中文摘要：

地震海洋学是一新思考地震学和物理海洋学跨纪律。地震海洋学和传统的思考地震学之间的最大的差别是它变化时间的海水的研究目标。怎么估计水里的反射镜的时间的变化在地震数据组织并且做一些修正是在地震海洋学研究的基本问题。这为海水运动的评价的一个方法基于反射镜被提供。这个方法到的应用程序结果模仿并且外面回答地震数据拐弯可接受。作为与以前的研究相比，这个方法有的优点在迁居速度和反射镜的剧降上低依赖，并且它对修正在很合适一光谱用地震数据的分析，它在海洋精力的研究是很有用的预算。

英文摘要：

Seismic oceanography is a new cross-discipline of reflection seismology and physical oceanography. The biggest difference between seismic oceanography and traditional reflection seismology is its research object of time-varied seawater. How to estimate the temporal variations of reflectors in water structure and make some corrections in seismic data are basic problems in seismic oceanography research. Here a method of estimation for seawater movement is provided based on the reflectors. The application results of this method to the simulated and field seismic data turn out to be acceptable. As compared with the previous research, this method has the advantages of low-dependence on migration velocity and dip of reflectors, and it is very suitable for correction in a spectral analysis using seismic data, which is very useful in the research of ocean energy budget.