Spatiotemporal Change Assessment of Lake Beseka, Ethiopia Using Time Series Landsat Images

Tewabe Melkamu, M. Bagyaraj, Melkamu Adimaw
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Abstract

Changes in lake surface area and fluctuations in water levels are common especially in the Ethiopian Rift Valley region. The aim of this study was to present the spatiotemporal changes of lake Beseka from 1985 to 2020 using multi-temporal Landsat images. Four spectral water indices, namely Normalized Differential Water Index (NDWI), Modified Normalized Difference Water Index (MNDWI) and Automated Water Extraction Index (AWEI) were used for the extraction of the lake water. The results of the study show that lake Beseka has tended to expand significantly and strongly over the past 35 years. During 1985, the lake surface area was around 30.9km2 and within the next 35 years, the lake surface area increased by 18.18 km2and in 2020, its surface area is about 49.1 km2. lake Beseka shows 0.2412km2 area change from 2015 to 2020. This indicates lake Beseka has a decreasing trend of expansion compared to its history. However, the topography of Lake Beseka is lower in elevation a small water level rise in the lake can cover a large area and lead to significant impacts on the surrounding environment. Therefore, the monitoring of lake surface changes by multi-temporal satellite images is very necessary and of decisive importance.
基于时间序列Landsat图像的埃塞俄比亚贝塞卡湖时空变化评价
湖泊表面积的变化和水位的波动是常见的,特别是在埃塞俄比亚裂谷地区。利用多时相Landsat影像,研究了1985 - 2020年塞贝卡湖的时空变化特征。采用归一化差分水指数(NDWI)、修正归一化差分水指数(MNDWI)和自动水提取指数(AWEI) 4种光谱水指数进行湖泊水提取。研究结果表明,在过去的35年中,贝塞卡湖有明显而强烈的扩张趋势。1985年湖泊面积约为30.9km2, 35年间湖泊面积增加18.18 km2,到2020年湖泊面积约为49.1 km2。2015 - 2020年塞贝卡湖面积变化0.2412km2。这表明贝塞卡湖的扩张与历史相比有减小的趋势。但由于贝塞卡湖地势高程较低,湖面小的水位上升就会覆盖较大的区域,对周边环境造成较大的影响。因此,利用多时相卫星影像监测湖面变化是十分必要的,具有决定性的意义。
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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