CORDIS Project
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PALEOCORE aims to enhance our understanding of Earth's core dynamics over long timescales by integrating paleomagnetic data and advanced modeling techniques. This project seeks to explain the recent decline in Earth's magnetic field strength and its implications for planetary habitability.
PALEOCORE will provide the first comprehensive observational constraints on the dynamics of Earth’s core on multi-centennial to millennial timescales.
Such constraints are essential to understand the core processes responsible for the rapid decay of Earth’s dipole field strength over the past century and to forecast future field changes.Generated through convective motions in the liquid iron core, Earth’s magnetic field acts as a shield against harmful cosmic radiation and plays a crucial role f…
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