% 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{Field:59801,
      author       = {Field, P. R. and Möhler, O. and Connolly, P. and Krämer,
                      M. and Cotton, R. and Heymsfield, A. J. and Schnaiter, M.
                      and Saathoff, H.},
      title        = {{S}ome ice nucleation characteristics of {A}sian and
                      {S}aharan desert dust},
      journal      = {Atmospheric chemistry and physics},
      volume       = {6},
      issn         = {1680-7316},
      address      = {Katlenburg-Lindau},
      publisher    = {EGU},
      reportid     = {PreJuSER-59801},
      pages        = {2991 - 3006},
      year         = {2006},
      note         = {Record converted from VDB: 12.11.2012},
      abstract     = {The large (7m x 4m cylinder, 84 m(3)) AIDA ( Aerosol
                      Interactions and Dynamics in the Atmosphere) cloud chamber
                      facility at Forschungszentrum, Karlsruhe, Germany was used
                      to test the ice nucleating ability of two desert dust
                      samples from the Sahara and Asia. Aerosol samples were
                      lognormally distributed with a mode diameter of 0.4(+/- 0.1)
                      mu m and geometric standard deviation of similar to 1.7(+/-
                      0.2). At temperatures warmer than -40 degrees C droplets
                      were formed before ice crystals formed and there was
                      generally no deposition nucleation observed. At temperatures
                      colder than -40 degrees C both dust samples exhibited dual
                      nucleation events that were observed during the same
                      expansion experiment. The primary nucleation event occurred
                      at ice saturation ratios of 1.1 to 1.3 and is likely to be a
                      deposition nucleation mode. The secondary nucleation event
                      occurred at ice saturation ratios between 1.35 and 1.5. We
                      cannot categorically determine whether this ice nucleation
                      event is via a further deposition mode or a condensation
                      mode, but the presence of some soluble material in the dust
                      samples leads us to favour the latter process. The activated
                      fractions of desert dust ranged from similar to $5-10\%$ at
                      -20 degrees C to $20-40\%$ at temperatures colder than -40
                      degrees C. There was no obvious difference between the
                      nucleation behaviour of the two dust samples.},
      keywords     = {J (WoSType)},
      cin          = {ICG-1},
      ddc          = {550},
      cid          = {I:(DE-Juel1)VDB790},
      pnm          = {Atmosphäre und Klima},
      pid          = {G:(DE-Juel1)FUEK406},
      shelfmark    = {Meteorology $\&$ Atmospheric Sciences},
      typ          = {PUB:(DE-HGF)16},
      UT           = {WOS:000239176200001},
      doi          = {10.5194/acp-6-2991-2006},
      url          = {https://juser.fz-juelich.de/record/59801},
}