摘要
利用伴随同化法得到的开边界和底摩擦数据,数值模拟了渤黄东海的M2分潮。计算出M2分潮调和常数的模拟值与实测值之差的绝对平均值:振幅差为3.46cm,迟角差为3.89°。得到M2分潮的潮汐潮流等结果,较好地反映了东中国海M2分潮的特征。
The open boundaries and the bottom friction coefficients obtained by adjoint method were used in the Mtide modal in the Bohai Sea, the Huanghai Sea and the East China Sea. The mean absolute differ- ences between the simulated and the observed were computed. The mean absolute difference of the amplitude is 3.46 cm, and the mean absolute difference of the phase-lag is 3.89°. Based on the computational results, the Mtide cotidal chart and ellipticity and rotating direction of current vector chart was mapped out. These results reflected the characteristics of the Mtide very well.
出处
《浙江海洋学院学报（自然科学版）》
CAS
2006年第3期278-281,共4页
Journal of Zhejiang Ocean University(Natural Science Edition)
基金
浙江海洋学院自然科学青年基金(X04QL01)
关键词
东中国海
M2分潮
潮汐潮流
数值模拟
伴随方法
The Bohai sea, the Huanghai sea and the East China Sea
Mtides
tide and tidal current
numerical simulation
adjoint method.
作者简介
周华民（1981-），男，浙江常山人，研究方向：物理海洋学、港口、海岸及近海工程．
