Show simple item record

dc.contributor.authorNanseera, Jonathan
dc.date.accessioned2022-05-26T06:09:59Z
dc.date.available2022-05-26T06:09:59Z
dc.date.issued2020-11-30
dc.identifier.citationNanseera, Jonathan. (2020). Remote sensing and GIS-based modelling of land cover change for runoff simulation. (Unpublished undergraduate dissertation) Makerere University; Kampala, Uganda.en_US
dc.identifier.urihttp://hdl.handle.net/20.500.12281/12949
dc.descriptionA final year project report submitted to the department of Geomatics and Land Management in partial fulfillment of the requirements for an award of a Bachelors degree of Bachelor of Science Land Surveying and Geomatics of Makerere University.en_US
dc.description.abstractThe Murchison Bay is a catchment located in the northern shoreline of Lake Victoria basin that supports several human related activities in Uganda. Because of this, the catchment has undergone remarkable land cover changes, over the years. This study aimed at quantifying the land cover changes between 2000 and 2020 as well as predicting the changes that will happen by 2030 in this area and simulating the runoff that will happen with these changes. These objectives were achieved through remote sensing and GIS techniques using ArcGIS 10.3 software with hydrological tool extensions added. The land cover changes were determined through classification of Landsat images in the different years and image differencing was done to determine the changes over those 20 years. The study determined that the dominant changes between 2000 and 2020 were increases of builtup land (44.09% to 50.19%), bare soil (5.28% to 9.19%) and water bodies (2% to 2.27%), and decreases in the following classes: wetlands lands (from 8.02% to 4.02%), grassland (from 30.53% to 25.5%), and trees (from 10.08% to 8.83%). Considering the driving forces responsible for the change, LRM was used to stimulate and forecast LCC over time till 2030. This procedure showed that the built-up class will keep expanding further for the same reasons such as population growth. By 2030, the built-up class will occupy 59.52% of this area. Surface runoff is the flow of water occurring when the soil is infiltrated from rain and other sources flow over land to maximum capacity and excess water. It is a major component of the water cycle and a key agent for soil erosion, floods and water contamination. The predicted land cover transformations will obviously have some negative environmental impacts among which is increased surface run off, by 2030, the simulated surface run off will have the deepest as 32mm by 2030.en_US
dc.language.isoenen_US
dc.publisherMakerere Universityen_US
dc.subjectLand Cover, Runoffen_US
dc.subjectSensing and GIS-based modellingen_US
dc.subjectLand coveren_US
dc.subjectRunoff simulationen_US
dc.titleRemote sensing and GIS-based modelling of land cover change for runoff simulation.en_US
dc.typeThesisen_US


Files in this item

Thumbnail

This item appears in the following Collection(s)

Show simple item record