Impacts of Changes in Natural Factors and Human Activities on Surface Water Variations in the Aral Sea Basin

IF 2.9 3区 地球科学 Q1 Environmental Science
Xuewen Yang, Ninglian Wang, Yujie Zhang
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Abstract

Surface water in the Aral Sea Basin has undergone rapid changes since the 1960s, leading to severe environmental issues that have attracted global attention. This study quantified surface water variations in the Aral Sea Basin from 1986 to 2021 based on all available Landsat images integrated in the Google Earth Engine platform, and further analysed the impacts of changes in natural factors and human activities on surface water variations in the upstream, midstream, and downstream of the basin. The results indicate that the total surface water area in the basin decreased significantly from 56 058.79 km2 to 26 292.35 km2 during 1986–2021, showing a net loss of 29 766.44 km2 at a rate of 845.36 km2/a. The surface water area in the upstream and midstream exhibited modest increases at the rates of 69.92 km2/a and 39.80 km2/a respectively, while that in the downstream suffered a drastic reduction at a rate of 955.08 km2/a. The Aral Sea experienced the most drastic shrinkage in space, shrinking from 68 478 km2 in 1960 to 9397.31 km2 in 2021 at a decreasing rate of 999.17 km2/a, accompanied by water level and volume decline rates of 0.37 m/a and 17.18 km3/a, respectively. Natural factors, particularly glacier melting induced by climate warming, primarily drive surface water variations in the upstream mountains. In contrast, human activities, especially damming and irrigation, dominate surface water variations in the mid-downstream areas. Although the increased reservoir storage has slightly boosted surface water in the midstream, the strong diversion of runoff has caused severe surface water depletion in the downstream, constituting the predominant driver of surface water deficits across the entire basin.

Abstract Image

自然因子变化和人类活动对咸海盆地地表水变化的影响
自20世纪60年代以来,咸海盆地的地表水发生了迅速的变化,导致了严重的环境问题,引起了全球的关注。本研究基于谷歌Earth Engine平台整合的所有可用Landsat图像,量化了1986 - 2021年咸海盆地地表水变化,并进一步分析了自然因素和人类活动变化对盆地上、中、下游地表水变化的影响。结果表明:1986—2021年,流域总地表水面积从56 058.79 km2显著减少至26 292.35 km2,净损失29 766.44 km2,净损失速率为845.36 km2/a;上游和中游的地表水面积分别以69.92 km2/a和39.80 km2/a的速率略有增加,而下游的地表水面积则以955.08 km2/a的速率急剧减少。咸海的空间萎缩最为剧烈,从1960年的68478 km2缩小到2021年的9397.31 km2,减少速率为999.17 km2/a,水位和体积分别下降0.37 m/a和17.18 km3/a。自然因素,特别是气候变暖导致的冰川融化,主要驱动上游山区地表水的变化。相反,人类活动,特别是筑坝和灌溉,主导了中下游地区地表水的变化。虽然水库蓄水量的增加略微增加了中游的地表水,但径流的强烈转移导致下游地表水严重枯竭,是整个流域地表水短缺的主要驱动因素。
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来源期刊
Hydrological Processes
Hydrological Processes 环境科学-水资源
CiteScore
6.00
自引率
12.50%
发文量
313
审稿时长
2-4 weeks
期刊介绍: Hydrological Processes is an international journal that publishes original scientific papers advancing understanding of the mechanisms underlying the movement and storage of water in the environment, and the interaction of water with geological, biogeochemical, atmospheric and ecological systems. Not all papers related to water resources are appropriate for submission to this journal; rather we seek papers that clearly articulate the role(s) of hydrological processes.
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