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@ARTICLE{Wolf:859798,
author = {Wolf, Veronika and Kuhn, Thomas and Milz, Mathias and
Voelger, Peter and Krämer, Martina and Rolf, Christian},
title = {{A}rctic ice clouds over northern {S}weden: microphysical
properties studied with the {B}alloon-borne {I}ce {C}loud
particle {I}mager {B}-{ICI}244},
journal = {Atmospheric chemistry and physics},
volume = {18},
number = {23},
issn = {1680-7324},
address = {Katlenburg-Lindau},
publisher = {EGU},
reportid = {FZJ-2019-00629},
pages = {17371 - 17386},
year = {2018},
abstract = {Ice particle and cloud properties such as particle size,
particle shape and number concentration influence the net
radiation effect of cirrus clouds. Measurements of these
features are of great interest for the improvement of
weather and climate models, especially for the Arctic
region. In this study, balloon-borne in situ measurements of
Arctic cirrus clouds have been analysed for the first time
with respect to their origin. Eight cirrus cloud
measurements have been carried out in Kiruna (68∘ N),
Sweden, using the Balloon-borne Ice Cloud particle Imager
(B-ICI). Ice particle diameters between 10 and 1200 µm
have been found and the shape could be recognized from
20 µm upwards. Great variability in particle size and
shape is observed. This cannot simply be explained by local
environmental conditions. However, if sorted by cirrus
origin, wind and weather conditions, the observed
differences can be assessed. Number concentrations between 3
and 400 L−1 have been measured, but the number
concentration has reached values above 100 L−1 only for
two cases. These two cirrus clouds are of in situ origin and
have been associated with waves. For all other measurements,
the maximum ice particle concentration is below 50 L−1
and for one in situ origin cirrus case only 3 L−1. In
the case of in situ origin clouds, the particles are all
smaller than 350 µm diameter. The PSDs for liquid origin
clouds are much broader with particle sizes between 10 and
1200 µm. Furthermore, it is striking that in the case of
in situ origin clouds almost all particles are compact
$(61 \%)$ or irregular $(25 \%)$ when examining the
particle shape. In liquid origin clouds, on the other hand,
most particles are irregular $(48 \%),$ rosettes
$(25 \%)$ or columnar $(14 \%).$ There are hardly any
plates in cirrus regardless of their origin. It is also
noticeable that in the case of liquid origin clouds the
rosettes and columnar particles are almost all hollow.},
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:000452384100002},
doi = {10.5194/acp-18-17371-2018},
url = {https://juser.fz-juelich.de/record/859798},
}