Modelling: new methodes and models
Improved Holocene global geomagnetic field reconstructions
Holocene Global Field
Improvement of global geomagnetic field reconstructions spanning the past millennia by investigating the quality of Holocene paleomagnetic sediment records.
Comparison of the terrestrial and Martian lithospheric magnetic field models, derived from satellite missions (CHAMP and MGS) data.
The project aims to elaborate the predictability of Earth's magnetic field changes from decadal to millennial time scale, by using numerical dynamo solution and reconstruction of Earth's magnetic field variation from observation.
Building time dependent magnetic field models satisfying the frozen-flux radial induction equation.