The dynamical effects of divergent wind on the intraseasonal variability of the East Asian circulation
Author:
Publisher
Springer Science and Business Media LLC
Subject
Atmospheric Science
Link
http://link.springer.com/content/pdf/10.1007/BF02656976.pdf
Reference12 articles.
1. Fein, J. S.(1977), Global vorticity budget over the tropics and subtropics at 200 hPa during the Northern Hemisphere summer,Pure Appl. Geophys. 115: 1493–1500.
2. Holton, J. R. and D. E. Colton (1972), A diagnostic study of the vorticity balance at 200 hPa in the tropics during the northern Hemisphere summer,J. Atmos. Sci., 29: 1124–1128.
3. 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, II,J. Meteor, soc. Japan, 60: 78–108.
4. Huang, R. H. and K. Gambo (1983), The response of a hemispheric multi-level model atmosphere to forcing by topography and stationary heat sources in summer,J. Meteor, soc. Japan, 61: 495–509.
5. Krishnamurti, T. N. and Y. Ramanathan (1982), Sensitivity of the monsoon onset to differential heating,J. Atmos, Sci., 39: 1290–1306.
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