Articles | Volume 13, issue 5
https://doi.org/10.5194/esurf-13-1059-2025
https://doi.org/10.5194/esurf-13-1059-2025
Research article
 | 
22 Oct 2025
Research article |  | 22 Oct 2025

Influence of network geometry on long-term morphodynamics of alluvial rivers

Fergus McNab, Taylor F. Schildgen, Jens M. Turowski, and Andrew D. Wickert

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Cited articles

Abrahams, A. A.: Channel networks: A geomorphological perspective, Water Resources Research, 20, 161–168, https://doi.org/10.1029/WR020i002p00161, 1984. a, b, c
Allen, P. A.: From landscapes into geological history, Nature, 430, 274–276, https://doi.org/10.1038/nature06586, 2008a. a
Allen, P. A.: Time scales of tectonic landscapes and their sediment routing systems, in: Landscape Evolution: Denudation, Climate and Tectonics Over Different Time and Space Scales, edited by: Gallagher, K., Jones, S. J., and Wainwright, J., Geological Society, London, Special Publications 296, 7–28, https://doi.org/10.1144/SP296.2, 2008b. a
Armitage, J. J., Duller, R. A., Whittaker, A. C., and Allen, P. A.: Transformation of tectonic and climatic signals from source to sedimentary archive, Nature Geoscience, 4, 231–235, https://doi.org/10.1038/ngeo1087, 2011. a, b, c
Armitage, J. J., Dunkley Jones, T., Duller, R. A., Whittaker, A. C., and Allen, P. A.: Temporal buffering of climate-driven sediment flux cycles by transient catchment response, Earth and Planetary Science Letters, 369–370, 200–210, https://doi.org/10.1016/j.epsl.2013.03.020, 2013. a
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Short summary
Alluvial rivers form networks, but many concepts we use to analyse their long-term evolution derive from models that treat them as single streams. We develop a model including tributary interactions and show that, while patterns of sediment output can be similar for network and single-segment models, complex signal propagation affects aggradation and incision within networks. We argue that understanding a specific catchment's evolution requires a model with its specific network structure.
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