How urban growth changes the heat island effect and human thermal sensations over the last 100 years and towards the future in a European city?

Abstract

Urban development exacerbates urban heat island effects of cities and thermal discomfort of the residents worldwide. However, such urban effects vary with the geographical and climatic conditions of the respective cities. This study is the first to quantitatively estimate the impact of past (1878), present (2012), and future (2050) urbanization on surface air temperatures and human thermal comfort in Sofia, the largest city of Bulgaria. We used the state‐of‐the‐art Weather Research and Forecasting (WRF) climate model, with a 1‐km horizontal resolution for three cases: LU1878, LU2012, and LU2050. We first validated the results of the control simulation (case LU2012) against actual observations. The model satisfactorily reproduced the diurnal variation of the observed monthly mean surface air temperatures for July (2011–2013) with a mean bias of ±0.6°C. We then estimated the potential impacts of past and future urbanization on surface temperature. Our results suggest that because of urbanization of Sofia, the surface air temperature at 0600 Local Standard Time (LST) has increased approximately 4.0°C in the past (1878–2012) and approximately 0.4°C in future (2012–2050). We also evaluated the impact of the urban thermal environment on human comfort levels. Considering the LU2050 case in the central part of Sofia, the temperature–humidity index during mid‐afternoon (1400–1700 LST) is estimated to be 24–26, indicating that approximately 50% of the residents could feel perceptibly uncomfortable.

Editorial: Atmospheric processes and applications in urban, coastal and mountainous terrain

“…Modifications in urban climate conditions can be caused by local land cover changes and alterations in the background climate, that is, by global warming. Vitanova et al (2021) explore the first aspect by means of simulations with the Weather Research and Forecasting (WRF) model, to evaluate the effects of urban growth on the UHI and human thermal sensations in the city of Sofia (Bulgaria). The authors highlight that past land cover changes (from 1878 to 2012) had a significant effect on urban temperatures, while weaker variations are estimated for the future since the growth of the urban area is expected to be less significant.…”