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Hydrographic data modeling methods for determining precise seafloor topography

机译:确定精确海底地形的水文数据建模方法

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Acoustic and light detection and ranging are the recent methods used in hydrographical surveying. Depth values depending on X and Y horizontal coordinates are measured in both methods. While processing the hydrographical data, all data with different density are interpolated and modeled for determining the seafloor model using different interpolation techniques. In this study, effects of different surface modeling methods are investigated. Data obtained from single-beam echo sounder (SBES) are modeled using inverse distance, kriging, local polynomial, minimum curvature, moving average, nearest-neighbor, and Delaunay interpolation methods. Interpolation results are compared with the multibeam echo sounder data which were collected on the same area for determining the accuracy of modeling methods. Depending on the maximum total vertical uncertainty values in hydrographic survey standards, the best results were determined by using the kriging method. The Delaunay, minimum curvature, and inverse distance methods can be used for modeling the SBES data in shallow waters.
机译:声光检测和测距是水文测量中使用的最新方法。在两种方法中都测量取决于X和Y水平坐标的深度值。在处理水文数据时,将对所有具有不同密度的数据进行插值和建模,以使用不同的插值技术确定海底模型。在这项研究中,研究了不同表面建模方法的效果。使用反距离,克里金法,局部多项式,最小曲率,移动平均,最近邻和Delaunay插值方法对从单束回声测深仪(SBES)获得的数据进行建模。将插值结果与在同一区域收集的多波束回声测深仪数据进行比较,以确定建模方法的准确性。根据水文测量标准中最大的总垂直不确定性值,使用克里金法确定最佳结果。 Delaunay,最小曲率和反距离方法可用于对浅水区的SBES数据进行建模。

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