三峡水库调蓄与流域来水对2020年以来鄱阳湖极端洪枯水情的影响
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1.南京信息工程大学地理科学学院;2.中国科学院南京地理与湖泊研究所,湖泊与流域水安全全国重点实验室;3.中国科学院大学南京学院;4.江西鄱阳湖国家级自然保护区管理局;5.江西省水文监测中心

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基金项目:

国家自然科学基金项目(面上项目,重点项目,重大项目)


Impacts of Three Gorges Reservoir Regulation and Basin Inflow on Extreme Flood-Drought Events in Lake Poyang since 2020
Author:
Affiliation:

1.Key Laboratory of Lake and Watershed Science for Water Security, Nanjing Institute of Geography and Limnology;2.Jiangxi Poyang Lake National Nature Reserve Authority;3.Jiangxi Hydrological Monitoring Center;4.School of Geographical Sciences, Nanjing University of Information Science and Technology

Fund Project:

The National Natural Science Foundation of China (General Program, Key Program, Major Research Plan)

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    摘要:

    受长江来水与流域五河等多因素的共同作用,近年来鄱阳湖极端洪枯事件频发,2020–2024年间出现涝旱急转现象,水文情势不确定性增加。本研究综合运用LSTM神经网络与MIKE21水动力模型构建基于实测边界条件、无三峡水库调蓄及常年平均流域来水三种情景,对比分析了三峡水库调蓄与流域来水对2020年以来鄱阳湖发生的极端洪枯事件的影响。结果显示:(1)三峡水库调蓄一定程度上减少了鄱阳湖洪水发生的风险;流域来水减少导致鄱阳湖低水位更低;二者共同作用导致鄱阳湖秋旱加剧。(2)三峡水库调蓄是鄱阳湖丰水期水位的主控因素,导致极端洪水下降0.09 ~ 0.38 m(占双因素综合影响的58% ~ 81%),而流域来水是枯水期水位降低的主因(降幅0.13 ~ 1.12 m,贡献率达35% ~ 100%)(3)极端洪水情势下,三峡水库调蓄的影响范围波及到整个湖区,水位下降区间最大达到1.32 ~ 1.38 m,水位降幅自北向南减弱;极端枯水情势下,流域来水主要影响主河道和南部抚河入湖区域,导致水位下降0 ~ 3.96 m,水域面积减少516.03 km2。研究成果可为精准识别鄱阳湖极端水文事件的主导因子、优化水位调控策略及提升区域水文风险管理能力提供科学依据。

    Abstract:

    Under the combined influence of multiple factors such as inflow from the Yangtze River and the Five Rivers Basin, extreme flood-drought events in Poyang Lake have occurred frequently in recent years, with rapid shifts between floods and droughts observed from 2020 to 2024, leading to increased uncertainty in hydrological regimes. This study integrated LSTM neural networks and the MIKE21 hydrodynamic model to construct three scenarios: measured boundary conditions, scenarios excluding Three Gorges Reservoir (TGR) regulation, and scenarios with average annual basin inflow. A scenario comparison method was systematically applied to analyze the impacts of TGR regulation and basin inflow on extreme flood-drought events in Poyang Lake since 2020. Key findings include: (1) TGR regulation positively mitigated flood peaks, reducing the maximum water level drop at Xingzi Station during extreme floods by 1.35 m. Conversely, basin inflow negatively affected low-water stability, exacerbating the maximum water level drop at Xingzi Station during extreme droughts by 3.26 m. (2) Under combined effects, TGR regulation dominated extreme flood water level variations (reduction of 0.09–0.38 m, contributing 58%–81%), while basin inflow was the primary driver of droughts, significantly lowering dry-season water levels (reduction of 0.13–1.12 m, contributing 35%–100%). (3) During extreme floods, TGR regulation impacted the entire lake area, reducing water levels by up to 1.32–1.38 m with diminishing effects from north to south. During extreme droughts, basin inflow predominantly affected the main channel and southern Fuhe River inflow zone, lowering water levels by 0–3.96 m and reducing water surface area by 516.03 km2. This research provides scientific support for water resource management, extreme disaster early warning, and ecological protection in the middle and lower Yangtze River basin.

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  • 收稿日期:2025-03-25
  • 最后修改日期:2025-06-17
  • 录用日期:2025-06-18
  • 在线发布日期: 2025-09-16
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