Top-heavy thermochemical geodynamo simulations show heterogeneous outer boundary heat flux reproduces observed longitudinal inclination anomaly variations, while elevated chemical driving reduces longitudinal structures and promotes polar radial field minima.
Bouffard , author G
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Paleomagnetic signatures of core-mantle interactions inferred from top-heavy thermochemical geodynamo simulations
Top-heavy thermochemical geodynamo simulations show heterogeneous outer boundary heat flux reproduces observed longitudinal inclination anomaly variations, while elevated chemical driving reduces longitudinal structures and promotes polar radial field minima.
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A Data Efficiency Study of Synthetic Fog for Object Detection Using the Clear2Fog Pipeline
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