Vorticity Equation of Transient Ultra-Long Waves in Middle Latitudes in Winter Regarded as Langevin's Equation in Brownian Motion
Author:
Affiliation:
1. Geophysical Institute, Tokyo University
Publisher
Meteorological Society of Japan
Subject
Atmospheric Science
Link
https://www.jstage.jst.go.jp/article/jmsj1965/60/1/60_1_206/_pdf
Reference8 articles.
1. Ashe, S., 1979: A nonlinear model of the timeaverage axially asymmetric flow induced by topography and diabatic heating. J. Atmos. Sci., 36, 109-126.
2. Berkofsky, L, and E. A. Bertoni, 1955: Mean topographic charts for the entire earth. Bull. Amer. Met. Soc., 36, 350-354.
3. Brown, J. A., 1964: A diagnostic study of tropospheric diabatic heating and the generation of available potential energy. Tellus, 16, 371-387.
4. Derome, J. F., and A. Wiin-Nielsen, 1971: The response of a middle latitude model atmosphere to forcing by topography and stationary heat sources. Mon. Wea. Rev., 99, 554-576.
5. Eliassen, A. and W. E. Hubert, 1953: Computations of vertical motion and vorticity budget in a blocking situation. Tellus, 5, 196-206.
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