Core-mantle boundary secular acceleration energy (top) and Earth-surface jerk energy (bottom), as functions of the dimensional simulation time in the ’71 percent of path’ model (Aubert and Gillet 2021). See the README files below for full details
The goal of the 4D-Earth-Swarm project, supported by the European Space Agency, is to improve our understanding of the rapid (interannual) changes in the geomagnetic field, as recorded by the three satellites of the Swarm mission of ESA - as well as earlier satellite missions and ground-based observatories. The work also involves input from state-of-the-art numerical simulations of the geodynamo. Full details on the project can be found after this link.
Time series of outputs computed at 100% of the parameter space path
Here I link to the trajectories A1-4, B1-4 presented in
Long time series of outputs from a geodynamo model approaching Earth's core conditions (deliverable D-C.1)
Here I link to the deliverable D-C.1 proposed by partner IPGP within the framework of this project. These consist in selected outputs from the ’71 percent of path’ model introduced in the following paper:
Aubert, J., Gillet, N.: The interplay of fast waves and slow convection in geodynamo simulations nearing Earth's core conditions, Geophys. J. Int., 2021, doi: 10.1093/gji/ggab054
See the README file
A catalogue of simulated jerks from a geodynamo model approaching Earth's core conditions (deliverable D-E.1)
Here I link to the deliverable D-E.1 proposed by partner IPGP within the framework of this project. These consist in selected outputs from the ’71 percent of path’ model introduced in the following paper:
Aubert, J., Livermore, P., Finlay, C., Fournier, A. and Gillet, N.: A taxonomy of simulated geomagnetic jerks, Geophys. J. Int. 231, 650-672, 2022, doi:10.1093/gji/ggac212
See the README file
Gauss_Bsurf.mat (high temporal resolution) for event
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Gauss_Vsurf.mat (high temporal resolution) for event
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Movie archive for event
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Full three-dimensional states (WARNING 4.5Gb DOWNLOADS) for events
MATLAB script for reading the full three-dimensional states
An ensemble of 3D base states for Earth's core dynamics at epoch 2000 determined by geomagnetic data assimilation in a numerical geodynamo model (deliverable D-O.1)
Here I link to the deliverable D-O.1 proposed by partner IPGP within the framework of this project.
See the README file