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Answer sheet V Dynamics of large-scale atmospheric flow. Autumn SemesterQuasi-Geostrophic Dynamics (a) At the ground, the vertical velocity is zero: w = ∂w/∂x = 0. Because f02 > 0, the term
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Document Date: 2014-12-02 12:48:04
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Answer sheet V Dynamics of large-scale atmospheric flow. Autumn SemesterQuasi-Geostrophic Dynamics (a) At the ground, the vertical velocity is zero: w = ∂w/∂x = 0. Because f02 > 0, the term