0000000000380753

AUTHOR

Sergey Khaykin

showing 2 related works from this author

Enhancements of the refractory submicron aerosol fraction in the Arctic polar vortex: feature or exception ?

2014

In situ measurements with a four-channel stratospheric condensation particle counter (CPC) were conducted at up to 20 km altitude on board the aircraft M-55 Geophysica from Kiruna, Sweden, in January through March (EUPLEX 2003, RECONCILE 2010) and in December (ESSenCe 2011). During all campaigns air masses from the upper stratosphere and mesosphere were subsiding inside the Arctic winter vortex, thus initializing a transport of refractory aerosol into the lower stratosphere (Θ 3 were generally detected. Up to 8 of these 11 particles per cm3 were found to contain thermo-stable (at 250 °C) residuals with diameters of 10 nm to about 1 μm. Particle mixing ratios (150 mg−1) and fractions of non-…

[PHYS.PHYS.PHYS-AO-PH]Physics [physics]/Physics [physics]/Atmospheric and Oceanic Physics [physics.ao-ph]Atmospheric Science010504 meteorology & atmospheric sciencesAtmospheric sciences010502 geochemistry & geophysics01 natural sciencesCondensation particle counterlcsh:QC1-999AerosolVortexMesospherelcsh:ChemistryAltitudelcsh:QD1-999Polar vortex13. Climate actionClimatology0103 physical sciencesddc:550Environmental science010303 astronomy & astrophysicsStratosphereRefractory (planetary science)lcsh:Physics0105 earth and related environmental sciences
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Convective hydration in the tropical tropopause layer during the StratoClim aircraft campaign: pathway of an observed hydration patch

2018

The source and pathway of the hydration patch in the TTL (tropical tropopause layer) that was measured during the Stratospheric and upper tropospheric processes for better climate predictions (StratoClim) field campaign during the Asian summer monsoon in 2017 and its connection to convective overshoots are investigated. During flight no. 7, two remarkable layers are measured in the TTL, namely (1) the moist layer (ML) with a water vapour content of 4.8–5.7 ppmv in altitudes of 18–19 km in the lower stratosphere and (2) the ice layer (IL) with ice content up to 1.9 eq. ppmv (equivalent parts per million by volume) in altitudes of 17–18 km in the upper tropo…

[PHYS.PHYS.PHYS-AO-PH]Physics [physics]/Physics [physics]/Atmospheric and Oceanic Physics [physics.ao-ph][SDU.OCEAN]Sciences of the Universe [physics]/Ocean AtmosphereAtmospheric ScienceTurbulent diffusion010504 meteorology & atmospheric sciencesCloud top0208 environmental biotechnology02 engineering and technologyAtmospheric sciences01 natural scienceslcsh:QC1-999020801 environmental engineeringTropospherelcsh:ChemistryDeposition (aerosol physics)lcsh:QD1-99913. Climate actionIce nucleusEnvironmental scienceStratosphereWater vaporAir masslcsh:Physics0105 earth and related environmental sciences
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