Heat waves and urban heat islands in Europe: A review of relevant drivers

Kathrin Ward; Steffen Lauf; Birgit Kleinschmit; Wilfried Endlicher

doi:10.1016/j.scitotenv.2016.06.119

Heat waves and urban heat islands in Europe: A review of relevant drivers

Sci Total Environ. 2016 Nov 1:569-570:527-539. doi: 10.1016/j.scitotenv.2016.06.119. Epub 2016 Jun 28.

Authors

Kathrin Ward¹, Steffen Lauf², Birgit Kleinschmit³, Wilfried Endlicher¹

Affiliations

¹ Humboldt Universität zu Berlin, Department of Geography, Climatological Section, Berlin, Germany.
² Technische Universität Berlin, Department of Landscape Architecture and Environmental Planning, Geoinformation in Environmental Planning Lab, Berlin, Germany. Electronic address: steffen.lauf@tu-berlin.de.
³ Technische Universität Berlin, Department of Landscape Architecture and Environmental Planning, Geoinformation in Environmental Planning Lab, Berlin, Germany.

PMID: 27366983
DOI: 10.1016/j.scitotenv.2016.06.119

Abstract

The climate change and the proceeding urbanization create future health challenges. Consequently, more people around the globe will be impaired by extreme weather events, such as heat waves. This study investigates the causes for the emergence of surface urban heat islands and its change during heat waves in 70 European cities. A newly created climate class indicator, a set of meaningful landscape metrics, and two population-related parameters were applied to describe the Surface Urban Heat Island Magnitude (SUHIM) - the mean temperature increase within the urban heat island compared to its surrounding, as well as the Heat Magnitude (HM) - the extra heat load added to the average summer SUHIM during heat waves. We evaluated the relevance of varying urban parameters within linear models. The exemplary European-wide heat wave in July 2006 was chosen and compared to the average summer conditions using MODIS land surface temperature with an improved spatial resolution of 250m. The results revealed that the initial size of the urban heat island had significant influence on SUHIM. For the explanation of HM the size of the heat island, the regional climate and the share of central urban green spaces showed to be critical. Interestingly, cities of cooler climates and cities with higher shares of urban green spaces were more affected by additional heat during heat waves. Accordingly, cooler northern European cities seem to be more vulnerable to heat waves, whereas southern European cities appear to be better adapted. Within the ascertained population and climate clusters more detailed explanations were found. Our findings improve the understanding of the urban heat island effect across European cities and its behavior under heat waves. Also, they provide some indications for urban planners on case-specific adaptation strategies to adverse urban heat caused by heat waves.

Keywords: Climate class indicator; Heat waves; Landscape metrics; Modis; Surface Urban Heat Island Magnitude; Urban green.