中国南海是一个半封闭、深海盆、多岛屿(海山)、多连通的边缘海,南海深层水十分活跃,更新时间快,具有典型的南海深层环流特征。综述了目前海洋学家对南海深层水的认知,厘清了南海深层水的来龙去脉,并阐述了南海深层环流的特色。
The South China Sea (SCS) is a semi-enclosed and multi-connected marginal deep sea with a large number of islands (seamounts). The deep SCS circulation is very robust with active deep water renewed. This paper reviews the current understanding of the deep water in the SCS, focusing on its origin and development, as well as the unique features of the SCS deep circulation.
[1] 苏纪兰. 南海环流动力机制研究综述[J]. 海洋学报, 2005, 27(6):1-8.
[2] Qu T, Girton J B, Whitehead J, et al. Deepwater overflow through Luzon Strait[J]. Journal of Geophysical Research, 2006, 111:C01002.
[3] 田纪伟, 曲堂栋. 南海深海环流研究进展[J]. 科学通报, 2012, 57(20):25-30.
[4] Wang G, Xie S P, Qu T, et al. Deep South China Sea circulation[J]. Geophysical Research Letters, 2011, 38:L05601.
[5] Ferrari R, Mashayek A, Mcdougall T J, et al. Turning ocean mixing upside down[J]. Journal of Physical Oceanography, 2016, 46(7):2239-2261.
[6] Tian J, Yang Q, Zhao W, et al. Enhanced diapycnal mixing in the South China Sea[J]. Journal of Physical Oceanography, 2009, 39(12):3191-3203.
[7] Wang D, Wang Q, Cai S, et al. Advances in research of the mid-deep South China Sea circulation[J]. Science China Earth Sciences, 2019, doi:10.1007/s11430-019-9546-3.
[8] Lavelle J W, Mohn C. Motion, commotion, and biophysical connections at deep ocean seamounts[J]. Oceanography, 2010, 23(1):90-103.