南海表层水温年循环的数值模拟

王东晓

南海表层水温年循环的数值模拟

王东晓

中国科学院大气物理研究所大气科学和地球流体力学数值模拟国家重点实验室, 北京 100080

基金项目: 中国气象局气候研究开放实验室和国家自然科学基金项目联合资助.

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出版历程
- 收稿日期: 1997-02-10
- 修回日期: 1997-02-24

Numerical modelling on annual cycle in sea surface temperature in the South China Sea

Wang Dongxiao

State Key Laboratory of Numerical Modelling for Atmospheric Sciences and Geophysical Fluid Dynamics (LASG), Institute of Atmospheric Physics, Chinesr Academy of Sciences, Beijing 100080

摘要

摘要: 本文采用一个非线性约化重力海洋模式对南海表层水温(SST)年循环过程进行了数值研究,探讨了南海表层水温年循环形成和维持的动力学和热力学机制·模拟结果表现出与观测分析相一致的年循环变化阶段性和空间结构,并发现南海SST年循环的阶段性是海面动力强迫和热力强迫共同作用的结果;南海上层海洋的热力平衡有着明显的季节特征.
- 南海表层水温 /
- 年循环 /
- 约化重力模式
Abstract: A nonlinear reduced-gravity oceanic model was applied to simulate the annual cycle in sea surface temperature in the South China Sea.Dynamic and thermodynamic mechanisms for formation and maintenance on the annual cycle were documented in series of numerical experiments forced by observational wind stresses and surface heat fluxes.The influences caused by changes in the external forcing functions and in the parameterization of entrainment occurring at the bottom of the upper mixed layer were investigated in this paper.Results showed that the variation stage and the spatial structure similar to observed climatology in the South China Sea had been achieved.It was found that the annual cycle was attributed to both wind stirring and surface heating.Moreover,the thermal balance in the upper layer in the South China Sea was strong seasonal time-dependent.
- Sea surface temperature in the South China Sea /
- annual cycle /
- reduced-gravity model

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参考文献(15)

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