BCampforts/SPLM
SPLM solves the 1D stream power law using different numerical methods:
% Case 1 : explicit upwind scheme (see Roberts 2010)
% Case 2 : implicit upwind scheme (see Braun and Willet 2013)
% Case 3 : TVD scheme Campforts and Govers 2014
When you use SPLM, please reference one of these publications:
Campforts, B. and Govers, G. (2015): Keeping the edge: A numerical method that avoids knickpoint smearing when solving the stream power law, J. Geophys. Res. Earth Surf., 120(7), 1189–1205, [doi:10.1002/2014JF003376]
Campforts, B., W. Schwanghart, and G. Govers (2016), Accurate simulation of transient landscape evolution by eliminating numerical diffusion: the TTLEM 1.0 model, Earth Surf. Dyn. Discuss., (2010), 1–32, doi:10.5194/esurf-2016-39.
Cite As
Benjamin Campforts (2026). BCampforts/SPLM (https://github.com/BCampforts/SPLM), GitHub. Retrieved .
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| Version | Published | Release Notes | |
|---|---|---|---|
| 1.0.0.0 |
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