Search results for "Spur"

showing 10 items of 110 documents

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
researchProduct

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
researchProduct

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
researchProduct

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
researchProduct

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
researchProduct

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
researchProduct

Evidence for heterogeneous chlorine activation in the tropical UTLS

2011

Airborne in-situ observations of ClO in the tropics were made during the TROCCINOX (Aracatuba, Brazil, February 2005) and SCOUT-O<sub>3</sub> (Darwin, Australia, November/December 2005) field campaigns. While during most flights significant amounts of ClO (≈10–20 parts per trillion, ppt) were present only in aged stratospheric air, instances of enhanced ClO mixing ratios of up to 40 ppt – significantly exceeding those expected from gas phase chemistry – were observed in air masses of a more tropospheric character. Most of these observations are associated with low temperatures or with the presence of cirrus clouds (often both), suggesting that cirrus ice particles and/or liquid …

Atmospheric Scienceairborne in-situ observationChemistrychemistry.chemical_elementAtmosphärische SpurenstoffeAtmospheric sciencesNitrogenlcsh:QC1-999JGas phaseAerosollcsh:ChemistryTropospherelcsh:QD1-999ddc:550ChlorineLife ScienceCirrusStratospherelcsh:Physics
researchProduct

Characterization of the inter-annual, seasonal, and diurnal variations of condensation particle concentrations at Neumayer, Antarctica

2011

Continuous condensation particle (CP) observations were conducted from 1984 through 2009 at Neumayer Station under stringent contamination control. During this period, the CP concentration (median 258 cm<sup>−3</sup>) showed no significant long term trend but exhibited a pronounced seasonality characterized by a stepwise increase starting in September and reaching its annual maximum of around 10<sup>3</sup> cm<sup>−3</sup> in March. Minimum values below 10<sup>2</sup> cm<sup>–3</sup> were observed during June/July. Dedicated time series analyses in the time and frequency domain revealed no significant correlations between…

Atmospheric Sciencefood.ingredient010504 meteorology & atmospheric sciencesAtmospheric circulationaerosolnon-volatile particles010501 environmental sciencesAtmospheric sciences01 natural scienceslcsh:ChemistryfoodUltrafine particlecondensation particlesmedicine14. Life underwater0105 earth and related environmental sciencesVulcanian eruptionSea saltCondensationAtmosphärische SpurenstoffeNeumayerSeasonalitymedicine.diseaselcsh:QC1-999Aerosollcsh:QD1-99913. Climate actionClimatologyEnvironmental scienceParticlelcsh:PhysicsAtmospheric Chemistry and Physics
researchProduct

Porous aerosol in degassing plumes of Mt. Etna and Mt. Stromboli

2016

Abstract. Aerosols of the volcanic degassing plumes from Mt. Etna and Mt. Stromboli were probed with in situ instruments on board the Deutsches Zentrum für Luft- und Raumfahrt research aircraft Falcon during the contrail, volcano, and cirrus experiment CONCERT in September 2011. Aerosol properties were analyzed using angular scattering intensities and particle size distributions simultaneously measured with the Polar Nephelometer and the Forward Scattering Spectrometer probes (FSSP series 100 and 300), respectively. Aerosols of degassing plumes are characterized by low values of the asymmetry parameter (between 0.6 and 0.75); the effective diameter was within the range of 1.5–2.8 µm and the…

Atmospheric Scienceporosity010504 meteorology & atmospheric sciences010502 geochemistry & geophysicsAtmospheric sciences01 natural scienceslcsh:ChemistryImpact craterLife Science0105 earth and related environmental sciences[PHYS.PHYS.PHYS-AO-PH]Physics [physics]/Physics [physics]/Atmospheric and Oceanic Physics [physics.ao-ph][SDU.OCEAN]Sciences of the Universe [physics]/Ocean Atmospheregeographygeography.geographical_feature_categoryNephelometerScatteringAtmosphärische Spurenstoffelcsh:QC1-999PlumeAerosolVolcanolcsh:QD1-999CirrusParticle size/dk/atira/pure/subjectarea/asjc/1900/1902volcanic aerosolGeologylcsh:Physics
researchProduct

Size distribution, mass concentration, chemical and mineralogical composition and derived optical parameters of the boundary layer aerosol at Tinfou,…

2009

During the SAMUM 2006 field campaign in southern Morocco, physical and chemical properties of desert aerosols were measured. Mass concentrations ranging from 30 Ã�¼g m-3 for PM2.5 under desert background conditions up to 300,000 Ã�¼g m-3 for total suspended particles (TSP) during moderate dust storms were measured. TSP dust concentrations are correlated with the local wind speed, whereas PM10 and PM2.5 concentrations are determined by advection from distant sources. Size distributions were measured for particles between 20 nm and 500 Ã�¼m diameter (parameterizations are given). Two major regimes of the size spectrum can be distinguished. Smaller than 500 nm particle diameter, the distrib…

Atmospheric Sciencerefractive index010504 meteorology & atmospheric sciencesaerosolAtmosphärische SpurenstoffeMineralogySingle particle analysis010501 environmental sciencesMineral dust01 natural sciencesAerosolSAMUMParticle-size distributionUltrafine particlechemical compositionsingle-particle analysisParticleMass concentration (chemistry)Chemical compositionGeology0105 earth and related environmental sciencesTellus B: Chemical and Physical Meteorology
researchProduct