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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Published in | Water resources research Vol. 30; no. 2 |
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Main Author | |
Format | Journal Article |
Language | English |
Published |
01.02.1994
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Subjects | |
Online Access | Get more information |
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