{"title":"HEAVY RAINFALL IN THE R.N. MACEDONIA","authors":"Violeta Gjeshovska, Goce Taseski, Bojan Ilioski","doi":"10.55302/sjce21102019gj","DOIUrl":null,"url":null,"abstract":"(i-T-p) of crucial data are in different parts of the world due to lack of sufficient measuring stations and also due to unprocessed, data. In the in practice. for these data is more than necessary, that is an extremely stochastic phenomenon. pluviographic eight measuring stations been analyzed Maximum precipitation series with a duration of 5, 10, 20, 40, 60, 90, 300,720 and 1440 have been established for the entire period from to All these arrays of data have been tested for homogeneity and statistically processed. The probability of occurrence of maximum annual precipitation has been defined according to the adopted mathematical probability function and the i-T-p curves have been constructed. The results of the analysis are presented in a tabular and graphical form. drainage of atmospheric waters, regulation of rivers with small catchment areas, regulation of torrents and sizing of anti-erosion protection","PeriodicalId":30755,"journal":{"name":"Selected Scientific Papers Journal of Civil Engineering","volume":"18 1","pages":""},"PeriodicalIF":0.0000,"publicationDate":"2021-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"Selected Scientific Papers Journal of Civil Engineering","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.55302/sjce21102019gj","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
引用次数: 0
Abstract
(i-T-p) of crucial data are in different parts of the world due to lack of sufficient measuring stations and also due to unprocessed, data. In the in practice. for these data is more than necessary, that is an extremely stochastic phenomenon. pluviographic eight measuring stations been analyzed Maximum precipitation series with a duration of 5, 10, 20, 40, 60, 90, 300,720 and 1440 have been established for the entire period from to All these arrays of data have been tested for homogeneity and statistically processed. The probability of occurrence of maximum annual precipitation has been defined according to the adopted mathematical probability function and the i-T-p curves have been constructed. The results of the analysis are presented in a tabular and graphical form. drainage of atmospheric waters, regulation of rivers with small catchment areas, regulation of torrents and sizing of anti-erosion protection