Abstract
This note reports the derivation of an alternative form of Andrews' conservation law for small-amplitude, quasi-geostrophic, transient eddies on a steady but spatially nonuniform flow.
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This note reports the derivation of an alternative form of Andrews' conservation law for small-amplitude, quasi-geostrophic, transient eddies on a steady but spatially nonuniform flow.
This note reports the derivation of an alternative form of Andrews' conservation law for small-amplitude, quasi-geostrophic, transient eddies on a steady but spatially nonuniform flow.