% 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{Vogel:47474,
      author       = {Vogel, B. and Müller, R. and Engel, A. and Grooß, J.-U.
                      and Toohey, D. and Woyke, Th. and Stroh, F.},
      title        = {{M}idlatitude {C}l{O} during the maximum atmospheric
                      chlorine burden: {I}n situ balloon measurments and model
                      simulations},
      journal      = {Atmospheric chemistry and physics},
      volume       = {5},
      issn         = {1680-7316},
      address      = {Katlenburg-Lindau},
      publisher    = {EGU},
      reportid     = {PreJuSER-47474},
      pages        = {1623 - 1638},
      year         = {2005},
      note         = {Record converted from VDB: 12.11.2012},
      abstract     = {Chlorine monoxide (ClO) plays a key role in stratospheric
                      ozone loss processes at midlatitudes. We present two
                      balloon-borne in situ measurements of ClO conducted in
                      northern hemisphere midlatitudes during the period of the
                      maximum of total inorganic chlorine loading in the
                      atmosphere. Both ClO measurements were conducted on board
                      the TRIPLE balloon payload, launched in November 1996 in
                      Leon, Spain, and in May 1999 in Aire sur l'Adour, France.
                      For both flights a ClO daylight and night-time vertical
                      profile was derived over an altitude range of approximately
                      15 - 35 km. ClO mixing ratios are compared to model
                      simulations performed with the photochemical box model
                      version of the Chemical Lagrangian Model of the Stratosphere
                      (CLaMS). Simulations along 24-hour backward trajectories
                      were performed to study the diurnal variation of ClO in the
                      midlatitude lower stratosphere. Model simulations for the
                      flight launched in Aire sur l'Adour 1999 show an excellent
                      agreement with the ClO measurements. For the flight launched
                      in Leon 1996, an overall good agreement is found, whereas
                      the flight is characterized by a more complex dynamical
                      situation due to a possible mixture of vortex and non-vortex
                      air. We note that for both flights at solar zenith angles
                      greater than 86 degrees - 87 degrees simulated ClO mixing
                      ratios are higher than observed ClO mixing ratios. However,
                      the present findings indicate that no substantial
                      uncertainties exist in midlatitude chlorine chemistry of the
                      stratosphere.},
      keywords     = {J (WoSType)},
      cin          = {ICG-I},
      ddc          = {550},
      cid          = {I:(DE-Juel1)VDB47},
      pnm          = {Chemie und Dynamik der Geo-Biosphäre},
      pid          = {G:(DE-Juel1)FUEK257},
      shelfmark    = {Meteorology $\&$ Atmospheric Sciences},
      typ          = {PUB:(DE-HGF)16},
      UT           = {WOS:000230113400001},
      url          = {https://juser.fz-juelich.de/record/47474},
}