By Xu Yigang
In this continuing there are paperbounds offered by means of the members at a gathering held in Beijing, China, 20-24 March 1984, together with these at the following vital features when it comes to mountain meteorology: the sector remark, the dynamic and thermal results of the mountains at the common movement, the implications acquired in the course of the numerical versions with the large-scale topography, and the movement structures at the Plateau.
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Extra resources for Proceedings of International Symposium on the Qinghai-Xizang Plateau and Mountain Meteorology
2) According to the monthly mean ~hart of 600 and 500 hPa (Fig. omitted) for the Plateau and Indian regions during May-August 1979, the level the monsoon heat low is able to reach, taking the Plateau region as the center, is lower than in normal years. From the mean 30 Tab. 1 The symbol contrast of pressure and height anomalies from ground to 600 hPa level between the Plateau and the Indian regions. surface pressure Plateau May India June Plateau India July August + + + India + + + Plateau + Plateau 850 hPa + 700 hPa 600 hPa + + + + + + + + India chart of years, the summer monsoon heat low may reach the vicinity of 400 hPa.
The cross-equatorial air current in the lower troposphere established itself as a result of the increase in sea level pressure in the Mascarene and Australia highs in the Southern Hemisphere. The southwest monsoon developed further, and moved to the north of 150 N over the 48 Indian peninsula. As the south-east monsoon predominated along the lower and middle reaches of the Changjiang River, the Mei-yu spell began. The characteristics of summer circulation became definitely established. IV. A DISCUSSION OF THE ROLE OF THE QINGHAI-XIZANG PLATEAU IN THE SEASONAL TRANSITION OF ATMOSPHERIC CIRCULATION The role of the Qinghai-Xizang Plateau has been studied at from a .
THE ESTABLISHMENT OF SUMMER MONSOON CIRCULATION SYSTEMS IN ASIA The abrupt set-in of the summer monsoon in the Asian continent during the transition period of atmospheric circulation in the Northern Hemisphere in early summer is a prominent meteorological phenomenon. During the transition period in June 1979, all synoptic com- 45 ponents of the summer monsoon system experienced obvious modification. First of all, the Indian hot low became suddenly deeper in early June (not shown). About ten days later, in the third pentad of June, the high at 100 hPa suddenly moved to the west about 10 degress longitude between two successive pentads, while at the same time the Easterly at the south of the high also intensified (Fig.
Proceedings of International Symposium on the Qinghai-Xizang Plateau and Mountain Meteorology by Xu Yigang