Polar Ice

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Polar ice is sea ice created from the freezing of sea water, ice sheets and glaciers. These in turn are formed from the build up and compaction of fallen snow. Both the ice sheets and glaciers cover vast areas of the Polar Regions. This polar ice is hugely important to our globe and takes up a large part of it. Global sea-ice coverage averages about 25 million kilometers square; this is the area of the entire North America continent. The ice sheets, which cover the land, with the glaciers cover about 15 million kilometers square; this is almost 10% of the Earth’s land area, with the majority on Antarctica (Earthobservatory.nasa.gov, 2013).
With talk of global warming still being threatened by scientists and governments, the depletion of the polar ice is a major concern. Many experiments have been done to monitor current ice levels and predict future ice levels. Since then scientists have tried to discover what would cause the melting of our polar ice. One major concern is that the melting of the polar ice would create extreme flooding for all costal and island inhabitants. Is the polar ice melting and could greenhouse gases be the cause?
Mikhail Veritsky from Yale University set out to discover if an increase in Carbon Dioxide, a manmade greenhouse gas, would lead to the depletion of the Antarctic ice sheet. To predict this they create a numerical experiment using an atmospheric general circulation model connected to a 3D ice-sheet model. They found that even doubling the Carbon Dioxide concentration did not show any significant changes in the ice sheet. This implies that an Antarctic collapse of ice as a consequence of increased greenhouse gases is unlikely (Verbitsky & Saltzman, 1995).
In Greenland the ice sheets h...

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References
Dahl-Jensen, D. (2000). CLIMATE CHANGE: Enhanced: The Greenland Ice Sheet Reacts.. Science, 289(5478), 404-5.
Earthobservatory.nasa.gov (2013). Polar Ice Fact Sheet : Feature Articles. [online] Retrieved from: http://earthobservatory.nasa.gov/Features/PolarIce/polar_ice.php [Accessed: 29 Nov 2013].
Nsidc.org (2013). A better year for the cryosphere | Arctic Sea Ice News and Analysis. [online] Retrieved from: http://nsidc.org/arcticseaicenews/2013/10/a-better-year-for-the-cryosphere/ [Accessed: 29 Nov 2013].
Toyota, T., Takatsuji, S. & Nakayama, M. (2006). Characteristics of sea ice floe size distribution in the seasonal ice zone. Geophysical research letters, 33 (2), 02616.
Verbitsky, M. & Saltzman, B. (1995). Behavior of the East Antarctic Ice Sheet as deduced from a coupled GCM/ice-sheet model. Geophysical research letters, 22 (21), 2913--2916.

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