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@ARTICLE{Tilmes:1627,
      author       = {Tilmes, S. and Müller, R. and Salawitch, R. J. and
                      Schmidt, U. and Webster, C. R. and Oelhaf, H. and
                      Camy-Peyret, C.C. and Russell III, J. M.},
      title        = {{C}hemical ozone loss in the {A}rctic winter 1991-1992},
      journal      = {Atmospheric chemistry and physics},
      volume       = {8},
      issn         = {1680-7316},
      address      = {Katlenburg-Lindau},
      publisher    = {EGU},
      reportid     = {PreJuSER-1627},
      pages        = {1897 - 1910},
      year         = {2008},
      note         = {Record converted from VDB: 12.11.2012},
      abstract     = {Chemical ozone loss in winter 1991-1992 is recalculated
                      based on observations of the HALOE satellite instrument,
                      Version 19, ER-2 aircraft measurements and balloon data.
                      HALOE satellite observations are shown to be reliable in the
                      lower stratosphere below 400 K, at altitudes where the
                      measurements are most likely disturbed by the enhanced
                      sulfate aerosol loading, as a result of the Mt. Pinatubo
                      eruption in June 1991. Significant chemical ozone loss ( 13
                      17 DU) is observed below 380K from Kiruna balloon
                      observations and HALOE satellite data between December 1991
                      and March 1992. For the two winters after the Mt. Pinatubo
                      eruption, HALOE satellite observations show a stronger
                      extent of chemical ozone loss towards lower altitudes
                      compared to other Arctic winters between 1991 and 2003. In
                      spite of already occurring deactivation of chlorine in March
                      1992, MIPAS-B and LPMA balloon observations indicate that
                      chlorine was still activated at lower altitudes, consistent
                      with observed chemical ozone loss occurring between February
                      and March and April. Large chemical ozone loss of more than
                      70 DU in the Arctic winter 1991-1992 as calculated in
                      earlier studies is corroborated here.},
      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:000254960800002},
      url          = {https://juser.fz-juelich.de/record/1627},
}