Search results for "Radiative Forcing"

showing 10 items of 60 documents

2018

Abstract. Detailed measurements of radiation, atmospheric and aerosol properties were carried out in summer 2013 during the Aerosol Direct Radiative Impact on the regional climate in the MEDiterranean region (ADRIMED) campaign in the framework of the Chemistry-Aerosol Mediterranean Experiment (ChArMEx) experiment. This study focusses on the characterization of infrared (IR) optical properties and direct radiative effects of mineral dust, based on three vertical profiles of atmospheric and aerosol properties and IR broadband and narrowband radiation from airborne measurements, made in conjunction with radiosonde and ground-based observations at Lampedusa, in the central Mediterranean. Satell…

Atmospheric Science010504 meteorology & atmospheric sciencesAstrophysics::Cosmology and Extragalactic AstrophysicsRadiative forcingMineral dustAtmospheric sciences01 natural sciencesAerosolAERONET010309 opticsAtmospheric radiative transfer codes13. Climate actionBrightness temperature0103 physical sciencesRadiative transferAstrophysics::Solar and Stellar AstrophysicsEnvironmental scienceAstrophysics::Earth and Planetary AstrophysicsPhysics::Atmospheric and Oceanic PhysicsAstrophysics::Galaxy AstrophysicsZenith0105 earth and related environmental sciencesRemote sensingAtmospheric Chemistry and Physics
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Computation of anthropogenic sulphate aerosol forcing using radiative perturbation theory

1994

The radiative forcing of the climate by anthropogenic aerosols has been a matter of some concern for many years now, especially in the northern hemisphere. Recently in these pages, Charlson et al. attempted to quantify this forcing. However, that calculation involved relatively crude optical and radiative transfer models. In this paper, we use a far more detailed sulphate optical model, and employ radiative perturbation theory (a technique ideally suited to answering questions of this sort) to repeat this radiation calculation. We obtain results which are similar to Charlson et al., provided that proper allowance is made for the effects of humidity. DOI: 10.1034/j.1600-0889.1994.00003.x

Atmospheric Science010504 meteorology & atmospheric sciencesComputationNorthern HemisphereForcing (mathematics)010501 environmental sciencesRadiative forcingAtmospheric sciences01 natural sciencesAerosolAtmospheric radiative transfer codesClimatologyRadiative transferEnvironmental sciencePerturbation theory0105 earth and related environmental sciencesTellus B
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2021

Abstract. The strong reduction of air traffic during the COVID-19 pandemic provides a unique test case for the relationship between air traffic density, contrails, and their radiative forcing of climate change. Here, air traffic and contrail cirrus changes are quantified for a European domain for March to August 2020 and compared to the same period in 2019. Traffic data show a 72 % reduction in flight distance compared with 2019. This paper investigates the induced contrail changes in a model study. The contrail model results depend on various methodological details as discussed in parameter studies. In the reference case, the reduced traffic caused a reduction in contrail length. The reduc…

Atmospheric Science010504 meteorology & atmospheric sciencesLongwaveForcing (mathematics)010501 environmental sciencesRadiative forcingAtmospheric sciences01 natural sciencesAtmosphereEnvironmental scienceCirrusShortwaveOptical depthWater vapor0105 earth and related environmental sciencesAtmospheric Chemistry and Physics
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Heating rate profiles and radiative forcing due to a dust storm in the Western Mediterranean using satellite observations

2017

Abstract We analyze the vertically-resolved radiative impact due to a dust storm in the Western Mediterranean. The dust plume travels around 3–5 km altitude and the aerosol optical depth derived by MODIS at 550 nm ranges from 0.33 to 0.52 at the overpass time (13:05 UT). The aerosol radiative forcing (ARF), forcing efficiency (FE) and heating rate profile (AHR) are determined throughout the dust trajectory in shortwave (SW) and longwave (LW) ranges. To do this, we integrate different satellite observations (CALIPSO and MODIS) and detailed radiative transfer modeling. The combined (SW + LW) effect of the dust event induces a net cooling in the studied region. On average, the FE at 22.4° sola…

