CALSxk (10.000 - 3.000 years BP) - Geomagnetic field model for the period 10.000 - 3.000 years BP
The 10ka averaged radial magnetic field at the core-mantle boundary (model CALS10k.2) shows clear deviations from a pure dipole field. (GFZ Potsdam)
Contact:
Web:
Infrastructure belongs to:
Geomagnetic field models of the last 3 to 10 kyrs based on archeo- and paleomagnetic data. This updated version of geomagnetic field description for the past 10 000 years is mainly based on the same data as CALS10k.1b. However, the model offers higher temporal and spatial resolution due to improved uncertainty estimates for the data and calibrations of sediment relative paleointensity. The large-scale field at the core-mantle boundary and the Earth’s surface is described better by this model than by the previous version CALS10k.1b.
Categories
Data Types
Disciplinary Keywords
Selected infrastructures
Link
Data Access via
Relationships
- is related to
- ArchKalmag14k - Correlation based model of the holocene core field, based on archeomagnetic and volcanic data
- ArchKalmag14k - Correlation based model of the holocene core field, based on archeomagnetic and volcanic data
- GGF100k - Model that covers the past 100.000 years and it is the longest global reconstruction of the geomagnetic field
- 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
- 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