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- W2010174864 abstract "We develop a theory to describe the topographic control of planetary-scale flows resulting from the variation of the Earth's rotation with latitude. We show that on passing over topography, an inertial, zonal current on an equatorial β-plane may pass through a control at which the flow changes from a subcritical to a supercritical solution branch. Downstream of this control, a transition back to the subcritical solution branch may occur, for example, by the generation of planetary eddies or radiating Rossby waves. We calculate the energy dissipated across such a transition and discuss the relevance of this theory for a number of atmospheric and oceanic phenomena. We also show that this phenomenon is analogous to the hydraulic control of a non-rotating, stratified flow passing through a channel of variable width." @default.
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- W2010174864 date "1993-02-01" @default.
- W2010174864 modified "2023-09-25" @default.
- W2010174864 title "The topographic control of planetary-scale flow" @default.
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- W2010174864 doi "https://doi.org/10.1017/s0022112093000588" @default.
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