This article was produced and financed by The Fram Centre
Declining sea ice is making the Arctic ocean warmer
Changes in the marine environment are causing shifts in ecosystems north of Svalbard.
The Fram Centre
A new study shows that the largest influx of water into the Arctic Ocean takes place in autumn and early winter and that the water is also warmest at this time of year.
Powerful pulses of water warmer than five degrees enter the area at the time of the year when the sea ice should freeze. But even if the air temperature is far below freezing, even during the months without the sun to warm the ground, new sea ice fails to appear.
"Only if the wind helps by blowing ice and fresh surface water from the interior of the Arctic Ocean or from the east will we see an ice cover on the Atlantic influx. We have been watching the ice cover on the Arctic Ocean become significantly thinner in recent years, along with reductions in distribution in time and space. This also reduces the supply of fresh water from the north," says Angelika Renner, an oceanographer at the Marine Research Institute and one of the researchers behind the study.
The mechanism that causes the warm and salty waters from the south to remain below the insulating cold and fresh layer of water in the north appears to have weakened in recent years.
More open waters in the north and east
The new study is part of the Fram Centre's Sea Ice in the Arctic Ocean research program, technology, and influencing systems (Havisen i Polhavet, teknologi og styringssystemer), part of the A-Twain Project.
A research paper was published this summer that shows how the northern Barents Sea is about to shift from an Arctic to an Atlantic climate.
"We see a similar atlantification of the sea to the north and east of Svalbard; less sea ice in the Arctic Ocean leads to less melt-water and thus the warm Atlantic water remains atop the water column for most of the year, staying entirely on the surface. It provides a larger ice-free area north of the Svalbard Archipelago and thinner ice further to the east," says co-author Arild Sundfjord, an oceanographer at the Norwegian Polar Institute.
Sundfjord and Renner point out that the Atlantic influx brings nutrients with it, which are necessary for the growth of phytoplankton and larger organisms such as copepods.
"This allows the fish that feed on such zooplankton to survive further north. So it is not just the physical environment that is changing; the ecosystem is changing as well. Research shows that global warming has sent a number of fish species in the Barents Sea farther northeast, at relatively great speed. We really need to keep our eyes open and monitor what is happening north of Svalbard," says Sundfjord.
Wind also plays an important role in how the sea ice forms. Southwestlies can reinforce the influx of Atlantic water from the south. The wind blows ice and the cold, fresh surface water towards the northeast, which allows for saltier and warmer waters at the surface. At the same time, strong winds help the heat mix more effectively up to the surface and thus can prevent the freezing of ice even at very low air temperatures.
"Northerly winds cause the cold freshwater and ice to be carried south. In some years, this might lead to ice-covered waters quite far south. We saw this in 2014 when the wind brought ice so far south that several of the expeditions to the Marine Research Institute and the Norwegian Polar Institute entered areas that had been ice-free in autumn in recent years," says Sundfjord.
"And we did not need to send temperature gauges very far into the water column before they registered warmer water. There could be ice on the surface and a temperature of seven degrees at a depth of 30 feet in the water column at the same place. The ice cover in 2014 was thus a result of the weather, not the climate. The wind threw the local ice cover over the more extensive climate problems," says Renner.