Search results for "stoffe"

showing 10 items of 71 documents

The evolution of microphysical and optical properties of an A380 contrail in the vortex phase

2012

A contrail from a large-body A380 aircraft at cruise in the humid upper troposphere has been probed with in-situ instruments onboard the DLR research aircraft Falcon. The contrail was sampled during 700 s measurement time at contrail ages of about 1–4 min. The contrail was in the vortex regime during which the primary wake vortices were sinking 270 m below the A380 flight level while the secondary wake remained above. Contrail properties were sampled separately in the primary wake at 90 and 115 s contrail age and nearly continously in the secondary wake at contrail ages from 70 s to 220 s. The scattering phase functions of the contrail particles were measured with a polar nephelometer. The …

Atmospheric Science010504 meteorology & atmospheric sciencesWakeAtmospheric sciences01 natural sciences010305 fluids & plasmaslcsh:ChemistryTroposphere0103 physical sciencesclimate impactWake turbulence0105 earth and related environmental sciences[SDU.OCEAN]Sciences of the Universe [physics]/Ocean AtmosphereInstitut für Physik der AtmosphäreNephelometerIce crystalsAtmosphärische SpurenstoffeRadiative forcinglcsh:QC1-999FalconVortexlcsh:QD1-99913. Climate actionEnvironmental sciencePolarlcsh:Physics
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Aerosol layers from the 2008 eruptions of Mount Okmok and Mount Kasatochi: In situ upper troposphere and lower stratosphere measurements of sulfate a…

2010

In 2008 Mount Okmok and Mount Kasatochi started erupting on 12 July and 7 August, respectively, in the Aleutians, depositing emissions of trace gases and aerosols as high as 15.2 km into the atmosphere. During an aircraft campaign, conducted over Europe in between 27 October and 2 November 2008, the volcanic aerosol was measured by an Aerodyne aerosol mass spectrometer, capable of particle chemical composition measurements covering a size diameter range between 40 nm and 1 mm. In the volcanic aerosol layer enhanced submicron particulate sulfate concentrations of up to 2.0 mg m−3 standard temperature and pressure (STP) were observed between 8 and 12 km altitude, while background values …

Atmospheric Science010504 meteorology & atmospheric sciences[SDE.MCG]Environmental Sciences/Global ChangesKasatochiSoil ScienceAerosol mass spectrometry010501 environmental sciencesAquatic ScienceOceanographyAtmospheric sciences01 natural sciencesTropospherechemistry.chemical_compoundGeochemistry and Petrology[SDU.STU.VO]Sciences of the Universe [physics]/Earth Sciences/VolcanologyEarth and Planetary Sciences (miscellaneous)Volcanic aerosolSulfate aerosolSulfateStratosphere0105 earth and related environmental sciencesEarth-Surface ProcessesWater Science and Technology[PHYS.PHYS.PHYS-AO-PH]Physics [physics]/Physics [physics]/Atmospheric and Oceanic Physics [physics.ao-ph]EcologyAtmosphärische SpurenstoffePaleontologyForestryParticulatesTrace gasAerosolGeophysicschemistry13. Climate actionSpace and Planetary ScienceAirborne aerosol measurementsAerosol mass spectrometryvolcanic aerosol volcanic aerosolJournal of Geophysical Research
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Influx of African biomass burning aerosol during the Amazonian dry season through layered transatlantic transport of black carbon-rich smoke

2020

Black carbon (BC) aerosols influence the Earth's atmosphere and climate, but their microphysical properties, spatiotemporal distribution, and long-range transport are not well constrained. This study presents airborne observations of the transatlantic transport of BC-rich African biomass burning (BB) smoke into the Amazon Basin using a Single Particle Soot Photometer (SP2) as well as several complementary techniques. We base our results on observations of aerosols and trace gases off the Brazilian coast onboard the HALO (High Altitude and LOng range) research aircraft during the ACRIDICON-CHUVA campaign in September 2014. During flight AC19 over land and ocean at the northeastern coastline …

