Providing solutions for data scarcity in urban flood modeling through sensitivity analysis and DEM modifications

Lea Dasallas, Hyunuk An, Seungsoo Lee
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Abstract

Developing countries face significant challenges in accessing sufficient and reliable hydro-meteorological data, hindering the implementation of effective disaster management strategies. This research proposes solutions for these limitations on performing flood simulations through parameter sensitivity analysis and digital elevation model (DEM) modifications. The methodology provides alternatives to account for insufficient data for rainfall, roughness coefficient, infiltration in simulating large-scale rainfall-runoff, and high-resolution DEMs incorporating road and building networks for urban flood modeling. By applying the method to an extreme flood event in the Marikina Basin, Philippines, a combination of ground-based and remotely retrieved rainfall data, roughness (n = 0.3861–0.5005), and infiltration parameters (Δθ = 0.326–0.505 and ψ = 0.4547–1.565) set at the maximum range were found to replicate the increase in the upstream water level. Simulations were able to accurately capture the flood propagation along the natural and artificial barriers in the urban area compared to untreated digital terrain and surface model (DTM and DSM) data, with root-mean-square error range improvements from 0–7.13 (DTM) and 0.29–4.20 (DSM) to 0–0.63 (modified DEM). The proposed methodology significantly improved the accuracy of the simulations, which is crucial for proposing adequate flood action plans, despite the lack of high-resolution data available for under-developed nations.
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通过敏感性分析和 DEM 修改为城市洪水模型中的数据稀缺问题提供解决方案
发展中国家在获取充足可靠的水文气象数据方面面临巨大挑战,阻碍了有效灾害管理战略的实施。本研究通过参数敏感性分析和数字高程模型(DEM)修改,提出了洪水模拟限制的解决方案。在模拟大尺度降雨-径流时,该方法提供了考虑降雨量、粗糙度系数、渗透等数据不足的替代方案,并提供了用于城市洪水模型的包含道路和建筑网络的高分辨率 DEM。通过将该方法应用于菲律宾马里基纳盆地的一次特大洪水事件,发现将地面和遥感雨量数据、粗糙度(n = 0.3861-0.5005)和渗透参数(Δθ = 0.326-0.505 和 ψ = 0.4547-1.565)设置在最大范围内的组合能够复制上游水位的上升。与未经处理的数字地形模型和地表模型(DTM 和 DSM)数据相比,模拟能够准确捕捉到洪水沿城市地区天然和人工屏障的传播,均方根误差范围从 0-7.13(DTM)和 0.29-4.20(DSM)提高到 0-0.63(修改后的 DEM)。尽管欠发达国家缺乏高分辨率数据,但所提出的方法大大提高了模拟的准确性,这对于提出适当的洪水行动计划至关重要。
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