0000000000602209

AUTHOR

C. Voigt

showing 10 related works from this author

The impact of mineral dust on cloud formation during the Saharan dust event in April 2014 over Europe

2018

A regional modeling study on the impact of desert dust on cloud formation is presented for a major Saharan dust outbreak over Europe from 2 to 5 April 2014. The dust event coincided with an extensive and dense cirrus cloud layer, suggesting an influence of dust on atmospheric ice nucleation. Using interactive simulation with the regional dust model COSMO-MUSCAT, we investigate cloud and precipitation representation in the model and test the sensitivity of cloud parameters to dust–cloud and dust–radiation interactions of the simulated dust plume. We evaluate model results with ground-based and spaceborne remote sensing measurements of aerosol and cloud properties, as well as the in situ meas…

lcsh:Chemistrylcsh:QD1-999lcsh:Physicslcsh:QC1-999Atmospheric Chemistry and Physics
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The ABCflux database: Arctic–boreal CO2 flux observations and ancillary information aggregated to monthly time steps across terrestrial ecosystems

2022

Past efforts to synthesize and quantify the magnitude and change in carbon dioxide (CO2) fluxes in terrestrial ecosystems across the rapidly warming Arctic–boreal zone (ABZ) have provided valuable information but were limited in their geographical and temporal coverage. Furthermore, these efforts have been based on data aggregated over varying time periods, often with only minimal site ancillary data, thus limiting their potential to be used in large-scale carbon budget assessments. To bridge these gaps, we developed a standardized monthly database of Arctic–boreal CO2 fluxes (ABCflux) that aggregates in situ measurements of terrestrial net ecosystem CO2 exchange and its derived partitioned…

Environmental sciencesQE1-996.5GE1-350GeologyEarth System Science Data
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Chlorine partitioning in the lowermost Arctic vortex during the cold winter 2015/2016

2019

Activated chlorine compounds in the polar winter stratosphere drive catalytic cycles that deplete ozone and methane, whose abundances are highly relevant to the evolution of global climate. The present work introduces a novel dataset of in situ measurements of relevant chlorine species in the lowermost Arctic stratosphere from the aircraft mission POLSTRACC–GW-LCYCLE–SALSA during winter 2015/2016. The major stages of chemical evolution of the lower polar vortex are presented in a consistent series of high-resolution mass spectrometric observations of HCl and ClONO2. Simultaneous measurements of CFC-12 are used to derive total inorganic chlorine (Cly) and active chlorine (ClOx). The new data…

lcsh:Chemistrylcsh:QD1-999lcsh:Physicslcsh:QC1-999Atmospheric Chemistry and Physics
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Aerosol responses to precipitation along North American air trajectories arriving at Bermuda

2021

North American pollution outflow is ubiquitous over the western North Atlantic Ocean, especially in winter, making this location a suitable natural laboratory for investigating the impact of precipitation on aerosol particles along air mass trajectories. We take advantage of observational data collected at Bermuda to seasonally assess the sensitivity of aerosol mass concentrations and volume size distributions to accumulated precipitation along trajectories (APT). The mass concentration of particulate matter with aerodynamic diameter less than 2.5 µm normalized by the enhancement of carbon monoxide above background (PM2.5/ΔCO) at Bermuda was used to estimate the degree of aerosol loss durin…

Atmospheric Sciencecloud droplet number concentrationfood.ingredient010504 meteorology & atmospheric sciencesaerosolQC1-999010501 environmental sciencesAtmospheric sciences01 natural sciencesArticlefoodcloudMass concentration (chemistry)14. Life underwaterPrecipitationQD1-999ScavengingAir masslow clouds0105 earth and related environmental sciencesPhysicsSea saltParticulatesAerosolAERONETChemistry13. Climate actionEnvironmental scienceAtmospheric Chemistry and Physics
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Aircraft-based observations of isoprene-epoxydiol-derived secondary organic aerosol (IEPOX-SOA) in the tropical upper troposphere over the Amazon reg…

2018

During the ACRIDICON-CHUVA field project (September–October 2014; based in Manaus, Brazil) aircraft-based in situ measurements of aerosol chemical composition were conducted in the tropical troposphere over the Amazon using the High Altitude and Long Range Research Aircraft (HALO), covering altitudes from the boundary layer (BL) height up to 14.4 km. The submicron non-refractory aerosol was characterized by flash-vaporization/electron impact-ionization aerosol particle mass spectrometry. The results show that significant secondary organic aerosol (SOA) formation by isoprene oxidation products occurs in the upper troposphere (UT), leading to increased organic aerosol mass concentratio…

