Antarctic Ice Shelf Disintegration Underscores a Warming World

 NSIDC Lead Scientist Ted Scambos, who first spotted the disintegration in March, said, "We believe the Wilkins has been in place for at least a few hundred years. But warm air and exposure to ocean waves are causing a break-up."

Satellite images indicate that the Wilkins began its collapse on February 28; data revealed that a large iceberg, 41 by 2.5 kilometers (25.5 by 1.5 miles), fell away from the ice shelf's southwestern front, triggering a runaway disintegration of 405 square kilometers (160 square miles) of the shelf interior (Figure 1). The edge of the shelf crumbled into the sky-blue pattern of exposed deep glacial ice that has become characteristic of climate-induced ice shelf break-ups such as the Larsen B in 2002. A narrow beam of intact ice, just 6 kilometers wide (3.7 miles) was protecting the remaining shelf from further breakup as of March 23 (Figure 2).

Scientists track ice shelves and study collapses carefully because some of them hold back glaciers, which if unleashed, can accelerate and raise sea level. Scambos said, "The Wilkins disintegration won't raise sea level because it already floats in the ocean, and few glaciers flow into it. However, the collapse underscores that the Wilkins region has experienced an intense melt season. Regional sea ice has all but vanished, leaving the ice shelf exposed to the action of waves."

With Antarctica's summer melt season drawing to a close, scientists do not expect the Wilkins to further disintegrate in the next several months. "This unusual show is over for this season," Scambos said. "But come January, we'll be watching to see if the Wilkins continues to fall apart."
Real-time collaboration

Images from NASA's Moderate Resolution Imaging Spectroradiometer (MODIS) and data from ICESat showed that the ice shelf was in a state of collapse in March. Scambos then alerted colleagues around the world, seeking to ensure that every means of gathering information was focused on the break-up.

British Antarctic Survey (BAS) mounted an overflight of the crumbling shelf, collecting video footage and other observations. BAS glaciologist David Vaughan said of the ice shelf, which is supported by a single strip of ice strung between two islands, "Wilkins is the largest ice shelf on West Antarctica yet to be threatened. This shelf is hanging by a thread."

Associate Professor Cheng-Chien Liu at Taiwan's National Cheng-Kung University (NCKU) also responded, requesting high-resolution color satellite images of the area from Taiwan's Formosat-2 satellite (Figure 3), operated by the National Space Organization. Cheng-Chien Liu said, "It looks as if something is slicing the ice shelf piece by piece on an incredible scale, kilometers long but only a few hundred meters in width."

South American scientists also got involved. Andrés Rivera and Gino Cassasa at the Laboratorio de Glaciología y Cambio Climático at the Centro de Estudios Científicos in Chile (CECS), acquired images of the Wilkins from the ASTER instrument, aboard NASA's Terra satellite.

The combined efforts of these international teams have begun to provide observational data that will improve scientific understanding of the mechanisms behind ice shelf collapse. Scambos said, "The Wilkins is an example of an event we don't see very often. But it's a key process in being able to predict how sea level will change in the future."
More information

The Wilkins is one of a string of ice shelves that have collapsed in the West Antarctic Peninsula in the past thirty years. The Larsen B became the most well-known of these, disappearing in just over thirty days in 2002. The Prince Gustav Channel, Larsen Inlet, Larsen A, Wordie, Muller, and the Jones Ice Shelf collapses also underscore the unprecedented warming in this region of Antarctica.

To view British Antarctic Survey's version of this joint release, visit the press area of their Web site at http://www.antarctica.ac.uk/about_bas/news/press_releases.php.

For more information on the Larsen B collapse, see http://nsidc.org/iceshelves/larsenb2002/index.html.