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@ARTICLE{Haenel:906526,
      author       = {Haenel, Florian and Woiwode, Wolfgang and Buchmüller,
                      Jennifer and Friedl-Vallon, Felix and Höpfner, Michael and
                      Johansson, Sören and Khosrawi, Farahnaz and Kirner, Oliver
                      and Kleinert, Anne and Oelhaf, Hermann and Orphal, Johannes
                      and Ruhnke, Roland and Sinnhuber, Björn-Martin and
                      Ungermann, Jörn and Weimer, Michael and Braesicke, Peter},
      title        = {{C}hallenge of modelling {GLORIA} observations of upper
                      troposphere–lowermost stratosphere trace gas and cloud
                      distributions at high latitudes: a case study with
                      state-of-the-art models},
      journal      = {Atmospheric chemistry and physics},
      volume       = {22},
      number       = {4},
      issn         = {1680-7316},
      address      = {Katlenburg-Lindau},
      publisher    = {EGU},
      reportid     = {FZJ-2022-01496},
      pages        = {2843 - 2870},
      year         = {2022},
      abstract     = {Water vapour and ozone are important for the thermal and
                      radiative balance of the upper troposphere (UT) and
                      lowermost stratosphere (LMS). Both species are modulated by
                      transport processes. Chemical and microphysical processes
                      affect them differently. Thus, representing the different
                      processes and their interactions is a challenging task for
                      dynamical cores, chemical modules and microphysical
                      parameterisations of state-of-the-art atmospheric model
                      components. To test and improve the models, high-resolution
                      measurements of the UT–LMS are required. Here, we use
                      measurements taken in a flight of the GLORIA (Gimballed Limb
                      Observer for Radiance Imaging of the Atmosphere) instrument
                      on HALO (High Altitude and LOng Range Research Aircraft).
                      The German research aircraft HALO performed a research
                      flight on 26 February 2016 that covered deeply subsided air
                      masses of the aged 2015/16 Arctic vortex, high-latitude LMS
                      air masses, a highly textured region affected by
                      troposphere-to-stratosphere exchange and high-altitude
                      cirrus clouds. Therefore, it provides a challenging
                      multifaceted case study for comparing GLORIA observations
                      with state-of-the-art atmospheric model simulations in a
                      complex UT–LMS region at a late stage of the Arctic winter
                      2015/16.},
      cin          = {IEK-7},
      ddc          = {550},
      cid          = {I:(DE-Juel1)IEK-7-20101013},
      pnm          = {2112 - Climate Feedbacks (POF4-211) / 2A3 - Remote Sensing
                      (CARF - CCA) (POF4-2A3)},
      pid          = {G:(DE-HGF)POF4-2112 / G:(DE-HGF)POF4-2A3},
      typ          = {PUB:(DE-HGF)16},
      UT           = {WOS:000765724400001},
      doi          = {10.5194/acp-22-2843-2022},
      url          = {https://juser.fz-juelich.de/record/906526},
}