Search results for " Atmosphere"

showing 10 items of 292 documents

Analysis of a jet stream induced gravity wave associated with an observed ice cloud over Greenland

2004

International audience; A polar stratospheric ice cloud (PSC type II) was observed by airborne lidar above Greenland on 14 January 2000. It was the unique observation of an ice cloud over Greenland during the SOLVE/THESEO 2000 campaign. Mesoscale simulations with the hydrostatic HRM model are presented which, in contrast to global analyses, are capable to produce a vertically propagating gravity wave that induces the low temperatures at the level of the PSC afforded for the ice formation. The simulated minimum temperature is ~8 K below the driving analyses and ~4.5 K below the frost point, exactly coinciding with the location of the observed ice cloud. Despite the high elevations of the Gre…

Atmospheric Science010504 meteorology & atmospheric sciences010502 geochemistry & geophysicsAtmospheric sciences01 natural sciences010305 fluids & plasmaslaw.inventionPhysics::Geophysicslcsh:Chemistrylaw0103 physical sciencesGravity wavePhysics::Atmospheric and Oceanic Physics0105 earth and related environmental sciences[SDU.OCEAN]Sciences of the Universe [physics]/Ocean AtmosphereJet (fluid)Ice cloud[SDU.OCEAN] Sciences of the Universe [physics]/Ocean AtmosphereOrographyJet streamlcsh:QC1-999lcsh:QD1-99913. Climate actionHydrostatic equilibriumTropopauselcsh:PhysicsGeologyGeostrophic wind
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Microphysical and radiative characterization of a subvisible midlevel Arctic ice cluod by airborne observations - a case study

2009

During the Arctic Study of Tropospheric Aerosol, Clouds and Radiation (ASTAR) campaign, which was conducted in March and April 2007, an optically thin ice cloud was observed south of Svalbard at around 3 km altitude. The microphysical and radiative properties of this particular subvisible midlevel cloud were investigated with complementary remote sensing and in situ instruments. Collocated airborne lidar remote sensing and spectral solar radiation measurements were performed at a flight altitude of 2300 m below the cloud base. Under almost stationary atmospheric conditions, the same subvisible midlevel cloud was probed with various in situ sensors roughly 30 min later. <br><br> …

Atmospheric Science010504 meteorology & atmospheric sciencesASTARArktische GrenzschichtMischphasenwolken[SDU.STU.ME]Sciences of the Universe [physics]/Earth Sciences/MeteorologyAtmospheric sciences01 natural sciences010309 opticslcsh:Chemistry0103 physical sciencesRadiative transferPhysics::Atmospheric and Oceanic Physics0105 earth and related environmental sciencesRemote sensing[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]geographyIce cloudLidargeography.geographical_feature_categoryIce crystalsNephelometerCloud topArctic ice packlcsh:QC1-999Lidarlcsh:QD1-99913. Climate actionCloud albedoEnvironmental scienceAstrophysics::Earth and Planetary Astrophysicslcsh:PhysicsWolkenphysik und Verkehrsmeteorologie
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African volcanic emissions influencing atmospheric aerosols over the Amazon rain forest

2018

Long-range transport (LRT) plays an important role in the Amazon rain forest by bringing in different primary and secondary aerosol particles from distant sources. The atmospheric oxidation of dimethyl sulfide (DMS), emitted from marine plankton, is considered an important sulfate source over the Amazon rain forest, with a lesser contribution from terrestrial soil and vegetation sulfur emissions. Volcanic sulfur emissions from Africa could be a source of particulate sulfate to the Amazonian atmosphere upon transatlantic transport but no observations have been published. By using satellite observations, together with ground‑based and airborne aerosol particle observations, this paper provide…

Atmospheric Science010504 meteorology & atmospheric sciencesAmazonian[SDE.MCG]Environmental Sciences/Global Changes010502 geochemistry & geophysicsAtmospheric sciences01 natural sciencescomplex mixtureslcsh:ChemistryAtmospherechemistry.chemical_compoundparasitic diseasesCloud condensation nucleiSulfate0105 earth and related environmental sciences[PHYS.PHYS.PHYS-AO-PH]Physics [physics]/Physics [physics]/Atmospheric and Oceanic Physics [physics.ao-ph][SDU.OCEAN]Sciences of the Universe [physics]/Ocean Atmospheregeographygeography.geographical_feature_category15. Life on landParticulateslcsh:QC1-999Trace gasAerosollcsh:QD1-999Volcanochemistry13. Climate actionEnvironmental sciencegeographic locationslcsh:Physics
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Nitric Acid Trihydrate (NAT) formation at low NAT supersaturation in Polar Stratospheric Clouds (PSCs)

