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Disquisitions Relating to Principles of Thermodynamic Equilibrium in Climate Modelling
1Department of Physics, University of Algarve, 8005-139 Faro, Portugal.
Abstract:
We revisit the fundamental principles of thermodynamic equilibrium in relation to heat transfer processes within the Earth’s atmosphere. A knowledge of equilibrium states at ambient temperatures (T) and pressures (p) and deviations for these p-T states due to various transport ‘forces’ and flux events give rise to gradients (dT/dz) and (dp/dz) of height z throughout the atmosphere. Fluctuations about these troposphere averages determine weather and climates. Concentric and time-span average values
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