Understanding Complex Processes of Flood Inundation in a Regulated Coastal Lowland River: A Modelling Framework Integrating Hydrological, Hydraulic, Tidal and Geomorphic Data

IF 2.9 3区 地球科学 Q1 Environmental Science
Zafar Beg, Kumar Gaurav, Gaurav Kailash Sonkar, Vikrant Jain
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引用次数: 0

Abstract

Inundation dynamics in lowland rivers are an outcome of a complex interaction between hydrologic and geomorphic factors. The co-occurrence of river flow and tidal surge in coastal regions further complicates these interactions. The extent to which these factors mediate inundation mechanisms in regulated lowland river reaches remains challenging and has been poorly understood. This study presents a novel framework that examines the combined effect of flood drivers (riverine and high tide) and geomorphic factors in determining the inundation mechanism along the Lower Tapi Basin (LTB) in western India through an integration of hydrological, tidal, hydrodynamic, and geomorphic datasets. Using variable infiltration capacity (VIC) and Hydrologic Engineering Center River Analysis System (2D HEC-RAS) with geomorphic characteristics of river channels, we explore how spatial inundation dynamics vary across different valley settings under different flood return periods. Our integrated modelling framework accurately simulates daily streamflow and flood inundation. Incorporation of multidisciplinary data through the integrated modelling framework has advanced our understanding of flood inundation dynamics in lowland rivers. We have further shown that the model uncertainty can be reduced by incorporating field data, bathymetric measurements and rule curve of reservoir operation in the model domain. Although this modelling framework has been developed on a specific lowland reaches of the Tapi River, it can be further extended to any lowland rivers in similar settings. Such multidisciplinary models will help to analyse river response to future projected climate and sea level change.

理解受调控的沿海低地河流洪水淹没的复杂过程:一个整合水文、水力、潮汐和地貌数据的建模框架
低地河流的淹没动态是水文和地貌因素复杂相互作用的结果。在沿海地区,河流流量和潮涌的共同出现使这些相互作用进一步复杂化。这些因素在多大程度上介导了受管制的低地河流流域的淹没机制仍然具有挑战性,而且人们对其了解甚少。本研究提出了一个新的框架,通过整合水文、潮汐、水动力和地貌数据集,研究了洪水驱动因素(河流和涨潮)和地貌因素在决定印度西部下塔皮盆地(LTB)淹没机制中的综合影响。利用变入渗能力(VIC)和水文工程中心河流分析系统(2D HEC-RAS)结合河道地貌特征,探讨不同流域背景下不同汛期的空间淹没动态变化。我们的综合建模框架精确地模拟了每日的河流流量和洪水泛滥。通过综合建模框架整合多学科数据,提高了我们对低地河流洪水淹没动力学的理解。进一步证明,在模型域内结合现场资料、水深测量资料和油藏运行规律曲线,可以降低模型的不确定性。虽然这个模型框架是在塔皮河的特定低地河段上开发的,但它可以进一步扩展到类似环境下的任何低地河流。这种多学科模型将有助于分析河流对未来预测的气候和海平面变化的反应。
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来源期刊
Hydrological Processes
Hydrological Processes 环境科学-水资源
CiteScore
6.00
自引率
12.50%
发文量
313
审稿时长
2-4 weeks
期刊介绍: Hydrological Processes is an international journal that publishes original scientific papers advancing understanding of the mechanisms underlying the movement and storage of water in the environment, and the interaction of water with geological, biogeochemical, atmospheric and ecological systems. Not all papers related to water resources are appropriate for submission to this journal; rather we seek papers that clearly articulate the role(s) of hydrological processes.
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