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@BOOK{Lehmann:136231,
      author       = {Lehmann, Catrin},
      title        = {{A}bleitung von atomarem {S}auerstoff und {W}asserstoff aus
                      {S}atellitendaten und deren {A}bhängigkeit vom solaren
                      {Z}yklus},
      volume       = {77},
      school       = {Universität Wuppertal},
      type         = {Dr.},
      address      = {Jülich},
      publisher    = {Forschungszentrum Jülich GmbH Zentralbibliothek, Verlag},
      reportid     = {PreJuSER-136231},
      isbn         = {978-3-89336-649-1},
      series       = {Schriften des Forschungszentrums Jülich. Reihe Energie und
                      Umwelt / Energy und Environment},
      pages        = {X, IV, 127 S.},
      year         = {2010},
      note         = {Record converted from JUWEL: 18.07.2013; Univ. Wuppertal,
                      Diss., 2010},
      abstract     = {Man-made climate change causes the global mean surface
                      temperature to rise. However, climate change also effects
                      the upper altitudes of the Earth’s atmosphere. Due to the
                      low air density and due to the efficient infrared radiation
                      cooling to space, temperature trends and other signals of
                      climate change are much more pronounced in the mesosphere
                      than at the ground. This work deals with the analysis and
                      interpretation of the emissions of excited hydroxyl radicals
                      (OH$^{∗}$), measured by SCIAMACHY (Scanning Imaging
                      Absorption Spectrometer for Atmospheric CHartographY).
                      SCIAMACHY is one of the ten instruments aboard ESA’s
                      Envisat Environmental Satellite) launched in March 2002. In
                      the upper mesosphere/ lower thermosphere excited OH∗ is
                      produced by oxygen-hydrogen-reactions. Between 83 and 95 km
                      altitude the reaction of ozone and atomic hydrogen, which
                      produces OH$^[∗]$, is the most important heat source. The
                      heating efficiency of the atmosphere in this region is
                      directly proportional to the measured emission by
                      OH$^{∗}$. In this work chemical heating rate, as well as
                      concentrations of atomic hydrogen and atomic oxygen are
                      derived from the measurements. The determination of atomic
                      hydrogen requires ozone measurements. These are provided by
                      GOMOS (Global Ozone Monitoring by Occultation of Stars),
                      which is another experiment aboard Envisat. The analysis
                      required the development of a complex non-LTE model, which
                      takes into account all production and loss mechanism of the
                      various vibrational states [...]},
      keywords     = {Dissertation (GND)},
      cin          = {ICG / ICG-1},
      ddc          = {500},
      cid          = {I:(DE-Juel1)VDB1109 / I:(DE-Juel1)VDB169},
      shelfmark    = {UMB - Atmospheric chemistry / UMB - Atmosphärische Chemie},
      typ          = {PUB:(DE-HGF)3 / PUB:(DE-HGF)11},
      url          = {https://juser.fz-juelich.de/record/136231},
}