SPECTRAL ELEMENT MODELLING OF THREE-DIMENSIONAL WAVE PROPAGATION IN A SELF-GRAVITATING EARTH WITH AN ARBITRARILY STRATIFIED OUTER CORE

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dc.contributor.author Chaljub E.
dc.contributor.author Valette B.
dc.date.accessioned 2022-09-23T00:35:28Z
dc.date.available 2022-09-23T00:35:28Z
dc.date.issued 2004
dc.identifier https://elibrary.ru/item.asp?id=6638730
dc.identifier.citation Geophysical Journal International, 2004, 158, 1, 131-141
dc.identifier.issn 0956-540X
dc.identifier.uri https://repository.geologyscience.ru/handle/123456789/38719
dc.description.abstract This paper deals with the spectral element modelling of seismic wave propagation on a global scale. Two aspects relevant to low-frequency studies are particularly emphasized. First, the method is generalized beyond the Cowling approximation in order to fully account for the effects of self-gravitation. In particular, the perturbation of the gravity field outside the Earth is handled by a projection of the spectral element solution onto the basis of spherical harmonics. Second, we propose a new formulation inside the fluid which allows us to account for an arbitrary density stratification. It is based upon a decomposition of the displacement into two scalar potentials, and results in a fully explicit fluid-solid coupling strategy. The implementation of the method is carefully detailed and its accuracy is demonstrated through a series of benchmark tests.
dc.subject BRUNT-VAISALA FREQUENCY
dc.subject ELASTODYNAMICS
dc.subject GLOBAL SEISMOLOGY
dc.subject NUMERICAL MODELLING
dc.subject SELF-GRAVITATION
dc.subject SPECTRAL ELEMENT METHOD
dc.subject SYNTHETIC SEISMOGRAMS
dc.title SPECTRAL ELEMENT MODELLING OF THREE-DIMENSIONAL WAVE PROPAGATION IN A SELF-GRAVITATING EARTH WITH AN ARBITRARILY STRATIFIED OUTER CORE
dc.type Статья


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