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Scientific study describes the nursery of sea ice and provides the basis for future assessments of research data

Scientific study describes the nursery of sea ice and provides the basis for future assessments of research data


Following the arrival of a new research team in June, study of the Arctic MOSAiC ice floe is continuing apace and the team behind the project has now published a paper on its findings to date in scientific journal The Cryosphere.

Among the findings is the observation that the New Siberian Islands were the birthplace of the MOSAiC floe: the sea ice in which the research vessel Polarstern is now drifting through the Arctic was formed off the coast of the archipelago, which separates the East Siberian Sea and the Laptev Sea to the north of Siberia, in December 2018.

Sediments, and even small pebbles and bivalves, were incorporated into the ice during the freezing process, which the ongoing melting process has brought to light on the surface of the MOSAiC floe. According to the paper, this is an increasingly rare phenomenon as nowadays most of the “dirty ice” melts before it even arrives in the Central Arctic.

In the paper, the team said of the evidence, “At first glance, it looks like a group of people with dirty shoes had left tracks all over the snow.” But in reality, the team stated, these are sediments, and small pebbles and bivalves, that the melting process has exposed. When the sea ice formed, they were frozen inside; they hail from the nursery of sea ice along the Siberian Shelf, which the project’s experts have now used a combination of model simulations and satellite data to describe in detail.

According to the research team, the MOSAiC floe had already drifted over 1,200 nautical miles in a meandering course when the research icebreaker Polarstern moored to it on October 4, 2019, at the coordinates 85° north and 137° east, and began to drift with it through the Arctic Ocean. While the current expedition team is busy taking readings in the Arctic, their colleagues back at home are analyzing the data gathered through the end of 2019 and early 2020.

“Our assessment shows that the entire region in which the two ships looked for suitable floes was characterized by unusually thin ice,” reported Dr Thomas Krumpen, a sea-ice physicist at the Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research (AWI).

Last autumn, Krumpen coordinated research activities on the Russian icebreaker Akademik Fedorov, which accompanied the flagship of the MOSAiC expedition, the Polarstern, for the first few weeks. The Akademik Fedorov was also instrumental in deploying monitoring stations at various locations across the MOSAiC floe – collectively referred to as the ‘Distributed Network’.

“Our study shows that the floe we ultimately chose was formed in the shallow waters of the Russian shelf seas in December 2018,” Krumpen explained, noting that off the coast of Siberia, strong offshore winds drive the young ice out to sea after it forms. In the shallow water, sediments are churned up from the seafloor and become trapped in the ice. Ice formation can also produce pressure ridges, the undersides of which sometimes scrape along the seafloor. As a result, stones can also become embedded in the sea ice. Now that the summertime melting has begun, all of this material is being revealed at the ice’s surface.

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“At several points we’ve found entire mounds of pebbles measuring several centimeters in diameter, plus a number of bivalves,” reported MOSAiC expedition leader Prof. Markus Rex directly from the Arctic with the current research team. Now back in Bremerhaven, Germany, Krumpen is thrilled to see that the now emerging ‘bivalve ice with pebbles’, as he has affectionately dubbed it, so clearly confirms the study’s findings.

The team of authors led by the AWI experts used a combination of satellite imagery, re-analysis data and a newly developed, coupled thermodynamics backtracking model to reconstruct the floe’s origins. Now Krumpen and his colleagues are devising a strategy for gathering samples of the sediments.

The extent to which these ‘dirty’ and therefore darker patches accelerate melting on the floe is an important question, and answering it could enhance understanding of the interactions between the ocean, ice and atmosphere, of biogeochemical cycles, and of life in the Arctic in general.

The group said that, in addition to mineral components, the sea ice also transports a range of other biogeochemical substances and gases from the coast to the central Arctic Ocean. They are an important aspect of MOSAiC research on biogeochemical cycles, i.e., on the formation or release of methane and other climate-relevant trace gases throughout the year.

However, as a result of the substantial loss of sea ice observed in the Arctic over the past several years, this ice, which comes from the shallow shelves and contains sediments and gases, is now melting more intensively in the summer, causing this material transport flow to break down.

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