Search results for "Troposphere"

showing 10 items of 206 documents

Growth of nucleation mode particles in the summertime Arctic: a case study

2016

Abstract. The summertime Arctic lower troposphere is a relatively pristine background aerosol environment dominated by nucleation and Aitken mode particles. Understanding the mechanisms that control the formation and growth of aerosol is crucial for our ability to predict cloud properties and therefore radiative balance and climate. We present an analysis of an aerosol growth event observed in the Canadian Arctic Archipelago during summer as part of the NETCARE project. Under stable and clean atmospheric conditions, with low inversion heights, carbon monoxide less than 80 ppbv, and black carbon less than 5 ng m−3, we observe growth of small particles,  <  20 nm in diameter, into sizes ab…

Earth's energy budgetAtmospheric Science010504 meteorology & atmospheric sciencesNucleation010501 environmental sciencesAtmospheric sciences01 natural sciencesMethanesulfonic acidcomplex mixturesTropospherelcsh:Chemistrychemistry.chemical_compoundCloud condensation nuclei14. Life underwater0105 earth and related environmental sciences[PHYS.PHYS.PHYS-AO-PH]Physics [physics]/Physics [physics]/Atmospheric and Oceanic Physics [physics.ao-ph]respiratory systemlcsh:QC1-999AerosolchemistryArcticlcsh:QD1-99913. Climate action[SDU.STU.CL]Sciences of the Universe [physics]/Earth Sciences/Climatologylcsh:PhysicsCarbon monoxide
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Aircraft-based operation of an aerosol mass spectrometer: Measurements of tropospheric aerosol composition

2006

The Aerodyne quadrupole aerosol mass spectrometer was deployed on the Falcon twin jet research aircraft operated by Deutsches Zentrum für Luft- und Raumfahrt (DLR). This was the first deployment of an AMS in a jet aircraft. Aerosol mass concentration measurements in the troposphere up to altitudes of about 11 km were performed within two measurement flights on 12 and 14 May 2003 over southern Germany. Background aerosol data were gained up to 6 km, while aircraft exhaust aerosol was be sampled at higher altitudes on 14 May, indicating the presence of sulfuric acid and unburned hydrocarbons in the exhaust particles. The boundary layer aerosol on 12 May was found to be composed of 49% organic…

Fluid Flow and Transfer ProcessesAtmospheric ScienceAmmonium sulfateEnvironmental EngineeringAerosol chemical compositionMechanical EngineeringAnalytical chemistryAtmosphärische SpurenstoffeAerosol mass spectrometryPollutionAerosolTropospherechemistry.chemical_compoundBoundary layerchemistryNitrateMass concentration (chemistry)Aerosol mass spectrometryDynamik der AtmosphäreSulfateAircraft measurements
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Dehydration potential of ultrathin clouds at the tropical tropopause

2003

[1] We report on the first simultaneous in situ and remote measurements of subvisible cirrus in the uppermost tropical troposphere. The observed cirrus, called UTTCs ( ultrathin tropical tropopause clouds), are the geometrically (200-300 m) and optically (t approximate to 10(-4)) thinnest large-scale clouds ever sampled (approximate to10(5) km(2)). UTTCs consist of only a few ice particles per liter with mean radius approximate to5 mum, containing only 1-5 % of the total water. Yet, brief adiabatic cooling events only 1-2 K below mean ambient temperature destabilize UTTCs, leading to large sedimenting particles (r approximate to 25 mm). Due to their extreme altitude above 17 km and low part…

Ice cloudMaterials scienceIce crystalsparticle micro-physicsdehydrationtropical tropopauseRadiusAtmospheric sciencesJTroposphereGeophysicsAltitudeddc:550General Earth and Planetary SciencesCirrussubvisible cirrus cloudsTropopauseStratosphere
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HNO3 partitioning in cirrus clouds

1999

During the 1997 POLSTAR-1 winter campaign in northern Sweden a flight was performed across a cold trough of air (similar or equal to 196 K) in the tropopause region. Measurements of total water vapour, nitric acid, particles and reactive nitrogen (NOy) were taken. The particle measurements indicate that about 3% of the particles in the moist tropospheric air were ice particles. Forward and backward facing NOy inlets were used simultaneously to determine condensed phase HNO3. The combined NOy and particle measurements reveal that less than 1% of a monolayer of NOy could have resided on the ice particles. This casts doubt on the hypothesis that sedimenting cirrus particles generally lead to a…

Ice cloudReactive nitrogenAtmospheric sciencesJTropospherechemistry.chemical_compoundGeophysicschemistryNitric acidddc:550General Earth and Planetary SciencesEnvironmental scienceCirrusNitrogen oxideTropopauseWater vapor
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Upper tropospheric water vapour and its interaction with cirrus clouds as seen from IAGOS long-term routine in-situ observations

2017

IAGOS (In-service Aircraft for a Global Observing System) performs long-term routinein situobservations of atmospheric chemical composition (O3, CO, NOx, NOy, CO2, CH4), water vapour, aerosols, clouds, and temperature on a global scale by operating compact instruments on board of passenger aircraft. The unique characteristics of the IAGOS data set originate from the global scale sampling on air traffic routes with similar instrumentation such that the observations are truly comparable and well suited for atmospheric research on a statistical basis. Here, we present the analysis of 15 months of simultaneous observations of relative humidity with respect to ice (RHice) and ice crystal number …

