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@ARTICLE{Fernandez:7701,
      author       = {Fernandez, R.P. and Kaufmann, M. and Toselli, B.M.},
      title        = {{R}elative importance of ozone energy transfer processes in
                      the middle and upper atmosphere},
      journal      = {Journal of atmospheric and solar-terrestrial physics},
      volume       = {71},
      issn         = {1364-6826},
      address      = {Amsterdam [u.a.]},
      publisher    = {Elsevier Science},
      reportid     = {PreJuSER-7701},
      year         = {2009},
      note         = {The authors would like to thank CONICET and SeCyT (UNC) for
                      partial support for this work and B. Funke for fruitful
                      discussions. R.P Fernandez thanks CONICET for a graduate
                      fellowship and DAAD for a research fellowship at Juelich
                      Research Center, Germany. B.M. Toselli thanks Prof. John
                      Barker for providing the original version of the SSH code
                      and for helpful discussions. We also thank an anonymous
                      reviewer for his/her corrections, suggestions and
                      constructive comments.},
      abstract     = {The relative importance of different processes and
                      transitions in the appearance of non-LTE populations for the
                      fundamental levels of ozone was studied by quantifying the
                      kinetic law of every process and transition that affect each
                      level population. The vibrational temperatures and the
                      relative contribution of every transition are presented as a
                      function of altitude. The results show that the appearance
                      of non-LTE Populations for the fundamental levels is not
                      produced by a direct imbalance between absorption and
                      emission but as a consequence of imbalanced collisional
                      transitions provoked by the overpopulation of O-3(0 nu(2) 0)
                      levels. This fact confirms that the relaxation cascade
                      drives through the bending mode nu(2). (C) 2009 Elsevier
                      Ltd. All rights reserved.},
      keywords     = {J (WoSType)},
      cin          = {ICG-1},
      ddc          = {530},
      cid          = {I:(DE-Juel1)VDB790},
      pnm          = {Atmosphäre und Klima},
      pid          = {G:(DE-Juel1)FUEK406},
      shelfmark    = {Geochemistry $\&$ Geophysics / Meteorology $\&$ Atmospheric
                      Sciences},
      typ          = {PUB:(DE-HGF)16},
      UT           = {WOS:000267572600003},
      doi          = {10.1016/j.jastp.2009.03.004},
      url          = {https://juser.fz-juelich.de/record/7701},
}