The importance of acquired vertical velocities, compressibility and released condensation heat in the sustaining of atmospheric convection phenomena. A review of conventional views on atmospheric convection. Recent experimental results. Arguments against the hydrostatic equilibrium and incompressibility theory. A continuous modification method for aerological diagrams, considering vertical velocities, and the forecasting of vertical cloud development.On rappelle les idées classiques sur la convection atmosphérique et on condense les résultats expérimentaux récents. On justifie le rejet de l'hypothèse de l'équilibre hydrostatique et de celle de l'incompressibilité. On propose une méthode de modification continue des diagrammes aérologiques, ...
L'écoulement du fluide atmosphérique est régi par l'équation de Navier-Stokes et le second principe ...
Some dynamical characteristics of atmospheric convection are investigated by ob-taining an analytica...
The dominant model of atmospheric circulation posits that hot air rises, creating horizontal winds. ...
Static instability in meteorology. Stability of the vertical equilibrium of the atmosphere under sma...
Cloud development as governed by latent heat released by condensing water vapour and freezing water....
A two-dimensional mathematical model of moist air convection in the sub-cloud and cloud layers is pr...
As long as convection is not completely resolved by the model grid, a subgrid deep convection scheme...
This dataset contains a collection of namelists describing the setups of the various model simulatio...
A new type of vertical motion of air different from penetrative convection is discussed. For small v...
The phenomenon of thermal and compositional (chemical) convection is very common in nature and there...
On dynamic instability developing in baroclinal models of the atmosphere. The use of baroclinal mode...
Both climate forcing and climate sensitivity persist as stubborn uncertainties limiting the extent ...
An attempt is made to investigate theoretically the controlling influence of compensating downward m...
Le but de la thèse est de comprendre l'influence dynamique des effets diabatiques, comme la convecti...
Abstract. Condensation removes water vapor molecules from the gas phase and reduces the weight of th...
L'écoulement du fluide atmosphérique est régi par l'équation de Navier-Stokes et le second principe ...
Some dynamical characteristics of atmospheric convection are investigated by ob-taining an analytica...
The dominant model of atmospheric circulation posits that hot air rises, creating horizontal winds. ...
Static instability in meteorology. Stability of the vertical equilibrium of the atmosphere under sma...
Cloud development as governed by latent heat released by condensing water vapour and freezing water....
A two-dimensional mathematical model of moist air convection in the sub-cloud and cloud layers is pr...
As long as convection is not completely resolved by the model grid, a subgrid deep convection scheme...
This dataset contains a collection of namelists describing the setups of the various model simulatio...
A new type of vertical motion of air different from penetrative convection is discussed. For small v...
The phenomenon of thermal and compositional (chemical) convection is very common in nature and there...
On dynamic instability developing in baroclinal models of the atmosphere. The use of baroclinal mode...
Both climate forcing and climate sensitivity persist as stubborn uncertainties limiting the extent ...
An attempt is made to investigate theoretically the controlling influence of compensating downward m...
Le but de la thèse est de comprendre l'influence dynamique des effets diabatiques, comme la convecti...
Abstract. Condensation removes water vapor molecules from the gas phase and reduces the weight of th...
L'écoulement du fluide atmosphérique est régi par l'équation de Navier-Stokes et le second principe ...
Some dynamical characteristics of atmospheric convection are investigated by ob-taining an analytica...
The dominant model of atmospheric circulation posits that hot air rises, creating horizontal winds. ...