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Volume 23 Issue 6

Nov.  2006

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Article >  ADVANCES IN ATMOSPHERIC SCIENCES  > 2006 >  23(6): 951-963

Characteristics of the Onset of the Asian Summer Monsoon and the Importance of Asian-Australian “Land Bridge”

  • 1.

    Jiangsu Key Laboratory of Meteorological Disaster (KLME) and School of Atmospheric Sciences, Nanjing University of Information Science and Technology, Nanjing 210044,State Key Laboratory of Severe Weather (LaSW), Chinese Academy of Meteorological Sciences, Beijing 100081,Jiangsu Key Laboratory of Meteorological Disaster (KLME) and School of Atmospheric Sciences, Nanjing University of Information Science and Technology, Nanjing 210044,Jiangsu Key Laboratory of Meteorological Disaster (KLME) and School of Atmospheric Sciences, Nanjing University of Information Science and Technology, Nanjing 210044


doi: 10.1007/s00376-006-0951-z

  • Based on summarizing previous achievements and using data as long and new as possible, the onset characteristics of Asian summer monsoon and the role of Asian-Australian “land bridge” in the onset of summer monsoon are further discussed. In particular, the earliest onset area of Asian summer monsoon is comparatively analyzed, and the sudden and progressive characteristics of the onset of summer monsoon in different regions are discussed. Furthermore, the relationships among such critical events during the onset of Asian summer monsoon as the splitting of subtropical high belt over the Bay of Bengal (BOB), the initiation of convection over Indo-China Peninsula, the westward advance, reestablishment of South Asian High, and the rapid northward progression of convection originated from Sumatra in early summer are studied. The important impact of the proper collocation of the latent heating over Indo-China Peninsula and the sensible heating over Indian Peninsula on the splitting of the subtropical high belt, the deepening of BOB trough, the activating of Sri Lanka vortex (twin vortexes in the Northern and Southern Hemispheres), and the subsequent onset of South China Sea summer monsoon are emphasized.
  • [1] DING Yihui, HE Chun, 2006: The Summer Monsoon Onset over the Tropical Eastern Indian Ocean: The Earliest Onset Process of the Asian Summer Monsoon, ADVANCES IN ATMOSPHERIC SCIENCES, 23, 940-950.  doi: 10.1007/s00376-006-0940-2
    [2] LI Chongyin, PAN Jing, 2006: Atmospheric Circulation Characteristics Associated with the Onset of Asian Summer Monsoon, ADVANCES IN ATMOSPHERIC SCIENCES, 23, 925-939.  doi: 10.1007/s00376-006-0925-1
    [3] Lin WANG, Hong-Li REN, Fang ZHOU, Nick DUNSTONE, Xiangde XU, 2023: Dynamical Predictability of Leading Interannual Variability Modes of the Asian-Australian Monsoon in Climate Models, ADVANCES IN ATMOSPHERIC SCIENCES, 40, 1998-2012.  doi: 10.1007/s00376-023-2288-2
    [4] HE Jinhai, SUN Chenghu, LIU Yunyun, Jun MATSUMOTO, LI Weijing, 2007: Seasonal Transition Features of Large-Scale Moisture Transport in the Asian-Australian Monsoon Region, ADVANCES IN ATMOSPHERIC SCIENCES, 24, 1-14.  doi: 10.1007/s00376-007-0001-5
    [5] WU Zhiwei, LI Jianping, 2008: Prediction of the Asian-Australian Monsoon Interannual Variations with the Grid-Point Atmospheric Model of IAP LASG (GAMIL), ADVANCES IN ATMOSPHERIC SCIENCES, 25, 387-394.  doi: 0.1007/s00376-008-0387-8
    [6] 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
    [7] 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
    [8] WANG Yafei, Fujiyaoshi YASUSHI, Kato KURANOSHIN, 2003: A Teleconnection Pattern Related with the Development of the Okhotsk High and the Northward Progress of the Subtropical High in East Asian Summer, ADVANCES IN ATMOSPHERIC SCIENCES, 20, 237-244.  doi: 10.1007/s00376-003-0009-4
    [9] Sun Shuqing, Ying Ming, 1999: Subtropical High Anomalies over the Western Pacific and Its Relations to the Asian Monsoon and SST Anomaly, ADVANCES IN ATMOSPHERIC SCIENCES, 16, 559-568.  doi: 10.1007/s00376-999-0031-2
    [10] Xinyu LI, Riyu LU, Gen LI, 2021: Different Configurations of Interannual Variability of the Western North Pacific Subtropical High and East Asian Westerly Jet in Summer, ADVANCES IN ATMOSPHERIC SCIENCES, 38, 931-942.  doi: 10.1007/s00376-021-0339-0
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    [12] 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
    [13] 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
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    • Manuscript History

    Manuscript received: 10 November 2006
    Manuscript revised: 10 November 2006
    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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    Characteristics of the Onset of the Asian Summer Monsoon and the Importance of Asian-Australian “Land Bridge”

    • 1. Jiangsu Key Laboratory of Meteorological Disaster (KLME) and School of Atmospheric Sciences, Nanjing University of Information Science and Technology, Nanjing 210044,State Key Laboratory of Severe Weather (LaSW), Chinese Academy of Meteorological Sciences, Beijing 100081,Jiangsu Key Laboratory of Meteorological Disaster (KLME) and School of Atmospheric Sciences, Nanjing University of Information Science and Technology, Nanjing 210044,Jiangsu Key Laboratory of Meteorological Disaster (KLME) and School of Atmospheric Sciences, Nanjing University of Information Science and Technology, Nanjing 210044
    • Manuscript received: 2006-11-10
    • Manuscript revised: 2006-11-10

    Abstract: Based on summarizing previous achievements and using data as long and new as possible, the onset characteristics of Asian summer monsoon and the role of Asian-Australian “land bridge” in the onset of summer monsoon are further discussed. In particular, the earliest onset area of Asian summer monsoon is comparatively analyzed, and the sudden and progressive characteristics of the onset of summer monsoon in different regions are discussed. Furthermore, the relationships among such critical events during the onset of Asian summer monsoon as the splitting of subtropical high belt over the Bay of Bengal (BOB), the initiation of convection over Indo-China Peninsula, the westward advance, reestablishment of South Asian High, and the rapid northward progression of convection originated from Sumatra in early summer are studied. The important impact of the proper collocation of the latent heating over Indo-China Peninsula and the sensible heating over Indian Peninsula on the splitting of the subtropical high belt, the deepening of BOB trough, the activating of Sri Lanka vortex (twin vortexes in the Northern and Southern Hemispheres), and the subsequent onset of South China Sea summer monsoon are emphasized.

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