Search results for "Single"

showing 10 items of 4920 documents

"Table 2" of "Investigation of the splitting of quark and gluon jets."

1998

Scaled energy distribution of charged hadrons produced in Gluon jets in 'Y'topology 3-JET events.

Astrophysics::High Energy Astrophysical PhenomenaE+ E- --> Z0Nuclear TheoryHigh Energy Physics::Phenomenology91.2Jet ProductionE+ E- --> CHGD-HADRONS XDSIG/DXInclusiveSingle Differential Cross SectionE+ E- --> 3JETE+ E- ScatteringExclusiveHigh Energy Physics::ExperimentNuclear Experiment
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"Table 4" of "Investigation of the splitting of quark and gluon jets."

1998

Scaled energy distribution of charged hadrons produced in Gluon jets in 'Mercedes' topology 3-JET events.

Astrophysics::High Energy Astrophysical PhenomenaE+ E- --> Z0Nuclear TheoryHigh Energy Physics::Phenomenology91.2Jet ProductionE+ E- --> CHGD-HADRONS XDSIG/DXInclusiveSingle Differential Cross SectionE+ E- --> 3JETE+ E- ScatteringExclusiveHigh Energy Physics::ExperimentNuclear Experiment
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"Table 11" of "Searches for supersymmetry with the ATLAS detector using final states with two leptons and missing transverse momentum in sqrt{s} = 7 …

2011

The missing-mass ET distribution for opposite-sign dilepton events before any jet requirement.

Astrophysics::High Energy Astrophysical PhenomenaHigh Energy Physics::PhenomenologyNuclear TheorySUSY7000.0Single Differential DistributionJet ProductionInclusiveProton-Proton ScatteringP P --> LEPTON+ LEPTON- JETS XDN/DETHigh Energy Physics::ExperimentSupersymmetryNuclear ExperimentDrell Yan
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Analysis of a strong wildfire event over Valencia (Spain) during Summer 2012 – Part 1: Aerosol microphysics and optical properties

2013

Abstract. The most intense wildfire experienced in Eastern Spain since 2004 happened in Valencia during summer 2012. Although the fire was mostly active during days 29–30 June, a longer temporal period (from 24 June to 4 July) was selected for this analysis. Column-integrated, vertical resolved and surface aerosol observations were performed continuously at the Burjassot station throughout the studied period. The aerosol optical depth at 500 nm shows values larger than 2 for the most intense part of the wildfire and an extremely high maximum of 8 was detected on 29 June. The simultaneous increase of the Ångström exponent was also observed, indicating the important contribution of small part…

AtmosphereAngstrom exponentMicrophysicsSingle-scattering albedoMie scatteringClimatologyParticleEnvironmental scienceParticulatesAtmospheric sciencesAerosol
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2017

Abstract. Size-resolved and vertical profile measurements of single particle chemical composition (sampling altitude range 50–3000 m) were conducted in July 2014 in the Canadian high Arctic during an aircraft-based measurement campaign (NETCARE 2014). We deployed the single particle laser ablation aerosol mass spectrometer ALABAMA (vacuum aerodynamic diameter range approximately 200–1000 nm) to identify different particle types and their mixing states. On the basis of the single particle analysis, we found that a significant fraction (23 %) of all analyzed particles (in total: 7412) contained trimethylamine (TMA). Two main pieces of evidence suggest that these TMA-containing particles origi…

Atmospheric Science010504 meteorology & atmospheric sciencesChemistryLevoglucosanSingle particle analysis010501 environmental sciencesParticulatesAtmospheric sciences01 natural sciencesAerosolchemistry.chemical_compoundArctic13. Climate actionParticleChemical compositionAir mass0105 earth and related environmental sciencesAtmospheric Chemistry and Physics
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Factors for inconsistent aerosol single scattering albedo between SKYNET and AERONET

2016

SKYNET and Aerosol Robotic Network (AERONET) retrieved aerosol single scattering albedo (SSA) values of four sites, Chiba (Japan), Pune (India), Valencia (Spain), and Seoul (Korea), were compared to understand the factors behind often noted large SSA differences between them. SKYNET and AERONET algorithms are found to produce nearly same SSAs for similarity in input data, suggesting that SSA differences between them are primarily due to quality of input data due to different calibration and/or observation protocols as well as difference in quality assurance criteria. The most plausible reason for high SSAs in SKYNET is found to be underestimated calibration constant for sky radiance (ΔΩ). T…

