“…The most used approach for investigating the role of urban trees on land surface temperature (LST) is based on multivariate spatial statistical models in which the normalized difference vegetation index (NDVI) is used as an explanatory variable (see Weng, Lu, & Schubring, 2004;Yuan & Bauer, 2007;Guo et al, 2015;Bonafoni, Anniballe, Gioli, & Toscano, 2016;;Zhao, Jensen, Weng, & Weaver, 2018). According to the literature, urban morphology also has an important role in shaping urban heat island phenomena; the relationship between LST and urban morphology has recently been analyzed using the Sky View Index (SVI) calculated based on 3D city models, which are derived from LiDAR data (Kokalj, Zakšek, & Oštir, 2011;Chun & Guldman, 2014;Tan, Lau, & Ng, 2016;Nakata-Osaki, Souza, & Rodrigues, 2018). Mirzaei (2015, p. 204) in a review of UHI assessment methods at different scales, concludes that "despite the ability of mesoscale models to investigate the large-scale effect of the UHI, their accuracy is not efficient to provide details on the urban canopy layer and this gap therefore will require further research to develop spatially and computationally efficient models."…”