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000001577 0247_ $$2DOI$$a10.1088/1748-9326/3/3/035003
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000001577 084__ $$2WoS$$aEnvironmental Sciences
000001577 084__ $$2WoS$$aMeteorology & Atmospheric Sciences
000001577 1001_ $$0P:(DE-Juel1)6110$$aGensch, I.$$b0$$uFZJ
000001577 245__ $$aSupersaturations, Microphysics and Nitric Acid Partitioning in a Cold Cirrus observed during CR-AVE 2006:An Observation-Modeling Intercomparison Study
000001577 260__ $$aBristol$$bIOP Publ.$$c2008
000001577 300__ $$a035003
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000001577 440_0 $$018901$$aEnvironmental Research Letters$$v3$$x1748-9326
000001577 500__ $$aWe 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.
000001577 520__ $$aSupersaturations, microphysics and nitric acid partitioning in a very cold subvisible tropical cirrus cloud observed on 2 February 2006, during the field campaign CR-AVE, are studied by comparing a simulated set of possible cloud development scenarios with the in situ observations. The scenario that best matches the observations is a cirrus cloud forming by heterogeneous freezing of a small number of ice nuclei with subsequent unimpeded mass accommodation of water on ice. Variation of the freezing process, the accommodation coefficient or the amount of available water leads to simulated clouds that differ microphysically from the observed cloud in important respects. In particular, the simulations suggest that heterogeneous ice nucleation or another freezing mechanism producing only a low number of ice crystals could be an important process for cold cirrus cloud formation, possibly explaining the frequent observations of high supersaturations inside the cirrus cloud in this temperature regime.
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000001577 65320 $$2Author$$asupersaturations
000001577 65320 $$2Author$$anitric acid
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000001577 7001_ $$0P:(DE-HGF)0$$aBunz, H.$$b1
000001577 7001_ $$0P:(DE-HGF)0$$aBaumgardner, D.$$b2
000001577 7001_ $$0P:(DE-HGF)0$$aChristensen, L. E.$$b3
000001577 7001_ $$0P:(DE-HGF)0$$aFahey, D. W.$$b4
000001577 7001_ $$0P:(DE-HGF)0$$aHermann, R. L.$$b5
000001577 7001_ $$0P:(DE-HGF)0$$aLawson, P.$$b6
000001577 7001_ $$0P:(DE-HGF)0$$aPopp, P.$$b7
000001577 7001_ $$0P:(DE-HGF)0$$aSmith, J. B.$$b8
000001577 7001_ $$0P:(DE-HGF)0$$aWebster, C. R.$$b9
000001577 7001_ $$0P:(DE-HGF)0$$aWeinstock, E. M.$$b10
000001577 7001_ $$0P:(DE-HGF)0$$aWilson, J. C.$$b11
000001577 7001_ $$0P:(DE-HGF)0$$aPeter, T.$$b12
000001577 7001_ $$0P:(DE-Juel1)129131$$aKrämer, M.$$b13$$uFZJ
000001577 773__ $$0PERI:(DE-600)2255379-4$$a10.1088/1748-9326/3/3/035003$$gVol. 3, p. 035003$$p035003$$q3<035003$$tEnvironmental research letters$$v3$$x1748-9326$$y2008
000001577 8567_ $$uhttp://dx.doi.org/10.1088/1748-9326/3/3/035003
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