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Observed evidence of the anomalous S outh C hina S ea western boundary current during the summers of 2010 and 2011
Author(s) -
Shu Yeqiang,
Xue Huijie,
Wang Dongxiao,
Xie Qiang,
Chen Ju,
Li Jian,
Chen Rongyu,
He Yunkai,
Li Daning
Publication year - 2016
Publication title -
journal of geophysical research: oceans
Language(s) - English
Resource type - Journals
eISSN - 2169-9291
pISSN - 2169-9275
DOI - 10.1002/2015jc011434
Subject(s) - ocean gyre , geology , anticyclone , climatology , current (fluid) , anomaly (physics) , mooring , submarine pipeline , oceanography , boundary current , ocean current , subtropics , physics , condensed matter physics , fishery , biology
Seven years of directly measured current data from a mooring in the Xisha area of the South China Sea (SCS), together with shipboard ADCP and satellite data, have shown the western boundary current (WBC) anomaly and its vertical structure during the summers of 2010 and 2011. The observed WBC presented obvious year‐to‐year variability, especially in the summer. Overall, the summer mean velocity at the mooring site over 7‐year (2007–2013) was northeastward. The moored ADCP showed that the northeastward velocity was particularly strong in the summer of 2010, but the increase was confined in the upper 120 m. In contrast, the northeastward current disappeared throughout the observed depth range (from 50 to 450 m) in the summer of 2011. Even at the deepest observed position, the monthly velocity anomalies reached 14 cm s −1 westward and 12 cm s −1 southward in the zonal and meridional directions, respectively. Both the Vietnam offshore current (VOC) and double gyres in the western SCS disappeared and the southern anticyclonic gyre expanded to strengthened the northward WBC in the summer of 2010. However, in summer of 2011, the VOC intensified, and the northern cyclonic gyre enlarged with its northern edge reaching 18°N, slightly north of mooring site, which weakened the northeastward WBC. The observed SCS circulation anomalies during 2010 and 2011 were mainly induced by the basin‐scale wind field anomalies associated with the 2009/2010 El Niño and 2010/2011 La Niña.