Press releases

Time to Say Goodbye

The MOSAiC floe’s days are numbered, but Polarstern will continue the expedition further north
Packing up instruments in Met City, which is situated directly next to a melt pond.
Deinstallation of Met City (Photo: Alfred-Wegener-Institut)

After exactly 300 days of drifting with the MOSAiC floe, the international team around Expedition Leader Markus Rex on Wednesday, 29 July 2020, started the dismantling of the research camp and evacuation of the floe. Just one day later the floe finally broke into several fragments. After accompanying the floe on its journey for ten months, the team will now shift its focus to the last remaining puzzle piece in the annual cycle of Arctic sea ice: the start of the ice formation process.

It came as expected: with a loud bang, on 30 July the MOSAiC floe broke into several fragments, which will drift out to the open ocean of Fram Strait within the next few days. Momentarily, the floe fragments are five kilometres apart from the ice edge. But the experts’ timing was flawless: they continued their work with the complete research camp until the very end, before efficiently dismantling it and bringing all their equipment back on board, all within a day. Thereby it was possible to also document the very last phase of the life of the MOSAiC floe as planned - an impressive success for the expedition.

“We’ve successfully monitored the lifecycle of the MOSAiC floe from early October last year to its end. It carried us through the Arctic Ocean for a total of 1700 kilometres, from the Laptev Sea, past the North Pole and all the way to Fram Strait. Here at the sea-ice edge its natural lifecycle comes to an end: the fragments will continue to grow thinner and be broken up by waves, until they ultimately melt and once again become part of the seawater, from which the floe was formed nearly two years ago off the Siberian coast. Accordingly, the concept for the expedition has been completely fulfilled,” says Expedition Leader Prof Markus Rex from the Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research. “Now we’ll focus on the last piece of the puzzle in the annual cycle: the start of freezing at the end of the summer. For this phase we’ll be heading farther north, where the ice formation will soon begin.”

Initially, however, the Polarstern will remain near the ice edge, until the Russian research icebreaker Akademik Tryoshnikov joins her in the near future. The latter ship will bring with her the research team for the last MOSAiC leg, new crewmembers, provisions and fuel, as well as consumables.

On 4 October 2019, following a fairly brief but intensive search, the participants in the MOSAiC expedition allowed their ship to freeze to the floe where they would subsequently erect their research camp for the drift through the Arctic Ocean. Finding the right floe proved to be an enormous challenge, since, after the warmest Arctic summer to date, there were very few floes in the expedition’s starting region that were suitably thick. The one they ultimately chose was formed – as they subsequently discovered – near the New Siberian Islands in December 2018, and had already covered a distance of 2,222 kilometres, following a zigzagging course. Above all, the team valued one exceptionally stable area of the floe, which proved to offer a good location for the research camp. At the same time, other parts of the floe were relatively thin and dynamic, making them good representatives of the ‘new Arctic’; it was precisely this combination that made the floe an outstanding candidate for the planned scientific projects. In the course of the year, storms repeatedly produced new leads and pressure ridges, which at times made the expedition participants’ work much harder. But generally speaking, the floe remained stable to the very end – even during the melting season, when neighbouring ice sheets broke up, one after the other.

“Last autumn we looked for, found, scouted, colonised and investigated our floe from every possible perspective. Ever since, it has been a steadfast, stable basis for our research camp. Over the many months the ice floe has become our home, and we’ll always remember it fondly. But now it becomes water again. The time has come to bid it farewell and head north for the final phase of the expedition,” says Markus Rex.

Contact

AWI Press Office
medien@awi.de

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Packing up instruments in Met City, which is situated directly next to a melt pond.
Packing up instruments in Met City, which is situated directly next to a melt pond. (Photo: Alfred-Wegener-Institut)
Tethered balloon 'Miss Piggy' has regularly been up in the air since autumn 2019. Flying several hundred metres high, sensors can be send up and down to measure radiation, temperature, humidity etc. in the lower atmosphere.
Tethered balloon 'Miss Piggy' has regularly been up in the air since autumn 2019. Flying several hundred metres high, sensors can be send up and down to measure radiation, temperature, humidity etc. in the lower atmosphere. (Photo: Alfred-Wegener-Institut)
Last time 'Beluga' is being taken down, the second tethered balloon and 'Miss Piggy's' big brother, which has been up in the air since spring 2020. Flying several hundred metres high, sensors can be send up and down to measure radiation, temperature, humidity etc. in the lower atmosphere.
Last time 'Beluga' is being taken down, the second tethered balloon and 'Miss Piggy's' big brother, which has been up in the air since spring 2020. Flying several hundred metres high, sensors can be send up and down to measure radiation, temperature, humidity etc. in th... (Photo: Alfred-Wegener-Institut)
Last time beluga is being taken down, the second tethered balloon and 'Miss Piggy's' big brother, which has been up in the air since spring 2020. Flying several hundred metres high, sensors can be send up and down to measure radiation, temperature, humidity etc. in the lower atmosphere.
Last time beluga is being taken down, the second tethered balloon and 'Miss Piggy's' big brother, which has been up in the air since spring 2020. Flying several hundred metres high, sensors can be send up and down to measure radiation, temperature, humidity etc. in the ... (Photo: Alfred-Wegener-Institut)
Lowering a tower in Met City, which has been picked with sensors to study atmosphere-seaice interactions.
Lowering a tower in Met City, which has been picked with sensors to study atmosphere-seaice interactions. (Photo: Alfred-Wegener-Institut)
All teams work together to recover instruments from the central observatory on the ice floe. The so-called ADCP (Acoustic Doppler Current Profiler) for oceanographic measurements has been deployed in the ocean under the ice and is now fixed on a sledge to transport it back home to Plarstern.
All teams work together to recover instruments from the central observatory on the ice floe. The so-called ADCP (Acoustic Doppler Current Profiler) for oceanographic measurements has been deployed in the ocean under the ice and is now fixed on a sledge to transport it b... (Photo: Alfred-Wegener-Institut)
Deistallation of sensors from an instrument of Team Atmos, before bringing it back on board. In the background, people recover the orange power cables, which supplied the central observatory with electricity.
Deistallation of sensors from an instrument of Team Atmos, before bringing it back on board. In the background, people recover the orange power cables, which supplied the central observatory with electricity. (Photo: Alfred-Wegener-Institut)
Remote Sensing Instruments, which measure ice and snow properties, are recovered and brought back to Polarstern.
Remote Sensing Instruments, which measure ice and snow properties, are recovered and brought back to Polarstern. (Photo: Alfred-Wegener-Institut)
The ship's crew helps packing up devices from the central observatory on the ice floe into containers on board Polarstern as we come closer to ice edge.
The ship's crew helps packing up devices from the central observatory on the ice floe into containers on board Polarstern as we come closer to ice edge. (Photo: Alfred-Wegener-Institut)
MOSAiC ice floe during Leg 4, June 30. 2020
Aerial of the MOSAiC ice floe during Leg 4, 30 June 2020. (Photo: Alfred-Wegener-Institut)