地球科学进展

地球科学进展 >

2021 , Vol. 36 >Issue 6: 579 - 591

DOI: https://doi.org/10.11867/j.issn.1001-8166.2021.066

综述与评述

印度洋偶极子研究进展回顾

  • 姜继兰 ,
  • 刘屹岷 ,
  • 李建平 ,
  • 张人禾
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  • 1.中国科学院大气物理研究所大气科学和地球流体力学数值模拟国家重点实验室，北京 100029
    2.中国科学院大学地球与行星科学学院，北京 100049
    3.中国海洋大学深海圈层与地球系统前沿 科学中心/物理海洋教育部重点实验室，山东 青岛 266100
    4.青岛海洋科学与技术 国家实验室区域海洋动力学与数值模拟功能实验室，山东 青岛 266237
    5.复旦大学 大气与海洋科学系/大气科学研究院，上海 200438
姜继兰（1994-），女，四川宜宾人，博士研究生，主要从事海气相互作用研究. E-mail： jiangjilan@lasg.iap.ac.cn

收稿日期: 2021-04-02

  修回日期: 2021-05-25

  网络出版日期: 2021-07-22

基金资助

中国科学院战略性先导科技专项“工业革命以来海陆气相互作用的气候环境影响”(XDB40030204);国家自然科学基金项目“青藏高原地—气耦合过程和海洋对区域能量和水分循环及全球气候的协同影响”(91637312)

收起

Indian Ocean Dipole： A Review and Perspective

  • Jilan JIANG ,
  • Yimin LIU ,
  • Jianping LI ,
  • Renhe ZHANG
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  • 1.State Key Laboratory of Numerical Modelling for Atmospheric Sciences and Geophysical Fluid Dynamics，Institute of Atmospheric Physics，Chinese Academy of Sciences，Beijing 100029，China
    2.College of Earth and Planetary Sciences，University of Chinese Academy of Sciences，Beijing 100049，China
    3.Frontiers Science Center for Deep Ocean Multispheres and Earth System （FDOMES）/ Key Laboratory of Physical Oceanography/ Institute for Advanced Ocean Studies，Ocean University of China，Qingdao 266100，China
    4.Laboratory for Ocean Dynamics and Climate，Pilot Qingdao National Laboratory for Marine Science and Technology，Qingdao 266237，China
    5.Department of Atmospheric and Oceanic Sciences & Institute of Atmospheric Sciences，Fudan University，Shanghai 200438，China
JIANG Jilan (1994-), female, Yibin City, Sichuan Province, Ph. D student. Research areas include sea-air interaction. E-mail: jiangjilan@lasg.iap.ac.cn

Received date: 2021-04-02

  Revised date: 2021-05-25

  Online published: 2021-07-22

Supported by

the Strategic Priority Research Program of Chinese Academy of Sciences "Climatic and environment impacts of sea-land-air interaction since the industrial revolution"(XDB40030204);The National Natural Science Foundation of China "The synergistic influence of coupling process of land-atmosphere of the Tibet Plateau and the ocean on regional energy and water cycles and global climate"(91637312)

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摘要

印度洋偶极子是热带印度洋中重要的年际变率之一，对印度洋周边国家乃至全球的气候有着重要的影响，关于其形成机制及气候影响的研究对于气候预测具有重要意义。主要回顾了近10年印度洋偶极子的相关研究进展，包括印度洋偶极子的基本特征、与热带太平洋中厄尔尼诺—南方涛动之间的关系、与亚洲夏季风之间的关系、对全球气候的影响以及全球变暖背景下的变化等。印度洋偶极子与热带太平洋中厄尔尼诺—南方涛动之间的关系体现为二者之间是相互影响的，但不同类型的印度洋偶极子对热带太平洋中厄尔尼诺—南方涛动的影响机制尚不明确，还需进一步的研究。印度洋偶极子与亚洲夏季风之间的关系体现为二者之间存在强烈的相互作用，印度洋偶极子与印度洋东部夏季风环流之间存在相互促进作用，而印度洋偶极子与印度夏季风环流之间的相互作用尚需进一步研究。此外，研究表明全球变暖背景下极端正印度洋偶极子的发生将增多，同时极端印度洋偶极子对我国极端气候事件的发生有着重要影响。以往的研究主要集中于单独的印度洋偶极子或印度洋偶极子和热带太平洋中厄尔尼诺—南方涛动的结合对我国极端气候的影响，而印度洋偶极子与中高纬环流系统或泛热带海洋之间的协同作用对我国极端气候事件的影响还亟需相关研究。对印度洋偶极子的系统性回顾可为未来印度洋偶极子的研究提供一定的科学基础。

关键词： 印度洋偶极子; 厄尔尼诺—南方涛动; 亚洲夏季风; 相互作用; 全球增暖

本文引用格式

姜继兰 , 刘屹岷 , 李建平 , 张人禾 . 印度洋偶极子研究进展回顾[J]. 地球科学进展, 2021 , 36(6) : 579 -591 . DOI: 10.11867/j.issn.1001-8166.2021.066

Abstract

The Indian Ocean Dipole （IOD） is one of the dominant interannual variabilities in the tropical Indian Ocean， which has important impacts on countries around the Indian Ocean and even the global climate. The research on the formation mechanism of IOD and its climatic effects is of great significance for climate prediction. This study mainly reviews the related research progress of IOD during the past 10 years， such as its basic characteristics， its relationship with El Ni?o-Southern Oscillation （ENSO） and the Asian summer monsoon， its climate effect， and its variation under the global warming. The relationship between IOD and ENSO is reflected in their mutual influence. The influence mechanism of different types of IOD on the development of ENSO is not clear and needs further investigation. A strong interaction between IOD and the Asian summer monsoon is found. The positive IOD and the summer monsoon circulation in the eastern Indian Ocean mutually promote， while the interaction between the IOD and the Indian summer monsoon needs further study. Furthermore， the extreme positive IOD will increase under the global warming， which has an important influence on extreme climatic events in China. Researches primarily focus on the effect of IOD alone or the combination effect of IOD and ENSO on extreme climatic events in China， but the synergistic effect between IOD and the mid-high latitude circulation system or the pan-tropical ocean on extreme climatic events in China needs further studies. A systematic review of IOD research progress during the past 10 years can provide a scientific basis for the future research of IOD.

Key words： Indian Ocean Dipole; ENSO; Asian summer monsoon; Interaction; Global warming

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