A physical explanation for an observed area-slope-elevation relationship for catchments with declining relief

A general relationship between the contributing area, slope, and mean elevation of catchments with relief declining after a tectonic uplift event is presented. This relationship is based on the continuity equation for runoff and erosion processes in the catchment. The key hypothesis underlying this...

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Bibliographic Details
Published inWater resources research Vol. 30; no. 2
Main Author Willgoose, G
Format Journal Article
LanguageEnglish
Published 01.02.1994
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