A new look at the Ο-equation
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B. J. Hoskins; I. Draghici; H. C. Davies
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Article
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1978
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John Wiley and Sons
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English
β 469 KB
## Abstract In the conventional quasiβgeostrophic form of the βomegaββequation, the forcing of vertical velocity is usually expressed as the sum of two terms associated respectively with vorticity and temperature advection. Consideration of each term in isolation is misleading and there can be a la