Water resources in Makindu Sub-County, Makueni County, Kenya, are under severe stress from
converging environmental and anthropogenic factors. This study employed GIS-based remote
sensing, meteorological time-series analysis, participatory GIS (PGIS) mapping, and quantitative
regression modelling to assess the combined effects of rainfall variability, temperature change,
and land use/land cover change (LULCC) on major water resources across the period 1994–
2024. SPOT satellite imagery classified across four epochs (1994, 2004, 2014, 2024) using
Maximum Likelihood Classification documented substantial LULCC, while Kenya
Meteorological Department records and CHIRPS gridded data were analysed for hydro-climatic
trends. A PGIS inventory covering nine sub-locations quantified functional boreholes, seasonal
rivers, dams, water pans, and springs for each epoch. Simple linear regression, multiple
regression, and chi-square analyses were conducted in SPSS Version 25. Results reveal a 2,400%
increase in functional boreholes (3 to 75) driven by population growth and surface water
depletion, while seasonal rivers remained stable but showed critical sub-location-level
deterioration, dams and water pans increased from 25 to 37 through community investment, and
springs remained constant at 4 functional units across all four epochs. Rising mean annual
temperatures (R² = 0.958–0.982; p < 0.01) and declining rainfall were statistically associated
with surface water loss across seasonal rivers, dams, and water pans, while springs remained
stable at 4 functional units unresponsive to temperature, rainfall, or population change reflecting
deep aquifer supply. The study provides a comprehensive evidence base for multi-stakeholder
water resource management and policy development in semi-arid Kenya.