An Azores Low is bound to cause a lot of uncertainty. Usually the models go too far with the conditions for intensification when it's beyond +120 hours away but of course there will always be some that do bomb out.
I remember in late Nov 2010 there was a time when a lot of ensemble members developed large LP to the SW and shoved the cold air away.
Usually, any large trough to the SW will be perturbed by the cold to a great enough extent that a secondary low develops on its NE flank and breaks away E or NE. I reckon the most likely outcome is either that sort of thing or the main low remaining smaller and moving NE in its entirety, much as the ECM 00z does but perhaps not developing as fast (i.e. as far SW from the UK). Both have similar implications for the UK, with a marked warm sector meaning mostly rain for an unlucky number, a snow-rain-snow or rain-snow event for a great many others, and a mostly snow event for the lucky few.
Having said all that, if the weak secondary low shown to the west of the UK in the below-left image doesn't develop or at least is a lot smaller, the door is likely to be shut in the face of that Azores low until a few days later in time. That's the best way forward IMO, as it allows the cold air to become better entrenched ahead of the potential intrusion.
The secondary low is still far enough away in time to be subject to a lot of uncertainty - after all, ECM's the soonest to develop it out of the morning op runs. GFS has no such feature even out to +216, with the Azores Low still trapped by the so-named Islands. The movement NE takes until lower-res, at which point you may as well ask a 3 year old how it will behave.
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