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
- Enter city population, impervious surface (%), and tree canopy/green space (%).
- Set urban and rural albedo values, solar radiation (W/m²), wind speed (m/s), and anthropogenic heat (W/m²).
- Review UHI Intensity (°C), Nighttime UHI (°C), and cooling potential from interventions.
- 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) |
|---|---|
| 2.45 | 4.45 |
| 7.32 | 2.9 |
| 13 | 2.06 |
| 18 | 1.65 |
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
- Identify Input Parameters4 parametersCity population = 500000, Impervious surface (%) = 60, Tree canopy / green space (%) = 15, Urban albedo (0-1) = 0.15 = 8 input(s) provided
- Calculate UHI intensityUHI intensity4.2 = 4.2
- Calculate Nighttime UHINighttime UHI = uhiIntensity * 1.77.14 = 7.14
- Calculate Summer peak UHISummer peak UHI = uhiIntensity * 1.87.56 = 7.56
Related Calculators
The questions that sit next to this one — chosen by subject, including calculators filed under a different category.
Climate Science
Carbon Footprint Calculator
Personal annual CO2 from transport, home, food, and goods.
Climate ScienceEmission Reduction Calculator
CO2 savings from specific lifestyle changes.
Urban PlanningUrban Growth Boundary Calculator
Analyze urban growth boundary capacity from population projections, vacant land inventory, and target density to determine expansion needs.
Climate ScienceClimate Model Interpreter Calculator
Temperature and radiative forcing from greenhouse gas concentrations using Myhre et al. formulas.
More in Environment, Weather & Climate.