气候变化对印度热带集水区土壤侵蚀率的影响

Anbazhagan M., Nanditha H. S., R. T. V.
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摘要

本研究使用经验性修订的通用土壤流失方程模型,结合 NEX 全球每日降尺度预测耦合模式相互比较项目第 6 阶段数据集所包含的全球气候模式(GCMs)中的气候变化情景,分析了印度一个热带集水区土壤侵蚀率的变化情况,以共享社会经济路径(SSP)126 和 SSP 585。初步选定了一组七个 GCM。根据其模拟当前情景降雨量的能力,采用 PROMETHEE-II 方法对全球气候模型进行排序,并采用表现最佳的前四个模型进行进一步分析。未来气候情景预测的土壤侵蚀率与当前情景进行了比较。预计在近期和本世纪中期,SSP 126 情景下的土壤侵蚀率将高于 SSP 585 情景下的土壤侵蚀率。预计到本世纪末,不同排放情景下的总体平均土壤侵蚀率将增加 15.41-25.94%,易受高和极高土壤侵蚀率影响的地区将增加到 40.3%。
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Effect of climate change on soil erosion rate in a tropical Indian catchment
This study analyzes the variations in soil erosion rate in a tropical catchment in India using the empirical revised universal soil loss equation model integrated with climate change scenarios from an ensemble of global climate models (GCMs) included in the NEX Global Daily Downscaled Projections Coupled Model Intercomparison Project Phase 6 dataset for shared socioeconomic pathways (SSP) 126 and SSP 585. A set of seven GCMs are initially selected. Based on their ability to simulate the rainfall for the current scenario, the PROMETHEE-II method is used to rank the GCMs and the top four best-performing models are used for further analysis. Soil erosion rates projected for the future climate scenarios are compared with the current scenario. In the near future and in the mid of the century, soil erosion rates under the SSP 126 scenario are projected to be higher than that under the SSP 585 scenario. The ensemble average soil erosion rate is projected to increase by 15.41–25.94% toward the end of the century for different emission scenarios, and the areas susceptible to high and very high soil erosion rates are projected to increase to 40.3%.
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