I have been noting this myself, the GFSP 00z being perhaps the best reflection so far of what tends to crop up in these situations - as soon as an Atlantic trough becomes negatively tilted, a sharp ridge from the mid-latitudes to the Arctic establishes and we very nearly see some proper blocking take hold to our N and NE - it was a poor time to hit lower-res in that run.
The GFS 06z nearly manages it days 7-8 but then hits lower-res with standard results.
The GFSP 06z sort of does it days 8-10 but it's not a very good effort. Things still turn interesting later on though as the jet digs further and further south (http://modeles.meteociel.fr/modeles/gfsp/runs/2014122706/gfsnh-0-360.png?6)
This signal for a lot of cold spilling into the mid-latitudes and the jet tracking a long way south is to be expected given the mangled state of the strat. vortex in 8 days time:
This should encourage a very ragged or broken-up polar vortex to develop starting about a week from now and it will then be a case of to what extent blocking highs are able to establish and interfere with attempts by the polar vortex to re-organise, and of course where exactly they locate relative to the UK.
Signs are that further warming events will continue to toss the vortex around while this is going on, mostly at the 10 hPa level with the 30hPa level looking more resilient, which will at least keep the vortex in a weakened state, with a reduced ability to drive a westerly flow in the troposphere.
The models will struggle to resolve whatever Arctic blocking establishes, which in turn makes the southward extent of the jet very uncertain from next weekend onward - and of course the track and angle of incoming troughs.
One big difference to early December that the models all agree on is the total absence of high pressure from the Azores to Europe this time around. Though this doesn't establish until day 8 so not a given - but a strong signal.
Originally Posted by: Stormchaser