Wednesday, August 29, 2018

'Archived' Heat Could Melt Entire Arctic Sea-Ice Pack

Arctic sea ice isn’t just threatened by the melting of ice around its edges, a new study has found: Warmer water that originated hundreds of miles away has penetrated deep into the interior of the Arctic.

That “archived” heat, currently trapped below the surface, has the potential to melt the region’s entire sea-ice pack if it reaches the surface, researchers say.

The study appears online Aug. 29 in the journal Science Advances.

“We document a striking ocean warming in one of the main basins of the interior Arctic Ocean, the Canadian Basin,” said lead author Mary-Louise Timmermans, a professor of geology and geophysics at Yale University.

Heat trapped below the surface has the potential to melt the Arctic region's entire sea-ice pack if it reaches the surface
A heat map of the Arctic interior
Credit: Yale University

The upper ocean in the Canadian Basin has seen a two-fold increase in heat content over the past 30 years, the researchers said. They traced the source to waters hundreds of miles to the south, where reduced sea ice has left the surface ocean more exposed to summer solar warming. In turn, Arctic winds are driving the warmer water north, but below the surface waters.

“This means the effects of sea-ice loss are not limited to the ice-free regions themselves, but also lead to increased heat accumulation in the interior of the Arctic Ocean that can have climate effects well beyond the summer season,” Timmermans said. “Presently this heat is trapped below the surface layer. Should it be mixed up to the surface, there is enough heat to entirely melt the sea-ice pack that covers this region for most of the year.”

The co-authors of the study are John Toole and Richard Krishfield of the Woods Hole Oceanographic Institution.

The National Science Foundation Division of Polar Programs provided support for the research.


Contacts and sources:
Jim Shelton
Yale University
Citation: Warming of the interior Arctic Ocean linked to sea ice losses at the basin margins.
Mary-Louise Timmermans, John Toole, Richard Krishfield. Science Advances, 2018; 4 (8): eaat6773 DOI: 10.1126/sciadv.aat6773

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