This series of images, taken between 31 January and 13 April, 2002, captured the collapse of the Larsen-B Ice Shelf. In January 1995, two events on the Larsen Ice Shelf attracted public attention: the calving of a 70 – by 25-kilometre iceberg from the Larsen B; and the disintegration of the remainder of the Larsen A. Larsen Ice Shelf. Icebridge, an airborne survey of polar ice, completed an eighth consecutive Antarctic deployment on Nov. 18. An ice shelf forms when a glacier on land reaches the coast and flows into the ocean. The retreat and collapse of Antarctic Peninsula ice shelves in tandem with a regional atmospheric warming has fueled speculation as to how these events may be related. Ice shelf schematic. Several of the ice shelves around Antarctica have recently collapsed dramatically, rather than retreating in a slow and steady manner. Ice shelf collapse. Scientists predict that the Larsen C ice shelf has at least three more years until it disintegrates. If the Larsen C Ice Shelf deteriorates in the same manner as Larsen B did in the year 2002, the slow-facing glaciers will have one less barrier as they move toward the ocean. Talk about glaring inconsistencies. The Larsen Ice Shelf is situated along the northeastern coast of the Antarctic Peninsula, one of the fastest-warming places on the planet. A new NASA study finds the last remaining section of Antarctica's Larsen B Ice Shelf, which partially collapsed in 2002, is quickly weakening and likely to disintegrate … To the northwest of the Weddell Sea, stretching along the eastern coast of the Antarctic Peninsula, stands an imposing ice shelf known as the Larsen Ice Shelf. Melting of Antarctica’s Larsen C Ice Shelf at 40-year record high, study says. Without the buffer of an ice shelf, the glacier’s flow accelerated, stretching and thinning the ice. The crack, now more than 100 miles long, could lead to a complete separation of the Larsen C ice shelf. Ice shelves fringe 75 percent of the Antarctic ice sheet and the Larsen C ice shelf, located on on the east side of the Antarctic Peninsula, is the fourth largest ice shelf ringing Earth’s southernmost continent. Ice shelves like the Larsen C are the floating portions of ice streams and glaciers, and they act as a buffer for the grounded ice behind them. Acquired in 2003, 2004,and 2005, these images show an intermittently ice-filled bay in the wake of the 2002 collapse of the Larsen B Ice Shelf on the Antarctic Peninsula. The ice shelves in question were particularly susceptible, being small fringing shelves at the limit of ice shelf stability for the recent global climate (the Northern Larsen Ice Shelf is the northernmost ice shelf on the east side of the Antarctic Peninsula; the Wordie Ice Shelf was the northernmost on the west side). Ice shelves. Larsen C Ice Shelf (LCIS, Fig. If global warming continues at the rate it is now, the Larsen C ice shelf has most likely one year until it is destroyed. The concern is that if Larsen C collapses, ice from glaciers would flow into the sea and melt, raising sea levels. The Larsen Ice Shelf is a long, fringing ice shelf in the northwest part of the Weddell Sea, extending along the east coast of Antarctic Peninsula from Cape Longing to the area just southward of Hearst Island.Named for Captain Carl Anton Larsen, the master of the Norwegian whaling vessel Jason, who sailed along the ice front as far as 68°10' South during December 1893. The Larsen C Ice Shelf is the fourth largest ice shelf found in the South Pole, and according to scientists, it holds several land-based glaciers behind it. After its disappearance, the glacier behind it sped up its flow toward the ocean, pushing up sea level faster than it otherwise would have. 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