Search results for "Mineral"

showing 10 items of 2711 documents

Properties of individual contrails: a compilation of observations and some comparisons

2017

International audience; Mean properties of individual contrails are characterized for a wide range of jet aircraft as a function of age during their life cycle from seconds to 11.5 h (7.4-18.7 km altitude, -88 to -31 °C ambient temperature), based on a compilation of about 230 previous in situ and remote sensing measurements. The airborne, satellite, and ground-based observations encompass exhaust contrails from jet aircraft from 1972 onwards, as well as a few older data for propeller aircraft. The contrails are characterized by mean ice particle sizes and concentrations, extinction, ice water content, optical depth, geometrical depth, and contrail width. Integral contrail properties includ…

Atmospheric Science010504 meteorology & atmospheric sciencesMeteorologyreviewice010502 geochemistry & geophysicsAtmospheric sciences01 natural sciencesoptical depthlcsh:Chemistryremote sensingPhase (matter)ddc:551Relative humidityOptical depth0105 earth and related environmental sciencesJet (fluid)Institut für Physik der AtmosphäreIce crystalsFernerkundung der AtmosphäreAtmosphärische Spurenstoffecontraillcsh:QC1-999Warm frontdatain-situlcsh:QD1-999Extinction (optical mineralogy)[SDU]Sciences of the Universe [physics]Environmental scienceCirrusmeasurementslcsh:PhysicsAtmospheric Chemistry and Physics
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The scavenging of two different types of marine aerosol particles calculated using a two-dimensional detailed cloud model

2011

Our 2-D dynamic model including spectral microphysics and scavenging has been evaluated for a warm precipitating convective cloud at Day 261 (18 September 1974) of the GATE campaign. Two different chemical species ((NH 4 ) 2 SO 4 and NaCl) of aerosol particles were followed in the air, inside the drops in the cloud, and inside the drops reaching the ground. Concerning the dynamics and microphysics, as well as the scavenging and wet deposition, the model results agree quite well with available observations. The cloud rained after 19 min of cloud life time. For the considered aerosol loading of the atmosphere, rough estimates are derived for the total material processed by such a warm convect…

Atmospheric Science010504 meteorology & atmospheric sciencesMicrophysicsChemistryDrop (liquid)Analytical chemistryMineralogy01 natural sciencesAerosol13. Climate actionLiquid water contentCloud baseMixing ratioRelative humidityScavenging0105 earth and related environmental sciencesTellus B
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2018

Abstract. A regional modeling study on the impact of desert dust on cloud formation is presented for a major Saharan dust outbreak over Europe from 2 to 5 April 2014. The dust event coincided with an extensive and dense cirrus cloud layer, suggesting an influence of dust on atmospheric ice nucleation. Using interactive simulation with the regional dust model COSMO-MUSCAT, we investigate cloud and precipitation representation in the model and test the sensitivity of cloud parameters to dust–cloud and dust–radiation interactions of the simulated dust plume. We evaluate model results with ground-based and spaceborne remote sensing measurements of aerosol and cloud properties, as well as the in…

Atmospheric Science010504 meteorology & atmospheric sciencesMicrophysicsMineral dust010502 geochemistry & geophysicsAtmospheric sciences01 natural sciencesPlumeAerosolDeposition (aerosol physics)13. Climate actionIce nucleusEnvironmental scienceCirrusPrecipitation0105 earth and related environmental sciencesAtmospheric Chemistry and Physics
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Ground-based off-line aerosol measurements at Praia, Cape Verde, during the Saharan Mineral Dust Experiment: microphysical properties and mineralogy

2011

A large field experiment of the Saharan Mineral Dust Experiment (SAMUM) was performed in Praia, Cape Verde, in January and February 2008. This work reports on the aerosol mass concentrations, size distributions and mineralogical composition of the aerosol arriving at Praia. Three dust periods were recorded during the measurements, divided by transitional periods and embedded in maritime-influenced situations. The total suspended particle mass/PM 10 /PM 2.5 were 250/180/74 μg/m 3 on average for the first dust period (17–21 January) and 250/230/83 μg/m 3 for the second (24–26 January). The third period (28 January to 2 February) was the most intensive with 410/340/130 μg/m 3 . Four modes were…

Atmospheric Science010504 meteorology & atmospheric sciencesMineralogy010501 environmental sciencesengineering.materialMineral dust01 natural sciencesAerosolCape verdedust ; aerosol ; clay particles ; microphysical propertiesIlliteengineeringEnvironmental sciencePlagioclaseKaoliniteHaliteQuartz0105 earth and related environmental sciencesTellus B
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Measurement report: Balloon-borne in situ profiling of Saharan dust over Cyprus with the UCASS optical particle counter

2021

This paper presents measurements of mineral dust concentration in the diameter range from 0.4 to 14.0 µm with a novel balloon-borne optical particle counter, the Universal Cloud and Aerosol Sounding System (UCASS). The balloon launches were coordinated with ground-based active and passive remote-sensing observations and airborne in situ measurements with a research aircraft during a Saharan dust outbreak over Cyprus from 20 to 23 April 2017. The aerosol optical depth at 500 nm reached values up to 0.5 during that event over Cyprus, and particle number concentrations were as high as 50 cm−3 for the diameter range between 0.8 and 13.9 µm. Comparisons of the total particle number concentration…

Atmospheric Science010504 meteorology & atmospheric sciencesParticle numberPhysicsQC1-9990208 environmental biotechnology02 engineering and technologyMineral dustMolar absorptivityAtmospheric sciences01 natural sciences020801 environmental engineeringAerosolSun photometerChemistryLidar13. Climate actionParticle-size distributionEnvironmental scienceParticle counterQD1-9990105 earth and related environmental sciencesAtmospheric Chemistry and Physics
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Assessments for the impact of mineral dust on the meningitis incidence in West Africa.

