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Case
Study: Animation of Larsen B breakup
When gigantic icebergs break off from
Antarctica, the images are dramatic and frequently make the
news. The recent collapse of the Larsen B ice shelf in West
Antarctica (closest to South America), covered an area larger
than the state of Rhode Island and sent thousands of icebergs
drifting into the Weddell Sea. This was the largest single
event in a series of retreats of the Larsen Ice Shelf in recent
years.
Ice inland are thick plates of ice fed by glaciers. The shelves
flow over the edge of the continent and float on the ocean
around much of Antarctica. The Antarctic Peninsula, where
the Larsen shelf is located, has experienced greater warming
than other parts of the continent. Over the last five years,
the shelf shrunk by about 5700 square kilometers (2200 square
miles).
While the Antarctic Peninsula is warming faster than the global
average, other parts of this huge continent are cooling, and
some of the ice shelves are gaining mass. For example, the
Ross Ice Shelf (closest to New Zealand) is thickening as the
glacier streams that flow over it slow down. At the same time,
this ice shelf has also calved its share of giant icebergs:
in March 2000 and again in March and May 2002.
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The dynamics of an ice sheet and
ice shelf are complex and not completely understood.
Scientists studying the flow rates of the Ross
Ice Shelf arent sure whether the ice is
responding to an internal process or to the climate
of parts of Antarctica.
They also cant say for sure whether the
collapse of the Larsen B Ice Shelf is attributable
to a warming trend. Researchers at the National
Snow and Ice Data Center, Portland State University,
and elsewhere think that there is a link between
warmer temperatures and ice shelf stability. They
theorize that pools of melting ice on top of the
glacier may enhance the fracturing and eventual
collapse of portions of the ice shelf.
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