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Maus, Stefan, Silva, Luis, Hulot, Gauthier (2008) Can core-surface flow models be used to improve the forecast of the Earth's main magnetic field?. Journal of Geophysical Research: Solid Earth, 113. doi:10.1029/2007jb005199

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Reference TypeJournal (article/letter/editorial)
TitleCan core-surface flow models be used to improve the forecast of the Earth's main magnetic field?
JournalJournal of Geophysical Research: Solid Earth
AuthorsMaus, StefanAuthor
Silva, LuisAuthor
Hulot, GauthierAuthor
Year2008 (August)Volume113
PublisherAmerican Geophysical Union (AGU)
DOIdoi:10.1029/2007jb005199Search in ResearchGate
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Mindat Ref. ID926328Long-form Identifiermindat:1:5:926328:8
GUID0
Full ReferenceMaus, Stefan, Silva, Luis, Hulot, Gauthier (2008) Can core-surface flow models be used to improve the forecast of the Earth's main magnetic field?. Journal of Geophysical Research: Solid Earth, 113. doi:10.1029/2007jb005199
Plain TextMaus, Stefan, Silva, Luis, Hulot, Gauthier (2008) Can core-surface flow models be used to improve the forecast of the Earth's main magnetic field?. Journal of Geophysical Research: Solid Earth, 113. doi:10.1029/2007jb005199
In(2008) Journal of Geophysical Research: Solid Earth Vol. 113. American Geophysical Union (AGU)

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Lesur, V., Wardinski, I. (2009) Comment on “Can core‐surface flow models be used to improve the forecast of the Earth's main magnetic field?” by Stefan Maus, Luis Silva, and Gauthier Hulot. Journal of Geophysical Research, 114. doi:10.1029/2008jb006188
Maus, Stefan, Silva, Luís, Hulot, Gauthier (2009) Reply to comment by V. Lesur et al. on “Can core‐surface flow models be used to improve the forecast of the Earth's main magnetic field”. Journal of Geophysical Research, 114. doi:10.1029/2008jb006242
Gubbins, David (1975) Can the Earth's magnetic field be sustained by core oscillations?. Geophysical Research Letters, 2 (9) 409-412 doi:10.1029/gl002i009p00409
Thébault, Erwan, Chulliat, Arnaud, Maus, Stefan, Hulot, Gauthier, Langlais, Benoit, Chambodut, Aude, Menvielle, Michel (2010) IGRF candidate models at times of rapid changes in core field acceleration. Earth, Planets and Space, 62 (10) 753-763 doi:10.5047/eps.2010.05.004
Voorhies, Coerte V. (1995) Time-varying fluid flow at the top of Earth's core derived from definitive geomagnetic reference field models. Journal of Geophysical Research: Solid Earth, 100. 10029-10039 doi:10.1029/95jb00863
Silva, Luís, Maus, Stefan, Hulot, Gauthier, Thébault, Erwan (2010) On the possibility of extending the IGRF predictive secular variation model to a higher SH degree. Earth, Planets and Space, 62 (10) 815-820 doi:10.5047/eps.2010.07.005
Voorhies, Coerte V. (1986) Steady flows at the top of Earth's core derived from geomagnetic field models. Journal of Geophysical Research: Solid Earth, 91. 12444-12466 doi:10.1029/jb091ib12p12444
Yuan, Liang, Steinle‐Neumann, Gerd (2024) Earth's “Missing” Chlorine May Be in the Core. Journal of Geophysical Research: Solid Earth, 129 (2) doi:10.1029/2023jb027731
Maus, Stefan, Dimri, Vijay (1995) Potential field power spectrum inversion for scaling geology. Journal of Geophysical Research: Solid Earth, 100. 12605-12616 doi:10.1029/95jb00758
Voorhies, C. V. (2004) Correction to “Narrow-scale flow and a weak field by the top of Earth's core: Evidence from Ørsted, Magsat, and secular variation”. Journal of Geophysical Research: Solid Earth, 109. doi:10.1029/2004jb003289
McFadden, Phillip L., Merrill, Ronald T. (1995) History of Earth's magnetic field and possible connections to core-mantle boundary processes. Journal of Geophysical Research: Solid Earth, 100. 307-316 doi:10.1029/94jb02362
 
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