Human-biometeorological assessment of the urban heat island in a city with complex topography – The case of Stuttgart, Germany

Abstract

The spatial and temporal differences of climate, urban heat island and future conditions were assessed for Stuttgart, a city located in complex topography in Southwest Germany. The present and future urban climate conditions were analysed using hourly measured data from 2000 to 2011 of 5 measuring stations and data from regional climate simulations. The urban heat island intensity was quantified applying thermal indices as Physiologically Equivalent Temperature (PET) and Universal Thermal Climate Index (UTCI) and compared to weather type classifications. In Stuttgart, wind speed was mostly less than 3ms−1, the wind roses were very inconsistent and local wind could be clearly observed. The average annual urban heat island of air temperature was between 0.3K in the suburb areas to 2K in the city centre and the maximum up to 12K. The assessed urban heat island with PET was in average 3.3K and maximum around 20K. Based on regional climate simulation we found that the amount of days with heat stress (PET⩾35°C) is estimated to increase by about 17days until the end of the 21st century. Urban heat island and intra-urban variability were most obvious using thermal indices rather than air temperature.