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@ARTICLE{Kbbeler:17013,
author = {Kübbeler, M. and Hildebrandt, M. and Meyer, J. and
Schiller, C. and Hamburger, Th. and Jurkat, T. and Minikin,
A. and Petzold, A. and Rautenhaus, M. and Schlager, H. and
Schumann, U. and Voigt, C. and Spichtinger, J.-F. and Gayet,
C. and Gourbeyre, C. and Krämer, M.},
title = {{T}hin and subvisible cirrus and contrails in a
subsaturated environment},
journal = {Atmospheric chemistry and physics},
volume = {11},
issn = {1680-7316},
address = {Katlenburg-Lindau},
publisher = {EGU},
reportid = {PreJuSER-17013},
pages = {5853 - 5865},
year = {2011},
note = {We greatly acknowledge Andreas Dornbrack for excellent
analysis of the meteorological situation during CONCERT,
Klaus Gierens for fruitful discussions about contrail
formation and development and Dominik Schauble for great
assistance with the campaign. Thanks are given to Eric
Jensen who provides computer code to calculate contrail
thermodynamics. Further, we thank the Falcon team operating
the aircraft for their support and the DLR flight department
for providing the meteorological parameters, as well as the
Deutsche Flugsicherung (DFS) and the Deutsche Lufthansa for
excellent help during the campaign. The CONCERT campaign was
organized by the Junior research group AEROTROP and in part
financed by the DLR project CATS (Climate optimized air
traffic system).},
abstract = {The frequency of occurrence of cirrus clouds and contrails,
their life time, ice crystal size spectra and thus their
radiative properties depend strongly on the ambient
distribution of the relative humidity with respect to ice
(RHice). Ice clouds do not form below a certain
supersaturation and both cirrus and contrails need at least
saturation conditions to persist over a longer period. Under
subsaturated conditions, cirrus and contrails should
dissipate. During the mid-latitude aircraft experiment
CONCERT 2008 (CONtrail and Cirrus ExpeRimenT), RHice and ice
crystals were measured in cirrus and contrails. Here, we
present results from 2.3/1.7 h of observation in
cirrus/contrails during 6 flights. Thin and subvisible
cirrus with contrails embedded therein have been detected
frequently in a subsaturated environment. Nevertheless, ice
crystals up to radii of 50 mu m and larger, but with low
number densities were often observed inside the contrails as
well as in the cirrus. Analysis of the meteorological
situation indicates that the crystals in the contrails were
entrained from the thin/subvisible cirrus clouds, which
emerged in frontal systems with low updrafts. From model
simulations of cirrus evaporation times it follows that such
thin/subvisible cirrus can exist for time periods of a
couple of hours and longer in a subsaturated environment and
thus may represent a considerable part of the cirrus
coverage.},
keywords = {J (WoSType)},
cin = {IEK-7},
ddc = {550},
cid = {I:(DE-Juel1)IEK-7-20101013},
pnm = {Atmosphäre und Klima},
pid = {G:(DE-Juel1)FUEK491},
shelfmark = {Meteorology $\&$ Atmospheric Sciences},
typ = {PUB:(DE-HGF)16},
UT = {WOS:000291939800019},
doi = {10.5194/acp-11-5853-2011},
url = {https://juser.fz-juelich.de/record/17013},
}