Icebergs that calve off Antarctica’s coast are often swept up by ocean currents circling the continent, and may remain relatively intact for months or years, so long as they remain in sufficiently cool conditions. Some icebergs, however, drift north to warmer climates and disintegrate. By observing the response of an iceberg to a warmer climate at a lower latitude, scientists can make predictions about how ice shelves—thick slabs of ice attached to coastlines—might respond to a warming climate.
Related links :
- localization in wikimapia
- Envisat image showing situation in december 2007 before the collision
- Science daily article
- video (392 Mb) from Australian Antarctic Division
- NASA Earth Observatory other image (MODIS sensor)
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