Search results for "QC"

showing 10 items of 3477 documents

Comparing airborne and satellite retrievals of cloud optical thickness and particle effective radius using a spectral radiance ratio technique: two c…

2018

Solar radiation reflected by cirrus and deep convective clouds (DCCs) was measured by the Spectral Modular Airborne Radiation Measurement System (SMART) installed on the German High Altitude and Long Range Research Aircraft (HALO) during the Mid-Latitude Cirrus (ML-CIRRUS) and the Aerosol, Cloud, Precipitation, and Radiation Interaction and Dynamic of Convective Clouds System – Cloud Processes of the Main Precipitation Systems in Brazil: A Contribution to Cloud Resolving Modelling and to the Global Precipitation Measurement (ACRIDICON-CHUVA) campaigns. On particular flights, HALO performed measurements closely collocated with overpasses of the Moderate Resolution Imaging Spectroradiometer (…

Atmospheric Science010504 meteorology & atmospheric sciences0211 other engineering and technologiescirrus02 engineering and technology01 natural sciencesPhysics::Geophysicslcsh:ChemistryNadirRadiative transferconvective cloudsWolkenphysiksatellite retrievalsAstrophysics::Galaxy AstrophysicsPhysics::Atmospheric and Oceanic Physics021101 geological & geomatics engineering0105 earth and related environmental sciencesRemote sensingEffective radiusAlbedolcsh:QC1-999lcsh:QD1-999RadianceEnvironmental scienceCirrusModerate-resolution imaging spectroradiometerspectral radiancecloud optical thicknessGlobal Precipitation Measurementlcsh:PhysicsAtmospheric Chemistry and Physics
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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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Real-time detection of highly oxidized organosulfates and BSOA marker compounds during the F–BEACh 2014 field study

2017

Abstract. The chemical composition of organic aerosols was analyzed using complementary mass spectrometric techniques during a field study in Central Europe in July 2014 (Fichtelgebirge – Biogenic Emission and Aerosol Chemistry, F–BEACh 2014). Aerosols were analyzed in real-time by Aerosol Flowing Atmospheric-Pressure Afterglow Mass Spectrometry (AeroFAPA–MS), Aerosol Mass Spectrometry (AMS), and Chemical Ionization Atmospheric-Pressure interface Time-of-Flight Mass Spectrometry (CI–APiToF–MS). In addition, offline detection of acidic organic compounds was conducted by non-target screening of filter samples using High Resolution Mass Spectrometry (HRMS) in combination with Ultra-High Pressu…

Atmospheric Science010504 meteorology & atmospheric sciencesAnalytical chemistrychemistry.chemical_element010501 environmental sciencesMass spectrometry010402 general chemistry01 natural scienceslcsh:Chemistrychemistry.chemical_compoundRelative humiditySulfateChemical composition0105 earth and related environmental sciences010401 analytical chemistry[CHIM.CATA]Chemical Sciences/CatalysisParticulatesSulfur[SDE.ES]Environmental Sciences/Environmental and Societylcsh:QC1-999Aerosol0104 chemical scienceslcsh:QD1-999chemistry13. Climate actionEnvironmental chemistryHYSPLITlcsh:Physics
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A convolution of observational and model data to estimate age of air spectra in the northern hemispheric lower stratosphere

2020

Abstract. Derivation of mean age of air (AoA) and age spectra from atmospheric measurements remains a challenge and often requires data from atmospheric models. This study tries to minimize the direct influence of model data and presents an extension and application of a previously established inversion method to derive age spectra from mixing ratios of long- and short-lived trace gases. For a precise description of cross-tropopause transport processes, the inverse method is extended to incorporate air entrainment into the stratosphere across the tropical and extratropical tropopause. We first use simulations with the Chemical Lagrangian Model of the Stratosphere (CLaMS) to provide a genera…

Atmospheric Science010504 meteorology & atmospheric sciencesAtmospheric modelsMonte Carlo methodInverse transform samplingEntrainment (meteorology)010502 geochemistry & geophysicsAtmospheric sciences01 natural scienceslcsh:QC1-999Trace gaslcsh:ChemistryTroposphereEarth scienceslcsh:QD1-999ddc:550Environmental scienceTropopauseStratospherelcsh:Physics0105 earth and related environmental sciences
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Evidence of small-scale quasi-isentropic mixing in ridges of extratropical baroclinic waves

