Search results for "Troposphere"

showing 6 items of 206 documents

Towards a representation of halogen chemistry within volcanic plumes in a chemistry transport model

2014

Volcanoes are a known source of halogens to the atmosphere. HBr volcanic emissions lead rapidly to the formation of BrO within volcanic plumes as shown by recent work based on observations and models. BrO, having a longer residence time in the atmosphere than HBr, is expected to have a significant impact on tropospheric chemistry, at least at the local and regional scales. The objective of this paper is to prepare a framework that will allow 3-D modelling of volcanic halogen emissions in order to determine their fate within the volcanic plume and then in the atmosphere at the regional and global scales. This work is based on a 1-D configuration of the chemistry transport model MOCAGE whose …

geographygeography.geographical_feature_categoryMeteorologyChemistryRadiusAtmospheric sciencesDilutionAerosolPlumeTroposphereAtmosphereImpact craterVolcano[SDU]Sciences of the Universe [physics]
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Modelling molecular iodine emissions in a coastal marine environment: The link to new particle formation

2006

International audience; A model of iodine chemistry in the marine boundary layer (MBL) has been used to investigate the impact of daytime coastal emissions of molecular iodine (I2). The model contains a full treatment of gas-phase iodine chemistry, combined with a description of the nucleation and growth, by condensation and coagulation, of iodine oxide nano-particles. In-situ measurements of coastal emissions of I2 made by the broadband cavity ring-down spectroscopy (BBCRDS) and inductively coupled plasma-mass spectrometry (ICP/MS) techniques are presented and compared to long path differential optical absorption spectroscopy (DOAS) observations of I2 at Mace Head, Ireland. Simultaneous me…

homogeneous nucleationspectroscopyAtmospheric ScienceAnalytical chemistryIodine oxideoiochemistrylcsh:ChemistryTropospherechemistry.chemical_compoundCloud condensation nucleiSpectroscopy[SDU.OCEAN]Sciences of the Universe [physics]/Ocean Atmospherepotential influenceChemistryDifferential optical absorption spectroscopyCondensationboundary-layerOzone depletionlcsh:QC1-999ozonelcsh:QD1-999troposphereParticleoxidespectrometer/dk/atira/pure/subjectarea/asjc/1900/1902lcsh:Physics
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Transport of Antarctic stratospheric strongly dehydrated air into the troposphere observed during the HALO-ESMVal campaign 2012

2015

Abstract. Dehydration in the Antarctic winter stratosphere is a well-known phenomenon that is annually observed by satellites and occasionally observed by balloon-borne measurements. However, in situ measurements of dehydrated air masses in the Antarctic vortex are very rare. Here, we present detailed observations with the in situ and GLORIA remote sensing instrument payload aboard the German aircraft HALO. Strongly dehydrated air masses down to 1.6 ppmv of water vapor were observed as far north as 47° S in an altitude between 12 and 13 km in the lowermost stratosphere. The dehydration can be traced back to individual ice formation events above the Antarctic Peninsula and Plateau, where ice…

polar vortexAtmospheric ScienceRossby waveAtmosphärische SpurenstoffedehydrationAtmospheric scienceslcsh:QC1-999Tropospherelcsh:ChemistryEarth scienceslcsh:QD1-999Potential vorticityMiddle latitudesClimatologyddc:550Environmental scienceAntarcticTropopauseStratosphereWater vaporAir masslcsh:PhysicsAtmospheric Chemistry and Physics
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In situ measurements of background aerosol and subvisible cirrus in the tropical tropopause region

2002

[1] In situ aerosol measurements were performed in the Indian Ocean Intertropical Convergence Zone (ITCZ) region during the Airborne Polar Experiment-Third European Stratospheric Experiment on Ozone (APE-THESEO) field campaign based in Mahe, Seychelles between 24 February and 6 March 1999. These are measurements of particle size distributions with a laser optical particle counter of the Forward Scattering Spectrometer Probe (FSSP)-300 type operated on the Russian M-55 high-altitude research aircraft Geophysica in the tropical upper troposphere and lower stratosphere up to altitudes of 21 km. On 24 and 27 February 1999, ultrathin layers of cirrus clouds were penetrated by Geophysica directly…

subvisualAtmospheric ScienceParticle numberMeteorologyaerosolsubvisible cirrusSoil SciencecirrusAquatic ScienceOceanographyAtmospheric sciencestropicsTroposphereGeochemistry and Petrologytropopauseddc:550Earth and Planetary Sciences (miscellaneous)StratosphereEarth-Surface ProcessesWater Science and TechnologyEcologybackgroundPaleontologyForestryJAerosolGeophysicsLidarSpace and Planetary ScienceEnvironmental scienceCirrusTropopauseParticle counterJournal of Geophysical Research: Atmospheres
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Lagrangian matches between observations from aircraft, lidar and radar in an orographic warm conveyor belt

2020

Warm conveyor belts (WCBs) are important airstreams in extratropical cyclones, often leading to the formation of intense precipitation and the amplification of upper-level ridges. This study presents a case study that involves aircraft, lidar and radar observations in a WCB ascending from western Europe towards the Baltic Sea during the Hydrological Cycle in the Mediterranean Experiment (HyMeX) and T-NAWDEX-Falcon in October 2012, a preparatory campaign for the THORPEX North Atlantic Waveguide and Downstream Impact Experiment (T-NAWDEX). Trajectories were used to link different observations along the WCB, that is, to establish so-called Lagrangian matches between observations. To this aim, …

warm conveyor beltLidar010504 meteorology & atmospheric sciencesAtmosphärische SpurenstoffeOrographyInflowtracer01 natural sciencesFalconTroposphereobservationsClimatologyExtratropical cycloneOutflowPrecipitationWater cycleWolkenphysikGeology0105 earth and related environmental sciencesOrographic lift
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Lagrangian matches between observations from aircraft, lidar and radar in a warm conveyor belt crossing orography

2021

Warm conveyor belts (WCBs) are important airstreams in extratropical cyclones, often leading to the formation of intense precipitation and the amplification of upper-level ridges. This study presents a case study that involves aircraft, lidar and radar observations in a WCB ascending from western Europe towards the Baltic Sea during the Hydrological Cycle in the Mediterranean Experiment (HyMeX) and T-NAWDEX-Falcon in October 2012, a preparatory campaign for the THORPEX North Atlantic Waveguide and Downstream Impact Experiment (TNAWDEX). Trajectories were used to link different observations along the WCB, that is, to establish so-called Lagrangian matches between observations. To this aim, a…

wind fieldformation mechanismorographic effectboundary layerhydrological cycleextratropical cycloneensemble forecastingairborne surveytroposphereLagrangian analysisatmospheric dynamicsairflowlidarradar
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