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Scaling and elevation in river networks

Tarboton, David G., Bras, Rafael L., Rodriguez‐Iturbe, Ignacio·1989·Water Resources Research

Abstract

The analysis of large river networks obtained from digital elevation models has given insight into the variation of channel slope with scale. Investigators have recently suggested that channel slopes are self‐similar with magnitude or area as a scaling parameter. Our data indicates otherwise; in particular, the variance of channel slope is larger than that predicted by simple self‐similarity. This suggests multiscaling. The scaling exponent for the standard deviation is approximately half the corresponding exponent in the relationship of the slope mean to magnitude or area. A model for channel slopes based on a point process of elevation drops along the channel is presented. The model reproduces observed multiscaling properties when the density of elevation increments is related to area (or magnitude) as A−θ.

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Metadata

Authors
Tarboton, D. G., Bras, R. L., & Rodriguez‐Iturbe, I.
Venue
Water Resources Research
Published
1989-09
Volume
25
Issue
9
Pages
2037-2051
ISSN
  • 0043-1397 (ISSN-L)
  • 1944-7973
OpenAlex
W2095152033
Cited by
223
References
0
FWCI
9.40
Type
journal article
Language
en
Open access
closed

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CoChat. (2026). Citation check: Scaling and elevation in river networks. https://app.cochat.ai/papers/10.1029/wr025i009p02037
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Tarboton, D. G., Bras, R. L., & Rodriguez‐Iturbe, I. (1989). Scaling and elevation in river networks. Water Resources Research. https://doi.org/10.1029/wr025i009p02037

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