Greenland Meltwater Contributes To Rising Sea Levels

2015-01-15T17:41:19+00:00 January 15, 2015|
A new study reveals a vast network of little-understood rivers and streams flowing on top of the ice sheet in Greenland that could be responsible for at least some of the world's sea-level rising. (Credit: Christine Zenino)

(Click to enlarge) A new study reveals a vast network of little-understood rivers and streams flowing on top of the ice sheet in Greenland that could be responsible for at least some of the world’s sea-level rising. (Credit: Christine Zenino)

As the largest single chunk of melting snow and ice in the world, the massive ice sheet that covers about 80 percent of Greenland is recognized as the biggest potential contributor to rising sea levels due to glacial meltwater.

(From ScienceDaily)– Until now, however, scientists’ attention has mostly focused on the ice sheet’s aquamarine lakes — bodies of meltwater that tend to abruptly drain — and on monster chunks of ice that slide into the ocean to become icebergs.

But a new study involving City College of New York scientist Marco Tedesco and a UCLA team reveals a vast network of little-understood rivers and streams flowing on top of the ice sheet that could be responsible for at least as much, if not more, sea-level rise as the other two sources combined.

“It’s the world’s biggest water park, with magnificent and beautiful — but deadly — rushing blue rivers cutting canyons into the ice,” said Laurence C. Smith, the study’s lead author and the chair of UCLA’s geography department.

The group also specifically examined the Isortoq River, which exits the ice sheet on land and drains about one-fifth of the mapped networks. Its output is critical because it’s a key element of the Modele Atmospherique Regional, or MAR, a climate model used by the Intergovernmental Panel on Climate Change to develop worldwide responses to global warming. The researchers found that the Isortoq’s amount of discharge was more than 25 percent less than the model predicted.

Read the full article here: http://www.sciencedaily.com/releases/2015/01/150113111621.htm