中国莫道门河口水位和潮差分布的一般单位水文图理论

IF 5.9 1区 地球科学 Q1 ENGINEERING, CIVIL
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引用次数: 0

摘要

了解河口河潮动态的空间分布及其对人类密集干预的响应至关重要。然而,对水位和潮差空间分布特征的研究还不够充分,直接建立的经验公式不足。在本研究中,我们基于最近提出的一般单位水文图(GUH)理论,提出了一个通用的分析性水位和潮差分布模型,并将其应用于中国的莫道门河口。由于人类的大量干预,莫道门河口的河潮动力学演变被划分为三个不同的时期:前人类时期、过渡时期和后人类时期。结果表明,从人类活动之前到人类活动之后,SZ 站的水位上升,而其他站的水位下降,从而使最大水位梯度平均降低了约 9.08 × 10-6。河道沿岸的潮差普遍增大,最大潮差梯度的绝对值平均减小了约 54%。相应地,最大水位梯度和最小潮差梯度的位置一般分别向海移动了约 27.25 千米和 0.34 千米。此外,在人为干预后,河流-潮汐动态的空间分布更趋于线性。模型输出结果与莫道门河口沿岸六个测量站观测结果的对应关系令人满意(水位最大均方根误差值为 0.05 米,潮差最大均方根误差值为 0.03米),这表明新提出的GUH模型可以作为一种简单的工具来描述特定河道中水位和潮差的空间分布及其对人为改造的响应,这对于识别河潮动态的制度转变和全球其他人为改造程度较高的河口的可持续水资源管理也特别有用。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
A general unit hydrograph theory for water level and tidal range distributions in the Modaomen Estuary, China

Understanding the spatial distributions of river-tide dynamics in estuaries and their response to intensive human interventions is critical. However, the studies on the characteristics of the spatial distributions of water level and tidal range are insufficient, with inadequate direct established empirical formulas. In this study, we propose a general and analytical water level and tidal range distribution model based on the recently proposed General Unit Hydrograph (GUH) theory and apply it to the Modaomen Estuary in China. Due to the intensive human interventions, the evolution of river-tide dynamics in the Modaomen Estuary was divided into three distinct periods: Pre-human, Transitional and Post-human Periods. The results show that the water level increased at the SZ station, yet decreased at other stations, thereby reducing the maximum water level gradient by approximately 9.08 × 10−6 on average from the Pre-human to the Post-human Periods. The tidal range generally increased along the channel and the absolute value of the maximum tidal range gradient decreased by approximately 54 % on average. Correspondingly, the positions of both maximum water level gradient and minimum tidal range gradient generally move seaward by approximately 27.25 km and 0.34 km, respectively. Additionally, the spatial distributions of river-tide dynamics tended more linear after human interventions. The satisfactory correspondence of the model outputs with observations at the six gauging stations along the Modaomen Estuary (with maximum RMSE values being 0.05 m for the water level and 0.03 m for the tidal range, respectively) indicate that the newly proposed GUH model could serve as a simple tool to describe the spatial distributions of water level and tidal range in a specific channel together with their response to anthropogenic modifications, which is also particularly useful for the identification of regime shifts in river-tide dynamics and sustainable water resources management in other highly human-modified estuaries worldwide.

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来源期刊
Journal of Hydrology
Journal of Hydrology 地学-地球科学综合
CiteScore
11.00
自引率
12.50%
发文量
1309
审稿时长
7.5 months
期刊介绍: The Journal of Hydrology publishes original research papers and comprehensive reviews in all the subfields of the hydrological sciences including water based management and policy issues that impact on economics and society. These comprise, but are not limited to the physical, chemical, biogeochemical, stochastic and systems aspects of surface and groundwater hydrology, hydrometeorology and hydrogeology. Relevant topics incorporating the insights and methodologies of disciplines such as climatology, water resource systems, hydraulics, agrohydrology, geomorphology, soil science, instrumentation and remote sensing, civil and environmental engineering are included. Social science perspectives on hydrological problems such as resource and ecological economics, environmental sociology, psychology and behavioural science, management and policy analysis are also invited. Multi-and interdisciplinary analyses of hydrological problems are within scope. The science published in the Journal of Hydrology is relevant to catchment scales rather than exclusively to a local scale or site.
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