2019
DOI: 10.1007/s13131-019-1418-2
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Classification and 3-D distribution of upper layer water masses in the northern South China Sea

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Cited by 16 publications
(15 citation statements)
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“…These water mass centers are illustrated in Figure 7b as brown triangles (the ZDW is also ignored). There are several differences and similarities between our results and those of Zhu et al (2019). For example, in the surface layer, surface-subsurface mixed layer, and subsurface-intermediate mixed layer, the fuzzy cluster and TSSN analysis did not distinguish the water sourcing from the NSCS or from the WPO.…”
Section: 1029/2019jc015676contrasting
confidence: 73%
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“…These water mass centers are illustrated in Figure 7b as brown triangles (the ZDW is also ignored). There are several differences and similarities between our results and those of Zhu et al (2019). For example, in the surface layer, surface-subsurface mixed layer, and subsurface-intermediate mixed layer, the fuzzy cluster and TSSN analysis did not distinguish the water sourcing from the NSCS or from the WPO.…”
Section: 1029/2019jc015676contrasting
confidence: 73%
“…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.…”
Section: Discussionmentioning
confidence: 99%
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