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Article >  Journal of Tropical Meteorology  > 1999 >  5(2): 199-207

THE STUDY ON EDDY TRANSPORT OF WATER VAPOR OVER SOUTH CHINA

  • Department of Atmospheric Sciences, Zhongshan University, Guangzhou 510275 China

  • MeteoroIOgical College of Air FOrce, 211101, China

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  • Water vapor transport is decomposed into mean transport and eddy transport. Analysis of water vapor over South China during the first flood season of 1994 shows that difference between season mean transport and season total transport is less than 10%. For the monthly and ten-day averages, the difference is above it.The transient transport of water vapor is the least among all kinds of eddy transport. its amount is only ±2% of total transpoft for column. The constant wave transport is the Iapest Sometimes it may be 1-6 times of total transport.
  • [1] CHEN Shi-xun, GAO Shao-feng, 1983. Characteristics of summer monsoon in South China and its relationship with precipitation in rainy seasons(in Chinese)[A]. In: Proceedings of National Seminar on Tropical.Summer Monsoon [C]. Kunming: Yunnan People's Press.
    [2] LIU Hui-Ian, 1987. Large-scale eddy transport of water vapor in eastern China in June and July 1979(in Chinese)[J] J. Trop. Meteor., 3(2): 129-133.
    [3] PEIXOTO J P, ROSEN R D, SALSTEIN D A, 1978. Seasonal variability in the pole-to-pole modes of water vapor transport during the IGY [J]. Arch.Met. Geoph.Biokl.,Ser.A.27: 233-255.
    [4] YE Du-zhen, ZENG Qing-cun, GUO Yu-fu, 1991. Contemporary Study of Climate(in Chinese)[M]. Beijing: China Meteorological Press. 19-32.
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GAO Shao-feng, LU Han-Cheng. THE STUDY ON EDDY TRANSPORT OF WATER VAPOR OVER SOUTH CHINA [J]. Journal of Tropical Meteorology, 1999, 5(2): 199-207.
GAO Shao-feng, LU Han-Cheng. THE STUDY ON EDDY TRANSPORT OF WATER VAPOR OVER SOUTH CHINA [J]. Journal of Tropical Meteorology, 1999, 5(2): 199-207.
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    Manuscript received: 15 July 1998
    Manuscript revised: 02 November 1998
    通讯作者: 陈斌, bchen63@163.com
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    THE STUDY ON EDDY TRANSPORT OF WATER VAPOR OVER SOUTH CHINA

    • Department of Atmospheric Sciences, Zhongshan University, Guangzhou 510275 China
    • MeteoroIOgical College of Air FOrce, 211101, China
    • Received Date: 1998-07-15
    • Rev Recd Date: 1998-11-02

    Abstract: Water vapor transport is decomposed into mean transport and eddy transport. Analysis of water vapor over South China during the first flood season of 1994 shows that difference between season mean transport and season total transport is less than 10%. For the monthly and ten-day averages, the difference is above it.The transient transport of water vapor is the least among all kinds of eddy transport. its amount is only ±2% of total transpoft for column. The constant wave transport is the Iapest Sometimes it may be 1-6 times of total transport.

    GAO Shao-feng, LU Han-Cheng. THE STUDY ON EDDY TRANSPORT OF WATER VAPOR OVER SOUTH CHINA [J]. Journal of Tropical Meteorology, 1999, 5(2): 199-207.
    Citation: GAO Shao-feng, LU Han-Cheng. THE STUDY ON EDDY TRANSPORT OF WATER VAPOR OVER SOUTH CHINA [J]. Journal of Tropical Meteorology, 1999, 5(2): 199-207.
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