Search results for " Radiation."

showing 10 items of 2788 documents

New particle formation events measured on board the ATR-42 aircraft during the EUCAARI campaign

2010

Aerosol properties were studied during an intensive airborne measurement campaign that took place at Rotterdam in Netherlands in May 2008 within the framework of the European Aerosol Cloud Climate and Air Quality Interactions project (EUCAARI). The objective of this study is to illustrate seven events of new particle formation (NPF) observed with two Condensation Particle Counters (CPCs) operated on board the ATR-42 research aircraft in airsectors around Rotterdam, and to provide information on the spatial extent of the new particle formation phenomenon based on 1-s resolution measurements of ultra-fine particle (in the size range 3–10 nm diameter, denoted N<sub>3-10</sub> herea…

Atmospheric ScienceRange (particle radiation)Meteorology010504 meteorology & atmospheric sciencesCondensationNucleation010501 environmental sciences01 natural scienceslcsh:QC1-999Aerosollcsh:ChemistryBoundary layerlcsh:QD1-99913. Climate actionEnvironmental scienceParticle[SDU.STU.GL]Sciences of the Universe [physics]/Earth Sciences/GlaciologyAir quality indexAir masslcsh:Physics0105 earth and related environmental sciencesATMOSPHERIC CHEMISTRY AND PHYSICS, 10, 6721-6735, 2010
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Sensitivity of the atmospheric temperature profile to the aerosol absorption in the presence of dust

2014

Abstract Radiative transfer simulations in the shortwave (SW) and longwave (LW) spectral regions have been carried out to investigate the time evolution of the atmospheric heating/cooling rates and their influence on the temperature profiles under different vertical distributions of the aerosol absorption. The case study is based on measurements made at Rome, Italy, on 20 June 2007, when a dust layer was present above the urban boundary layer (BL) and the column aerosol optical depth at 550 nm was about 0.37. Column-integrated aerosol optical depth and single scattering albedo, as well as vertical profiles of aerosol extinction and meteorological variables have been derived from observation…

Atmospheric ScienceSingle-scattering albedoChemistryLongwaveAerosol radiative forcingSensible heatAtmospheric sciencesAtmospheric temperatureAerosolTemperature profileRadiative transferAerosol absorption/scatteringAerosol radiative forcing;Aerosol absorption/scattering;Atmospheric heating rate;Temperature profileAbsorption (electromagnetic radiation)ShortwaveGeneral Environmental ScienceAtmospheric heating rate
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An analysis of VLF electric field spectra measured in Titan's atmosphere by the Huygens probe

2009

[1] A numerical simulation of Titan's electromagnetic cavity in the VLF band is carried out using the Transmission Line Matrix (TLM) method, with the aim of assessing the VLF electric field spectra sent by the Huygens probe. In an Earth-like model, successive peaks would be expected in the spectra, associated with multiple reflections of the electromagnetic wave on the external surfaces of Titan's electromagnetic cavity, formed by the ionosphere and a conductive ground or underground surface. However, owing to high losses conferred by the electrical conductivity to Titan's atmosphere, the direct numerical and experimental spectra are decreasing functions of the frequency without resonances …

Atmospheric ScienceSoil ScienceAquatic ScienceOceanographyElectromagnetic radiationSpectral linesymbols.namesakeOpticsGeochemistry and PetrologyElectrical resistivity and conductivityElectric fieldElectromagnetic cavityEarth and Planetary Sciences (miscellaneous)Earth-Surface ProcessesWater Science and TechnologyPhysicsEcologybusiness.industryPaleontologyResonanceForestryComputational physicsGeophysicsSpace and Planetary SciencePhysics::Space PhysicssymbolsAstrophysics::Earth and Planetary AstrophysicsIonosphereTitan (rocket family)businessJournal of Geophysical Research
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Optical properties of deep glacial ice at the South Pole

2006

We have remotely mapped optical scattering and absorption in glacial ice at the South Pole for wavelengths between 313 and 560 nm and depths between 1100 and 2350 m. We used pulsed and continuous light sources embedded with the AMANDA neutrino telescope, an array of more than six hundred photomultiplier tubes buried deep in the ice. At depths greater than 1300 m, both the scattering coefficient and absorptivity follow vertical variations in concentration of dust impurities, which are seen in ice cores from other Antarctic sites and which track climatological changes. The scattering coefficient varies by a factor of seven, and absorptivity (for wavelengths less than ∼450 nm) varies by a fact…

Atmospheric ScienceSoil ScienceMineralogyAquatic ScienceOceanographyLight scatteringPhysics::GeophysicsIce coreGeochemistry and PetrologyEarth and Planetary Sciences (miscellaneous)Absorption (electromagnetic radiation)Physics::Atmospheric and Oceanic PhysicsEarth-Surface ProcessesWater Science and Technologygeographygeography.geographical_feature_categoryEcologyScatteringPaleontologyForestryGlacierMolar absorptivityWavelengthGeophysicsSpace and Planetary ScienceAttenuation coefficientAstrophysics::Earth and Planetary AstrophysicsGeologyJournal of Geophysical Research
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The impact of geoengineering on vegetation in experiment G1 of the GeoMIP

