forcing (ARF), forcing efficiency (FE) and heating rate profile (AHR) are determined throughout the dust trajectory in shortwave (SW) and longwave (LW) ranges. To do this, we integrate different satellite observations (CALIPSO and MODIS) and detailed radiative transfer modeling. The combined (SW + LW) effect of the dust event induces a net cooling in the studied region. On average, the FE at 22.4° sola…

Atmospheric Science010504 meteorology & atmospheric sciencesLongwaveSolar zenith angleRadiative forcing010502 geochemistry & geophysicsAtmospheric sciences01 natural sciencesPlumeDust stormRadiative transferEnvironmental scienceShortwaveRefractive index0105 earth and related environmental sciencesGeneral Environmental ScienceAtmospheric Environment
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A new technique for observationally derived boundary conditions for space weather

2018

This research has received funding from the European Research Council (ERC) under the European Union’s Horizon 2020 research and innovation programme (grant agreement No 647214). D.H.M. would like to thank STFC and the Leverhulme Trust for their financial support. ARY was supported by STFC consortium grant ST/N000781/1 to the universities of Dundee and Durham. Context.  In recent years, space weather research has focused on developing modelling techniques to predict the arrival time and properties of coronal mass ejections (CMEs) at the Earth. The aim of this paper is to propose a new modelling technique suitable for the next generation of Space Weather predictive tools that is both efficie…

Atmospheric Science010504 meteorology & atmospheric sciencesMHDNDASWeather forecastingFluxFOS: Physical sciencesContext (language use)Space weatherlcsh:QC851-999computer.software_genre01 natural sciencesSolar Corona0103 physical sciencesCMECoronal mass ejectionQB AstronomyAstrophysics::Solar and Stellar AstrophysicsQA MathematicsBoundary value problemQA010303 astronomy & astrophysicsR2CSolar and Stellar Astrophysics (astro-ph.SR)QB0105 earth and related environmental sciencesPhysicssolar CoronaMechanicsMagnetic fluxAstrophysics - Solar and Stellar Astrophysics13. Climate actionSpace and Planetary SciencePhysics::Space Physicslcsh:Meteorology. ClimatologyMagnetohydrodynamicsBDCcomputerJournal of Space Weather and Space Climate
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Simulation of Future Geostationary Ocean Color Images

2012

The objective of this work is to simulate global images that would be provided by a theoretical ocean color sensor on a geostationary orbit at longitude 0, in order to assess the range of radiance value data reaching the sensor throughout the day for 20 spectral bands similar to those of the Ocean and Land Color Imager (OLCI). The secondary objective is to assess the illumination and viewing geometries that result in sunglint. For this purpose, we combined a radiative transfer model for ocean waters (Hydrolight) and a radiative transfer model for atmosphere (MODTRAN) to construct the simulated radiance images at the sea surface and at the Top-Of-Atmosphere (TOA). Bio-optical data from GlobC…

Atmospheric Science010504 meteorology & atmospheric sciencesMeteorologyMODTRANSolar zenith angleSunglint01 natural sciences010309 opticsAtmospheric radiative transfer codes13. Climate actionOcean color0103 physical sciencesGeostationary orbitRadianceEnvironmental scienceComputers in Earth Sciences[SPI.SIGNAL]Engineering Sciences [physics]/Signal and Image processingComputingMilieux_MISCELLANEOUSZenith0105 earth and related environmental sciencesRemote sensingIEEE Journal of Selected Topics in Applied Earth Observations and Remote Sensing
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Effective cloud optical depth and enhancement effects for broken liquid water clouds in Valencia (Spain)

2017

Partly cloudy skies with liquid water clouds have been analysed, founding that it is essential to distinguish data if the Sun is obstructed or not by clouds. Both cases can be separated considering simultaneously the Cloud Modification Factor (CMF) and the clearness index (kt). For partly cloudy skies and the Sun obstructed the effective cloud optical depth (τ) has been obtained by the minimization method for overcast skies. This method was previously developed by the authors but, in this case, taking into account partial cloud cover. This study has been conducted for the years 2011–2015 with the multiple scattering model SBDART and irradiance measurements for the UV Erythemal Radiation (UV…

Atmospheric Science010504 meteorology & atmospheric sciencesMeteorologybusiness.industryCloud coverIrradianceSolar zenith angleCloud computingRadiation010502 geochemistry & geophysics01 natural sciencesCloud optical depthOvercastRange (statistics)Environmental sciencebusinessAstrophysics::Galaxy Astrophysics0105 earth and related environmental sciencesAtmospheric Research
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Reconstruction of the Parker spiral with the Reverse in situ data and MHD APproach - RIMAP

