Linked from

The 13 pages that link to Pine Island Glacier, each with the reason it gives.

• Antarctic ice sheetBroader topic: Its retreat illustrates how ocean-driven changes can affect Antarctic ice discharge.

• Ice shelfBroader topic: Its floating ice shelf loses mass rapidly through basal melting.

• West Antarctic Ice SheetBroader topic: Its thinning and retreat illustrate ocean-driven change in the region.

• Marine ice-sheet instabilityBroader topic: Its grounding-line retreat illustrates how ocean-driven ice loss can interact with bed geometry.

• Climate change in AntarcticaBroader topic: Its changes provide a closely monitored example of ocean-driven ice loss.

• Ice sheet dynamicsBroader topic: Its thinning and retreat show how ocean-driven shelf melt can affect inland ice.

• Thwaites GlacierRelated: It is a neighboring outlet glacier facing related ocean-driven ice loss.

• Marie Byrd LandRelated: Its evolution offers a nearby comparison for ice loss along West Antarctica’s coast.

• Ice-shelf buttressingBroader topic: Its floating ice shelf provides buttressing that affects the glacier’s discharge.

• West AntarcticaBroader topic: Ocean-driven thinning has accelerated its flow and retreat.

• West Antarctic Rift SystemBroader topic: Its catchment overlies rifted terrain relevant to bed shape and ice motion.

• Bellingshausen SeaBroader topic: Its retreat is a nearby comparison for ice-sheet change farther west.

• Amundsen SeaBroader topic: Its thinning and retreat provide a closely observed example of ocean-driven ice loss.