Cities, then, are warmer than the surrounding rural areas, and together they produce a phenomenon known as the urban heat island.
Heat islands develop best under particular conditions associated with light winds, but they can form almost any time. [■]The precise configuration of a heat island depends on several factors. [■]For example, the wind can make a heat island stretch in the direction it blows. [■]When a heat island is well developed, variations can be extreme; in winter, busy streets in cities can be 1.7℃ warmer than the side streets. [■]Areas near traffic lights can be similarly warmer than the areas between them because of the effect of cars standing in traffic instead of moving. The maximum differences in temperature between neighboring urban and rural environments is called the heat-island intensity for that region. In general, the larger the city, the greater its heat-island intensity. The actual level of intensity depends on such factors as the physical layout, population density, and productive activities of a metropolis.Another possibility is for the heat island to be stretched along the course of major rivers, since large waterways typically have a warming effect on the air directly above them..