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Modelling secondary microseismic noise by normal mode summation ArchiMer
Gualtieri, L.; Stutzmann, E.; Capdeville, Y.; Ardhuin, Fabrice; Schimmel, M.; Mangeney, A.; Morelli, A..
Secondary microseisms recorded by seismic stations are generated in the ocean by the interaction of ocean gravity waves. We present here the theory for modelling secondary microseismic noise by normal mode summation. We show that the noise sources can be modelled by vertical forces and how to derive them from a realistic ocean wave model. We then show how to compute bathymetry excitation effect in a realistic earth model by using normal modes and a comparison with Longuet-Higgins approach. The strongest excitation areas in the oceans depends on the bathymetry and period and are different for each seismic mode. Seismic noise is then modelled by normal mode summation considering varying bathymetry. We derive an attenuation model that enables to fit well the...
Tipo: Text Palavras-chave: Surface waves and free oscillations; Seismic attenuation; Theoretical seismology; Wave propagation.
Ano: 2013 URL: http://archimer.ifremer.fr/doc/00146/25703/24020.pdf
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Modelling the ocean site effect on seismic noise body waves ArchiMer
Gualtieri, Lucia; Stutzmann, Eleonore; Farra, V.; Capdeville, Y.; Schimmel, M.; Ardhuin, Fabrice; Morelli, A..
Secondary microseismic noise is generated by non-linear interactions between ocean waves at the ocean surface. We present here the theory for computing the site effect of the ocean layer upon body waves generated by noise sources distributed along the ocean surface. By defining the wavefield as the superposition of plane waves, we show that the ocean site effect can be described as the constructive interference of multiply reflected P waves in the ocean that are then converted to either P or SV waves at the ocean-crust interface. We observe that the site effect varies strongly with period and ocean depth, although in a different way for body waves than for Rayleigh waves. We also show that the ocean site effect is stronger for P waves than for S waves. We...
Tipo: Text Palavras-chave: Body waves; Site effects; Theoretical seismology.
Ano: 2014 URL: http://archimer.ifremer.fr/doc/00190/30087/28634.pdf
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