Search results for "BED"

showing 10 items of 1605 documents

Measurement-based J(NO2) sensitivity in a cloudless atmosphere under low aerosol loading and high solar zenith angle conditions

2000

Abstract The comparison between measured and simulated photodissociation frequencies of NO 2 , J( NO 2 ) , in a cloudless atmosphere in a recent paper by Fruh et al., 2000 (Journal of Geophysical Research 105, 9843–9857) revealed an overestimation of J(NO2) near ground level by model calculations compared with measurements and an underestimation in the upper part of the aerosol layer. A possible reason for the disagreement is the changing sun position during the vertical ascent. To resolve this problem we carried out a sensitivity study varying the solar zenith angle of 74° by 1.4° (which corresponds to the change of sun position during the vertical flight patterns). This results in a consi…

AtmosphereAtmospheric ScienceWavelengthMaterials scienceAltitudeMeteorologySolar zenith angleHumidityRelative humidityAlbedoAtmospheric sciencesGeneral Environmental ScienceAerosol
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Narrow-band to broad-band conversion for Meteosat-visiible channel and broad-band albedo using both AVHRR-1 and -2 channels

1995

Abstract Satellite-derived broad-band albedo offers a useful tool for monitoring surface conditions. Given the limited wavelength window of most satellite radiometers, satellite albedo studies need to define narrow-band to a broad-band transformations. Signals from the AVHRR channels on board the NOAA-11 satellite, the Meteosat visible channel and a rectangular spectral band from 0-3 to 2.5 μm were simulated for a set of 20 representative land surfaces. The radiative transfer code described in Tanre et al. (1990) was used to obtain top of the atmosphere radiances. The derived signals were then correlated to predict broadband albedo and the Meteosal response via the two AVHRR signals. The re…

AtmosphereWavelengthRadiometerRadiative transferGeneral Earth and Planetary SciencesEnvironmental scienceRadiometrySatelliteSpectral bandsAlbedoRemote sensingInternational Journal of Remote Sensing
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Comparing airborne and satellite retrievals of cloud optical thickness and particle effective radius using a spectral radiance ratio technique: two c…

2018

Solar radiation reflected by cirrus and deep convective clouds (DCCs) was measured by the Spectral Modular Airborne Radiation Measurement System (SMART) installed on the German High Altitude and Long Range Research Aircraft (HALO) during the Mid-Latitude Cirrus (ML-CIRRUS) and the Aerosol, Cloud, Precipitation, and Radiation Interaction and Dynamic of Convective Clouds System – Cloud Processes of the Main Precipitation Systems in Brazil: A Contribution to Cloud Resolving Modelling and to the Global Precipitation Measurement (ACRIDICON-CHUVA) campaigns. On particular flights, HALO performed measurements closely collocated with overpasses of the Moderate Resolution Imaging Spectroradiometer (…

Atmospheric Science010504 meteorology & atmospheric sciences0211 other engineering and technologiescirrus02 engineering and technology01 natural sciencesPhysics::Geophysicslcsh:ChemistryNadirRadiative transferconvective cloudsWolkenphysiksatellite retrievalsAstrophysics::Galaxy AstrophysicsPhysics::Atmospheric and Oceanic Physics021101 geological & geomatics engineering0105 earth and related environmental sciencesRemote sensingEffective radiusAlbedolcsh:QC1-999lcsh:QD1-999RadianceEnvironmental scienceCirrusModerate-resolution imaging spectroradiometerspectral radiancecloud optical thicknessGlobal Precipitation Measurementlcsh:PhysicsAtmospheric Chemistry and Physics
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Microphysical and radiative characterization of a subvisible midlevel Arctic ice cluod by airborne observations - a case study

2009

During the Arctic Study of Tropospheric Aerosol, Clouds and Radiation (ASTAR) campaign, which was conducted in March and April 2007, an optically thin ice cloud was observed south of Svalbard at around 3 km altitude. The microphysical and radiative properties of this particular subvisible midlevel cloud were investigated with complementary remote sensing and in situ instruments. Collocated airborne lidar remote sensing and spectral solar radiation measurements were performed at a flight altitude of 2300 m below the cloud base. Under almost stationary atmospheric conditions, the same subvisible midlevel cloud was probed with various in situ sensors roughly 30 min later. <br><br> …

