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首页> 外文期刊>IEEE Journal of Oceanic Engineering >Wind- and wave-field measurements using marine X-band radar-image sequences
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Wind- and wave-field measurements using marine X-band radar-image sequences

机译:使用海洋X波段雷达图像序列进行风场和波场测量

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This paper describes two algorithms for the retrieval of high-resolution wind and wave fields from radar-image sequences acquired by a marine X-band radar. The wind-field retrieval algorithm consists of two parts. In the first part, wind directions are extracted from wind-induced streaks, which are approximately in line with the mean surface wind direction. The methodology is based on the retrieval of local gradients from the mean radar backscatter image and assumes the surface wind direction to be oriented normal to the local gradient. In the second part, wind speeds are derived from the mean radar cross section. Therefore, the dependence of the radar backscatter on the wind vector and imaging geometry has to be determined. Such a relationship is developed by using neural networks (NNs). For the verification of the algorithm, wind directions and speeds from nearly 3300 radar-image sequences are compared to in situ data from a colocated wind sensor. The wave retrieval algorithm is based on a methodology that, for the first time, enables the inversion of marine radar-image sequences to an elevation-map time series of the ocean surface without prior calibration of the acquisition system, and therefore, independent of external sensors. The retrieved ocean-surface elevation maps are validated by comparison of the resulting radar-derived significant wave heights, with the significant wave heights acquired from three colocated in situ sensors. It is shown that the accuracy of the radar-retrieved significant wave height is consistent with the accuracy of the in situ sensors.
机译:本文介绍了两种从船用X波段雷达获取的雷达图像序列中检索高分辨率风和波场的算法。风场检索算法由两部分组成。在第一部分中,从风条纹中提取风向,这些风条纹大致与平均地面风向一致。该方法基于从平均雷达反向散射图像中检索局部梯度,并假设表面风向垂直于局部梯度。在第二部分中,从雷达的平均横截面得出风速。因此,必须确定雷达后向散射对风矢量和成像几何形状的依赖性。通过使用神经网络(NN)开发了这种关系。为了验证该算法,将来自近3300个雷达图像序列的风向和速度与来自同一位置的风传感器的原位数据进行了比较。波浪检索算法基于一种方法,该方法首次无需事先对采集系统进行校准即可将海洋雷达图像序列反演为海面高程图时间序列,因此与外界无关传感器。通过比较得出的雷达衍生的重要波高与从三个共置的原位传感器获取的重要波高进行比较,可以验证检索到的海面高程图。结果表明,雷达-回有效波高的精度与原位传感器的精度一致。

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