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showing 10 items of 2599 documents

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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Mountain waves modulate the water vapor distribution in the UTLS

2017

Abstract. The water vapor distribution in the upper troposphere–lower stratosphere (UTLS) region has a strong impact on the atmospheric radiation budget. Transport and mixing processes on different scales mainly determine the water vapor concentration in the UTLS. Here, we investigate the effect of mountain waves on the vertical transport and mixing of water vapor. For this purpose we analyze measurements of water vapor and meteorological parameters recorded by the DLR Falcon and NSF/NCAR Gulfstream V research aircraft taken during the Deep Propagating Gravity Wave Experiment (DEEPWAVE) in New Zealand. By combining different methods, we develop a new approach to quantify location, direction…

Atmospheric Science010504 meteorology & atmospheric sciencesTransportmountain wavesAtmospheric sciences01 natural sciences010305 fluids & plasmaslcsh:ChemistryTroposphere0103 physical sciencesUTLSGravity waveWolkenphysikDropsondeStratosphere0105 earth and related environmental sciencesVerkehrsmeteorologieRadiative forcinglcsh:QC1-999water vapourWavelengthlcsh:QD1-999ClimatologyEnvironmental scienceTropopauselcsh:PhysicsWater vapor
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Observed versus simulated mountain waves over Scandinavia – improvement of vertical winds, energy and momentum fluxes by enhanced model resolut…

2017

Abstract. Two mountain wave events, which occurred over northern Scandinavia in December 2013 are analysed by means of airborne observations and global and mesoscale numerical simulations with horizontal mesh sizes of 16, 7.2, 2.4 and 0.8 km. During both events westerly cross-mountain flow induced upward-propagating mountain waves with different wave characteristics due to differing atmospheric background conditions. While wave breaking occurred at altitudes between 25 and 30 km during the first event due to weak stratospheric winds, waves propagated to altitudes above 30 km and interfacial waves formed in the troposphere at a stratospheric intrusion layer during the second event. Global an…

Atmospheric Science010504 meteorology & atmospheric sciencesairborne observationsFlow (psychology)Mesoscale meteorologygravity waves010502 geochemistry & geophysicsAtmospheric sciences01 natural sciencesPhysics::GeophysicsTropospherelcsh:ChemistryGW-LCYCLE IPhysics::Atmospheric and Oceanic Physics0105 earth and related environmental sciencesMomentum (technical analysis)Institut für Physik der AtmosphäreLidarTurbulent diffusionVerkehrsmeteorologieBreaking wavelcsh:QC1-999WavelengthAmplitudenumerical modelinglcsh:QD1-999Geologylcsh:PhysicsAtmospheric Chemistry and Physics
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Microphysical and optical properties of Arctic mixed-phase clouds. The 9 April 2007 case study.

2009

Abstract. Airborne measurements in Arctic boundary-layer stratocumulus were carried out near Spitsbergen on 9 April 2007 during the Arctic Study of Tropospheric Aerosol, Clouds and Radiation (ASTAR) campaign. A unique set of co-located observations is used to describe the cloud properties, including detailed in situ cloud microphysical and radiation measurements along with airborne and co-located spaceborne remote sensing data (Lidar on Cloud-Aerosol Lidar and Infrared Pathfinder Satellite Observations [CALIPSO] and radar on CloudSat satellites). The CALIPSO profiles evidence a cloud top temperature which varies between −24°C and −21°C. The in situ cloud observations reveal that the attenua…

Atmospheric ScienceASTARArktische Grenzschicht010504 meteorology & atmospheric sciencesBackscatterCloud coverCALIPSOMischphasenwolken010502 geochemistry & geophysicsAtmospheric sciences01 natural sciences010309 opticslcsh:Chemistry0103 physical sciencesPrecipitation0105 earth and related environmental sciencesLidarIce crystalsCloud toplcsh:QC1-999Lidarlcsh:QD1-999Arctic13. Climate actionExtinction (optical mineralogy)Environmental sciencelcsh:PhysicsWolkenphysik und VerkehrsmeteorologieAtmospheric Chemistry and Physics
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Lidar characterization of the Arctic atmosphere during ASTAR 2007: Four cases studies of boundary layer, mixed-phase and multi-layer clouds

2010

During the Arctic Study of Tropospheric Aerosol, Clouds and Radiation (ASTAR), which was conducted in Svalbard in March and April 2007, tropospheric Arctic clouds were observed with two ground-based backscatter lidar systems (micro pulse lidar and Raman lidar) and with an airborne elastic lidar. In the time period of the ASTAR 2007 campaign, an increase in low-level cloud cover (cloud tops below 2.5 km) from 51% to 65% was observed above Ny-Ålesund. Four different case studies of lidar cloud observations are analyzed: With the ground-based Raman lidar, a layer of spherical particles was observed at an altitude of 2 km after the dissolution of a cloud. The layer probably consisted of small h…

Atmospheric ScienceASTARArktische Grenzschicht010504 meteorology & atmospheric sciencesCloud coverMischphasenwolkenAtmospheric sciences01 natural scienceslcsh:Chemistry010309 opticsAtmosphereTroposphere0103 physical sciences0105 earth and related environmental sciencesRemote sensingLidarCloud topOrographylcsh:QC1-999Boundary layerLidarlcsh:QD1-999Arctic13. Climate actionEnvironmental sciencelcsh:PhysicsWolkenphysik und Verkehrsmeteorologie
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SAL—A Novel Quality Measure for the Verification of Quantitative Precipitation Forecasts

