Description
For low values of carbon dioxide there are three equilibrium points: one stable corresponding to present day temperatures, one stable corresponding to much higher temperatures, and an unstable in between. Once carbon dioxide is raised above the bifurcation point, the low-stable and unstable equilibrium point annihilate one another (a saddle-node bifurcation), resulting in the system converging to the lone remaining high-stable equilibrium point.
Students will use both graphing and numerical techniques to find equilibrium points. Matlab software for numerical solution of the ODE is included in an attached file.
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