urban heat island
Introduction
The urban heat island effect[note 1] (abbreviated UHI) or simply heat island is the localized rise in temperature in urban environments with respect to the surrounding rural area.[1][2] [3].
It occurs in large cities and consists of the difficulty of heat dissipation during nighttime hours, when non-urban areas cool noticeably due to the lack of heat accumulation.[4] The urban center, where buildings and asphalt release the heat accumulated during the day at night, causes local winds from the outside to the inside. The phenomenon of temperature rise commonly occurs in densely built urban areas caused by a combination of factors[5] such as buildings, lack of green spaces, polluting gases or heat generation.[3] It has been observed that the heat island phenomenon increases with the size of the city and that it is directly proportional to the size of the urban area,[6] and that the sectors that store more heat can coincide with racial and class disparities.[7].
Causes
Built-up areas offer more surface area for the absorption of heat, which radiates slowly during the night.[8][9] Another effect of tall buildings is the multiple horizontal reflections of the received radiation, which increase the probability that this energy remains on the ground in what is known as the cannon effect.[10].
The lack of large green areas and the piping of aqueous tributaries in the city reduces the opportunities to transform solar energy through the processes of photosynthesis or evaporation "Evaporation (physical process)") of water.[5] Various studies show the direct relationship between high urban temperatures and the lack of vegetation.[11][12].
On the other hand, industrial and domestic activity generates a contribution of heat to the environment. In particular, cooling systems in the city are part of a vicious circle, since they generate extra heat and their use increases with temperature. Some authors explain the heat island as a local greenhouse effect, since the gases are locked in a single place, causing a capsule of gases that absorbs heat from the sun.[13] The materials that make up the city absorb short-wave solar radiation and subsequently emit it with a longer wavelength, a frequency that is retained by suspended particles and combustion gases.
The gas capsule can only be broken when the winds are higher than , if on the surface there are too many high-rise buildings the air will be obstructed and the capsule will not break, but nevertheless even the most natural thing can cause a heat capsule. Cities located in a valley surrounded by mountains are more prone to a heat island, as the air is obstructed by the surrounding mountains, making the capsule denser and thicker.