Articles | Volume 5, issue 1
https://doi.org/10.5194/esurf-5-47-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/esurf-5-47-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Accurate simulation of transient landscape evolution by eliminating numerical diffusion: the TTLEM 1.0 model
Benjamin Campforts
CORRESPONDING AUTHOR
Division Geography, Department of Earth and Environmental Sciences, KU Leuven, Leuven, Belgium
Wolfgang Schwanghart
Institute of Earth and Environmental Science, Universität Potsdam, Potsdam, Germany
Gerard Govers
Division Geography, Department of Earth and Environmental Sciences, KU Leuven, Leuven, Belgium
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- Tectonic Accretion Controls Erosional Cyclicity in the Himalaya S. Mandal et al. 10.1029/2021AV000487
- Orographic rainfall drives the Himalaya drainage divide to move north S. Bian et al. 10.1016/j.geomorph.2023.108952
- How does the newly-formed drainage divide migrate after a river capture event? S. Bian et al. 10.1016/j.epsl.2024.119165
- Parameterization of river incision models requires accounting for environmental heterogeneity: insights from the tropical Andes B. Campforts et al. 10.5194/esurf-8-447-2020
- The influence of landslide morphology on erosion rate variability across western Himalayan catchments: Role of westerlies and summer monsoon interaction in the landscape characterization A. Kashyap & M. Behera 10.1002/gj.4913
- Global sensitivity analysis of parameter uncertainty in landscape evolution models C. Skinner et al. 10.5194/gmd-11-4873-2018
- Short communication: Analytical models for 2D landscape evolution P. Steer 10.5194/esurf-9-1239-2021
- A cross-divide contrast index (C) for assessing controls on the main drainage divide stability of a mountain belt C. Zhou et al. 10.1016/j.geomorph.2021.108071
- Accelerated Miocene incision along the Yangtze River driven by headward drainage basin expansion A. Rohrmann et al. 10.1126/sciadv.adh1636
- Transient emergence of ramified river channels: simulations of geographical cycle by Erosion-Diffusion Model (EDM) H. Serizawa et al. 10.15748/jasse.10.221
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- Tectonic advection of contacts enhances landscape transience N. Mitchell & A. Forte 10.1002/esp.5559
- Landslide mobilization rates: A global analysis and model J. Broeckx et al. 10.1016/j.earscirev.2019.102972
- Short communication: flow as distributed lines within the landscape J. Armitage 10.5194/esurf-7-67-2019
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- Rivers as linear elements in landform evolution models S. Hergarten 10.5194/esurf-8-367-2020
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Latest update: 26 Dec 2024
Short summary
Despite a growing interest in landscape evolution models, accuracy assessment of the numerical methods they are based on has received little attention. We test a higher-order flux-limiting finite-volume method to simulate river incision and tectonic displacement. We show that this scheme significantly influences the evolution of simulated landscapes and the spatial and temporal variability of erosion rates. Moreover, it allows for the simulation of lateral tectonic displacement on a fixed grid.
Despite a growing interest in landscape evolution models, accuracy assessment of the numerical...