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Volume 22 Issue 2

Mar.  2005

Article Contents
Article >  ADVANCES IN ATMOSPHERIC SCIENCES  > 2005 >  22(2): 220-229

The Shallow Meridional Overturning Circulation in the Northern Indian Ocean and Its Interannual Variability

  • 1.

    Physical Oceanography Laboratory & Ocean-Atmosphere Interaction and Climate Laboratory; Ocean University of China; Qingdao 266003,Physical Oceanography Laboratory & Ocean-Atmosphere Interaction and Climate Laboratory; Ocean University of China; Qingdao 266003,Physical Oceanography Laboratory & Ocean-Atmosphere Interaction and Climate Laboratory; Ocean University of China; Qingdao 266003,CSIRO; Division of Marine Research; GPO Box 1538; Hobart; Tasmania; Australia,Physical Oceanography Laboratory & Ocean-Atmosphere Interaction and Climate Laboratory; Ocean University of China; Qingdao 266005


doi: 10.1007/BF02918511

  • The shallow meridional overturning circulation (upper 1000 m) in the northern Indian Ocean and its interannual variability are studied, based on a global ocean circulation model (MOM2) with an integration of 10 years (1987-1996). It is shown that the shallow meridional overturning circulation has a prominent seasonal reversal characteristic. In winter, the flow is northward in the upper layer and returns southward at great depth. In summer, the deep northward inflow upwells north of the equator and returns ...
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    [2] CHEN Xiao, YAN Youfang, CHENG Xuhua, QI Yiquan, 2013: Performances of Seven Datasets in Presenting the Upper Ocean Heat Content in the South China Sea, ADVANCES IN ATMOSPHERIC SCIENCES, 30, 1331-1342.  doi: 10.1007/s00376-013-2132-1
    [3] Ya GAO, Huijun WANG, Dong CHEN, 2017: Interdecadal Variations of the South Asian Summer Monsoon Circulation Variability and the Associated Sea Surface Temperatures on Interannual Scales, ADVANCES IN ATMOSPHERIC SCIENCES, 34, 816-832.  doi: 10.1007/ s00376-017-6246-8
    [4] NIU Ning, LI Jianping, 2008: Interannual Variability of Autumn Precipitation over South China and its Relation to Atmospheric Circulation and SST Anomalies, ADVANCES IN ATMOSPHERIC SCIENCES, 25, 117-125.  doi: 10.1007/s00376-008-0117-2
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    [6] Riyu LU, Saadia HINA, Xiaowei HONG, 2020: Upper- and Lower-tropospheric Circulation Anomalies Associated with Interannual Variation of Pakistan Rainfall during Summer, ADVANCES IN ATMOSPHERIC SCIENCES, 37, 1179-1190.  doi: 10.1007/s00376-020-0137-0
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    • Manuscript History

    Manuscript received: 10 March 2005
    Manuscript revised: 10 March 2005
    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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    The Shallow Meridional Overturning Circulation in the Northern Indian Ocean and Its Interannual Variability

    • 1. Physical Oceanography Laboratory & Ocean-Atmosphere Interaction and Climate Laboratory; Ocean University of China; Qingdao 266003,Physical Oceanography Laboratory & Ocean-Atmosphere Interaction and Climate Laboratory; Ocean University of China; Qingdao 266003,Physical Oceanography Laboratory & Ocean-Atmosphere Interaction and Climate Laboratory; Ocean University of China; Qingdao 266003,CSIRO; Division of Marine Research; GPO Box 1538; Hobart; Tasmania; Australia,Physical Oceanography Laboratory & Ocean-Atmosphere Interaction and Climate Laboratory; Ocean University of China; Qingdao 266005
    • Manuscript received: 2005-03-10
    • Manuscript revised: 2005-03-10

    Abstract: The shallow meridional overturning circulation (upper 1000 m) in the northern Indian Ocean and its interannual variability are studied, based on a global ocean circulation model (MOM2) with an integration of 10 years (1987-1996). It is shown that the shallow meridional overturning circulation has a prominent seasonal reversal characteristic. In winter, the flow is northward in the upper layer and returns southward at great depth. In summer, the deep northward inflow upwells north of the equator and returns ...

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