A. Urzică, Alin Mihu-Pintilie, E. Huțanu, B. Ghindaoanu, L. Albu
{"title":"USING GIS METHODS FOR MODELLING EXCEPTIONAL FLOOD EVENTS IN BASEU RIVER BASIN, NE ROMANIA","authors":"A. Urzică, Alin Mihu-Pintilie, E. Huțanu, B. Ghindaoanu, L. Albu","doi":"10.18509/gbp.2018.51","DOIUrl":null,"url":null,"abstract":"The Baseu catchment basin is situated in the northeast of Romanian and it is a right-side tributary of the Prut River. At the end of spring the most significant floods occur on the Romanian territory. They are due to the maximum amounts of rainfall and to snow melting. The phenomenon is also specific to the Baseu catchment basin. The last 20 years have witnessed a change in temporal manifestation, with maximum intensities during the summer (the months of July and August) when heavy rainfall is recorded. In the last 40 years, several critical episodes occurred, which endangered the lives of 79,000 inhabitants. In order to assess the hazard associated with maximum runoff, a floodable stripe with an assurance of 1% (once every 100 years) was modelled. Flood modelling involved the manipulation in GIS setting of the parameters of digital elevation model (DEM) and of their relations with the hydrological system. The main objective of the study is the modelling of an exceptional flood with a probability of 1%, similar to the one of 1969, when the Stefanesti gauging station recorded a flow of 330 m/s. Based in the analysis of the hydrological data spanning over 50 years, recorded at three gauging stations, a maximum flow of 248.1 m/s was determined (the Stefanesti gauging station), using the Pearson III probability curve. The findings have highlighted the significant vulnerability of the human settlements situated in the flood plain of the Baseu River. A surface of 17,000 ha would be flooded, accounting for around 17.5% of the total basin surface.","PeriodicalId":179095,"journal":{"name":"Proceedings 2018","volume":"21 1","pages":"0"},"PeriodicalIF":0.0000,"publicationDate":"2018-09-24","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"4","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"Proceedings 2018","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.18509/gbp.2018.51","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
引用次数: 4
Abstract
The Baseu catchment basin is situated in the northeast of Romanian and it is a right-side tributary of the Prut River. At the end of spring the most significant floods occur on the Romanian territory. They are due to the maximum amounts of rainfall and to snow melting. The phenomenon is also specific to the Baseu catchment basin. The last 20 years have witnessed a change in temporal manifestation, with maximum intensities during the summer (the months of July and August) when heavy rainfall is recorded. In the last 40 years, several critical episodes occurred, which endangered the lives of 79,000 inhabitants. In order to assess the hazard associated with maximum runoff, a floodable stripe with an assurance of 1% (once every 100 years) was modelled. Flood modelling involved the manipulation in GIS setting of the parameters of digital elevation model (DEM) and of their relations with the hydrological system. The main objective of the study is the modelling of an exceptional flood with a probability of 1%, similar to the one of 1969, when the Stefanesti gauging station recorded a flow of 330 m/s. Based in the analysis of the hydrological data spanning over 50 years, recorded at three gauging stations, a maximum flow of 248.1 m/s was determined (the Stefanesti gauging station), using the Pearson III probability curve. The findings have highlighted the significant vulnerability of the human settlements situated in the flood plain of the Baseu River. A surface of 17,000 ha would be flooded, accounting for around 17.5% of the total basin surface.
Baseu集水区位于罗马尼亚东北部,是Prut河的右侧支流。春天结束时,罗马尼亚领土上发生了最严重的洪水。它们是由于最大的降雨量和积雪融化。这种现象也只出现在Baseu流域。过去20年的时间表现发生了变化,在夏季(7月和8月)记录到强降雨时强度最大。在过去的40年里,发生了几次严重事件,危及到7.9万居民的生命。为了评估与最大径流相关的危害,模拟了一个保证1%(每100年一次)的可淹水条带。洪水建模涉及到在GIS设置中对数字高程模型(DEM)参数及其与水文系统关系的处理。这项研究的主要目的是模拟一场概率为1%的异常洪水,类似于1969年的那次,当时Stefanesti测量站记录的流量为330米/秒。基于对三个测量站记录的50多年水文数据的分析,利用Pearson III概率曲线确定了最大流量为248.1 m/s (Stefanesti测量站)。调查结果突出了位于巴苏河洪泛区的人类住区的严重脆弱性。17000公顷的土地将被淹没,约占整个流域面积的17.5%。