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@ARTICLE{Ebert:821064,
author = {Ebert, Martin and Weigel, Ralf and Kandler, Konrad and
Günther, Gebhard and Molleker, Sergej and Grooß, Jens-Uwe
and Vogel, Bärbel and Weinbruch, Stephan and Borrmann,
Stephan},
title = {{C}hemical analysis of refractory stratospheric aerosol
particles collected within the arctic vortex and inside
polar stratospheric clouds},
journal = {Atmospheric chemistry and physics},
volume = {16},
number = {13},
issn = {1680-7324},
address = {Katlenburg-Lindau},
publisher = {EGU},
reportid = {FZJ-2016-06308},
pages = {8405 - 8421},
year = {2016},
abstract = {Stratospheric aerosol particles with diameters larger than
about 10 nm were collected within the arctic vortex during
two polar flight campaigns: RECONCILE in winter 2010 and
ESSenCe in winter 2011. Impactors were installed on board
the aircraft M-55 Geophysica, which was operated from
Kiruna, Sweden. Flights were performed at a height of up to
21 km and some of the particle samples were taken within
distinct polar stratospheric clouds (PSCs). The chemical
composition, size and morphology of refractory particles
were analyzed by scanning electron microscopy and
energy-dispersive X-ray microanalysis. During ESSenCe no
refractory particles with diameters above 500 nm were
sampled. In total 116 small silicate, Fe-rich, Pb-rich and
aluminum oxide spheres were found. In contrast to ESSenCe in
early winter, during the late-winter RECONCILE mission the
air masses were subsiding inside the Arctic winter vortex
from the upper stratosphere and mesosphere, thus
initializing a transport of refractory aerosol particles
into the lower stratosphere. During RECONCILE, 759
refractory particles with diameters above 500 nm were
found consisting of silicates, silicate ∕ carbon
mixtures, Fe-rich particles, Ca-rich particles and complex
metal mixtures. In the size range below 500 nm the
presence of soot was also proven. While the data base is
still sparse, the general tendency of a lower abundance of
refractory particles during PSC events compared to non-PSC
situations was observed. The detection of large refractory
particles in the stratosphere, as well as the experimental
finding that these particles were not observed in the
particle samples (upper size limit ∼ 5 µm) taken
during PSC events, strengthens the hypothesis that such
particles are present in the lower polar stratosphere in
late winter and have provided a surface for heterogeneous
nucleation during PSC formation.},
cin = {IEK-7},
ddc = {550},
cid = {I:(DE-Juel1)IEK-7-20101013},
pnm = {244 - Composition and dynamics of the upper troposphere and
middle atmosphere (POF3-244)},
pid = {G:(DE-HGF)POF3-244},
typ = {PUB:(DE-HGF)16},
UT = {WOS:000381091400022},
doi = {10.5194/acp-16-8405-2016},
url = {https://juser.fz-juelich.de/record/821064},
}