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Intra‐urban differences in canopy layer air temperature at a mid‐latitude city
156
Citations
37
References
2006
Year
Mid‐latitude CityEngineeringIntra‐urban DifferencesUrban Climate ImpactUrban Heat IslandAir TemperatureUrban WeatherEarth ScienceSocial SciencesAtmospheric ScienceUrban Canopy ModelingMicrometeorologyUrban MeteorologyUrban ClimatologyUrban CanopyClimate ChangeMeteorologyGeographyCentral AdelaideUrban Heat MitigationClimate DynamicsClimatologyAtmospheric ConditionSurface AreaAir PollutionUrban Climate
The study measured meteorological variables for nearly a year in two Adelaide street canyons and reference sites, attributing observed temperature differences to increased surface area and thermal mass that dampen diurnal ranges and delay daytime cool island peaks. Measurements show significant temperature differences between Adelaide street canyons and reference sites, including a nocturnal urban heat island and a weaker daytime cool island, with additional thermal mass dampening diurnal ranges and delaying peak temperatures, and differing daily temperature progression between canyon orientations. © 2006 Royal Meteorological Society.
Abstract Detailed meteorological measurements were carried out in two urban street canyons in central Adelaide and at two reference sites in a suburban location and at an exposed site near the middle of the city for an extended period of nearly a year. The meteorological records revealed substantial differences between air temperature in the urban street canyons and both reference sites. The nocturnal urban heat island observed in most cities was noted in Adelaide street canyons, too. However, the frequent occurrence of a daytime cool island during summer, albeit much weaker than the night‐time phenomenon, is less expected. Both phenomena are attributed at least in part to the increase in surface area participating in energy exchanges with the atmosphere in an urban street canyon compared to a typical rural site, and hence in an increase in the effective thermal mass. The presence of additional thermal mass is manifested not only in the dampening of the diurnal temperature range in the city, but also in a noticeable time lag in the maximum intensity of the daytime cool island. The measurements also demonstrate an observable difference in the daily progression of air temperature between a north–south street canyon and an adjacent east–west oriented street. Copyright © 2006 Royal Meteorological Society
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