Scientists take sea ice samples out of Polarstern’s mummy chair, which is used to investigate sea ice without actually setting a foot on it.
(Image Credit: Alfred-Wegener-Institute)
The area of sea ice in the Arctic fell to a summer minimum of around 5.0 million square kilometres this year, which is about 1.6 million square kilometres more than the record low in 2012.
According to sea ice physicist Marcel Nicolaus from the Alfred Wegener Institute (AWI) and Lars Kaleschke from the Hamburg Cluster of Excellence for Climate Research (CliSAP) this confirms the long-term downward trend in the Arctic. On the other hand, the winter ice sheet in the South Polar Ocean has expanded to an area of 20.0 million square kilometres, as the researchers report, which exceeds the 30-year-maximum from the previous year. This Thursday, September 18, Marcel Nicolaus, Lars Kaleschke and other leading sea ice experts will be available for discussions and interviews at an international sea ice symposium in Hamburg.
“The current minimum sea ice in the Arctic illustrates the continuation of a long-term downward trend. With an area of 5.0 million square kilometres, the 2014 minimum approximately equals last year’s minimum. This by no means represents a trend reversal in Arctic sea ice developments – despite the fact that the remaining sea ice area is larger than in the two ‘extreme years’ 2007 and 2012,” says sea ice physicist Marcel Nicolaus from the Alfred Wegener Institute Helmholtz Centre for Polar and Marine Research.
Current ice cover middle of September 2014 with an ice free Nordeast Passage compared to the mean extent.
(Graph: Lars Kaleschke/University of Hamburg, Data: Japan Aerospace Exploration Agency AMSR-2; Climatology IFREMER/CERSAT; Background NASA Blue Marble)
In the negative-record years, weather phenomena led to a particularly large reduction in sea ice. “In 2007, a stable high pressure area in early summer resulted in numerous melt pools forming on the ice. They absorbed energy from the sun, which further intensified the melting. In summer 2012, there was exceptional melting on the underside of the ice, and in August that year there was a severe storm, which stirred up the ice. Such extreme weather was largely absent in 2014,” explains Lars Kaleschke from the Hamburg Cluster of Excellence for Climate Research CliSAP.
In the last few weeks, there have been unusually marked regional differences in ice development. For example: In the last two weeks of August, on its way to the region of the undersea mountain chain Alpha Ridge, the German research ice breaker Polarstern was unable to break the ice north of the Canadian Archipelago, while the ice in the Russian Laptev Sea retreated further north than ever before observed by satellites. “In the first days of September, the ice edge in the Laptev Sea was north of the 85th parallel, only about 500 km from the North Pole. In 2006, the distance from the North Pole to open sea was more than more than twice that,” says Lars Kaleschke.
There are currently exceptionally large areas of sea ice in the Antarctic, where the ice sheet generally reaches its spring maximum in September or October. “At the moment, ice covers a sea area of around 20 million square kilometres and therewith exceeds the 30-year-maximum of 19.65 million square kilometres from the previous year. This data backs up our observation that sea ice coverage in the Antarctic has increased in recent years. This is especially true for the Weddell Sea, where we do most of our research,” says Marcel Nicolaus.
However, the researchers do not feel the sea ice situation in the Antarctic can be compared with the conditions in the Arctic, given the differences in their geographical and meteorological circumstances. “Whereas the Arctic Ocean represents a Mediterranean of sorts surrounded by land masses, what we see in the Antarctic is an ice-covered continent surrounded by the Southern Ocean. Here the Antarctic Circumpolar Current limits the maximum sea ice expansion. Wind and waves greatly influence the ice edge – and the amounts of precipitation and glacial meltwater determine the percentage of fresh water, which in turn helps to determine how much sea ice forms in winter,” explains Lars Kaleschke.
The international scientific community is currently discussing a variety of factors as possible explanations for the major expansion of Antarctic sea ice.
Source: Alfred Wegener Institute
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