首页|期刊导航|华南理工大学学报(自然科学版)|隐潭溪流域山洪预警模型构建与应急避险分析

隐潭溪流域山洪预警模型构建与应急避险分析OA

Construction of a Flash Flood Early Warning Model and Emergency Evacuation Analysis for Yintanxi Watershed

中文摘要英文摘要

全球气候变化引发极端暴雨频发加之山区河道水流运动的复杂性,使得山洪预警始终是一个科学难题.目前常用于洪水预测的各类水文、水动力模型虽各有侧重,但均难以指导地形数据要求较高的小尺度山洪预警.该研究以隐潭溪为例,基于高精度地形数据构建了水文水动力耦合模型,以提高山洪预警与风险评估能力,制定隐潭溪山洪预警指标体系并探究山洪危险区、避险路径及安置点分布.结果表明:新安江模型模拟2015-2021年的4次台风洪水事件中,径流深和洪峰流量相对误差均低于20%,确定系数超过0.70,适用性较高,且在场次洪水模拟中效果亦优;通过HEC-RAS模型开展20210721场次洪水一维与二维非恒定流耦合模拟,依托网格单元划分,探明洪水主要淹没河道低地与泛洪区;采用水位(流量)反推法构建隐潭溪山洪预警指标体系,发现临界雨量指标随预警时段延长而增加,但随前期土壤湿润度增大而减小;河道由内向外山洪风险递减,且由于各村地形、水文条件等不同,使得面临洪水时的山洪危险区、避险路径及安置点存在区域性差异.针对小流域山洪预警技术短板,该研究从模型耦合、动态预警、防灾闭环3个维度优化技术方法,构建了南方山丘区小流域山洪全流程技术体系,可为同类流域防灾减灾提供技术支撑.

The frequent occurrence of extreme rainstorms triggered by global climate change,combined with the complex flow dynamics of mountainous river channels,makes flash flood early warning a persistent scientific challenge.Although various hydrological and hydrodynamic models widely adopted for flood forecasting each have their own strengths,they are generally difficult to apply to small-scale flash flood early warning,which demands high-resolution topographic datasets.Taking the Yintanxi Watershed as a case study,this research constructs a coupled hydrological-hydrodynamic model based on high-precision topographic datasets to improve flash flood early warning and risk assessment capabilities,establishes a flash flood early warning indicator system for the Yintanxi Watershed,and investigates the distribution of flash flood hazard zones,evacuation routes,and shelter locations.The results show that,in the simulation of four typhoon flood events from 2015 to 2021 using the Xin'anjiang model,the relative errors of runoff depth and peak discharge are all below 20%,with determination coefficients exceeding 0.70,indicating high applicability,and the model also performs well in individual flood event simulations.Using the HEC-RAS Model,this study carries out coupled one-dimensional and two-dimensional unsteady flow simulations for the 20210721 flood event.Based on grid cell division,the primary inundated areas are identified as low-lying river channels and floodplains.A flash flood early warning indicator system for the Yintanxi Watershed is constructed using the water level(discharge)back-calculation method.It is found that the critical rainfall threshold rises with extended warning periods but decreases with the increase of antecedent soil moisture content.The flash flood risk gradually decreases from the river channel outward to the surrounding areas.Due to variations in terrain,hydrological conditions,and other factors among different villages,there are regional differences in flood hazard zones,evacuation routes,and shelter locations.To tackle the technical bottlenecks restricting flash flood early warning in small watersheds,this study optimizes the technical approach from three dimensions including model coupling,dynamic early warning and closed-loop disaster prevention,and establishes a full-process technical system for flash flood management in small watersheds in southern hilly regions.This can provide technical support for disaster prevention and mitigation in similar watersheds.

王高振;王兆礼;王文辉;田露;喻凤娇;王京晶;吴旭树

华南理工大学 土木与交通学院,广东 广州 510640华南理工大学 土木与交通学院,广东 广州 510640河海大学 水利水电学院,江苏 南京 210098华南理工大学 土木与交通学院,广东 广州 510640华南理工大学 土木与交通学院,广东 广州 510640华南理工大学 土木与交通学院,广东 广州 510640华南理工大学 土木与交通学院,广东 广州 510640

建筑与水利

新安江模型HEC-RAS模型山洪预警风险评估

Xin'anjiang modelHEC-RAS modelflash flood early warningrisk assessment

《华南理工大学学报(自然科学版)》 2026 (9)

43-56,14

国家自然科学基金面上项目(52479015,52379010)国家自然科学基金重点项目(52539005) Supported by the General Program of the National Natural Science Foundation of China(52479015,52379010)and the Key Program of the National Natural Science Foundation of China(52539005)

10.12141/j.issn.1000-565X.260054

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