🏙️ Urban Heat Island

ΔT (UHI intensity)—
Urban T—
Rural T—
Urban albedo α—
Rural albedo α—
Net radiation Q*—
Energy Balance
Q* = K↓(1−α) + L↓ − L↑ − QH − QE

Cities absorb more solar radiation due to lower albedo (α=0.1–0.2 vs rural 0.3–0.4) and release stored heat at night, creating a warm island.