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基于WebGIS的流域级洪水管理系统集成与应用 总被引：1，自引：0，他引：1
流域级洪水管理系统指为流域机构服务的洪水管理系统,是基于计算机网络、地理信息系统、数据库技术,专业分析模型,采用人机交互方式,按照统一标准与规范建立的流域洪水管理平台。为洪水预报、预警、预案编制、应急调度、风险评价、洪水整治、决策会商提供先进技术手段。本文首先讨论了流域洪水管理系统的结构设计与数据库,然后,以松花江流域洪水管理系统为例,对系统功能与分析模型进行了讨论。功能模块包括基础信息管理、洪水监视预警、洪水预报调度、二维洪水仿真、灾情评估、防汛管理等功能模块;分析模型方面,建立了水文-水力学耦合模型、全流域洪水预报模型与洪水调度模型。该模型由基于MIKE NAM的全流域降雨径流模型与基于MIKE11 HD的嫩江、二松、松干河道一维水动力模型组成。此外,在哈尔滨等4个重点城市与两个蓄滞洪区构建了MIKE21的二维洪水模拟模型,在城市、蓄滞洪区与防洪重点保护区,建立了灾情影响分析模型等。最后,利用WebGIS技术对这些功能模块进行了集成,建立了功能齐全的松花江流域洪水管理系统。作为国内第一个流域级洪水管理系统,松花江流域洪水管理系统的设计与建设,对流域级洪水管理系统的研究进行了有益的探索。 相似文献
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洪水研究包括径流与淹没两种模式。为了探究流域降雨产汇流与淹没情况、提高洪水预报精度,本研究在传统流域水文模型的基础上耦合二维水动力学模型,建立水文-水动力耦合模型。以我国吉林温德河流域为研究实例,模拟了2017年“7·13”洪水在下游口前镇所处子流域洪水淹没过程。首先对基础数据进行预处理,建立HEC-HMS水文模型并进行参数优化后,最终获得流量过程水文结果作为水动力学模型边界条件,之后建立HEC-RAS二维水动力学模型对重要子流域进行淹没模拟。耦合模型计算结果显示,水文模型经多参数优化流量模拟的NSE系数为0.988,水动力计算最大淹没水深达9.3 m相对误差为-5.2%。从泛洪模拟结果来看,子流域上游部分的农田大量被淹,淹没水深范围在0.5~2.0 m,平均流速基本在1 m/s以下。下游口前镇内最大淹没水深接近1 m,水流速度0.2 m/s至1.5 m/s,与实际的淹没情况相吻合。研究表明,所建水文水动力耦合模型模拟计算的结果准确率较高,对具有复杂水文、水力条件的流域的洪水预报具有重要的指导意义。 相似文献
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流域水文模型研究的进展 总被引：14，自引：2，他引：12
流域水文模型是对流域上发生的水文过程进行模拟计算的数学模型 ,在水文过程模拟中 ,对流域内的产流 ,坡面汇流以及河道汇流过程的模拟是很重要的。坡面产汇流模型模拟从降水到流域产流和流域坡面汇流的水文子过程 ,河道演进模型模拟河网汇流水文子过程 ,现有的水文模型大多数是没有考虑水文变量和水文参数空间变化的概念性水文模型。随着地理信息技术的发展 ,考虑水文变量和水文参数空间变化的分布式水文模型得到了极大的重视与发展 ,而且 ,遥感技术的发展满足了分布式水文模型对空间信息的需求. 相似文献
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虚拟现实的三维时态GIS模式研究 总被引：3，自引：1，他引：2
三维场景是三维地理信息系统中人机交互的主界面。本系统中包括地球和流域两个场景,其中流域的两大基本要素是地形和河道。系统将DEM地形和河网表达在三维场景中,通过读取连续时段的河网格网数据进行水流的动态演示,体现时态GIS的历史回溯性;同时与虚拟现实结合,在场景中实时增加模型,并可以对其选择,变换,删除等。最后实现了对地形任意点的位置查询和不同时刻河流各格网点的水位、流速和流向的查询等功能,具备良好的人机交互性。 相似文献
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GIS在黄河防汛业务中的应用 总被引：1，自引：0，他引：1
1998年开始,黄河水利委员会(以下简称黄委)信息中心先后开发了基于GIS的山东防汛指挥系统、河南黄河工情险情会商系统和黄河下游工情险情会商系统。系统采用Sybase数据库,运行方式为客户机/服务器(C/S)方式。随着黄委“数字黄河”工程建设的开展以及计算机广域网络的扩大、开发技术运行方式的变化和用户的迅速增长,原有系统已不能满足实际需求。2002年开始,黄委基于WebGIS(MapXtreme)和地图服务中间件搭建了黄委地图服务平台。在此平台上,开发完成了Internet/Intranet版本的“黄河下游工情险情会商系统”。此系统可以在不同比例尺电子地图上实现无缝自动漫游(1∶1000000→1∶250000→1∶50000→1∶10000),实现了水文信息查询,防洪工程基础信息查询,防汛部署基本信息查询,实时工情、险情信息上报、查询统计,实时险情信息报警、处理、滚动显示,险情批复以及系统管理维护等功能。平台是按“数字黄河”三层架构搭建的,在平台的基础上对黄河下游工情、险情会商系统进行整合,以满足更广泛的需求。 相似文献
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基于DEM的流域水系分维计算与结果分析 总被引：7，自引：0，他引：7
利用ArcGIS8.3和ArcVIEW3.2中的水文分析模块,根据不同最小河流长度,提取晋江流域河网信息,采用传统的网格法计算提取的不同河网的分维,研究以最小河流长度所提取的不同河网密度与分维的关系,确定晋江流域分维,分析流域地貌的演变。 相似文献
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基于AO的洪水灾害风险分析模型设计与构建 总被引：2，自引：0，他引：2
中国是一个自然灾害尤其是洪涝灾害发生较频繁的国家,洪水灾害的风险分析与评估是抗洪救灾中的一个重要组成部分,洪灾风险分析的时效性、科学性对于防汛抗洪、抢险救灾具有重要的意义。本文针对流域洪水灾害的特点与其复杂的风险分析过程,考虑影响流域洪水灾害的因子,结合层次分析方法(AHP),以COM组件的架构思想为基础,采用ArcObjects语言的相关接口和方法,构建了流域洪水灾害风险分析模型,将各因子对洪水灾害的危险性和风险的影响进行了量化,分别得出洪水灾害风险性分布图和洪水灾害易损性分布情况。通过对洞庭湖试验区域的模型检验,结果表明,所构造的模型简单易操作,能够较好地对区域洪水灾害进行风险分析。 相似文献
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Located in the headwater upstream of the Taihu Lake region, which is a densely populated and economically developed area in
China, the West Tiaoxi River catchment is a frequently food-hit area due to its nature and climatic characteristics. During
the last several decades, more than ten catastrophic floods happened in this area, causing huge economic losses. Since 1990,
due to the increasing property vulnerability to flood hazard, the disasters were even more serious than before, and economic
losses increased year by year. Thus, there have great importance to study flood behaviors, flood risks and their consequences.
In this paper the hydrologic/hydraulic modelling is presented firstly. It is the method to study the relationship between
rainfall and runoff and the flood propagation process. Secondly, the author gives the summary of the current study methods