2005

International audience; A PSC was detected on 6 February 2003 in the Arctic stratosphere by in-situ measurements onboard the high-altitude research aircraft Geophysica. Low number densities (~10-4cm-3) of small nitric acid (HNO3) containing particles (dTNAT, these NAT particles have the potential to grow further and to remove HNO3 from the stratosphere, thereby enhancing polar ozone loss. Interestingly, the NAT particles formed in less than a day at temperatures just slightly below TNAT (T>TNAT-3.1K). This unique measurement of PSC formation at extremely low NAT saturation ratios (SNAT?10) constrains current NAT nucleation theories. We suggest, that the NAT particles have formed heterogeneo…

Atmospheric Science010504 meteorology & atmospheric sciencesAnalytical chemistryNucleation010402 general chemistryAtmospheric sciences01 natural scienceslcsh:Chemistrychemistry.chemical_compoundNitric acidStratosphere0105 earth and related environmental sciences[SDU.OCEAN]Sciences of the Universe [physics]/Ocean AtmosphereSupersaturationChemistrylcsh:QC1-9990104 chemical sciencesThe arcticozonelcsh:QD1-99913. Climate actionNatpolar stratospheric cloud (PSC)PolarSaturation (chemistry)nitric acid trihydrate (NAT)lcsh:Physics
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In situ observations of new particle formation in the tropical upper troposphere: the role of clouds and the nucleation mechanism

2011

New particle formation (NPF), which generates nucleation mode aerosol, was observed in the tropical Upper Troposphere (UT) and Tropical Tropopause Layer (TTL) by in situ airborne measurements over South America (January–March 2005), Australia (November–December 2005), West Africa (August 2006) and Central America (2004–2007). Particularly intense NPF was found at the bottom of the TTL. Measurements with a set of condensation particle counters (CPCs) with different <i>d</i><sub>p50</sub> (50% lower size detection efficiency diameter or "cut-off diameter") were conducted on board the M-55 <i>Geophysica</i> in the altitude range of 12.0–20.5 km and on board …

Atmospheric Science010504 meteorology & atmospheric sciencesDISPERSION MODEL FLEXPARTaerosolnucleationNucleationclouds010502 geochemistry & geophysicsAtmospheric sciences01 natural sciencestropicsTropospherelcsh:Chemistrynew particle formationddc:550Cloud condensation nucleiLife ScienceStratosphere0105 earth and related environmental sciencesGeophysica[PHYS.PHYS.PHYS-AO-PH]Physics [physics]/Physics [physics]/Atmospheric and Oceanic Physics [physics.ao-ph][SDU.OCEAN]Sciences of the Universe [physics]/Ocean AtmosphereIce cloudAtmosphärische SpurenstoffeFalconlcsh:QC1-999AerosolJAQUEOUS SULFURIC-ACIDlcsh:QD1-99913. Climate actionClimatologyupper troposphereEnvironmental scienceOutflowAEROSOL NUCLEATIONLOWER STRATOSPHERETropopauselcsh:PhysicsGALACTIC COSMIC-RAYS
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Design, construction and commissioning of the Braunschweig Icing Wind Tunnel

2018

Beyond its physical importance in both fundamental and climate research, atmospheric icing is considered as a severe operational condition in many engineering applications like aviation, electrical power transmission and wind-energy production. To reproduce such icing conditions in a laboratory environment, icing wind tunnels are frequently used. In this paper, a comprehensive overview on the design, construction and commissioning of the Braunschweig Icing Wind Tunnel is given. The tunnel features a test section of 0.5 m  ×  0.5 m with peak velocities of up to 40 m s−1. The static air temperature ranges from −25 to +30 °C. Supercooled droplet icing with liquid water contents up to 3 g m−3 c…