2019

Abstract. Stratosphere–troposphere exchange within extratropical cyclones provides the potential for anthropogenic and natural surface emissions to rapidly reach the stratosphere as well as for ozone from the stratosphere to penetrate deep into the troposphere, even down into the boundary layer. The efficiency of this process directly influences the surface climate, the chemistry in the stratosphere, the chemical composition of the extratropical transition layer, and surface pollution levels. Here, we present evidence for a mixing process within extratropical cyclones which has gained only a small amount of attention so far and which fosters the transport of tropospheric air masses into the…

Atmospheric Science010504 meteorology & atmospheric sciencesBaroclinityJet stream010502 geochemistry & geophysicsAtmospheric sciences01 natural scienceslcsh:QC1-999lcsh:ChemistryTropospherelcsh:QD1-999ddc:550Extratropical cyclonePotential temperatureOutflowTropopauseStratospherelcsh:Physics0105 earth and related environmental sciencesAtmospheric Chemistry and Physics
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Reappraising the appropriate calculation of a common meteorological quantity: Potential Temperature

2020

Abstract. The potential temperature is a widely used quantity in atmospheric science since it is conserved for dry air's adiabatic changes of state. Its definition involves the specific heat capacity of dry air, which is traditionally assumed as constant. However, the literature provides different values of this allegedly constant parameter, which are reviewed and discussed in this study. Furthermore, we derive the potential temperature for a temperature-dependent parameterisation of the specific heat capacity of dry air, thus providing a new reference potential temperature with a more rigorous basis. This new reference shows different values and vertical gradients, in particular in the str…

Atmospheric Science010504 meteorology & atmospheric sciencesBreaking wave02 engineering and technologyMechanics01 natural sciencesHeat capacitylcsh:QC1-999Articlelcsh:ChemistryTropospherelcsh:QD1-999020401 chemical engineeringEnvironmental sciencePotential temperatureGravity wave0204 chemical engineeringConstant (mathematics)Adiabatic processStratospherelcsh:PhysicsPhysics::Atmospheric and Oceanic Physics0105 earth and related environmental sciences
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The tropopause inversion layer in baroclinic life-cycle experiments: the role of diabatic processes

2016

Abstract. Recent studies on the formation of a quasi-permanent layer of enhanced static stability above the thermal tropopause revealed the contributions of dynamical and radiative processes. Dry dynamics leads to the evolution of a tropopause inversion layer (TIL), which is, however, too weak compared to observations and thus diabatic contributions are required. In this study we aim to assess the importance of diabatic processes in the understanding of TIL formation at midlatitudes. The non-hydrostatic model COSMO (COnsortium for Small-scale MOdelling) is applied in an idealized midlatitude channel configuration to simulate baroclinic life cycles. The effect of individual diabatic processe…

Atmospheric Science010504 meteorology & atmospheric sciencesChemistryBaroclinityDiabatic010502 geochemistry & geophysicsAtmospheric sciences01 natural scienceslcsh:QC1-999lcsh:ChemistryTropospherelcsh:QD1-999Latent heatRadiative transferTropopauseStratospherelcsh:PhysicsWater vapor0105 earth and related environmental sciencesAtmospheric Chemistry and Physics
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Biogenic and biomass burning organic aerosol in a boreal forest at Hyytiälä, Finland, during HUMPPA-COPEC 2010

2013

Abstract. Submicron aerosol particles were collected during July and August 2010 in Hyytiälä, Finland, to determine the composition and sources of aerosol at that boreal forest site. Submicron particles were collected on Teflon filters and analyzed by Fourier transform infrared (FTIR) spectroscopy for organic functional groups (OFGs). Positive matrix factorization (PMF) was applied to aerosol mass spectrometry (AMS) measurements and FTIR spectra to identify summertime sources of submicron aerosol mass at the sampling site. The two largest sources of organic mass (OM) in particles identified at Hyytiälä were (1) biogenic aerosol from surrounding local forest and (2) biomass burning aerosol, …

Atmospheric Science010504 meteorology & atmospheric sciencesChemistryTaiga15. Life on land010501 environmental sciencesMass spectrometry01 natural scienceslcsh:QC1-999Aerosollcsh:Chemistrylcsh:QD1-99913. Climate actionAtmospheric chemistryEnvironmental chemistryMass spectrumAerosol mass spectrometryGas chromatography–mass spectrometryBiomass burninglcsh:Physics0105 earth and related environmental sciences
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