Atmospheric Science010504 meteorology & atmospheric sciencesMeteorologySingle-scattering albedomedia_common.quotation_subjectSKYNETAlbedo01 natural sciencesAERONETAerosol010309 opticsGeophysicsIntegrating sphereSpace and Planetary ScienceSky0103 physical sciencesEarth and Planetary Sciences (miscellaneous)RadianceEnvironmental science0105 earth and related environmental sciencesRemote sensingmedia_commonJournal of Geophysical Research: Atmospheres
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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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Black and brown carbon over central Amazonia: long-term aerosol measurements at the ATTO site

2018

The Amazon rainforest is a sensitive ecosystem experiencing the combined pressures of progressing deforestation and climate change. Its atmospheric conditions oscillate between biogenic and biomass burning (BB) dominated states. The Amazon further represents one of the few remaining continental places where the atmosphere approaches pristine conditions during occasional wet season episodes. The Amazon Tall Tower Observatory (ATTO) has been established in central Amazonia to investigate the complex interactions between the rainforest ecosystem and the atmosphere. Physical and chemical aerosol properties have been analyzed continuously since 2012. This paper provides an in-depth analysis of t…

Atmospheric Science010504 meteorology & atmospheric sciencesSingle-scattering albedoAmazon rainforest010501 environmental sciencesCombustionAtmospheric sciences01 natural scienceslcsh:QC1-999Aerosollcsh:ChemistryAtmospherelcsh:QD1-999Dry seasonForest ecologyEnvironmental scienceAbsorption (electromagnetic radiation)lcsh:Physics0105 earth and related environmental sciencesAtmospheric Chemistry and Physics
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Contrast in column-integrated aerosol optical properties during heating and non-heating seasons at Urumqi — Its causes and implications

2017

Abstract Aerosol optical properties were retrieved from two years' worth of Sunphotometer measurements at Urumqi, an urban station in western China. Distinct seasonal variations of aerosol optical properties were revealed. During the heating season, mean aerosol optical depth at 550 nm (τ a ), Angstrom exponent calculated from aerosol optical depth at wavelength of 440 and 870 nm (α) as well as PM 2.5 concentration were 0.58 ± 0.33, 1.11 ± 0.34 and 79.5 ± 69.6 μg m − 3 , respectively, which contrasted their counterparts during the non-heating season of 0.32 ± 0.22, 0.79 ± 0.26, and 35.0 ± 20.1 μg m − 3 . Seasonal variations of τ a and PM 2.5 at Urumqi contrasted with corresponding values in…

Atmospheric ScienceAngstrom exponent010504 meteorology & atmospheric sciencesSingle-scattering albedo010501 environmental sciencesSeasonalityAtmospheric sciencesmedicine.disease01 natural sciencesAerosolWavelengthSpectroradiometermedicineEnvironmental scienceRelative humidityAbsorption (electromagnetic radiation)0105 earth and related environmental sciencesAtmospheric Research
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Aerosol influence on radiative cooling

2011

Aerosol particles have a complex index of refraction and therefore contribute to atmospheric emission and radiative cooling rates. In this paper calculations of the longwave flux divergence within the atmosphere at different heights are presented including water vapour and aerosol particles as emitters and absorbers. The spectral region covered is 5 to 100 microns divided into 23 spectral intervals. The relevant properties of the aerosol particles, the single scattering albedo and the extinction coefficient, were first calculated by Mie-theory and later by an approximation formula with a complex index of refraction given by Volz. The particle growth with relative humidity is also incorporat…

Atmospheric ScienceAngstrom exponentMaterials science010504 meteorology & atmospheric sciencesRadiative coolingSingle-scattering albedoLongwaveGeneral MedicineOceanographyAtmospheric sciences01 natural sciencesAerosolParticleRelative humidityWater vaporPhysics::Atmospheric and Oceanic Physics0105 earth and related environmental sciencesTellus A
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