Search results for "LBE"

showing 10 items of 1617 documents

Columnar aerosol properties in a Northeastern Atlantic site (Plymouth, United Kingdom) by means of ground based skyradiometer data during years 2000-…

2012

Between 2000 and 2008, columnar optical and radiative properties were measured at the Plymouth Marine Laboratory (PML), UK (50° 21.95'N, 4° 8.85'W) using an automatic Prede POM01L sun-sky photometer. The database was analyzed for aerosol optical properties using the SKYRAD radiative inversion algorithm and calibrated using the in situ SKYIL calibration method. Retrievals include aerosol optical depth, ångström wavelength exponent, aerosol volume distribution, refractive index and single scattering albedo. The results show that the Plymouth site is characterized by low values of aerosol optical depth with low variability (0.18 ± 0.08 at 500 nm) and a mean annual ångström exponent of 1.03 ± 0…

Atmospheric ScienceAngstrom exponentSKYNETSingle-scattering albedoMarine aerosolsSKYNETAODMineral dustAerosolWavelengthSkyradiometerClimatologyRadiative transferPrede POMAir massGeneral Environmental ScienceESR
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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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Modeling the outdoor cooling impact of highly radiative “super cool” materials applied on roofs

2021

Abstract Highly reflective “cool materials” are commonly used to reduce temperatures in the urban environment. Recently developed “super cool” materials feature an even higher albedo and emissivity (both above 0.95) than traditional cool materials. To examine the impacts of super cool roofing materials on outdoor air temperature compared to traditional cool roofs and green roofs, we conduct a sensitivity study with the microclimate model ENVI-met. Simulated surface temperature of super cool roofs remained around 6 K below ambient air temperature during high solar irradiation, which is consistent with observations. Super cool roofs – with an averaged street-level air temperature cooling of a…

Atmospheric ScienceGeography Planning and DevelopmentAir exchangeMicroclimateEnvironmental Science (miscellaneous)AlbedoAtmospheric sciencesAmbient airUrban StudiesEmissivityRadiative transferEnvironmental scienceReflective surfacesRoofUrban Climate
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A new method to retrieve the aerosol layer absorption coefficient from airborne flux density and actinic radiation measurements

2010

A new method is presented to derive the mean value of the spectral absorption coefficient of an aerosol layer from combined airborne measurements of spectral net irradiance and actinic flux density. While the method is based on a theoretical relationship of radiative transfer theory, it is applied to atmospheric radiation measurements for the first time. The data have been collected with the Spectral Modular Airborne Radiation Measurement System (SMARTA¢Â€ÂAlbedometer), the Solar Spectral Flux Radiometer (SSFR), and the Actinic Flux Spectroradiometer (AFSR) during four field campaigns between 2002 and 2008 (the Saharan Mineral Dust Experiment (SAMUM), the Influence of Clouds on the Spectra…

Atmospheric ScienceIrradianceSoil ScienceFluxAquatic ScienceOceanographySSFRTroposphereRadiative fluxAtmospheric radiative transfer codesGeochemistry and PetrologySMART‐AlbedometerEarth and Planetary Sciences (miscellaneous)Radiative transferOptical depthPhysics::Atmospheric and Oceanic PhysicsEarth-Surface ProcessesWater Science and TechnologyRemote sensingARCTAS/ARCPACLidarRadiometerEcologyPaleontologyForestrySAMUMGeophysicsSpace and Planetary ScienceEnvironmental science
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In situ measurements of optical properties at Tinfou (Morocco) during the Saharan Mineral Dust Experiment SAMUM 2006

2009

In situ measurements of optical and physical properties of mineral dust were performed at the outskirts of the Saharan Desert in the framework of the Saharan Mineral Dust Experiment part 1 (SAMUM-1). Goals of the field study were to achieve information on the extent and composition of the dust particle size distribution and the optical properties of dust at the ground. For the particle number size distribution, measured with a DMPS/APS, a size dependent dynamic shape factor was considered. The mean refractive index of the particles in this field study is 1.53–4.1 × 10 -3 i at 537 nm wavelength and 1.53–3.1 × 10 -3 i at 637 nm wavelength derived from measurements of scattering and absorption…

Atmospheric ScienceMaterials science010504 meteorology & atmospheric sciencesParticle numberSingle-scattering albedoScatteringMineralogy010501 environmental sciencesMineral dustAlbedo01 natural sciencesAerosolWavelengthParticle-size distribution0105 earth and related environmental sciencesTellus B: Chemical and Physical Meteorology
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Approximation for the absorption coefficient of airborne atmospheric aerosol particles in terms of measurable bulk properties

