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Volume 12 Issue 3

Jul.  1995

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Article >  ADVANCES IN ATMOSPHERIC SCIENCES  > 1995 >  12(3): 311-318

Evolution of Asian Summer Monsoon and the Slowly Varying Disturbances

  • 1.

    Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100080


doi: 10.1007/BF02656979

  • The evolution of Asian summer monsoon is analyzed by means of decomposition of the atmospheric circulation into basic current and slowly varying monsoon disturbances. It is seen that the major slowly varying disturbances are two vortical couples, one located in the Indian Ocean and Indian Peninsula, and another in the Northern Hemispheric western Pacific Ocean and the East Asia. This indicates that the Asian summer monsoon consists of two branches, the Indian monsoon and the East Asian monsoon. Moreover, the analysis shows that the evolutionary processes of these two vortical couples are rather independent each other, and they all can be qualitatively interpreted by the dynamical theory of wave packet. The different stages of summer monsoon can be very well characterized by the location and in?tensity of the two vortical couples. Besides, in particular years there exists also some quasistationary wave train and its characteristics should be further analyzed.
  • [1] ZHU Yali, 2012: Variations of the Summer Somali and Australia Cross-Equatorial Flows and the Implications for the Asian Summer Monsoon, ADVANCES IN ATMOSPHERIC SCIENCES, 29, 509-518.  doi: 10.1007/s00376-011-1120-6
    [2] Bueh Cholaw, Ji Liren, Sun Shuqing, Cui Maochang, 2001: EAWM-Related Air-Sea-Land Interaction and the Asian Summer Monsoon Circulation, ADVANCES IN ATMOSPHERIC SCIENCES, 18, 659-673.
    [3] LIU Xiangwen, WU Tongwen, YANG Song, JIE Weihua, NIE Suping, LI Qiaoping, CHENG Yanjie, LIANG Xiaoyun, 2015: Performance of the Seasonal Forecasting of the Asian Summer Monsoon by BCC_CSM1.1(m), ADVANCES IN ATMOSPHERIC SCIENCES, 32, 1156-1172.  doi: 10.1007/s00376-015-4194-8
    [4] ZOU Liwei, ZHOU Tianjun, 2015: Asian Summer Monsoon Onset in Simulations and CMIP5 Projections Using Four Chinese Climate Models, ADVANCES IN ATMOSPHERIC SCIENCES, 32, 794-806.  doi: 10.1007/s00376-014-4053-z
    [5] YAN Renchang, BIAN Jianchun, 2015: Tracing the Boundary Layer Sources of Carbon Monoxide in the Asian Summer Monsoon Anticyclone Using WRF-Chem, ADVANCES IN ATMOSPHERIC SCIENCES, 32, 943-951.  doi: 10.1007/s00376-014-4130-3
    [6] BIAN Jianchun, YAN Renchang, CHEN Hongbin, Lu Daren, Steven T. MASSIE, 2011: Formation of the Summertime Ozone Valley over the Tibetan Plateau: The Asian Summer Monsoon and Air Column Variations, ADVANCES IN ATMOSPHERIC SCIENCES, 28, 1318-1325.  doi: 10.1007/s00376-011-0174-9
    [7] Song YANG, WEN Min, Rongqian YANG, Wayne HIGGINS, ZHANG Renhe, 2011: Impacts of Land Process on the Onset and Evolution of Asian Summer Monsoon in the NCEP Climate Forecast System, ADVANCES IN ATMOSPHERIC SCIENCES, 28, 1301-1317.  doi: 10.1007/s00376-011-0167-8
    [8] Yiran GUO, Jie CAO, Hui LI, Jian WANG, Yuchao DING, 2016: Simulation of the Interface between the Indian Summer Monsoon and the East Asian Summer Monsoon: Intercomparison between MPI-ESM and ECHAM5/MPI-OM, ADVANCES IN ATMOSPHERIC SCIENCES, 33, 294-308.  doi: 10.1007/s00376-015-5073-z
    [9] Min WEI, 2005: A Coupled Model Study on the Intensification of the Asian Summer Monsoon in IPCC SRES Scenarios, ADVANCES IN ATMOSPHERIC SCIENCES, 22, 798-806.  doi: 10.1007/BF02918680
    [10] LU Riyu, Buwen DONG, 2008: Response of the Asian Summer Monsoon to Weakening of Atlantic Thermohaline Circulation, ADVANCES IN ATMOSPHERIC SCIENCES, 25, 723-736.  doi: 10.1007/s00376-008-0723-z
