Search results for "soil"

showing 10 items of 3493 documents

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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Mixing relationships and the effects of secondary alteration in the Wishstone and Watchtower Classes of Husband Hill, Gusev Crater, Mars

2006

[1] The Wishstone and Watchtower Class rocks on Husband Hill preserve evidence for a geochemical relationship consistent with two-component mixing between a high Al 2 O 3 , TiO 2 , CaO, Na 2 O, P 2 O 5 end-member and a second end-member enriched in the elements MgO, Zn, S, Br, and Cl. The first end-member appears to be reasonably well represented by rocks of the Wishstone Class, while the second end-member is consistent with a chemical component, not represented by any lithology encountered by Spirit. The Watchtower Class appears to be an intermediate in the mixture. The concentration of the redox sensitive elements Fe and Mn display no systematic variation between rock classes, and the Fe-…

Atmospheric ScienceLithologyAnalytical chemistrySoil ScienceMineralogyWeatheringAquatic ScienceOceanographychemistry.chemical_compoundImpact craterGeochemistry and PetrologyEarth and Planetary Sciences (miscellaneous)SulfateDissolutionEarth-Surface ProcessesWater Science and TechnologyEcologyPaleontologyForestryPhosphateGeophysicschemistrySpace and Planetary ScienceSoil waterSedimentary rockGeologyJournal of Geophysical Research: Planets
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On the angular variation of thermal infrared emissivity of inorganic soils

2012

[1] Land surface temperature (LST), a key parameter for many environmental studies, can be most readily estimated by using thermal infrared (TIR) sensors onboard satellites. Accurate LST are contingent upon simultaneously accurate estimates of land surface emissivity (e), which depend on sensor viewing angle and the anisotropy of optical and structural properties of surfaces. In the case of inorganic bare soils (IBS), there are still few data that quantify emissivity angular effects. The present work deals with the angular variation of TIR emissivity for twelve IBS types, representative of nine of the twelve soil textures found on Earth according to United States Department of Agriculture c…

Atmospheric ScienceMaterials scienceEcologyIsotropyPaleontologySoil ScienceMineralogyForestryAquatic ScienceOceanographyViewing angleGeophysicsSpace and Planetary ScienceGeochemistry and PetrologyInfrared windowEarth and Planetary Sciences (miscellaneous)EmissivityNadirOutgoing longwave radiationAnisotropyWater vaporEarth-Surface ProcessesWater Science and TechnologyRemote sensingJournal of Geophysical Research: Atmospheres
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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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Effects of ice crystal habit on thermal infrared radiative properties and forcing of cirrus

2007

[1] The impact of assumed ice crystal morphology on thermal infrared (IR) radiative properties of subtropical cirrus is quantified. In particular, the crystal-shape-dependent profiles of downwelling and upwelling thermal IR (broadband and spectral) irradiances and the radiative forcing of cirrus (at the top and bottom of the atmosphere) are investigated. For this purpose, airborne measurements of ice crystal size distribution (in terms of ice crystal maximum dimension) from the CRYSTAL-FACE campaign and a recently published library of thermal IR optical properties of nonspherical ice crystal habits are implemented into radiative transfer simulations. Two cirrus cases are studied in detail: …

Atmospheric ScienceMaterials scienceInfraredPhysics::OpticsSoil ScienceAstrophysics::Cosmology and Extragalactic AstrophysicsAquatic ScienceOceanographyOpticsGeochemistry and PetrologyEarth and Planetary Sciences (miscellaneous)Radiative transferAbsorption (electromagnetic radiation)Astrophysics::Galaxy AstrophysicsPhysics::Atmospheric and Oceanic PhysicsEarth-Surface ProcessesWater Science and TechnologyIce cloudEcologyIce crystalsbusiness.industryPaleontologyForestryRadiative forcingComputational physicsGeophysicsSpace and Planetary ScienceInfrared windowCirrusAstrophysics::Earth and Planetary AstrophysicsbusinessJournal of Geophysical Research
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Depth selective Mössbauer spectroscopy: Analysis and simulation of 6.4 keV and 14.4 keV spectra obtained from rocks at Gusev Crater, Mars, and layere…

2008

[1] The miniaturized Mossbauer spectrometer (MIMOS) II Mossbauer spectrometers on the Mars Exploration Rovers (MER) simultaneously obtained 6.4 keV and 14.4 keV Mossbauer spectra from rock and soil targets. Because photons with lower energy have a shallower penetration depth, 6.4 keV spectra contain more mineralogical information about the near-surface region of a sample than do 14.4 keV spectra. The influence of surface layers of varying composition and thickness on Mossbauer spectra was investigated by Monte Carlo simulation and by measurement using a copy of the MER MIMOS II instrument and samples with one or two layers of known thicknesses. Thin sections of minerals or metallic Fe foil …

