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《Chinese Journal of Atmospheric Sciences》 1991-01
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EFFECT OF THERMAL REGIME OVER THE TIBETAN PLATEAU ON SOUTH ASIA HIGH ACTIVITIES

Ren Guangcheng(Meteorological Division, Second Artillery Headquarters)  
In this paper, the thermodynamic influence of the Tibetan Plateau on South Asia high is discussed based on the analyses of the thermal regimes in the atmosphere over the Plateau and its underlying surface. It is pointed out that the interannual change of temperature in the atmosphere is consistent with that of the underlying surface, but the inter-monthly changes are different. The temperature of the underlying surface rises sharply from February, while the explosive warming in the atmosphere happens in May. The maximum of temperature decreasing in the atmosphere appears in October, and in November for the underlying surface. It is also found that the latitudinal and longitudinal oscillations of South Asia high are closely tied with the thermal regimes in the atmosphere over the Tibetan Plateau and its underlying surface respectively. The thermal regimes in the atmosphere over the Tibetan Plateau seems to be more useful than the latter for the forecast of South Asia high.
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