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水力发电学报 ›› 2023, Vol. 42 ›› Issue (8): 42-50.doi: 10.11660/slfdxb.20230805

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东洞庭湖水位模拟及水情变化归因

  

  • 出版日期:2023-08-25 发布日期:2023-08-25

Simulations of water levels in East Dongting Lake and attribution analysis of its hydrological regime changes

  • Online:2023-08-25 Published:2023-08-25

摘要: 东洞庭湖水文情势近年来发生了较大变化,需要评估不同驱动因子对水文情势变化的贡献量。构建长短时记忆神经网络模型模拟东洞庭湖水位变化过程,采用水文改变指标分析东洞庭湖水文情势,并设置情境进行分析,评估长江干流流量变化、四水入湖流量变化和地形条件变化对东洞庭湖水文情势变化的贡献量。结果表明:长江干流流量变化是东洞庭湖丰水期水位下降和枯水脉冲平均历时减少的主要驱动因子。四水入湖流量变化是东洞庭湖水位逆转次数增加的主导因素。地形条件变化显著拉低了东洞庭湖枯水期水位,对东洞庭湖水位主要表现为拉低作用。研究成果可为东洞庭湖水资源管理与利用提供科学依据,为其他河流、湖泊等水系的水情变化归因研究提供参考。

关键词: 东洞庭湖, 水文情势变化, 驱动因子, 贡献量, 长短时记忆神经网络

Abstract: The hydrological regime in East Dongting Lake has changed greatly in recent years; it needs an evaluation on the contributions of different driving factors to the regime change. This study constructs a long short-term memory neural network model to simulate the lake’s water level variations, and uses the indicators of hydrological alteration (IHA) to evaluate the existing hydrological regime. Four scenarios are examined for the major contributing factors: changes in the flow in the Yangtze mainstream and the lake’s four tributaries, and changes in its topographic conditions. The results show that the Yangtze flow changes are the main factor driving the drop in flood season water levels in the lake and the shortened average duration of its low water level pulses. The tributary flow changes are the main factor driving the increase in the number of the lake’s water level reversals. The topographic changes have significantly lowered its water level, and this effect is significant in the dry season. The results help manage the lake’s water resources and evaluate hydrologic regime change factors for other river systems.

Key words: East Dongting Lake, hydrologic regime changes, driving factor, contribution, long short-term memory neural network

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