摘要
咸海是亚洲仅次于里海的第二大内陆咸水湖,20世纪60年代以来湖泊面积急剧萎缩。基于1960-2018年咸海的面积数据、CRU气温和降水数据以及咸海流域灌溉面积、水库容量等资料,定量分析了1960年以来咸海湖泊面积的变化情况,并从气候变化与人类活动两方面探究了咸海面积变化的主要影响因素。结果表明:1960-2018年咸海的面积由6.85×104km2持续萎缩至(8.32±0.19)×103km2,共减少了(6.02±0.02)×104km2(约87.85%),其中1960-2009年面积萎缩了(5.94±0.02)×104km2(约86.77%),而在2009-2018年其面积萎缩速率明显放缓,减少了740.04km2(约8.17%)。统计结果显示,1960年以来强烈的人类活动(主要表现为灌溉用水和水库储水量的持续增加)是导致咸海面积急剧萎缩的主要因素,其对咸海面积变化的影响远大于气候变化。在中亚地区气候继续向暖湿变化的背景下,咸海流域应尽快调整以农业灌溉为主的用水结构,否则在上游冰川融水达到峰值后,咸海可能面临干涸的危险。
Utilizing datasets of the Aral Sea area,global CRU meteorological data and the irrigation area and reservoir capacity,we quantitatively assessed the long-term area variation of the Aral Sea during the period of1960-2018,and then investigated the dominant influence factors including climate change and human activities. It is revealed that area of the Aral Sea had shrunk dramatically from6.85×10~4 km^2 to(8.32±0.19)×10~3 km^2 with a shrinkage of(6.02±0.02)×10~4 km^2(about87.85%)from1960 to2018. The area of the Aral Sea had shrunk by(5.94±0.02)×10~4 km^2(about86.77%)during the period of1960-2009,while the shrinkage rate had slowed down obviously and the area had decreased by740.04 km^2(about8.17%)during the period of2009-2018. The results of this statistical analysis show that the enhanced human activities since1960,especially the increase of irrigation water consumption and reservoir capacity,is the dominant factor rendering the rapid shrinkage of the Aral Sea. Hence,water consumption,especially for irrigation should be adjusted to adapt ongoing warming in the Aral Sea basin as soon as possible.
作者
杨雪雯
王宁练
陈安安
张伟
YANG Xuewen;WANG Ninglian;CHEN An'an;ZHANG Wei(Shaanxi Key Laboratory of Earth Surface System and Environmental Carrying Capacity,Xi'an 710127,China;Institute of Earth Surface System and Hazards,College of Urban and Environmental Sciences,Northwesi University,xi’an 710127.China;CAS Center for Excellence in Tibetan Plateau Earth Sciences,Beijing 100101,China;State Key Laboratory of Cryospheric Science,Norhwest Institute of Eco-Environment and Resources,Chinese Academy of Sciences,Lanzhou 730000,China)
出处
《冰川冻土》
CSCD
北大核心
2020年第2期681-692,共12页
Journal of Glaciology and Geocryology
基金
中国科学院战略性先导科技专项(A类)(XDA20060201)
中国科学院“一带一路”科技合作专项(131C11KYSB20160061)
国家自然科学基金项目(41971083)
第二次青藏高原综合科学考察研究专项(2019QZKK020102)资助。
关键词
咸海
面积变化
气候变化
冰川变化
人类活动
Aral Sea
area variation
climate change
glacier change
human activity