Urban climate is defined as peculiar conditions in a city which develop according to urbanization. The purpose of urban climatology is to make clear of structure and mechanism of urban climate, and predict the future change caused by the development of urbanization. Urban climate is usually expressed as differences of climatic elements between urban and rural. Among the urban climate phenomena, heat island is the most closely related to the living environment of our ordinal life. Due to the increasing energy consumption, heat island appears not only during the nighttime but also during the daytime of summer, which is called as thermal pollution type. One feature of heat island is the dense isothermal lines in suburban areas, which is called cliff, and another is the comparatively sparse lines in the central urban area, which is called plateau. However, some secondary heat island is forming inside a big city like Tokyo. On the other hand, the parks and the green areas are existing in the urban area to form a cool island which is called heat sink. As a whole a large heat island come into being at a big city. For example a huge heat island of about 40 km diameter appears in Tokyo. It is very important to make clear of relationships between the different scales of heat island from the phenomena inside the canopy layer to those remotesensed by Landsat. There is discussion on the merit of heat island which means that a huge city can save total energy consumption of the whole earth because of the concentration of human activity on a city. However, this idea is very questionable. Further, cities should be planned introducing amenity based on ecological systems.
View full abstract