International audienceThe concept of available potential energy has been developed in meteorology by E. N. Lorenz in order to understand how the incoming solar energy is transformed within the atmosphere and why the observed values of kinetic energy of wind are much smaller than might be expected. Lorenz has succeeded in explaining, on a global scale, the energy cycle associated with general circulation of the atmosphere.This paper presents the history of other theories of the conversion of energy that have been introduced by the founders of thermodynamics. It is shown that one of them, the available enthalpy approach, can be applied to meteorology. A local available enthalpy cycle is derived to investigate the conversions that take place w...
The atmospheric circulation is driven by heat transport from the tropics to the polar regions, embed...
The thermodynamics of the atmosphere is the subject of several chapters in most textbooks on dynamic...
Formulas are derived that correctly account for the uneven surface topography (mountains) in calcula...
International audienceHydrodynamical applications of the thermodynamic concept of available enthalpy...
Obtention du Prix Prud'Homme de la SMF en 1995.The available energy of a system is that sub-part of ...
The possibility of constructing Lorenz's concept of available potential energy (APE) from a local pr...
The Lorenz energy cycle (Lorenz 1955) describes how the solar heating generates potential energy tha...
A major problem in atmospheric energetic dynamics is addressed. In using a particular mathematical ...
International audienceA diagnostic package is derived from the concept of specific available enthalp...
International audienceThe exergy of the dry atmosphere can be considered as another aspect of the me...
The global energetics analysis performed in the diagnostics program (IGFLUX) of the Reading spectral...
The energetics considerations based on Lorenz’s available potential energy A focus on identification...
The purpose of this study is to provide an overview of the science and development of atmospheric en...
How much wind energy does the atmosphere generate, and how much of it can at best be used as renewab...
The problem of calculating the global entropy production of the climate system is revisited. In the ...
The atmospheric circulation is driven by heat transport from the tropics to the polar regions, embed...
The thermodynamics of the atmosphere is the subject of several chapters in most textbooks on dynamic...
Formulas are derived that correctly account for the uneven surface topography (mountains) in calcula...
International audienceHydrodynamical applications of the thermodynamic concept of available enthalpy...
Obtention du Prix Prud'Homme de la SMF en 1995.The available energy of a system is that sub-part of ...
The possibility of constructing Lorenz's concept of available potential energy (APE) from a local pr...
The Lorenz energy cycle (Lorenz 1955) describes how the solar heating generates potential energy tha...
A major problem in atmospheric energetic dynamics is addressed. In using a particular mathematical ...
International audienceA diagnostic package is derived from the concept of specific available enthalp...
International audienceThe exergy of the dry atmosphere can be considered as another aspect of the me...
The global energetics analysis performed in the diagnostics program (IGFLUX) of the Reading spectral...
The energetics considerations based on Lorenz’s available potential energy A focus on identification...
The purpose of this study is to provide an overview of the science and development of atmospheric en...
How much wind energy does the atmosphere generate, and how much of it can at best be used as renewab...
The problem of calculating the global entropy production of the climate system is revisited. In the ...
The atmospheric circulation is driven by heat transport from the tropics to the polar regions, embed...
The thermodynamics of the atmosphere is the subject of several chapters in most textbooks on dynamic...
Formulas are derived that correctly account for the uneven surface topography (mountains) in calcula...