Maintenance of mid-latitude oceanic fronts by mesoscale eddies

Author:

Jing Zhao123ORCID,Wang Shengpeng12ORCID,Wu Lixin12ORCID,Chang Ping345,Zhang Qiuying134ORCID,Sun Bingrong12,Ma Xiaohui123,Qiu Bo6,Small Justing37,Jin Fei-Fei8ORCID,Chen Zhaohui12ORCID,Gan Bolan12ORCID,Yang Yun9ORCID,Yang Haiyuan12,Wan Xiuquan12

Affiliation:

1. Key Laboratory of Physical Oceanography and Frontiers Science Center for Deep Ocean Multispheres and Earth System, Ocean University of China, Qingdao, China.

2. Qingdao National Laboratory for Marine Science and Technology, Qingdao, China.

3. International Laboratory for High-Resolution Earth System Prediction, Texas A&M University, College Station, TX, USA.

4. Department of Oceanography, Texas A&M University, College Station, TX, USA.

5. Department of Atmospheric Sciences, Texas A&M University, College Station, TX, USA.

6. Department of Oceanography, University of Hawaii at Manoa, Honolulu, HI, USA.

7. Climate and Global Dynamics Division, National Center for Atmospheric Research, Boulder, CO, USA.

8. Department of Atmospheric Sciences, University of Hawaii at Manoa, Honolulu, HI, USA.

9. College of Global Change and Earth System Science, Beijing Normal University, Beijing, China.

Abstract

Vertical heat transport by ocean mesoscale eddies plays an important role in maintaining western boundary current extension fronts.

Funder

National Natural Science Foundation of China

Publisher

American Association for the Advancement of Science (AAAS)

Subject

Multidisciplinary

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