On the Response of Forced Rossby Waves to the Time Change of Zonal Wind and Forcing
Author:
Affiliation:
1. National Center for Atmospheric Research
Publisher
Meteorological Society of Japan
Subject
Atmospheric Science
Link
https://www.jstage.jst.go.jp/article/jmsj1965/49A/0/49A_545/_pdf
Reference16 articles.
1. Charney, J. G., and P. G. Drazin, 1961: Propagation of planetary-scale disturbances from the lower into the upper atmosphere. J. Geophys. Res., 66, 83-110.
2. Dickinson, R E., 1968a: On the exact and approximate linear theory of vertically propagating planetary Rossby waves forced at a spherical lower boundary. Mon. Wea. Rev., 96, 405-415.
3. —, 1968b: Planetary Rossby waves propagating vertically through weak westerly wind wave guides. J. Atmos. Sci., 25, 984-1002.
4. —, 1969: Vertical propagation of planetary Rossby waves through an atmosphere with Newtonian cooling. J. Geophys. Res., 74, 929-938.
5. Hirota, 1., 1968a: Planetary waves in the upper stratosphere in early 1966. J. Meteor. Soc. Japan, 46, 418-430.
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1. Baroclinic instability of a midlatitude zonal mean state changing with time;Tellus;1982-06
2. General circulation of the atmosphere;Reviews of Geophysics;1975
3. Wave motions in the atmosphere and related ionospheric phenomena;Space Science Reviews;1974-10
4. Excitation of Planetary Rossby Waves in the Winter Stratosphere by Periodic Forcing;Journal of the Meteorological Society of Japan. Ser. II;1971
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