

Larger, 100% versions of these maps can be viewed at the bottom of this page (or you can click on the above maps also). I created these particular renditions of these maps for Encyclopædia Britannica in 2008 from data supplied by the Intergovernmental Panel on Climate Change.
Below is a map showing the disintegration of Antarctica's Larsen ice shelf in 2002, a bellweather event that alerted many to the reality of global warming (click on map to see the 100% image):

The following map shows the diminishing extent of sea ice in the Arctic Ocean. Summer 2007 set a record for loss in sea ice, as determined by aerial extent.
The volume of sea ice, possibly a more critical factor affecting future climate scenarios, has  also been determined from satellite photos, which indicate that Arctic sea ice has thinned by more than 40% since 2004 (Nasa satellites reveal extent of Arctic sea ice loss).A direct consequence of increasing global temperatures and the melting of ice in the polar regions, especially the Antarctic and Greenland ice sheets, will be a rise in sea level. A worse-case scenario is that mean sea level will rise by 3 meters, or nearly 20 feet, by the end of the century. Currently a more modest (though also catastophic) 1-meter to 2-meter rise is predicted, but natural systems can change in unpredictable ways and "abrupt climate change" having more severe consequences is certainly possible.  A 3-meter rise in sea level will flood many low-lying coastal areas and submerge many islands. The following map shows the effect of a 3-meter rise in sea level on several Atlantic coastal areas (a larger version of this map is also available below, or by clicking on this map):



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