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The Quasi-Geostrophic Omega Equation (without friction and diabatic terms)

THE TRENBERTH (1978) INTERPRETATION. The Quasi-Geostrophic Omega Equation (without friction and diabatic terms). PROBLEM: TERM 1 and 2 on the RHS are often large and opposite leading to ambiguity about the sign and magnitude of ? when analyzing weather maps.

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Geostrophic terms - PowerPoint PPT Presentation

The Quasi-Geostrophic Omega Equation (without friction and diabatic terms)