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Research icebreaker Polarstern begins the Antarctic season

What does it look like below the ice shelf of the calved massive iceberg A68?
Das Forschungsschiff Polarstern des Alfred-Wegener-Instituts verlässt seinen Heimathafen Bremerhaven.
Arial Polarstern in Bremerhaven (Photo: Alfred-Wegener-Institut)

Due to retarded work on the Polarstern the departure is delayed - On Sunday, 11 November 2018, the research icebreaker Polarstern will leave its homeport of Bremerhaven, bound for Cape Town, South Africa. This will mark the beginning of its Antarctic season, in which oceanographic fieldwork in the Weddell Sea, a resupply mission to the Neumayer Station III, and explorations of the Larsen C ice shelf region and the South Shetland Islands are on the agenda. The ship is expected to return to Bremerhaven in June 2019.

An expedition to the Larsen C ice shelf abutting the Antarctic Peninsula will be at the heart of the upcoming Antarctic season. The Peninsula is one of the fastest-warming regions of our planet, which may also explain why first the Larsen A (1995) and later the Larsen B ice shelf (2002) virtually disintegrated, leaving only Larsen C as the last major ice shelf in the western Weddell Sea. In July 2017 the iceberg A68 – with an area of 5,800 square kilometres, one of the largest ever observed – calved from the shelf.

In early February 2019, the Polarstern will set out for this region, departing from Punta Arenas, Chile. More than 50 experts from 17 institutes and five countries hope to precisely catalogue the seafloor landscapes and life forms below the ice shelf. The expedition will be led by Dr Boris Dorschel, a bathymetry expert at the Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research (AWI). In addition to survey work on the seafloor, he will be coordinating the geosciences and biology groups on board, as well as the sea-ice physicists. The expedition members are especially excited to see whether the sea-ice conditions will allow them to reach the Larsen C ice shelf. In the Antarctic summer (February / March) of 2018, the British research ship James Clark Ross sought in vain to penetrate so far south. Some of the biologists who were on board then will now try their luck again, this time on the Polarstern.

The calving of A68 has shifted the shelf front landwards. This retreat has had, and continues to have, a major influence on environmental factors and ecosystems in the area previously covered by the ice shelf. Thanks to the shelf, for up to 120,000 years this area remained untouched by the atmosphere and the effects of sunlight. Yet recent events have opened the door for exchange processes between the ocean and atmosphere, and single-cell algae can now grow in the upper water column. These changes are taking place rapidly, forcing the ecosystems affected to quickly react and adapt. In order to understand these ongoing transformations and the ecosystems’ adaptation mechanisms and robustness, it is imperative that the current conditions be recorded as soon as possible. Given their remote location – the nearest harbour is more than 1,500 kilometres away – there is currently only limited data on Larsen A and B; Larsen C is essentially uncharted territory. Accordingly, the Polarstern expedition PS118 will pursue a highly interdisciplinary approach, its goal being to explore and record the current status and natural diversity of this largely unknown region from a range of perspectives.

Before the ship heads for the southern reaches of the Antarctic Ocean, students from the POLMAR Graduate School will be on board for the transit cruise from Bremerhaven, and will learn how the Polarstern’s on-board echo sounders and sonar systems work. By scanning the seafloor, this equipment can help to find the best location for collecting samples, making it a valuable tool for experts from a range of disciplines. In mid-December the Polarstern will reach Cape Town and take on new expedition members before engaging in long-term oceanographic investigations in the Weddell Sea and resupplying the Neumayer Station III with research equipment, fuel and provisions. Once the voyage to the Larsen C ice shelf is over, there will be a subsequent, geosciences-focused expedition to the South Shetland Islands in April/May 2019. Instructors on board will use the return journey across the Atlantic to offer courses for international oceanography students. The Polarstern is expected to return to Bremerhaven on 29 June 2019.

