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Dynamic puddle delineation and modeling of puddle-to-puddle filling-spilling-merging-splitting overland flow processes

机译:水坑间水流-灌水-合并-分流陆上水流过程的动态水坑定界和建模

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摘要

Surface microtopography affects overland flow, infiltration, soil erosion, pollutant transport, and other fundamental hydrologic and environmental processes across scales. Under the influence of surface depressions, overland flow essentially features a series of progressive puddle-to-puddle (P2P) filling, spilling, merging, and splitting processes. The objectives of this study are to characterize puddles and their hierarchical relationships and model the microtopography-controlled P2P processes. We proposed a new modeling framework for simulating the P2P overland flow dynamics through cell-to-cell (C2C) and P2P routing for a set of puddle-based units (PBUs) in a well-delineated, cascaded P2P drainage system. Testing of the P2P model demonstrated its potential to improve overland flow modeling and hydrologic connectivity analysis by explicitly incorporating the hydrologic roles of depressions and quantifying the real microtopography-controlled P2P dynamics.
机译:表面微观形貌影响跨尺度的陆上径流,渗透,土壤侵蚀,污染物运输以及其他基本的水文和环境过程。在地表凹陷的影响下,陆上水流本质上具有一系列渐进式的水到水(P2P)填充,溢出,合并和分裂过程。这项研究的目的是表征水坑及其分层关系,并对微地形控制的P2P过程进行建模。我们提出了一个新的建模框架,用于在精心描绘的级联P2P排水系统中,通过一组基于水坑的单元(PBU),通过单元间(C2C)和P2P路由来模拟P2P陆上水流动力学。对P2P模型的测试表明,通过明确纳入凹陷的水文作用并量化实际的微观地形控制的P2P动力学,可以改善陆上水流模型和水文连通性分析。

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  • 来源
    《Water resources research》 |2013年第6期|3825-3829|共5页
  • 作者单位

    Department of Civil Engineering, North Dakota State University, Dept 2470, PO Box 6050, Fargo, ND 58108,USA;

    Department of Civil Engineering, North Dakota State University,Fargo, North Dakota, USA;

    Department of Civil Engineering, North Dakota State University,Fargo, North Dakota, USA;

    Department of Civil Engineering, North Dakota State University,Fargo, North Dakota, USA;

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