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Chiara Corbari and Marco Mancini

aerodynamic resistance in the turbulent fluxes estimate. So, following the proposed approach, LST can be seen as a proxy of soil moisture and, thus, is a key variable in the fluxes estimates ( Anderson et al. 2012 ). The runoff routing throughout the hillslope and the river network is performed via a diffusion wave scheme based on the Muskingum–Cunge method in its nonlinear form with the time variable celerity. Details are given by Montaldo et al. (2007) . Runoff is computed according to a modified Soil

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