A researchteam with scientist from UNIS and the Bjerknes Centre for Climate Research found the coldest surface water ever measured in the Arctic.

In a review article of available evidence published in Quaternary Science Reviews professor Atle Nesje at the Bjerknes Centre for Climate Research shows how climate variations led to considerable fluctuations in numerous glaciers in Scandinavia since the last ice age.

A recent paper shows that newly generated deep water is organized in large, subsurface vortices. It explains how newly formed deep water is exported from the generation region, and why the vortices observed have appeared rather locked to the observed position.

In a newly published study scientists reveal how the deep water that exits the Nordic Seas is transported from the source region, which is tightly controlled by the bottom topography.

In a new publication in Climate Dynamics, Bjerknes researchers apply a new method in order to improve the spatial and temporal resolution in an atmospheric dataset over the last 40 years.

In a new research paper published in Journal of Paleolimnology Bjerknes researchers show the changes in the reconstructed mean July temperatures (Tjul) during the last 2000 years in northern parts of Fennoscandia and the Kola Peninsula.

In a new study in the distinguished science magazine Nature, scientist from the Bjerknes Center for Climate Research in collaboration with international partners, reject earlier concern about a weakened Gulfstream.

The sea-ice transport in the Arctic was crucial for 2007 and its alltime low ice cover. The contribution from the warm water transport in the ocean was on the other hand modest. This is shown in a new study from the Bjerknes Center for Climate Research, which was published in Geophysical Research Letters.
 

A new paper in Nature shows that the predicted increase in organic carbon supply to the Arctic Ocean, due to global warming, may reduce the oceanic sink for atmospheric carbon and reinforce the predicted atmospheric CO2 increase.

In a new article, published in Advances in Atmospheric Sciences and written by Odd Helge Otterå at the Nansen- and Bjerknes Centre, a numerical atmospheric general circulation model, ARPEGE, is used to simulate the climate changes following the volcanic eruption on Mount Pinatubo on June 15th 1991.