The ice sheet is made up of layers of compressed snow from more than 100,000 years. It contains valuable climate data from years past. Scientists have drilled ice cores up to 4 kilometres (2.5 mi) deep. These ice cores provide information on past climate factors such as temperature, ocean volume, precipitation, chemistry and gas composition of the lower atmosphere, volcanic eruptions, solar variability, sea-surface productivity, desert extent and forest fires.
During the summer (June to September), about 50% of the ice sheet's surface naturally melts. At high elevations, most of that melt water quickly refreezes in place. The melt water coming from the ice sheet that is near the coastal areas are retained by the sheet and the rest falls into the ocean.
Greenland melting breaks record 4 weeks before season's end
Melting over the Greenland ice sheet shattered the seasonal record on August 8 – a full four weeks before the close of the melting season, reports Marco Tedesco, assistant professor of Earth and atmospheric sciences at The City College of New York.
The melting season in Greenland usually lasts from June – when the first puddles of meltwater appear – to early-September, when temperatures cool. This year, cumulative melting in the first week in August had already exceeded the record of 2010, taken over a full season, according to Professor Tedesco's ongoing analysis.
"With more yet to come in August, this year's overall melting will fall way above the old records. That's a goliath year – the greatest melt since satellite recording began in 1979," said Professor Tedesco.
This spells a change for the face of southern Greenland, he added, with the ice sheet thinning at its edges and lakes on top of glaciers proliferating.
Professor Tedesco noted that these changes jibe with what most of the models predict – the difference is how quickly this seems to be happening.