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High resolution (100m) hourly temperature (2008-2017) was simulated with the urban climate model UrbClim (De Ridder et al., 2015). Summer season is June, July and August. The intensity of UHI is represented by spatial P90 (90th percentile) UHI intensity of a given city. This indicator is calculated by subtracting the rural (non-water) spatial P10 (10th percentile) temperature value from the average, height-corrected (to exclude terrain effects), air temperature map.
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References:
De Ridder, K, Lauwaet D. and Maiheu, B. (2015): UrbClim &#8211; A fast urban boundary layer climate model, Urban Climate, Vol. 12, pp. 21&#8211;48. https://doi.org/10.1016/j.uclim.2015.01.001.
Dosio, A. (2016), Projections of climate change indices of temperature and precipitation from an ensemble of bias-adjusted high-resolution EURO-CORDEX regional climate models, J. Geophys. Res. Atmos., 121, 5488&#8211;5511, doi:10.1002/2015JD024411.</gco:CharacterString>
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