Abstract
In this chapter, we show how the MaxEP hypothesis may be used to build simple climate models without representing explicitly the energy transport by the atmosphere. The purpose is twofold. First, we assess the performance of the MaxEP hypothesis by comparing a simple model with minimal input data to a complex, state-of-the-art General Circulation Model. Next, we show how to improve the realism of MaxEP climate models by including climate feedbacks, focusing on the case of the water-vapour feedback. We also discuss the dependence of the entropy production rate and predicted surface temperature on the resolution of the model.
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Notes
- 1.
The uniform relative humidity in version 3 is chosen as the mean relative humidity in the MaxEP v0 case.
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Herbert, C., Paillard, D. (2014). Predictive Use of the Maximum Entropy Production Principle for Past and Present Climates. In: Dewar, R., Lineweaver, C., Niven, R., Regenauer-Lieb, K. (eds) Beyond the Second Law. Understanding Complex Systems. Springer, Berlin, Heidelberg. https://doi.org/10.1007/978-3-642-40154-1_9
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