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A reduced thermodynamic model on the formation of the Nansha warm water

Acta Oceanologica Sinica 2004年第2期23卷 239-249页

作者： CAIShuqun GANZijun LIChiwai longxiaomin DONGDanpeng LED SouthChinaSeaInstituteofOceanologyChineseAcademyofSciencesGuangzhou510301China HongKongPolytechnicUniversity HongKongChina

A reduced vertically integrated upper mixed layer model is set up to numerically study the thermodynamic process of the formation of the 'Nansha warm water'(NWW) in the Nansha Islands sea areas in spring. According to the numerical experiments, it is shown that, in spring, the formation of the NWW is mainly due to the sea surface net heat flux and the local weak current strength; the contribution from temperature advection transport and warm water exchange with the outer seas (Sulu Sea or south of Sunda shelf) is very little. In the sea areas where the current is strong, the advection may also play an important role in the temperature field.

关键词： numerical modeling warm water thermodynamic process Nansha Islands South China Sea

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Numerical study on the summer circulation of the upper South China Sea and its establishment

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Acta Oceanologica Sinica 2005年第1期24卷 31-38页

作者： CAIShuqun SUJilan longxiaomin WANGShengan HUANGQizhou LED SouthChinaSeaInstituteofOceanologyChineseAcademyofSciencesGuangzhou510301China LOPSO SecondInstituteofOceanographyStateOceanicAdministrationHangzhou310012China

A coupled single-layer/two-layer model is employed to study the South China Sea (SCS) upper circulation and its response before and after the onset of summer monsoon. It is found that, in summer, due to the β effect and the first baroclinic mode of the wind-driven current, a northward western boundary jet current is formed along the Indo-China Peninsula coast, and it leaves the coast at about 13° N and diffuses towards northeast; next to the Indo-China Peninsula, a large anticyclonic gyre in the southern SCS and a cyclonic eddy to the north of this gyre are induced. There are two possible mechanisms for the generation of this anticyclonic gyre: first, it is induced by the summer wind stress curl; second, it is associated with the westward moving of two anticyclonic eddies, which are originally generated to the west of Palawan Island and over the Nansha Trough respectively, in winter. The cyclonic eddy north of this anti-cyclonic gyre may be induced by the summer wind stress curl or related to the southwestward moving of the cyclonic eddy/gyre induced by the Kuroshio branch in the northern SCS.

关键词： numerical modeling circulation monsoon eddy South China Sea

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