Titlebook: Dynamics of the Earth; Theory of the Planet V. I. Ferronsky,S.V. Ferronsky Book 2010 Springer Science+Business Media B.V. 2010 Dynamical eq

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,Irrelevance of the Hydrostatics Model and the Earth’s Dynamic Equilibrium,damentals for solution of the problem date back to the distant past and are related to the names of founders of modern science. But even at that early time, these pioneers well understood that applicability of hydrostatic equilibrium to a body’s dynamic problems is restricted by certain boundary con

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Fundamentals of the Theory of Dynamic Equilibrium,es of the potential and kinetic energy within a certain period of time to be the averaged virial theorem. Conversely, the virial theorem for a system moving in its own force field and establishing a relationship between the potential and kinetic energy of the oscillating polar moment of inertia, is

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,Solution of Jacobi’s Virial Equation for Conservative Systems,dynamics of natural systems. We showed that, instead of the traditional description of a system in co-ordinates and velocities, the problem of dynamics can be studied from the position of an external observer. In this case the system as a whole is described by a compact and elegant equation and is c

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,Dynamics of the Earth’s Atmosphere and Oceans,phase. These shells exist in the solid Earth’s outer force field but the atmosphere exists in dynamical equilibrium, and the oceans are in a weighted transition to a hydrostatic state. The atmosphere as a gaseous shell is totally “dissolved” in the Earth’s outer force field in the form of atomic and

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