

FOLLOWUS
1.Key Laboratory of Ocean Circulation and Waves, Institute of Oceanology, Chinese Academy of Sciences and Qingdao National Laboratory for Marine Science and Technology, Qingdao 266071, China
2.University of Chinese Academy of Sciences, Beijing 100049, China
YIN Baoshu, bsyin@qdio.ac.cn
收稿:2016-12-01,
录用:2017-1-17,
网络首发:2017-02-22,
纸质出版:2018-01
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齐继峰, 尹宝树, 徐振华, 等. Spatiotemporal variations of the surface Kuroshio east of Taiwan Island derived from satellite altimetry data[J]. 海洋湖沼学报(英文), 2018,36(1):77-91.
Jifeng QI, Baoshu YIN, Zhenhua XU, et al. Spatiotemporal variations of the surface Kuroshio east of Taiwan Island derived from satellite altimetry data[J]. Chinese Journal of Oceanology and Limnology, 2018, 36(1): 77-91.
齐继峰, 尹宝树, 徐振华, 等. Spatiotemporal variations of the surface Kuroshio east of Taiwan Island derived from satellite altimetry data[J]. 海洋湖沼学报(英文), 2018,36(1):77-91. DOI: 10.1007/s00343-018-6314-7.
Jifeng QI, Baoshu YIN, Zhenhua XU, et al. Spatiotemporal variations of the surface Kuroshio east of Taiwan Island derived from satellite altimetry data[J]. Chinese Journal of Oceanology and Limnology, 2018, 36(1): 77-91. DOI: 10.1007/s00343-018-6314-7.
Spatiotemporal variation of the surface Kuroshio east of Taiwan Island is investigated by quantitatively analyzing 23-year (1993-2015) sea surface Absolute Dynamic Topography data. The annual mean state of the Kuroshio is shown
with a flow width~136 km and surface transport~7.75×10
4
m
2
/s. The corresponding standard deviations of these are 28 km and 2.14×10
4
m
2
/s. Results of power spectrum analysis indicate that the primary periods of Kuroshio surface transport east of Taiwan Island are 1 and 2.8 years
respectively. Spatially
the Kuroshio surface transport southeast of Taiwan Island has greater variability than that to its northeast. That transport showed strong seasonality
with a maximum 8.8×10
4
m
2
/s in summer and minimum 7.5×10
4
m
2
/s in winter
which was mainly caused by local monsoon winds. A linear long-term upward trend of Kuroshio surface transport during 1993-2015 was found
during which the mean
southeast
and northeast of the Kuroshio east of Taiwan Island increased by 0.30×10
4
0.22×10
4
and 0.36×10
4
m
2
/s
respectively. Correlation and composite analysis show that the Philippines-Taiwan Oscillation (PTO) is important in the interannual variability of the Kuroshio. PTO-induced relative intensity of anticyclonic and cyclonic eddies is the dominant influence on the interannual variability of the Kuroshio east of Taiwan Island.
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