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A new mapping method of underwater bottom topography in the shallow sea by using SAR images

机译:使用SAR图像一种新的浅水水下底部地形的新映射方法

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Synthetic aperture radar (SAR) is an active instrument which is used to create images of an object. Underwater bottom topography can be retrieved indirectly by measuring variations of the sea surface roughness in the SAR images, although the microwaves cannot penetrate into the water. In this paper, we present a new simple method for bathymetric mapping in the shallow sea. Based on the radiometric correction, sea surface roughness is derived using SAR images. These results are then used for water depth inversions based on the Alpers-Hennings (AH) model, supported by a few true depth data points (sounding data or chart data). This method is used to bathymetric mapping of two areas in the Subei shoal. The study results of the two cases show that the trend of the inversion and true depths match well. The retrieval accuracy depends on the true depth data points. In a case, the true depth data is the sounding data, the relative errors between the inversion and true depths is less than 20%. In the other case, the true depth data is the chart data. And the result is worse, because the measure time of the chart is 1979, and the time of SAR images are 2000s. The bottom topography was changed. The proposed method has two advantages in that it does not require environmental parameters and it is relatively simple to operate.
机译:合成孔径雷达(SAR)是用于创建物体图像的有源仪器。可以通过测量SAR图像中的海面粗糙度的变化来间接检索水下底部地形,尽管微波不能渗透到水中。在本文中,我们在浅海中提出了一种新的简单方法。基于辐射尺寸,使用SAR图像导出海面粗糙度。然后,这些结果基于Alpers-Hennings(AH)模型用于水深反转,由一些真实深度数据点(探测数据或图表数据)支持。该方法用于潜水浅中的两个区域的划分。这两种情况的研究结果表明,反转和真实深度的趋势匹配良好。检索准确性取决于真实的深度数据点。在一个情况下,真正的深度数据是探测数据,反转和真实深度之间的相对误差小于20%。在另一个情况下,真正的深度数据是图表数据。结果更糟糕,因为图表的测量时间是1979年,并且SAR图像的时间为2000s。底部地形改变了。所提出的方法具有两个优点,因为它不需要环境参数,并且操作相对简单。

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