• Six to ten million years ago: Ice-free summers at the North Pole

    have managed to open a new window into the climate history of the Arctic Ocean. Using unique sediment samples from the Lomonosov Ridge, the researchers found that six to ten million years ago the central Arctic was completely ice-free during summer and sea-surface temperature reached values of 4 to 9 degrees Celsius. In spring, autumn and [...] new findings from the Arctic region provide new benchmarks for groundtruthing global climate reconstructions and modelling.

  • The Arctic is facing a decline in sea ice that might equal the negative record of 2012

    Arctic sea ice
    Sea ice physicists from the Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research (AWI), are anticipating that the sea ice cover in the Arctic Ocean this summer may shrink to the record low of 2012. The scientists made this projection after evaluating current satellite data about the thickness of the ice cover. The data show that the arctic sea ice was already extraordinarily thin in the summer of 2015. Comparably little new ice formed during the past winter. Today Dr

  • New equipment for the AWI - "Gardener"

    RV Polarstern starts the Arctic season
    Scientists from the Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research (AWI) are setting out with [...] towards Spitsbergen, to use newly developed equipment in the Arctic Ocean. Autonomous instruments on the seabed, in the water column and in the air will complement the long-term measurements of the [...] In this way researchers can analyse the climatic changes in the Arctic and their impact on the fauna in the future with higher temporal and spatial resolution.

  • We are on the way – finally!

    2016 we set sail for the long passage from Bremerhaven to the Arctic. We, that is 45 crew members and a total of 51 scientists, engineers, technicians and students with the common goal to conduct [...] in the atmosphere, the water column and at the seafloor of the Arctic Ocean.

  • PS101 KARASIK

    and sources of hydrothermalism at Gakkel Ridge of the Central Arctic. Such integrated studies of ultraslow oceanic spreading zones are rare, because the most extensive of these systems, the Arctic

  • Open waters around the North Pole: Arctic sea ice in retreat

    Arctic Ocean
    This September, the Arctic sea ice extent has shrunk to 4.1 million square kilometres (sq km)-the second lowest in the [...] sq km in 2012. "Once again, a massive loss of sea ice in the Arctic," says Prof. Lars Kaleschke from Universität Hamburg's Center for Earth System Research and Sustainability (CEN). His colleague Prof

  • Ice algae: The engine of life in the central Arctic Ocean

    live in and under the sea ice play a much greater role for the Arctic food web than previously assumed. In a new study, biologists of the Alfred Wegener Institute, Helmholtz Centre for Polar and Marine [...] carbon from these algae. This also means that the decline of the Arctic sea ice may have far-reaching consequences for the entire food web of the Arctic Ocean. Their results have been published online

  • Great potential for comprehensive monitoring of the water masses in the ocean

    Arctic Ocean
    More melt water is entering the Artic Ocean from the glaciers due to climbing temperatures. In addition, the rivers are carrying large amounts of sediment from thawing permafrost. How the Arctic Ocean will react to such changes is a very big question, which is concerning scientists around the world. Researchers from the Alfred

  • New tools and concepts to observe the changing Arctic Ocean

    several new types of instrumentation for the observation of ice, ocean and seafloor processes in the Central Arctic. A main aim is to observe and analyse the changes in the sea ice cover, and its causes and consequences for ocean and life.

  • Week 6: From East Svalbard towards the deep Arctic Ocean

    zone east of Svalbard, and then set course north into the central Arctic Ocean.The marginal sea ice zone was mostly covered with decaying sea ice and some larger ice-free areas. On this side of Svalbard