
The term "heat island" refers to urban air and surface temperatures that are higher than nearby rural areas. Many U.S. cities and suburbs have air temperatures up to 10°F warmer than the surrounding natural land cover.
Heat islands form as cities replace natural land cover with pavement, buildings, and other infrastructure. These changes contribute to higher urban temperatures in a number of ways:
- Displacing trees and vegetation minimizes the natural cooling effects of shading and evaporation of water from soil and leaves.
- Tall buildings and narrow streets can heat air trapped between them and reduce air flow.
- Waste heat from vehicles, factories, and air conditioners may add warmth to their surroundings, further exacerbating the heat island effect.
SS Credit 7.1: Heat Island Effect – Non-Roof
SS Credit 7.2: Heat Island Effect - Roof
