Weakly Non-linear Aspects of Steady Hydrostatic Mountain Waves in a 2-layered Stratified Fluid of Infinite Depth over a 2-dimensional Mountain
Author:
Affiliation:
1. Meteorological Research Institute
Publisher
Meteorological Society of Japan
Subject
Atmospheric Science
Link
https://www.jstage.jst.go.jp/article/jmsj1965/68/3/68_3_357/_pdf
Reference16 articles.
1. Aihara. M. and M. Hirasawa, 1988: On severe downslope wind due to the mountain wave-induced critical level. Papers in Meteor. and Geophys., 36, 119-135 (published by Meteorological Research Institute attached to Japan Meteorological Agency)
2. Durran, DR., 1986: Another look at downslope windstorms. Part 1. J. Atmos. Sci., 43, 2527-2543.
3. Durran, D.R. and J.B. Klemp, 1987: Another look at downslope windstorms. Part 2. J. Atmos. Sci., 44, 3402-3412.
4. Grimshaw, R.H. and N. Smyth, 1986: Resonant flow of a stratified fluid over topography. J. Fluid Mech., 169, 429-464.
5. Houghton, D.D. and A. Kasahara,1968: Nonlinear shallow fluid over an isolated ridge. Commun. Pure Appl. Math., 21, 1-23.
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2. Recent Studies of Local-scale Climate in Japan;Geographical review of Japan, Series B.;1996
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4. A Numerical Study of the Local Downslope Wind "Yamaji-kaze" in Japan;Journal of the Meteorological Society of Japan. Ser. II;1991
5. Weakly Non-linear Aspects of Steady Hydrostatic Mountain Waves in a 2-layered Stratified Fluid of Infinite Depth over a 2-dimensional Mountain;Journal of the Meteorological Society of Japan. Ser. II;1990
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