southward geostrophic flow over most of the width of the South Pacific, and permits northward flow only in a higher-order boundary current. We are not at all certain that such simple dynamics do ...
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Gravity waves caused by complex terrain over the Tibetan Plateau can enhance the intensity of spring rainfallThe breaking of orographic gravity waves induces a zonal wave drag in the middle troposphere, which destroys the geostrophic balance of the large-scale westerly flow and thus drives an ...
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