Linked from

The 20 pages that link to Greenland ice sheet, each with the reason it gives.

• Arctic amplificationRelated: Arctic warming accelerates surface melting and can increase ice-sheet mass loss.

• Last Glacial MaximumRelated: Its LGM extent and contribution to sea-level change remain important reconstruction questions.

• Atlantic meridional overturning circulationRelated: Its meltwater is one possible source of freshening near North Atlantic deep-water formation regions.

• Laurentide Ice SheetRelated: It is a surviving North American ice sheet that provides a contrast in scale and persistence.

• Ice ageRelated: It is a surviving ice sheet whose cores preserve records of past climate swings.

• North Atlantic OceanRelated: Its meltwater can alter salinity and density in the adjacent North Atlantic.

• Middle PleistoceneRelated: Its changing extent records and influenced North Atlantic climate during glacial cycles.

• Effects of climate change on oceansRelated: Its meltwater contributes to sea-level rise and can freshen nearby North Atlantic waters.

• Olafur EliassonRelated: Ice Watch brought fragments of its glacial ice into public spaces as a climate encounter.

• Older DryasRelated: Greenland temperature reconstructions are central to the interval's standard chronology.