Dynamical Effects of Mountains on the General Circulation of the Atmosphere: II. Effects of Mountain Barrier on a Barotropic Jet
Author:
Affiliation:
1. Geophysical Institute, Tokyo University
Publisher
Meteorological Society of Japan
Subject
Atmospheric Science
Link
https://www.jstage.jst.go.jp/article/jmsj1965/56/5/56_5_341/_pdf
Reference9 articles.
1. Charney, J., and A. Eliassen, 1949: A numerical method for predicting the perturbations of the middle latitude westerlies. Tellus, 1, 38-54.
2. Egger, J., 1972: Incorporation of steep mountains into numerical forecasting models. Tellus, 24, 325-335.
3. Holloway, J. L., Jr., and S. Manabe, 1971: Simulation of climate by a global general circulation model. I. Hydrologic cycle and heat balance. Mon. Wea. Rev., 99, 335-370.
4. Kasahara, A., 1966: The dynamical influence of orography on the large-scale motion of the atmos-phere. J. Atinos. Sci., 23, 259-271.
5. Manabe, S., J. Smagorinsky, J. L. Holloway, Jr., and H. M. Stone, 1970: Simulated climatology of a general circulation model with a hydrologic cycle: III. Effects of increased horizontal computational resolution. Mon. Wea. Rev., 98, 175-212.
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