“…This flow, often organized in a convergence line, is then forced to rise due to the steep orography, thus triggering or reinforcing convection and generating, usually, prefrontal orographic precipitation and enhancing frontal precipitation (e.g., Kozari ć and Ivančan-Picek, 2006;Ivančan-Picek et al, 2014;Davolio et al, 2016). The HPEs observed during the first Hydrological cycle in the Mediterranean Experiment (HyMeX; Ducrocq et al, 2014) Special Observation Period (SOP1) developed under similar conditions (Ivančan-Picek et al, 2016). During the SOP1, the northern Adriatic was one of the most affected areas, with more than 1,000 mm of precipitation recorded at several stations.…”