Watershed hydrological responses to land use land cover changes at Bilata watershed, Rift Valley Basin, southern Ethiopia

M. Beza, Eden Tatek, Mandefro Chala, Alene Moshe
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Abstract

Most anthropogenic activities have a profound effect on land cover that affects the water cycle and, ultimately, the availability of water in the watershed. The idea of this study was to evaluate the hydrological response to land use and land cover change in the Bilata watershed. To achieve this objective, supervised land use land cover classification was applied for the years 2000, 2010, and 2020 using ERDAS IMAGINE 2015. The watershed underwent significant land use and land cover changes from 2000 to 2020. There was an abrupt expansion of agricultural land and a reduction of forest. The SWAT model was applied to evaluate the impact of land use and land cover change on hydrological processes. The calibration and validation of the SWAT model showed that the model has performed well in simulating the hydrology of the watershed with a coefficient of determination, Nash–Sutcliffe efficiency, and per cent of bias greater than 0.6 for both calibration and validation. Due to intensive agricultural expansion and settlement, the surface runoff increased from 172 to 259.5 and 265.0 mm in 2000, 2010, and 2020, respectively. The average streamflow increased from 132 to 134 and 150 m3/s between 2000, 2010, and 2020.
埃塞俄比亚南部裂谷盆地 Bilata 流域对土地利用和土地覆被变化的流域水文响应
大多数人为活动都会对土地覆盖产生深远影响,从而影响水循环,并最终影响流域的水供应。本研究的目的是评估 Bilata 流域的水文对土地利用和土地覆被变化的响应。为实现这一目标,使用 ERDAS IMAGINE 2015 对 2000 年、2010 年和 2020 年的土地利用和土地覆被进行了监督分类。从 2000 年到 2020 年,该流域的土地利用和土地覆被发生了显著变化。农田面积骤然扩大,森林面积骤然减少。SWAT 模型用于评估土地利用和土地覆被变化对水文过程的影响。SWAT 模型的校准和验证结果表明,该模型在模拟流域水文方面表现良好,校准和验证的决定系数、纳什-苏克里夫效率和偏差百分比均大于 0.6。由于密集的农业扩张和定居,2000 年、2010 年和 2020 年的地表径流量分别从 172 毫米增加到 259.5 毫米和 265.0 毫米。2000 年、2010 年和 2020 年的平均溪流流量分别从 132 m3/s 增加到 134 m3/s 和 150 m3/s。
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