Tuesday, September 25, 2012

Arctic snow too melting fast

A recent estimate from climate researchers suggested that the melting of Arctic sea ice could result in the warming equivalent of 20 years of CO2 emissions, due largely to the loss of huge swaths of the color white. White reflects light — including sunlight. More white means less absorbed heat. Now it seems not only sea ice but snow on land too is melting at record rate. A study by Canadian researchers finds that springtime snow is melting away even faster than Arctic ice. That also has profound implications for the Earth’s climate.
Springtime snowmelt matters a lot: It determines when spring runoff comes out of the mountain to fill our rivers. And Chris Derksen at Environment Canada in Toronto says snow also reflects sunlight back into space, helping to keep the Earth from heating up too fast.

“When you remove the snow cover form the land surface, much as when you remove the sea ice from the ocean, you take away a highly reflective, bright surface, and you expose the bare land or tundra underneath, and that absorbs more solar energy,” he says.

What’s worse is that the decline of springtime snow is happening faster than that of Arctic ice. The Environment Canada team calculated that snowmelt is declining at 18 percent per decade, compared to 11 percent for the ice cap. And what’s even worse is that the snowmelt is only the first layer of the problem. Beneath the snow is the permafrost, which is no longer as “perma.” Thawing permafrost, as we’ve mentioned before, releases methane into the atmosphere, contributing more to warming than the same amount of carbon dioxide.

Apocalypse in the making?

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