On the dynamical interaction between overshooting convection and an underlying dipole magnetic field -- I. The non-dynamo regime (2020)
Attributed to:
A new model of the geodynamo: large-scale vortices in the Earth's core
funded by
NERC
Abstract
No abstract provided
Bibliographic Information
Digital Object Identifier: http://dx.doi.org/10.48550/arxiv.2008.01857
Publication URI: https://arxiv.org/abs/2008.01857
Type: Other