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General overview: European Integrated project on Aerosol Cloud Climate and Air Quality interactions (EUCAARI)-integrating aerosol research from nano …

2011

In this paper we describe and summarize the main achievements of the European Aerosol Cloud Climate and Air Quality Interactions project (EUCAARI). EUCAARI started on 1 January 2007 and ended on 31 December 2010 leaving a rich legacy including: (a) a comprehensive database with a year of observations of the physical, chemical and optical properties of aerosol particles over Europe, (b) comprehensive aerosol measurements in four developing countries, (c) a database of airborne measurements of aerosols and clouds over Europe during May 2008, (d) comprehensive modeling tools to study aerosol processes fron nano to global scale and their effects on climate and air quality. In addition a new Pan…

Atmospheric ScienceEuropean aerosol010504 meteorology & atmospheric sciencesaerosolAerosol radiative forcingClimateclouds010501 environmental sciencesAtmospheric sciences01 natural scienceslcsh:Chemistry/dk/atira/pure/sustainabledevelopmentgoals/climate_actionAerosol cloud11. SustainabilitySDG 13 - Climate Actionddc:550particle propertiesEnvironmental policysaturation vapor-pressureschemical-transport modelMiljövetenskapair qualitylcsh:QC1-999General Circulation Model/dk/atira/pure/subjectarea/asjc/1900/1902EUCAARIEELS - Earth Environmental and Life SciencesION-INDUCED NUCLEATIONChemical transport modelMeteorologyEarth & EnvironmentEnergy / Geological Survey NetherlandsSIMULATION CHAMBER SAPHIRnuclei number concentrationSECONDARY ORGANIC AEROSOLpure component propertiesAir quality indexEnvironmental quality0105 earth and related environmental sciencesPARTICLE FORMATION EVENTSAtmosphärische Spurenstoffe[CHIM.CATA]Chemical Sciences/CatalysisCAS - Climate Air and Sustainability[SDE.ES]Environmental Sciences/Environmental and SocietyFalconAerosollcsh:QD1-99913. Climate actionmixed-phase cloudsEnvironmental scienceatmospheric sulfuric-acidEnvironmental Scienceslcsh:Physics
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Radio emissions from double RHESSI TGFs

2016

Abstract A detailed analysis of Reuven Ramaty High Energy Solar Spectroscopic Imager (RHESSI) terrestrial gamma ray flashes (TGFs) is performed in association with World Wide Lightning Location Network (WWLLN) sources and very low frequency (VLF) sferics recorded at Duke University. RHESSI clock offset is evaluated and found to experience changes on the 5 August 2005 and 21 October 2013, based on the analysis of TGF‐WWLLN matches. The clock offsets were found for all three periods of observations with standard deviations less than 100 μs. This result opens the possibility for the precise comparative analyses of RHESSI TGFs with the other types of data (WWLLN, radio measurements, etc.) In ca…

Atmospheric ScienceHigh energy010504 meteorology & atmospheric sciencesAtmospheric ElectricityFOS: Physical sciencesRHESSI clock offsetterrestrial gamma ray flashesAstrophysicsRadio atmospheric01 natural sciencesLightningPhysical Geography and Environmental GeoscienceAerosol and CloudsAtmospheric SciencesRemote SensingPhysics - Space Physics0103 physical sciencesEarth and Planetary Sciences (miscellaneous)Instruments and TechniquesVery low frequency010303 astronomy & astrophysicsResearch ArticlesTGF‐WWLLN match0105 earth and related environmental sciencesRadiative ProcessesPhysicsHigh Energy Astrophysical Phenomena (astro-ph.HE)Remote Sensing and DisastersGamma raymultipeak TGFsWorld wideLightningRHESSI TGFsSpace Physics (physics.space-ph)Geophysicsradio emission from TGFClock offset13. Climate actionSpace and Planetary ScienceAtmospheric ProcessesAstrophysics - High Energy Astrophysical PhenomenaNatural HazardsResearch Article
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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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The Pagami Creek smoke plume after long-range transport to the upper troposphere over Europe – aerosol properties and black carbon mixing state

2014

Abstract. During the CONCERT 2011 field experiment with the DLR research aircraft Falcon, an enhanced aerosol layer with particle linear depolarization ratios of 6–8% at 532 nm was observed at altitudes above 10 km over northeast Germany on 16 September 2011. Dispersion simulations with HYSPILT suggest that the elevated aerosol layer originated from the Pagami Creek forest fire in Minnesota, USA, which caused pyro-convective uplift of particles and gases. The 3–4 day-old smoke plume had high total refractory black carbon (rBC) mass concentrations of 0.03–0.35 μg m−3 at standard temperature and pressure (STP) with rBC mass equivalent diameter predominantly smaller than 130 nm. Assuming a cor…

Atmospheric ScienceMicrophysicsChemistryaerosolAtmosphärische Spurenstoffemedicine.disease_causeAtmospheric scienceslcsh:QC1-999SootCONCERT 2011FalconPlumeAerosollcsh:ChemistryTroposphererefractory black carbon (rBC)lcsh:QD1-999medicineRadiative transferParticleStratospherelcsh:Physics
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In-situ observations of young contrails – overview and selected results from the CONCERT campaign

