On the Scales of Dynamic Topography in Whole‐Mantle Convection Models

Abstract Mantle convection shapes Earth's surface by generating dynamic topography. Observational constraints and regional convection models suggest that surface topography could be sensitive to mantle flow for wavelengths as short as 1,000 and 250 km, respectively. At these spatial scales, sur...

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Bibliographic Details
Main Authors: M. Arnould, N. Coltice, N. Flament, V. Seigneur, R. D. Müller
Format: Article
Language:English
Published: Wiley 2018-09-01
Series:Geochemistry, Geophysics, Geosystems
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Online Access:https://doi.org/10.1029/2018GC007516
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