Arctic turns green as sea ice melts to record low levels

The pristine white of the Arctic is turning green because massive blooms of plankton can grow beneath the thinning sheets of sea ice, according to a new study.

The phenomenon was first noticed in 2011 and was something of a surprise as it had been believed that the water beneath the ice was far too dark for plants to photosynthesize.

But now researchers have established the reason the plankton can flourish in such a usually alien environment is that rising temperatures have melted the ice to the point where light can pass through.

The green shows the area of sea ice where plankton is able to grow (Christopher Horvat)

After developing a mathematical model, they concluded about 30 per cent of the Arctic sea ice is thin enough for this to happen, compared to just three to four per cent only 20 years ago, they reported in the journal Science Advances.

In addition to the thinning of the ice, large pools of water have been forming on the surface, which help the sunlight get through the normally impenetrable ice.

Sea ice has been at record low levels for much of this year with 14.1 million square kilometres on 28 March, compared to the average between 1981 and 2010 of 15.4 million at the same time of year.

The Arctic has seen astonishing rises in temperatures over the last few decades with Spitsbergen experiencing winters of up to 11 degrees Celsius warmer than the average between 1961 and 1990.

One of the researchers, Dr Chris Horvat, of Harvard University, said: “Our big question was how much sunlight gets transmitted through the sea ice, both as a function of thickness, which has been decreasing, and the melt pond percentage, which has been increasing.

“What we found was that we went from a state where there wasn’t any potential for plankton blooms to massive regions of the Arctic being susceptible to these types of growth.”

The thickness of sea ice in the Arctic has reduced by an average of about a metre in the past 30 years.

And Dr…

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