Antarctica's ice sheet is the planet's largest freshwater reservoir—and it's losing mass at an accelerating rate. Here are seven key facts:
The Antarctic Ice Sheet covers 14 million km² (5.4M mi²), averages 2,160 m (7,100 ft) thick, and holds 70% of Earth's fresh water. If it all melted, seas would rise ~58 m (190 ft).
Gravity drives ice outward from the center at ~100 m/year (328 ft/year). Fast-flowing outlet glaciers and ice streams move much faster.
Annual ice loss jumped from 40 billion tons (1970s) to 252 billion tons (2010s)—a sixfold increase. West Antarctica and the Antarctic Peninsula are the biggest losers.
Antarctic melt contributes ~0.4 mm/year to global sea-level rise (currently ~3.4 mm/year total). Projections: up to 1 m (3 ft) by 2100 if emissions stay high.
Ice reflects sunlight (high albedo). As it shrinks, darker ocean absorbs more heat, amplifying warming—a dangerous positive feedback loop.
Krill, penguins, seals, and whales depend on sea ice and stable coastal conditions. Habitat loss, shifting food webs, and breeding failures are already documented.
Marine ice sheet instability (e.g., Thwaites "Doomsday Glacier") could trigger runaway collapse. Limiting warming to 1.5°C is critical to avoid multi-meter sea-level commitment over centuries.
Bottom line: Antarctic melt isn't a future threat—it's happening now, with global consequences.