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Authors
Zhang, Yimin
Zhao, Zhonghua
Liao, Enhui
Jiang, Yuwu
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Funding
Funding for this research was provided by:
Natural Science Foundation of China (U1805241, 41876004)
Chinese Ministry of Science and Technology (2018YFC1407502)
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Article History
Received: 11 October 2021
Accepted: 19 March 2022
First Online: 4 June 2022
Significance Statement
: Wintertime sea surface temperature along the coast of China exhibits the largest temporal variability in the Taiwan Strait. We propose a mechanism to explain how the PDO and ENSO alternately control the sea surface temperature in the Taiwan Strait in different PDO phases under the background of global warming. This mechanism can help predict the sea surface temperature trend along the western coast of the North Pacific and can be useful to explain the occurrence of extreme warm and cold events in such a typical subtropical strait.
: All authors certify that they have no affiliations with or involvement in any organization or entity with any financial interest or non-financial interest in the subject matter or materials discussed in this manuscript.
