Abstract

Synthetic aperture radar (SAR) is an important means of estimating significant wave height with obvious advantages of all-day, all-weather, high resolution and wide swath coverage. At present, the estimation methods of significant wave height are based on visible ocean waves in SAR images. However, due to the characteristic of long integration time for low-frequency SAR (such as P-band, L-band), the ocean waves are usually invisible in SAR images. In addition, in the case that there are multiple wave systems, significant wave height of only one wave system can be estimated for the reason that only a blurred wave system can be observed in SAR images. In order to solve the above two problems, a method of estimating significant wave height from SAR with long integration times is proposed in this paper. Firstly, each ocean wave system is refocused from single-look complex (SLC) data, respectively. Then, without any additional processing, the 180° ambiguity of wave propagation direction is removed based on the optimum focus setting. Finally, significant wave height is estimated in combination with azimuth cutoff, wavelength and propagation direction of ocean waves. This method is applied to two airborne SAR field data with long integration times. One case is that ocean waves are invisible in SAR images, the other is that there are two wave systems on the real ocean surface, but only one is visible in the SAR images. The results show that the proposed method can estimate significant wave height in the cases of invisible ocean waves and multiple ocean waves. The estimation results of significant wave height are compared with the European Centre for Medium-Range Weather Forecast (ECMWF) data, and the error is basically stable within 0.2 m, which verifies the effectiveness of the proposed method.

Highlights

  • National Key Lab of Microwave Imaging Technology, Beijing 100190, China; Aerospace Information Research Institute, Chinese Academy of Sciences, Beijing 100190, China

  • In order to solve the problems that the present methods cannot estimate the significant wave height when the ocean waves are invisible and that can estimate the significant wave height of only one wave system in the case of multiple wave systems, a method of estimating significant wave height from Synthetic aperture radar (SAR) with long integration times is proposed in this paper

  • When long integration time SAR observes the ocean, the motion of ocean waves will have a great impact on the imaging quality, resulting in waves blurred or even invisible in SAR images

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Summary

Introduction with regard to jurisdictional claims in

Waves are the ocean’s most obvious surface feature. Significant wave height (SWH) is defined as the average of the highest one-third of the observed waves [1]. In order to solve the problems that the present methods cannot estimate the significant wave height when the ocean waves are invisible and that can estimate the significant wave height of only one wave system in the case of multiple wave systems, a method of estimating significant wave height from SAR with long integration times is proposed in this paper. The clear SAR images of ocean waves can be obtained by refocusing, breaking through the limitation that the present methods cannot estimate the significant wave height when the wave texture is invisible from SAR with long integration times.

Estimating Significant Wave Height from SAR with Long Integration Times
Pre-Processing
Significant Wave
Azimuth Cutoff Calculation
Ocean Wave Refocusing
Scanning Distortion Calibration
Wavelength and Propagation Direction Calculation of nth Ocean Waves
Propagation Direction Calculation of nth Ocean Wave
Significant Wave Height Estimation
Experiments of Estimating Significant Wave Height from SAR with Long
Case 1-Invisible Ocean Waves from SAR with Long Integration Times
Case 2-Multiple Ocean Waves from SAR with Long Integration Times
Experiment of Significant Wave Height Estimation of the First Ocean Waves
Experiment of Significant Wave Height Estimation of the Second Ocean Wave
Validation of the Experimental Results With ECMWF
Sensitivity Analysis of Significant Wave Height Estimation
Sensitivity Analysis of Significant Wave Height to Azimuth Cutoff
Sensitivity Analysis of Significant Wave Height to Wavelength of Ocean Waves
Sensitivity Analysis of Significant Wave Height to Propagation Direction of
Conclusions
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