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便携式高频地波雷达东海表面流探测试验
引用本文:文必洋,李自立,周浩,石振华,吴世才,王晓亮,杨华,李四明.便携式高频地波雷达东海表面流探测试验[J].电子学报,2009,37(12):2778-2782.
作者姓名:文必洋  李自立  周浩  石振华  吴世才  王晓亮  杨华  李四明
作者单位:1. 武汉大学电子信息学院,湖北武汉,430079
2. 国家海洋局东海预报中心,上海,200081
3. 武汉德威斯电子技术有限公司,湖北武汉,430074
基金项目:国家高技术研究发展计划,国家自然科学基金 
摘    要: 便携式高频地波雷达系统(OSMAR-S)采用了线性中断调频连续波体制和单极子/交叉环紧凑型天线阵,通过双站合成得到海洋表面矢量流.2007年11月在洋山海域进行了OSMAR-S与其他海洋测量设备的表面流现场探测对比验证试验.试验采用了构成二个断面的五个定点和运用漂流浮标的一个动点同时进行的对比监测方式.试验结果表明了OSMAR-S系统的表面流测量效果与其他海洋测量设备的一致性.

关 键 词:便携式高频地波雷达  海洋表面流  比测  相关系数
收稿时间:2008-11-22

Sea Surface Currents Detection at The Eastern China Sea by HF Ground Wave Radar OSMAR-S
WEN Bi-yang,LI Zi-Li,ZHOU Hao,SHI Zhen-hua,WU Shi-cai,WANG Xiao-liang,YANG Hua,LI Si-ming.Sea Surface Currents Detection at The Eastern China Sea by HF Ground Wave Radar OSMAR-S[J].Acta Electronica Sinica,2009,37(12):2778-2782.
Authors:WEN Bi-yang  LI Zi-Li  ZHOU Hao  SHI Zhen-hua  WU Shi-cai  WANG Xiao-liang  YANG Hua  LI Si-ming
Affiliation:WEN Bi-yang1,LI Zi-Li1,ZHOU Hao1,SHI Zhen-hua1,WU Shi-cai1,WANG Xiao-liang2,YANG Hua2,LI Si-ming3(1.School of Electronic Information,Wuhan University,Wuhan,Hubei 430079,China,2.East China Sea forecasting center,State of Oceanic Administration,Shanghai,200081,3.Wuhan Devices Electronic Technology company Limited,Hubei 430074,China)
Abstract:Portable HF surface wave radar system OSMAR-S adopts Freguency Modulated Interrupted Continuous Waveform (FMICW) and Orthogonal Loop/Whip Antenna Arrays. OSMAR-S obtians surface vector currents by composeing two station sur-face radical currents. Verification tests of OSMAR-S system against in situ neamurements had been accomplished on Nov. 12 ~ 17, 2007.A observing method of fixed five-point and a movable point simultaneity comparison was used in the test. This paper intro-duces the system Structure of OSMAR-S system, and then presents comparison results of surface currents measurements. The results indicate the OSMAR-S system is meet the need of design.
Keywords:portable HF ground wave radar system  sea surface current  compared to measuring  correlation coefficie
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