NASA NTRS · 19800007446
Numerical modeling of baroclinic instability
Abstract
The Eady model of baroclinic instability applied to a rotating channel with Ekman layers at the top and bottom is extended to a beta-plane channel. Changes in the shape and position of the boundary separating the regions of axially symmetric and wavelike motion are predicted.
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Geisler, J. F.. 1979-12-15. Numerical modeling of baroclinic instability. https://ntrs.nasa.gov/citations/19800007446
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