Currents in the Taiwan Strait as observed by surface drifters |
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Authors: | Yun Qiu Li Li Chen-Tung Arthur Chen Xiaogang Guo Chunsheng Jing |
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Institution: | (1) The Third Institute of Oceanography, State Oceanic Administration, Xiamen, 361005, Fujian, China;(2) Institute of Marine Geology and Chemistry, National Sun Yat-Sen University, Kaohsiung, 80424, Taiwan;(3) State Key Laboratory of Marine Environmental Science, Xiamen University, Xiamen, 361005, Fujian, China |
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Abstract: | The trajectories of 110 satellite-tracked surface drifters from 1989 to 2007 were analyzed to elucidate near-surface circulation
in the Taiwan Strait. Although the summer circulation observed generally agrees with previous studies, several aspects of
the winter circulation were revealed by the analyses. Unlike many earlier studies, which have suggested that a northward (southward)
current prevails in the eastern (western) part of the Taiwan Strait during the northeast monsoon season, this study shows
that almost all winter drifters that entered the Taiwan Strait eventually moved southward. Inside the Taiwan Strait, northward
moving tracks can only be found in the Penghu Channel. After passing the Penghu Channel, the drifters were blocked by the
northeast monsoon wind and the Yun-Chang Rise, and turned southward. None of the drifters flowed persistently northward through
the Taiwan Strait in winter. In the southern Taiwan Strait, three typical patterns of circulation were observed for the winter
trajectories—the “throughflow” pattern that enters the South China Sea flowing westward along the slope; the loop current
pattern that circulates anticyclonically and returns to the Kuroshio; and the blocked intrusion pattern that penetrates into
the Taiwan Strait through the Penghu Channel. |
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