Climate Dynamics

  • Andrew Fowler
Part of the Interdisciplinary Applied Mathematics book series (IAM, volume 36)


Chapter 2 treats simple models of climate dynamics. It begins by describing radiative transfer in the atmosphere, with particular attention to the simple case of a grey, one-dimensional atmosphere. Following this, the convective temperature structure of the troposphere is discussed. The latter part of the chapter deals with energy balance models, in particular with a view to understanding ice age causes. This introduces successively the ice-albedo feedback mechanism, the carbon cycle in atmosphere and ocean, and the rôle of bicarbonate buffering in the ocean.


Dissolve Inorganic Carbon Radiative Heat Transfer Deep Water Formation Heinrich Event Planetary Albedo 
These keywords were added by machine and not by the authors. This process is experimental and the keywords may be updated as the learning algorithm improves.


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Copyright information

© Springer-Verlag London Limited 2011

Authors and Affiliations

  1. 1.MACSI, Department of Mathematics & StatisticsUniversity of LimerickLimerickIreland

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