Chemical Tadpole is a coupled model of soil chemical weathering and landscape evolution. This is the model used to perform the simulations in:
Ferrier K.L., Perron J.T., in review. The importance of hillslope scale in responses of chemical erosion rate to changes in tectonics and climate. Journal of Geophysical Research - Earth Surface.
The code is based on the Tadpole landscape evolution model available at
https://github.com/MITGeomorph/Tadpole
and described in:
Perron, J.T., W.E. Dietrich and J.W. Kirchner (2008), Controls on the spacing of first-order valleys. Journal of Geophysical Research, 113, F04016, doi: 10.1029/2007JF000977.
Perron, J.T., J.W. Kirchner and W.E. Dietrich (2009), Formation of evenly spaced ridges and valleys. Nature, 460, 502–505, doi: 10.1038/nature08174.
Perron, J.T., P.W. Richardson, K.L. Ferrier, and M. Lapôtre (2012), The root of branching river networks. Nature, 492, 100–103, doi: 10.1038/nature11672.
To run a simulation, start with the master script admwx.m and read the comments in it. All other functions assist in running this script.
This code is citable at the following DOI: https://doi.org/10.5281/zenodo.3901757.