I guess that the 2 main factors that will determine remaining melt to minimum are the warmth accumulated in the central Arctic Ocean and the Albedo Warming Potential as it is now combined with the weather for the remainder of the year in the central Arctic.
The attached map suggests that where open water has emerged, positive SST anomalies are high
The 2 months of maximum insolation (May 21 to July 21) have passed. Insolation drops quickly from now on. The AWP as at 22 July is well below that of recent years, and in the High Arctic well below the 2010's average.
It seems to me that despite the very large area of extreme low concentration in the central arctic from the NP to the Laptev at 80 North, the potential for massive sea ice loss is limited.
click images to enlarge
Agree. There should be two ways that would be disatrous for the ice.
1) a bombcyclone over the soup in the next 2, at most 3 weeks, would do massive damage to that ice, especially if warm sea water from Kara-Barents is being pumped up, I.e a reversed dipole of just warm air being transported northward.
2) a continous warm air flow from Kara-Barents might be sufficient to connect a potential polynya with the Atlantic.
Of those two, number 1 would be the worst outcome.
In any ways, the ice is fortune that this nelting season has been one of the weakest for years. The most interesting things for now are:
1) how much of the CAA will melt out?
2) how much of the soup will melt out?
3) how much of the Beaufort and Pacific front will resist melting?
4) will we see a minimum above 5 million wrt NSIDC numbers?