The influence of turbulent mixing on the subsurface chlorophyll maximum layer in the northern South China Sea

Author:

Shang Chenjing,Liang Changrong,Chen Guiying,Gao Yongli

Publisher

Springer Science and Business Media LLC

Subject

Water Science and Technology,Oceanography

Reference50 articles.

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2. Cullen J J. 2015. Subsurface chlorophyll maximum layers: enduring enigma or mystery solved? Annual Review of Marine Science, 7: 207–239, https://doi.org/10.1146/annurev-marine-010213-135111.

3. Egbert G D, Erofeeva S Y. 2002. Efficient inverse modeling of barotropic ocean tides. Journal of Atmospheric and Oceanic Technology, 19(2): 183–204, https://doi.org/10.1175/1520-0426(2002)019<0183:EIMOBO>2.0.CO;2.

4. Gan J P, Lu Z M, Dai M H, Cheung A Y Y, Liu H B, Harrison P. 2010. Biological response to intensified upwelling and to a river plume in the northeastern South China Sea: a modeling study. Journal of Geophysical Research: Oceans, 115(C9): C09001, https://doi.org/10.1029/2009JC005569.

5. Gong X, Shi J, Gao H W. 2014. Modeling seasonal variations of subsurface chlorophyll maximum in South China Sea. Journal of Ocean University of China, 13(4): 561–571, https://doi.org/10.1007/s11802-014-2060-4.

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