for flood risk assessment. The West Tiaoxi River catchment has a long history of the construction of polders and hydraulic
engineering. Most farmlands have been protected against floods. So the combination method has been used to obtain the real
risk area. The results have been obtained by using this method, which, the authors think, will be used in disaster preparedness,
property insurance etc.
Foundation item: Under the auspices of the National Natural Science Foundation of China (No. 49671028) and Deutsche Forschungsgemeinschaft
(DFG).
Biography: XU Peng-zhu (1965 —), male, a native of Funing County of Jiangsu Province, associate researcher. His research interests
include hydrology and water resources, numerical modelling, and application of GIS to hydrology. 相似文献
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Efficiency in solving the Saint-Venant equations for watershed rainfall-runoff routing is important in flood hydrology. This paper presents a high-efficiency numerical solution of one-dimensional dynamic wave equations (HEDWE) for watershed rainfall-runoff routing, in which the full momentum equation is written as a quadratic equation with only one unknown variable Q, water depth is derived from the continuity equation using the two-step predictor-corrector method, and the discrete scheme is the explicit upwind scheme. The results of numerical tests showed the HEDWE approach has several major advantages. 1) It is a stable numerical method, even for an initially dry area. 2) Its computational efficiency is higher than 4.76E+05 times/s. 3) It can be used for overland flow, river flow, and combinations thereof. The primary disadvantages of the HEDWE approach are its unsuitability for rapidly varying flow, such as dam-break floods. 相似文献
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在气候变化和城市化背景下,城市暴雨的局部特征愈发明显,而降雨监测和预报数据空间分辨率难以满足空间分布描述要求,造成城市洪涝模拟和预测结果存在不确定性。本文选择深圳市城区的3个流域,基于118场实测降雨数据,通过逐步增大网格尺寸以达到降低降雨空间分辨率的效果,同时以流域边界作为限制,保证流域内面平均雨量不变,然后将不同空间分辨率的降雨数据分别作为城市洪涝模型的输入条件,对流域出口断面的洪水过程进行模拟计算,每场降雨得到6种不同空间分辨率下的洪峰流量。结合降雨中心、流域几何中心等空间特征参数,分析降雨空间分辨率对流域洪峰的影响。研究结果表明,针对118场实测降雨,随着降雨数据空间分辨率逐渐降低,3个流域的出口断面的洪峰变化幅度逐渐增大;如果忽略了流域内部降雨数据的空间分布差异,洪峰变化幅度和方向与降雨中心和流域几何中心的空间关系具有相关性,降雨中心在流域几何中心上游方向的距离越大,洪峰降低的幅度越大。本文基于3个城市流域得到了相似的研究结论,研究方法可为城市流域洪涝模拟提供借鉴,研究结果可为河道洪水风险评价提供参考。 相似文献
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RESEARCH ON SYSTEM OF FLOOD DISASTER CONTROL AND REDUCTION SUPPORTED BY GIS IN MEDIUM AND SMALL BASINS 总被引：2，自引：0，他引：2
Southeast China coastal areas belong to subtropical monsoon climatic zone,thus easily affected by floods resulted from typhoons and rainstorm.Since the areas of river basins are small,rivers flood regulation capacities are low,and therefore flood hazard is grave.In the paper,taking the Yongjiang basin in southeast China as an example,the approaches and methods of geographic information system(GIS) applied to flood disaster control and reduction research on small basin are explred.On GIS help the rainfall-runoff calculation model and the river dchannel flood routing model are developed.And the evaluating flood submerged are and the damage assessment models are built supported by digit elevation models.Lastly the decision support system on GIS supported for flood control in research basin has been set up.This greatly improves flood-proofing decision-making capacities in river basin,and provides valuable information and a mode for flood prevention and reduction in the medium and small basin .Meanwhile,the research indicates that technologies of GIS provide a powerful tool for flood disaster control. 相似文献
