On the impact of the Qinghai-Tibet Plateau uplift on climate, many scholars use mathematical models to infer the geological circulation of the atmosphere to show that the modern atmospheric circulation and the geological age of the differences in atmospheric circulation. In January, the Siberian high pressure does not exist, in 30 ° N near the emergence of a weak high pressure (temporarily called the Lhasa high pressure), the Qinghai-Tibet region in the southern part of the Qinghai-Tibet Plateau, the Qinghai-Tibet Plateau, The previ- ous easterly airstream prevails in the north, while the southerly airstream prevails in the north and the southward in the south. In July, the low pressure in India did not exist. The eastern part of China was a hot low pressure. The temperature in the Tibetan area was much warmer than that in the south China and Myanmar and India in the vicinity of 25 ° N and the tropical troposphere over India.
Note
Black lines in the figure indicate that there is no isobaric distribution in the plateau
The red line in the figure indicates that there is an isobaric distribution of the plateau terrain
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