A persistent Kuroshio in the glacial East China Sea and implications for coral paleobiogeography
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 whi...
| Main Authors: | , |
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| Format: | Journal article |
| Language: | English |
| Published: |
Wiley
2020
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