This derivative model adds to Berner's original the dynamics of ocean acidification and CaCO3 neutralization of a CO2 pulse, which should improve the simulation on time scales of decades to centuries.
Model atmospheric pCO2 concentrations after 1,000 and 3,000 Gton C spikes, showing the "long tail" as the persistent increase in pCO2 after the spike.
You have the option of releasing a Spike of CO2 to the atmosphere at the instant of the transition from the Spinup to the Simulation stages. For the default case when the model loads, there is a 1000 Gton C release at the transition, while the driving parameters for the two stages, like CO2 degassing rates, are the same. You have to expand the time view by selecting Show 1 million years before you can see the carbon cycle return to its equilibrium.
The Silicate thermostat plot shows the weathering rate of CO2 uptake and the CO2 degassing rates, both in units of 1012 moles / year. The CaCO3 budget plot shows CaCO3 weathering and burial rates in the ocean, in 1012 moles / year. There are also plots of ocean chemistry (the alkalinity and total CO2 concentrations, in mole equivalents / m3, and the carbon isotopic composition of dissolved carbon in the ocean on the PDB scale, labeled del13C) and ocean and atmosphere temperatures.
You can compare two model runs by running the first, then selecting Save This Run to Background. The run will be saved on the plot, and you can superimpose a second by changing model options. Get rid of the backround plot by Deleting it.
|How long does it take for a CO2 spike to decay away completely? Which chemical balance or process determines this time scale?|
|Make a plot of the weathering rate as a function of atmospheric CO2 by setting the volcanic degassing flux to different values and running to equilibrium.|
|Vary the geologic time to see how the intensity of the sun changes the model behavior.|
|Introduce plants, keeping everything else constant, to see whether plants make it warm or cool when they appear. Where does the carbon go or come from, to change the atmospheric value?|
|The University of Chicago|
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