Flood risk assessment of Attabad lake: adopting a scenario-based approach for disaster preparedness

IF 2.8 4区 环境科学与生态学 Q3 ENVIRONMENTAL SCIENCES
Muhammad Qamar Javed Pirzada, Junaid Aziz Khan, Muhammad Fahim Khokhar
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引用次数: 0

Abstract

Attabad Lake is a debris-dammed lake formed due to a landslide disaster on 4th January 2010 in Gojal Valley. Multiple villages are located downstream of the lake along Hunza River. As this lake was formed by a massive landslide, there always remain questions about dam’s stability. The lake is in an active seismic zone which makes it prone to future earthquake and landslide disasters. Considering the sensitivity of region and ambiguities about dam’s structural integrity, this study adopts scenario-based approach for flood risk assessment and identification of potential inundation hotspots downstream. Seven hypothetical flow scenarios ranging from 5 to 50% flow were hydrologically modeled using HEC-RAS 6.5. Based on unsteady flow analysis, inundation boundary, depth, velocity, and product of depth and velocity were computed for all scenarios. The inundation boundary was highest (26.1 km2) in 50% flow scenario followed by 35% (19.6 km2), 25% (8.5 km2), 20% (5.1 km2), 15% (3.5 km2), 10% (3.1 km2), and 5% (2.5 km2). Threshold value of depth i.e., 0.35 m surpassed in all scenarios, whereas threshold velocity (1.5 m/s) was exceeded only in 50% flow scenario. In all flow scenarios, mean value of depth times velocity was higher than the threshold value of 0.52 m2/s. Based on analysis of flood critical parameters, flooding hotspots were mapped, and socio-economic impacts were evaluated. Using risk assessment maps, strategies for infrastructure development downstream, timely evacuation of villages in high-risk zones, and extensive disaster management plans can be prepared by administrative authorities to avoid casualties and economic loss.

Graphical Abstract

阿塔巴德湖洪水风险评估:采用基于场景的备灾方法
阿塔巴德湖是由于2010年1月4日在Gojal山谷发生的山体滑坡灾害而形成的一个堰塞湖。多个村庄位于罕萨河下游。由于这个湖是由一次大规模的滑坡形成的,所以人们对大坝的稳定性一直存在疑问。该湖处于地震活跃带,未来容易发生地震和滑坡灾害。考虑到区域的敏感性和大坝结构完整性的模糊性,本研究采用基于场景的方法进行洪水风险评估和下游潜在淹没热点的识别。使用HEC-RAS 6.5对流量为5%至50%的七个假设流量情景进行了水文建模。在非定常流分析的基础上,计算了各情景下的淹没边界、淹没深度、淹没速度以及淹没深度与淹没速度的乘积。50%流量情景下淹没边界最大(26.1 km2),依次为35% (19.6 km2)、25% (8.5 km2)、20% (5.1 km2)、15% (3.5 km2)、10% (3.1 km2)、5% (2.5 km2)。深度阈值(0.35 m)在所有场景中均被超过,而流速阈值(1.5 m/s)仅在50%流量场景中被超过。在所有流动场景中,深度乘以流速的平均值均高于0.52 m2/s的阈值。在分析洪水关键参数的基础上,绘制了洪水热点分布图,并对洪水的社会经济影响进行了评价。行政当局可以利用风险评估地图、下游基础设施发展战略、及时疏散高风险地区的村庄以及广泛的灾害管理计划,以避免人员伤亡和经济损失。图形抽象
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来源期刊
Environmental Earth Sciences
Environmental Earth Sciences 环境科学-地球科学综合
CiteScore
5.10
自引率
3.60%
发文量
494
审稿时长
8.3 months
期刊介绍: Environmental Earth Sciences is an international multidisciplinary journal concerned with all aspects of interaction between humans, natural resources, ecosystems, special climates or unique geographic zones, and the earth: Water and soil contamination caused by waste management and disposal practices Environmental problems associated with transportation by land, air, or water Geological processes that may impact biosystems or humans Man-made or naturally occurring geological or hydrological hazards Environmental problems associated with the recovery of materials from the earth Environmental problems caused by extraction of minerals, coal, and ores, as well as oil and gas, water and alternative energy sources Environmental impacts of exploration and recultivation – Environmental impacts of hazardous materials Management of environmental data and information in data banks and information systems Dissemination of knowledge on techniques, methods, approaches and experiences to improve and remediate the environment In pursuit of these topics, the geoscientific disciplines are invited to contribute their knowledge and experience. Major disciplines include: hydrogeology, hydrochemistry, geochemistry, geophysics, engineering geology, remediation science, natural resources management, environmental climatology and biota, environmental geography, soil science and geomicrobiology.
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