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Volume 18 Issue 5

Sep.  2001

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Article >  ADVANCES IN ATMOSPHERIC SCIENCES  > 2001 >  18(5): 1005-1017

Relations of Water Vapor Transport from Indian Monsoon with That over East Asia and the Summer Rainfall in China

  • 1.

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

  • A diagnostic study is made to investigate the relationship between water vapor transport from Indian monsoon and that over East Asia in Northern summer. It is found that water vapor transport from Indian monsoon is inverse to that over East Asia. More (less) Indian monsoon water vapor transport corresponds to less (more) water vapor transport over East Asia and less (more) rainfall in the middle and lower reaches of the Yangtze River valley. The Indian summer monsoon water vapor transport is closely related to the in tensity of the western Pacific subtropical high in its southwestern part. The stronger (weaker) the Indian sum mer monsoon water vapor transport, the weaker (stronger) the western Pacific subtropical high in its southwestern part, which leads to less (more) water vapor transport to East Asia, and thus less (more) rain fall in the middle and lower reaches of the Yangtze River valley. Analysis of the out-going longwave radia tion anomalies suggests that the convective heating anomalies over the Indian Ocean may have significant impact not only on the Indian monsoon, but also on the East Asian monsoon.
  • [1] Yi Lan, 1995: Characteristics of the Mean Water Vapor Transport over Monsoon Asia, ADVANCES IN ATMOSPHERIC SCIENCES, 12, 195-206.  doi: 10.1007/BF02656832
    [2] XUE Feng, ZENG Qingcun, HUANG Ronghui, LI Chongyin, LU Riyu, ZHOU Tianjun, 2015: Recent Advances in Monsoon Studies in China, ADVANCES IN ATMOSPHERIC SCIENCES, 32, 206-229.  doi: 10.1007/s00376-014-0015-8
    [3] B. KNOPF, K. ZICKFELD, M. FLECHSIG, V. PETOUKHOV, 2008: Sensitivity of the Indian Monsoon to Human Activities, ADVANCES IN ATMOSPHERIC SCIENCES, 25, 932-945.  doi: 10.1007/s00376-008-0932-5
    [4] SUN Li, SHEN Baizhu, GAO Zongting, SUI Bo, Lesheng BAI, Sheng-Hung WANG, AN Gang, LI Jian, 2007: The Impacts of Moisture Transport of East Asian Monsoon on Summer Precipitation in Northeast China, ADVANCES IN ATMOSPHERIC SCIENCES, 24, 606-618.  doi: 10.1007/s00376-007-0606-8
    [5] HUANG Ronghui, ZHOU Liantong, CHEN Wen, 2003: The Progresses of Recent Studies on the Variabilities of the East Asian Monsoon and Their Causes, ADVANCES IN ATMOSPHERIC SCIENCES, 20, 55-69.  doi: 10.1007/BF03342050
    [6] Lin Zhaohui, Zeng Qingcun, 1997: Simulation of East Asian Summer Monsoon by Using an Improved AGCM, ADVANCES IN ATMOSPHERIC SCIENCES, 14, 513-526.  doi: 10.1007/s00376-997-0069-y
    [7] Ronghui HUANG, Yong LIU, Zhencai DU, Jilong CHEN, Jingliang HUANGFU, 2017: Differences and Links between the East Asian and South Asian Summer Monsoon Systems: Characteristics and Variability, ADVANCES IN ATMOSPHERIC SCIENCES, 34, 1204-1218.  doi: 10.1007/ s00376-017-7008-3
    [8] Ma Henian, Ding Yihui, 1997: The Present Status and Future of Research of the East Asian Monsoon, ADVANCES IN ATMOSPHERIC SCIENCES, 14, 125-140.  doi: 10.1007/s00376-997-0015-z
    [9] WU Yunfei, ZHANG Renjian, HAN Zhiwei, ZENG Zhaomei, 2010: Relationship between East Asian Monsoon and Dust Weather Frequency over Beijing, ADVANCES IN ATMOSPHERIC SCIENCES, 27, 1389-1398.  doi: 10.1007/s00376-010-9181-5
    [10] Yang Yan, Li Zhijin, Ji Liren, 1997: Adjoint Sensitivity Analyses on the Anomalous Circulation Features in East Asian Summer Monsoon, ADVANCES IN ATMOSPHERIC SCIENCES, 14, 111-123.  doi: 10.1007/s00376-997-0050-9
    [11] Cheng Anning, Chen Wen, Huang Ronghui, 1998: The Sensitivity of Numerical Simulation of the East Asian Monsoon to Different Cumulus Parameterization Schemes, ADVANCES IN ATMOSPHERIC SCIENCES, 15, 204-220.  doi: 10.1007/s00376-998-0040-6
    [12] Wang Shiyu, Qian Yongfu, 2001: Modeling of the 1998 East Asian Summer Monsoon by a Limited Area Model with Incorporated Coordinate, ADVANCES IN ATMOSPHERIC SCIENCES, 18, 209-224.  doi: 10.1007/s00376-001-0014-4
    [13] Wang Huijun, 2000: The Interannual Variability of East Asian Monsoon and Its Relationship with SST in a Coupled Atmosphere-Ocean-Land Climate Model, ADVANCES IN ATMOSPHERIC SCIENCES, 17, 31-47.  doi: 10.1007/s00376-000-0041-6
    [14] SUN Bo, ZHU Yali, WANG Huijun, 2011: The Recent Interdecadal and Interannual Variation of Water Vapor Transport over Eastern China, ADVANCES IN ATMOSPHERIC SCIENCES, 28, 1039-1048.  doi: 10.1007/s00376-010-0093-1
    [15] XU Xiangde, ZHOU Li, ZHANG Shengjun, MIAO Qiuju, 2003: Characteristics of the Correlation between Regional Water Vapor Transport along with the Convective Action and Variation of the Pacific Subtropical High in 1998, ADVANCES IN ATMOSPHERIC SCIENCES, 20, 269-283.  doi: 10.1007/s00376-003-0013-8
    [16] Yuanhai FU, Riyu LU, Dong GUO, 2021: Projected Increase in Probability of East Asian Heavy Rainy Summer in the 21st Century by CMIP5 Models, ADVANCES IN ATMOSPHERIC SCIENCES, 38, 1635-1650.  doi: 10.1007/s00376-021-0347-0
    [17] ZHANG Ran, JIANG Dabang, ZHANG Zhongshi, 2015: Causes of Mid-Pliocene Strengthened Summer and Weakened Winter Monsoons over East Asia, ADVANCES IN ATMOSPHERIC SCIENCES, 32, 1016-1026.  doi: 10.1007/s00376-014-4183-3
    [18] HUANG Ronghui, CHEN Wen, YANG Bangliang, ZHANG Renhe, 2004: Recent Advances in Studies of the Interaction between the East Asian Winter and Summer Monsoons and ENSO Cycle, ADVANCES IN ATMOSPHERIC SCIENCES, 21, 407-424.  doi: 10.1007/BF02915568
    [19] Kunhui YE, Renguang WU, 2017: Autumn Snow Cover Variability over Northern Eurasia and Roles of Atmospheric Circulation, ADVANCES IN ATMOSPHERIC SCIENCES, 34, 847-858.  doi: 10.1007/s00376-017-6287-z
    [20] Shan LU, Zeyong HU, Haipeng YU, Weiwei FAN, Chunwei FU, Di WU, 2021: Changes of Extreme Precipitation and its Associated Mechanisms in Northwest China, ADVANCES IN ATMOSPHERIC SCIENCES, 38, 1665-1681.  doi: 10.1007/s00376-021-0409-3
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    • Manuscript History

