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机构地区:[1]中海油能源发展股份有限公司北京分公司,北京100027 [2]中国海洋大学海洋环境学院,青岛266100
出 处:《海洋与湖沼》2011年第6期906-912,共7页Oceanologia Et Limnologia Sinica
基 金:国家自然科学基金项目;40706055号
摘 要:为了克服基于两层海洋的内孤立波SAR遥感仿真模型的缺陷,使用基于连续分层海洋模型的GK-dV方程,在南海东北部深水海域进行了大振幅内孤立波传播模拟,模拟输出内孤立波振幅91.0m,半波宽度262.0m。然后使用新建立的基于连续分层海洋模型的内孤立波SAR遥感仿真模型进行了内孤立波反演,反演出内孤立波半波宽度251.5m,相对输入误差为4.0%,比旧模型的34.2%有了较大改进。In order to improve the simulation results of the SAR (Synthetic aperture radar) signatures on the basis of two-layer oceanic model, the simulation of the propagation of the large-amplitude internal solitary waves in the deep northeast South China Sea was made based on a continuous stratified oceanic model using the GK-dV equation, the simulation results of the amplitude and half-width of internal solitary wave were 91.0 m, 262.0 m respectively. The simulation of the SAR signatures of the large-amplitude internal solitary waves was also made, the simulation of half-width is 251.5 m, relative error was only 4.0%, far less than the relative error of 34.2% based on the traditional model.
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