dc.description.abstract |
Flood is a natural disaster that occurs suddenly which runs from hilly land to low land
area of river banks when runoff exceeds the capacity of the natural or artificial water
conveyance structures. Currently, the hazard of flood is common in some parts of Ethiopia
including Bilate watershed and cause heart breaking losses in terms of property and even
human life in flat river flood plains due to elevation difference and climatic factors. The
main cause of flood disaster vulnerability is due to unavailability of proper river and
watershed management. Hence, the intended aim of this research is to carryout inundation
mapping and hazard assessment of Bilate River flood plain. The required data for this
analysis were, Digital Elevation Model, streamflow data, soil type and land use land cover
map. These data were collected from Ministry of Water, Irrigation and Electricity in legal
request. Hydraulic Engineering Center- Geographic River Analysis System (HEC-GeoRAS
10.3) was used to prepare RAS import file for steady flow analysis on Hydraulic
Engineering Center-River Analysis System(HEC-RAS5.0.1). Stream flow data was checked
for outlier, consistency and homogeneity at different significance level using Grubbs and
Beck(G-B) test, double mass curve method and Mann-Whitney tests respectively. For flood
frequency analysis parameter estimation of worldwide used distribution functions was
done by three important parameter estimation methods such as: method of moment,
probability weight method and maximum likelihood method. Best fitted Pearson type
distribution function was selected by linear moment(L-moment), D-index, root mean
square and correlation coefficient methods. The estimated peak floods in Bilate at Tena
Bilate gauging station for 5, 10, 50, 100 and 200 years return periods were 153.2, 193.2,
273.6, 305.3 and 335.9 m
3
/s respectively. Mapping of flood inundation was processed with
inter connection of GIS extension tool HEC-GeoRAS and HEC-RAS software. The flood
inundations for 5,10,50,100 and 200 years return period were 6840.244, 7284, 8029.13,
8270.031 and 8463 ha respectively. Flood hazard map were prepared by reclassifying
depth grid and its area bounding polygon. Also the assessment of hazard lever with
integrating flood causative agent land use land cover map with hazard map prepared after
post-RAS processing. Area inundated at sever to moderate hazard is ranges between 4% to
10.3% and around 58% was very low hazard area and out of these shrub land, cultivation
area and grass land covers large portion of delineated flood area 44%, 25-28% and 13-
15% respectively in all return periods. Hence, the result of the level of hazard indicates
that there is significant potential of flood and the consequence risk on livelihood in study
area. It is recommended that, the watershed management party or any stakeholder, should
use this research finding to take appropriate measure and reduce flood disaster. |
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