“…Various work at different scales and in different geographic settings focussed on connectivity within the hillslope–riparian–stream (HRS) system in low‐gradient (Jackson et al ., ; Klaus et al ., ) and steep (McGlynn and McDonnell, ; Detty and McGuire, ) environments and its spatial patterns (Jencso et al ., ; Jencso and McGlynn, ). Hydrological connectivity can be strongly non‐linear and controls streamflow response (Zehe et al ., ; Detty and McGuire, ; Gannon et al ., ; Tetzlaff et al ., ) and stream chemistry (Burt and Pinay, ), preferential flow and solute transport (Alletto et al, ; Klaus and Zehe , ; Klaus et al ., ). Eventually, it is a hydrologic process that is relevant from hillslopes (Lehmann et al ., ; Jackson et al ., ), over headwaters (Jencso et al ., , ), to landscapes (Tetzlaff et al ., ).…”