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|a 10.1088/1748-9326/3/3/035003
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|a WOS:000259569300012
037 _ _ |a PreJuSER-1577
041 _ _ |a eng
082 _ _ |a 690
084 _ _ |2 WoS
|a Environmental Sciences
084 _ _ |2 WoS
|a Meteorology & Atmospheric Sciences
100 1 _ |0 P:(DE-Juel1)6110
|a Gensch, I.
|b 0
|u FZJ
245 _ _ |a Supersaturations, Microphysics and Nitric Acid Partitioning in a Cold Cirrus observed during CR-AVE 2006:An Observation-Modeling Intercomparison Study
260 _ _ |a Bristol
|b IOP Publ.
|c 2008
300 _ _ |a 035003
336 7 _ |a Journal Article
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336 7 _ |a article
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440 _ 0 |0 18901
|a Environmental Research Letters
|v 3
|x 1748-9326
500 _ _ |a We thank the scientific team of CR-AVE for providing the data. ECMWF provided the meteorological operational analyses. We thank the CLaMS-team of ICG-1, and especially Rolf P Muller, Forschungszentrum Julich, for support and useful discussions. We gratefully acknowledge Peter Spichtinger, ETH Zurich, for fruitful discussions and suggestions. This work was partly supported by the EU within SCOUT-O3 and by the Swiss National Foundation (SNF). Work performed at the Jet Propulsion Laboratory, California Institute of Technology, was done under contract with NASA.
520 _ _ |a Supersaturations, microphysics and nitric acid partitioning in a very cold subvisible tropical cirrus cloud observed on 2 February 2006, during the field campaign CR-AVE, are studied by comparing a simulated set of possible cloud development scenarios with the in situ observations. The scenario that best matches the observations is a cirrus cloud forming by heterogeneous freezing of a small number of ice nuclei with subsequent unimpeded mass accommodation of water on ice. Variation of the freezing process, the accommodation coefficient or the amount of available water leads to simulated clouds that differ microphysically from the observed cloud in important respects. In particular, the simulations suggest that heterogeneous ice nucleation or another freezing mechanism producing only a low number of ice crystals could be an important process for cold cirrus cloud formation, possibly explaining the frequent observations of high supersaturations inside the cirrus cloud in this temperature regime.
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653 2 0 |2 Author
|a cirrus clouds
653 2 0 |2 Author
|a supersaturations
653 2 0 |2 Author
|a nitric acid
700 1 _ |0 P:(DE-HGF)0
|a Bunz, H.
|b 1
700 1 _ |0 P:(DE-HGF)0
|a Baumgardner, D.
|b 2
700 1 _ |0 P:(DE-HGF)0
|a Christensen, L. E.
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700 1 _ |0 P:(DE-HGF)0
|a Fahey, D. W.
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700 1 _ |0 P:(DE-HGF)0
|a Hermann, R. L.
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700 1 _ |0 P:(DE-HGF)0
|a Lawson, P.
|b 6
700 1 _ |0 P:(DE-HGF)0
|a Popp, P.
|b 7
700 1 _ |0 P:(DE-HGF)0
|a Smith, J. B.
|b 8
700 1 _ |0 P:(DE-HGF)0
|a Webster, C. R.
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700 1 _ |0 P:(DE-HGF)0
|a Weinstock, E. M.
|b 10
700 1 _ |0 P:(DE-HGF)0
|a Wilson, J. C.
|b 11
700 1 _ |0 P:(DE-HGF)0
|a Peter, T.
|b 12
700 1 _ |0 P:(DE-Juel1)129131
|a Krämer, M.
|b 13
|u FZJ
773 _ _ |0 PERI:(DE-600)2255379-4
|a 10.1088/1748-9326/3/3/035003
|g Vol. 3, p. 035003
|p 035003
|q 3<035003
|t Environmental research letters
|v 3
|x 1748-9326
|y 2008
856 7 _ |u http://dx.doi.org/10.1088/1748-9326/3/3/035003
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