    [11] CHEN Bin, XU Xiang-De, YANG Shuai, ZHANG Wei, 2012: On the Temporal and Spatial Structure of Troposphere-to- Stratosphere Transport in the Lowermost Stratosphere over the Asian Monsoon Region during Boreal Summer, ADVANCES IN ATMOSPHERIC SCIENCES, 29, 1305-1317.  doi: 10.1007/s00376-012-1171-3
    [12] WU Bingyi, WANG Dongxiao, HUANG Ronghui, 2003: Relationship between Sea Level Pressures of the Winter Tropical Western Pacific and the Subsequent Asian Summer Monsoon, ADVANCES IN ATMOSPHERIC SCIENCES, 20, 496-510.  doi: 10.1007/BF02915494
    [13] Li Chongyin, Mu Mingquan, 2001: The Influence of the Indian Ocean Dipole on Atmospheric Circulation and Climate, ADVANCES IN ATMOSPHERIC SCIENCES, 18, 831-843.
    [14] P. L. S. Rao, 2000: The Influence of Systematic Errors on the Asian Summer Monsoon Circulation, ADVANCES IN ATMOSPHERIC SCIENCES, 17, 576-586.  doi: 10.1007/s00376-000-0021-x
    [15] Chen Longxun, Luo Shaohua, Shen Rugui, 1984: THE ASIAN SUMMER MONSOON AND ITS RELATIONS TO THE RAINFALL IN CHINA, ADVANCES IN ATMOSPHERIC SCIENCES, 1, 263-285.  doi: 10.1007/BF02678139
    [16] K.-M. Lau, Song Yang, 1997: Climatology and Interannual Variability of the Southeast Asian Summer Monsoon, ADVANCES IN ATMOSPHERIC SCIENCES, 14, 141-162.  doi: 10.1007/s00376-997-0016-y
    [17] Chen Qiying, Yu Yongqiang, Guo Yufu, 1997: Simulation of East Asian Summer Monsoon with IAP CGCM, ADVANCES IN ATMOSPHERIC SCIENCES, 14, 461-472.  doi: 10.1007/s00376-997-0064-3
    [18] HAN Jinping, WANG Huijun, 2007: Interdecadal Variability of the East Asian Summer Monsoon in an AGCM, ADVANCES IN ATMOSPHERIC SCIENCES, 24, 808-818.  doi: 10.1007/s00376-007-0808-0
    [19] Chen Wen, Hans-F. Graf, Huang Ronghui, 2000: The Interannual Variability of East Asian Winter Monsoon and Its Relation to the Summer Monsoon, ADVANCES IN ATMOSPHERIC SCIENCES, 17, 48-60.  doi: 10.1007/s00376-000-0042-5
    [20] YAN Hongming, YANG Hui, YUAN Yuan, LI Chongyin, 2011: Relationship Between East Asian Winter Monsoon and Summer Monsoon, ADVANCES IN ATMOSPHERIC SCIENCES, 28, 1345-1356.  doi: 10.1007/s00376-011-0014-y
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    • Manuscript History

    Manuscript received: 10 July 1995
    Manuscript revised: 10 July 1995
    通讯作者: 陈斌, bchen63@163.com
    • 1. 

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    Evolution of Asian Summer Monsoon and the Slowly Varying Disturbances

    • 1. Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100080
    • Manuscript received: 1995-07-10
    • Manuscript revised: 1995-07-10

    Abstract: The evolution of Asian summer monsoon is analyzed by means of decomposition of the atmospheric circulation into basic current and slowly varying monsoon disturbances. It is seen that the major slowly varying disturbances are two vortical couples, one located in the Indian Ocean and Indian Peninsula, and another in the Northern Hemispheric western Pacific Ocean and the East Asia. This indicates that the Asian summer monsoon consists of two branches, the Indian monsoon and the East Asian monsoon. Moreover, the analysis shows that the evolutionary processes of these two vortical couples are rather independent each other, and they all can be qualitatively interpreted by the dynamical theory of wave packet. The different stages of summer monsoon can be very well characterized by the location and in?tensity of the two vortical couples. Besides, in particular years there exists also some quasistationary wave train and its characteristics should be further analyzed.

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