Atmospheric Science010504 meteorology & atmospheric sciences010501 environmental sciencesMass spectrometry01 natural sciencesTropospherelcsh:Chemistrychemistry.chemical_compoundAltitudeNitrateddc:550WolkenphysikAerosolNOxIsoprene0105 earth and related environmental sciencesaerosol chemical compositionisoprene oxidationAtmosphärische SpurenstoffeACRIDICON15. Life on landOberpfaffenhofenlcsh:QC1-999Aerosolchemistrylcsh:QD1-99913. Climate actionEnvironmental chemistryHALOMass spectrumEnvironmental sciencesecondary organic aerosol (SOA)lcsh:PhysicsAtmospheric Chemistry and Physics
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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
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Aerosol influences on low-level clouds in the West African monsoon

2019

Abstract. Low-level clouds (LLC) cover a wide area of southern West Africa (SWA) during the summer monsoon months, and have an important cooling effect on the regional climate. Previous studies of these clouds have focused on modelling and remote sensing via satellite. We present the first comprehensive set of regional, in situ measurements of cloud microphysics, taken during June – July 2016, as part of the DACCIWA (Dynamics-Aerosol-Chemistry-Clouds Interactions in West Africa) campaign, assessing spatial and temporal variation in the properties of these clouds. LLC developed overnight and mean cloud cover peaked a few hundred kilometres inland around 10:00 local solar time (LST), before c…

Atmospheric Science010504 meteorology & atmospheric sciencesCloud coverPopulationclouds[SDU.STU.ME]Sciences of the Universe [physics]/Earth Sciences/Meteorology010502 geochemistry & geophysicsMonsoonAtmospheric sciences01 natural sciencescomplex mixtureslcsh:Chemistrylow level cloudsddc:550Cloud condensation nuclei1902WolkenphysikeducationSouthern Hemisphere0105 earth and related environmental sciencesOrographic lifteducation.field_of_studyaerosol effectmicropyhsicslcsh:QC1-999AerosolEarth scienceslcsh:QD1-99913. Climate action[SDU.STU.CL]Sciences of the Universe [physics]/Earth Sciences/ClimatologySolar timeEnvironmental sciencesense organs/dk/atira/pure/subjectarea/asjc/1900/1902lcsh:Physics
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Aerosol characteristics and particle production in the upper troposphere over the Amazon Basin

2018

Airborne observations over the Amazon Basin showed high aerosol particle concentrations in the upper troposphere (UT) between 8 and 15 km altitude, with number densities (normalized to standard temperature and pressure) often exceeding those in the planetary boundary layer (PBL) by 1 or 2 orders of magnitude. The measurements were made during the German–Brazilian cooperative aircraft campaign ACRIDICON–CHUVA, where ACRIDICON stands for Aerosol, Cloud, Precipitation, and Radiation Interactions and Dynamics of Convective Cloud Systems and CHUVA is the acronym for Cloud Processes of the Main Precipitation Systems in Brazil: A Contribution to Cloud Resolving Modeling and to the GPM …

ConvectionAtmospheric ScienceMeteorology010504 meteorology & atmospheric sciences0207 environmental engineeringparticle production02 engineering and technology010501 environmental sciencesAtmospheric sciences01 natural sciencesAtmosphereTropospherelcsh:Chemistryddc:550PrecipitationWolkenphysik020701 environmental engineeringAerosol0105 earth and related environmental sciencesChemistryCondensationAtmosphärische Spurenstoffelcsh:QC1-999AerosolTrace gasEarth scienceslcsh:QD1-99913. Climate actionupper troposphereParticlelcsh:Physics
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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

2013

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 core-shell pa…

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The ABCflux database: Arctic-boreal CO2flux observations and ancillary information aggregated to monthly time steps across terrestrial ecosystems

2022

Past efforts to synthesize and quantify the magnitude and change in carbon dioxide (CO2) fluxes in terrestrial ecosystems across the rapidly warming Arctic–boreal zone (ABZ) have provided valuable information but were limited in their geographical and temporal coverage. Furthermore, these efforts have been based on data aggregated over varying time periods, often with only minimal site ancillary data, thus limiting their potential to be used in large-scale carbon budget assessments. To bridge these gaps, we developed a standardized monthly database of Arctic–boreal CO2 fluxes (ABCflux) that aggregates in situ measurements of terrestrial net ecosystem CO2 exchange and its derived partitioned…

hiilidioksidiarktinen aluemaaperäClimate ResearchEDDY COVARIANCE TECHNIQUECARBON-DIOXIDE EXCHANGESPATIAL VARIABILITYkausivaihtelutFOREST114 Physical sciencesPERMAFROST CARBONPhysical Geography and Environmental GeoscienceTUNDRAAtmospheric SciencesNETkasvihuonekaasutGeochemistryRESPIRATION/dk/atira/pure/sustainabledevelopmentgoals/climate_actionMeteorology and Atmospheric SciencesSDG 13 - Climate ActionSTOCKSpäästöttutkimusaineistoCHAMBEREarth System Science Data
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