利用X波段导航雷达探测海洋表面流速的方法  

A Method to Detect Ocean Surface Current Based on X-Band Marine Radar

作　　者：王立[1] 吴雄斌[1] 马克涛[1] 沈志奔[1] 

机构地区：[1]武汉大学电子信息学院,湖北武汉430072

出　　处：《武汉大学学报（信息科学版）》2015年第1期90-95,共6页Geomatics and Information Science of Wuhan University

基　　金：国家863计划资助项目(2012AA091701);中央高校自主科研资助项目(2014212020203)~~

摘　　要：针对X波段导航雷达对海杂波的成像,研究了利用多谱勒频移和布拉格散射来探测海表面流的方法。提出了一种结合几何滤波模型的X波段雷达海流反演预处理算法,此算法不需要已知的最大海流流速进行带通滤波处理,结合线性波理论色散方程以及最小二乘算法,可以得到精确的海表面流速。与传统的X波段导航雷达测流方法相比,该算法简单高效,占用资源少,并且不仅适用于岸基X波段导航雷达,还适用于船载X波段导航雷达。与附近站点高频地波雷达表面流数据进行对比实验,二者结果的一致性表明了本文方法是可行的。A detection method for ocean surface currents based on the Doppler shift and Bragg scattering for sea clutter imaging using X-band marine radar is addressed in this research. A preprocessing algorithm for current inversion combined with geometric filtering model is presented. Maximun current velocity is not required for band-pass filter processing, since accurate current velocity can be obtained only with liner wave theory dispersion equation and a least-squares algorithm. As compared with the conventional flow detection method using X-band navigation radar, this new algorithm is simple and efficient. It uses resources effectively, and can be applied to both shore-based X-band and shipborne X-band navigation radar. A validation comparison with sea surface current data from a nearby HFGWR shows that this algorithm effectively improves the accuracy and stability of the radar.

关 键 词：X波段导航雷达 海洋表面流速 几何滤波模型 线性波理论 高频地波雷达 最小二乘法 

分 类 号：P234.4[天文地球—摄影测量与遥感] P237[天文地球—测绘科学与技术]