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Flashfloodsaretheimportanteventsofthehydrologicalregimeofriversinaridareas.IntheTarilncaver(Fig.1),northwesternChina,flashfledarebeingmonitored.TheobSerVeddataandinvestigationdemonstratethedifferenceintime,place,frequencyandintensityoftheiroccurrences.Therearethreet~offlagescommontotheThermcaverbasin.AlmOSteveryyea-rhighwateroccursinmonthesofJuly,AugUstandseptembercausedbyablationrunoff.However,themostdamagingflowSarefromoccasionalflashfindsbyinstenserainstormandglacierlakeoutburstflags(… 相似文献
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Use of numerical simulation of the tidal flow of the Changjiang River Estuary and the HuangpuRiver to forecast flood in the Taihu Lake lower reach drainage system for the case of future sea level riseof 0.4 m and 0.8 m,and floods preventing and reducing methods are discussed in this paper. 相似文献
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Mountain effect and differences in storm floods between northern and southern sources of the Songhua River Basin 总被引：2，自引：2，他引：0
In this study, the differences in annual rainstorm changes in the Second Songhua River Basin and the Nenjiang River basin and their causes were compared from the perspective of mountain effects. The following results were drawn: (1) Altitude effect is the primary factor leading to increased rainstorms in the southern source; (2) Slope effect primarily leads to differences of the weather systems in the two sources, and thus cause the difference of the rainstorms; (3) Slope effect is responsible for the greater fluctuation in the observed floods in the southern source. These landform differences eventually lead to the differences in the characteristics of floods in the southern and northern sources. Commensurability method was used to identify the period of rainstorms in the southern and northern sources. The results showed that although rainstorms do not appear at the same time in the two sources they are characteristic of a 10 years’ period in both areas. These results can serve as hydrological references for flood control and long-term flood disaster predictions. 相似文献
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MECHANISM AND EFFECT OF CHANNEL EVOLUTION AT ESTUARY OF WEIHE RIVER TO HUANGHE RIVER 总被引：2，自引：0，他引：2
LI Jing-yi SHI Chang-wei XU Xi-bao FU Zhi-jun 《中国地理科学(英文版)》2006,16(2):122-126
1INTRODUCTION Physiognomycharacteristicofawatershedisasymbolof ground erosion and incision, and it has been one of the most important factors influencing soil erosion and sedi- ment in the drainage area. Therefore physiognomy char- acteristic of the watershed and its influences on hydro- logical bed load have been one important focus in the watershed research both domestic and abroad (SCHUMM, 1977; QIAN et al., 1987) since the classical study by Horton in 1942 (HORTON, 1954). In rec… 相似文献
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The heavy floods in the Taihu Basin Showed increasing trend in recent years.In this work,a typical area in the northern Taihu Basin was selected for flood rish analysis and potential flood losses assessment.human activities have strong impact on the study area‘s flood situation(as affected by the polders built,deforestation,population increase,urbanization,etc.) and have made water level higher,flood duration shorter,and flood peaks sharper.Five years of different flood return periods[(1970),5(1962),10(1987),20(1954),50(1991)] were used to calculate the potential flood risk area and its losses.The potential flood risk map,economic losses,and flood-impacted population were also calculated.The study‘s main conclusions are:1) Human activities have strongly changed the natural flood situation in the study area,increasing runoff and flooding;2) The flood risk area is closely related with the precipitation center;3) Polder construction has successfully protected land from flood.Shortened the flood duration,and elevated water leel in rivers outside the polders;4) Economic and social development have caused flood losses to increase in recent years. 相似文献