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Das Forschungsschiff Polarstern des Alfred-Wegener-Instituts verlässt seinen Heimathafen Bremerhaven.
RV Polarstern leaves its homeport Bremerhaven, Germany. (Photo: Alfred-Wegener-Institut)
Treibender Eisberg, umgeben von Meereis, im Weddellmeer

Polarsternexpedition ANT-XXIX/6; 8. Juni - 12. August 2013; Kapstadt-Punta Arenas
Ziel der Expedition: Ein interdisziplinäres Forschungsprogramm in Atmosphäre, Meereis, Ozean und Ökosystem im antarktischen Winter, um die physikalischen und biogeochemischen Eigenschaften und Prozesse während der Wachstumsphase des Meereises besser zu verstehen. Fahrt war die erste antarktische Winterexpedition seit dem Jahr 2006. (Kurs wie im Winterexperiment 1992) 


English

Drifting iceberg in the Weddell Sea, surrounded by sea ice. 

Polarsternexpedition ANT-XXIX/6; 8. June - 12. August 2013; Cape Town -Punta Arenas (Chile); The aim of the cruise is to carry out an interdisciplinary research programm on atmosphere, sea ice, ocean, and ecosystem during winter to obtain an understanding of physical and biogeochemical properties and processes during the sea ice growth season. It was the first Antarctic winter expedition since the year 2006.
Polarsternexpedition ANT-XXIX/6; 8. June - 12. August 2013; Cape Town -Punta Arenas (Chile); The aim of the cruise is to carry out an interdisciplinary research programm on atmosphere, sea ice, ocean, and ecosystem during winter to obtain an understanding of physical an... (Photo: Alfred-Wegener-Institut)
Kühlcontainer werden entladen. Reefer Container are unloaded.
Unloading RV Polarstern to supply Neumayer Station III (Photo: Alfred-Wegener-Institut)
Dies ist ein Tiefsee-Seestern, der im ehemals Schelfeis-bedeckten Larsen A/B Gebiet in flachem Wasser lebt. 200m
Sea star inhabiting the formerly ice shelf covered Larsen A/B area in 200 meteres water depth. (Photo: Alfred-Wegener-Institut)
Antarktisches Meereis, Weddellmeer.


Polarsternexpedition ANT-XXIX/6; 8. Juni - 12. August 2013; Kapstadt-Punta Arenas
Ziel der Expedition: Ein interdisziplinäres Forschungsprogramm in Atmosphäre, Meereis, Ozean und Ökosystem im antarktischen Winter, um die physikalischen und biogeochemischen Eigenschaften und Prozesse während der Wachstumsphase des Meereises besser zu verstehen. Fahrt war die erste antarktische Winterexpedition seit dem Jahr 2006. (Kurs wie im Winterexperiment 1992) 


English

Antarctic sea ice, Weddell Sea.

Polarsternexpedition ANT-XXIX/6; 8. June - 12. August 2013; Cape Town -Punta Arenas (Chile); The aim of the cruise is to carry out an interdisciplinary research programm on atmosphere, sea ice, ocean, and ecosystem during winter to obtain an understanding of physical and biogeochemical properties and processes during the sea ice growth season. It was the first Antarctic winter expedition since the year 2006.
Antarctic sea ice, Weddell Sea. (Photo: Alfred-Wegener-Institut)
Scotoplanes globosa, a deep-sea sea cucumber found in shallow waters in the former Larsen B ice-shelf area, taken during the Polarstern cruise ANTXXIII-8.
Scotoplanes globosa, a deep-sea sea cucumber found in shallow waters in the former Larsen B ice-shelf area, taken during the Polarstern cruise ANTXXIII-8. (Photo: Alfred-Wegener-Institut)
Diese Tiefseeseegurken sind im Larsen B Gebiet auffallend häufig. Interessanterweise laufen sie allen in dieselbe Richtung. 

