Linked from

The 14 pages that link to Marine ice-sheet instability, each with the reason it gives.

• Antarctic ice sheetRelated: Much of West Antarctica is grounded below sea level, making retreat sensitive to ocean contact.

• Greenland ice sheetRelated: Some Greenland outlet glaciers retreat into deep fjords, where this feedback may matter.

• Ice sheetRelated: Retreat into deeper water can expose thicker ice and increase ice discharge.

• Ice shelfRelated: Shelf thinning can reduce the restraint on grounded marine ice.

• West Antarctic Ice SheetRelated: Much of the ice sheet rests below sea level, creating conditions for this retreat feedback.

• Climate change in AntarcticaRelated: It can accelerate West Antarctic ice loss once retreat passes a threshold.

• Pine Island GlacierRelated: The glacier’s bed deepens inland, making this instability relevant to its long-term retreat.

• Ice sheet dynamicsRelated: Its potential to accelerate West Antarctic retreat remains a major source of sea-level uncertainty.

• Thwaites GlacierRelated: Thwaites rests on bedrock below sea level, making this instability a concern.

• Quaternary glaciationRelated: It may help explain rapid retreat and potential instability of marine-based ice in past and future climates.

• Ice-shelf buttressingRelated: Buttressing can delay retreat, but its loss can expose an unstable grounding line.

• West AntarcticaRelated: Much of the West Antarctic Ice Sheet rests on a bed that deepens inland.

• East AntarcticaRelated: The contrast between the mostly high-based eastern sheet and marine basins sharpens concern about vulnerable sectors.

• Amundsen SeaRelated: Thinning and retreat of glaciers here raise concern about this feedback.