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The role of lateral pipe flow in hillslope runoff response: an intercomparison of non-linear hillslope response

机译:横向管道流量在坡面径流响应中的作用:非线性坡面响应的比较

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The importance of lateral pipe flow on runoff generation in wet steep hillslopes has been described in many case studies from around the world. However, most hillslope studies are done in isolation and usually focus on the idiosyncrasies of individual hillslope characteristics and pipe flow response at a single site. Consequently, the first order controls on pipe flow responses remain poorly understood. We present a new intercomparison of pipe flow response to storm rainfall at four well instrumented sites: Panola (Georgia, USA), Toinotani (Kyoto, Japan), Jozankei (Hokkaido, Japan) and Hakyuchi (Tokyo, Japan). Our objective was to minimize the complexities of lateral pipe flow on hillslopes by looking for commonality across different hillslope types. Despite the large differences between the study sites in topography, climate, soil type and soil matrix hydraulic conductivity, we found several common pipe flow responses to storm rainfall: (1) the relationship between total rainfall amount and total pipe flow volume was highly non-linear at each site, (2) initiation of measurable pipe flow was threshold-dependent, controlled by the total rainfall amount and the pre-storm wetness, (3) once significant pipe flow response occurred, the maximum pipe flow rate was sensitive to the measured rainfall intensity, and (4) the ratio of total pipe flow to total hillslope discharge for each site was constant, regardless of total rainfall amount once the precipitation threshold for significant pipe flow response was reached. We used these results to develop a decision tree to determine the general conditions necessary for significant pipe flow to occur. The controls derived from our comparisons agree largely with the controls reported by the previous individual hillslope pipe flow studies in the literature. The commonality of response between our four very different forested hillslope settings indicates that site intercomparison may be effective for extracting common first order controls on complex hillslope processes. We argue that a decision tree may be a useful organizational framework to summarize and organize comparative analyses and may provide a structure for defining the hierarchy of process controls necessary for model development. (c) 2005 Elsevier B.V. All rights reserved.
机译:在世界各地的许多案例研究中都已经描述了侧向管道流动对湿润陡峭山坡径流产生的重要性。但是,大多数坡度研究都是孤立进行的,通常集中在单个坡度特征和单个位置的管道流动响应的特质上。因此,对管道流动响应的一阶控制仍然知之甚少。我们提出了一种新的比较方法,用于比较四个设备良好的站点对降雨对管道流量的响应:Panola(美国乔治亚州),Toinotani(日本京都),Jozankei(日本北海道)和Hakyuchi(日本东京)。我们的目标是通过寻找不同类型的山坡之间的共性来最大程度地减少山坡上侧向管道流动的复杂性。尽管研究地点在地形,气候,土壤类型和土壤基质水力传导率方面存在很大差异,但我们发现了几种常见的降雨对雨水流量的响应:(1)总降雨量和总流量之间的关系高度不(2)可测量的管道流量的开始是阈值相关的,受总降雨量和暴雨前的湿度控制。(3)一旦发生显着的管道流量响应,最大管道流量就对最大流量敏感。 (4)每个地点的总管道流量与总山坡流量之比是恒定的,而与总降雨量无关,一旦达到显着管道流量响应的降水阈值。我们使用这些结果来制定决策树,以确定发生大量管道流动所需的一般条件。从我们的比较中得出的控制与文献中先前的单个坡道管流研究报告的控制基本吻合。我们在四个截然不同的森林山坡设置之间的响应共性表明,现场比较可以有效地提取复杂山坡过程中的常见一阶控制。我们认为,决策树可能是总结和组织比较分析的有用组织框架,并且可能为定义模型开发所需的过程控制层次结构提供结构。 (c)2005 Elsevier B.V.保留所有权利。

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