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Extremal climatic states simulated by a 2-dimensional model: Part II : Different climatic scenarios
Different climatic simulations have been obtained by using a 2-Dim horizontal energy balance model (EBM), which has been constrained to satisfy several extremal principles on dissipation and convection. Moreover, 2 different versions of the model with fixed and variable cloud-cover have been used. T...
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Published in: | Tellus. Series A, Dynamic meteorology and oceanography Dynamic meteorology and oceanography, 2000-08, Vol.52 (4), p.440-454 |
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container_title | Tellus. Series A, Dynamic meteorology and oceanography |
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creator | PUJOL, T LLEBOT, J. E |
description | Different climatic simulations have been obtained by using a 2-Dim horizontal energy balance model (EBM), which has been constrained to satisfy several extremal principles on dissipation and convection. Moreover, 2 different versions of the model with fixed and variable cloud-cover have been used. The assumption of an extremal type of behaviour for the climatic system can acquire additional support depending on the similarities found with measured data for past conditions as well as with usual projections for possible future scenarios. |
doi_str_mv | 10.1034/j.1600-0870.2000.00193.x |
format | article |
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subjects | Atmospheric radiation Earth, ocean, space Entropia Entropy Exact sciences and technology External geophysics Meteorology Other topics in atmospheric geophysics Radiació atmosfèrica Termodinàmica Thermodynamic |
title | Extremal climatic states simulated by a 2-dimensional model: Part II : Different climatic scenarios |
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