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- W2054461783 abstract "Vegetation zones of the eastern coast of China represent a series of forests from the tropical to the cold-temperate zone. There is also a change from forest through steppe to desert from the southeastern coast to the northwestern interior (11). These patterns are quite different from those in western Eurasia where the vegetation pattern of the western part from south to north is: tropical, subtropical desert and savanna, Mediterranean sclerophyllous forest, deciduous forest, and coniferous forest. This series shows a pattern, drier in the south and moister in the north, that basically reflects Hadley's classic diagram of atmospheric circulations (10, 25, 26, 28). Therefore, the differences between the eastern and western parts of Eurasia reflect an asymmetric distribution of vegetation (Fig. 1). The geographic distribution of vegetation in China-Eastern Asia should be interpreted primarily in terms of patterns of atmospheric circulation in Asia because it reflects the projection of atmospheric circulation onto the land surface of the earth. Recent research in atmospheric physics indicates that the Tibetan Plateau in eastern Asia is a huge Hot Island that hinders atmospheric circulation (5). The powerful thermal and orographic effects of the Plateau cause great changes in the atmospheric circulation of the northern hemisphere, especially in Asia, and have a direct effect on patterns of vegetation in that part of the world. Hereafter I will discuss the uplift of the Plateau in relation to atmospheric circulation and the distribution of vegetation in China. The most important events in this regard are the formation of the Tibetan High, the establishment of the Mongolian anticyclone, and the reinforcement of the Eastern Asian Monsoon." @default.
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- W2054461783 date "1983-01-01" @default.
- W2054461783 modified "2023-10-17" @default.
- W2054461783 title "The Tibetan Plateau in Relation to the Vegetation of China" @default.
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- W2054461783 doi "https://doi.org/10.2307/2992087" @default.
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