Conserved Quantities in a 2-dimensional Steady Flow on an f-plane with an Application to a Flow over a Mountain
Author:
Affiliation:
1. Meteorological Research Institute
Publisher
Meteorological Society of Japan
Subject
Atmospheric Science
Link
https://www.jstage.jst.go.jp/article/jmsj1965/75/6/75_6_1165/_pdf
Reference11 articles.
1. Bannon, P. R., 1988: Anelastic semigeostrophic flow over a mountain ridge. J. Atmos. Sci., 45, 1020-1029.
2. Bennets, D. A. and B. J. Hoskins, 1979: Conditional symmetric instability-a possible explanation for frontal rainbands. Quart. J. Roy. Meteor. Soc., 105, 945-962.
3. Gutmann, L. N., 1991: Downslope windstorms. Part 1: Effect of air density decrease with height. J. Atmos. Sci., 48, 2545-2551.
4. Kanehisa, H., 1993: Density currents in jet shear flows. J. Meteor. Soc. Japan, 71, 633-636.
5. Kanehisa, H., 1995: Downslope windstorms in a uniform environmental flow with non-uniform potential temperature gradient. J. Meteor. Soc. Japan, 73, 833-837.
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1. A Conserved Quantity Related to Vorticity Component in the Direction of .NABLA..THETA. * u;Journal of the Meteorological Society of Japan. Ser. II;2004
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