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But the Greenland ice sheet is not one solid, smooth mass of ice.
As the ice sheet became bigger and thicker, the surrounding air became cold.
The blue diamond is one vivid pointer to the antiquity of the Greenland ice sheet.
"The key difference between our model and previous models is that we include heat exchange between water flowing through the ice sheet and the ice," said Rajaram.
As the ice flows towards the coast, grating on bedrock, crevasses and new fractures form in the upper 100 feet of the ice sheet.
The strait’s status in turn affected ocean currents, which affected the rate of ice sheet melting during the last glacial period.
A meltwater lake on the Greenland ice sheet that contained 44 billion litres and covered 5.7 sq km gurgled away within 24 hours in 2006.
The new study showed ice sheets like the Greenland ice sheet can respond to such warming on the order of decades rather than the centuries projected by conventional thermal models.
The 2007 report predicted a sea level rise of 30cm-60cm by 2100, but did not account for the impact of glaciers breaking into the sea from areas such as the Greenland ice sheet.
That is why a team from the National Aeronautics and Space Administration was surprised when they lowered a video camera to get the first long look at the underbelly of an ice sheet in Antarctica.
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In addition, warmer ice sheets are more susceptible to increases of water flow, including the basal lubrication of ice that allows ice to flow more readily on bedrock.
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A relic of the last ice Age, this is one of three great ice sheets in the world.
In the designing and building of ice rinks, the heat loads imposed on ice sheets must be calculated exactly.
The interaction between ice sheet and sloping structure is studied.
According to Straneo, the rapid changes to the ice sheet have taken glaciologists by surprise.
Placea sphere of nuclear waste in a stable ice sheet and it could melt its way down, the ice re-solidifying behind it.
A massive iceberg juts from the stark expanse of an ice sheet as an orange moon looks on in the Bellingshausen Sea near Antarctica.
No one quite knows why glaciers and ice shelves are melting so fast, or how a meltwater lake on the Greenland ice sheet covering six square kilometres could drain away in 24 hours, as it did in 2006.
But whereas the Alps' snowcaps are just deep enough for skiing, Antarctic mountains are swallowed up by their caps, and lie buried beneath an ice sheet that is five kilometers thick.
Ice flows more readily as it warms, so a warming climate can increase ice flows on ice sheets much faster than previously thought, said the study authors.
The ice sheets that cover Greenland and Antarctica now are remnants of this and previous ice ages.
The satellite USES radar to measure its altitude above the ice sheet.
Melt along the southern edge of Greenland's ice sheet is now moving up its northwest coast, a new study shows.
Scatterometer and radiometer image data have a greater spatial and more frequent coverage, albeit at a lower spatial resolution, making these instruments ideal for monitoring the Antarctic ice sheet.
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A 2009 study found that the Greenland ice sheet shed roughly 385 cubic miles of ice over the previous seven years.
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For physicists, the permanent ice sheet will allow them to study mysterious sub-atomic particles that may reveal the very first moments of our universe.
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