Intensification of the Winter South China Sea Western Boundary Current During 2014–2024

IF 3.3 2区 地球科学 Q1 OCEANOGRAPHY
Xuwen Wang, Qiang Wang, Lili Zeng, Rui Shi, Yikai Yang, Ju Chen, Yunkai He
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引用次数: 0

Abstract

Understanding the low-frequency variability of the western boundary current (WBC) is essential for the redistribution of heat, salt and energy in the South China Sea (SCS). Long-term acoustic Doppler current profiler (ADCP) mooring observations show a strengthening trend in the winter SCS WBC from 2014 to 2024. Diagnosis of the vorticity budget suggests that the trend is primarily attributed to the enhanced basin-scale wind stress curl and secondarily to the weakening of the joint effect of baroclinicity and relief (JEBAR), which overall serves as a vorticity sink. The trend of JEBAR is associated with a warming center west of the Luzon Strait, which enhances the baroclinic effect along the northern SCS continental slope, leading to a positive trend of JEBAR and weakening of vorticity consumption.

2014-2024年冬季南海西部边界流的增强
了解南海西部边界流的低频变率对南海热、盐、能的再分配具有重要意义。长期声学多普勒电流廓线(ADCP)系泊观测显示,2014 - 2024年冬季南海WBC有增强趋势。涡度收支诊断表明,这一趋势主要是由于盆地尺度风应力旋度的增强,其次是斜压和缓压联合效应(JEBAR)的减弱,后者总体上起到涡度汇的作用。JEBAR趋势与吕宋海峡以西的暖化中心有关,该暖化中心增强了南海北部大陆坡的斜压效应,导致JEBAR呈正趋势,涡度消耗减弱。
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来源期刊
Journal of Geophysical Research-Oceans
Journal of Geophysical Research-Oceans Earth and Planetary Sciences-Oceanography
CiteScore
7.00
自引率
13.90%
发文量
429
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