
Canada’s gravity puzzle: mantle dynamics take the lead over ice rebound
GRACE satellite data show that the Hudson Bay gravity low cannot be explained by glacial rebound alone; older ice-sheet models account for only about 25–45% of the anomaly, leaving a substantial portion attributed to deep mantle structure and slow convection beneath Laurentia. The mantle’s buoyancy and deep-root dynamics, not surface ice history, appear to shape the regional gravity field, though quantifying the split depends on rebound modeling and longer observation records from GRACE Follow-On.


