Time variations in geomagnetic intensity

By J. Valet. 2003

284 citations recorded by the source corpus.

Subfields: Atmospheric Science, Geophysics, Molecular Biology

View Paper: https://www.semanticscholar.org/paper/3aae7c811ae5c26c1dd76ff35fb470addcbaf976

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Citations in the corpus

Climate change and solar variability: what's new under the sun? (2006, background): “Advanced normalization techniques may help in correcting lithological signals (see [87] for a comprehensive overview).”
Geomagnetic field for 0–3 ka: 1. New data sets for global modeling (2009, background): “[25] Valet [2003] , Korte et al. [2005], Donadini et al. [2007], and more recently Genevey et al. [2008] discuss in detail the problems related to paleointensity determinations.”
Energetics of the Core (2015, background): “Despite these difficulties, it is clear that, over timescales greater than a few thousand years, the mean position of the magnetic axis coincides with the rotation axis (Valet 2003).”
The Magnetic Field of Planet Earth (2010, methodology): “Discussions of these and other recent methods can be found in Valet (2003), Tauxe and Yamazaki (2007).”
Reliable absolute palaeointensities independent of magnetic domain state (2006, background): “There is little consensus, however, on how far the intensity can drop during periods of stable polarity or what the fieldstrength range is during the reversal process itself [3].”
Toward an optimal geomagnetic field intensity determination technique (2004, methodology): “[7] Detailed reviews of various Thellier-type techniques are given by Selkin and Tauxe [2000] and Valet [2003] .”
Depositional remanent magnetization: Toward an improved theoretical and experimental foundation (2006, background): “, recent review by [6]).”
The paleomagnetism of single silicate crystals: Recording geomagnetic field strength during mixed polarity intervals, superchrons, and inner core growth (2006, background): “Diligent efforts to detect experimental alteration and nonideal behavior related to magnetic mineral domain state characterize recent studies of lavas formed during the last 5 million years [e.g., Laj and Kissel, 1999; Valet, 2003].”
The geomagnetic dipole moment over the last 7000 years—new results from a global model (2005, background): “contributions results from different regions can differ significantly [2].”
Solar activity during the last 1000 yr inferred from radionuclide records (2007, background): “values. The mean reconstructed geomagnetic field decreases by approximately 5% during the last century, which is in accordance with instrumental measurements ( Valet, 2003 ).”
PADM2M: a penalized maximum likelihood model of the 0–2 Ma palaeomagnetic axial dipole moment (2011, methodology): “This result is consistent with the conclusions of Valet et al. (2005) for Sint-2000, but with a smaller difference in mean PADM for the two chrons (1.”