Abstract
A new model of terrestrial rock weathering - the Rock Geochemical Model (RokGeM) - was developed for incorporation into the GENIE Earth System modelling framework. In this paper we describe the model. We consider a range of previously devised parameterizations, ranging from simple dependencies on global mean temperature following Berner et al. (1983), to spatially explicit dependencies on run-off and temperature (GKWM, Bluth and Kump, 1994; GEM-CO2, Amiotte-Suchet et al., 2003) - fields provided by the energy-moisture balance atmosphere model component in GENIE. Using long-term carbon cycle perturbation experiments, we test the effects of a wide range of model parameters, including whether or not the atmosphere was "short-circuited" in the carbon cycle; the sensitivity and feedback strength of temperature and run-off on carbonate and silicate weathering; different river-routing schemes; 0-D (global average) vs. 2-D (spatially explicit) weathering schemes; and the lithology dependence of weathering. Included are details of how to run the model and visualize the results. © Author(s) 2013.
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CITATION STYLE
Colbourn, G., Ridgwell, A., & Lenton, T. M. (2013). The Rock Geochemical Model (RokGeM) v0.9. Geoscientific Model Development, 6(5), 1543–1573. https://doi.org/10.5194/gmd-6-1543-2013
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