“…The vertical profile of rain is assumed to be constant up to the rain height as suggested by Recommendation ITU-R P.839-4 (ITU-R P.839-4, 2013). Simulations were carried out from 5°, here assumed as the minimum operational elevation, to 90°, by applying the integration in Equation 7 at all the virtual ground stations set in each pixel of the rain maps (Tomaz et al, 2017): indeed, this approach allows increasing the number of samples and consequently achieving the required statistical stability of the results. Two meteorologically different sites were considered: Spino d'Adda, Italy (45.4°N, 9.5°E), in the temperate region, and Miami, USA (25.5°N, 80.3°W), in the tropical region.…”