2015

Solar Radiation Management (SRM) has been proposed as a mean to partly counteract global warming. The Geoengineering Model Intercomparison Project (GeoMIP) has simulated the climate consequences of a number of SRM techniques. Thus far, the effects on vegetation have not yet been thoroughly analyzed. Here the vegetation response to the idealized GeoMIP G1 experiment from eight fully coupled Earth system models (ESMs) is analyzed, in which a reduction of the solar constant counterbalances the radiative effects of quadrupled atmospheric CO2 concentrations (abrupt4 × CO2). For most models and regions, changes in net primary productivity (NPP) are dominated by the increase in CO2, via the CO2 fe…

Atmospheric ScienceSolar constantbusiness.industryGlobal warmingPrimary productionVegetationCarbon cycleGeophysicsSpace and Planetary ScienceSolar radiation managementClimatologyEarth and Planetary Sciences (miscellaneous)Environmental scienceClimate engineeringbusinessNitrogen cycleJournal of Geophysical Research: Atmospheres
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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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Comparison of global ultraviolet (290–385 nm) and global irradiation measured during the warm season in valencia, spain

1994

This paper studies data of ultraviolet (290–385 nm band) horizontal solar irradiation and global horizontal solar irradiation measured at Valencia (Spain) during the period March 1991 to September 1991. Analysis of error estimations and correlation coefficients show that the 10 minute, hourly, and daily values of ultraviolet (UV) and global irradiation are highly correlated. Improved figures and less dependence on location are achieved by defining a clearness index for the UV 290–385 nm band and relating it to the conventional whole-band clearness index. The novel clearness index obtained from Valencia data is approximately half of the conventional clearness index. Considering solar elevati…

Atmospheric SciencebiologyClimatologyCorrelation analysismedicineEnvironmental scienceIrradiationWarm seasonmedicine.disease_causebiology.organism_classificationUltraviolet radiationValenciaUltravioletInternational Journal of Climatology
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2009

Abstract. A characterization of the ultra-fine aerosol particle counter COPAS (COndensation PArticle counting System) for operation on board the Russian high altitude research aircraft M-55 Geophysika is presented. The COPAS instrument consists of an aerosol inlet and two dual-channel continuous flow Condensation Particle Counters (CPCs) operated with the chlorofluorocarbon FC-43. It operates at pressures between 400 and 50 hPa for aerosol detection in the particle diameter (dp) range from 6 nm up to 1 μm. The aerosol inlet, designed for the M-55, is characterized with respect to aspiration, transmission, and transport losses. The experimental characterization of counting efficiencies of th…

Atmospheric SciencegeographyRange (particle radiation)geography.geographical_feature_categoryChemistryCondensationAnalytical chemistryParticleInletParticle counterCondenser (heat transfer)AerosolLine (formation)Atmospheric Measurement Techniques
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Application of aerosol optical properties to estimate aerosol type from ground-based remote sensing observation at urban area of northeastern China

2015

Abstract Aerosol optical properties were derived from ground-based sunphotometer observations between 2009-2013 at three urban sites of Shenyang, Anshan, Fushun in northeastern China. The annual means for extinction aerosol optical depths (EAOD) at 500 nm were 0.57±0.38, 0.52±0.35, and 0.41±0.31 at Shenyang, Anshan, Fushun, respectively. The corresponding annual means for the extinction Angstrom exponents (EAE) computed for the wavelengths of 440 and 870 nm were 0.86±0.32, 0.86±0.34 and 0.91±0.35, respectively, indicating that urban area of Northeast China were affected by both coarse and fine particles. Hygroscopic growth in summer and incursions of dust aerosols in spring were evidently r…

Atmospheric Sciencegeographygeography.geographical_feature_categoryMeteorologyCoal combustion productsMineral dustUrban areaAtmospheric sciencesAerosolGeophysicsSpace and Planetary ScienceExtinction (optical mineralogy)Environmental scienceAngstromBiomass burningAbsorption (electromagnetic radiation)Journal of Atmospheric and Solar-Terrestrial Physics
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Saharan dust absorption and refractive index from aircraft-based observations during SAMUM 2006

2009

During the Saharan Mineral Dust Experiment (SAMUM) conducted in summer 2006 in southeast Morocco, the complex refractive index of desert dust was determined from airborne measurements of particle size distributions and aerosol absorption coefficients at three different wavelengths in the blue (467 nm), green (530 nm) and red (660 nm) spectral regions. The vertical structure of the dust layers was analysed by an airborne high spectral resolution lidar (HSRL). The origin of the investigated dust layers was estimated from trajectory analyses, combined with Meteosat 2nd Generation (MSG) scenes and wind field data analyses. The real part n of the dust refractive index was found almost constant w…

Atmospheric Sciencerefractive indexMaterials science010504 meteorology & atmospheric sciencesaerosolAtmosphärische SpurenstoffeMineralogy010501 environmental sciencesMineral dust01 natural sciencesAerosolSAMUMTroposphereWavelengthLidarSpectral resolutionAbsorption (electromagnetic radiation)absorptionRefractive index0105 earth and related environmental sciencesRemote sensingTellus B: Chemical and Physical Meteorology
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