These deep-sea sea cucumbers are abundant in the Larsen B area. Interestingly they are all heading in the same direction.
These deep-sea sea cucumbers are abundant in the Larsen B area. Interestingly they are all heading in the same direction. (Photo: Alfred-Wegener-Institut)
Im Larsen B Gebiet gibt es in ungewöhnlich großer Tiefe von ca. 120m blanken Felsen. Korallen gibt es nicht nur in den Tropen und bei 800m Wassertiefe vor unserer europäischen Küste; sondern auch hier in der Antarktis.

In the Larsen B area at unusual great water depths of approx. 120m pure bed rock exists. Corals are not only existant in warm tropical waters and along the continental slopes of the Atlantic but also at this site in the Antarctic.
In the Larsen B area at unusual great water depths of approx. 120m pure bed rock exists. Corals are not only existant in warm tropical waters and along the continental slopes of the Atlantic but also at this site in the Antarctic. (Photo: Alfred-Wegener-Institut)
Containerentladung. container unloading
Unloading RV Polarstern to supply Neumayer Station III (Photo: Alfred-Wegener-Institut)
de: Teilausschnitt der Abbruchkante des Larsen-B-Schelfeises an der Antarktischen Halbinsel. Aufgenommen auf der Polarstern-Expedition ANTXXIII/8 im Weddellmeer 2006/07. <br />
en: Part of the broken conection between Larsen-B-Iceshelf and the Antarctic peninsula. The picture was taken during the RV 'Polarstern'-expedition ANTXXIII/8 in the Weddell Sea 2006/07
Part of the broken conection between Larsen-B-Iceshelf and the Antarctic peninsula. The picture was taken during the RV 'Polarstern'-expedition ANTXXIII/8 in the Weddell Sea 2006/07 (Photo: Alfred-Wegener-Institut)
de: Gletscher bei Larsen A <br />
en: Glacier at Larsen A
Glacier at Larsen A in 2007 (Photo: Alfred-Wegener-Institut)
Antarctic Landscape (Photo: Alfred-Wegener-Institut)
Pelagic net sampling. (Photo: Alfred-Wegener-Institut)
Dieser antarktische Polarfisch (Trematomus sp.) nutzt einen Glasschwamm als Versteck. Foto: Thomas Lundaelv, Alfred-Wegener-Institut


ROV-Aufnahmen von GlasschwŠmmen (Bodenbewohnern) im westlichen Weddellmeer (ehemaliges Larsen-A-Schelfeisgebiet), aufgenommen waehrend der Polarstern-Expedition ANT-XXVII/3; 

Dazugehoerige Veroeffentlichung: Fillinger, L; Janussen, D; LundŠlv, T et al. (2013): Rapid glass sponge expansion after climate-induced Antarctic Ice Shelf Collapse. Current Biology

Over 30 percent of the Antarctic continental shelf is permanently covered by floating ice shelves, providing aphotic conditions for a depauperate fauna sustained by laterally advected food. In much of the remaining Antarctic shallows (<300 m depth), seasonal sea-ice melting allows a patchy primary production supporting rich megabenthic communities dominated by glass sponges (Porifera, Hexactinellida). The catastrophic collapse of ice shelves due to rapid regional warming along the Antarctic Peninsula in recent decades has exposed over 23,000 km**2 of seafloor to local primary production. The response of the benthos to this unprecedented flux of food is, however, still unknown. In 2007, 12 years after disintegration of the Larsen A ice shelf, a first biological survey interpreted the presence of hexactinellids as remnants of a former under-ice fauna with deep-sea characteristics. Four years later, we revisited the original transect, finding 2- and 3-fold increases in glass sponge biomass and abundance, respectively, after only two favorable growth periods. Our findings, along with other long-term studies, suggest that Antarctic hexactinellids, locked in arrested growth for decades, may undergo boom-and-bust cycles, allowing them to quickly colonize new habitats. The cues triggering growth and reproduction in Antarctic glass sponges remain enigmatic.
Antarctic fish (Trematomus sp.) uses a glass sponge to hide. (Photo: Alfred-Wegener-Institut)