An Empirical Mode Decomposition Method for Sea Surface Wind Measurements From X-Band Nautical Radar Data

被引:32
|
作者
Huang, Weimin [1 ]
Liu, Xinlong [1 ]
Gill, Eric W. [1 ]
机构
[1] Mem Univ Newfoundland, Fac Engn & Appl Sci, St John, NF MEM UNIV NE, Canada
来源
基金
加拿大自然科学与工程研究理事会;
关键词
Ensemble empirical mode decomposition (EEMD); rain; wind; X-band nautical radar; IMAGE SEQUENCES; OCEAN; RETRIEVAL; WAVES; RAIN;
D O I
10.1109/TGRS.2017.2723431
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, sea surface wind direction and speed are obtained from X-band nautical radar images. A data control strategy is proposed to distinguish rain-free and rain-contaminated radar data. The radar data are decomposed by an ensemble empirical mode decomposition method into several intrinsic mode functions (IMFs) and a residual. A normalization scheme is applied to the first IMF to obtain the amplitude modulation (AM) component. Wind direction is determined from the residual for the rain-free and high-wind-speed rain-contaminated data, and from the AM portion of the first IMF for the low-wind-speed rain-contaminated data, based on curve fitting a harmonic function. Wind speed is determined from a combination of the residual and the AM part of the first IMF for both rain-free and rain-contaminated data using a logarithmic relationship. Results employing ship-borne radar and anemometer data collected in a sea trial off the east coast of Canada are presented. The root-mean-square differences for wind direction and speed measurements are 11.5 degrees and 1.31 m/s, respectively, compared with reference values from anemometers.
引用
收藏
页码:6218 / 6227
页数:10
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