Impacts of arti fi cial dams on terrestrial water storage changes and the Earth's elastic load response during 1950- 2016: A case study of medium and large reservoirs in Chinese mainland

被引:5
作者
Wang, Linsong [1 ,2 ]
Zhu, Mingtao [1 ]
Zhong, Yulong [3 ]
Sun, Jianwei [1 ]
Peng, Zhenran [1 ]
机构
[1] China Univ Geosci, Sch Geophys & Geomatics, Hubei Subsurface Multiscale Image Key Lab, Wuhan 430074, Peoples R China
[2] China Univ Geosci, Gorges Res Ctr Geohazard 3, Minist Educ, Wuhan 430074, Peoples R China
[3] China Univ Geosci, Sch Geog & Informat Engn, Wuhan 430078, Peoples R China
基金
中国国家自然科学基金;
关键词
Man-made dams; Terrestrial water storage; Elastic load response; Sea level changes; Chinese mainland; GRACE DATA; DATA ASSIMILATION; MODELS; DISPLACEMENTS; DEFORMATION; VARIABILITY; GROUNDWATER; LANDSLIDE; GRAVITY; LEVEL;
D O I
10.1016/j.geog.2023.07.009
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
The construction of dams for intercepting and storing water has altered surface water distributions, landsea water exchanges, and the load response of the solid Earth. The lack of accurate estimation of reservoir properties through the land surface and hydrological models can lead to water storage simulation and extraction errors. This impact is particularly evident in many artificial reservoirs in China. The study aims to comprehensively assess the spatiotemporal distribution and trends of water storage in medium and large reservoirs (MLRs) in Chinese mainland during 1950-2016, and to investigate the gravity, displacement, and strain effects induced by the reservoir mass concentration using the load elasticity theory. In addition, the impoundment contributions of MLRs to the relative sea level changes were assessed using a sea-level equation. The results show impoundment increases in the MLRs during 1950-2016, particularly in the Yangtze River (Changjiang) and southern basins, causing significant elastic load effects in the surrounding areas of the reservoirs and increasing the relative sea level in China's offshore. However, long-term groundwater estimation trends are overestimated and underestimated in the Yangtze River and southwestern basins, respectively, due to the neglect of the MLRs impacts or the uncertainty of the hydrological model's output (e.g., soil moisture, etc.). The construction of MLRs may reduce the water mass input from land to the ocean, thus slowing global sea level rise. The results of the impact of human activities on the regional water cycle provide important references and data support for improving the integration of hydrological models, evaluating Earth's viscoelastic responses under longterm reservoir storage, enhancing in-situ and satellite geodetic measurements, and identifying the main factors driving sea level changes. (c) 2023 Editorial office of Geodesy and Geodynamics. Publishing services by Elsevier B.V. on behalf of KeAi Communications Co. Ltd. This is an open access article under the CC BY-NC-ND license (http:// creativecommons.org/licenses/by-nc-nd/4.0/).
引用
收藏
页码:252 / 263
页数:12
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