The urban metropolitan area of Turin (Italy) was studied to characterize its seasonal thermal and moisture behaviour with respect to the rural surroundings. The area exhibits a complex topography and a set of ground level stations was selected in the urban and rural environment for a period of 14 years (2007-2020). The Urban Heat Island (UHI) effect clearly emerges from the analysis, with the largest values, up to 4-5 degrees C on average, occurring during the night. Also a light Urban Cool Island (UCI) effect, between 0.5 degrees C and 1 degrees C, occurs in some conditions. An Urban Dry Island (UDI) effect during daytime up to 3-4 g/m3 was identified by the analysis of absolute humidity. Moreover, the interaction between UHI, UDI and wind intensity showed that the urban-rural differences are swept up when wind velocity is higher than approximate to 4 m/s. The availability of temperature data measured by three radiometers, one in the city center and two in the rural area (north and south of Turin) between 2007-2020, allowed the investigation of the city boundary layer. The vertical limit of UHI was found at 150-200 m above the ground level, surmounted in some cases by a very weak cross-over or cold lens effect.
Characterization of the Urban Heat and Dry Island effects in the Turin metropolitan area / Milelli, M; Bassani, F; Garbero, V; Poggi, Davide; von Hardenberg, J; Ridolfi, Luca. - In: URBAN CLIMATE. - ISSN 2212-0955. - 47:(2023), p. 101397. [10.1016/j.uclim.2022.101397]
Characterization of the Urban Heat and Dry Island effects in the Turin metropolitan area
Bassani, F;Garbero, V;Poggi, Davide;von Hardenberg, J;Ridolfi, Luca
2023
Abstract
The urban metropolitan area of Turin (Italy) was studied to characterize its seasonal thermal and moisture behaviour with respect to the rural surroundings. The area exhibits a complex topography and a set of ground level stations was selected in the urban and rural environment for a period of 14 years (2007-2020). The Urban Heat Island (UHI) effect clearly emerges from the analysis, with the largest values, up to 4-5 degrees C on average, occurring during the night. Also a light Urban Cool Island (UCI) effect, between 0.5 degrees C and 1 degrees C, occurs in some conditions. An Urban Dry Island (UDI) effect during daytime up to 3-4 g/m3 was identified by the analysis of absolute humidity. Moreover, the interaction between UHI, UDI and wind intensity showed that the urban-rural differences are swept up when wind velocity is higher than approximate to 4 m/s. The availability of temperature data measured by three radiometers, one in the city center and two in the rural area (north and south of Turin) between 2007-2020, allowed the investigation of the city boundary layer. The vertical limit of UHI was found at 150-200 m above the ground level, surmounted in some cases by a very weak cross-over or cold lens effect.File | Dimensione | Formato | |
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https://hdl.handle.net/11583/2979853