Atmospheric Science010504 meteorology & atmospheric sciencesASTARArktische GrenzschichtMischphasenwolken[SDU.STU.ME]Sciences of the Universe [physics]/Earth Sciences/MeteorologyAtmospheric sciences01 natural sciences010309 opticslcsh:Chemistry0103 physical sciencesRadiative transferPhysics::Atmospheric and Oceanic Physics0105 earth and related environmental sciencesRemote sensing[SDU.OCEAN]Sciences of the Universe [physics]/Ocean Atmosphere[PHYS.PHYS.PHYS-AO-PH]Physics [physics]/Physics [physics]/Atmospheric and Oceanic Physics [physics.ao-ph]geographyIce cloudLidargeography.geographical_feature_categoryIce crystalsNephelometerCloud topArctic ice packlcsh:QC1-999Lidarlcsh:QD1-99913. Climate actionCloud albedoEnvironmental scienceAstrophysics::Earth and Planetary Astrophysicslcsh:PhysicsWolkenphysik und Verkehrsmeteorologie
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Cloud phase identification of Arctic boundary-layer clouds from airborne spectral reflection measurements: test of three approaches

2008

Abstract. Arctic boundary-layer clouds were investigated with remote sensing and in situ instruments during the Arctic Study of Tropospheric Aerosol, Clouds and Radiation (ASTAR) campaign in March and April 2007. The clouds formed in a cold air outbreak over the open Greenland Sea. Beside the predominant mixed-phase clouds pure liquid water and ice clouds were observed. Utilizing measurements of solar radiation reflected by the clouds three methods to retrieve the thermodynamic phase of the cloud are introduced and compared. Two ice indices IS and IP were obtained by analyzing the spectral pattern of the cloud top reflectance in the near infrared (1500–1800 nm wavelength) spectral range whi…

Atmospheric Science010504 meteorology & atmospheric sciencesIce crystals01 natural sciencesPhysics::Geophysics010309 opticsArctic13. Climate actionPhase (matter)0103 physical sciencesCloud albedoSpectral slopeRadiative transferEnvironmental scienceAstrophysics::Earth and Planetary AstrophysicsSea ice concentrationAstrophysics::Galaxy AstrophysicsPhysics::Atmospheric and Oceanic Physics0105 earth and related environmental sciencesRemote sensingOptical properties of water and iceAtmospheric Chemistry and Physics
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A case study of the radiative effect of aerosols over Europe: EUCAARI-LONGREX

2016

Abstract. The radiative effect of anthropogenic aerosols over Europe during the 2008 European Integrated Project on Aerosol Cloud Climate and Air Quality Interactions Long Range Experiment (EUCAARI-LONGREX) campaign has been calculated using measurements collected by the Facility for Airborne Atmospheric Measurements (FAAM) BAe-146 aircraft and radiative transfer modelling. The aircraft sampled anthropogenically perturbed air masses across north-western Europe under anticyclonic conditions with aerosol optical depths ranging from 0.047 to 0.357. For one specially designed “radiative closure” flight, simulated irradiances have been compared to radiation measurements for a case of aged Europe…

Atmospheric Science010504 meteorology & atmospheric sciencesMeteorology010401 analytical chemistryAlbedoRadiationAtmospheric sciences01 natural scienceslcsh:QC1-9990104 chemical sciencesAerosollcsh:ChemistryAtmospheric radiative transfer codeslcsh:QD1-999AnticycloneRadiative transferEnvironmental scienceSpectral resolutionAir quality indexlcsh:Physics0105 earth and related environmental sciencesAtmospheric Chemistry and Physics
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Factors for inconsistent aerosol single scattering albedo between SKYNET and AERONET

2016

SKYNET and Aerosol Robotic Network (AERONET) retrieved aerosol single scattering albedo (SSA) values of four sites, Chiba (Japan), Pune (India), Valencia (Spain), and Seoul (Korea), were compared to understand the factors behind often noted large SSA differences between them. SKYNET and AERONET algorithms are found to produce nearly same SSAs for similarity in input data, suggesting that SSA differences between them are primarily due to quality of input data due to different calibration and/or observation protocols as well as difference in quality assurance criteria. The most plausible reason for high SSAs in SKYNET is found to be underestimated calibration constant for sky radiance (ΔΩ). T…

