% 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{Riese:155640,
      author       = {Riese, M. and Oelhaf, H. and Preusse, P. and Blank, J. and
                      Ern, M. and Friedl-Vallon, F. and Fischer, H. and
                      Guggenmoser, T. and Höpfner, M. and Hoor, P. and Kaufmann,
                      M. and Orphal, J. and Ploeger, Felix and Spang, R. and
                      Suminska-Ebersoldt, O. and Ungermann, J. and Vogel, B. and
                      Woiwode, W.},
      title        = {{G}imballed {L}imb {O}bserver for {R}adiance {I}maging of
                      the {A}tmosphere ({GLORIA}) scientific objectives},
      journal      = {Atmospheric measurement techniques discussions},
      volume       = {7},
      number       = {2},
      issn         = {1867-8610},
      address      = {Katlenburg-Lindau},
      publisher    = {Copernicus},
      reportid     = {FZJ-2014-04697},
      pages        = {1535 - 1572},
      year         = {2014},
      abstract     = {The upper troposphere/lower stratosphere (UTLS) plays a
                      crucial role in the climate system. Changes in the
                      composition and dynamic structure of this atmospheric region
                      result in particularly large changes in the atmospheric
                      radiation balance. Quantifying the physical and chemical
                      processes that control UTLS composition therefore represents
                      an important task. Currently, there is a lack of UTLS
                      observations with sufficient three-dimensional resolution.
                      The Gimballed Limb Observer for Radiance Imaging of the
                      Atmosphere (GLORIA) aircraft instrument addresses this
                      observational lack by providing observations of numerous
                      trace constituents as well as temperature and cloud
                      structures with an unprecedented combination of vertical
                      resolution (up to 300 m) and horizontal resolution (up to 20
                      km × 20 km). As a result, important scientific questions
                      concerning stratosphere–troposphere-exchange, the
                      occurrence of subvisible cirrus clouds in the lowermost
                      stratosphere (LMS), polar chemistry and gravity wave
                      processes can be addressed, as reviewed in this paper.},
      cin          = {IEK-7},
      ddc          = {550},
      cid          = {I:(DE-Juel1)IEK-7-20101013},
      pnm          = {234 - Composition and Dynamics of the Upper Troposphere and
                      Stratosphere (POF2-234)},
      pid          = {G:(DE-HGF)POF2-234},
      typ          = {PUB:(DE-HGF)16},
      doi          = {10.5194/amtd-7-1535-2014},
      url          = {https://juser.fz-juelich.de/record/155640},
}