'Doomsday glacier' won't collapse the way we thought, new study suggests

Antarctica's Thwaites Glacier got its nickname the "Doomsday Glacier" for its potential to flood coastlines around the world if it collapsed. It is already contributing about 4% of annual sea-level rise as it loses ice, and one theory suggests the glacier could soon begin to collapse into the ocean like a row of dominoes.

But is that kind of rapid collapse really as likely as feared? A new study of Thwaites Glacier's susceptibility to what's known as marine ice cliff instability offers some hope. But the findings don't mean Thwaites is stable.

Polar scientist Mathieu Morlighem, who led the study, explains the results.

Why is the Thwaites Glacier so important?

Thwaites Glacier drains a huge area of Antarctica's ice sheet — about 74,000 square miles (192,000 square kilometers), an expanse bigger than Florida. If a snowflake falls within that drainage system, it will eventually end up as part of an iceberg in the ocean off Thwaites.

What we are seeing with Thwaites Glacier right now is a disaster in slow motion.

The bedrock under Thwaites Glacier sits below sea level and slopes downward going inland, so the glacier gets deeper toward the interior of the ice sheet. Once the glacier begins losing more ice than it gains from new snowfall and starts to retreat, it's very hard to slow it down because of this slope. And Thwaites is already retreating at an accelerating rate as the climate warms.

Related: 'We were in disbelief': Antarctica is behaving in a way we've never seen before. Can it recover?