Antarctic gravity low strengthens as mantle dynamics reshape the geoid
Scientists mapped Earth’s interior with earthquakes to build a 3D mantle model and a map of the Antarctic Geoid Low, finding the depression has persisted for about 70 million years but has intensified over the last 40–50 million years as subducted slabs sank and buoyant mantle material rose. The results, which also align with true polar wander, suggest deep Earth processes can subtly shift sea level and influence the growth of Antarctica’s ice sheet; the work was published in Scientific Reports.
