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未来气候变化和人类活动下的黄河流域水资源短缺。

Water scarcity in the Yellow River Basin under future climate change and human activities.

机构信息

Key Laboratory of Regional Climate-Environment-Research for Temperate East Asia (RCE-TEA), Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100029, China; College of Earth and Planetary Sciences, University of Chinese Academy of Sciences, Beijing 100049, China.

Bӧckingstr. 55, Kӧln Mülheim 51063, Germany.

出版信息

Sci Total Environ. 2020 Dec 20;749:141446. doi: 10.1016/j.scitotenv.2020.141446. Epub 2020 Aug 3.

Abstract

Under global climate change and pressure from human activities, water scarcity is becoming a major concern in the quest for regional sustainable development in the Yellow River Basin (YRB). This study integrates scenarios of climate change and human activities under the Representative Concentration Pathway (RCP4.5 and RCP8.5) with a watershed-scale hydrological model, and uses the Water Use-to-Availability Ratio (WUAR) to study future water scarcity over six sub-catchments in the YRB. It further investigates the relationship between the future water scarcity and hydroclimatic and anthropogenic drivers. The results suggest that the average WUAR under both RCP4.5 and RCP8.5 will likely exceed the water scarcity threshold (WUAR >20%) and will reach up to 39.9 and 44.7%, respectively. The average WUAR for the upstream and downstream sub-catchments will likely range from 23.8 to 51.6% under RCP4.5 and from 25.5% to 73.8% under RCP8.5, indicating moderate to severe and moderate to extreme water scarcity, respectively. Future WUAR correlates negatively (r-value = -0.85) with the streamflow drought index (SDI) in the upstream sub-catchments, i.e., hydrological drought will likely intensify water scarcity. Conversely, WUAR and SDI would be positively correlated (r-value = +0.70) in the downstream sub-catchments, i.e., water scarcity will become severer despite decreasing severity of hydrological drought. Under climate change, water scarcity in these sub-catchments will exhibit high dependency (Kendall τ correlation coefficient = 0.84) on water-use patterns than on water availability. The regression analysis indicates that the WUAR will increase significantly (p < 0.05) with projected woodland, cropland, and buildup areas under RCP4.5. This relationship will become even more significant (p < 0.01) under RCP8.5. This study provides insights into the potential drivers of future water scarcity in the YRB, which is likely to confront water supply crises. The study should help policymaking towards attaining sustainable water management in the basin.

摘要

在全球气候变化和人类活动的压力下,水资源短缺正成为黄河流域(YRB)追求区域可持续发展的主要关注点。本研究整合了代表性浓度路径(RCP4.5 和 RCP8.5)下的气候变化和人类活动情景与流域尺度水文模型,并使用水利用-可得性比(WUAR)研究了 YRB 六个子流域未来的水资源短缺情况。进一步探讨了未来水资源短缺与水文气候和人为驱动因素之间的关系。结果表明,在 RCP4.5 和 RCP8.5 下,平均 WUAR 很可能超过水资源短缺阈值(WUAR>20%),分别达到 39.9%和 44.7%。在 RCP4.5 下,上游和下游子流域的平均 WUAR 可能在 23.8%至 51.6%之间,在 RCP8.5 下可能在 25.5%至 73.8%之间,分别表示中度至重度和中度至极度水资源短缺。未来 WUAR 与上游子流域的流域枯水指数(SDI)呈负相关(r 值=-0.85),即水文干旱可能加剧水资源短缺。相反,在下游子流域,WUAR 和 SDI 呈正相关(r 值=+0.70),即尽管水文干旱的严重程度下降,但水资源短缺将变得更加严重。在气候变化下,这些子流域的水资源短缺将表现出对用水模式的高度依赖(肯德尔 τ 相关系数=0.84),而不是对水资源可用性的依赖。回归分析表明,在 RCP4.5 下,WUAR 将随着林地、耕地和建设用地的预计增加而显著增加(p<0.05)。在 RCP8.5 下,这种关系将更加显著(p<0.01)。本研究提供了对黄河流域未来水资源短缺潜在驱动因素的深入了解,该流域可能面临供水危机。本研究应有助于为流域实现可持续水资源管理制定政策。

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