“…While it is well known that the relationship between rainfall, runoff, and sediment is highly nonlinear (de Vente & Poesen, ; de Vente et al, ; Nyssen et al, ; Parsons, Brazier, Wainwright, & Powell, ), it is expected that on this catchment scale (1 km 2 ), the net effect of increasing erosion processes, connectivity, and sediment storage will lead to increased sediment transport (de Vente & Poesen, ). The assumption that runoff and erosion can increase proportionally is supported by the experimental work of Hairsine and Rose () and the regional assessment in Gebremicael et al () as well as rating curve studies (Guzman et al, ; Moges et al, ; Vanmaercke et al, ), though seasonality and scale play a role. Above 10 km 2 , the effect of sediment sinks, and (re)deposition within the landscape often becomes more dominant than sediment sources resulting in gradually declining sediment yield for increasing area (de Vente & Poesen, ).…”