The vibration of a layered rotating planet and Bryan’s effect

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Sea-Level Changes. Post-seismic Deformation. Icy Moons. Back Matter Pages It looks at our planet in an integrated fashion, linking the physics of its interior to geophysical and geodetic techniques that record, over a broad spectrum of spatial wavelengths and time scales, the ongoing modifications in the shape and gravity field of the planet. Basic issues related to the rheological properties of the Earth and to its slow deformation are considered, in both mathematical and physical terms, within the framework of an analytical relaxation theory.

Fundamentals of this theory are developed in the first two Chapters. This Second Edition improves substantially our formalism implementing compressibility in viscoelastic relaxation. Chapter 5 now contains new developments in the physics of the gravitational effects of large earthquakes at subduction zones, made possible by new gravity data from space missions. The physics of high-velocity ions in the Hall thruster near-field. Numerical simulation and subgrid-scale modeling of mixing and wall-bounded turbulent flows.

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The Vibration of a Layered Rotating Planet and Bryan’s Effect

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