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@ARTICLE{Schiller:58068,
author = {Schiller, C. and Krämer, M. and Afchine, A. and Spelten,
N. and Sitnikov, N.},
title = {{I}ce water content of {A}rctic, midlatitude, and tropical
cirrus},
journal = {Journal of Geophysical Research},
volume = {113},
issn = {0148-0227},
address = {Washington, DC},
publisher = {Union},
reportid = {PreJuSER-58068},
pages = {D24208},
year = {2008},
note = {We would like to thank R. Bauer, J. Beuermann, M. Blasner,
O. Bujok, N. Eicke, A. Mangold, S. Rohs, S. Schlicht, G.
Shur, F. H. Silva dos Santos, A. Schonfeld, V. Tan, and M.
Zoger who were involved in the experimental work during the
different campaigns, as well as the aircraft teams of DLR
Oberpfaffenhofen, GfD Hohn, enviscope Frankfurt, and MDB
Moscow and the coordinators of the different field
experiments. Funding for the campaigns was granted by the
BMBF within the Ozonforschungsprogramm and the program
"Angewandte Klima- und Atmospharenforschung,'' by the EU DG
XII within Framework Programmes 5 and 6, and by ESA within
the ENVISAT validation program. Water vapor measurement by
FLASH and data preparation was supported by the Russian
Foundation for Basic Research grants 06-05-64165-a and
07-05-00486-a.},
abstract = {In situ measurements of total water have been obtained
during several airborne field experiments in the Arctic
(POLSTAR 1997 and 1998; EUPLEX/ENVISAT 2003), at
midlatitudes (ENVISAT 2002, Cirrus 2003 and 2004, TROCCINOX
2005), and in the tropics (APE-THESEO 1999,
TROCCINOX/ENVISAT 2005, SCOUT-O3 2005) in 52 flights in
cirrus using the Julich Lyman-alpha fluorescence hygrometer
FISH. For a subset of 28 flights, the measurements are
complemented by gas phase measurements of H2O. From the data
set obtained in these experiments, the ice water content
(IWC) in cirrus clouds is derived using two different
approaches and functions of the minimum, mean, median, and
maximum IWC are provided. The data are analyzed as a
function of temperature in the range 183-250 K for Arctic,
midlatitudinal, and tropical regions thus extending previous
climatologies to much lower temperatures and lower
detectable IWC. For each temperature, IWC covers a broad
band, decreasing with temperature over the whole temperature
range. In the tropics, several events of enhanced ice water
content are observed which are related to recent impact of
convection.},
keywords = {J (WoSType)},
cin = {ICG-1},
ddc = {550},
cid = {I:(DE-Juel1)VDB790},
pnm = {Atmosphäre und Klima},
pid = {G:(DE-Juel1)FUEK406},
shelfmark = {Meteorology $\&$ Atmospheric Sciences},
typ = {PUB:(DE-HGF)16},
UT = {WOS:000262041500002},
doi = {10.1029/2008JD010342},
url = {https://juser.fz-juelich.de/record/58068},
}