Atmospheric ScienceMaterials scienceMonte Carlo methodSoil ScienceMineralogyAquatic Scienceengineering.materialOceanographyPhysics::GeophysicsGeochemistry and PetrologyMössbauer spectroscopyEarth and Planetary Sciences (miscellaneous)Surface layerPenetration depthEarth-Surface ProcessesWater Science and TechnologyThin layersOlivineEcologySpectrometerPaleontologyForestryMars Exploration ProgramGeophysicsSpace and Planetary ScienceengineeringJournal of Geophysical Research
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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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Pore-space characterization of an altered tonalite by X-ray computed microtomography and the14C-labeled-polymethylmethacrylate method

2012

[1] The structure of geological materials strongly affects migration processes that take place in them and are also important in their weathering and alteration processes. Further information of that structure will also be important for many applications that involve geological materials. The emphasis of this study was thus to characterize the pore structure and porosity of altered tonalite by combining different measuring techniques: X-ray tomography, the14C-polymethylmethacrylate method, electron microscopy, and argon pycnometry. Intragranular porosities were determined using chemical staining of rock surfaces. Three-dimensional distributions of minerals and porosities were evaluated with…

Atmospheric ScienceMaterials scienceScanning electron microscope0207 environmental engineeringSoil ScienceMineralogy02 engineering and technologyAquatic Science010502 geochemistry & geophysicsOceanography01 natural sciencesTexture (geology)Geochemistry and PetrologyEarth and Planetary Sciences (miscellaneous)Diffusion (business)020701 environmental engineeringPorosity0105 earth and related environmental sciencesEarth-Surface ProcessesWater Science and TechnologyEcologyPaleontologyForestryMicrostructureCharacterization (materials science)GeophysicsSpace and Planetary ScienceGas pycnometerPorous mediumJournal of Geophysical Research: Solid Earth
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Influence of ice crystal shape on retrieval of cirrus optical thickness and effective radius: A case study

2009

Airborne measurements of spectral upwelling radiances (350A¢Â�Â�2200 nm) reflected by cirrus using the Spectral Modular Airborne Radiation measurement sysTem (SMART)-Albedometer were made over land and water surfaces. Based on these data, cloud optical thickness tau and effective radius Reff of the observed cirrus were retrieved. By using different crystal shape assumptions (hexagonal plates, solid and hollow columns, rough aggregates, planar and spatial rosettes, ice spheres, and a mixture of particle habits) in the retrieval, the influence of crystal shape on the retrieved tau and Reff was evaluated. With relative differences of up to 70%, the influence of particle habit on t is larger th…

Atmospheric ScienceMaterials scienceiceSoil SciencecirrusAquatic ScienceOceanographycrystalCrystalOpticsGeochemistry and PetrologyEarth and Planetary Sciences (miscellaneous)Physics::Atmospheric and Oceanic PhysicsEarth-Surface ProcessesWater Science and TechnologyEffective radiusLidarIce cloudEcologyIce crystalsFernerkundung der Atmosphärebusiness.industryAtmosphärische SpurenstoffePaleontologyForestryFalconGeophysicsLidarSpace and Planetary ScienceRadianceCIRCLE-2SPHERESCirrusbusinessJournal of Geophysical Research
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Approaches to partitioning the global UVER irradiance into its direct and diffuse components in Valencia, Spain

2012

[1] The paper explores methods of partitioning the hourly average UV erythemal flux into its direct and diffuse components for Valencia, Spain. It is shown that the cloud modification factor, the ratio of measured to cloudless erythemal flux relates linearly to the fraction of the measured irradiance that is diffuse. This relationship was developed further into two simple models- a linear and nonlinear one. The models are characterized by an effective cloud cover to partition the global erythemal flux. The diffuse fraction increases linearly with cloud cover in the linear model, but exponentially in the nonlinear one. The models may be used to partition the direct and diffuse irradiance wit…

Atmospheric ScienceMeteorologyCloud coverIrradianceSoil ScienceAquatic ScienceOceanographyAtmospheric sciencesGeochemistry and PetrologyEarth and Planetary Sciences (miscellaneous)Partition (number theory)ValenciaEarth-Surface ProcessesWater Science and TechnologyEcologybiologyLinear modelPaleontologyForestryModification factorbiology.organism_classificationNonlinear systemGeophysicsSpace and Planetary ScienceNonlinear modelEnvironmental scienceJournal of Geophysical Research: Atmospheres
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