Skip to main page content
Access keys NCBI Homepage MyNCBI Homepage Main Content Main Navigation
Filters applied. Clear all
. 2014 Jul 10;511(7508):216-9.
doi: 10.1038/nature13462.

Strong Contributions of Local Background Climate to Urban Heat Islands

Affiliations

Strong Contributions of Local Background Climate to Urban Heat Islands

Lei Zhao et al. Nature. .

Abstract

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.

Comment in

  • Climate science: City heat.
    Mitchinson A. Mitchinson A. Nature. 2014 Jul 10;511(7508):163. doi: 10.1038/511163a. Nature. 2014. PMID: 25008518 No abstract available.

Similar articles

See all similar articles

Cited by 44 articles

See all "Cited by" articles

References

    1. Nature. 2011 Nov 16;479(7373):384-7 - PubMed
    1. Environ Sci Technol. 2012 Jan 17;46(2):696-703 - PubMed
    1. Nature. 2003 May 29;423(6939):528-31 - PubMed
    1. Nature. 2004 Jan 22;427(6972):332-6 - PubMed
    1. Proc Natl Acad Sci U S A. 2012 Sep 11;109(37):E2415-23 - PubMed

Publication types

LinkOut - more resources

Feedback