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- W2205320237 abstract "We find that the circulation in the middle atmosphere is significantly sensitive to the details of the OGW scheme. In particular, the vertical diffusion induced by saturation of OGWs has a considerable impact on the polar night jet during northern hemispheric winter, both by the diffusivity itself and by the secondary effect due to an upward shift of the breaking levels of NGWs. In turn, these changes affect the summer mesopause region by the interhemispheric coupling mechanism. A strong sensitivity of the mesosphere to GWs has also been found in the simulations of sudden stratospheric warmings (McLandress et al. [2012]). The damping of OGWs by boundary layer turbulence and the energy deposition by OGWs are found to be of minor importance." @default.
- W2205320237 created "2016-06-24" @default.
- W2205320237 creator A5003321930 @default.
- W2205320237 date "2013-06-14" @default.
- W2205320237 modified "2023-09-23" @default.
- W2205320237 title "Sensitivity of a middle atmosphere GCM to consistent scale-interaction of parameterized orographic gravity waves" @default.
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- W2205320237 doi "https://doi.org/10.6084/m9.figshare.719785.v1" @default.
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