The Kuroshio flow-through in the East China Sea: A numerical model
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Cited by (37)
Structural characteristics of the Chiwei Platform and their implications for the back-arc rifting of the Okinawa Trough, East China Sea
2022, Marine and Petroleum GeologyCitation Excerpt :As the western boundary current of the Pacific Ocean, the Kuroshio Current enters the East China Sea through the East Taiwan Channel (Hsueh et al., 1997) between Taiwan and Yonaguni Island and then leaves through the Tokara Strait (Fig. 1a). In the East China Sea, the main stream of the Kuroshio Current flows northeastward along the continental margin and the western Okinawa Trough (Hsueh et al., 1997). As a strong warm current, the volume transport of the Kuroshio in the East China Sea was estimated to be ∼23–29 Sv (1 Sv = 1 × 106 m3/s) (Ichikawa and Beardsley, 1993; Yuan et al., 1998; Liu and Yuan, 1999; Zhu et al., 2006).
Weakened Yellow Sea Warm Current over the last 2-3 centuries
2014, Quaternary InternationalCitation Excerpt :Physical oceanographic observation studies (e.g. Xie et al., 2002; Huang et al., 2005; Xu et al., 2009) suggest that the YSWC intensity is largely controlled by the local wind and the Kuroshio Current originating from the North Equatorial Current in the Western Pacific. The Kuroshio Current strongly influences the upper-ocean thermal structure and the distribution of marine sediments in the ECS and YS regions (Hsueh et al., 1997). Further, the East Asian monsoon, especially the winter monsoon activities, could also affect the strength of the YSWC (Yuan and Hsueh, 2010).