Search results for "Radiative forcing"

showing 10 items of 60 documents

Spectral optical layer properties of cirrus from collocated airborne measurements and simulations

2016

Abstract. Spectral upward and downward solar irradiances from vertically collocated measurements above and below a cirrus layer are used to derive cirrus optical layer properties such as spectral transmissivity, absorptivity, reflectivity, and cloud top albedo. The radiation measurements are complemented by in situ cirrus crystal size distribution measurements and radiative transfer simulations based on the microphysical data. The close collocation of the radiative and microphysical measurements, above, beneath, and inside the cirrus, is accomplished by using a research aircraft (Learjet 35A) in tandem with the towed sensor platform AIRTOSS (AIRcraft TOwed Sensor Shuttle). AIRTOSS can be re…

Effective radiusAtmospheric Science010504 meteorology & atmospheric sciencesRadiative coolingCloud topAlbedoRadiative forcingAtmospheric sciences01 natural scienceslcsh:QC1-999lcsh:Chemistry010309 opticslcsh:QD1-9990103 physical sciencesRadiative transferEnvironmental scienceCirrusShortwavelcsh:Physics0105 earth and related environmental sciencesRemote sensingAtmospheric Chemistry and Physics
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Extinction and optical depth of contrails

2011

[1] One factor limiting the understanding of the climate impact from contrails and aircraft induced cloud modifications is the accurate determination of their optical depth. To this end, 14 contrails were sampled for 2756 s with instruments onboard the research aircraft Falcon during the CONCERT (CONtrail and Cirrus ExpeRimenT) campaign in November 2008. The young (<10 min old) contrails were produced by 9 commercial aircraft with weights of 47 to 508 t, among them the largest operating passenger aircraft, the Airbus A380. The contrails were observed at temperatures between 214 and 224 K and altitudes between 8.8 and 11.1 km. The measured mean in-contrail relative humidity with respect to i…

Effective radiusGeophysicsMeteorologyExtinction (optical mineralogy)Range (aeronautics)Radiative transferGeneral Earth and Planetary SciencesEnvironmental scienceCirrusRelative humidityRadiative forcingAtmospheric sciencesOptical depthGeophysical Research Letters
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Understanding the Effects of Fires on Surface Evapotranspiration Patterns Using Satellite Remote Sensing in Combination with an Energy Balance Model

2011

Forest fires are highly destructive for nature, affecting the landscape, the natural cicle of the vegetation, and the structure and functioning of ecosystems. Beyond that, they also provoke changes in the local and regional meteorology, and particularly in the surface energy flux patterns. In a fire-affected area, changes in the ecosystem structure and species composition modify the evapotranspiration (LE) and the rest of the terms involved in the energy balance equation. Besides, these changes in the local energy balance may persist for decades (Randerson et al., 2006). There is an increasing concern among the scientific community about the effect of forest fires on climate change at this …

GeographyPhysical modelMeteorologyEvapotranspirationClimatologyEnergy balanceClimate changeEnergy fluxVegetationRadiative forcingScale (map)
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Contrail ice particles in aircraft wakes and their climatic importance

2013

[1] Measurements of gaseous (NO, NOy, SO2, HONO) and ice particle concentrations in young contrails in primary and secondary wakes of aircraft of different sizes (B737, A319, A340, A380) are used to investigate ice particle formation behind aircraft. The gas concentrations are largest in the primary wake and decrease with increasing altitude in the secondary wake, as expected for passive trace gases and aircraft-dependent dilution. In contrast, the measured ice particle concentrations were found larger in the secondary wake than in the primary wake. The contrails contain more ice particles than expected for previous black carbon (soot) estimates. The ice concentrations may result from soot-…

MeteorologyRadiative forcingAtmospheric sciencesmedicine.disease_causeSootcontrail soot wake climate aviation aircraft ice emissionsTrace gasAerosolGeophysicsIce nucleusmedicineGeneral Earth and Planetary SciencesEnvironmental scienceParticleCirrusOptical depth
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Stratospheric sulfur and its implications for radiative forcing simulated by the chemistry climate model EMAC

2015

Multiyear simulations with the atmospheric chemistry general circulation model EMAC with a microphysical modal aerosol module at high vertical resolution demonstrate that the sulfur gases COS and SO2, the latter from low-latitude and midlatitude volcanic eruptions, predominantly control the formation of stratospheric aerosol. Marine dimethyl sulfide (DMS) and other SO2 sources, including strong anthropogenic emissions in China, are found to play a minor role except in the lowermost stratosphere. Estimates of volcanic SO2 emissions are based on satellite observations using Total Ozone Mapping Spectrometer and Ozone Monitoring Instrument for total injected mass and Michelson Interferometer fo…

Ozone Monitoring InstrumentAtmospheric Scienceradiative forcingTotal Ozone Mapping SpectrometervolcanoesRadiative forcingAtmospheric sciences7. Clean energyAerosolchemistry climate modelchemistry.chemical_compoundGeophysicschemistrystratospheric sulfur13. Climate actionSpace and Planetary ScienceAtmospheric chemistryClimatologyEarth and Planetary Sciences (miscellaneous)Radiative transferEnvironmental scienceSulfate aerosolStratosphereResearch ArticlesJournal of Geophysical Research: Atmospheres
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A new radiation infrastructure for the Modular Earth Submodel System (MESSy, based on version 2.51)