1977

The absorption coefficient of airborne atmospheric aerosol particles can be approximated by where λ is the wavelength of radiation, n — ik is the mean complex refractive index, ρ the mean bulk density, and M / V k the mass of the particles per unit volume of air. This approximation gives good results at relative humidities between 0 and 0.95 for the wavelengths of radiation between 0.55 μm and 2.0 μm and between 9.25 μm and 12.0 μm. Basing on this approximation it is possible to determine the single scattering albedo of airborne atmospheric aerosol particles with known measuring techniques. DOI: 10.1111/j.2153-3490.1977.tb00711.x

Atmospheric ScienceMaterials science010504 meteorology & atmospheric sciencesSingle-scattering albedobusiness.industryMie scatteringAnalytical chemistryGeneral MedicineRadiationOceanography01 natural sciencesAerosolWavelengthOpticsAttenuation coefficientAbsorptanceAtmospheric refractionbusiness0105 earth and related environmental sciencesTellus A
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The Single-Scattering Albedo of Atmospheric Aerosol Particles as a Function of Relative Humidity

1976

Atmospheric ScienceMaterials scienceSingle-scattering albedoRelative humidityFunction (mathematics)AlbedoAtmospheric sciencesSea salt aerosolAerosolJournal of the Atmospheric Sciences
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The surface shortwave net flux from the scanner for radiation budget (SCARAB)

2002

Abstract Shortwave surface net radiation is usually determined by combining the measurement of insolation with an independent estimate of surface albedo. However, uncertainties associated with each of these quantities may lead to large errors in the value of net surface solar radiation. An alternative approach is to deduce the net solar flux (the term flux is used here as the radiometric quantity flux density) at the surface directly from the budget at the top of the atmosphere, without explicit knowledge of surface albedo. The Satellite Application Facility on Climate Monitoring is a joint project of the German Meteorological Service and other European Meteorological Services dedicated to …

Atmospheric ScienceMeteorologyPolar orbitAerospace EngineeringFluxAstronomy and AstrophysicsContext (language use)AlbedoAtmosphereNet radiometerGeophysicsSpace and Planetary ScienceGeneral Earth and Planetary SciencesEnvironmental scienceSatelliteAstrophysics::Earth and Planetary AstrophysicsShortwavePhysics::Atmospheric and Oceanic PhysicsRemote sensingAdvances in Space Research
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Comparison of AERONET and SKYRAD4.2 inversion products retrieved from a Cimel CE318 sunphotometer

2012

SKYNET is an international research network of ground based sky – sunphotometers for the observation and monitoring of columnar aerosol properties. The algorithm developed by SKYNET is called SKYRAD.pack, and it is used on Prede instruments only. In this study, we have modified the SKYRAD.pack software in order to adapt it to Cimel sunphotometers. A one month database of Cimel data obtained at Burjassot (Valencia, Spain) has been processed with this program and the obtained inversion products have been compared with AERONET retrievals. In general, the differences found were consistent with the individual error assessments for both algorithms. Although the aerosol optical depth com…

Atmospheric ScienceMeteorologySingle-scattering albedolcsh:TA715-787media_common.quotation_subjectlcsh:Earthwork. FoundationsSKYNETInversion (meteorology)AERONETAerosollcsh:Environmental engineeringWavelengthSkyEnvironmental sciencelcsh:TA170-171Refractive indexRemote sensingmedia_common
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Effective cloud optical depth for overcast conditions determined with a UV radiometers

2014

Using a sky camera, episodes characterized by overcast low clouds in the Valencia region of Spain have been selected for analysis. One year of cloud optical depth data have been produced by inverting UV erythemal irradiance measured with a UVB-1 radiometer from Yankee Environmental Systems using the LibRadtran radiative transfer model. Measurement uncertainties, aerosol single scattering albedo and cloud properties are, in order of decreasing importance, the most important factors influencing the accuracy of cloud optical depth retrieval when using UV erythemal radiometers. Statistics for cloud optical depth show a highly skewed frequency distribution best described by a gamma distribution …

Atmospheric ScienceRadiometerSingle-scattering albedomedia_common.quotation_subjectIrradianceAtmospheric sciencesAerosolAtmospheric radiative transfer codesOvercastSkyCloud albedoEnvironmental sciencemedia_commonRemote sensingInternational Journal of Climatology
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