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Abstract

As seen from the 100 hPa mean monthly charts, in summer the middle and lower latitudes of the Northern Hemisphere are occupied by an ultra-long wave system of wave number 2 with ridges located over two continents and troughs over two oceans. One of the ridges situated in South Asia develops a upper troposphere anticyclone, which is called the South Asia high, over the Qinghai-Xizang Plateau.

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References

  1. Zhu Fukang, et al., South Asia high, Science Press, 1–95, 1980 (in Chinese).

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  2. Yao Lanchang, et al., Studies of the mean atmospheric heat sources over the Qinghai-Xizang Plateau and its surrounding regions in summer, Collected Papers of the Qinghai-Xizang Plateau Meteorological Science Experiment (1), Science Press, 291–302, 1984 (in Chinese).

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  3. Sun Guowu and Zhou Yi., The relationship between the seasonal formation of the South Asia high on Qinghai-Xizang Plateau and the typhoon movement, collected papers of meteorological science and technology (6), Meteorological Press,(To be Published in Chinese).

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  4. Long-Range Numerical Forecast Cooperation Group, The figures and data of monthly average of the heating field in the Northern Hemisphere, Meteorological Press, 1982 (in Chinese).

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© 1986 Science Press and American Meteorological Society

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Sun, G. (1986). A Study of the First Arrival of the South Asia High on the Qinghai-Xizang Plateau. In: Xu, Y. (eds) Proceedings of International Symposium on the Qinghai-Xizang Plateau and Mountain Meteorology. American Meteorological Society, Boston, MA. https://doi.org/10.1007/978-1-935704-19-5_31

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  • DOI: https://doi.org/10.1007/978-1-935704-19-5_31

  • Publisher Name: American Meteorological Society, Boston, MA

  • Online ISBN: 978-1-935704-19-5

  • eBook Packages: Springer Book Archive

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