“…Their complex geomorphology comprises three branches (Western, Central, and Eastern) separated by two major long intra‐Andean valleys drained by the Magdalena and Cauca rivers (Figure 2a). Research directly or indirectly related to the hydroclimate of this region includes studies of variability at diurnal time‐scales (Bedoya‐Soto, Aristizábal, et al., 2019; Poveda et al., 2005), annual time and seasonal time‐scales (Alvarez‐Villa et al., 2011; Poveda, 2004; Urrea et al., 2019; Vallejo‐Bernal et al., 2021); interannual time‐scales (Bedoya‐Soto, Poveda, et al., 2019; Córdoba‐Machado et al., 2015a, 2015b; Posada‐Marín et al., 2018; Poveda and Mesa, 1997, 2000; Poveda et al., 2001, 2006, 2011, 2020); activity of low level‐jets and moisture sources (Arias et al., 2015; Builes‐Jaramillo et al., 2022; Durán‐Quesada et al., 2012; Hoyos et al., 2018, 2019; Jiménez‐Sánchez et al., 2019; Morales et al., 2021; Poveda et al., 2014; Poveda & Mesa, 2000; Yepes et al., 2019); activity of mesoscale convective systems (Jaramillo et al., 2017; Poveda et al., 2020; Sakamoto et al., 2011; Zuluaga & Houze, 2015); and climate change (Carmona & Poveda, 2014; Mesa et al., 2021; Pabón‐Caicedo et al., 2020; Sierra et al., 2015, 2021); among others.…”