“…In this context, ground-based microwave radiometers (MWR) are exploited for their ability to sense the atmospheric thermodynamic features of a satellite channel [Tanner and Riley, 2003;Ware at al., 2003;Crewell et al, 2009]. Based on brightness temperature values T b (f), measured by a MWR at 20/30 GHz band, the authors developed a scalar indicator, the Sky Status Indicator (SSI), that can help in discriminating among clear, cloudy and rainy sky conditions [Bosisio and Capsoni, 1995;Bosisio et al, 2012]. A dataset of T b (f) values, collected in Cabauw (NL) by the ESA ATPROP System [Rose, 2008] along zenithal (θ=90°) and slant path (at θ=69.6°), was used to compute the SSI as the ratio of T b (f) values at 31.4 and 23.8 GHz, properly modified to subtract the contribution of the gaseous dry emission (mainly due to O 2 ) of the Earth atmosphere [Bosisio et al, 2012].…”