在沙特阿拉伯 NEOM 采用模糊分析层次过程-地理信息系统方法绘制洪水易发区地图

Barra Faisal Bokhari, Bassam Tawabini, H. Baalousha
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摘要

作为 "2030 愿景 "的一部分,沙特阿拉伯王国正在经历大规模的快速城市化。这包括沙特阿拉伯红海沿岸的开发项目。沿海地区,尤其是沙特西部地区的沿海地区,很容易遭受洪水等自然灾害。NEOM 是沙特阿拉伯西北部正在开发的一座未来城市,由于其地理位置和拟议中的城市化计划,该城市具有潜在的洪水灾害。本研究旨在通过将模糊分析层次过程 (FAHP) 与地理信息系统 (GIS) 结合使用,加强 NEOM 的洪水灾害评估。考虑到与数据可用性和参数选择共识相关的传统局限性,本研究精心选择了排水密度、海拔、坡度、降雨量、土地利用/土地覆被 (LULC)、土壤类型、归一化差异植被指数 (NDVI) 和地形湿润指数 (TWI) 等参数。30 米 DEM 用于得出排水密度、坡度和 TWI,而 LULC 数据则有助于评估土地覆被的变化。降雨数据与土壤类型信息相结合,以评估它们对洪水易感性的影响。采用 NDVI 分析植被覆盖。利用 ArcGIS Pro 的加权叠加模型,将各项标准结合起来,生成最终的洪水易感性地图。研究成果体现在洪水易发性地图上,该地图将地区划分为七个不同的易发性等级,从 "极低 "到 "极高 "不等。通过汇总表中的定量细分,可以深入了解洪水风险的比例分布。结果表明,东北部大部分地区属于不同程度的中度易受洪水影响范围,极端易受洪水影响的地区相对有限,相当于 "低至中度 "易受洪水影响的地区为 4322.8 平方公里,"中度 "易受洪水影响的地区为 5109.69 平方公里,"中度至高度 "易受洪水影响的地区为 4081.39 平方公里。本研究绘制的洪水易发区地图可帮助我们了解洪水缓解措施的最佳潜在区域(即建立雨水收集点的最佳位置)。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
A fuzzy analytical hierarchy process -GIS approach to flood susceptibility mapping in NEOM, Saudi Arabia
The Kingdom of Saudi Arabia is undergoing massive and rapid urbanization as part of Vision 2030. This includes development projects along Saudi Arabia’s coastline across the Red Sea. Coastal areas, especially the ones along Saudi’s western regions are susceptible to natural disasters such as flooding. NEOM, a futuristic city currently being developed in the northwest of Saudi Arabia, exemplifies a potential flooding hazard due to its geographic location and proposed urbanization plans. This research aims to enhance flood hazard assessment in NEOM by applying the Fuzzy Analytical Hierarchy Process (FAHP) in combination with Geographic Information System (GIS). Acknowledging traditional limitations related to data availability and parameter selection consensus, the study carefully selects parameters such as drainage density, elevation, slope, rainfall, land use/land cover (LULC), soil type, normalized difference vegetation index (NDVI), and topographic wetness index (TWI). The 30 m DEM was used to derive Drainage Density, Slope, and TWI while LULC data helped assess land cover changes. Rainfall data and soil type information are integrated to evaluate their impact on flood susceptibility. NDVI is employed to analyze vegetation cover. Utilizing ArcGIS Pro’s weighted overlay model, the criteria were combined to generate the final flood susceptibility map. The research outcomes manifest in a flood susceptibility map categorizing areas into seven distinct susceptibility classes, ranging from ‘very low’ to ‘very high.’ A quantitative breakdown in a summary table provides insights into the proportional distribution of flood risk. Results indicate a significant portion of NEOM falls within varying degrees of moderate susceptibility range with relatively limited distribution of flood susceptibility on the extremes, equating to areas with ‘low to moderate’ susceptibility is 4,322.8 km2, areas with ‘moderate’ susceptibility is 5,109.69 km2, areas with ‘moderate to high’ is 4,081.39 km2. The flood susceptibility map developed in this study can shed insights on potential optimum areas for flood mitigation measures (i.e., optimum locations for establishing stormwater collection points).
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