Thank you for the analysis Stephan.
As the extent maximum is determined by the peripheral seas, mainly the "four Bs" Baffin, Barents, Bering and (B)Okhotsk which have high variability, it is not surprising that years with low extent have a higher probability to grow further at this time.
Regarding the ice thickness distribution, it is a great mystery that can never be resolved without detailed local measurements. I find it rather surprising and gratifying that CS2SMOS and PIOMAS are in such agreement as to the location of the main bulk, though PIOMAS adds some significant hotspot on the Siberian coast and in the Beaufort. Hycom is indeed quite different, my current tendency is to take CS2SMOS as the more probably correct representation of reality, but this is just layman intuition. And indeed the increased mobility of the ice plus its purported location in a region quite easily exportable is a cause for grave concern. Hopefully the Arctic will avoid the export regime of last year around this time, or a large region of thick ice will be lost before anyone can find out if it's really there or not.
Maybe the ensuing melting season will reveal where the ice was thicker or thinner than claimed by the various sources, should a certain region disappear in a flash or persist much longer than it should. I vividly recall Big Block persisting in the Beaufort in 2016 for months only to disappear on the last days of the season, proving beyond a doubt its high original thickness and age.