REVERSALS AND LARGE-SCALE VARIATIONS OF THE GEOMAGNETIC FIELD: SIMILARITIES AND DIFFERENCES

Capa

Citar

Texto integral

Sobre autores

M. Reshetnyak

Schmidt Institute of Physics of the Earth; Pushkov Institute of Terrestrial Magnetism, Ionosphere and Radio Wave Propagation of the Russian Academy of Sciences

Autor responsável pela correspondência
Email: m.reshetnyak@gmail.com
ORCID ID: 0000-0002-4909-6336
Código SPIN: 5443-5061

Bibliografia

  1. Bonhommet, N., and J. Zähringer (1969), Paleomagnetism and potassium argon age determinations of the Laschamp geomagnetic polarity event, Earth and Planetary Science Letters, 6(1), 43–46, https://doi.org/10.1016/0012-821X(69)90159-9.
  2. Christensen, U., P. Olson, and G. A. Glatzmaier (1999), Numerical modelling of the geodynamo: a systematic parameter study, Geophysical Journal International, 138(2), 393–409, https://doi.org/10.1046/j.1365-246x.1999.00886.x.
  3. Christensen, U. R., and J. Aubert (2006), Scaling properties of convection-driven dynamos in rotating spherical shells and application to planetary magnetic fields, Geophysical Journal International, 166(1), 97–114, https://doi.org/10.1111/j.1365-246x.2006.03009.x.
  4. Hulot, G., and J. L. Le Mouël (1994), A statistical approach to the Earth’s main magnetic field, Physics of the Earth and Planetary Interiors, 82(3–4), 167–183, https://doi.org/10.1016/0031-9201(94)90070-1.
  5. Krause, F., and K.-H. Rädler (1980), Mean-field magnetohydrodynamics anddynamo theory, Akademie-Verlag, Berlin.
  6. Liu, J., N. R. Nowaczyk, S. Panovska, M. Korte, and H. W. Arz (2020), The Norwegian-Greenland Sea, the Laschamps, and the Mono Lake Excursions Recorded in a Black Sea Sedimentary Sequence Spanning From 68.9 to 14.5 ka, Journal of Geophysical Research: Solid Earth, 125(8), https://doi.org/10.1029/2019jb019225.
  7. Lowes, F. J. (1974), Spatial Power Spectrum of the Main Geomagnetic Field, and Extrapolation to the Core, Geophysical Journal International, 36(3), 717–730, https://doi.org/10.1111/j.1365-246x.1974.tb00622.x.
  8. Panovska, S., C. G. Constable, and M. Korte (2018), Extending Global Continuous Geomagnetic Field Reconstructions on Timescales Beyond Human Civilization, Geochemistry, Geophysics, Geosystems, 19(12), 4757–4772, https://doi.org/10.1029/2018gc007966.
  9. Reshetnyak, M. Y. (2017), Tuning of the mean-field geodynamo model, Izvestiya, Physics of the Solid Earth, 53(4), 581–587, https://doi.org/10.1134/S1069351317030090.
  10. Reshetnyak, M. Y. (2021), Reversals of the Geomagnetic Field: Constraint on Convection Intensity in the Earth’s Core, Geomagnetism and Aeronomy, 61(2), 266–271, https://doi.org/10.1134/S0016793221020134.
  11. Valet, J.-P. (2003), Time variations in geomagnetic intensity, Reviews of Geophysics, 41(1), https://doi.org/10.1029/2001RG000104.
  12. Valet, J.-P., L. Meynadier, and Y. Guyodo (2005), Geomagnetic dipole strength and reversal rate over the past two million years, Nature, 435(7043), 802–805, https://doi.org/10.1038/nature03674.
  13. Wicht, J. (2002), Inner-core conductivity in numerical dynamo simulations, Physics of the Earth and Planetary Interiors, 132(4), 281–302, https://doi.org/10.1016/s0031-9201(02)00078-x.

Declaração de direitos autorais © Reshetnyak M., 2024

Creative Commons License
Este artigo é disponível sob a Licença Creative Commons Atribuição 4.0 Internacional.

Este site utiliza cookies

Ao continuar usando nosso site, você concorda com o procedimento de cookies que mantêm o site funcionando normalmente.

Informação sobre cookies