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@ARTICLE{Gisinger:836825,
      author       = {Gisinger, Sonja and Dörnbrack, Andreas and Matthias,
                      Vivien and Doyle, James D. and Eckermann, Stephen D. and
                      Ehard, Benedikt and Hoffmann, Lars and Kaifler, Bernd and
                      Kruse, Christopher G. and Rapp, Markus},
      title        = {{A}tmospheric {C}onditions during the {D}eep {P}ropagating
                      {G}ravity {W}ave {E}xperiment ({DEEPWAVE})},
      journal      = {Monthly weather review},
      volume       = {145},
      issn         = {1520-0493},
      address      = {Washington, DC [u.a.]},
      publisher    = {AMS87486},
      reportid     = {FZJ-2017-05867},
      pages        = {MWR-D-16-0435.1},
      year         = {2017},
      abstract     = {This paper describes results of a comprehensive analysis of
                      the atmospheric conditions during the DEEPWAVE campaign in
                      austral winter 2014. Different datasets and diagnostics are
                      combined to characterize the background atmosphere from the
                      troposphere to the upper mesosphere. We report on how
                      weather regimes and the atmospheric state compare to
                      climatological conditions and also explore how they relate
                      to the airborne and ground-based gravity wave observations.
                      Key results of this study are the dominance of tropospheric
                      blocking situations and low-level southwesterly flows over
                      New Zealand during June, July, and August 2014. A varying
                      tropopause inversion layer was found to be connected to
                      varying vertical energy fluxes and is, therefore, an
                      important feature with respect to wave reflection. The
                      subtropical jet was frequently diverted south from its
                      climatological position at 30°S and was most often involved
                      in strong forcing events of mountain waves at the Southern
                      Alps. The polar front jet was typically responsible for
                      moderate and weak tropospheric forcing of mountain waves.
                      The stratospheric planetary wave activity amplified in July
                      leading to a displacement of the Antarctic polar vortex.
                      This reduced the stratospheric wind minimum by about 10 m
                      s-1 above New Zealand making breaking of large amplitude
                      gravity waves more likely. Satellite observations in the
                      upper stratosphere revealed that orographic gravity wave
                      variances for 2014 were largest in May, June and July, i.e.
                      the period of the DEEPWAVE field phase.},
      cin          = {JSC},
      ddc          = {550},
      cid          = {I:(DE-Juel1)JSC-20090406},
      pnm          = {511 - Computational Science and Mathematical Methods
                      (POF3-511)},
      pid          = {G:(DE-HGF)POF3-511},
      typ          = {PUB:(DE-HGF)16},
      UT           = {WOS:000412896100018},
      doi          = {10.1175/MWR-D-16-0435.1},
      url          = {https://juser.fz-juelich.de/record/836825},
}