A Time Dependent Model of the Atmospheric Response to Midlatitude Heating with Various Zonal Structures
Author:
Affiliation:
1. Department of Mathematics and Oceanography, University of British Columbia
2. Clinate Researh Crap, Department of Meteorology, McGill University
Publisher
Meteorological Society of Japan
Subject
Atmospheric Science
Link
https://www.jstage.jst.go.jp/article/jmsj1965/66/2/66_2_227/_pdf
Reference15 articles.
1. Chervin, R.M., W.M. Washington, and S.H. Schneider, 1976: Testing the statistical significance of the response of the NCAR general circulation model to North Pacific Ocean surface temperature anomalies. J. Atmos. Sci., 33, 413-423.
2. Chervin, J.E. Kutzbach, D.D. Houghton, and R.G. Gallimore, 1980: Response of the NCAR general circulation model to prescribed changes in ocean surface temperature, II. Midlatitude and subtropical changes. J. Atmos Sci., 37, 308-322.
3. Frankignoul, C., 1985a:' Sea surface temperature anomalies, planetary waves, and air-sea feedback in the middle latitudes. Rev. Geophys•23, 357-390.
4. Frankignoul, C., 1985b: Multivariate analysis of sensitivity studies with atmospheric GCM's. In Coupled Atmosphere-Ocean Models, Elsevier Oceanography Series, Vol. 40, edited by J.C.J. Nihoul, pp.199-209, Elsevier, New York.
5. Holton, J.R., 1979: An Introduction to Dynamic Meteorology. 2nd ed. Academic Press, New York, 319pp.
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