Articles | Volume 12, issue 6
https://doi.org/10.5194/esurf-12-1227-2024
https://doi.org/10.5194/esurf-12-1227-2024
Short communication
 | 
04 Nov 2024
Short communication |  | 04 Nov 2024

Short Communication: Numerically simulated time to steady state is not a reliable measure of landscape response time

Nicole M. Gasparini, Adam M. Forte, and Katherine R. Barnhart

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Cited articles

Adams, B. A., Whipple, K. X., Forte, A. M., Heimsath, A. M., and Hodges, K. V.: Climate controls on erosion in tectonically active landscapes, Sci. Adv., 6, eaaz3166, https://doi.org/10.1126/sciadv.aaz3166, 2020. a
Allen, P. A. and Densmore, A.: Sediment flux from an uplifting fault block, Basin Res., 12, 367–380, 2000. a
Anders, A. M., Roe, G. H., Montgomery, D. R., and Hallet, B.: Influence of precipitation phase on the form of mountain ranges, Geology, 36, 479, https://doi.org/10.1130/G24821A.1, 2008. a, b
Armitage, J. J., Duller, R. A., Whittaker, A. C., and Allen, P. A.: Transformation of tectonic and climatic signals from source to sedimentary archive, Nat. Geosci., 4, 231–235, 2011. a
Armitage, J. J., Whittaker, A. C., Zakari, M., and Campforts, B.: Numerical modelling of landscape and sediment flux response to precipitation rate change, Earth Surf. Dynam., 6, 77–99, https://doi.org/10.5194/esurf-6-77-2018, 2018. a
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Short summary
The time it takes for a landscape to adjust to new environmental conditions is critical for understanding the impacts of past and future environmental changes. We used different computational models and methods and found that predicted times for a landscape to reach a stable condition vary greatly. Our results illustrate that reporting how timescales are measured is important. Modelers should ensure that the measurement technique addresses the question.
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