The large changes between the GFS 12z and the previous few runs can be traced back to a southward dip in the jet stream that forms on Friday and hits peak on Saturday. The 12z is just that little bit less pronounced with this Fri-Sat i.e. it keeps the jet flatter (first two images; 06z on left, 12z right).
As a result, less in the way of cool polar maritime air is drawn south (second two images, same relative positions) - note, to the south of Iceland, how much less southward progress the bold 0 isotherm has made.
This in turn means that there is more of a thermal gradient in the vicinity of Iceland, as more cool air is retained to the north of warm air. This leads to a stronger and much more coherent jet heading WSW-ENE to the north of the UK (third two images).
At this point, the stage is set for what follows a good way into the following week; that jet to the north of the UK builds more in the way of high pressure across from the Azores while also preventing as much ridging toward Scandinavia. Not only that, but the Iberian trough has less in the way of cool air to interact with. So, it stays more south, and pressure stays higher across the UK.
With more energy diverted away NE of the UK, and a stronger thermal gradient maintained across the regions north of the UK, the Atlantic trough can't make inroads like it did on the previous runs, even next Friday the main jet is still running north of the UK:
Only with some amplification of the upstream pattern (buckling of the jet) is GFS able to find a way to bring the Atlantic trough more into play for the UK. At this time we reach a new conundrum; this is where tropical forcing could step in at just the right moment to keep any Atlantic trough intrusion brief and limited (as I detailed more this morning), but GFS is clearly not interested at this time (but it does have a bias away from the desired forcing, so it may be worth favouring ECM at that range - but then, that's usually the case anyway ).
Originally Posted by: Stormchaser