In the new Sea-Quester project, the university is investigating shallow water and tidal systems dominated by large algae in Svalbard and Greenland. It is an EU project with ten partners led by the Technical University of Denmark, which the EU is fund
<p style="text-align:start"><em>The Antarctic Circumpolar Current plays an important part in global overturning circulation, the exchange of heat and CO2 between the ocean and atmosphere, and the stability of Antarctica’s ice sheets. An international research team led by the Alfred Wegener Institute and the Lamont-Doherty Earth Observatory have now used sediments taken from the South Pacific to reconstruct the flow speed in the last 5.3 million years. Their data show that during glacial periods, the current slowed; during interglacials, it accelerated. Consequently, if the current global warming intensifies in the future, it could mean that the Southern Ocean stores less CO2 and that more heat reaches Antarctica. The study was just released in the journal </em>Nature<em>.</em></p>
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