Abstract

This study investigated the impact of seasonal land cover changes on human thermal comfort outdoors in Harare, Zimbabwe in Southern Africa. Multi-temporal thermal infrared and in situ air temperature data were used to develop simple linear regression model for retrieving air temperature from land surface temperature (r2=0.6897). Season specific simple linear regression models for deriving relative humidity from land surface temperature were also developed (r2 greater than 0.78). When tested against in situ observations, the LST-based approach retrieved DI with high accuracy for each sub-season (mean percentage error less than 20%). The findings showed that vegetation fraction was higher (0.60) in the most comfortable post-rainy season than in the most thermally uncomfortable season (0.43), hot season. Outdoor thermal discomfort was high in hot season (mean DI of 31 °C), while the post-rainy season was the most thermally comfortable (mean DI of 19.9 °C). During the hot season, thermal discomfort was higher in densely built-up areas (DI greater than 27 °C) than in the northern areas where low-density residential areas, forests and most well maintained parks are located (DI less than 27 °C). It was concluded that Landsat 8 data detects seasonal land use/cover and thermal discomfort changes with high accuracy.

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