人类活动及气候变化下伊犁河河流水温时空尺度特征及演变
作者:
作者单位:

(1.石河子大学水利建筑工程学院,新疆 石河子 832003;2.中国水利水电科学研究院水生态环境研究所,北京 100038 )

作者简介:

杜思哲(1998—),男,硕士研究生,主要从事水文水资源研究。E-mail:286404948@qq.com 通信作者:陈伏龙(1978—),男,教授,博士,主要从事水文水资源研究。E-mail:cfl103@shzu.edu.cn

基金项目:

国家自然科学基金项目(U2040211,U2340224);兵团科技创新人才计划项目(2023CB008-08);第三次新疆综合科学考察项目(2021xjkk0405)


Spatio-temporal scale characteristics and evolution of water temperature of Ili River under human activities and climate change//
Author:
Affiliation:

(1.College of Water Conservancy & Architectural Engineering, Shihezi University, Shihezi 832003, China;2.Department of Water Ecology and Environment, China Institute of Water Resources and Hydropower Research, Beijing 100038, China)

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    摘要:

    为了梳理内陆干旱区河流热动力特征及驱动因子,在对伊犁河水温系统调查的基础上,构建了基于HEC-RAS的河流水动力-水温数值模型,采用遥感气象时空数据分析了伊犁河出山口水库下游210km河道水温变化规律,量化并探讨了水资源开发利用以及未来气候变化对河流水温的影响。结果表明:构建的HEC-RAS模型能够识别水资源开发利用及气候变化的影响; 4月大型水库下泄的低温水受限于较小的水气温差、下游河流沿程复温缓慢、分层取水等措施效果有限;取用水等行为导致的河流流量变化改变了河流的热容量,水温变化规律呈现差异,4月河流流量减少时水温升幅不显著,但流量增加使水温降低明显,最大降幅达-0.60℃,而7月流量减少时水温升幅变化明显,最大升幅为0.65℃,水量增加时水温变化不大;在未来低、中、高碳排放情景不同的气候模式下,2020—2080年长时间尺度上伊犁河水温均呈上升态势,水温升幅与波动范围均低于气温,2号断面10a温升平均速率分别为0.09、0.21、0.56℃;预测到2080年,河流水量减小导致水温上升,4月和7月的影响占比分别为6%和21%。

    Abstract:

    In order to sort out the thermal dynamic characteristics and driving factors of rivers in the inland arid region, based on the systematic investigation of the water temperature of Yili River, a numerical model of river hydrodynamic-water temperature based on HEC-RAS was constructed. Remote sensing meteorological spatio-temporal data was used to analyze the variation law of the water temperature of the 210 km section downstream of the reservoir at the outlet of the Yili River. The impacts of the development and utilization of water resources and future climate change on the water temperature of the river were quantified and discussed.The results show that the constructed HEC-RAS model can identify the impacts of the development and utilization of water resources and climate change. In April, the low-temperature water discharged from large reservoirs is limited by the small temperature difference between water and air, and the downstream river warms up slowly along the way, and measures such as stratified water intake have limited effects. The changes in river flow caused by water intake and other behaviors have changed the heat capacity of the river, resulting in differences in the variation law of water temperature. When the river flow decreases in April, the rise in water temperature is not significant, but when the flow increases, the water temperature decreases significantly, with a maximum decrease of -0.60℃. When the flow decreases in July, the rise in water temperature changes significantly, with a maximum increase of 0.65℃, and when the water volume increases, the water temperature changes little.Under different climate models of low, medium and high carbon emission scenarios in the future, the water temperature of the Yili River will show an upward trend on the long time scale from 2020 to 2080. The increase range and fluctuation range of the water temperature are both lower than the air temperature. The average 10-year temperature increase rate at section 2 is 0.09,0.21, and 0.56℃ respectively. It is predicted that by 2080, the increase in water temperature caused by the decrease of river water volume will account for 6% and 21% in April and July, respectively. Keywords: river thermal dynamics; human activities; reanalysis data; climate change; long-term scale; HEC-RAS model; Ili River 〖FL

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引用本文

杜思哲,杜彦良,陈伏龙,等.人类活动及气候变化下伊犁河河流水温时空尺度特征及演变[J].水资源保护,2025,41(2):216-225, 232.(DU Sizhe, DU Yanliang, CHEN Fulong, et al. Spatio-temporal scale characteristics and evolution of water temperature of Ili River under human activities and climate change//[J]. Water Resources Protection,2025,41(2):216-225, 232.(in Chinese))

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  • 收稿日期:2024-06-12
  • 在线发布日期: 2025-04-14