Linear Response of the Global Atmosphere to Thermal Forcing during Northern Summer
Author:
Affiliation:
1. Numerical Prediction Division
Publisher
Meteorological Society of Japan
Subject
Atmospheric Science
Link
https://www.jstage.jst.go.jp/article/jmsj1965/63/5/63_5_739/_pdf
Reference12 articles.
1. Asakura, T., 1968: Dynamical climatology of at-mospheric circulation over East Asia centered in Japan. Papers in Meteorology and Geophysics, 19, 1-68.
2. Dickinson, R. E., 1973: Method of parametarization for infrared cooling between the altitudes of 30 and 70 kilometers. J. Geophys. Res., 78, 4451-4457.
3. Gambo, K. and K. Kudo, 1983: Teleconnections in the zonally asymmetric height field during the northern hemispheric summer. J. Met. Soc. Japan, 61, 36-50.
4. Hoskins, B. J. and D. J. Karoly, 1981: The steady linear response of a spherical atmosphere to thermal and orographic forcing. J. Atmos. Sci., 38, 1179-1196.
5. Huang, R. H. and K. Gambo, 1982: The response of a hemispheric multi-level model atmosphere to forcing by topography and stationary heat sources. Part I and Part II. J. Meteor. Soc. Japan, 60, 78-108.
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1. Relationships between the Quasi-Stationary Rossby Waves in the Subtropical Jet and the Mass and Heat Transport in the Northern Periphery of the Tibetan High;Journal of the Meteorological Society of Japan. Ser. II;1999
2. Barotropic Disturbances on Intraseasonal Time Scales Observed in the Midlatitudes over the Eurasian Continent during the Northern Summer;Journal of the Meteorological Society of Japan. Ser. II;1998
3. On the Processes of Transitions between Circulation Regimes during Winter over the Pacific and North America;Journal of the Meteorological Society of Japan. Ser. II;1988
4. Low-Frequency Interactions between the Summer Monsoon and the Northern Hemisphere Westerlies;Journal of the Meteorological Society of Japan. Ser. II;1986
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