2013

9 pages; International audience; Recently, mineral dust has been suspected to be one of the important environmental risk factor for meningitis epidemics in West Africa. The current study is one of the first which relies on long-term robust aerosol measurements in the Sahel region to investigate the possible impact of mineral dust on meningitis cases (incidence). Sunphotometer measurements, which allow to derive aerosol and humidity parameters, i.e., aerosol optical thickness, Angström coefficient, and precipitable water, are combined with quantitative epidemiological data in Niger and Mali over the 2004-2009 AMMA (African Monsoon Multidisciplinary Analysis) program period. We analyse how th…

Atmospheric Science010504 meteorology & atmospheric sciences[SDE.MCG]Environmental Sciences/Global ChangesDry seasonContext (language use)010501 environmental sciencesMineral dustMonsoon01 natural sciencescomplex mixtures[SDV.MHEP.MI]Life Sciences [q-bio]/Human health and pathology/Infectious diseasesDry seasonWest AfricamedicineMeningitis0105 earth and related environmental sciencesGeneral Environmental Science2. Zero hungerPrecipitable waterHumidityDustmedicine.diseaseAerosol[ SDE.MCG ] Environmental Sciences/Global Changes[ SDV.MHEP.MI ] Life Sciences [q-bio]/Human health and pathology/Infectious diseases13. Climate action[SDU.STU.CL]Sciences of the Universe [physics]/Earth Sciences/ClimatologyClimatologyEnvironmental science[ SDU.STU.CL ] Sciences of the Universe [physics]/Earth Sciences/ClimatologyMeningitis
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Electrical conductivity of magma in the course of crystallization controlled by their residual liquid composition.

2005

International audience; The electrical conductivity of a magma in the course of crystallization was experimentally investigated in the temperature range of 1350–1018°C. Large samples of basaltic composition with a homogeneous crystal content were synthesized in a gas mixing furnace at 1 atm pressure. The samples were analyzed by electron microprobe. The relative proportions of the phases as a function of temperature were determined. Depending on temperature, the phase assemblies included quenched silicate liquid, ±plagioclase, ±pyroxene, ±Fe-Ti oxides. The crystal content varied from 0 to 80 wt %. In response to partial crystallization, the residual liquid changed composition from basalt, t…

Atmospheric Science010504 meteorology & atmospheric sciences[SDE.MCG]Environmental Sciences/Global ChangesMagmaSoil ScienceMineralogyThermodynamicsSilicate meltLiquidusAquatic ScienceConductivity010502 geochemistry & geophysicsOceanography01 natural sciencesSilicate melt.law.inventionchemistry.chemical_compoundGeochemistry and PetrologyElectrical resistivity and conductivityLiquid crystallawEarth and Planetary Sciences (miscellaneous)Electrical conductivity[SDU.STU.VO]Sciences of the Universe [physics]/Earth Sciences/VolcanologyElectrical measurementsCrystallization0105 earth and related environmental sciencesEarth-Surface ProcessesWater Science and TechnologyFractional crystallization (geology)EcologyPaleontologyForestrySilicateGeophysicschemistry13. Climate actionSpace and Planetary ScienceGeology
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Anisotropic scaling of tectonic stylolites: A fossilized signature of the stress field?

2010

International audience; [1] Vertical stylolites are pressure solution features, which are considered to be caused by horizontal tectonic loading, with the largest principal compressive stress being (sub-) parallel to the Earth's surface. In the present study we analyze the roughness of such tectonic stylolites from two tectonic settings in southern Germany and northeastern Spain, aiming to investigate their scaling properties with respect to the stress during formation. High-resolution laser profilometry was carried out on opened stylolite surfaces of nine samples. These data sets were then analyzed using one-and two-dimensional Fourier power spectral approaches. We found that tectonic styl…

Atmospheric Science010504 meteorology & atmospheric sciences[SDU.STU]Sciences of the Universe [physics]/Earth SciencesSoil ScienceMineralogyGeometryAquatic Science010502 geochemistry & geophysicsOceanography01 natural sciencesPhysics::GeophysicsStress (mechanics)Geochemistry and PetrologyEarth and Planetary Sciences (miscellaneous)AnisotropyScaling0105 earth and related environmental sciencesEarth-Surface ProcessesWater Science and Technology[PHYS]Physics [physics]EcologyCauchy stress tensorPaleontologyForestryStress fieldTectonicsGeophysics13. Climate actionSpace and Planetary ScienceStylolitePressure solutionGeologyJournal of Geophysical Research
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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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2012

Abstract. One of the major uncertainties in the understanding of Earth's climate system is the interaction between solar radiation and aerosols in the atmosphere. Aerosols exposed to high humidity will change their chemical, physical, and optical properties due to their increased water content. To model hydrated aerosols, atmospheric chemistry and climate models often use the volume weighted mixing rule to predict the complex refractive index (RI) of aerosols when they interact with high relative humidity, and, in general, assume homogeneous mixing. This study explores the validity of these assumptions. A humidified cavity ring down aerosol spectrometer (CRD-AS) and a tandem hygroscopic DMA…

Atmospheric Science010504 meteorology & atmospheric sciencesbusiness.industryChemistryScatteringMie scatteringAnalytical chemistry010501 environmental sciencesMolar absorptivity01 natural sciencesAerosolOptics13. Climate actionExtinction (optical mineralogy)Differential mobility analyzerRelative humiditybusinessMixing (physics)0105 earth and related environmental sciencesAtmospheric Chemistry and Physics
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