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Assessment of Current and Future Climate Change Impact on Soil Loss Rate of Agewmariam Watershed, Northern Ethiopia

机译:评估当前和未来的气候变化对埃塞俄比亚北部黎穆里亚姆流域土壤流失率的影响

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Soil erosion is 1 of the most important environmental problems that pose serious challenges to food security and the future development prospects of Ethiopia. Climate change influences soil erosion and is critical for the planning and management of soil and water resources. This study aimed to assess the current and future climate change impact on soil loss rate for the near future (2011-2040), middle future (2041-2070), and far future (2071-2100) periods relative to the reference period (1989-2018) in the Agewmariam watershed, Northern Ethiopia. The 20 models of Coupled Model Intercomparison Project phase 5 global climate models (GCMs) under Representative Concentration Pathway (RCP) 4.5 (intermediate scenario) and 8.5 (high emissions scenario) scenarios were used for climate projection. The statistical bias correction method was used to downscale GCMs. Universal Soil Loss Equation integrated with geographic information system was used to estimate soil loss. The results showed that the current average annual soil loss rate and the annual total soil loss on the study area were found to be 25?t?ha~(?1)?year~(?1) and 51?403.13?tons, respectively. The soil loss has increased by 3.0%, 4.7%, and 5.2% under RCP 4.5 scenarios and 6.0%, 9.52%, and 14.32% under RCP 8.5 scenarios in the 2020s, 2050s, and 2080s, respectively, from the current soil loss rate. Thus, the soil loss rate is expected to increase on all future periods (the 2020s, 2050s, and 2080s) under both scenarios (RCP 4.5 and RCP 8.5) due to the higher erosive power of the future intense rainfall. Thus, climate change will exacerbate the existing soil erosion problem and would need for vigorous new conservation policies and investments to mitigate the negative impacts of climate change on soil loss.
机译:土壤侵蚀是最重要的环境问题,对粮食安全和埃塞俄比亚的未来发展前景构成了严峻挑战。气候变化影响土壤侵蚀,对土壤和水资源的规划和管理至关重要。本研究旨在评估当前和未来的气候变化对不久的未来土壤流失率(2011-2040),中间未来(2041-2070)和迄今为止(2071-2100)期间(1989年) -2018)在埃塞俄比亚北部的Agewmariam流域。在代表性浓度途径(RCP)4.5(中间场景)和8.5(高排放情景)方案下,20型耦合模型互相熟项项目阶段5全球气候模型(GCMS)用于气候投影。统计偏压校正方法用于低档GCM。与地理信息系统一体化的通用土壤损失方程用于估算土壤损失。结果表明,目前的年平均土壤损失率和研究区的年度整体土壤损失是25?T?HA〜(?1)?一年〜(?1)和51?403.13?吨。 RCP 4.5场景下,土壤损失增加了3.0%,4.7%和5.2%,在2020年代,2050年代和2080年代的RCP 8.5场景下,6.0%,9.52%和14.32%,从目前的土壤损失率下降。因此,由于未来的强烈降雨量越高,土壤损失率预计将在两种情况下(RCP 4.5和RCP 8.5)下的所有未来期间(2020年代,2050年代和2080年)增加。因此,气候变化将加剧现有的土壤侵蚀问题,并需要有蓬勃的新保护政策和投资,以减轻气候变化对土壤损失的负面影响。

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