Abstract:
This study examines the spatiotemporal dynamics of the Urban Heat Island (UHI) effect in
the Southeastern region of Sri Lanka, from 2019 to 2025, utilizing Landsat-8/9 satellite
imagery and ArcGIS Pro analysis. Despite minimal land use changes, results indicate a
significant rise in Land Surface Temperature (LST) from 36.31 °C in 2019 to 37.54 °C in
2025, with Urban Heat Island Intensity (UHII) increasing from 0.009172 to 0.01159.
Supervised classification revealed a decline in vegetation cover (NDVI from +0.81 to -0.13)
and an increase in urban (9% to 16%) and bare land (2% to 15%) areas, correlating with
elevated LST and UHII, particularly during dry seasons. Albedo measurements using a lux
meter showed low reflectivity (0.055-0.278) for urban surfaces like roads and concrete,
enhancing heat retention, while paddy fields (0.07-0.11) contributed to temperature rises
under reduced moisture. It indicates Sammanthurai has low albedo surface and it causes to
rice temperature of the area. Weather data from 2024 highlighted a peak temperature of 38.7
°C, with a weak positive correlation (slope 0.02) between solar radiation (224.64 W/m²) and
temperature, exacerbating UHI effects. Comparative analysis with Kitulgala’s wetter,
forested region (207.065 W/m², 24-31 °C) underscores the role of vegetation and climate in
mitigating heat. The study, achieving 91% classification accuracy (Kappa 0.88541),
emphasizes climatic factors and land management as key drivers of UHI in semi-rural,
agrarian landscapes.
