What Is the Urban Heat Island Effect?
An urban heat island (UHI) is a metropolitan area that is significantly warmer than its surrounding rural areas. The temperature difference is most pronounced at night, when cities can be 5-10°C warmer than the nearby countryside.
Why Cities Are Hotter
- Dark surfaces: Asphalt roads and tar roofs absorb solar radiation and re-radiate it as heat
- Reduced vegetation: Trees and grass cool air through evapotranspiration; concrete does not
- Waste heat: Cars, air conditioners, and industry all release heat
- Canyon effect: Tall buildings trap heat and block wind, reducing cooling
- Less evaporation: Impermeable surfaces prevent water from pooling and evaporating
The Numbers
| City | UHI Intensity (typical night) |
|---|---|
| Tokyo | +8-10°C |
| New York | +5-8°C |
| London | +4-7°C |
| Singapore | +4-7°C |
| Phoenix | +5-10°C |
Health Impact
UHIs amplify heat waves, increasing heat-related illness and death. The most vulnerable — elderly, children, outdoor workers, and people without air conditioning — are disproportionately affected.
Solutions Being Implemented
- Green roofs and walls: Vegetation cools buildings through shade and evapotranspiration
- Cool roofs: Light-coloured or reflective roofing materials
- Urban tree canopy: Shade from trees can reduce surface temperatures by 10-15°C
- Permeable paving: Allows water to soak in and evaporate, cooling the air
- Urban parks: Large green spaces act as cooling islands within the city
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