INTERACTIVE THERMODYNAMICS 3.0 20 =LINK=
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The paper is organized as follows. In section 1, we introduce the most important concepts and methods. Section 2 is devoted to the description of the models and the simulation setup. Section 3 reports the results of the study, while section 4 highlights their implications. The main findings are discussed in section 5. Finally, section 6 summarizes the main conclusions and points out directions for future work.
1. Introduction
Thermodynamic quantities of the climate system, such as the radiation, heat and mass fluxes, temperature and moist-air potential temperature, are determined by two distinct, but interconnected, processes: thermodynamics and dynamics. The former processes, such as baroclinicity, the Lorenz energy cycle (LEC) and the Carnot efficiency, are determined by quantities known as irreversible entropy production (IEP), material entropy production (MEP) and energy dissipation (ED), respectively, with respect to a suitable working substance. The latter processes, such as the dynamic energy budget (DEB), the moist-air energy budget (MAEB), and the latent heat flux (LEF), are governed by the mass, momentum and energy transfer, respectively, and are determined by quantities generally known as the enthalpy, the moist-air potential temperature, and the heat capacity, respectively, with respect to the atmosphere (Wunsch et al. 2005; Wunsch et al. 2009; Meehl et al. 2012, 2013). The LEC and the DEB, also known as total heating/cooling, respectively, are closely related to the global mean feedback by virtue of their dependence on the value of the ratio between the latent heat flux and the effective radiative heat flux, and can be expressed as a function of (cf. Wunsch et al. 2009) (1) :
H = E(latent heat flux) - E(effective radiative heat flux)
(1)
where E and H are the respective functions of the atmosphere's enthalpy and the heat capacity, respectively. The global mean feedback, written as the time derivative of H, is expressed as
2.
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