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Christoph Zülicke, Erich Becker, Vivien Matthias, Dieter H. W. Peters, Hauke Schmidt, Han-Li Liu, Laura de la Torre Ramos, and Daniel M. Mitchell

circulation by GWs is considered in order to derive a relation between temperature anomalies and the GW phase speed. According to Holton (1982) the zonal-mean residual circulation is driven by the zonal GW pseudomomentum flux (GWF) divergence The induced residual meridional circulation enforces a certain vertical motion through the continuity equation From the thermodynamic equation, which is modeled as a radiative relaxation to an equilibrium temperature T e , the dynamically forced temperature is

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