高频地波雷达反演海浪的海上对比验证方法研究  

A Technological Study of Sensing Ocean Hydrological Parameters with High Frequency Ground Wave Radar

作　　者：韩树宗[1] 王海龙[1] 郭佩芳[1] 赵可胜[1] 

机构地区：[1]青岛海洋大学海洋环境学院,青岛266003

出　　处：《青岛海洋大学学报（自然科学版）》2002年第5期687-694,共8页Journal of Ocean University of Qingdao

基　　金：国家 8 6 3海洋高科技发展计划项目(818- 0 1- 0 2 )资助

摘　　要：在介绍高频地波雷达反演海浪要素工作原理的基础上 ,利用 2 0 0 0年 10月在浙江舟山海域进行的 OSMAR2 0 0 0和 SZF1- 海上对比验证实验中所获取的资料进行系统比较分析 ,验证了OSMAR2 0 0 0探测海洋海浪要素的精度 ,并分析了 OSMAR2 0 0Compared with the traditional ocean investigation methods, the high frequency ground wave radar(HF radar) has many evident advantages. After the completion of the equipment and corresponding inversion software, it is necessary to conduct test at sea to verify the function and precision of the HF radar. Because of the fundamental difference in the method of data collection between the HF radar and traditional wave measuring instruments, the method of test has to be studied systemetically and thoroughly. Based on the elucidation of the principle of inversion of the HF radar backscatter data to obtain ocean wave elements, this paper makes a systematic analysis and comparison of the data collected with the OSMAR 2000 and SZF1 Ⅱ during the sea test condueted from October to November, 2000 in the Zhoushan area, Zhejiang Province. The precision of the OSMAR2000 in wave elements detection is verified and the sources of error in the inversion are discussed.

关 键 词：高频地波雷达 海浪 对比验证 风浪场 有效波高 

分 类 号：P731.22[天文地球—海洋科学] P715.6