The Response of a Hemispheric Multi-Level Model Atmosphere to Forcing by Topography and Stationary Heat Sources in Summer-Reference-Cited by-同舟云学术

The Response of a Hemispheric Multi-Level Model Atmosphere to Forcing by Topography and Stationary Heat Sources in Summer

Published:1983 Issue:4 Volume:61 Page:495-509
ISSN:0026-1165
Container-title:Journal of the Meteorological Society of Japan. Ser. II
language:en
Short-container-title:Journal of the Meteorological Society of Japan

Author:

Huang Rong-hui¹,Gambo K.²

Affiliation:

1. Institute of Atmospheric Physics, Academia Sinica

2. Geophysical Institute, Tokyo University

Publisher

Meteorological Society of Japan

Subject

Atmospheric Science

Link

https://www.jstage.jst.go.jp/article/jmsj1965/61/4/61_4_495/_pdf

Reference11 articles.

1. Ashe, S., 1979: A nonlinear model of the time average axially asymmetric flow induced by topography and diabatic heating. J. Atmos. Sci., 36, 109-126.

2. Charney, J. G. and P. G. Drazin, 1961: Propagation of planetary-scale disturbances from the lower into the upper atmosphere. J. Geophys. Res., 66, 83-109.

3. Huang, Rang-hui and K. Gambo, 1981: The response of a model atmosphere in middle latitudes to forcing by topography and stationary heat sources. J. Meteor. Soc. Japan, 59, 220-237.

4. Huang, Rang-hui and K. Gambo, 1982: The response of a hemispheric multi-level model atmosphere to forcing by topography and stationary heat sources. Part I & II. J. Meteor. Soc. Japan, 60, 78-108.

5. Iwashima, T., 1980: Analysis of stationary planetary waves in summer (Presented at the annual meeting of the Meteorological Society of Japan in March 1980).

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