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Impacts of land cover and land use changes on stream flow: A case from the Nile Basin. By Simon Mutie, Hussein Gadain, and Guleid Artan. Background. Since 1960’s LULC changes have been a threat to life in the Nile Basin;
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Impacts of land cover and land use changes on stream flow:A case from the Nile Basin By Simon Mutie, Hussein Gadain, and Guleid Artan
Background • Since 1960’s LULC changes have been a threat to life in the Nile Basin; • High population increases has led to changes in land tenure systems resulting in deforestation expansion and intensification of agriculture; • These changes in land cover have caused changes in the water balance of the basin.
Deforestation-Mau Problem Statement • Population growth rate 7.5%, • High population = changes in land tenure systems, • Deforestation and intensification of agriculture and overstocking, • Reduction of perennial natural vegetation, • Rise in bare and agricultural lands. • Modifications of land cover and soils affect runoff hence water availability, • High sedimentation and water quality concerns. Wheat-Narok Flooding-Nzoia
Study Area Upper Nile Basin
Economic Importance of the basins • Both basins originate from the indigenous and exotic greater Mau, Mt. Elgon and Cherangany forests. • Large-scale/cash crop plantation • Tea, sugarcane, rice, wheat and high value horticultural crops. Small-scale mixed farming also practised • Pastoralists with the nomadic Maasai community in Mara River basin. • Mara basin houses the Serena-Mara-Serengeti wildlife sanctuary declared the seventh wonder in the world • Swamps (Yala & Mosirori) which support a lot of biodiversity.
Deforestation-Mau Major Ecosystem Threats • Widespread encroachment and deforestation of the Mau forest tower, Mt Elgon Forest • Rapid population growth and immigration into the basins. • Expansion and intensification of agriculture • Conversion and rehabilitation of basin wetlands for agricultural production e.g. Yala swamp Rice Growing-Yala swamp Source: Nation media Mosirori Swamp Overstocking-Mara
Overall objective To determine the effects of land use & land cover changes on the river flow in the two basins
Data and Methods • LANDSAT images for the dry season (MSS and TM/ETM, for the years 1973, 1986 and the 2000 respectively) • Image processing and classification; GPS used for surveys to collect ground-truth data on vegetation and land use/cover Pixel Resolution MSS – 79 * 56 m TM and ETM – 28.5 * 28.5 m Source: USGS
False Color composite of bands 2,3&4 – 1986 data LULC Mapping
LULC Changes Mara River Basin
Stream Flow Model Data Preprocessing Rain MAP Water Balance MAE Evap Basin Soil Lumped Routing Linkage Routing Parameters LU/LC Dist. Routing Soil Parameters DEM Obsv. S.Flow Data Streamflow Geo-spatial SFM System Diagram
Effects of Land use change on stream flow • Earlier than normal peaks • Higher peaks • Change in evaporation process • Soil erosion and sedimentation • produced streamflow at rainfall magnitudes that did not generate any streamflow with the 1973 dataset. • Changes are slight in Nzoia
Conclusions • There has been decline of natural vegetation in the two basins and a rise in land covers due to anthropogenic influences in the basin. • The changes have caused higher and earlier occurrence of flood peaks. • Increase in agriculture coupled with poor farming practices in the two basins has led to high sediment loads deposited on the river mouths. • In Mara basin, sediment deposition at river mouth has caused backwater flow which has increased the wetland submerging farms. • In Nzoia basin, deposition at lower river stages is raising the river channel, hence water topping the flood dykes every season
Potentialities/Limitations RS Limitations • Data Availability • Cost • High cost analysing Potentialities • Descision making and planning