In the preceding post on Global sea ice minimum records getting broken for the third year in a row, I mentioned how the situation on the Pacific side of the Arctic was quite unprecedented, with the sea ice graph for the Bering Sea showing a sharp downturn (and even a small one for the Chukchi Sea). Well, there's an equally unprecedented event taking place on the Atlantic side of the Arctic as well. Yesterday, Prof. Dr. Lars Kaleschke from the University Hamburg tweeted out the following:
There is open water north of #Greenland where the thickest sea ice of the #Arctic used to be. It is not refreezing quickly because air temperatures are above zero confirmed by @dmidk's weather station #KapMorrisJesup. Wacky weather continues with scary strength and persistence. pic.twitter.com/YMnvCD8XvL
— Lars Kaleschke (@seaice_de) February 25, 2018
This probably has a lot to do with the splitting of the Polar Vortex due to a sudden stratospheric warming event a while back. I'm grateful for a bit of winter, finally, in my neck of the European woods, but not too happy about the consequences for the Arctic. The cause of all this heat and ice being pushed away from the northern coast of Greenland is an atmospheric set-up that during summer we'd be referring to as a Reverse Dipole (low pressure over the Canadian side of the Arctic, high pressure over the Siberian side). This animation of DMI SLP maps shows how the set-up got set up in the past 10 days, resulting in a pressure gradient as high as 75 hPa:
Such a pressure gradient means lots of winds. The animation in Kaleschke's tweet shows what happened to the ice between Fram Strait and the Lincoln Sea, but here are two images by ASIF commenters Uniquorn and A-Team showing the situation (from the 2017/2018 freezing season thread):
Recent Comments