Emergence of opposite trends in daytime and night-time urban heat island intensities in England
- 1University of Bristol, United Kingdom of Great Britain and Northern Ireland (eunice.lo@bristol.ac.uk)
- 2MetOffice@Reading, Department of Meteorology, University of Reading, UK
- 3University of Exeter, UK
- 4National Centre for Atmospheric Science, Department of Meteorology, University of Reading, UK
- 5University of Edinburgh, UK
- 6University of East Anglia, UK
- 7Met Office Hadley Centre, UK
Urban environments are known to be warmer than their sub-urban or rural surroundings, particularly at night. In summer, urban heat islands exacerbate the occurrence of extreme heat events, posing health risks to urban residents. In the UK where 90% of the population is projected to live in urban areas by 2050, projecting changes in urban heat islands in a warming climate is essential to adaptation and urban planning.
With the use of the new UK Climate Projections (UKCP18) in which urban land use is constant, I will show that both summer urban and sub-urban temperatures are projected to increase in the 10 most populous built-up areas in England between 1980 and 2080. However, differential warming rates in urban and sub-urban areas, and during day and at night suggest a trend towards a reduced daytime urban heat island effect but an enhanced night-time urban heat island effect. These changes in urban heat islands have implications on thermal comfort and local atmospheric circulations that impact the dispersion of air pollutants. I will further demonstrate that the opposite trends in daytime and night-time urban heat island effects are projected to emerge from current variability in more than half of the studied cities below a global mean warming of 3°C above pre-industrial levels.
How to cite: Lo, E., Mitchell, D., Bohnenstengel, S., Collins, M., Hawkins, E., Hegerl, G., Joshi, M., and Stott, P.: Emergence of opposite trends in daytime and night-time urban heat island intensities in England, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-5671, https://doi.org/10.5194/egusphere-egu2020-5671, 2020