大型水库气候效应研究进展OACHSSCD
The climatic effects of large reservoirs:a review of research progress
水库在支撑经济社会发展的同时,也给周边地区的气候条件带来了影响,尤以大型水库的影响更为明显.然而当前关于大型水库气候效应的研究尚缺乏系统性梳理.将水库的气候效应分为局地尺度和区域尺度,进而分别论述两种尺度研究的发展历程、影响的程度和空间范围.选取已发表文献中覆盖不同气候区的45座大型水库,量化气候效应与水库规模(库容、水体面积、平均水深)和纬度的关系.研究结果:(1)蓄水后周边地区白天或夏季气温下降,夜晚或冬季气温上升,夏季降温幅度小于冬季升温幅度,对降水的影响在不同研究中结论差异较大,水电型水库建设提高流域尺度蒸发比.(2)在夏季和年尺度上,温带气候区水库以增温效应为主,但热带亚热带气候区主要为降温效应,干旱带气候区变化不明显,冬季各气候区均为增温效应;蓄水后,中低纬度非干旱气候地区水库年均降水量以减少为主,干旱气候区变化不大.(3)随着水库面积或库容的增加,库区大气冬季增温的幅度显著增大;水库面积或库容与夏季降水量的变化显著负相关,但影响程度不大.(4)水库对冬季气温的影响程度存在显著的纬度变化规律,中低纬度非干旱气候区水库的降水量变化与纬度负相关.未来应着力解决监测数据缺失条件下局地气候效应分析,厘清局地气候效应的驱动机制,准确归因水库周边的局地和区域气候变化.可为水资源合理利用与生态环境保护等相关研究与实践提供科学参考.
In the process of supporting global and regional economic and social development,reservoirs have simultaneously exerted considerable influences on the climatic conditions of surrounding areas,among which large reservoirs produced particularly notable effects.However,research on the climatic effects of large reservoirs at that time still lacked systematic synthesis.To address this gap,the climatic effects of reservoirs were first categorized into local and regional scales,based on spatial extent and mechanism differences,and then the research progress,magnitude of impact,and spatial extent for each scale were elaborated.A total of 45 large reservoirs across different climate zones,as reported in published literature,were selected to quantify the relationship between climatic effects and reservoir characteristics(storage capacity,water surface area,average depth)as well as latitude.The main findings were as follows:(1)After reservoir impoundment,surrounding areas experienced decreased temperatures during daytime or summer and increased temperatures during nighttime or winter,with the magnitude of summer cooling being smaller than that of winter warming.The impact on precipitation varied considerably across studies,while hydropower-oriented reservoir construction was found to increase the evaporation ratio at the watershed scale.(2)On summer and annual scales,reservoirs in temperate climate zones primarily exhibited warming effects,whereas those in tropical and subtropical zones mainly showed cooling effects;reservoirs in arid zones showed insignificant changes.In winter,all climate zones demonstrated warming effects.After impoundment,the mean annual precipitation at reservoirs in non-arid regions at low to mid latitudes tended to decrease,while changes in arid regions were minimal.(3)As reservoir surface area or storage capacity increased,the magnitude of winter warming over the reservoir area significantly increased;reservoir area or storage capacity was significantly negatively correlated with changes in summer precipitation,although the effect size was modest.(4)The extent of the reservoir's impact on winter temperatures exhibited a significant latitudinal pattern,and changes in precipitation at reservoirs in non-arid regions at low to mid latitudes were negatively correlated with latitude.Future efforts were suggested to focus on analyzing local climate effects under conditions of scarce monitoring data,clarifying the driving mechanisms of local climate effects,and accurately attributing local and regional climate changes around reservoirs by distinguishing reservoir-induced modifications from background climate variability.This study could provide a scientific reference for related research and practices in rational water resource utilization and ecological environmental protection,particularly under evolving climate change scenarios.
孙炼;陶正伟;蔡宴朋;李春晖
安徽师范大学地理与旅游学院,芜湖 241002安徽师范大学地理与旅游学院,芜湖 241002广东工业大学环境生态工程研究院,广州 510006北京师范大学环境学院,北京 100875
水库气候效应气象要素局地区域
reservoirclimatic effectmeteorological variablelocal changeregional change
《生态学报》 2026 (7)
3347-3360,14
国家自然科学基金项目(52309075,U2243236)安徽省自然科学基金项目(2308085QD116)国家重点研发计划课题(2016YFC0502209)
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