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History of the Petermann Glacier

... north-western sector of the Greenland Ice Sheet into the Petermann Fjord. It is an active glacier with an ice stream that extends into the fjord as a floating ice tongue, also known as an ice shelf. The ice tongue appears to be thinning and ...

Cruise report

Radar for measuring sea ice thickness

Radar antennas on board Oden. The icebreaker Frey is visible in the background. Photo: Per Holmlund Vessels that sail in ice-covered areas disturb the sea ice and trigger a number of processes. The vessel may break the ice sheet into ...

Cruise report

Navigating in sea ice with the help of satellite images

... Hanna Hagelin The ice has a major bearing on how vessels in both the Bay of Bothnia and the Arctic choose to navigate during the season when the sea is covered by ice. Choosing to sail in areas of open water or thin ice makes it possible ...

Cruise report

How is climate change affecting Arctic biodiversity?

Nedim Curic, Lucy Naud and Lukas Scholtz going through the sample protocols, Abisko Scientific Research Station is seen in the background. Photo: Fredrik Daleru We believe that global warming will contribute to a northerly ...

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First Steps to and from the Water – Part 2

Searching for Ichthyostega bone fragments near the summit of Celsius Bjerg. Photo: Benjamin Kear Vertebrates first emerged onto land during the Devonian 358 million years ago. 108 million years later in the earliest Triassic, ...

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Early Career Scientists Programme 2016

In conjunction with the Swedish-Canadian research expedition Arctic Ocean 2016, the Swedish Polar Research Secretariat invited researchers in the early stages of their careers to participate in the expedition under the auspices of the ...

Cruise report

Who has the rights to the seabed resources in the Arctic Ocean?

... icebreaker Oden in the Arctic Ocean. Photo: Åsa Lindgren The appearance and structure of the seabed can reveal a great deal about the history of our planet. It is the movement of the continental plates that has shaped the polar regions as ...

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