Gray Wolf,
1) Is there really any precedent for such a large mass of ice making such a fast progress into the Beaufort / Siberian Regions such that it will be guaranteed to melt out? I don't think so.
2) Thickness levels aren't much down on 2011/2012. Volume is slightly above 2012 same time. Spring volume loss 2012 was the steepest so far, this year will be steeper. April Avg minus Jun Avg gives losses of 6 to 7k km^3 post 2010, and 4 to 5k km^3 pre-2010, 2012 was the greatest loss at 7.03k km^3. However June to Sept losses pre 2010 were of the order of 12 to 13k km^3, post 2010 they have been between 11 and 12k km^3 - i.e. while spring melt has grown by around 2k km^3, later summer losses have dropped by around 1k km^3, making a net increase of 1k km^3 loss throughout the melt season.
So what volume does 1M km^2 extent mean? Well extent is a crap metric, how much area is 1M km^2 extent? For 2012 August Dispersion Index was around 1.6, that's NSIDC EXtent / CT Area.
http://www.flickr.com/photos/54059206@N07/8581338180/#so 1M extent / 1.6 => 0.625M area.
At a finishing thickness for Sept of around 1.1m in 2012: 0.0011*625,000 ~ 700 km^3, lets round that further in your favour and say it only has to get down to 1k km^3. Which gives a closely compacted pack of 1M extent with thickness 1m, any low concentration areas mean you need to lose more volume to get to 1M extent. Given that daily min volume 2012 was 3.261k km^3, this year would need to lose 2.261k km^3 below last year's minimum.
So this year needs to lose 2.2k km^3 more than last year did from max to min volume in order to get to 1M km^2 extent. That's taking into account the extra 1k km^3 spring melt that's already happened due to more FYI since 2010.
Short of a massive meteor impact on the pack, 1M is not possible.