2015
DOI: 10.1016/j.pocean.2014.05.012
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Kuroshio intrusion into the South China Sea: A review

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Cited by 273 publications
(216 citation statements)
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“…The intrusion of the Kuroshio loop current into the Luzon Strait is generally observed from November to March as a result of the northeast monsoon during the winter (e.g., Hsin et al 2012;Nan et al 2015). Observational data show that the anticyclonic intrusion of the Kuroshio can occur during any season, although winter is the most favorable time of the year (Yuan et al 2006).…”
Section: Seasonal Comparisonmentioning
confidence: 99%
“…The intrusion of the Kuroshio loop current into the Luzon Strait is generally observed from November to March as a result of the northeast monsoon during the winter (e.g., Hsin et al 2012;Nan et al 2015). Observational data show that the anticyclonic intrusion of the Kuroshio can occur during any season, although winter is the most favorable time of the year (Yuan et al 2006).…”
Section: Seasonal Comparisonmentioning
confidence: 99%
“…As pointed out in Hu et al (2000), there were four main features of the Kuroshio intrusion as follows: a direct branch from the Kuroshio (Williamson, 1970;Fang et al, 1996;Chern and Wang, 1998;Qu et al, 2000), a form of loop (Zhang et al, 1995;Liu et al, 1996;Farris and Wimbush, 1996), a form of extension (Hu et al, 1999), and a form of ring (Li et al, 1998a, b) at present. Nan et al (2015) reviewed and summarized the Kuroshio intruding processes from observed data, numerical experiments, and theoretical analyses, and concluded that there were three typical paths of the Kuroshio intruding the SCS, the looping path, the leaking path, and the leaping path, which could be distinguished quantitatively by a Kuroshio SCS Index (Nan et al, 2011a) derived from the integral of geostrophic vorticity southwest of Taiwan. The three paths can change from one to another over several weeks.…”
Section: Introductionmentioning
confidence: 99%
“…Therefore, strong NIGWs near the Luzon Strait can be detected in the deep SCSMOC south of the Luzon Strait as far as 10 • N. Although the Kuroshio intrusion is a low-frequency process, it can provide the background vorticity field for the vertical propagation through the chimney effect (Lee and Niiler, 1998;Zhai et al, 2005) because negative vorticity west of the Kuroshio near the Luzon Strait always exists. When the Kuroshio intrusion changes states among the looping path, the leaking path, and the leaping path (Nan et al, 2014), the geostrophic adjustment also triggers near-inertial waves. This process is well depicted by Nagai et al (2015) in relation to the Kuroshio meander.…”
Section: Discussionmentioning
confidence: 99%