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Recognition of debris flow, debris flood and flood hazard through watershed morphometrics

机译:通过分水岭形态计量学识别泥石流,泥石流和洪水灾害

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摘要

Debris flows, debris floods and floods in mountainous areas are responsible for loss of life and damage to infrastructure, making it important to recognize these hazards in the early stage of planning land developments. Detailed terrain information is seldom available and basic watershed morphometrics must be used for hazard identification. An existing model uses watershed area and relief (the Melton ratio) to differentiate watersheds prone to flooding from those subject to debris flows and debris floods. However, the hazards related to debris flows and debris floods are not the same, requiring further differentiation. Here, we demonstrate that a model using watershed length combined with the Melton ratio can be used to differentiate debris-flow and debris-flood prone watersheds. This model was tested on 65 alluvial and colluvial fans in west central British Columbia, Canada, that were examined in the field. The model correctly identified 92% of the debris-flow, 83% of the debris-flood, and 88% of the flood watersheds. With adaptation for different regional conditions, the use of basic watershed morphometrics could assist land managers, scientists, and engineers with the identification of hydrogeomorphic hazards on fans elsewhere. © Springer-Verlag 2004.
机译:泥石流,泥石流和山区洪水是造成生命损失和基础设施损坏的原因,因此在规划土地开发的早期阶段认识到这些危害非常重要。很少有详细的地形信息,必须使用基本的分水岭形态计量学来进行危害识别。现有模型使用分水岭面积和浮雕(梅尔顿比)将易于洪水的分水岭与易发生泥石流和泥石流的水域区分开。但是,与泥石流和泥石流有关的危害并不相同,需要进一步区分。在这里,我们证明了使用分水岭长度与梅尔顿比率相结合的模型可用于区分泥石流和泥石流易发性分水岭。该模型在加拿大不列颠哥伦比亚省中西部的65个冲积扇和冲积扇上进行了测试,并在现场进行了检验。该模型正确地识别了92%的泥石流,83%的泥石流和88%的洪水流域。通过适应不同的区域条件,使用基本的分水岭形态计量学可以帮助土地管理人员,科学家和工程师识别其他地方的风机的水文地质灾害。 ©Springer-Verlag 2004。

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