claim: But gravity measurements of ice-mass loss are  complicated by glacial isostatic adjustments—compensation for the rise or fall of the underlying crustal material.
evidences.evidence_id: GRACE and GRACE-FO:34
evidences.article: GRACE and GRACE-FO
evidences.evidence: Glacial isostatic adjustment—the slow rise of land masses once depressed by the weight of ice sheets from the last ice age—is chief among these signals.
evidences.votes: SUPPORTS SUPPORTS
evidences.evidence_id: Post-glacial rebound:1
evidences.article: Post-glacial rebound
evidences.evidence: Post-glacial rebound and isostatic depression are phases of glacial isostasy (glacial isostatic adjustment, glacioisostasy), the deformation of the Earth's crust in response to changes in ice mass distribution.
evidences.votes: SUPPORTS SUPPORTS
evidences.evidence_id: Post-glacial rebound:105
evidences.article: Post-glacial rebound
evidences.evidence: Mass changes of ice sheets can be monitored by measuring changes in the ice surface height, the deformation of the ground below and the changes in the gravity field over the ice sheet.
evidences.votes: SUPPORTS SUPPORTS
evidences.evidence_id: Post-glacial rebound:107
evidences.article: Post-glacial rebound
evidences.evidence: However, glacial isostatic adjustment of the ice sheets affect ground deformation and the gravity field today.
evidences.votes: SUPPORTS SUPPORTS
evidences.evidence_id: Post-glacial rebound:5
evidences.article: Post-glacial rebound
evidences.evidence: The enormous weight of this ice caused the surface of the Earth's crust to deform and warp downward, forcing the viscoelastic mantle material to flow away from the loaded region.
evidences.votes: SUPPORTS SUPPORTS