Intensification and Dynamics of the Westward Equatorial Undercurrent During the Summers of 1998 and 2016 in the Indian Ocean

Author:

Huang Ke123,Wang Dongxiao4ORCID,Chen Gengxin13ORCID,Nagura Motoki5ORCID,Han Weiqing6ORCID,McPhaden Michael J.7ORCID,Feng Ming8ORCID,Chen Ju1ORCID,Wu Ying9ORCID,Zhang Xiaolin10ORCID,Li Yuanlong11,Xie Qiang12,Wang Weiqiang13ORCID,Zhou Feng2ORCID

Affiliation:

1. State Key Laboratory of Tropical Oceanography South China Sea Institute of Oceanology Guangzhou China

2. State Key Laboratory of Satellite Ocean Environment Dynamics Second Institute of Oceanography Ministry of Natural Resources Hangzhou China

3. Southern Marine Science and Engineering Guangdong Laboratory (Guangzhou) Guangzhou China

4. School of Marine Sciences Sun Yat‐sen University and Southern Marine Science and Engineering Guangdong Laboratory (Zhuhai) Zhuhai China

5. Japan Agency for Marine‐Earth Science and Technology Yokosuka Japan

6. Department of Atmospheric and Oceanic Sciences University of Colorado, Boulder Boulder CO USA

7. Pacific Marine Environmental Laboratory National Oceanic and Atmospheric Administration Seattle WA USA

8. CSIRO Oceans and Atmosphere Crawley WA Australia

9. State Key Laboratory of Estuarine and Coastal Research East China Normal University Shanghai China

10. Kyushu University Fukuoka Japan

11. CAS Key Laboratory of Ocean Circulation and Waves Institute of Oceanology Chinese Academy of Sciences Qingdao China

12. Institute of Deep‐Sea Science and Engineering Chinese Academy of Sciences Sanya China

Publisher

American Geophysical Union (AGU)

Subject

General Earth and Planetary Sciences,Geophysics

Reference63 articles.

1. Babonneix A. Gourdeau L. Durand F. Menkes C. E. &Djath N.(2012).Impact of ENSO variability on the Pacific Equatorial Undercurrent (EUC) sources: A modeling approach depending on the horizontal resolution. InGeophysical Research Abstracts Volume 14 EGU2012‐10485‐1 EGU General Assembly.

2. Atlantic Equatorial Undercurrent intensification counteracts warming-induced deoxygenation

3. The Equatorial Undercurrent and the Oxygen Minimum Zone in the Pacific

4. Seasonal-to-Interannual Time-Scale Dynamics of the Equatorial Undercurrent in the Indian Ocean

5. The role of Equatorial Undercurrent in sustaining the Eastern Indian Ocean upwelling

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