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The study delves into the multifaceted influence of the Arctic dipole on the Arctic Ocean climate.

UK-based aquaculture start-up sinks biomass bales, as it seeks to prove carbon removal potential of seaweed cultivation

And tidal waves couldn't save the world from Atlantification.

Fairbanks, Alaska (UAF) - New research by an international team of scientists explains what’s behind a stalled trend in Arctic Ocean sea ice loss since 2007. The findings indicate that stronger declines in sea ice will occur when an atmospheric feature known as the Arctic dipole reverses itself in its recurring cycle.

New research by an international team of scientists explains what’s behind a stalled trend in Arctic Ocean sea ice loss since 2007. The findings indicate that stronger declines in sea ice will occur when an atmospheric feature known as the Arctic dipole reverses itself in its recurring cycle. The many environmental responses to the Arctic dipole are described in a paper published online today in the journal Science. This analysis helps explain how North Atlantic water influences Arctic Ocean climate. Scientists call it Atlantification.