In situ010504 meteorology & atmospheric sciencesIce crystalsSampling (statistics)010501 environmental sciencesAtmospheric sciences01 natural sciencesGeneralLiterature_MISCELLANEOUSTroposphereddc:550Environmental scienceRelative humidityCirrusPhysical and Theoretical ChemistryTropopauseWater vapor0105 earth and related environmental sciences
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Vertical profiling of Saharan dust with Raman lidars and airborne HSRL in southern Morocco during SAMUM

2009

Three groundâÂ�Â�based Raman lidars and an airborne highâÂ�Â�spectralâÂ�Â�resolution lidar (HSRL) were operated during SAMUM 2006 in southern Morocco to measure height profiles of the volume extinction coefficient, the extinctionâÂ�Â�toâÂ�Â�backscatter ratio, and the depolarization ratio of dust particles in the Saharan dust layer at several wavelengths. Aerosol Robotic Network (AERONET) Sun photometer observations and radiosounding of meteorological parameters complemented the groundâÂ�Â�based activities at the SAMUM station of Ouarzazate. Four case studies are presented. Two case studies deal with the comparison of observations of the three groundâÂ�Â�based lidars during a heavy du…

LidarAtmospheric ScienceSaharan dust010504 meteorology & atmospheric sciencesaerosol detectiondepolrization ratioPhotometer010501 environmental sciencesMineral dust01 natural scienceslidar ratiolaw.inventionAerosolAERONETTroposphereSun photometerLidarlawRaman lidarDepolarization ratioEnvironmental scienceHSRL0105 earth and related environmental sciencesRemote sensingTellus B
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Stratosphere–troposphere exchange (STE) in the vicinity of North Atlantic cyclones

2015

Atmospheric Chemistry and Physics, 15 (19)

Maximum intensityAtmospheric ScienceGeopotential heightStormAtmospheric scienceslcsh:QC1-999lcsh:ChemistryTropospherelcsh:QD1-999ClimatologyExtratropical cycloneCycloneTropopauseStratospherelcsh:PhysicsGeologyAtmospheric Chemistry and Physics
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Mount Etna volcano (Italy) as a major “dust” point source in the Mediterranean area

2016

Volcanic emissions represent one of the most relevant natural sources of trace elements to the troposphere. Due to their potential toxicity, they may have important environmental impacts from local to global scale. They can also severely affect the atmospheric and terrestrial environment at timescales ranging from a few to millions of years. Mt. Etna volcano is known as one of the largest global contributors of magmatic gases (CO2, SO2 and halogens) and particulate matter, including some toxic trace elements. The aim of this study is to characterize the chemical composition and the mineralogical features of the volcanogenic aerosol passively emitted from Mt. Etna. Twenty-five samples were c…

Mediterranean climate010504 meteorology & atmospheric sciencesEarth scienceGeochemistry010502 geochemistry & geophysics01 natural sciencesTroposphereAtmosphereEnvironmental impactchemistry.chemical_compoundChemical compositionAerosol0105 earth and related environmental sciencesGeneral Environmental SciencegeographyVolcanic emissiongeography.geographical_feature_category2300ParticulatesSilicateAerosolSettore GEO/08 - Geochimica E VulcanologiaVolcanochemistryTrace elementGeneral Earth and Planetary SciencesEarth and Planetary Sciences (all)Geology
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CONCENTRATION MEASUREMENTS OF 7Be AT GROUND LEVEL AIR AT PALERMO, ITALY- COMPARISON WITH SOLAR ACTIVITY OVER A PERIOD OF 21 YEARS

2003

Air activity concentrations of (7)Be in Palermo determined for the period January 1995-December 2002 by gamma-ray spectrometric analysis of particulate samples collected on paper filter by a high-volume sampler (approximately 900 m(3) h(-1)) are reported. The temporal behaviour of (7)Be concentration presents the same characteristics already observed in the measurements carried out over the previous 13-year (1982-1994) investigated period. The mean value of 5.06 mBq m(-3) obtained from the analysis of the 4636 particulate samples collected from 1982 to 2002 can be considered a representative value of (7)Be air concentration at ground level in our geographical zone. The comparison of long-te…

MeteorologyPeriod (periodic table)Health Toxicology and MutagenesisSolar activityAir pollutionAtmospheric sciencesmedicine.disease_causePalermoTroposphere7BemedicinePaper filterEnvironmental ChemistryInverse correlationWaste Management and DisposalRadioisotopesActivity concentrationMean valueGeneral MedicineParticulatesHistory 20th CenturyPollutionTemporal variationGround levelSpectrometry GammaItalyEnvironmental scienceBerylliumCosmic RadiationEnvironmental Monitoring
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In situ detection of stratosphere-troposphere exchange of cirrus particles in the midlatitudes

2015

Airborne trace gas, microphysical, and radiation measurements were performed during the AIRcraft TOwed Sensor Shuttle - Inhomogeneous Cirrus Experiment over northern Germany in 2013. Based on high-precision nitrous oxide (N2O) and carbon monoxide (CO) in situ data, stratospheric air could be identified, which contained cirrus cloud particles. Consistent with the stratospheric N2O data, backward trajectories indicate that the sampled air masses crossed the dynamical tropopause in the last 3 h before the measurement. These air masses contained cirrus particles, which were formed during slow ascent in the troposphere and subsequently mixed with stratospheric air. From the CO-N2O correlation th…

MeteorologyRadiationAtmospheric sciencesTrace gasTropospherechemistry.chemical_compoundGeophysicschemistryMiddle latitudesddc:550General Earth and Planetary SciencesEnvironmental scienceCirrusTropopauseStratosphereCarbon monoxideGeophysical Research Letters
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