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@ARTICLE{Khosrawi:44376,
      author       = {Khosrawi, F. and Müller, R. and Beuermann, J. and Konopka,
                      Paul and Schiller, C.},
      title        = {{D}ehydration in the {N}orthern {H}emisphere midlatitudes
                      during {STREAM} 1998: {T}racer-tracer correlations and model
                      studies},
      journal      = {Tellus / B},
      volume       = {58},
      issn         = {0280-6509},
      address      = {Oxford [u.a.]},
      publisher    = {Wiley-Blackwell},
      reportid     = {PreJuSER-44376},
      pages        = {206 - 207},
      year         = {2006},
      note         = {Record converted from VDB: 12.11.2012},
      abstract     = {Measurements in the vicinity of the polar jet stream during
                      the STREAM 1998 campaign in Timmins, Canada, show that
                      during the flight on 15 July, a deep intrusion of
                      stratospheric air into the troposphere occurred. At the edge
                      of the deep intrusion dehydration was observed. The
                      dehydration can be identified in tracer–tracer
                      correlations of H2O and O3 and by the comparison of these
                      correlations with correlations of H2O and O3 derived from
                      two other flights of the STREAM 1998 campaign. Trajectories,
                      calculated backwards for 10 days starting at each point of
                      the measurement for the flight on 15 July, show that the
                      saturation ratios required for homogeneous freezing are
                      reached. However, box model simulations along the
                      trajectories indicate no substantial growth of H2SO4/H2O
                      particles due to H2O uptake. Since ice nuclei were not
                      measured during the campaign, it cannot be precisely
                      determined which freezing process, heterogeneous or
                      homogeneous, is responsible for the formation of the ice
                      particles. Most likely, both processes were involved in the
                      formation of ice particles that led to the observed
                      dehydration on 15 July 1998.},
      cin          = {ICG-I},
      ddc          = {550},
      cid          = {I:(DE-Juel1)VDB47},
      pnm          = {Atmosphäre und Klima},
      pid          = {G:(DE-Juel1)FUEK406},
      shelfmark    = {Meteorology $\&$ Atmospheric Sciences},
      typ          = {PUB:(DE-HGF)16},
      UT           = {WOS:000238842500005},
      doi          = {10.1111/j.1600-0889.2006.00182.x},
      url          = {https://juser.fz-juelich.de/record/44376},
}