2010

Lineshaped contrails were detected with the research aircraft Falcon during the CONCERT – CONtrail and Cirrus ExpeRimenT – campaign in October/November 2008. The Falcon was equipped with a set of instruments to measure the particle size distribution, shape, extinction and chemical composition as well as trace gas mixing ratios of sulfur dioxide (SO<sub>2</sub>), reactive nitrogen and halogen species (NO, NO<sub>y</sub>, HNO<sub>3</sub>, HONO, HCl), ozone (O<sub>3</sub>) and carbon monoxide (CO). During 12 mission flights over Europe, numerous contrails, cirrus clouds and a volcanic aerosol layer were probed at altitudes between 8.5 and 11.6 km…

Atmospheric ScienceOzoneMeteorologyicecirrusSO2medicine.disease_causeAtmospheric scienceslcsh:Chemistrychemistry.chemical_compoundAltitudetrace gasesddc:550medicineLife ScienceFlugabteilung OberpfaffenhofenStratosphereIce crystalsInstitut für AntriebstechnikAtmosphärische SpurenstoffecontrailSootlcsh:QC1-999JTrace gaschemistrylcsh:QD1-999Extinction (optical mineralogy)Cirruslcsh:PhysicsAtmospheric Chemistry and Physics
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Spectral Observations of Optical Emissions Associated with Terrestrial Gamma-Ray Flashes

2021

This is an open access article under the terms of the Creative Commons Attribution-NonCommercial-NoDerivs License, which permits use and distribution in any medium, provided the original work is properly cited, the use is non-commercial and no modifications or adaptations are made.

Atmospheric SciencePhoton010504 meteorology & atmospheric sciencesOptical measurementsAtmospheric Composition and StructureAstrophysics010502 geochemistry & geophysics01 natural sciences7. Clean energyCloud OpticsCloud/Radiation InteractionResearch LetterStreamer0105 earth and related environmental sciencesPhysicsScatteringPulse (signal processing)ISSResearchGamma rayAtmosphärische SpurenstoffeLightningTGFASIMGeophysicsAmplitude13. Climate actionLeaderGeneral Earth and Planetary Sciences
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Airborne measurements of dust layer properties, particle size distribution and mixing state of Saharan dust during SAMUM 2006

2009

The Saharan Mineral Dust Experiment (SAMUM) was conducted in May/June 2006 in southern Morocco. As part of SAMUM, airborne in situ measurements of the particle size distribution in the diameter range 4 nm < Dp < 100 μm were conducted. The aerosol mixing state was determined below Dp < 2.5 μm. Furthermore, the vertical structure of the dust layers was investigated with a nadir-looking high spectral resolution lidar (HSRL). The desert dust aerosol exhibited two size regimes of different mixing states: below 0.5 μm, the particles had a non-volatile core and a volatile coating; larger particles above 0.5 μm consisted of non-volatile components and contained light absorbing material. In…

Atmospheric ScienceRange (particle radiation)Materials science010504 meteorology & atmospheric sciencesgiant particlesAnalytical chemistryAtmosphärische Spurenstoffemixing state010501 environmental sciencesMineral dust01 natural sciencesAerosoldust layer structureTroposphereSAMUMdesert dustParticle-size distributionUltrafine particleParticle sizeparticle size distributionSpectral resolutionairborne measurements0105 earth and related environmental sciencesRemote sensingTellus B
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Airborne measurements of the nitric acid partitioning in persistent contrails

2009

This study reports the first systematic measurements of nitric acid (HNO3) uptake in contrail ice particles at typical aircraft cruise altitudes. During the CIRRUS-III campaign cirrus clouds and almost 40 persistent contrails were probed with in situ instruments over Germany and Northern Europe in November 2006. Besides reactive nitrogen, water vapor, cloud ice water content, ice particle size distributions, and condensation nuclei were measured during 6 flights. Contrails with ages up to 12 h were detected at altitudes 10–11.5 km and temperatures 211–220 K. These contrails had a larger ice phase fraction of total nitric acid (HNO3ice/HNO3tot = 6%) than the ambient cirrus layers (3%). On av…

Atmospheric ScienceReactive nitrogencontrailsAtmosphärische SpurenstoffecirrusAtmospheric scienceslcsh:QC1-999Plumelcsh:Chemistrychemistry.chemical_compoundlcsh:QD1-999chemistryNitric acidPhase (matter)uptakepartitioningEnvironmental scienceCloud condensation nucleiCirrusParticle sizeNitric acidaircraft measurementslcsh:PhysicsWater vapor
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Regional Saharan dust modelling during the SAMUM 2006 campaign

2011

The regional dust model system LM-MUSCAT-DES was developed in the framework of the SAMUM project. Using the unique comprehensive data set of near-source dust properties during the 2006 SAMUM field campaign, the performance of the model system is evaluated for two time periods in May and June 2006. Dust optical thicknesses, number size distributions and the position of the maximum dust extinction in the vertical profiles agree well with the observations. However, the spatio-temporal evolution of the dust plumes is not always reproduced due to inaccuracies in the dust source placement by the model. While simulated winds and dust distributions are well matched for dust events caused by dry syn…

Atmospheric ScienceSaharan dust010504 meteorology & atmospheric sciencesMeteorologyExtinction (astronomy)Air pollutionAstrophysics::Cosmology and Extragalactic Astrophysics010501 environmental sciencesMineral dustmedicine.disease_causeAtmospheric sciences01 natural sciencesTropospherePanachemedicineAstrophysics::Solar and Stellar AstrophysicsAstrophysics::Galaxy Astrophysics0105 earth and related environmental sciencesLidarAtmosphärische SpurenstoffeAerosolSAMUMLidar13. Climate actionAeolian processesEnvironmental scienceAstrophysics::Earth and Planetary AstrophysicsLM-MUSCATTellus B
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