2008

Abstract A novel object-based quality measure, which contains three distinct components that consider aspects of the structure (S), amplitude (A), and location (L) of the precipitation field in a prespecified domain (e.g., a river catchment) is introduced for the verification of quantitative precipitation forecasts (QPF). This quality measure is referred to as SAL. The amplitude component A measures the relative deviation of the domain-averaged QPF from observations. Positive values of A indicate an overestimation of total precipitation; negative values indicate an underestimation. For the components S and L, coherent precipitation objects are separately identified in the forecast and obser…

Atmospheric ScienceMatching (statistics)MeteorologyforecastDiagramprecipitationForecast verificationMeasure (mathematics)Displacement (vector)AmplitudeQuantitative precipitation forecastPrecipitationverificationWolkenphysik und VerkehrsmeteorologieradarMathematicsMonthly Weather Review
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Influence of ice crystal shape on retrieval of cirrus optical thickness and effective radius: A case study

2009

Airborne measurements of spectral upwelling radiances (350A¢Â�Â�2200 nm) reflected by cirrus using the Spectral Modular Airborne Radiation measurement sysTem (SMART)-Albedometer were made over land and water surfaces. Based on these data, cloud optical thickness tau and effective radius Reff of the observed cirrus were retrieved. By using different crystal shape assumptions (hexagonal plates, solid and hollow columns, rough aggregates, planar and spatial rosettes, ice spheres, and a mixture of particle habits) in the retrieval, the influence of crystal shape on the retrieved tau and Reff was evaluated. With relative differences of up to 70%, the influence of particle habit on t is larger th…

Atmospheric ScienceMaterials scienceiceSoil SciencecirrusAquatic ScienceOceanographycrystalCrystalOpticsGeochemistry and PetrologyEarth and Planetary Sciences (miscellaneous)Physics::Atmospheric and Oceanic PhysicsEarth-Surface ProcessesWater Science and TechnologyEffective radiusLidarIce cloudEcologyIce crystalsFernerkundung der Atmosphärebusiness.industryAtmosphärische SpurenstoffePaleontologyForestryFalconGeophysicsLidarSpace and Planetary ScienceRadianceCIRCLE-2SPHERESCirrusbusinessJournal of Geophysical Research
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Aircraft type influence on contrail properties

2013

The investigation of the impact of aircraft parameters on contrail properties helps to better understand the climate impact from aviation. Yet, in observations, it is a challenge to separate aircraft and meteorological influences on contrail formation. During the CONCERT campaign in November 2008, contrails from 3 Airbus passenger aircraft of types A319-111, A340-311 and A380-841 were probed at cruise under similar meteorological conditions with in situ instruments on board DLR research aircraft Falcon. Within the 2 min-old contrails detected near ice saturation, we find similar effective diameters Deff (5.2–5.9 μm), but differences in particle number densities nice (162–235 cm−3) and…

Atmospheric ScienceMeteorologyParticle numberMicrophysicsAviationbusiness.industryAtmosphärische SpurenstoffeInitializationaircraft typecontrailAtmospheric scienceslcsh:QC1-999aircraft effectlcsh:ChemistryOn boardlcsh:QD1-999Fuel flowddc:550Environmental scienceCirrusRelative humiditybusinessclimatelcsh:PhysicsWolkenphysik und Verkehrsmeteorologie
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Reproducing cloud microphysical and irradiance measurements using three 3D cloud generators

2007

Using three cloud generators, three-dimensional (3D) cloud fields are reproduced from microphysical cloud data measured in situ by aircraft. The generated cloud fields are used as input to a 3D radiative transfer model to calculate the corresponding fields of downward and upward irradiance, which are then compared with airborne and ground-based radiation measurements. One overcast stratocumulus scene and one broken cumulus scene were selected from the European INSPECTRO field experiment, which was held in Norwich, UK, in September 2002. With these data, the characteristics of the three different cloud reproduction techniques are assessed. Besides vertical profiles and histograms of measured…

Atmospheric SciencePixelMeteorologybusiness.industryFernerkundung der Atmosphärecloud generatorAutocorrelationIrradianceCloud computingradiationAtmospheric radiative transfer codesOvercastLiquid water contentRadiative transferEnvironmental sciencethree-dimensionalradiative transfer modelbusinessRemote sensing
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Apparent absorption of solar spectral irradiance in heterogeneous ice clouds

2010

[1] Coordinated flight legs of two aircraft above and below extended ice clouds played an important role in the Tropical Composition, Cloud and Climate Coupling Experiment (Costa Rica, 2007). The Solar Spectral Flux Radiometer measured up- and downward irradiance on the high-altitude (ER-2) and the low-altitude (DC-8) aircraft, which allowed deriving apparent absorption on a point-by-point basis along the flight track. Apparent absorption is the vertical divergence of irradiance, calculated from the difference of net flux at the top and bottom of a cloud. While this is the only practical method of deriving absorption from aircraft radiation measurements, it differs from true absorption when…

Atmospheric ScienceSpectral shape analysisIrradianceSoil ScienceAquatic ScienceOceanographyice cloud absorptionAtmosphereAtmospheric radiative transfer codesGeochemistry and PetrologyEarth and Planetary Sciences (miscellaneous)3-D radiative transferAbsorption (electromagnetic radiation)Physics::Atmospheric and Oceanic PhysicsEarth-Surface ProcessesWater Science and TechnologyRemote sensingPhysicsEffective radiusRadiometerEcologyFernerkundung der AtmosphärePaleontologyForestryGeophysicsSpace and Planetary Sciencesolar spectral measurementsModerate-resolution imaging spectroradiometer
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