Cited by 660Geomagnetism and Paleomagnetism StudiesHigh-pressure geophysics and materialsGeological and Geophysical Studies

A three-dimensional convective dynamo solution with rotating and finitely conducting inner core and mantle

Glatzmaier, Gary A., Roberts, Paul H.·1995·Physics of the Earth and Planetary Interiors

Integrity signals

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Crossref · 10.1016/0031-9201(95)03049-3

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  • The Earth's solid inner core is expected to rotate at a different rate from the mantle under its electromagnetic coupling with the fluid outer core.

    “The Earth's solid inner core (IC) is expected to rotate at a different rate from the mantle under its electromagnetic coupling with the fluid outer core, which hosts the geodynamo (Glatzmaier & Roberts, 1995).”

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Authors
Glatzmaier, G. A., & Roberts, P. H.
Affiliations
  • Los Alamos National Laboratory (US)
  • University of California, Los Angeles (US)
Corresponding author
Glatzmaier, Gary A.
Venue
Physics of the Earth and Planetary Interiors
Publisher
Elsevier BV
Published
1995-09
Volume
91
Issue
1-3
Pages
63-75
ISSN
0031-9201 (ISSN-L)
OpenAlex
W2126388052
Cited by
660
References
0
Citations by year
2026: 6 · 2025: 17 · 2024: 11 · 2023: 18 · 2022: 8 · 2021: 28 · 2020: 33 · 2019: 37 · 2018: 13 · 2017: 14 · 2016: 21 · 2015: 14 · 2014: 14 · 2013: 24 · 2012: 16
FWCI
8.93
Type
journal article
Language
en
Open access
closed
Locations
Physics of The Earth and Planetary Interiors (publishedVersion)
Funders
  • National Science Foundation
  • Laboratory Directed Research and Development
Topics
  • Life Sciences › Biochemistry, Genetics and Molecular Biology › Molecular Biology › Geomagnetism and Paleomagnetism Studies
  • Physical Sciences › Earth and Planetary Sciences › Geophysics › High-pressure geophysics and materials
  • Physical Sciences › Earth and Planetary Sciences › Geology › Geological and Geophysical Studies
Keywords
geodynamo, thermal convection, rotating spherical shell, Earth's inner core, core-mantle boundary, magnetic field reversal, magnetic helicity, magnetic diffusion, length of day variations, core rotation, secular variation, 3D MHD simulations, geomagnetic field

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Registry, retraction, Cites and statistics results are computed, not judged, with one exception: a printed reference that no index lists is read once by a model before it counts as a citation error. Claims are extracted by a model and kept only when their quote appears verbatim in the text; each cited source is then checked, with a model’s help, for whether it says what the claim relies on. Those verdicts can be wrong — read the claim’s quote and the cited source before relying on one.

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