ArchKalmag14k - Correlation based model of the holocene core field, based on archeomagnetic and volcanic data
ArchKalmag14k
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Correlation based geomagnetic field model of the holocene core field, based on archeomagnetic and volcanic data. ArchKalmag14k is constructed using methods from Bayesian statistics, in particular Gaussian processes and the Kalman filter, to reflect uncertainties in data and modeling. Additionally to the field coefficients, covarianz matrices and a model ensemble are provided, to be able to include the uncertainties in further processing. The model covers the last 14.000 years, but an analysis shows that only the last 8.000 years can be resolved from the archeomagnetic and volcanic data.
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- is related to
- CALSxk (10.000 - 3.000 years BP) - Geomagnetic field model for the period 10.000 - 3.000 years BP
- CALSxk (10.000 - 3.000 years BP) - Geomagnetic field model for the period 10.000 - 3.000 years BP
- GGF100k - Model that covers the past 100.000 years and it is the longest global reconstruction of the geomagnetic field
- GGFSS70 - Geomagnetic model that covers the period of 70 - 15 kyrs, that includes 3 geomagnetic excursions
- LSMOD Models - Models for the periode of 30 to 50 kyrs that contain the Laschamp and Mono Lake field excursions
- Mag.num - Model of the geomagnetic core field, based on satellite and observatory data