% IMPORTANT: The following is UTF-8 encoded. This means that in the presence
% of non-ASCII characters, it will not work with BibTeX 0.99 or older.
% Instead, you should use an up-to-date BibTeX implementation like “bibtex8” or
% “biber”.
@ARTICLE{DeLeon:22462,
author = {De Leon, R.R. and Krämer, M. and Lee, D.S. and Thelen,
J.C.},
title = {{S}ensitivity of radiative properties of persistent
contrails to the ice water path},
journal = {Atmospheric chemistry and physics},
volume = {12},
issn = {1680-7316},
address = {Katlenburg-Lindau},
publisher = {EGU},
reportid = {PreJuSER-22462},
pages = {7893 - 7901},
year = {2012},
note = {This work was supported by the United Kingdom Department
for Transport. The authors wish to thank a number of people
for providing us with the data used in this study. Christine
Fromming for providing the contrail cover distribution data
calculated during the TRADEOFF project. (TRADEOFF was a
project in the European Fifth Framework Programme,
http://www.iac.ethz.ch/tradeoff/); Prof. Piers Forster for
the climatology of the monthly atmospheric composition,
cloud cover and surface albedo, and Dr. Anthony Baran for
the hexagonal prisms database. We thank our colleague, Dr
Michael Bennett for valuable discussions and his help to
improve the readability of the manuscript. We also thank two
anonymous referees and the editor for their helpful comments
and suggestions.},
abstract = {The dependence of the radiative properties of persistent
linear contrails on the variability of their ice water path
is assessed in a two-stream radiative transfer model. It is
assumed that the ice water content and the effective size of
ice crystals in aged contrails do not differ from those
observed in natural cirrus; the parameterization of these
two variables, based on a correlation with ambient
temperature derived from in situ observations, allows a more
realistic representation than the common assumption of fixed
values for the contrail optical depth and ice crystal
effective radius.The results show that the large variability
in ice water content that aged contrails may share with
natural cirrus, together with an assumed contrail vertical
thickness between 220 and 1000 m, translate into a wider
range of radiative forcings from linear contrails [1 to 66 m
Wm(-2)] than that reported in previous studies, including
IPCC's [3 to 30 m Wm(-2)]. Further field and modelling
studies of the temporal evolution of contrail properties
will thus be needed to reduce the uncertainties associated
with the values assumed in large scale contrail studies.},
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:000308753800002},
doi = {10.5194/acp-12-7893-2012},
url = {https://juser.fz-juelich.de/record/22462},
}