For those interested in what happened in the Beaufort, back in 2016 (so as to compare to this year's siutation), I wrote about it extensively on the ASIB. Here's a
blog post from May 21st, with links to previous blog posts in the first paragraph.
One thing I wondered about back then, and do again now:
The other thing is that there is actually not that much ice left between the large polynya (expanse of open water) in the Beaufort Sea and the smaller one in the Chukchi Sea:
Once this ice is gone, there will be open water all along the American coast of the Arctic Ocean. My guess is this could happen within two weeks or maybe even faster, which would be extremely early, given that the earliest time this has happened in the past decade (and probably much, much beyond that), was between July 1st and 7th in both 2009 and 2011.
My guess turned out to be wrong. It also took until the first week of July for open water to take over all along the Alaskan-Canadian coast.
But how about this year? Here's a comparison:
The maps look very similar, so much so that one would be tempted to think there is something causing the ice to stay glued to the coast, all the way up to Utqiaġvik. But there's no "Chukchi polynya" now, with open water all the way to the Pacific and far into the Chukchi, meaning there is less ice to be blown back towards the coast, should the winds turn.
And the winds are another similarity. Both the weather forecast back then and the one this year show a change in the set-up that caused the early Beaufort opening, around the same time. However, this year there may be a return to that set-up next week.
So, wondering if there will be open water all along the Alaskan-Canadian coast before July this year...