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      An Evidence-Based Review of Impacts, Strategies and Tools to Mitigate Urban Heat Islands

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          Abstract

          The impacts of climate changes on cities, which are home to over half of the world’s population, are already being felt. In many cases, the intensive speed with which urban centres have been growing means that little attention has been paid to the role played by climatic factors in maintaining quality of life. Among the negative consequences of rapid city growth is the expansion of the problems posed by urban heat islands (UHIs), defined as areas in a city that are much warmer than other sites, especially in comparison with rural areas. This paper analyses the consistency of the UHI-related literature in three stages: first it outlines its characteristics and impacts in a wide variety of cities around the world, which poses pressures to public health in many different countries. Then it introduces strategies which may be employed in order to reduce its effects, and finally it analyses available tools to systematize the initial high level assessment of the phenomenon for multidisciplinary teams involved in the urban planning process. The analysis of literature on the characteristics, impacts, strategies and digital tools to assess on the UHI, reveals the wide variety of parameters, methods, tools and strategies analysed and suggested in the different studies, which does not always allow to compare or standardize the diagnosis or solutions.

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          Local Climate Zones for Urban Temperature Studies

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            Strong contributions of local background climate to urban heat islands.

            The urban heat island (UHI), a common phenomenon in which surface temperatures are higher in urban areas than in surrounding rural areas, represents one of the most significant human-induced changes to Earth's surface climate. Even though they are localized hotspots in the landscape, UHIs have a profound impact on the lives of urban residents, who comprise more than half of the world's population. A barrier to UHI mitigation is the lack of quantitative attribution of the various contributions to UHI intensity (expressed as the temperature difference between urban and rural areas, ΔT). A common perception is that reduction in evaporative cooling in urban land is the dominant driver of ΔT (ref. 5). Here we use a climate model to show that, for cities across North America, geographic variations in daytime ΔT are largely explained by variations in the efficiency with which urban and rural areas convect heat to the lower atmosphere. If urban areas are aerodynamically smoother than surrounding rural areas, urban heat dissipation is relatively less efficient and urban warming occurs (and vice versa). This convection effect depends on the local background climate, increasing daytime ΔT by 3.0 ± 0.3 kelvin (mean and standard error) in humid climates but decreasing ΔT by 1.5 ± 0.2 kelvin in dry climates. In the humid eastern United States, there is evidence of higher ΔT in drier years. These relationships imply that UHIs will exacerbate heatwave stress on human health in wet climates where high temperature effects are already compounded by high air humidity and in drier years when positive temperature anomalies may be reinforced by a precipitation-temperature feedback. Our results support albedo management as a viable means of reducing ΔT on large scales.
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              Synergistic Interactions between Urban Heat Islands and Heat Waves: The Impact in Cities Is Larger than the Sum of Its Parts*

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                Author and article information

                Journal
                Int J Environ Res Public Health
                Int J Environ Res Public Health
                ijerph
                International Journal of Environmental Research and Public Health
                MDPI
                1661-7827
                1660-4601
                19 December 2017
                December 2017
                : 14
                : 12
                : 1600
                Affiliations
                [1 ]HAW Hamburg, Faculty of Life Sciences, Research and Transfer Centre “Sustainable Development and Climate Change Management”, Ulmenliet 20, D-21033 Hamburg, Germany; walter.leal@ 123456haw-hamburg.de (W.L.F.); VictoriaOmeche.EMANCHE@ 123456haw-hamburg.de (V.O.E.)
                [2 ]School of Science and the Environment, Manchester Metropolitan University, Chester Street, Manchester M1 5GD, UK
                [3 ]Faculty of Architecture and the Built Environment, Delft University of Technology, Julianalaan 134, 2628 BL Delft, The Netherlands
                [4 ]Institute of Energy Policy and Research (IEPRe), Universiti Tenaga Nasional (UNITEN), 43000 Kajang, Malaysia; abulquasem@ 123456cust.edu.bd
                Author notes
                [* ]Correspondence: L.EchevarriaIcaza@ 123456tudelft.nl ; Tel.: +34-619-803-271
                Article
                ijerph-14-01600
                10.3390/ijerph14121600
                5751017
                29257100
                9cf31881-75cb-443e-8ba4-1a793f7a2b0e
                © 2017 by the authors.

                Licensee MDPI, Basel, Switzerland. This article is an open access article distributed under the terms and conditions of the Creative Commons Attribution (CC BY) license ( http://creativecommons.org/licenses/by/4.0/).

                History
                : 18 October 2017
                : 04 December 2017
                Categories
                Article

                Public health
                climate change,urban heat islands,cities-urban,health models
                Public health
                climate change, urban heat islands, cities-urban, health models

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