Atmospheric Science010504 meteorology & atmospheric sciences[SDE.MCG]Environmental Sciences/Global ChangesPopulation010502 geochemistry & geophysicsAtmospheric sciences01 natural sciencesAtmospherelcsh:ChemistryAltitudeConvective mixingddc:550Cloud condensation nucleiMass concentration (chemistry)educationbiomass burning aerosol transport airborne measurement Amazon basin0105 earth and related environmental sciences[SDU.OCEAN]Sciences of the Universe [physics]/Ocean Atmosphere[PHYS.PHYS.PHYS-AO-PH]Physics [physics]/Physics [physics]/Atmospheric and Oceanic Physics [physics.ao-ph]education.field_of_studyAmazon rainforestAtmosphärische Spurenstoffe15. Life on landOberpfaffenhofenBACIA HIDROGRÁFICAlcsh:QC1-999Aerosollcsh:QD1-99913. Climate actionEnvironmental sciencelcsh:Physics
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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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In-situ observations and modeling of small nitric acid-containing ice crystals

2007

Measurements in nascent ice forming regions are very rare and help understand cirrus cloud formation and the interactions of trace gases with ice crystals. A tenuous cirrus cloud has been probed with in-situ and remote sensing instruments onboard the high altitude research aircraft Geophysica M55 in the tropical upper troposphere. Besides microphysical and optical particle properties, water (H<sub>2</sub>O) and reactive nitrogen species (NO<sub>y</sub>) have been measured. In slightly ice supersaturated air between 14.2 and 14.9 km altitude, an unusually low ice water content of 0.031 mg m<sup>−3</sup> and small ice crystals with mean radii of 5…

Atmospheric Science010504 meteorology & atmospheric sciencesiceAnalytical chemistrycirrus010502 geochemistry & geophysicsAtmospheric sciences01 natural sciencesTropospherelcsh:Chemistryddc:5500105 earth and related environmental sciences[SDU.OCEAN]Sciences of the Universe [physics]/Ocean AtmosphereSupersaturationIce crystalsChemistryAtmosphärische Spurenstoffelcsh:QC1-999Trace gasAerosolJnitric acidDeposition (aerosol physics)lcsh:QD1-99913. Climate actionCirrustrace gas uptakeWater vaporlcsh:Physics
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The airborne mass spectrometer AIMS – Part 2: Measurements of trace gases with stratospheric or tropospheric origin in the UTLS

2016

Understanding the role of climate-sensitive trace gas variabilities in the upper troposphere and lower stratosphere region (UTLS) and their impact on its radiative budget requires accurate measurements. The composition of the UTLS is governed by transport and chemistry of stratospheric and tropospheric constituents, such as chlorine, nitrogen oxide and sulfur compounds. The Atmospheric chemical Ionization Mass Spectrometer AIMS has been developed to accurately measure a set of these constituents on aircraft by means of chemical ionization. Here we present a setup using SF5− reagent ions for the simultaneous measurement of trace gas concentrations of HCl, HNO3 and SO2 in the  pptv to ppmv (1…

Atmospheric Science010504 meteorology & atmospheric scienceslcsh:TA715-787ChemistryMass spectrometerlcsh:Earthwork. FoundationsAtmosphärische SpurenstoffeTACTS-ESMVal010501 environmental sciencesMass spectrometryAtmospheric sciences01 natural sciencesIon sourcelcsh:Environmental engineeringTrace gasTropospherechemistry.chemical_compoundUTLSHALONitrogen oxidelcsh:TA170-171TropopauseStratosphereWater vapor0105 earth and related environmental sciences
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State of mixing, shape factor, number size distribution, and hygroscopic growth of the Saharan anthropogenic and mineral dust aerosol at Tinfou, Moro…

2009

The Saharan Mineral Dust Experiment (SAMUM) was conducted in May and June 2006 in Tinfou, Morocco. A H-TDMA system and a H-DMA-APS system were used to obtain hygroscopic properties of mineral dust particles at 85% RH. Dynamic shape factors of 1.11, 1.19 and 1.25 were determined for the volume equivalent diameters 720, 840 and 960 nm, respectively. During a dust event, the hydrophobic number fraction of 250 and 350 nm particles increased significantly from 30 and 65% to 53 and 75%, respectively, indicating that mineral dust particles can be as small as 200 nm in diameter. Log-normal functions for mineral dust number size distributions were obtained from total particle number size distributio…

