When Ice the Size of Delaware Disappears
In July 2017, a trillion-ton iceberg (A68, 5,800 sq km—larger than Delaware) broke off Antarctica’s Larsen C ice shelf, creating one of the largest icebergs ever recorded. The calving reduced the ice shelf by 12% and accelerated concerns about Antarctic instability. Earlier, Larsen A (1995) and Larsen B (2002, disintegrating in just 35 days) collapsed entirely, demonstrating how rapidly ice shelves can vanish.
The Doomsday Glacier
Thwaites Glacier in West Antarctica, nicknamed the “Doomsday Glacier,” became a focus of intense scientific alarm. The Florida-sized glacier holds enough ice to raise global sea levels by 65cm, but more critically, it acts as a cork preventing the entire West Antarctic Ice Sheet from sliding into the ocean. Warm ocean water eroding Thwaites’ underwater base could trigger collapse within decades, potentially raising seas by 3+ meters over centuries—flooding coastal cities worldwide.
How Ice Shelves Stabilize Glaciers
Ice shelves are floating extensions of land-based glaciers, acting like buttresses or dams slowing glacier flow into the ocean. When ice shelves collapse, land glaciers accelerate dramatically—Larsen B’s disintegration caused tributary glaciers to speed up 2-8 times. This positive feedback means ice loss accelerates: warming ocean water melts ice shelves → glaciers flow faster → more ice enters ocean → sea level rises faster.
Underestimated Risks
Climate models historically underestimated Antarctic ice loss, assuming slow, gradual change over millennia. Recent observations reveal rapid, nonlinear processes (ice cliff collapse, hydrofracturing from meltwater) could trigger faster disintegration. 2021 IPCC reports increased worst-case sea level rise estimates, acknowledging Antarctica represents the largest uncertainty in climate projections. Paleoclimate evidence suggests Antarctic ice sheets collapsed rapidly during past warm periods.
Sources:
- Nature Larsen C calving: https://www.nature.com/articles/s41586-018-0212-1
- Science Thwaites research: http://web.archive.org/web/20250915153240/https://www.science.org/doi/10.1126/science.aaz5845
- IPCC AR6 Sea Level: https://www.ipcc.ch/report/ar6/wg1/chapter/chapter-9/