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@PHDTHESIS{Rhode:1024910,
      author       = {Rhode, Sebastian},
      title        = {{M}odeling orographic gravity waves from source to
                      termination to improve parameterization schemes in climate
                      models},
      volume       = {627},
      school       = {Univ. Wuppertal},
      type         = {Dissertation},
      address      = {Jülich},
      publisher    = {Forschungszentrum Jülich GmbH Zentralbibliothek, Verlag},
      reportid     = {FZJ-2024-02560},
      isbn         = {978-3-95806-750-9},
      series       = {Schriften des Forschungszentrums Jülich Reihe Energie $\&$
                      Umwelt / Energy $\&$ Environment},
      pages        = {xii, ii, 138},
      year         = {2024},
      note         = {Dissertation, Univ. Wuppertal, 2023},
      abstract     = {Gravity waves (GWs) are one of the most important drivers
                      of middle atmospheric circulations and strongly affect the
                      polar vortex of the winter hemisphere. These waves are of
                      comparatively small horizontal scales and are generated by a
                      multitude of processes, of which wind flow over orography
                      and convection are the most common. The resolution of
                      today’s climate models is, however, too coarse for
                      resolving GWs explicitly; therefore, they need to be
                      parameterized within long-term climate projections. These
                      parameterizations are a first approximation of the GW’s
                      effect on the atmosphere. A technical shortcoming common to
                      parameterization schemes is their vertical column-wise
                      application without the possibility of horizontal
                      communication between adjacent grid cells due to
                      computation-cost intensity. Hence, parametrization schemes
                      do not account for the horizontal propagation of GWs, even
                      though many studies show the far propagation of gravity
                      waves (and especially mountain waves, MWs) from their
                      sources. This horizontal propagation transports the momentum
                      carried by the orographic GWs away from regions of high
                      orographic variability; thereby spreading the effect of the
                      orography on the atmosphere dynamics. Studies attribute
                      highvariability and model biases in the southern hemisphere
                      to this lack of horizontal propagation of mountain waves
                      within climate models.},
      cin          = {IEK-7},
      cid          = {I:(DE-Juel1)IEK-7-20101013},
      pnm          = {2112 - Climate Feedbacks (POF4-211)},
      pid          = {G:(DE-HGF)POF4-2112},
      typ          = {PUB:(DE-HGF)3 / PUB:(DE-HGF)11},
      urn          = {urn:nbn:de:0001-20240516100449746-1117656-7},
      doi          = {10.34734/FZJ-2024-02560},
      url          = {https://juser.fz-juelich.de/record/1024910},
}