Mengistu Abiy Getachew, Woldesenbet Tekalegn Ayele, Dile Yihun Taddele, Bayabil Haimanote Kebede, Tefera Gebrekidan Worku
Ethiopian Institute of Water Resource, Addis Ababa University, Addis Ababa, Ethiopia.
Department of Natural Resource Management, Mizan-Tepi University, Mizan, Teferi, Ethiopia.
Heliyon. 2023 Feb 24;9(3):e13965. doi: 10.1016/j.heliyon.2023.e13965. eCollection 2023 Mar.
In terms of land use and climate, the world is changing at an unprecedented rate and these changes have a significant influence on our water resources. This study was conducted to examine the individual and combined potential impacts of land use and climate change on the water balance of the Baro basin in Ethiopia for the baseline period (1985-2002) and near-future period (2023-2040) using the Soil and Water Assessment Tool (SWAT). The plausible land use scenarios considering current (CUR), business as usual (BAU), and further expansion of altitudinal forest and watershed management practices (CON), as well as climate change scenarios from regional climate model outputs (RCMs) under two representative concentration pathways (RCP4.5 and RCP8.5) for the 2023-2040 time frame, were used as inputs to the models. The monthly calibrated and validated SWAT model produced an acceptable result, which was then used for water balance simulations. Findings show that forest decreased from 54.5% to 48.9% and 41.2% while agricultural land increased from 21.8% to 29.7% and 39.8% under the CUR and BAU land use change scenarios, respectively. The results from the ensemble mean showed an increase in maximum and minimum temperatures and a decrease in rainfall under the RCP4.5 and RCP8.5 climate change scenarios, which in turn resulted in an increase in evapotranspiration (ET) and a decrease in water availability. Climate change outweighed the impact of land-use change, thus indicating an increase in annual ET by up to 12% and a decrease of 42% in surface runoff (SURQ) under the RCP8.5 scenario. The BAU land use scenario projection triggers a respective increase of 18% in annual SURQ and reduction of ET by 2%. However, under the CON land use scenario, SURQ decreased by 24%. The study concluded that future land use and climate change will further challenge the basin's water supply capacity to meet the increased water demand. Understanding the changes in the basin's water balance is critical for mitigation and adaptation options. As a result, this study proposes restoration efforts and climate-resilient water management strategies that can increase the resilience of the river basin.
在土地利用和气候方面,世界正以前所未有的速度发生变化,这些变化对我们的水资源产生了重大影响。本研究旨在利用土壤和水资源评估工具(SWAT),考察埃塞俄比亚巴罗河流域在基准期(1985 - 2002年)和近期(2023 - 2040年)土地利用和气候变化对水平衡的单独及综合潜在影响。考虑当前(CUR)、照常营业(BAU)以及海拔森林和流域管理实践的进一步扩展(CON)等合理的土地利用情景,以及2023 - 2040年时间框架下两种代表性浓度路径(RCP4.5和RCP8.5)下区域气候模型输出(RCMs)的气候变化情景,被用作模型的输入。经过月度校准和验证的SWAT模型产生了可接受的结果,随后用于水平衡模拟。研究结果表明,在CUR和BAU土地利用变化情景下,森林面积分别从54.5%降至48.9%和41.2%,而农业用地面积分别从21.8%增至29.7%和39.8%。集合均值结果显示,在RCP4.5和RCP8.5气候变化情景下,最高和最低气温升高,降雨量减少,进而导致蒸散量(ET)增加,可用水量减少。气候变化对土地利用变化的影响更大,因此在RCP8.5情景下,年ET增加高达12%,地表径流(SURQ)减少42%。BAU土地利用情景预测导致年SURQ分别增加18%,ET减少2%。然而,在CON土地利用情景下,SURQ减少了24%。该研究得出结论,未来的土地利用和气候变化将进一步挑战流域满足增加的用水需求的供水能力。了解流域水平衡的变化对于缓解和适应措施至关重要。因此,本研究提出了恢复措施和气候适应型水资源管理策略,以提高流域的复原力。