Circulation in the South China Sea is in a state of forced oscillation: Results from a simple reduced gravity model with a closed boundary
Author:
Publisher
Springer Science and Business Media LLC
Subject
Aquatic Science,Oceanography
Link
https://link.springer.com/content/pdf/10.1007/s13131-022-2013-5.pdf
Reference17 articles.
1. Cai Shuqun, Long Xiaomin, Wu Renhao, et al. 2008. Geographical and monthly variability of the first baroclinic Rossby radius of deformation in the South China Sea. Journal of Marine Systems, 74(1–2): 711–720, doi: https://doi.org/10.1016/j.jmarsys.2007.12.008
2. Chu P C, Edmons N L, Fan Chenwu. 1999. Dynamical mechanisms for the South China Sea seasonal circulation and thermohaline variabilities. Journal of Physical Oceanography, 29(11): 2971–2989, doi: https://doi.org/10.1175/1520-0485(1999)029<2971:DMFTSC>2.0.CO;2
3. Fang Wendong, Fang Guohong, Shi Ping, et al. 2002. Seasonal structures of upper layer circulation in the southern South China Sea from in situ observations. Journal of Geophysical Research: Oceans, 107(C11): 3202, doi: https://doi.org/10.1029/2002JC001343
4. Gan Jianping, Li H, Curchitser E N, et al. 2006. Modeling South China Sea circulation: Response to seasonal forcing regimes. Journal of Geophysical Research: Oceans, 111(C6): C06034
5. He Zhigang, Lyu Kewei, Quan Qi. 2020. The South China Sea western boundary current. In: Hu J, Ho C R, Xie L, et al., eds. Regional Oceanography of the South China Sea. Singapore: World Scientific, 77–99
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