Depressional runoff cascade networks of the Des Moines Lobe of Iowa

Abstract

Runoff generation within and from watersheds has long been thought to occur continuously and seamlessly across spatial and temporal scales in response to precipitation events. However, results from recent field and modeling studies challenge this traditional viewpoint (see McDonnell et al., 2021; Spence, 2010 and references therein). Instead, it has been proposed that watershed runoff generation across spatial