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Bathymetry Determination via X-Band Radar Data: A New Strategy and Numerical Results

机译:X波段雷达数据进行测深的确定:一种新的策略和数值结果

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摘要

This work deals with the question of sea state monitoring using marine X-band radar images and focuses its attention on the problem of sea depth estimation. We present and discuss a technique to estimate bathymetry by exploiting the dispersion relation for surface gravity waves. This estimation technique is based on the correlation between the measured and the theoretical sea wave spectra and a simple analysis of the approach is performed through test cases with synthetic data. More in detail, the reliability of the estimate technique is verified through simulated data sets that are concerned with different values of bathymetry and surface currents for two types of sea spectrum: JONSWAP and Pierson-Moskowitz. The results show how the estimated bathymetry is fairly accurate for low depth values, while the estimate is less accurate as the bathymetry increases, due to a less significant role of the bathymetry on the sea surface waves as the water depth increases.
机译:这项工作涉及使用海洋X波段雷达图像进行海况监测的问题,并将其注意力集中在海深估计问题上。我们提出并讨论了一种通过利用表面重力波的色散关系来估算测深的技术。这种估计技术基于测得的海浪频谱与理论海浪频谱之间的相关性,并且通过使用综合数据的测试案例对方法进行了简单分析。更详细地,估计技术的可靠性通过模拟数据集验证,该数据集涉及两种类型的海图:JONSWAP和Pierson-Moskowitz的测深和地表水流的不同值。结果表明,对于低深度值,估计的测深法如何相当准确,而随着测深法的增加,估计值的准确性就会降低,这是因为随着水深的增加,测深法在海面波浪中的作用不那么重要。

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