2012
DOI: 10.1016/j.rse.2012.08.025
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Satellite air temperature estimation for monitoring the canopy layer heat island of Milan

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Cited by 93 publications
(60 citation statements)
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References 41 publications
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“…Zakšek et al [29] set up a parameterization for Central Europe based on SEVIRI that resulted into a Rho of 0.95 and a RMSE of 2.0 °C. Pichierri et al [24] used a split window approach to directly estimate canopy layer air temperatures for Milan (Italy) from the Moderate Resolution Imaging Spectroradiometer (MODIS) BTs, which yielded a RMSE of 1.8 °C for daytime data from May to September. Bechtel et al [20] proposed a new approach based on multi-temporal geostationary LST data resulted in a RMSE of 1.8 °C, but they are valid only for six stations in Hamburg, Germany.…”
Section: Discussionmentioning
confidence: 99%
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“…Zakšek et al [29] set up a parameterization for Central Europe based on SEVIRI that resulted into a Rho of 0.95 and a RMSE of 2.0 °C. Pichierri et al [24] used a split window approach to directly estimate canopy layer air temperatures for Milan (Italy) from the Moderate Resolution Imaging Spectroradiometer (MODIS) BTs, which yielded a RMSE of 1.8 °C for daytime data from May to September. Bechtel et al [20] proposed a new approach based on multi-temporal geostationary LST data resulted in a RMSE of 1.8 °C, but they are valid only for six stations in Hamburg, Germany.…”
Section: Discussionmentioning
confidence: 99%
“…Between the canopy UHI and surface UHI, the former is a more suitable concept because TA regulates many surface processes and is the driving force of heat transfer between the human body and the surrounding air [22,23]. However, TA data are usually retrieved from irregularly-spaced meteorological stations (point measurements) and, hence, cannot provide a spatially-continuous and simultaneous view of the whole city [24].…”
Section: Introductionmentioning
confidence: 99%
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“…Milan is an important Italian city, as well as the second most populous city in Italy. The UHI in Milan was diagnosed in the 1990s [17,18] using urban and airport temperature series, that showed an average difference between the city center and Linate airport close to 1.4 • C. The UHI in Milan was analyzed also using satellite maps [19,20], and surface and canopy layer heat islands were distinguished; the surface UHI effect was found to be a noticeable phenomenon throughout the whole diurnal cycle, while the canopy layer UHI emerged after sunset and was absent during the daytime. Regarding the application of UHI mitigation strategies in Milan, the authors of [21] addressed the issue in terms of urban design options (e.g., the partitioning of trees, grass, asphalt and buildings), highlighting the importance of the increased size of soil water reservoirs to enhance the mitigating effect of urban vegetation.…”
Section: Introductionmentioning
confidence: 99%
“…The UHI typologies may be grouped in three categories [2]: the surface urban heat island (SUHI); the boundary layer heat island, and; the canopy layer heat island. The canopy layer UHI is affected by the air temperature heating in the atmosphere extending up to the top of buildings, while the boundary layer UHI extends up to 1 km [5]. The SUHI concerns the land surface temperature (LST) pattern, having greater variability and higher thermal peaks with respect to the air temperature.…”
Section: Introductionmentioning
confidence: 99%