“…Comparatively, on the surface of 25.7 kg/m 3 corresponding to the subsurface-intermediate layer, there are no clear intrusion features, revealing either homogeneous characteristics of water masses or a relatively weak east-west movement of water masses in this layer. Moreover, some high potential spicity patches can be detected in the central NSCS on the 22.9 and 24.5 kg/m 3 surfaces, which could be the signature of nonlinear Rossby eddies propagating into the NSCS through the Luzon Strait from the WPO (e.g., Cheng et al, 2014;Hu et al, 2012;Xie et al, 2016;Zheng et al, 2011Zheng et al, , 2017Zhu et al, 2019). The WPUW can traverse westward through the Luzon Strait and mix with the SUW, resulting in a subsequent decrease in its potential spicity, but it still has higher potential spicity than the local water.…”