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 "shortcircuited" 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.
| Original language | English |
|---|---|
| Pages (from-to) | 1543-1573 |
| Number of pages | 31 |
| Journal | Geoscientific Model Development |
| Volume | 6 |
| Issue number | 5 |
| DOIs | |
| Publication status | Published - 2013 |
UN SDGs
This output contributes to the following UN Sustainable Development Goals (SDGs)
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SDG 13 Climate Action
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SDG 15 Life on Land
Keywords
- EARTH SYSTEM MODEL
- FOSSIL-FUEL CO2
- ATMOSPHERIC CARBON-DIOXIDE
- GLOBAL CHEMICAL EROSION
- PHANEROZOIC TIME
- CLIMATE-CHANGE
- LIFE-SPAN
- BIOTIC ENHANCEMENT
- REVISED MODEL
- GEOLOGIC TIME
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