摘要
本文用二维流体动力学差分方法计算了南海北部的半日潮与全日潮,得到与实际观测符合良好的结果。根据计算结果给出了潮汐、潮流和能通量的分布。文章还对陆架上潮汐增大的现象作了动力学解释。
Diurnal and semi-diurnal tides and tidal currents in the north part of South China Sea are calculated by using twodimensional finite-difference method. The model-produced results agree well with the observational data. The charts of tides, tidal currents and tidal energy fluxes are given. The amplification of the tides on the South China shelf is explained by means of the theory of Clarke and Battisti.
出处
《热带海洋》
CSCD
1990年第2期63-70,共8页
基金
中国科学院资源环境局和原合同局的支持和资助
