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Article >  Journal of Tropical Meteorology  > 2000 >  6(1): 65-74

A BAROTROPIC QUASI-GEOSTROPHIC MODEL WITH LARGE-SCALE TOPOGRAPHY, FRICTION AND HEATING

  • Department of Geophysics, Peking University, Beijing 100871 China

Funding:

  • Based on the barotropic equations including large-scale topography, friction and heat factor, a barotropic quasi-geostrophic model with large-scale topography, friction and heating is obtained by means of scale analysis and small parameter method. It is shown that this equation is a basic one, which is used to study the influence of the Tibetan Plateau on the large-scale flow in the atmosphere. If the friction and heating effect of large-scale topography are neglected, this model will degenerate to the general barotropic quasi-geostrophic one.
  • [1] Charney J G,Neumann J V,1950.Numerical Integration of the Barotropic Vorticity Equation[J]Tellus,2: 237-254.
    [2] LI Guo-qing,SONG Zheng-shan,1981.The importance of the Tibetan Plateau on the formation of the
    [3] low-latitude temperature field and atmospheric circulation[C]The Tibetan Plateau Meteorology Symposium,Beijing,33-51.
    [4] LIAO Dong-xian,LI Zeng-zhong,SONG Qing-li,1981.The function of mountain pattern on the genesis and development of vortex,The Tibetan Plateau Meteorology Symposium,Beijing,52-60.
    [5] LIU Shi-kuo,LIU Shi-da,1991.The Dynamics of Atmosphere[M].Beijing:Peking University Publishing House.
    [6] QIAN Yong-fu,YAN Hong,WANG Qian-qian,etc.,1988.The numerical studies on topographic effect in the planetary atmosphere[M]Beijing:Science Publishing House.
    [7] QU Zhang,WANG Qian-qian,QIAN Yong-Fu,etc.,1981.The numerical experiment on the dynamic role that the Tibetan Plateau plays on atmospheric circulation of East Asia in summer and winter[C].The Tibetan Plateau Meteorology Symposium,Beijing,18-32.
    [8] WANG An-yu,HU Qi,QIN Guang-yan,1983.The numerical experiment on the influence that the heat field of east Asia and large-scale topography play on the seasonal variance of atmospheric circulation[J].Plateau Meteor.,2(1):31-38.
    [9] WANG An-yu,WANG Qian-qian,QU Zhang,etc.,1981.The numerical experiment on the dynamic role that topography of different scales over the Tibetan Plateau plays on the atmospheric circulation of East Asia [C].The Tibetan Plateau Meteorology Symposium,Beijing,61-78.
    [10] WANG Qian-qian,QU Zhang,YAN Hong,etc.,1981.The numerical experiment on the dynamic role that the Tibetan Plateau plays on atmospheric circulation of East Asia in summer[C]The Tibetan Plateau Meteorology Symposium,Beijing,1-17.
    [11] WU Jun,ZHENG Qing-lin,1995.Topographic influence on inter-monthly long-term numerical forecast effect[J] Plateau Meteorology,14(3):276-303.
    [12] YE Du-zheng,GAO You-xi,1979.The Tibetan Plateau Meteorology[M]Beijing:Science Publishing House.
    [13] YE Du-zheng,LUO Si-wei,ZHU Bao-zhen,etc.,1957.The structure of stream field over the Tibetan Plateau and the heat balance of the tropospheric atmosphere[J].Acta Meteor.Sin.,28:108-121.
    [14] ZHANG Ji-jia,ZHU Bao-zhen,ZHU Fu-kang,etc.,1988.The Tibetan Plateau Meteorology Progress[M]Beijing:Science Publishing House.
    [15] ZHU Bao-zhen,1957.The constant disturbance influence of the large-scale heat source,heat sink and topography on the Westerlies[J]Acta Meteor.Sin.,28:122-140.
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JIANG Xun, CHEN Jiong, LIU Shi-kuo. A BAROTROPIC QUASI-GEOSTROPHIC MODEL WITH LARGE-SCALE TOPOGRAPHY, FRICTION AND HEATING [J]. Journal of Tropical Meteorology, 2000, 6(1): 65-74.
JIANG Xun, CHEN Jiong, LIU Shi-kuo. A BAROTROPIC QUASI-GEOSTROPHIC MODEL WITH LARGE-SCALE TOPOGRAPHY, FRICTION AND HEATING [J]. Journal of Tropical Meteorology, 2000, 6(1): 65-74.
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    • Manuscript History

    Manuscript received: 26 August 1999
    Manuscript revised: 15 March 2000
    通讯作者: 陈斌, bchen63@163.com
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    A BAROTROPIC QUASI-GEOSTROPHIC MODEL WITH LARGE-SCALE TOPOGRAPHY, FRICTION AND HEATING

    • Department of Geophysics, Peking University, Beijing 100871 China
    • Received Date: 1999-08-26
    • Rev Recd Date: 2000-03-15

    Abstract: Based on the barotropic equations including large-scale topography, friction and heat factor, a barotropic quasi-geostrophic model with large-scale topography, friction and heating is obtained by means of scale analysis and small parameter method. It is shown that this equation is a basic one, which is used to study the influence of the Tibetan Plateau on the large-scale flow in the atmosphere. If the friction and heating effect of large-scale topography are neglected, this model will degenerate to the general barotropic quasi-geostrophic one.

    JIANG Xun, CHEN Jiong, LIU Shi-kuo. A BAROTROPIC QUASI-GEOSTROPHIC MODEL WITH LARGE-SCALE TOPOGRAPHY, FRICTION AND HEATING [J]. Journal of Tropical Meteorology, 2000, 6(1): 65-74.
    Citation: JIANG Xun, CHEN Jiong, LIU Shi-kuo. A BAROTROPIC QUASI-GEOSTROPHIC MODEL WITH LARGE-SCALE TOPOGRAPHY, FRICTION AND HEATING [J]. Journal of Tropical Meteorology, 2000, 6(1): 65-74.
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