So far today I have been sitting back a bit, as I may be for much of the time 25th-26th depending on how the model output develops.
I see GFSP has shifted a long way toward the ECM/UKMO treatment of the weekend storm system but the motion continues to have too much of an eastward component to get the cold undercut that those two models have.
UKMO's output seems the most promising of the 00z runs, though ECM at day 6 has a very good dig of energy south in the Atlantic and was probably a whisker away from producing a decent continental feed days 7-10; the angle of the jet is just a little too much toward SW-NE.
The GFSP 06z is the most interesting run for a while as far as height rises to our E and NE are concerned, despite lower heights the NW than the ECM run. This is thanks to the jet alignment being just a little more toward S-N on day 6.
The day 8 chart screams 'battleground' but while the Atlantic low does disrupt days 9-10, it refuses to slide SE properly which makes a hash of things. Lower-res then ramps up the Atlantic, though we still see a heavily disrupted low days 11-12, angled SE-NW, which is quite a thing to see on the lower-res charts.
GFS continues to stubbornly pile energy NE which is what we're used to seeing from that model. Perhaps GFSP is showing us the benefits of the upgraded computation... it would be a good time to find out that it has a better clue when handling Scandi Height rises!
It's nice to be landing on familiar ground, with these potential easterlies infamous for teasing us with lengthy cold spells for days on end, with the end result depending on the Atlantic jet over the western half of the North Atlantic tracking far enough south to force the jet to either turn sharply north or continue travelling on underneath the blocking high.
For this purpose, the more low heights we can get down to the Med. this weekend, the better, as that will encourage the jet to power straight on under the blocking high.
Usually we end up with the jet splitting, the balance between the strength going over the block and the strength going under being the difference between a strong block at reasonably high latitude advecting cold east and a suppressed block at lower latitudes giving at best a 'continental whiff'.
For the best alignment of the easterly to get the properly cold air to the UK, a flat jet running underneath is best, unless low pressure development occurs due south of the UK i.e. somewhere from Spain to the Balearic Isles.
On the GFSP 06z there is only the merest hint of that split jet on day 7:
...which almost does the job for us during the following two days, but too much energy curves round to the north as the stronger jet arrives from the east, and curve this is unable to become sharp enough to permit a decent undercut of the Atlantic low pressure.
So as so often happens, we're seeking a reduction in energy going north/northeast, in favour of energy undercutting the blocking high.
These situations usually cause the models to struggle so it's not the best time to for it to turn up given the lower data counts that can be expected over Christmas
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T-Max: 30.2°C 9th Sep (...!) | T-Min: -7.1°C 22nd & 23rd Jan | Wettest Day: 25.9mm 2nd Nov | Ice Days: 1 (2nd Dec -1.3°C in freezing fog)
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