German icebreaker back from research trip to better understand Arctic ice

By Eilis Quinn

The goal of the trip was to better understand how ice conditions, water layering and fluxes in heat influence melt, and how climate change is impacting the Arctic. The focus was on the marginal ice zone, the area between open water and sea ice edge, north of Svalbard, the Norwegian Arctic archipelago.

The researchers had left in June, at the beginning of the annual sea-ice melt.

“One of the greatest successes while taking measurements in the ice zone was the first-ever deployment of the TOP-AWI sensor platform below the sea ice, which allowed us to document the interplay of sea-ice cover, ocean stratification, nutrient and plankton distribution at unprecedented resolution,” Torsten Kanzow, expedition leader and a physical oceanographer at the Alfred Wegener Institute, Helmholtz Center for Polar and Marine Research, said in a news release.

Recovery of the towed sensor platform TOP-AWI in dense sea ice. Photo: Alfred-Wegener-Institut

Ice buoys were also used in the marginal ice zone to better understand changes to the ice floes.

“It was impressive to see how, at one station, the swell from the open ocean came in, and how the floe we were working on moved in time with the waves, and ultimately broke into pieces beneath our feet,” Kanzow said.

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“Later, from the ship we could see that the sea ice floe over a wide range of our working area had suffered the same fate. We posit that the erosion of sea ice in the marginal ice zone, produced by the swell, has a major effect on ice melting, and on the ecosystem connected to the sea ice.”

Looking at Greenland’s glaciers

In the late portion of the trip, researchers traveled to Greenland.

They first went to northeast Greenland to examine how Atlantic water circulation was affecting glaciers in the region, but were hampered by weather conditions.

“The combination of a stable barrier of fast ice off the coast and permanent fog made taking measurements near the glaciers impossible – both from the ship and by helicopter – the teams still succeeded in characterizing the oceanic inflow of warm water,” the Alfred Wegener Institute said in a news release.

A view of an ice floe during a floe station on the PS131. Photo: Christian Haas / Alfred Wegener Institute

The last leg of the trip saw the Polarstern head to Scoresby Sound, a fjord system, in eastern Greenland, so researchers could collect observatories that have been collecting data from the bottom of the fjord system for four years.

Maps, photos and other information related to the Polarstern’s voyages can be seen at the Follow-Polarstern link on the Alfred Wegener Institute website.


This story is posted on the Barents Observer as part of Eye on the Arctic, a collaborative partnership between public and private circumpolar media organizations.

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