地球科学进展 ›› 2019, Vol. 34 ›› Issue (3): 243 -254. doi: 10.11867/j.issn.1001-8166.2019.03.0243

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印度洋热带环流圈热盐输运及其对区域气候模态的影响
杜岩 1, 2( ),张涟漪 1, 2,张玉红 1   
  1. 1. 中国科学院南海海洋研究所热带海洋环境国家重点实验室,广东 广州 510301
    2. 中国科学院大学,北京 100049
  • 收稿日期:2018-12-27 修回日期:2019-01-26 出版日期:2019-03-10
  • 基金资助:
    国家自然科学基金重点项目“南印度洋热带环流的低频变异及其对热盐输运和气候模态的影响”(编号:41830538);国家自然科学基金杰出青年科学基金项目“物理海洋学”(编号:41525019)

Review of the Tropical Gyre in the Indian Ocean with Its Impact on Heat and Salt Transport and Regional Climate Modes

Yan Du 1, 2( ),Lianyi Zhang 1, 2,Yuhong Zhang 1   

  1. 1. State Key Laboratory of Tropical Oceanography, South China Sea Institute of Oceanology, Chinese Academy of Sciences, Guangzhou 510301,China
    2. University of Chinese Academy of Sciences, Beijing 100049,China
  • Received:2018-12-27 Revised:2019-01-26 Online:2019-03-10 Published:2019-04-28
  • About author: Du Yan (1975-), male, Linyi City, Shandong Province, Professor. Research areas include ocean circulation and ocean-atmosphere interaction. E-mail: duyan@scsio.ac.cn | Du Yan (1975-), male, Linyi City, Shandong Province, Professor. Research areas include ocean circulation and ocean-atmosphere interaction. E-mail: duyan@scsio.ac.cn
  • Supported by:
    Project supported by the National Natural Science Foundation of China “The low-frequency variability of southern tropical Indian Ocean circulation and its impact on heat and salt transport and climate modes”(No. 41830538);The National Science Fund for Distinguished Young Scholars "Physical Oceanography"(No. 41525019)

受季风系统影响,热带印度洋的环流具有明显的季节变化,这在北印度洋尤其明显。但在气候平均态意义上,热带印度洋环流在赤道为东向流动,在赤道以南为西向流动,在东、西部边界分别向南、向北流动,从而与其他大洋类似,形成一个相对闭合的热带环流圈,称之为印度洋热带环流圈。立足于此环流圈,从环流热盐输运及其气候影响等方面,综述了相关的研究,讨论了印度洋热带环流系统与温盐分布和区域主要气候模态的关系。

Due to the IO monsoon impact, the tropical IO circulation has significant seasonal variation, especially in the northern IO. However, in mean-state, a relatively closed current loop is established by eastward current along the equator and westward current south of equator, which is regarded as Tropical Gyre in the Indian Ocean. Based on this circulation system, relevant studies were reviewed. Its impact on heat and salt transports and regional climate changes were discussed.

中图分类号: 

图1 印度洋热带环流圈浮标轨迹(编号:9217260)示踪图
Fig.1 Trajectory of a surface drifter (ID: 9217260) to indicate the Tropical Gyre in the Indian Ocean
图2 热带印度洋海表盐度(填色,基于Argo浮标网格化数据)和海表流速(箭头,基于海洋表层流场实时分析数据集(OSCAR))的气候态分布
Fig.2 Climatologic state of sea surface salinity (shading based on Argo gridded data) and surface current (vector based on Ocean Surface Current Analyses- Real Time data (OSCAR)) in the tropical Indian Ocean
图3 热带印度洋海表温度(填色,基于最优插值海表面温度数据(OISST))和海表风场(箭头,基于多平台交叉校准风场数据(CCMP))的气候态分布
Fig.2 Climatologic state of sea surface temperature (shading based on Optimum Interpolation Sea Surface Temperature data, OISST) and surface wind (vector based on the Cross-Calibrated Multi-Platform wind dat(CCMP)) in the tropical Indian Ocean
图4 基于经验正交分解方法得到的热带印度洋海表温度的前2个模态
Fig.4 First two modes of the tropical Indian Ocean sea surface temperature derived by Empirical Orthogonal Function(EOF) method
图5 印度洋偶极子的低频变化与热带东南印度洋温跃层的关系(基于SODA模式结果,据参考文献[ 97 ]修改)
Fig.5 Low-frequency variability of IOD and its relationship with thermocline over the southeastern tropical Indian Ocean (Based on Simple Ocean Data Assimilation data(SODA) modified after reference [ 97 ])
图6 印度洋热带环流圈示意图
Fig.6 Schematic diagram of the Tropical Gyre in the Indian Ocean
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