Geospatial analysis of shoreline change of ethekwini coastline from 1990 – 2023

IF 2.7 Q2 MULTIDISCIPLINARY SCIENCES
Zachariah H. Mshelia, Ekang C. Amatebelle, Johanes A. Belle
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引用次数: 0

Abstract

Coastal areas are dynamic environments impacted by both natural and anthropogenic processes. Hence, it is important to continually and accurately monitor these areas for change and develop coastal management strategies. The present study uses the Digital Shoreline Analysis System (DSAS) and satellite imagery to assess the changing dynamics of the Durban coastal stretch of the eThekwini Municipality from 1990 to 2023. Net Shoreline Movement (NSM), End Point Rate (EPR), and Linear Regression Rate (LRR) were calculated in DSAS to analyse the shoreline changes. The analysis revealed significant variations in erosion and accretion across the coastline. The average shoreline movement was 2.49 m in the north and -7.42 m in the south, indicating predominant erosion in the southern regions. Specifically, 53.85 % of transects in the north and 71.9 % in the south were negative distances, highlighting erosion areas. The EPR analysis indicated an average annual change rate of 0.09 m/year for the north and -0.22 m/year for the south, with erosion rates averaging -2.05 m/year in the north and -1.21 m/year in the south between 1990 and 2023. The LRR method corroborated these findings with annual changes of -0.01 and -0.37 m/year, respectively. High erosion rates were concentrated in areas such as Umhlanga Rocks and Beachwood, while engineered structures contributed to accretion in parts of Durban North. Conversely, the southern coastline, particularly around Amanzimtoti and Isipingo, experienced more erosion than accretion due to fewer protective structures. This study highlights the dynamic nature of shoreline changes along the Durban coast. Understanding these trends is essential for effective coastal planning and management and building resilience against the multiple hazards ravaging coastal communities.
1990 - 2023年德累尼尼省海岸线变化地理空间分析
沿海地区是受自然和人为过程影响的动态环境。因此,重要的是要持续和准确地监测这些地区的变化,并制定沿海管理战略。本研究使用数字海岸线分析系统(DSAS)和卫星图像来评估1990年至2023年德班德班市沿海地区的变化动态。利用DSAS计算净岸线移动(NSM)、终点率(EPR)和线性回归率(LRR)来分析岸线变化。分析揭示了海岸线上侵蚀和增生的显著变化。北岸岸线平均移动量为2.49 m,南岸岸线平均移动量为-7.42 m,以南岸侵蚀为主。其中,北侧53.85%的样带和南侧71.9%的样带为负距离,侵蚀区突出。EPR分析表明,1990 - 2023年间,北方的年平均变化速率为0.09 m/年,南方为-0.22 m/年,北方的年平均侵蚀速率为-2.05 m/年,南方的年平均侵蚀速率为-1.21 m/年。LRR方法的年变化分别为-0.01 m/年和-0.37 m/年,证实了这些发现。高侵蚀率集中在乌姆兰加岩石和比奇伍德等地区,而工程结构在德班北部的部分地区造成了增生。相反,南部海岸线,特别是在Amanzimtoti和Isipingo周围,由于较少的保护结构,经历了更多的侵蚀而不是增生。这项研究强调了德班沿海岸线变化的动态性质。了解这些趋势对于有效的沿海规划和管理以及建立抵御破坏沿海社区的多重灾害的能力至关重要。
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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来源期刊
Scientific African
Scientific African Multidisciplinary-Multidisciplinary
CiteScore
5.60
自引率
3.40%
发文量
332
审稿时长
10 weeks
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