I’ve been looking at Wave Activity Flux once more to try to get a grip of what’s upon the Arctic at present. The circulation seems to rapidly accelerate from the known climatic mean into unknown patterns.
It led me to question how heat would be transferred to the Arctic. I tried to generalize the Rossby Wave patterns, FI like this in ’13:

It resembles mean 10-day positions of ridges and troughs during winter ’12-’13.
Right now the pattern seems stuck around these positions:

In the 3D mental visualization that I’ve learned to make (which is subject to my limited capacities, I’m aware…), the transfer of heat would concentrate on the tips of the ridges.
Following that visualization, I struck on this study:
http://www.meteo.psu.edu/~sbf1/papers/Flournoy_etal_2016.pdfIt describes a mechanism that may very well have influenced the Arctic winter that just ended:
Tropically Excited Arctic Warming (TEAM)Now that sunlight has arrived all over the Arctic, import of large volumes of humid air may have changed into the build-up of that persistent high over the Beaufort sector of the Central Arctic Basin.
And very persistent it is, like the ridging over Western North America, Greenland and the Ural region between Russia and Siberia. Not to speak of the nasty trough over Western Europe, that causes wet, cold weather seemingly without an end over here.
Anyway, let’s keep an eye on proceeding melt/disruption in the Beaufort Sea. But that’s not the only place where this melt season will produce surprises. The ridges over Greenland and the Ural have preconditioned the Labrador Sea/baffin Bay and the Kara Sea.
Expect some rapid extent losses over there next two weeks.