Atmospheric Science010504 meteorology & atmospheric sciencesMeteorologySingle-scattering albedomedia_common.quotation_subjectSKYNETAlbedo01 natural sciencesAERONETAerosol010309 opticsGeophysicsIntegrating sphereSpace and Planetary ScienceSky0103 physical sciencesEarth and Planetary Sciences (miscellaneous)RadianceEnvironmental science0105 earth and related environmental sciencesRemote sensingmedia_commonJournal of Geophysical Research: Atmospheres
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Vertical profiles of light absorption and scattering associated with black carbon particle fractions in the springtime Arctic above 79° N

2020

Despite the potential importance of black carbon (BC) for radiative forcing of the Arctic atmosphere, vertically resolved measurements of the particle light scattering coefficient (σsp) and light absorption coefficient (σap) in the springtime Arctic atmosphere are infrequent, especially measurements at latitudes at or above 80∘ N. Here, relationships among vertically distributed aerosol optical properties (σap, σsp and single scattering albedo or SSA), particle microphysics and particle chemistry are examined for a region of the Canadian archipelago between 79.9 and 83.4∘ N from near the surface to 500 hPa. Airborne data collected during April 2015 are combined with gro…

Atmospheric Science010504 meteorology & atmospheric sciencesMicrophysicsSingle-scattering albedo010501 environmental sciencesRadiative forcingAtmospheric sciences01 natural scienceslcsh:QC1-999Light scatteringAerosollcsh:ChemistryTroposphereAtmospherelcsh:QD1-999Arctic13. Climate actionlcsh:Physics0105 earth and related environmental sciencesAtmospheric Chemistry and Physics
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Black and brown carbon over central Amazonia: long-term aerosol measurements at the ATTO site

2018

The Amazon rainforest is a sensitive ecosystem experiencing the combined pressures of progressing deforestation and climate change. Its atmospheric conditions oscillate between biogenic and biomass burning (BB) dominated states. The Amazon further represents one of the few remaining continental places where the atmosphere approaches pristine conditions during occasional wet season episodes. The Amazon Tall Tower Observatory (ATTO) has been established in central Amazonia to investigate the complex interactions between the rainforest ecosystem and the atmosphere. Physical and chemical aerosol properties have been analyzed continuously since 2012. This paper provides an in-depth analysis of t…

Atmospheric Science010504 meteorology & atmospheric sciencesSingle-scattering albedoAmazon rainforest010501 environmental sciencesCombustionAtmospheric sciences01 natural scienceslcsh:QC1-999Aerosollcsh:ChemistryAtmospherelcsh:QD1-999Dry seasonForest ecologyEnvironmental scienceAbsorption (electromagnetic radiation)lcsh:Physics0105 earth and related environmental sciencesAtmospheric Chemistry and Physics
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Desert dust aerosol air mass mapping in the western Sahara, using particle properties derived from space-based multi-angle imaging

2009

Coincident observations made over the Moroccan desert during the Sahara mineral dust experiment (SAMUM) 2006 field campaign are used both to validate aerosol amount and type retrieved from multi-angle imaging spectroradiometer (MISR) observations, and to place the suborbital aerosol measurements into the satellite's larger regional context. On three moderately dusty days during which coincident observations were made, MISR mid-visible aerosol optical thickness (AOT) agrees with field measurements point-by-point to within 0.05–0.1. This is about as well as can be expected given spatial sampling differences; the space-based observations capture AOT trends and variability over an extended regi…

Atmospheric Science010504 meteorology & atmospheric sciencesaerosolAtmosphärische SpurenstoffeContext (language use)010501 environmental sciencesMineral dustAlbedoAtmospheric sciences01 natural sciencesPlumeAerosolSAMUMMIRSTroposphereEnvironmental scienceAeolian processesAir mass0105 earth and related environmental sciencesRemote sensingTellus B: Chemical and Physical Meteorology
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