Search results for "Mineral"

showing 10 items of 2711 documents

Orographic Effects and Evaporative Cooling along a Subtropical Cold Front: The Case of the Spectacular Saharan Dust Outbreak of March 2004

2012

Abstract On 2 March 2004 a marked upper-level trough and an associated surface cold front penetrated into the Sahara. High winds along and behind this frontal system led to an extraordinary, large-scale, and long-lived dust outbreak, accompanied by significant precipitation over parts of Algeria, Tunisia, and Libya. This paper uses sensitivity simulations with the limited-area model developed by the Consortium for Small-Scale Modeling (COSMO) together with analysis data and surface observations to test several hypotheses on the dynamics of this case proposed in previous work. It is demonstrated that air over central Algeria is cooled by evaporation of frontal precipitation, substantially en…

Atmospheric ScienceLeading edgeCold frontMountain chainClimatologyEnvironmental scienceSubtropicsMineral dustAtmospheric sciencesTrough (meteorology)Evaporative coolerOrographic liftMonthly Weather Review
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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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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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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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Hygroscopic properties and extinction of aerosol particles at ambient relative humidity in South-Eastern China

2008

Abstract During the “Program of Regional Integrated Experiments of Air Quality over Pearl River Delta 2004 (PRIDE-PRD2004)” hygroscopic properties of particles in the diameter range 22 nm to 10 μ m were determined. For that purpose, a Humidifying Differential Mobility Particle Sizer (H-DMPS) and a Micro-Orifice Uniform Deposition Impactor (MOUDI) were operated. The derived size-dependent particle hygroscopic growth factors were interpolated to ambient relative humidity (RH) and used to calculate the particle number size distributions (PNSDs) at ambient conditions. A comparison between the modeled particle extinction coefficients ( σ ext , Mie ) and those observed with a Raman lidar was made…

Atmospheric ScienceMaterials scienceDeposition (aerosol physics)Particle numberExtinction (optical mineralogy)Ultrafine particleParticle-size distributionAnalytical chemistryMineralogyParticleRelative humidityGeneral Environmental ScienceAerosolAtmospheric Environment
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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 laboratory study on the uptake of HCl, HNO3, and SO2 gas by ice crystals and the effect of these gases on the evaporation rate of the crystals

1998

The results of our new and earlier laboratory studies on the uptake of gases by ice crystals are summarized in terms of (1) the equilibrium phase diagram for a system gas/H2O, (2) the effect of these gases on the evaporation rate of ice crystals, and (3) in terms of the uptake of the gases by water drops. It is shown that the intrinsic quasi-liquid layer significantly affects the uptake of a gas by an ice surface in that, depending on the gas phase concentration, the layer thickness may be considerably increased by depressing the equilibrium freezing point causing additional surface melting. It is further shown that the evaporation rate of ice particles previously exposed to a gas may becom…

Atmospheric ScienceMaterials scienceIce crystalsEvaporationAnalytical chemistryMineralogyFreezing pointchemistry.chemical_compoundAdsorptionchemistryAstrophysics::Earth and Planetary AstrophysicsClear iceScavengingPhysics::Atmospheric and Oceanic PhysicsSulfur dioxidePhase diagramAtmospheric Research
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Chemical composition and complex refractive index of Saharan Mineral Dust at Izaña, Tenerife (Spain) derived by electron microscopy

2007

Abstract Samples from two strong homogeneous dust plumes from the Saharan desert reaching Izana (Tenerife, Spain) in July and August 2005 were taken with a miniature impactor system and filter samplers. Size, aspect ratio and chemical composition of more than 22,000 individual particles were studied by scanning electron microscopy. The mineralogical phase composition of about 200 particles was investigated by transmission electron microscopy. In addition, the aerosol size distribution was measured with an optical particle spectrometer. In all samples, the aerosol was dominated by mineral dust with an average composition (by volume) of 64% silicates, 6% quartz, 5% calcium-rich particles, 14%…

Atmospheric ScienceMaterials scienceMineralogyHematiteMineral dustmedicine.disease_causecomplex mixturesSootAerosolvisual_artParticle-size distributionmedicinevisual_art.visual_art_mediumParticle sizeQuartzChemical compositionGeneral Environmental ScienceAtmospheric Environment
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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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The ice nucleating ability of pollen:

2002

Abstract Laboratory tests were conducted of the ice nucleating ability of four kinds of pollen in the immersion and the contact freezing modes. The diameters of the selected pollen were between 25 and 70 μm. The experiments were carried out at the Mainz vertical wind tunnel with freely suspended supercooled droplets at temperatures down to −28 °C. The immersion freezing experiments were conducted with drops of radii between 250 and 375 μm formed from distilled water with a defined amount of pollen added. The drops were freely floated in the wind tunnel while being supercooled. For the contact freezing experiments, a short burst of pollen was allowed to collide with freely suspended, superco…

Atmospheric ScienceMaterials scienceNucleationAnalytical chemistryMineralogymedicine.disease_causeAerosolDistilled waterPollenCongelationIce nucleusmedicineSupercoolingWind tunnelAtmospheric Research
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