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@ARTICLE{Gensch:1577,
      author       = {Gensch, I. and Bunz, H. and Baumgardner, D. and
                      Christensen, L. E. and Fahey, D. W. and Hermann, R. L. and
                      Lawson, P. and Popp, P. and Smith, J. B. and Webster, C. R.
                      and Weinstock, E. M. and Wilson, J. C. and Peter, T. and
                      Krämer, M.},
      title        = {{S}upersaturations, {M}icrophysics and {N}itric {A}cid
                      {P}artitioning in a {C}old {C}irrus observed during
                      {CR}-{AVE} 2006:{A}n {O}bservation-{M}odeling
                      {I}ntercomparison {S}tudy},
      journal      = {Environmental research letters},
      volume       = {3},
      issn         = {1748-9326},
      address      = {Bristol},
      publisher    = {IOP Publ.},
      reportid     = {PreJuSER-1577},
      pages        = {035003},
      year         = {2008},
      note         = {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.},
      abstract     = {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.},
      keywords     = {J (WoSType)},
      cin          = {ICG-1},
      ddc          = {690},
      cid          = {I:(DE-Juel1)VDB790},
      pnm          = {Atmosphäre und Klima},
      pid          = {G:(DE-Juel1)FUEK406},
      shelfmark    = {Environmental Sciences / Meteorology $\&$ Atmospheric
                      Sciences},
      typ          = {PUB:(DE-HGF)16},
      UT           = {WOS:000259569300012},
      doi          = {10.1088/1748-9326/3/3/035003},
      url          = {https://juser.fz-juelich.de/record/1577},
}