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@ARTICLE{Tilmes:47476,
      author       = {Tilmes, S. and Müller, R. and Grooß, J.-U. and Spang, R.
                      and Sugitta, T. and Nakajima, H. and Sasano, Y.},
      title        = {{C}hemical ozone loss and related processes in the
                      {A}ntarctic winter 2003 based on {ILAS}-{II} observations},
      journal      = {Journal of Geophysical Research},
      volume       = {111},
      issn         = {0148-0227},
      address      = {Washington, DC},
      publisher    = {Union},
      reportid     = {PreJuSER-47476},
      pages        = {D11S12},
      year         = {2006},
      note         = {Record converted from VDB: 12.11.2012},
      abstract     = {In this study, ILAS-II (Improved Limb Atmospheric
                      Spectrometer) measurements were used to analyze chemical
                      ozone loss during the entire Antarctic winter 2003, using
                      the tracer-tracer correlation technique. The temporal
                      evolution of both the accumulated local chemical ozone loss
                      and the loss in column ozone in the lower stratosphere is in
                      step with increasing solar illumination. Half of the entire
                      loss in column ozone of 157 DU occurred during September
                      2003. By the end of September 2003, almost the total amount
                      of ozone was destroyed between 380 and 470 K. Further, ozone
                      loss rates increased strongly during September for the
                      entire lower stratosphere. The values of accumulated ozone
                      loss and ozone loss rates are strongly dependent on
                      altitude. Once ozone loss is saturated during September,
                      especially at latitudes between 380 and 420 K, ozone loss
                      rates decrease, and accumulated ozone loss can no longer
                      increase. Moreover, at altitudes above 470 K, accumulated
                      ozone loss depends on the amount of PSCs occurring during
                      winter and spring. During September, ozone mixing ratios
                      show a large day to day variation. Box model simulations by
                      the Chemical Lagrangian Model of the Stratosphere (CLaMS)
                      show that this is a result of the different histories of the
                      observed air masses. Further, the box model supports the
                      general evolution of ozone loss values during September as a
                      result of the strong increase of halogen catalyzed ozone
                      destruction.},
      keywords     = {J (WoSType)},
      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:000237447400001},
      doi          = {10.1029/2005JD006260},
      url          = {https://juser.fz-juelich.de/record/47476},
}