Abstract

Although Urban Heat Island (UHI) is a fundamental effect modifying the urban climate, being widely studied, the relative weight of the parameters involved in its generation is still not clear. This paper investigates the hierarchy of importance of eight parameters responsible for UHI intensity in the Mediterranean context. Sensitivity analyses have been carried out using the Urban Weather Generator model, considering the range of variability of: 1) city radius, 2) urban morphology, 3) tree coverage, 4) anthropogenic heat from vehicles, 5) building’s cooling set point, 6) heat released to canyon from HVAC systems, 7) wall construction properties and 8) albedo of vertical and horizontal surfaces. Results show a clear hierarchy of significance among the considered parameters; the urban morphology is the most important variable, causing a relative change up to 120% of the annual average UHI intensity in the Mediterranean context. The impact of anthropogenic sources of heat such as cooling systems and vehicles is also significant. These results suggest that urban morphology parameters can be used as descriptors of the climatic performance of different urban areas, easing the work of urban planners and designers in understanding a complex physical phenomenon, such as the UHI.

Highlights

  • Urban Heat Island (UHI), is one of the most profound climatic modification linked to urbanization, being reported and theorized since the seminal studies of Oke during the 80’s [1]

  • Results show a clear hierarchy of significance among the considered parameters; the urban morphology is the most important variable, causing a relative change up to 120% of the annual average UHI intensity in the Mediterranean context

  • Impact of the single parameters on the UHI intensity The variation of the monthly average UHI intensity according to the tested values for each of the eight parameters is reported in figure 3

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Summary

Introduction

Urban Heat Island (UHI), is one of the most profound climatic modification linked to urbanization, being reported and theorized since the seminal studies of Oke during the 80’s [1]. Regardless the relevant advances in the understanding of urban climate, the relative weight of urban variables such as impervious materials, urban form, anthropogenic heat sources and the like contributing to the general UHI effect remains unclear, needing more empirical research. This shortcoming constrains the development of predictive studies with lower levels of uncertainty.

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