Introduction

Introduction

In the previous unit we discussed the equilibrium simulations of global climate in which a model is run with the present greenhouse gas concentrations and then run again with doubled (or in some cases quadrupled) amounts of greenhouse gases. In each model run, the model is allowed to continue until all the effects of initial conditions have died away and the model ocean, atmosphere, and ice masses come into balance with the heating effects of the assumed level of greenhouse gases. This is verified by observing that the global temperatures are not drifting off to a warmer or colder average.

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