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Flood risk assessment in Kalu river basin Sri Lanka using geospatial techniques and hydrological modelling

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dc.contributor.advisor Wijayaratna TMN
dc.contributor.author Gurung R
dc.date.accessioned 2022
dc.date.available 2022
dc.date.issued 2022
dc.identifier.citation Gurung, R. (2022). Flood risk assessment in Kalu river basin Sri Lanka using geospatial techniques and hydrological modelling [Master's theses, University of Moratuwa]. Institutional Repository University of Moratuwa. http://dl.lib.uom.lk/handle/123/21989
dc.identifier.uri http://dl.lib.uom.lk/handle/123/21989
dc.description.abstract Kalu Ganga basin is one of the main waterway basins in Sri Lanka which gets exceptionally high rainfalls with higher discharges. This report is about how the different zones, having a higher likelihood of a flood in the Kalu Ganga basin can be identified through remote sensing and geospatial approach. RRI model was additionally used to get the flood extents to verify the flood susceptibility map. Six flood influencing parameters (elevation, slope, land use, flow accumulation, soil, and rainfall) were taken for obtaining a flood susceptibility map with the AHP method in ArcMap. In the RRI model, the built-in data (Flow Direction, Flow Accumulation, DEM, Soil, and Land Cover) with observed rainfall data was used for generating a flood inundation map. The flood susceptibility map has a flood susceptibility area under the Very High category of 267 km² (8.4%) in the Kalu Ganga basin which is the most probable flood occurrence area. The flood inundation maps of May 2003, April 2008, and May 2008 have an area of 217.9 km² (6.3%), 193.6 km² (5.6%), and 108.5 km² (3.1%), respectively with flood depths greater than or equivalent to 1 meter in Kalu Ganga basin where the flood depths greater than or equivalent to 1 meter cover all the flood depths. In the AHP method, the rainfall parameter greatly influenced the flood susceptibility map. The built-in data with nr river value and ns slope values greatly influence the flood inundation map in the RRI model. The flood susceptibility map from the AHP method in ArcMap has a higher flood potential area than the flood inundation map obtained from the RRI model, and this is because the simulated or observed flood maps are always a subset of the flood susceptibility map. The flood susceptibility map obtained from the AHP method in ArcMap is a flood probability map and the flood inundation map from the RRI model is a simulated flood map. Therefore, they are different. However, the flood inundation area occurs within the flood susceptibility map. The Analytical Hierarchy Process (AHP) method is an alternative quick method of identifying flood potential areas and it can be applied to any other place around the world for the prevention and management of flood hazards. en_US
dc.language.iso en en_US
dc.subject ANALYTICAL HIERARCHY PROCESS (AHP) en_US
dc.subject FLOOD MAPPING en_US
dc.subject FLOOD RISK ANALYSIS en_US
dc.subject RAINFALL-RUNOFF-INUNDATION (RRI) MODEL en_US
dc.subject WATER RESOURCES ENGINEERING AND MANAGEMENT – Dissertation en_US
dc.subject CIVIL ENGINEERING - Dissertation en_US
dc.title Flood risk assessment in Kalu river basin Sri Lanka using geospatial techniques and hydrological modelling en_US
dc.type Thesis-Abstract en_US
dc.identifier.faculty Engineering en_US
dc.identifier.degree MSc in Water Resources Engineering and Management en_US
dc.identifier.department Department of Civil Engineering - Madanjeet Singh Centre en_US
dc.date.accept 2022
dc.identifier.accno TH4960 en_US


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