claim: Wu et al (2010) use a new method to calculate ice sheet mass balance.
evidences.evidence_id: Geoid:176
evidences.article: Geoid
evidences.evidence: "Interannual variations of the mass balance of the Antarctica and Greenland ice sheets from GRACE".
evidences.votes: NOT_ENOUGH_INFO NOT_ENOUGH_INFO
evidences.evidence_id: Post-glacial rebound:284
evidences.article: Post-glacial rebound
evidences.evidence: "A method of combining ICESat and GRACE satellite data to constrain Antarctic mass balance".
evidences.votes: SUPPORTS NOT_ENOUGH_INFO
evidences.evidence_id: Retreat of glaciers since 1850:13
evidences.article: Retreat of glaciers since 1850
evidences.evidence: The mass balance, or difference between accumulation and ablation (melting and sublimation), of a glacier is crucial to its survival.
evidences.votes: SUPPORTS NOT_ENOUGH_INFO
evidences.evidence_id: Sea level rise:497
evidences.article: Sea level rise
evidences.evidence: "A Reconciled Estimate of Ice-Sheet Mass Balance".
evidences.votes: NOT_ENOUGH_INFO NOT_ENOUGH_INFO
evidences.evidence_id: Sea level rise:91
evidences.article: Sea level rise
evidences.evidence: A combination of satellite observations of its changing volume, flow and gravitational attraction with modelling of its surface mass balance suggests the overall mass balance of the East Antarctic Ice Sheet was relatively steady or slightly positive for much of the period 1992–2017.
evidences.votes: SUPPORTS NOT_ENOUGH_INFO