利用归一化后向散射数据通过最佳估计掠射角进行海底表征

T. Hou, L. Huff
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引用次数: 2

摘要

如今的多波束回声测深仪(MBES)提供详细的水深信息,允许对同时收集的声学后向散射图像进行局部坡度校正,从而提高海底表征的可能性。尽管有这些数据,但在后向散射处理方案中通常不应用局部斜率校正。我们描述了一种在确定海底波束入射角时考虑船舶偏航、俯仰角和横摇角,并在一定半径内使用所有可用的最近邻探测的方法来补偿局部斜率的后向散射的方法。然后通过对周围表面的加权最小二乘拟合计算每个梁位置的三维局部曲率的法线。该方法可以利用同一测量线或多测量线(如果存在重叠线)的共配深度和反向散射强度的所有可用几何信息。通过计算实际掠射角,估计发射和接收波束方向图,对测量数据进行处理和分析,为复杂地形起伏地区海底属性信息的提取提供依据。作为本研究的一个例子,利用Simrad EM1000声纳系统在新泽西边缘外大陆架中部收集的多波束数据生成的后向散射图像,通过真实掠角进行归一化。归一化后,独立测量的粒度与后向散射之间的相关性优于非归一化后向散射数据。利用墨西哥湾多波束测量的后向散射与掠角曲线,对后向散射模型参数进行了优化,以期通过其空间变化特征来表征海底。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Seabed characterization using normalized backscatter data by best estimated grazing angles
Today's multibeam echo-sounders (MBES) provide detailed bathymetric information that allows local slope corrections to be made to the concurrently collected acoustic backscatter imagery, thus improving the seabed characterization possibilities. Despite the availability of these data, local-slope corrections are not typically applied in the backscatter-processing scheme. We describe an approach that compensates backscatter for local slope by taking into account the vessel yaw, pitch and roll angles when determining the beam incident angle at the sea floor, and using all the available closest neighbor soundings within a certain radius. The normal of the 3D local curvature at each beam location is then calculated by a weighted least squares fit to the surrounding surface. The proposed method can use all the available geometric information from the co-registered depths and backscatter strengths either from a single survey line, or multiple survey lines, if overlapping lines exist. With the actual grazing angles computed, the transmitting and receiving beam patterns can be estimated to process and analyze the survey data for the extraction of seafloor property information in regions of complex topographic relief. As an example of this research, a backscatter image created from the multibeam data collected using a Simrad EM1000 sonar system on the mid-outer continental shelf off the New Jersey Margin, was normalized by the true grazing angles. When normalized, a better correlation between the independently measured grain size and backscatter was found, than with non-normalized backscatter data. With backscatter vs. grazing angle curve from a Gulf of Mexico multibeam survey, backscatter model parameter optimization was pursued in order to characterize the seabed by their spatial variations.
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