Urban heat island

What is an Urban heat island?

The urban heat island effect describes higher near-surface air temperatures in urban areas compared to surrounding rural areas, primarily caused by reduced vegetation, usage of heat-absorbing materials, and man-caused heat.

An urban heat island is a phenomenon where cities experience significantly higher temperatures than the rural areas around them. This occurs because urban environments are built with materials that absorb and retain heat, have fewer natural cooling elements like vegetation and water bodies, and generate extra heat from human activities.

The urban heat island effect can lead to increased energy consumption, poor air quality, and health risks associated with heat, making it an important issue for urban planning and sustainability.

The role of materials in urban heat retention

The materials used in urban environments play a key role in how much heat is retained and for how long. Surfaces like asphalt, concrete, and brick absorb significant amounts of solar radiation during the day and release it slowly at night. In contrast, natural surfaces such as soil, vegetation, and water bodies reflect more sunlight and retain less heat.

  • Asphalt and concrete: These materials are dark and dense, absorbing up to 80 to 95 percent of incoming solar radiation. Their slow heat release at night keeps cities significantly warmer than surrounding rural areas.
  • Brick and stone: Older buildings, especially those made from brick or stone, store heat, contributing to urban heat island effects, particularly in historic districts.
  • Glass and steel: Reflective glass can reduce some heat absorption, but urban canyons formed by tall buildings can trap heat, reducing airflow and raising local temperatures.
  • Green spaces and water bodies: Vegetation and water help cool their surroundings through evapotranspiration, releasing moisture into the air, which lowers temperatures. Well-vegetated areas, such as parks, are often several degrees cooler than nearby built-up spaces.

Urban versus rural temperature differences

The temperature difference between urban and rural areas can be significant, especially at night when rural areas cool down much faster. On average, urban areas can be 2 to 7 degrees Celsius warmer than rural areas, with extreme cases exceeding 10 degrees Celsius. The variation depends on factors such as urban density, material composition, and local climate.

  • Daytime: Urban and rural areas may experience similar temperatures under direct sunlight.
  • Nighttime: Rural areas cool rapidly due to greater exposure to the sky and lower heat retention, while cities release stored heat more slowly, keeping temperatures elevated.
  • Seasonal variation: The urban heat island effect is often more pronounced in summer, due to increased solar radiation and reduced nighttime cooling, but it can also influence winter temperatures by reducing frost and snowfall in urban centers.

How city size affects the urban heat island effect

The intensity of the urban heat island effect tends to increase with city size. Larger cities, with denser infrastructure and fewer green spaces, experience stronger heat retention compared to smaller towns or suburban areas.

  • Small cities (fewer than 100,000 people):
    • Urban heat island effects are moderate, with urban areas typically being 1 to 3 degrees Celsius warmer than rural surroundings.
    • Green spaces and lower building density help reduce temperature differences.
  • Medium cities (100,000 to 1 million people):
    • Urban heat island effects become more pronounced, with urban centers being 3 to 6 degrees Celsius warmer than rural areas.
    • Higher building density and reduced airflow contribute to longer heat retention.
  • Mega cities (more than 10 million people):
    • The urban heat island effect can exceed 7 to 10 degrees Celsius due to extreme urban density, traffic congestion, industrial activity, and limited vegetation.
    • Heat stress in these environments can be significant, leading to higher energy demands for air conditioning and exacerbating health risks.

Mitigating urban heat islands through better design

The urban heat island effect is a complex phenomenon influenced by material choices, city size, and land use patterns. While smaller cities experience milder temperature differences, larger cities with dense infrastructure tend to see significant heat retention, often exceeding 7 degrees Celsius above surrounding rural areas. 

Sustainable urban planning—such as increasing green spaces, using reflective materials, and optimizing city layouts—can help mitigate these effects and create more livable environments.

Published:

April 9, 2025

Alternate names:

Urban Heat Island Effect

UHI

Heat Island Effect

Urban Heat Effect

Metropolitan Heat Island

Heat Island Phenomenon