An integral approach to bedrock river profile analysis

ABSTRACT Bedrock river profiles are often interpreted with the aid of slope–area analysis, but noisy topographic data make such interpretations challenging. We present an alternative approach based on an integration of the steady‐state form of the stream power equation. The main component of this ap...

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Bibliographic Details
Published inEarth surface processes and landforms Vol. 38; no. 6; pp. 570 - 576
Main Authors Perron, J. Taylor, Royden, Leigh
Format Journal Article
LanguageEnglish
Published Chichester Blackwell Publishing Ltd 01.05.2013
Wiley
Wiley Subscription Services, Inc
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Summary:ABSTRACT Bedrock river profiles are often interpreted with the aid of slope–area analysis, but noisy topographic data make such interpretations challenging. We present an alternative approach based on an integration of the steady‐state form of the stream power equation. The main component of this approach is a transformation of the horizontal coordinate that converts a steady‐state river profile into a straight line with a slope that is simply related to the ratio of the uplift rate to the erodibility. The transformed profiles, called chi plots, have other useful properties, including co‐linearity of steady‐state tributaries with their main stem and the ease of identifying transient erosional signals. We illustrate these applications with analyses of river profiles extracted from digital topographic datasets. Copyright © 2012 John Wiley & Sons, Ltd.
Bibliography:istex:674388363BAC89BD9509CC3C2AAA42AF910226B9
ark:/67375/WNG-XW9SKP15-5
ArticleID:ESP3302
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SourceType-Scholarly Journals-1
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ISSN:0197-9337
1096-9837
DOI:10.1002/esp.3302