2021

The reconstruction of plasma parameters in the interplanetary medium is very important to understand the interplanetary propagation of solar eruptions and for Space Weather application purposes. Because only a few spacecraft are measuring in situ these parameters, reconstructions are currently performed by running complex numerical Magneto-hydrodynamic (MHD) simulations starting from remote sensing observations of the Sun. Current models apply full 3D MHD simulations of the corona or extrapolations of photospheric magnetic fields combined with semi-empirical relationships to derive the plasma parameters on a sphere centered on the Sun (inner boundary). The plasma is then propagated in the i…

Atmospheric Science010504 meteorology & atmospheric sciencesSpace weatherSolar windInterplanetary mediumSpace weatherlcsh:QC851-99901 natural sciencesHeliosphere0103 physical sciencesCoronal mass ejectionAstrophysics::Solar and Stellar Astrophysics010303 astronomy & astrophysics0105 earth and related environmental sciencesPhysicsModelingCoronal mass ejections; Heliosphere; Interplanetary medium; Modeling; Solar wind; Space weatherComputational physicsSolar windSpace and Planetary SciencePhysics::Space PhysicsCoronal mass ejectionslcsh:Meteorology. ClimatologyHeliospheric current sheetAstrophysics::Earth and Planetary AstrophysicsMagnetohydrodynamicsInterplanetary spaceflightHeliosphereInterplanetary medium
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Intermittent release of transients in the slow solar wind: 1. Remote sensing observations

2010

[1] The Heliospheric Imager (HI) instruments on board the STEREO spacecraft are used to analyze the solar wind during August and September 2007. We show how HI can be used to image the streamer belt and, in particular, the variability of the slow solar wind which originates inside and in the vicinity of the streamer belt. Intermittent mass flows are observed in HI difference images, streaming out along the extension of helmet streamers. These flows can appear very differently in images: plasma distributed on twisted flux ropes, V-shaped structures, or “blobs.” The variety of these transient features may highlight the richness of phenomena that could occur near helmet streamers: emergence of…

Atmospheric ScienceAstrophysics::High Energy Astrophysical PhenomenaSoil ScienceFluxInterplanetary mediumAquatic ScienceOceanographyPhysics::Plasma PhysicsGeochemistry and PetrologyEarth and Planetary Sciences (miscellaneous)Astrophysics::Solar and Stellar AstrophysicsInterplanetary magnetic fieldEjectaEarth-Surface ProcessesWater Science and TechnologyPhysicsEcologyPaleontologyAstronomyForestryHelmet streamerCoronaSolar windGeophysicsSpace and Planetary SciencePhysics::Space PhysicsOutflowAstrophysics::Earth and Planetary AstrophysicsJournal of Geophysical Research: Space Physics
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Influence of air mass history on the columnar aerosol properties at Valencia, Spain

2007

[1] The physical and radiative properties of atmospheric aerosols have been obtained in Valencia (latitude 39.508°, longitude −0.418°, 60 m a. s. l.), a city of the Spanish Mediterranean coast, by the inversion of direct solar irradiance and diffuse sky irradiance measurements made with a CIMEL CE318 system, from January 2002 to July 2005. The data acquired by the CE318 were used to determine the instantaneous values of the aerosol optical depth (AOD), the columnar water vapor content (w) and the Angstrom wavelength exponent (α). The SKYRAD code was used to obtain the size distribution, the asymmetry parameter, the complex refractive index and the single scattering albedo of the aerosols. B…

Atmospheric ScienceEcologyMeteorologySingle-scattering albedoIrradiancePaleontologySoil ScienceForestryAquatic ScienceOceanographySolar irradianceAtmospheric sciencesAerosolGeophysicsSpace and Planetary ScienceGeochemistry and PetrologyEarth and Planetary Sciences (miscellaneous)Radiative transferEnvironmental scienceLongitudeWater vaporAir massEarth-Surface ProcessesWater Science and TechnologyJournal of Geophysical Research
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Simulation of a biomass-burning plume: Comparison of model results with observations

2002

[1] We have simulated the dynamical evolution of the plume from a prescribed biomass fire, using the active tracer high- resolution atmospheric model (ATHAM). Initialization parameters were set to reflect the conditions during the fire. The model results are compared with airborne remote-sensing and in situ measurements of the plume. ATHAM reproduces the injection height (250-600 m) and the horizontal extent of the plume (similar to4 km) with good accuracy. The aerosol mass concentrations are underestimated but still in the range of the observations. Remaining differences between the model results and the measurements are attributed to limited meteorological and fire emission information. A…

Atmospheric ScienceEcologyMicrophysicsMeteorologySolar zenith anglePaleontologySoil ScienceForestryAtmospheric modelAquatic ScienceRadiative forcingOceanographyPlumeAerosolGeophysicsSpace and Planetary ScienceGeochemistry and PetrologyEarth and Planetary Sciences (miscellaneous)Radiative transferOptical depthEarth-Surface ProcessesWater Science and Technology
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