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Dissipation at the core-mantle boundary on a small-scale topography

  • The parameters of the nutations are now known with a good accuracy, and the theory accounts for most of their values. Dissipative friction at the core-mantle boundary (CMB) and at the inner core boundary is an important ingredient of the theory. Up to now, viscous coupling at a smooth interface and electromagnetic coupling have been considered. In some cases they appear hardly strong enough to account for the observations. We advocate here that the CMB has a small- scale roughness and estimate the dissipation resulting from the interaction of the fluid core motion with this topography. We conclude that it might be significant

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Author details:Jean-Louis Le Mouel, Clement Narteau, Marianne Greff-Lefftz, Matthias HolschneiderORCiDGND
URL:http://www.agu.org/journals/jb/
DOI:https://doi.org/10.1029/2005jb003846
ISSN:0148-0227
Publication type:Article
Language:English
Year of first publication:2006
Publication year:2006
Release date:2017/03/24
Source:Journal of geophysical research : solid earth. ISSN 0148-0227. - 111 (2006), B4, Art. B04413
Organizational units:Mathematisch-Naturwissenschaftliche Fakultät / Institut für Physik und Astronomie
Peer review:Referiert
Institution name at the time of the publication:Mathematisch-Naturwissenschaftliche Fakultät / Institut für Physik
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