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A persistent Kuroshio in the glacial East China Sea and implications for coral paleobiogeography

Abstract:

The Kuroshio Current is a major hydrographical feature of the modern East China Sea, but it has been suggested that its flow was diverted to the east of the Ryukyu Arc at the Last Glacial Maximum. Shoaling of the Yonaguni Depression has also been proposed as a cause of Kuroshio Current diversion which, while unlikely to have been significant at the Last Glacial Maximum, may have been an important consideration further back in time. Using an ensemble of high‐resolution ocean simulations with c...

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Publication status:
Published
Peer review status:
Peer reviewed

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Publisher copy:
10.1029/2020pa003902

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Institution:
University of Oxford
Division:
MPLS
Department:
Earth Sciences
Role:
Author
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Role:
Author
ORCID:
0000-0003-3033-2332
Publisher:
Wiley Publisher's website
Journal:
Paleoceanography and Paleoclimatology Journal website
Volume:
35
Issue:
7
Article number:
e2020PA003902
Publication date:
2020-07-07
Acceptance date:
2020-05-27
DOI:
EISSN:
2572-4525
ISSN:
2572-4517
Language:
English
Keywords:
Pubs id:
1145084
Local pid:
pubs:1145084
Deposit date:
2020-11-12

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