Impact of Climate Variability and Land Use Change on Streamflow in Thika River Watershed, Kenya

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dc.contributor.author Njoroge, James Muiruri
dc.date.accessioned 2025-11-28T11:50:19Z
dc.date.available 2025-11-28T11:50:19Z
dc.date.issued 2025-11-28
dc.identifier.citation NjorogeJM2025 en_US
dc.identifier.uri http://localhost/xmlui/handle/123456789/6835
dc.description MSc in Environmental Engineering and Management en_US
dc.description.abstract Streamflow variability poses challenges to water security in Nairobi City, which relies heavily on the Thika River watershed upstream of RGS 4CB05 in the Upper Tana catchment. Over the past few decades, the watershed has faced marked streamflow declines that have intensified water shortages and entrenched rotational rationing. This was evident particularly during severe droughts such as the 2016/2017 event when Thika Dam dropped to critically low levels. At present, Nairobi’s installed production capacity of approximately 525–560 million liters/day remains far below the city’s demand, which exceeds 850 million liters per day. Therefore, there is urgent need to disentangle the impacts of climate and land use changes on Thika River watershed hydrology, as they are the main drivers of streamflow variability. The objective of this study was to assess and quantify these impacts on streamflow dynamics in the Thika River watershed. Mann-Kendall and sequential Mann-Kendall tests were applied to detect trends and breakpoints, while the Wang-Tang Budyko model partitioned the relative contributions of climate variability and land use change. Drought patterns were analyzed using the Standardized Precipitation-Evapotranspiration Index (SPEI) and Standardized Runoff Index (SRI). Future streamflow was simulated using the SWAT (Soil and Water Assessment Tool) model under the IPCC RCP 4.5 scenario for 2050–2065. Findings revealed a significant decline in streamflow with a breakpoint in 2003. Climate variability accounted for 46% of the reduction, mainly through decreased precipitation and rising evapotranspiration, while land use changes dominated by deforestation and agricultural expansion contributed 54%. Post-2003, hydrological droughts became more severe and recurrent, with projections indicating worsening conditions mid-century due to temperature rise and rainfall variability. The study recommends strengthening hydro-climatic monitoring and drought preparedness systems, mainstreaming climate and land use considerations into watershed planning, and enforcing land use regulations alongside community-based reforestation, afforestation, agroforestry, and soil-water conservation. Further research should incorporate a wider range of climate (RCP 2.6, 6.0, 8.5) and land use scenarios to better capture future uncertainties. By integrating the Budyko framework with drought indices, this study provides a robust, transferable approach for managing water resources in the Thika River watershed and similar climate-sensitive catchments globally. en_US
dc.description.sponsorship Dr. Hosea Munge Mwangi, PhD JKUAT, Kenya Prof. John Mwangi Gathenya, PhD JKUAT, Kenya Prof. (Eng.) Bancy Mati, PhD JKUAT, Kenya en_US
dc.language.iso en en_US
dc.publisher COHRED- JKUAT en_US
dc.subject Climate Variability en_US
dc.subject Land Use Change en_US
dc.subject Streamflow en_US
dc.subject River Watershed en_US
dc.title Impact of Climate Variability and Land Use Change on Streamflow in Thika River Watershed, Kenya en_US
dc.type Thesis en_US


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