If anything says the situation with the ice, for me, today, it is the mosaic image of the tip of the Laptev bite.
To the left, the rapidly shredding Pacific side. To the right, clockwise, the disorganised and rapidly separating Atlantic side ice encroaching on the Laptev Bite. Just out of image on the right is the large open water area which has been growing steadily over the last two weeks.
The arctic stands poised on a knife edge. Fall off one side and all that open water within the slush and mini floes will freeze and we're heading for the impression that the ice "recovered". Some relatively active storms (no need for GAC's with this mess) and we could be rapidly heading for a record.
As we stand at this cusp all we do know is that every storm will do more damage than the same intensity storm in years/decades past. We do not know if the storms will appear and how strong they will be.
My bet is that all the open water there already will tend to suck the weather systems in and keep driving the loss, rather than 2017 taking a 2011 path and heading for minor loss and a #4/5 level finish.
That one image says to me that we are seeing yet another change in the way things melt and how melt seasons emerge. This should not be a surprise. We could hardly expect the Arctic to keep on losing volume but then carry on melting and responding to heat import events in the same way. It is why even the very best models have issues. Because we can't finely model a system which keeps on changing its responses to the same stimulus.
It is also why a fast moving system does not lend itself to studies which explain the current position in that journey. Studies are funded and carried out based upon existing knowledge of ice dynamics in order to study it in greater detail. Witness Dr Barber and his voyage to study the interaction of MYI north of the CAA, only to find that the ice there only looked like MYI, it responded to force of an ice breaker with less strength than FYI.
Studies on polynya dynamics do tell us that late July/early August open water leads, within the pack, drive more moist and more stormy weather. How that applies to ice which can't form polynia's because there is not enough solid ice to create one, not even slush but thousands/millions of small floes with open water between and the impact on weather events which damage the ice, I expect to be studied and modelled in the next decade when it has become "the norm". Sadly that doesn't help us determine what is going to happen in the next 5 weeks.
So we are back to guessing.
My guess? New record or very, very close.