Robust Subsurface Biological Response During the Decaying Stage of an Extreme Indian Ocean Dipole in 2019-Reference-Cited by-同舟云学术

Robust Subsurface Biological Response During the Decaying Stage of an Extreme Indian Ocean Dipole in 2019

Published:2022-08-15 Issue:16 Volume:49 Page:
ISSN:0094-8276
Container-title:Geophysical Research Letters
language:en
Short-container-title:Geophysical Research Letters

Author:

Li Hongliang¹²³^ORCID,Zhang Jingjing¹²³,Wang Xinyang¹⁴^ORCID,Zhu Yuanli¹³,Liu Lin²⁵^ORCID,Wang Baodong⁶,Zhang Xuelei⁶^ORCID,Wei Qinsheng⁶^ORCID,Ding Ruibin⁷⁸^ORCID,Xuan Jiliang³⁷^ORCID,Shou Lu¹³,Zhou Feng³⁴⁷^ORCID,Chen Jianfang¹³⁷^ORCID

Affiliation:

1. Key Laboratory of Marine Ecosystem Dynamics Second Institute of Oceanography Ministry of Natural Resources Hangzhou China

2. Southern Marine Science and Engineering Guangdong Laboratory (Zhuhai) Zhuhai China

3. Observation and Research Station of Yangtze River Delta Marine Ecosystems Ministry of Natural Resources Zhoushan China

4. School of Oceanography Shanghai Jiao Tong University Shanghai China

5. Ministry of Natural Resources and Laboratory for Regional Oceanography and Numerical Modeling Pilot National Laboratory for Marine Science and Technology First Institute of Oceanography Qingdao China

6. Key Laboratory of Marine Eco‐Environmental Science and Technology First Institute of Oceanography Ministry of Natural Resources Qingdao China

7. State Key Laboratory of Satellite Ocean Environment Dynamics Hangzhou China

8. Institute of Polar and Ocean Technology Second Institute of Oceanography Ministry of Natural Resources Hangzhou China

Publisher

American Geophysical Union (AGU)

Subject

General Earth and Planetary Sciences,Geophysics

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1029/2022GL099721

Reference44 articles.

1. Carbon and nitrogen productivity during spring in the oligotrophic Indian Ocean along the GO-SHIP IO9N transect

2. Increased frequency of extreme Indian Ocean Dipole events due to greenhouse warming

3. Projected response of the Indian Ocean Dipole to greenhouse warming

4. The role of nutricline depth in regulating the ocean carbon cycle

5. Marine Primary Production in Relation to Climate Variability and Change

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