Atmospheric Science010504 meteorology & atmospheric sciencesLongwaveSolar zenith angleRadiative forcing010502 geochemistry & geophysicsAtmospheric sciences01 natural sciencesPlumeDust stormRadiative transferEnvironmental scienceShortwaveRefractive index0105 earth and related environmental sciencesGeneral Environmental ScienceAtmospheric Environment
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Vertical profiles of light absorption and scattering associated with black carbon particle fractions in the springtime Arctic above 79° N

2020

Despite the potential importance of black carbon (BC) for radiative forcing of the Arctic atmosphere, vertically resolved measurements of the particle light scattering coefficient (σsp) and light absorption coefficient (σap) in the springtime Arctic atmosphere are infrequent, especially measurements at latitudes at or above 80∘ N. Here, relationships among vertically distributed aerosol optical properties (σap, σsp and single scattering albedo or SSA), particle microphysics and particle chemistry are examined for a region of the Canadian archipelago between 79.9 and 83.4∘ N from near the surface to 500 hPa. Airborne data collected during April 2015 are combined with gro…

Atmospheric Science010504 meteorology & atmospheric sciencesMicrophysicsSingle-scattering albedo010501 environmental sciencesRadiative forcingAtmospheric sciences01 natural scienceslcsh:QC1-999Light scatteringAerosollcsh:ChemistryTroposphereAtmospherelcsh:QD1-999Arctic13. Climate actionlcsh:Physics0105 earth and related environmental sciencesAtmospheric Chemistry and Physics
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Intercomparison and evaluation of global aerosol microphysical properties among AeroCom models of a range of complexity

2014

Many of the next generation of global climate models will include aerosol schemes which explicitly simulate the microphysical processes that determine the particle size distribution. These models enable aerosol optical properties and cloud condensation nuclei (CCN) concentrations to be determined by fundamental aerosol processes, which should lead to a more physically based simulation of aerosol direct and indirect radiative forcings. This study examines the global variation in particle size distribution simulated by 12 global aerosol microphysics models to quantify model diversity and to identify any common biases against observations. Evaluation against size distribution measurements from…

Atmospheric Science010504 meteorology & atmospheric sciencesParticle numbergeneral-circulation modelmixing state010501 environmental sciencesEnvironmentclimate modelblack carbonAtmospheric sciences01 natural sciencesTropospherelcsh:ChemistryZeppelinobservatorietUrban Developmentddc:550Cloud condensation nucleiBuilt Environmentnumber size distributionsPhysics::Atmospheric and Oceanic Physics0105 earth and related environmental sciencesMicrophysicsparticle formationEarth / EnvironmentalCloud physicsatmospheric aerosolCAS - Climate Air and SustainabilityRadiative forcinglcsh:QC1-999Aerosolcloud condensation nucleimarine boundary-layerlcsh:QD1-99913. Climate actionClimatologyEnvironmental scienceClimate modelELSS - Earth Life and Social Sciencesoff-line modellcsh: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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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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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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The June 2007 Saharan dust event in the central Mediterranean: Observations and radiative effects in marine, urban, and sub-urban environments

2011

Abstract A desert dust episode in June 2007 and its radiative effects on the energy budget have been studied at three Italian stations (Rome, Lecce and Lampedusa) with the aim of investigating the interactions with different conditions and aerosol types over the Mediterranean. The three sites are representative for urban (Rome), sub-urban/rural (Lecce), and marine (Lampedusa) environment, respectively in the central Mediterranean region. Measured ground-based column-averaged aerosol optical properties and aerosol extinction profiles were used to initialize the MODTRAN4 radiative transfer model. The radiative transfer model was used to estimate the shortwave aerosol radiative forcing ( ARF )…

Atmospheric ScienceAngstrom exponentAerosol Optical PropertiePlanetary boundary layerRadiative forcingMineral dustAtmospheric sciencesAerosol optical properties; Vertical distribution; Radiative forcing; Desert dust eventAERONETAerosolAtmospheric radiative transfer codesRadiative transferEnvironmental sciencedesert dust event; aerosol optical properties; radiative forcing; vertical distributionVertical DistributionRadiative ForcingGeneral Environmental Science
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