Continuous geomagnetic field models for the past 7 millennia: 2. CALS7K

By Monika Korte, Catherine Constable. 2005

319 citations recorded by the source corpus.

Subfields: Atmospheric Science, Geophysics, Molecular Biology

View Paper: https://www.semanticscholar.org/paper/35ad5810ed944bfdf6e2d39b914ed42432709144

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Citations in the corpus

Geomagnetic field for 0–3 ka: 2. A new series of time‐varying global models (2009, methodology): “On the basis of investigations of present field data and VADMs from model predictions we proposed that about half of the difference can be explained by a systematic bias of the VADMs due to the geographical data distribution [Korte and Constable, 2005b, 2006].”
Solar activity during the last 1000 yr inferred from radionuclide records (2007, methodology): “record and the alternative estimate for the global geomagnetic dipole moment (Korte and Constable, 2005).”
Reconstructing Holocene geomagnetic field variation: new methods, models and implications (2014, methodology): “The methodology follows that of Bloxham & Jackson (1992) used for historical field models and adapted for archaeomagnetic and palaeomagnetic data by Korte & Constable (2005, 2011) and Korte et al. (2009).”
Geomagnetic field for 0–3 ka: 1. New data sets for global modeling (2009, methodology): “We expect that our CALS3k.3.0 model should be comparable in large scale to the CALS3k.2 version [Korte and Constable, 2005], but with substantially improved resolution as measured by the model spherical harmonic spectra [Korte et al., 2009, Figure 8].”
Large variations in Holocene solar activity: Constraints from 10Be in the Greenland Ice Core Project ice core (2006, result): “New reconstructions of the geomagnetic dipole field [ Korte and Constable, 2005 ] generally show lower values and a different long-term trend than Yang et al. [2000] which is in better agreement with the long-term trend of the GRIP 10Be flux.”
Improving geomagnetic field reconstructions for 0–3 ka (2011, background): “Global compilations from numerous publications of archeo-9 magnetic data (Donadini et al., 2006; Genevey et al., 2008; Donadini et al., 2009) and10 paleomagnetic records from sediments with high accumulation rates (Korte et al., 2005;11 Korte and Constable, 2006; Donadini et al., 2009) are the basis”
Continuous geomagnetic field models for the past 7 millennia: 1. A new global data compilation (2005, methodology): “In a subsequent paper we will use this data set for improving CALS3K.1 and developing a CALS7K model for the past 7000 years [see Korte and Constable, 2005].”
The Magnetic Field of Planet Earth (2010, methodology): “…use the Korte et al. (2005) archeomagnetic data to rescale the 1590–1840 gufm1 g 0 1 linear trend; from the CALS7K.2 archeomagnetic field model of Korte and Constable (2005) (blue), which only relies on the Korte et al. (2005) archeomagnetic data; and by the earlier Hongre et al. (1998)…”
Reliable absolute palaeointensities independent of magnetic domain state (2006, background): “The expected value for the palaeointensity ranges 43–47 μT based on historical field models GUFM1 [46] and CAL37K [47].”
Reconstructing the Holocene geomagnetic field (2011, methodology): “2 [6], covering the past 3 ky and 7 ky respectively, have found widespread applications in investigations of regional motions in the core [e.”
ArcheoInt: An upgraded compilation of geomagnetic field intensity data for the past ten millennia and its application to the recovery of the past dipole moment (2008, unknown): “These estimates were indeed necessary for the computations of global geomagnetic field models [ Korte and Constable , 2005a].”
A regional archeomagnetic model for Europe for the last 3000 years, SCHA.DIF.3K: Applications to archeomagnetic dating (2009, methodology): “…on archeomagnetic data have been obtained during the last decade by using the Spherical Harmonic Analysis (SHA) technique, like the one proposed by Hongre et al. [1998], and the CALS family of models [Korte and Constable, 2003, 2005], which also includes lava flows and lake sediments as input data.”
Conditions for Earth-like geodynamo models (2010, methodology): “We use the model CALS7K.2 for the geomagnetic field structure during the past 7000 yr (Korte and Constable, 2005), which is based on archeomagnetic and lake sediment data.”