Abstract
The radiative forcing due to increased CO2 and some simple climate feedbacks are illustrated using results from one-dimensional model studies. The simulated response of climate to CO2 in three-dimensional models is described with emphasis on the physical mechanisms responsible. The role of the oceans, the simulation of the transient response and the problems of detecting CO2-induced climate change are discussed briefly, and priorities for future research are outlined.
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Mitchell, J.F.B. (1988). Simulation of Climate Change Due to Increased Atmospheric CO2 . In: Schlesinger, M.E. (eds) Physically-Based Modelling and Simulation of Climate and Climatic Change. NATO ASI Series, vol 243. Springer, Dordrecht. https://doi.org/10.1007/978-94-009-3043-8_11
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DOI: https://doi.org/10.1007/978-94-009-3043-8_11
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