Longitudinal structure of Earth’s magnetic field controlled by lower mantle heat flow
Author:
Funder
RCUK | Natural Environment Research Council
Publisher
Springer Science and Business Media LLC
Subject
General Earth and Planetary Sciences
Link
https://www.nature.com/articles/s41561-023-01148-9.pdf
Reference62 articles.
1. Landeau, M., Fournier, A., Nataf, H.-C., Cébron, D. & Schaeffer, N. Sustaining Earth’s magnetic dynamo. Nat. Rev. Earth Environ. 3, 255–269 (2022).
2. Nakagawa, T. & Tackley, P. J. Lateral variations in CMB heat flux and deep mantle seismic velocity caused by a thermal-chemical-phase boundary layer in 3D spherical convection. Earth Planet. Sci. Lett. 271, 348–358 (2008).
3. Stackhouse, S., Stixrude, L. & Karki, B. B. First-principles calculations of the lattice thermal conductivity of the lower mantle. Earth Planet. Sci. Lett. 427, 11–17 (2015).
4. Olson, P., Coe, R., Driscoll, P., Glatzmaier, G. & Roberts, P. Geodynamo reversal frequency and heterogeneous core–mantle boundary heat flow. Phys. Earth Planet. Inter. 180, 66–79 (2010).
5. Laj, C., Mazaud, A., Weeks, R., Fuller, M. & Herrrero-Bervera, E. Geomagnetic reversal paths. Nature 351, 447 (1991).
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