2016

Abstract. The Modular Earth Submodel System (MESSy) provides an interface to couple submodels to a basemodel via a highly flexible data management facility (Jöckel et al., 2010). In the present paper we present the four new radiation related submodels RAD, AEROPT, CLOUDOPT and ORBIT. The submodel RAD (with shortwave radiation scheme RAD_FUBRAD) simulates the radiative transfer, the submodel AEROPT calculates the aerosol optical properties, the submodel CLOUDOPT calculates the cloud optical properties, and the submodel ORBIT is responsible for Earth orbit calculations. These submodels are coupled via the standard MESSy infrastructure and are largely based on the original radiation scheme of …

PhysicsECHAMEarth's orbit010504 meteorology & atmospheric sciencesMeteorologybusiness.industrylcsh:QE1-996.5Radiative forcingGeneral Medicine010501 environmental sciencesRadiative forcingModular design55101 natural scienceslcsh:Geologymodularised EMAC radiationErdsystem-ModellierungOrbit (dynamics)Radiative transferShortwave radiationAerospace engineeringbusinessStratosphere0105 earth and related environmental sciences
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High Arctic aircraft measurements characterising black carbon vertical variability in spring and summer

2019

The vertical distribution of black carbon (BC) particles in the Arctic atmosphere is one of the key parameters controlling their radiative forcing and thus role in Arctic climate change. This work investigates the presence and properties of these light-absorbing aerosols over the High Canadian Arctic (&gt;70∘&thinsp;N). Airborne campaigns were performed as part of the NETCARE project (Network on Climate and Aerosols: Addressing Key Uncertainties in Remote Canadian Environments) and provided insights into the variability of the vertical distributions of BC particles in summer 2014 and spring 2015. The observation periods covered evolutions of cyclonic disturbances at the polar front, which f…

Polar frontAtmospheric Scienceeducation.field_of_study010504 meteorology & atmospheric sciencesPopulation010501 environmental sciencesRadiative forcingAtmospheric sciences01 natural scienceslcsh:QC1-999LatitudeAerosolAtmospherelcsh:ChemistryAltitudeArcticlcsh:QD1-99913. Climate actionEnvironmental scienceeducationlcsh:Physics0105 earth and related environmental sciencesAtmospheric Chemistry and Physics
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Column aerosol optical properties and aerosol radiative forcing during a serious haze-fog month over North China Plain in 2013 based on ground-based …

2014

In January 2013, North China Plain experienced several serious haze events. Cimel sunphotometer measurements at seven sites over rural, suburban and urban regions of North China Plain from 1 to 30 January 2013 were used to further our understanding of spatial-temporal variation of aerosol optical parameters and aerosol radiative forcing (ARF). It was found that Aerosol Optical Depth at 500 nm (AOD500 nm) during non-pollution periods at all stations was lower than 0.30 and increased significantly to greater than 1.00 as pollution events developed. The Angstrom exponent (Alpha) was larger than 0.80 for all stations most of the time. AOD500 nm averages increased from north to south during both…

PollutionAtmospheric ScienceAngstrom exponentHaze010504 meteorology & atmospheric sciencesmedia_common.quotation_subjectRadiative forcing010501 environmental sciencesAtmospheric sciences01 natural sciencesAtmospherelcsh:Chemistry11. SustainabilityAerosolesmedia_common0105 earth and related environmental sciencesHydrologyAerosolsSingle-scattering albedoRadiative forcingAlbedoCalimalcsh:QC1-999Aerosollcsh:QD1-99913. Climate actionEnvironmental scienceHazeForzamiento radiativolcsh:Physics
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What Drove Past Teleconnections?

2003

Ice core records from Greenland and Antarctica and sediment records from the world9s oceans have shown that over the past 100,000 years, climate has varied substantially across the globe. In his Perspective, Sirocko asks what drove these--sometimes very rapid--climate oscillations. He highlights the report of Burns et al., whose monsoon record from the Indian Ocean shows strong similarities with ice core records from Greenland. Sirocko argues that the large areas of homogeneous sea surface temperature in the cold circum-Antarctic current and in the warm-water masses of the low latitudes must have played an important role in linking climate forcing between distant parts of the world. The muc…

Sea surface temperatureMultidisciplinaryGeographymedicine.anatomical_structureOceanographyIce coreHomogeneousmedicineGlobeRadiative forcingMonsoonLatitudeTeleconnectionScience
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Abundance of cellular material and proteins in the atmosphere.

2005

Suspended atmospheric particles play a crucial role in any global climate scenario: They can both enforce and suppress radiative forcing. In developing climate modeling further, a deeper understanding of atmospheric aerosol is needed. Because of extreme local and temporal variations, proper incorporation of aerosols into models requires modeling of the aerosol itself. It turns out that cellular material and proteins compose up to 25% of the atmospheric aerosol. Consequently, the source strength of the biogenic aerosol in general must be corrected and should be estimated on the order of other major aerosol sources.

SporesMeteorologyCellsAir MicrobiologyEnvironmentAtmospheric sciencesTroposphereAtmosphereAnimalsHumansParticle SizeAerosolsMultidisciplinaryBacteriaAtmosphereFungiBiogeochemistryEukaryotaProteinsRadiative forcingAerosolAtmospheric chemistryVirusesEnvironmental sciencePollenClimate modelSeasonsBioaerosolScience (New York, N.Y.)
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