Search results for "Length"

showing 10 items of 2188 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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In-line holography of cloud volumes applied to the measurement of raindrops and snowflakes

1998

Abstract The ground-based HODAR (HOlographic Droplet and Aerosol Recording) of the University of Mainz has been operational since 1989 on the Kleiner Feldberg Mountain Observatory near Frankfurt/Main, Germany, in a `small volume' configuration. With this setup an air volume of approximately 1 l can be in situ recorded, which allows it to image all aerosol particles and droplets with diameter larger than 6 μm contained in the sample volume in situ. Recently the beam diameter and optical path length of the inline system have been enlarged such that large cloud volumes (approximately 500 l) can be recorded on single holograms. During the holographic image reconstruction step in the laboratory,…

Atmospheric ScienceBeam diameterMaterials scienceIce crystalsMeteorologybusiness.industryHolographyCloud physicsAerosollaw.inventionOpticslawSnowflakebusinessRain and snow mixedOptical path lengthAtmospheric Research
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Three-dimensional solar radiation effects on the actinic flux field in a biomass-burning plume

2003

[1] Three-dimensional (3-D) solar radiative transfer models describe radiative transfer under inhomogeneous atmospheric conditions more accurately than the commonly used one-dimensional (1-D) radiative transfer models that assume horizontal homogeneity of the atmosphere. Here results of 3-D radiative transfer simulations for a biomass-burning plume are presented and compared with local one-dimensional (l-1-D) simulations, i.e., 1-D simulations in every column of the model domain. The spatial distribution of the aerosol particles was derived from a 3-D atmospheric transport simulation. We studied the impact of 3-D radiative effects on the actinic flux within the plume center. The differences…

Atmospheric ScienceEcologySolar zenith anglePaleontologySoil ScienceForestryAquatic ScienceOceanographyAtmospheric sciencesAerosolPlumeRadiative fluxWavelengthGeophysicsAtmospheric radiative transfer codesSpace and Planetary ScienceGeochemistry and PetrologyEarth and Planetary Sciences (miscellaneous)Radiative transferPanacheEnvironmental sciencePhysics::Atmospheric and Oceanic PhysicsEarth-Surface ProcessesWater Science and TechnologyJournal of Geophysical Research
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Improving RAMS and WRF mesoscale forecasts over two distinct vegetation covers using an appropriate thermal roughness length parameterization

2019

Land Surface Models (LSM) have shown some difficulties to properly simulate day-time 2-m air and surface skin temperatures. This kind of models are coupled to atmospheric models in mesoscale modelling, such as the Regional Atmospheric Modeling System (RAMS) and the Weather Research and Forecasting (WRF) Model. This model coupling is used within Numerical Weather Prediction Systems (NWP) in order to forecast key physical processes for agricultural meteorology and forestry as well as in ecological modelling. The current study first evaluates the surface energy fluxes and temperatures simulated by these two state-of-the-art NWP models over two distinct vegetated covers, one corresponding to a …

Atmospheric ScienceGlobal and Planetary ChangeMeteorologyNumerical weather prediction/forecastingFísica de la TierraMesoscale meteorologyEuropean Regional Development FundSurface-layer parameterizationForestryVegetationMesoscale modellingBoscos i silviculturaSurface energy fluxRoughness lengthThermal roughness lengthWeather Research and Forecasting ModelEnvironmental scienceLand surface modelsSurface energy fluxesAgronomy and Crop SciencePhysics::Atmospheric and Oceanic Physics
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Depolarization�ratio profiling at several wavelengths in pure Saharan dust during SAMUM 2006

2009

Vertical profiles of the linear particle depolarization ratio of pure dust clouds were measured during the Saharan Mineral Dust Experiment (SAMUM) at Ouarzazate, Morocco (30.9°N, –6.9°E), close to source regions in May–June 2006, with four lidar systems at four wavelengths (355, 532, 710 and 1064 nm). The intercomparison of the lidar systems is accompanied by a discussion of the different calibration methods, including a new, advanced method, and a detailed error analysis. Over the whole SAMUM periode pure dust layers show a mean linear particle depolarization ratio at 532 nm of 0.31, in the range between 0.27 and 0.35, with a mean Ångström exponent (AE, 440–870 nm) of 0.18 (range 0.04–0.34…

Atmospheric ScienceLidarMaterials science010504 meteorology & atmospheric sciencesSaharan dustbusiness.industryAnalytical chemistry010501 environmental sciencesMineral dust01 natural sciencesAerosolTroposphereSAMUMWavelengthOpticsLidardepolarizationExtinction (optical mineralogy)Depolarization ratioParticlebusiness0105 earth and related environmental sciences
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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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A generalized single‐channel method for retrieving land surface temperature from remote sensing data

2003

[1] Many papers have developed algorithms to retrieve land surface temperature from at-sensor and land surface emissivity data. These algorithms have been specified for different thermal sensors on board satellites, i.e., the algorithm used for one thermal sensor (or a combination of thermal sensors) cannot be used for other thermal sensor. The main goal of this paper is to propose a generalized single-channel algorithm that only uses the total atmospheric water vapour content and the channel effective wavelength (assuming that emissivity is known), and can be applied to thermal sensors characterized with a FWHM (Full-Width Half-Maximum) of around 1 μm actually operative on board satellites…

Atmospheric ScienceMaterials scienceEcologyPaleontologySoil ScienceForestryAquatic ScienceOceanographyAtmospheric temperatureRoot mean squareWavelengthGeophysicsSpace and Planetary ScienceGeochemistry and PetrologyThematic MapperEarth and Planetary Sciences (miscellaneous)EmissivitySatelliteWater vaporEarth-Surface ProcessesWater Science and TechnologyRemote sensingCommunication channelJournal of Geophysical Research: Atmospheres
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Ground-based measured and calculated spectra of actinic flux density and downward UV irradiance in cloudless conditions and their sensitivity to aero…

2003

Ground-based spectral measurements of actinic flux density (300–660 nm wavelength) and downward UV irradiance (300–324 nm) under cloudless conditions have been compared with the results of one-dimensional radiative transfer calculations employing concurrent airborne vertical profile measurements of aerosol particle size distributions. Good agreement (within ±10%) between measured and calculated spectra was found. The remaining differences were explained by uncertainties inherent in the aerosol particle microphysical input data and the column ozone content. A respective sensitivity analysis of the calculated spectra, which was based on the observed variability of microphysical properties, ha…

Atmospheric ScienceMaterials scienceParticle numberIrradianceSoil ScienceAquatic ScienceOceanographyAtmospheric sciencesSpectral lineOpticsGeochemistry and PetrologyEarth and Planetary Sciences (miscellaneous)Radiative transferUV irradiancePhysics::Atmospheric and Oceanic Physicsactinic fluxEarth-Surface ProcessesWater Science and Technologyradiative transfer simulationstransmission and scattering of radiationEcologybusiness.industryPaleontologyForestryaerosols and particlesAerosolWavelengthGeophysicsSpace and Planetary ScienceParticle-size distributionParticlebusinessaerosol radiative forcingJournal of Geophysical 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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