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A Spatiotemporal Multiscale Analysis of Runoff and Erosion in a Mediterranean Marly Catchment

Runoff and erosion were continuously monitored for 7 yr at four nested spatial scales. A small number of runoff and erosive events were very important. There was a seasonal time lag between runoff and erosive response due to shrink–swell processes. Topsoil erosion processes and high hydro‐erosive connectivity were predominant. A simple linear model explained mean annual erosion rates between spatial scales.