Analysing the changes in the bathymetry of Saldanha Bay between the years 1977 and 2021

IF 0.3 Q4 REMOTE SENSING
L. Du Toit, Ivan Henrico, J. Bezuidenhout, B. Mtshawu
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引用次数: 0

Abstract

The construction of the Saldanha Port has been the reason for the major changes in the bathymetry and sediment dynamics observed in Saldanha Bay in the last decades. In this paper, newly acquired soundings from the National Hydrographer were used to analyse the changes between 1977 and 2021 - over a 44-year period - in the bathymetry of Saldanha Bay. The Ordinary Kriging (OK) interpolation method, available through the Geostatistical Wizard in ArcGIS Pro, was used for creating surface models to conduct comparisons with the bathymetry of Saldanha Bay. The results indicate a general increase in depth since 1977 of between 0.395 and 3.203 m, and an average increase in depth within the Big Bay of 1.799 m. Between 1977 and 2021, a total volume loss of 49 364 560.0 m3 in sediment was calculated - an indication of how the sedimentation process in Saldanha Bay has changed subsequent to the construction of the harbour.
分析1977年至2021年间萨尔达尼亚湾水深的变化
萨尔达那港的建设是过去几十年中在萨尔达那湾观测到的水深和沉积物动力学发生重大变化的原因。在本文中,国家水文局新获得的测深数据被用于分析1977年至2021年期间(44年期间)萨尔丹哈湾测深的变化。ArcGIS Pro中的Geostatistical Wizard提供了普通克里格(OK)插值方法,该方法用于创建表面模型,以与Saldanha湾的测深进行比较。结果表明,自1977年以来,深度普遍增加了0.395至3.203米,大湾内的平均深度增加了1.799米。1977年至2021年间,计算出沉积物的总体积损失为49 364 560.0立方米,这表明萨尔达尼亚湾的沉积过程在港口建设后发生了怎样的变化。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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