摘要
一、引言南黄海是一个平均深度不超过45米的陆架浅海。其独有的地理条件,使该海域潮运动独具特征。早从本世纪三十年代开始,日本学者就已对黄海的潮汐进行了研究。近年来,我国、苏联、日本和南朝鲜等国学者又运用数值计算等方法进一步探讨了该海域的潮汐、潮流运动。然而,这些研究多偏重于揭示海域潮波运动的规律。对潮流的计算基本上未经实测资料校核。尤其是,对于由潮流的非线性效应所产生的潮汐余流研究甚少。
In. this article, a two-dimensional, non-linear numerical model is used to study the tidal and tide-induced residual currents in the southern Huanghai Sea. The results obtained with the model are strongly supported by observations available. The main features of the tidal and tide-induced residual currents in the southern Huanghai Sea are presented by analysing the results calculated.
出处
《海洋湖沼通报》
CSCD
北大核心
1989年第2期1-7,共7页
Transactions of Oceanology and Limnology
