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Calcimator

Urban Heat Island Calculator

Temperature differential from land cover and albedo.

Inputs

%
%

Results

UHI intensity (°C)

4.2

Nighttime UHI (°C)7.14
Summer peak UHI (°C)7.56
Cooling energy increase (%)29.4%
Albedo heating (°C)0.2
Greenspace cooling (°C)0.6
Wind dispersal factor0.69
Cool roof mitigation (°C)0.28
How to Use This Calculator
  1. Enter city population, impervious surface (%), and tree canopy/green space (%).
  2. Set urban and rural albedo values, solar radiation (W/m²), wind speed (m/s), and anthropogenic heat (W/m²).
  3. Review UHI Intensity (°C), Nighttime UHI (°C), and cooling potential from interventions.
  4. Each 10% increase in green space typically reduces UHI intensity by 0.3–0.5°C.

How the result changes with Wind speed (m/s)

Wind speed (m/s)UHI intensity (°C)
2.454.45
7.322.9
132.06
181.65

What each input means

City population
City population — larger cities have stronger UHI effect (Oke 1973).
Impervious surface (%)
Percentage of land covered by pavement, buildings, and other impervious surfaces.
Tree canopy / green space (%)
Percentage of land with tree canopy or vegetated green space.
Urban albedo (0-1)
Surface reflectivity: dark asphalt ~0.10, concrete ~0.20, cool roofs ~0.35.
Rural albedo (0-1)
Surrounding rural albedo: grassland ~0.25, forest ~0.15, desert ~0.35.
Solar radiation (W/m²)
Mean daily incoming solar radiation. ~150 temperate, ~250 tropical.
Wind speed (m/s)
Average wind speed — higher winds disperse the heat island.
Anthropogenic heat (W/m²)
Waste heat from buildings, vehicles, industry. Typical: 10-50 W/m².

What each result means

UHI intensity (°C)
Average urban-rural temperature differential.
Nighttime UHI (°C)
Nighttime UHI is typically 1.5-2× daytime due to thermal mass release.
Summer peak UHI (°C)
Peak summer UHI intensity.
Cooling energy increase (%)
Estimated increase in cooling energy demand from UHI.
Albedo heating (°C)
Temperature contribution from urban-rural albedo difference.
Greenspace cooling (°C)
Cooling provided by vegetation and evapotranspiration.
Wind dispersal factor
Wind speed reduction factor on UHI (1.0 = calm, lower = more dispersal).
Cool roof mitigation (°C)
Potential UHI reduction if urban albedo increased to 0.35 (cool roofs).

How this is calculated

Worked example, using the default values

  1. Identify Input Parameters
    4 parameters
    City population = 500000, Impervious surface (%) = 60, Tree canopy / green space (%) = 15, Urban albedo (0-1) = 0.15 = 8 input(s) provided
  2. Calculate UHI intensity
    UHI intensity
    4.2 = 4.2
  3. Calculate Nighttime UHI
    Nighttime UHI = uhiIntensity * 1.7
    7.14 = 7.14
  4. Calculate Summer peak UHI
    Summer peak UHI = uhiIntensity * 1.8
    7.56 = 7.56

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