I don't see ENSO being much of a factor in the overall regime this winter, or if anything, any influences of ENSO would be minimal for us. Given this, IMO, the biggest driver for the winter pattern across North America is going to be totally dominated by the PDO and secondly by short-term influences on the NP/PNA.
At least in terms of SST structure, we are in a rather remarkable negative PDO right now and to the point of where you don't even have the strip of below average SSTs along the west coast of North America from the PAC NW into the Gulf of Alaska.
Now, this could be a great thing and it could be a very bad thing. One big wild card I think will have to do with the Aleutian Low. Despite the -PDO last winter the Aleutian Low was relatively strong (though displaced towards the dateline) and that that didn't help us at all.
One worry I have though is we are going to continue with the theme of very fast flow alot and something more along the lines of zonal (gradient). This would yield another super challenging short and medium range forecasting with models struggling with shortwaves, shortwave interactions, and storm evolution.
A counter would be getting substantial help from the Arctic domain but my worry is much of our source region is going to be flooded with milder (with respect to climo) temperatures so even if we get a "good look Arctic" the delivery of "colder" temperatures is crap.