New NASA research on Antarctica, including the first map of iceberg calving, doubles the previous estimates of loss from ice shelves and details how the continent is changing. In forecasting global sea level rise, the greatest uncertainty is how Antarctica’s ice loss will accelerate as the climat
The 200-foot-tall front of the Getz Ice Shelf in Antarctica is scored with cracks where icebergs are likely to break off, or calve, in this 2016 photo. The first estimate of Antarctic calving has found that since 1997 ice shelves have lost as much ice from calving as from melting. Credit: NASA/GSFC/OIB/Jeremy Harbeckresearch on Antarctica, including the first map of iceberg calving, doubles the previous estimates of loss from ice shelves and details how the continent is changing.
Most Antarctic glaciers flow to the ocean, where they end in floating ice shelves that are up to 2 miles thick and 500 miles across. Ice shelves act like buttresses to glaciers, keeping the ice from simply sliding into the ocean. When ice shelves are stable, they have a natural cycle of calving and replenishment that maintains their size fairly consistently over the long term.
Part of the reason is that satellite imagery has been challenging to interpret. “For example,” said Greene, “you can imagine looking at a satellite image and trying to figure out the difference between a white iceberg, white ice shelf, white sea ice, and even a white cloud. That’s always been a difficult task. But we now have enough data from multiple satellite sensors to see a clear picture of how Antarctica’s coastline has evolved in recent years.
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