Skip to main content

Thank you for visiting You are using a browser version with limited support for CSS. To obtain the best experience, we recommend you use a more up to date browser (or turn off compatibility mode in Internet Explorer). In the meantime, to ensure continued support, we are displaying the site without styles and JavaScript.


Surface heat led to ice-shelf demise

The collapse of Antarctica's giant Larsen B Ice Shelf in 2002 was probably caused by warming at the surface rather than by instability at the bottom of the ice sheet.

Eugene Domack at the University of South Florida in St Petersburg and his colleagues mapped the sea floor below where the shelf used to be. They also analysed marine sediment cores to reconstruct characteristics of the ice shelf's grounding zone — where the floating ice shelf meets underlying bedrock — before the ice collapsed.

They found that this zone had remained stationary for some 12,000 years, challenging the idea that structural changes at the bottom of the ice shelf might have caused Larsen B's disintegration.

The findings could inform estimates of how much Antarctic melting will contribute to future sea level rise, the authors say.

Science 345, 1354–1358 (2014)

Rights and permissions

Reprints and Permissions

About this article

Verify currency and authenticity via CrossMark

Cite this article

Surface heat led to ice-shelf demise. Nature 513, 282–283 (2014).

Download citation


Quick links

Nature Briefing

Sign up for the Nature Briefing newsletter — what matters in science, free to your inbox daily.

Get the most important science stories of the day, free in your inbox. Sign up for Nature Briefing