about
Secondary organic aerosols from anthropogenic and biogenic precursors.Revising the hygroscopicity of inorganic sea salt particles.Ice residual properties in mixed-phase clouds at the high-alpine Jungfraujoch site.Collocated observations of cloud condensation nuclei, particle size distributions, and chemical composition.Water uptake of clay and desert dust aerosol particles at sub- and supersaturated water vapor conditions.The role of low-volatility organic compounds in initial particle growth in the atmosphere.New particle formation in the free troposphere: A question of chemistry and timing.The influence of small aerosol particles on the properties of water and ice clouds.Aqueous phase oxidation of sulphur dioxide by ozone in cloud dropletsEvolution of particle composition in CLOUD nucleation experimentsRecent increase in black carbon concentrations from a Mt. Everest ice core spanning 1860-2000 ADHygroscopic properties of submicrometer atmospheric aerosol particles measured with H-TDMA instruments in various environments—a reviewA synthesis of cloud condensation nuclei counter (CCNC) measurements within the EUCAARI networkEvaluation of the absorption Ångström exponents for traffic and wood burning in the Aethalometer-based source apportionment using radiocarbon measurements of ambient aerosolEUCAARI ion spectrometer measurements at 12 European sites – analysis of new particle formation eventsMobility particle size spectrometers: harmonization of technical standards and data structure to facilitate high quality long-term observations of atmospheric particle number size distributionsGround-based and airborne in-situ measurements of the Eyjafjallajökull volcanic aerosol plume in Switzerland in spring 2010Hygroscopic growth and water uptake kinetics of two-phase aerosol particles consisting of ammonium sulfate, adipic and humic acid mixturesMass spectrometry of refractory black carbon particles from six sources: carbon-cluster and oxygenated ionsHygroscopic properties of fresh and aged wood burning particlesSubarctic atmospheric aerosol composition: 2. Hygroscopic growth propertiesIn situ determination of atmospheric aerosol composition as a function of hygroscopic growthBlack carbon physical properties and mixing state in the European megacity ParisThe Pagami Creek smoke plume after long-range transport to the upper troposphere over Europe – aerosol properties and black carbon mixing stateCCN activity and volatility of β-caryophyllene secondary organic aerosolVolatility and hygroscopicity of aging secondary organic aerosol in a smog chamberCloud forming potential of secondary organic aerosol under near atmospheric conditionsSingle particle characterization of black carbon aerosols at a tropospheric alpine site in SwitzerlandCloud droplet activation properties and scavenged fraction of black carbon in liquid-phase clouds at the high-alpine research station Jungfraujoch (3580 m a.s.l.)Droplet activation behaviour of atmospheric black carbon particles in fog as a function of their size and mixing stateWidening the gap between measurement and modelling of secondary organic aerosol properties?Inversion of tandem differential mobility analyser (TDMA) measurementsA modified hygroscopic tandem DMA and a data retrieval method based on optimal estimationOptimized method for black carbon analysis in ice and snow using the Single Particle Soot PhotometerSeasonal and elevational variations of black carbon and dust in snow and ice in the Solu-Khumbu, Nepal and estimated radiative forcingsHygroscopicity of aerosol particles at low temperatures. 1. New low-temperature H-TDMA instrument: setup and first applicationsHygroscopicity of aerosol particles at low temperatures. 2. Theoretical and experimental hygroscopic properties of laboratory generated aerosols
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description
researcher
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researcher
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հետազոտող
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name
Martin Gysel
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Martin Gysel
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Martin Gysel
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Martin Gysel
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Martin Gysel
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Martin Gysel
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Martin Gysel
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Martin Gysel
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Martin Gysel
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Martin Gysel
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Martin Gysel
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Martin Gysel
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Martin Gysel
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Martin Gysel
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Martin Gysel
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Martin Gysel
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Martin Gysel
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Martin Gysel
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P106
P31
P496
0000-0002-7453-1264