Hydrology and Water Resources College, Hohai University, Nanjing, 210098, P.R. China.
Jackson School of Geosciences, University of Texas at Austin, Austin, 78712, USA.
Sci Rep. 2017 Aug 15;7(1):8254. doi: 10.1038/s41598-017-09215-z.
Understanding contributions of climate change and human activities to changes in streamflow is important for sustainable management of water resources in an arid area. This study presents quantitative analysis of climatic and anthropogenic factors to streamflow alteration in the Tarim River Basin (TRB) using the double mass curve method (DMC) and the Budyko methods. The time series (19602015) are divided into three periods: the prior impacted period (19601972) and the two post impacted periods, 19731986 and 19872015 with trend analysis. Our results suggest that human activities played a dominant role in deduction in the streamflow in TRB with contribution of 144.6% to 120.68% during the post impacted period I and 228.68% to 140.38% during the post impacted period II. Climatic variables accounted for 20.68%~44.6% of the decrease during the post impacted period I and 40.38% ~128.68% during the post impacted period II. Sensitivity analysis indicates that the streamflow alteration was most sensitive to changes in landscape parameters. The aridity index and all the elasticities showed an obvious increasing trend from the upstream to the downstream in the TRB. Our study suggests that it is important to take effective measures for sustainable development of eco-hydrological and socio-economic systems in the TRB.
了解气候变化和人类活动对干旱地区水资源可持续管理的影响,需要对径流量变化进行定量分析。本研究采用双质量曲线法(DMC)和 Budyko 方法,对塔里木河流域(TRB)气候和人为因素对径流量变化的影响进行了定量分析。该时间序列(19602015 年)分为三个时期:前期影响期(19601972 年)和两个后期影响期,19731986 年和 19872015 年,并进行了趋势分析。结果表明,人类活动在 TRB 径流量减少中起主导作用,在后期影响期 I 中,贡献率为 144.6%120.68%,在后期影响期 II 中,贡献率为 228.68%140.38%。气候变量在后期影响期 I 中占径流量减少的 20.68%44.6%,在后期影响期 II 中占 40.38%128.68%。敏感性分析表明,流域景观参数变化对径流量变化最敏感。塔里木河流域的干旱指数和所有弹性系数均表现出从上游到下游明显增加的趋势。本研究表明,在塔里木河流域,采取有效措施促进生态水文和社会经济系统的可持续发展至关重要。