“…Rainfall temporal distribution influences runoff hydraulics and soil moisture: the former regulates flow erosivity while the latter before rainfall events influences both generation of runoff (Descroix et al, 2002;Castillo et al, 2003;Capra et al, 2012) and soil resistance to erosion (Bocco, 1991;Nachtergaele et al, 2002;Poesen et al, 2003;Torri et al, 2006;Bou Kheir et al, 2007;Magliulo, 2012;Torri et al, 2012b). Volume and velocity of concentrated flow are controlled by topographic attributes such as contributing drainage area, slope curvature and slope steepness (Moore et al, 1988;Vandekerckhove et al, 1998Vandekerckhove et al, , 2000aPoesen et al, 2003;Valentin et al, 2005;Zucca et al, 2006;Gómez Gutiérrez et al, 2009a, b;Kakembo et al, 2009;Nazari Samani et al, 2009;Capra et al, 2012;Svoray et al, 2012;Chaplot, 2013;Conoscenti et al, 2013). Depth and cross-sectional morphology of gullies are regulated by erodibility of soil horizons (Ireland et al, 1939;Imeson and Kwaad, 1980;Poesen et al, 2003) and characteristics of geological substrata (Vandekerckhove et al, 2000a;Zucca et al, 2006;Conoscenti et al, 2008;Conforti et al, 2010;Lucà et al, 2011;Marzolff et al, 2011;El Maaoui et al, 2012).…”