Geomagnetic field for 0–3 ka: 1. New data sets for global modeling
By F. Donadini, Monika Korte, Catherine Constable. 2009
184 citations recorded by the source corpus.
Subfields: Atmospheric Science, Geophysics, Molecular Biology
View Paper: https://www.semanticscholar.org/paper/ccc2794de3e1fab7257834880e182df4c5a00cac
How researchers see this paper
The researchers whose trusted networks rank it highest, strongest advocate first. Every researcher gets a different order.
In Atmospheric Science
In Geophysics
- Catherine Constable
- Monika Korte
- F. Donadini
- G. Hulot
- Mioara Mandea
- Christopher C. Finlay
- R. Holme
- Nils Olsen
In Molecular Biology
- Catherine Constable
- Monika Korte
- G. Hulot
- F. Donadini
- R. Holme
- Mioara Mandea
- Nils Olsen
- Christopher C. Finlay
Citations in the corpus
- The Magnetic Field of Planet Earth (2010, background): “Ongoing efforts with data gathering and compilations are generating significantly larger global data sets (Donadini et al. 2009), but with similar intrinsic limitations.”
- Geomagnetic field for 0–3 ka: 2. A new series of time‐varying global models (2009, methodology): “The GEOMAGIA50 intensity database by Donadini et al. [2006] has now been expanded [Donadini et al., 2009] and updated and contains all archeomagnetic intensity and directional data that are known to us.”
- Reconstructing Holocene geomagnetic field variation: new methods, models and implications (2014, methodology): “The sedimentary relative palaeointensity data were converted to absolute palaeointensites, following the approach of Korte & Constable (2006) and Donadini et al. (2009), by multiplying each entire record with a constant scaling factor.”
- PADM2M: a penalized maximum likelihood model of the 0–2 Ma palaeomagnetic axial dipole moment (2011, background): “The most recent Geomagia50.v2 database (Donadini et al. 2009) compiles API data from archaeological and igneous sources with ages less than 50 kyr.”
- Improving geomagnetic field reconstructions for 0–3 ka (2011, methodology): “In recent work, Donadini et al. (2009) and Korte et al.38 (2009) constructed a suite of models using various classes of data and were able to show that39 even those based exclusively on sedimentary records, comprising magnetic field directions40 and suitably calibrated intensities, provide…”