Surface Current Measurements Using X-Band Marine Radar With Vertical Polarization

被引:46
|
作者
Huang, Weimin [1 ]
Carrasco, Ruben [2 ]
Shen, Chengxi [1 ]
Gill, Eric W. [1 ]
Horstmann, Jochen [2 ]
机构
[1] Mem Univ Newfoundland, Fac Engn & Appl Sci, St John, NF A1B 3X9, Canada
[2] Helmholtz Zentrum Geesthacht, Ctr Mat & Coastal Res, Dept Radar Hydrog, D-21502 Geesthacht, Germany
来源
IEEE TRANSACTIONS ON GEOSCIENCE AND REMOTE SENSING | 2016年 / 54卷 / 05期
基金
加拿大自然科学与工程研究理事会;
关键词
Marine radar; remote sensing; surface current; vertical polarization; OCEAN WAVE; ALGORITHM;
D O I
10.1109/TGRS.2015.2509781
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
In this paper, the retrieval of sea surface current velocity from vertically polarized (V-pol) X-band marine radar data is presented. Three different methods, including the iterative least square approach, the normalized scalar product method, and the polar current shell algorithm, that have been used for horizontally polarized data are employed here. A comprehensive comparison of the performance of the three methods is conducted using the radar images collected by the V-pol radar deployed on the Forschungsplattformen in Nord- und Ostsee No. 3 (FINO3) offshore research platform and the acoustic Doppler current profiler (ADCP) data in the North Sea. The results indicate that all three methods are capable of providing reliable current speed and direction measurements from V-pol data, with similar performance. Based on the experimental data for which the current magnitude is less than 0.5 m/s, the radar-derived results agree best with the ADCP data at a depth of 6-8 m, with the root mean square difference for current velocity x- and y-components being 7.2-8.9 cm/s. The correlation coefficients between the radar-derived and ADCP-measured current velocity components are as high as 0.87-0.93.
引用
收藏
页码:2988 / 2997
页数:10
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