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@PHDTHESIS{Rhode:1020915,
      author       = {Rhode, Sebastian},
      title        = {{M}odeling orographic gravity waves from source to
                      termination to improve parameterization schemes in climate
                      models},
      school       = {Bergische Universität Wuppertal},
      type         = {Dissertation},
      reportid     = {FZJ-2024-00391},
      pages        = {156},
      year         = {2023},
      note         = {Dissertation, Bergische Universität Wuppertal, 2023},
      abstract     = {Gravity waves (GWs) are one of the most important drivers
                      of middle atmospheric circulationsand strongly affect the
                      polar vortex of the winter hemisphere. These waves are
                      ofcomparatively small horizontal scales and are generated by
                      a multitude of processes, of whichwind flow over orography
                      and convection are the most common. The resolution of
                      today’sclimate models is, however, too coarse for
                      resolving GWs explicitly; therefore, they need tobe
                      parameterized within long-term climate projections. These
                      parameterizations are a firstapproximation of the GW’s
                      effect on the atmosphere. A technical shortcoming common
                      toparameterization schemes is their vertical column-wise
                      application without the possibilityof horizontal
                      communication between adjacent grid cells due to
                      computation-cost intensity.Hence, parametrization schemes do
                      not account for the horizontal propagation of GWs,
                      eventhough many studies show the far propagation of gravity
                      waves (and especially mountainwaves, MWs) from their
                      sources. This horizontal propagation transports the
                      momentumcarried by the orographic GWs away from regions of
                      high orographic variability; therebyspreading the effect of
                      the orography on the atmosphere dynamics. Studies attribute
                      highvariability and model biases in the southern hemisphere
                      to this lack of this horizontal propagationof 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)11},
      doi          = {10.34734/FZJ-2024-00391},
      url          = {https://juser.fz-juelich.de/record/1020915},
}