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Estimation Of Probable Maximum Precipitation And Isohyete Map In Didessa Sub Basin, Abbay Basin Ethiopia

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dc.contributor.author Nigatu Nura
dc.contributor.author Tamene Adugna
dc.contributor.author Chala Hailu
dc.date.accessioned 2022-04-14T11:47:45Z
dc.date.available 2022-04-14T11:47:45Z
dc.date.issued 2021-01
dc.identifier.uri https://repository.ju.edu.et//handle/123456789/7099
dc.description.abstract Probable Maximum Precipitation (PMP) is theoretically maximum depth of precipitation for a given duration: It is physically possible over a given size storm area at a specific geographical location at a particular time of year. The PMP is used for the design of a hydraulic structure appropriately in the study area. The procedure for estimation of PMP used in the country is based on Hershfield’s graphical estimation, but different studies show that the value founded from the chart was not reliable. Therefore, the main objective of this study is to Estimate the Probable Maximum Precipitation and develop Isohyetal Map in Didessa Sub Basin using Hershfield’s statical method. Microsoft excel, RAINBOW, Easy fit and Arc GIS software where the materials used for this study Double mass curve is employed for consistency test. The study shows that for 1day, 2and 3day the maximum Frequency factor Km and PMP value obtained by Hershfield’s statical method are 5.10 and 255.57mm respectively. Whereas, the computed maximum km and PMP from the chart is 16 and 513.96. The values exhibited deviation about 213.73 for km and 101.10% for PMP. This result confirmed that the value of PMP from chart is over estimated which can leads to uneconomical designs in the Didessa Sub Basin. The ratio of one day rainfall depth for a return period of 2,5,10,25,50,100,200,500,1000,2000,5000 and 10,000 year floods had been estimated and found to vary from minimum 52.69mm to maximum 210.74m. The estimated PMP values to 10,000 years return period founded by Hershfield’s statical methods was 1.12, 1.17 and 1.26 times that of 10,000 years return period rainfall depth for 1day 2day and 3day duration respectively in the DSB. Isohyete maps were generated by IDW interpolation method and PMP grid values were varying between 124mm to 167mm. This study clearly indicates that the Hershfield chart gives highest values of PMP due to highest value of Km from the chart. So, further researches should be conducted on the rest of Ethiopian basins for fixing the country’s reliable maximum Frequency fator (km). en_US
dc.language.iso en_US en_US
dc.subject Didessa Sub Basin, Hershfield Statistical Method, Isohyetal Map, Probable Maximum Precipitation en_US
dc.title Estimation Of Probable Maximum Precipitation And Isohyete Map In Didessa Sub Basin, Abbay Basin Ethiopia en_US
dc.type Thesis en_US


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