Atmospheric Science010504 meteorology & atmospheric sciencesMeteorologyMesoscale meteorology02 engineering and technology7. Clean energy01 natural sciencesArticlelaw.inventionPhysics::GeophysicsIcing conditions0203 mechanical engineeringlawddc:6Veröffentlichung der TU Braunschweigicing wind tunnelddc:62lcsh:TA170-171WolkenphysikPhysics::Atmospheric and Oceanic Physics0105 earth and related environmental sciencesIcingWind tunnel[SDU.OCEAN]Sciences of the Universe [physics]/Ocean Atmosphere020301 aerospace & aeronauticsIce crystalslcsh:TA715-787lcsh:Earthwork. FoundationsCondensed Matter::Mesoscopic Systems and Quantum Hall EffectAtmospheric icinglcsh:Environmental engineeringPhysics::Space PhysicsParticleEnvironmental scienceAstrophysics::Earth and Planetary AstrophysicsCloud chamberddc:620Publikationsfonds der TU BraunschweigMarine engineering
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Sun-Earth System Interaction studies over Vietnam: an international cooperative project

2006

International audience; During many past decades, scientists from various countries have studied separately the atmospheric motions in the lower atmosphere, in the Earth's magnetic field, in the magnetospheric currents, etc. All of these separate studies lead today to the global study of the Sun and Earth connections, and as a consequence, new scientific programs (IHY- International Heliophysical Year, CAWSES- Climate and Weather in the Sun-Earth System) are defined, in order to assume this new challenge. In the past, many scientists did not have the possibility to collect data at the same time in the various latitude and longitude sectors. Now, with the progress of geophysical sciences in …

Atmospheric Science010504 meteorology & atmospheric sciencesMeteorology[SDE.MCG]Environmental Sciences/Global ChangesContext (language use)Monsoon01 natural sciences[SDU.STU.CL] Sciences of the Universe [physics]/Earth Sciences/Climatology0103 physical sciencesEarth and Planetary Sciences (miscellaneous)lcsh:Science010303 astronomy & astrophysicsdiurnal to secular)0105 earth and related environmental sciences[SDU.OCEAN]Sciences of the Universe [physics]/Ocean Atmospherelcsh:QC801-809GeologyAstronomy and AstrophysicsEquatorial electrojetOrographylcsh:QC1-999International Heliophysical YearIonosphere (Electric fields and currents)lcsh:Geophysics. Cosmic physics[SDE.MCG] Environmental Sciences/Global Changes[ SDE.MCG ] Environmental Sciences/Global ChangesGeography13. Climate actionSpace and Planetary Science[SDU.STU.CL]Sciences of the Universe [physics]/Earth Sciences/ClimatologyGeomagnetism and paleomagnetism (Time variationsMeteorology and dynamics (Tropical meteorology)lcsh:QTropical cycloneIonosphere[ SDU.STU.CL ] Sciences of the Universe [physics]/Earth Sciences/ClimatologyLongitudelcsh:Physics
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Aviation Contrail Cirrus and Radiative Forcing Over Europe During 6 Months of COVID‐19

2021

Abstract The COVID‐19 pandemic led to a 72% reduction of air traffic over Europe in March–August 2020 compared to 2019. Modeled contrail cover declined similarly, and computed mean instantaneous radiative contrail forcing dropped regionally by up to 0.7 W m−2. Here, model predictions of cirrus optical thickness and the top‐of‐atmosphere outgoing longwave and reflected shortwave irradiances are tested by comparison to Meteosat‐SEVIRI‐derived data. The agreement between observations and modeled data is slightly better when modeled contrail cirrus contributions are included. The spatial distributions and diurnal cycles of the differences in these data between 2019 and 2020 are partially caused…

Atmospheric Science010504 meteorology & atmospheric sciencesPollution: Urban Regional and GlobalcirrusForcing (mathematics)Atmospheric Composition and Structure010502 geochemistry & geophysicsAtmospheric sciencesBiogeosciences01 natural sciencesOceanography: Biological and ChemicalCloud/Radiation InteractionRadiative transferWolkenphysikInstitut für Physik der AtmosphäreMarine PollutioncontrailOceanography: GeneralGeophysicsPollution: Urban and RegionalAtmospheric ProcessesCirrusClouds and AerosolssatelliteMegacities and Urban Environmentcontrail aircraft climate observation model traffic Meteosat CoCiPRadiation: Transmission and ScatteringAtmospherePaleoceanographyEvolution of the EarthCOVID‐19Research LetterGlobal ChangeBiosphere/Atmosphere InteractionsUrban Systems0105 earth and related environmental sciencesEvolution of the AtmosphereAerosolsradiative forcingVerkehrsmeteorologieAtmosphereLongwaveAtmosphärische SpurenstoffeRadiative forcingAerosols and ParticlesNumerical weather predictionTectonophysicsaviationGeneral Earth and Planetary SciencesEnvironmental scienceShortwaveNatural HazardsGeophysical Research Letters
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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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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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