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@ARTICLE{Riese:155628,
      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 Plöger, F. 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},
      volume       = {7},
      number       = {7},
      issn         = {1867-8548},
      address      = {Katlenburg-Lindau},
      publisher    = {Copernicus},
      reportid     = {FZJ-2014-04686},
      pages        = {1915 - 1928},
      year         = {2014},
      abstract     = {The upper troposphere/lower stratosphere (UTLS) represents
                      an important part of the climate system. Even small changes
                      in the composition and dynamic structure of this region have
                      significant radiative effects. Quantifying the underlying
                      physical and chemical processes therefore represents a
                      crucial 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 (about 30
                      km × 30 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},
      UT           = {WOS:000339937200001},
      doi          = {10.5194/amt-7-1915-2014},
      url          = {https://juser.fz-juelich.de/record/155628},
}