Abstract

The land surfaces of hot-humid tropical urban areas are exposed to significant levels of solar radiation. Increased heat gain adds to different land surface temperature profiles in cities, resulting in different thermal discomfort thresholds. Using multi-temporal (1986, 2001, and 2017) landsat data, this study examined the impact of land use change on urban temperature profiles in Umuahia, Nigeria. The findings revealed that over time, built-up regions grow in surface area and temperature at the expense of other land use. The transfer matrix, showed that approximately 59.88 percent of vegetation and 8.23 percent of bareland were respectively changed into built up during the course of 31 years. The highest annual mean temperature in built-up regions was 21.50°C in 1986, 22.20°C in 2001, and 26.01°C in 2017. Transect profiles across the landuses reveals that surface Temperature rises slowly around water/vegetation and quickly over built-up and bare land area. The study observed drastic changes in land cover with a corresponding increase in surface temperature for the period between 1986 and 2017 with consistent decrease in water bodies and bare land in the study area. Overall, the spatio-temporal distribution of surface temperature in densely built up areas was higher than the adjacent rural surroundings, which is evidence of Urban Heat Island. The impact of landuse change on urban surface temperature profiles could provide detailed data to planners and decision makers in evaluating thermal comfort levels and other risk considerations in the study area.

Highlights

  • Different land uses in urban areas result in a variety of natural and man-made surfaces which alters their surface structure, energy balance, and micro-atmospheric conditions

  • The aim of this study is to provide understanding on the influence of land use change and its impact on surface temperature profiles in a hot humid urban area

  • As at 1986, vegetation had the highest spatial coverage followed by bare land, built up and water bodies

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Summary

Introduction

Different land uses in urban areas result in a variety of natural and man-made surfaces which alters their surface structure, energy balance, and micro-atmospheric conditions. Temperature profiles of cities in the humid tropics are modified by anthropogenic factors resulting from many physical and economic activities These changes in temperature can adversely impact our health, occupation, infrastructure and thermal comfort (Edward et al, 2021). Studies such as Arnfield (2003) and Mukherjee and Singh (2020) have found considerable thermal differences in urban areas, during the day, as well as a strong association between land use changes and temperature distribution. These shifts are linked to changes in urban land use and land cover patterns including physical and morphological factors

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