Ice in Motion - Glaciers

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Ice in Motion In the article Ice in Motion by Alexandra Witze, the author essentially examines "ice dynamics", the movement and melting of glaciers, and the consequences of these changes to our environment currently and in centuries to come. Greenland and Antarctica are home to some of the world's largest glacial masses; this article also provides details of multiple studies conducted in those regions. To provide some perspective: Greenland loses as much ice in a year as is in the entire Alps. Antarctica's Pine Island Glacier is a major contributor to rising sea levels and recently produced an iceberg of 720 square kilometers - approximately eight times the size of the island of Manhattan. (Witze, 2011). Glaciers of Greenland In 2009, an Ohio State glaciologist, Jason Box, anchored his ship near Petermann Glacier in the north-west quadrant of Greenland. With multiple cameras trained on the glacier, Box's hopes were to catch the ice mass in action as it "calved". The glacier remained solid and steady until August 4, 2010 when it lost a piece four times the size of Manhattan - after Box had already given up and departed his post. (Witze, 2011). "Jakobshavn Isbrae", a major glacier located on the western coast of Greenland, is an approximately 110,l000 kilometers and is responsible for a majority of ice loss. Scientists say Jakobshavn was likely an intrinsic element of the iceberg that sank the Titanic. After 1997, the Jakobshavn ice fields began to thin. Thinner ice moves quicker; this iceberg increased its movement from two to almost five percent between 2004 and 2007. Helheim is yet another Greenland glacier; this one located on the east coast. In the early to mid 2000's, it also hastened its pace by almost two miles per year. Eventually, Helheim slowed its pace and has recently gained mass. (Witze, 2011). Glaciers of Antarctica Although some parts of

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