Atmospheric ScienceAmmonium sulfateMaterials science010504 meteorology & atmospheric sciencesParticle numberaerosolhygroscopicityAtmosphärische SpurenstoffeMineralogyFraction (chemistry)010501 environmental sciencesMineral dustcomplex mixtures01 natural sciencesstate of mixingAerosolSAMUMchemistry.chemical_compoundchemistryParticle-size distributionAeolian processesShape factor0105 earth and related environmental sciencesTellus B: Chemical and Physical Meteorology
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Measurement of low-ppm mixing ratios of water vapor in the upper troposphere and lower stratosphere using chemical ionization mass spectrometry

2018

A chemical ionization mass spectrometer (CIMS) instrument has been developed for the fast, precise, and accurate measurement of water vapor (H2O) at low mixing ratios in the upper troposphere and lower stratosphere (UT/LS). A low-pressure flow of sample air passes through an ionization volume containing an α-particle radiation source, resulting in a cascade of ion-molecule reactions that produce hydronium ions (H3O+) from ambient H2O. The production of H3O+ ions from ambient H2O depends on pressure and flow through the ion source, which were tightly controlled in order to maintain the measurement sensitivity independent of changes in the airborne sampling environment. The instrument w…

Atmospheric ScienceChemical ionizationlcsh:TA715-787Chemistrylcsh:Earthwork. FoundationsAnalytical chemistryAtmosphärische SpurenstoffeWater vapourAtmospheric sciencesMass spectrometryIon sourcelcsh:Environmental engineeringTroposphereIonizationlcsh:TA170-171TropopauseStratosphereWater vapormass spectrometryAtmospheric Measurement Techniques
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Nitric acid trihydrate nucleation and denitrification in the Arctic stratosphere

2014

Abstract. Nitric acid trihydrate (NAT) particles in the polar stratosphere have been shown to be responsible for vertical redistribution of reactive nitrogen (NOy). Recent observations by Cloud–Aerosol Lidar with Orthogonal Polarization (CALIOP) aboard the CALIPSO satellite have been explained in terms of heterogeneous nucleation of NAT on foreign nuclei, revealing this to be an important formation pathway for the NAT particles. In state of the art global- or regional-scale models, heterogeneous NAT nucleation is currently simulated in a very coarse manner using a constant, saturation-independent nucleation rate. Here we present first simulations for the Arctic winter 2009/2010 applying a n…

Atmospheric ScienceDenitrification010504 meteorology & atmospheric sciencesForward scatterNucleationAtmospheric sciences01 natural sciences010309 opticslcsh:Chemistry0103 physical sciencesddc:550Life ScienceStratosphere0105 earth and related environmental sciencesSpectrometerozone holeChemistryAtmosphärische Spurenstoffelcsh:QC1-999Earth sciencesLidarnitric acid trihydratelcsh:QD1-99913. Climate actionPolarParticle sizelcsh:PhysicsArctic stratosphere
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EARLINET observations of the 14-22-may long-range dust transport event during SAMUM 2006: validation of results from dust transport modelling

2009

We observed a long-range transport event of mineral dust from North Africa to South Europe during the Saharan Mineral Dust Experiment (SAMUM) 2006. Geometrical and optical properties of that dust plume were determined with Sun photometer of the Aerosol Robotic Network (AERONET) and Raman lidar near the North African source region, and with Sun photometers of AERONET and lidars of the European Aerosol Research Lidar Network (EARLINET) in the far field in Europe. Extinction-to-backscatter ratios of the dust plume over Morocco and Southern Europe do not differ. Ångstr¨om exponents increase with distance from Morocco. We simulated the transport, and geometrical and optical properties of the dus…

Atmospheric ScienceEnvironmental EngineeringAerosol Robotic Network (AERONET)010504 meteorology & atmospheric sciencesMeteorologySaharan dustAEROSOL OPTICAL-PROPERTIES010501 environmental sciencesMineral dust01 natural sciencesMineral dustSun photometerLIDARSouth EuropeSKY RADIANCE MEASUREMENTSNETWORKAerosolOptical depth0105 earth and related environmental sciencesOptical propertiesEuropean Aerosol Research Lidar Network (EARLINET)Geometrical propertiesAtmosphärische SpurenstoffeDustNorth AfricaAerosolAERONETPlumeSAMUMLidarEnvironmental scienceAeolian processesEngineering and TechnologyDust aerosolsSaharan Mineral Dust Experiment (SAMUM)Sun photometersAERONET
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