The Beaufort stands out. This melting season which is quite aggressive everywhere else has left the region with very high area, second only to 2013 in the AMSR2 record. PIOMAS also indicates high volume. Normally the Beaufort loses a lot of ice due to transport towards the Chukchi, compensated by some thicker ice arriving from the CAB and the CAA. This year the westward transport has been very muted, while the in-situ melting in the Beaufort is not enough to generate open water this early in the season. Thus the positive feedback loop of open water soaking up the sun's energy and leading to more open water is much weaker this year. At the same time, the Chukchi has been running rather high as well, the western CAB shows no special signs of weakness, and the CAA ice is unbroken in the main channels. So while import from the CAB is expected to increase in the coming days due to the anti-cyclone, export doesn't have too many open outlets and will probably continue to be low.
This can change if the CAA breaks up very early and a "garlic press" export begins, or the Chukchi ice crashes making room for import from the Beaufort, or the in-situ melting reaches a critical threshold, maybe with the help of some storm.
But in general I am predicting a high Beaufort area at the end of the melting season, probably over 100k km2 and not close to zero as most years. The only year that managed to get from a similarly high point on this date to near-zero was 2015, all other low minimum years were also much lower on this date. 2019 and 2016 had 200k km2 less area on this date, a very large difference.
Note: numbers based on Wipneus, using the smaller "CT" Beaufort region.