11. January 2019
In order to arrive at a better understanding of the processes at work, as well as the seasonal and interannual changes in the fast ice of Atka Bay, sea-ice measurements have been taken there on a regular basis since 2010. The fast ice in Atka Bay is predominantly seasonal. The routine measurements in Atka Bay are taken by the overwintering team at the Neumayer Station from early spring to the thawing of the bay in January / February. Essentially, they gather measurements of snow, fast-ice and platelet-ice thickness along a uniform 24-km transect that covers the entire bay from west to east. Read more here ...

19 November 2018
“The demand for reliable forecasts that describe the evolution of the sea ice from days to months in advance has substantially grown in the last decades,” explains Lorenzo Zampieri –a PhD student at the Alfred Wegener Institute’s Young Investigator Group Seamless Sea Ice Prediction (SSIP). The prediction of Arctic sea ice extent and sea ice edge is by now a major challenge but is increasingly in demand in traditional forecasting systems. Read more here...

6 November 2018
“This year, the autumnal rebound in the size of sea-ice cover has been a very slow process; as a result, we’re still at a very low level. Possible causes include the continued warm atmospheric temperatures during the past several weeks, and the residual heat stored in the ocean,” explains Professor Christian Haas, head of the sea-ice physics section at the AWI. Read more here...

13 September 2018
“We are approaching this year’s minimum sea-ice extent in the Arctic, and this summer the ice concentration has descreased to its lowest value since observations started, in 1979,” according to Professor Christian Haas, Head of the Sea Ice Physics Section at the AWI. The absolute minimum will probably be 4,4 ± 0.1 million km². “Due to uncertainties resulting from the different analysis methods, there can be slight discrepencies between the values from different data centres.” Read more here…

30 August 2018
The ice north of Greenland is particularly thick, several years old and is mainly formed on the Russian continental shelf. The Transpolar Drift – which acts like a transarctic conveyor belt – transports the sea ice over a few years to the coast of Greenland. Here, the landward drift compresses the pack ice, creating the compact ice cover typical for the region. The following explains which processes are responsible for the formation of ice-free zones north of Greenland in summer, and why the ice concentration was particularly low this year. Read more here…

22 August 2018
After the sea-ice extent in the Arctic showed a moderate loss, hovering in the lower portion of the double standard deviation range from the long-term average with in the first half of July, the retreat significantly accelerated in the second half of the month. In terms of the monthly average, July 2018 was characterised by a higher sea-ice extent than last year in the Pacific sector (Chukchi Sea and East Siberian Sea), but a significantly lower extent in the Atlantic sector. More here…