    Manuscript received: 10 September 2001
    Manuscript revised: 10 September 2001
    通讯作者: 陈斌, bchen63@163.com
    • 1. 

      沈阳化工大学材料科学与工程学院 沈阳 110142

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    Relations of Water Vapor Transport from Indian Monsoon with That over East Asia and the Summer Rainfall in China

    • 1. LASG, Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100080
    • Manuscript received: 2001-09-10
    • Manuscript revised: 2001-09-10

    Abstract: A diagnostic study is made to investigate the relationship between water vapor transport from Indian monsoon and that over East Asia in Northern summer. It is found that water vapor transport from Indian monsoon is inverse to that over East Asia. More (less) Indian monsoon water vapor transport corresponds to less (more) water vapor transport over East Asia and less (more) rainfall in the middle and lower reaches of the Yangtze River valley. The Indian summer monsoon water vapor transport is closely related to the in tensity of the western Pacific subtropical high in its southwestern part. The stronger (weaker) the Indian sum mer monsoon water vapor transport, the weaker (stronger) the western Pacific subtropical high in its southwestern part, which leads to less (more) water vapor transport to East Asia, and thus less (more) rain fall in the middle and lower reaches of the Yangtze River valley. Analysis of the out-going longwave radia tion anomalies suggests that the convective heating anomalies over the Indian Ocean may have significant impact not only on the Indian monsoon, but also on the East Asian monsoon.

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