中文摘要：

一个数字方法被设计检验真实的海区域的反应性质打开强迫的海洋。到为瓷器邻近的海建模的这个方法的申请证明 Bohai 海有 1.52 d 的最高的山峰反应频率(PRF )< 啜 class= “ a-plus-plus ” > 1 ；北黄海有 1.69 d 的 PRF < 啜 class= “ a-plus-plus ” > 1 ；Gyeonggi 海湾从 1.7 ～ 2.7 d 粗略地在频率乐队有一个高振幅获得高原 < 啜 class= “ a-plus-plus ” > 1 ；黄海(包括 Gyeonggi 海湾)，华东海架和台湾海峡在 1.76～1.78 d 附近与频率有一个普通高振幅获得乐队<啜class=“ a-plus-plus ”> 1 并且被显示是对强迫赞成在这与频率放大波浪的开的海洋作出回应的一个系统乐队；Beibu 海湾，泰国的海湾和华南海深盆有 0.91， 1.01 和 0.98 d 的 PRF < 啜 class= “ a-plus-plus ” > 1 分别地。另外，华东海有 3.91 d 的 Poincare 模式 PRF < 啜 class= “ a-plus-plus ” > 1 。Bohai 海，北黄海， Beibu 海湾和华南海的 PRF 能到一个古典季度(为 Bohai 海的一半) 被解释波长回声理论。结果证明进一步的调查为泰国的黄海东方中国海台湾海峡系统，华东海 Poincare 模式，台湾海峡，和海湾的反应动力学被需要。

英文摘要：

A numerical method is designed to examine the response properties of real sea areas to open ocean forcing. The application of this method to modeling the China＇s adjacent seas shows that the Bohai Sea has a highest peak response frequency （PRF） of 1.52 d^-1; the northern Yellow Sea has a PRF of 1.69 d^-1; the Gyeonggi Bay has a high amplitude gain plateau in the frequency band roughly from 1.7 to 2.7 d^-1; the Yellow Sea （includ- ing the Gyeonggi Bay）, the East China Sea shelf and the Taiwan Strait have a common high amplitude gain band with frequencies around 1.76 to 1.78 d^-1 and are shown to be a system that responds to the open ocean forcing in favor of amplifying the waves with frequencies in this band; the Beibu Gulf, the Gulf of Thailand and the South China Sea deep basin have PRFs of 0.91, 1.01 and 0.98 d^-1 respectively. In addition, the East China Sea has a Poincare mode PRF of 3.91 d^-1. The PRFs of the Bohal Sea, the northern Yellow Sea, the Bei- bu Gulf and the South China Sea can be explained by a classical quarter （half for the Bohai Sea） wavelength resonance theory. The results show that further investigations are needed for the response dynamics of the Yellow Sea-East China Sea-Taiwan Strait system, the East China Sea Poincare mode, the Talwan Strait, and the Gulf of Thailand.