Impact of land use/land cover change on surface water hydrology in Akaki river catchment, Awash basin, Ethiopia

被引:0
|
作者
Yohannes, Hamere [1 ]
Argaw, Mekuria [2 ]
Seifu, Weldemariam [3 ]
机构
[1] Addis Ababa Univ, Addis Ababa Inst Technol, Sch Civil & Environm Engn, Addis Ababa, Ethiopia
[2] Addis Ababa Univ, Coll Nat & Computat Sci, Ctr Environm Sci, Addis Ababa, Ethiopia
[3] Salale Univ, Coll Agr & Nat Resource Sci, Dept Hort, Fiche, Ethiopia
关键词
Akaki catchment; LULC change scenario; Sediment export; Soil loss; Surface water hydrology; Water yield; BLUE NILE BASIN; SOIL-EROSION; VARIABILITY; STREAMFLOW; RESOURCES; CLIMATE; BALANCE; RUNOFF;
D O I
10.1016/j.pce.2024.103690
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
Watershed reactions to environmental changes is critical for water resource use and management planning. The change in land use/land cover (LUCC) alters surface water hydrology and water balance, subsequently it affects the availability of water resources. This study examined Akaki River catchment surface hydrological responses to future land use scenarios. The future LULC simulated using Cellular Automata-Markov Chain (CA-Markov) model in IDRISI software for 2031, 2041, and 2051 under Business as Usual (BAU) and Forest Patch Protection (FPP) scenarios. Water yield (WY), sediment export (SE), and soil loss (SL) were simulated using the Integrated Valuation of Ecosystem Services and Tradeoffs (InVEST) model. The findings indicate that under BAU, forest and settlement areas increased 42.64% and 31.47%, whereas water body, grass land, and agriculture dropped 31.99%, 25.72%, and 10.4%, respectively, from 2021 to 2051. The FPP scenario shows a 66.42% increase in forest coverage and a 31.97% decrease in cultivated land between 2021 and 2051. Overall settlement expansion will expand by 31.44%, while water body and grassland will decline by 11.12% and 24.9%. As a result of LULC changes in BAU scenario, the proportions of WY (4.36%), SE (26%), and SL (22.45%) increased. The hydrological components exhibited more gradual variations of 0.55%, 18.8%, and 14.24% for the WY, SE, and SL, respectively, under the FPP scenario. Therefore, the alteration has resulted in a concerning state within the area, necessitating the implementation of comprehensive management techniques to restore the hydrology of the catchment.
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页数:16
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