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Flash flood susceptibility modeling using geo-morphometric and hydrological approaches in Panjkora Basin, Eastern Hindu Kush, Pakistan

机译:巴基斯坦东兴都库什省Panjkora盆地采用地貌和水文方法进行山洪敏感性分析

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This main objective of this study is flash flood susceptibility modeling using geo-morphometric and hydrological approaches in Panjkora Basin, Eastern Hindu Kush, Pakistan. In the study region, flash flood is one of the horrific and recurrent hydro-meteorological disasters causing damages to human life, their properties, and infrastructure. Watershed modeling approach is implemented to delineate Panjkora Basin, its sub-basins, and extract drainage network by utilizing Advance Space borne Thermal Emission and Reflection Radiometer Global Digital Elevation Model as an input data in geographic information system environment. A total of 30 sub-basins were delineated using threshold of 25km(2). The geo-morphometric parameters of each sub-basin were computed by applying Hortonian, Schumm, and Strahler Geo-morphological laws. The value of each parameter was normalized and aggregated into geo-morphometric ranking number depicting the degree of flash flood susceptibility. Surface run-off depth of each sub-basin is estimated by applying Natural Resource Conservation Service Curve Number hydrological model. Both models outputs were integrated by implementing weighted overlay analysis technique and susceptibility map is obtained. The resultant map was analyzed and zonated into very high, high, moderate, low, and very low flash flood susceptibility zones. These zones were spread over an area of 1441km(2) (27%), 1950km(2) (36.5%), 1252km(2) (23.4%), 604km(2) (11.3%), and 98km(2) (1.8%), respectively. Spatially, the very high susceptible zone is located in the upstream areas, characterized by snow covered peaks, steep gradient (30 degrees), and high drainage density (1.7km/km(2)), and geologically dominated by igneous and metamorphic lithological units. Analysis indicated that flash flood susceptibility is directly increases with increasing surface run-off and geo-morphometric ranking number. A new model is developed to geo-visualize the spatial pattern of flash flood susceptibility. Accuracy of the model is assessed using global positioning system-based primary data regarding past-flood damages and flood marks. The study results can facilitate Disaster Management Authorities and flood dealing line agencies to initiate location-specific flood-risk reduction strategies in highly susceptible areas of Panjkora Basin. Similarly, this methodological approach can be adapted for any highland river system.
机译:这项研究的主要目的是在巴基斯坦东兴都库什邦的Panjkora盆地利用地貌和水文方法对山洪敏感性进行建模。在研究区域,山洪暴发是造成人类生命,财产和基础设施受损的可怕且反复发生的水文气象灾害之一。通过利用先进的星载热发射和反射辐射计全球数字高程模型作为地理信息系统环境中的输入数据,实现了分水岭建模方法来划定Panjkora盆地及其子盆地并提取排水网络。使用25 km(2)的阈值划定了总共30个子流域。通过应用Hortonian,Schumm和Strahler地貌法则来计算每个子流域的地貌参数。将每个参数的值归一化并汇总到描述山洪敏感性的程度的地貌等级排名中。通过应用自然资源保护服务曲线编号水文模型估算每个子流域的地表径流深度。通过实施加权叠加分析技术对两个模型的输出进行整合,并获得磁化率图。分析所得的图并将其划分为非常高,很高,中等,低和非常低的山洪敏感性区域。这些区域分布在1441km(2)(27%),1950km(2)(36.5%),1252km(2)(23.4%),604km(2)(11.3%)和98km(2)的区域( 1.8%)。在空间上,非常高的敏感区位于上游地区,其特征是积雪覆盖的山峰,陡峭的坡度(> 30度)和高的排水密度(> 1.7km / km(2)),并且在地质上以火成岩和变质岩为主岩性单位。分析表明,山洪敏感性随地表径流和地貌等级数的增加而直接增加。开发了一种新模型来对山洪暴发敏感性的空间格局进行地理可视化。该模型的准确性是使用基于全球定位系统的主要数据来评估的,该数据涉及过去的洪水破坏和洪水标记。该研究结果可以帮助灾难管理部门和洪水处理线机构在Panjkora盆地高度敏感的地区启动针对特定地点的减少洪水风险的策略。同样,这种方法学方法可以适用于任何高原河流系统。

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