Watching how the U.S. trough moves, ECM would most likely go on to be similar to GFSP but the flattening upstream would take a bit longer to occur as the LP hasn't made it as quite as far toward Greenland as of day 10.
Anyway, I reckon the real issues lie with the behaviour of the jet stream in the 5-7 day range.
You see, GFSP is consistently going for the jet riding up the western side of the mid-Atlantic ridge with no real attempt to cut underneath it (see below-right, little in the way of LP to the south of the ridge). This results in a huge meander in the jet which on our side favours a push of low heights into Europe from Scandinavia.
The ECM and GFS models insist otherwise - they have the jet undercutting, with lows developing SW of the UK (ECM above-left, with notable LP development south of the ridge). This is great for getting a proper cut-off high over Greenland which can draw a lot of deep cold air south toward the UK... but that's of little use if the LP to the SW develops too rapidly and tracks too far north (stronger lows typically track further north).
The GFS 12z was kind enough to keep the first LP from the SW as a weak feature until reaching the UK, with rapid development as it crosses our lands. This results in a sequence of events that's far from ideal but could easily deliver a widespread rain-snow event (I'm not taking the precipitation charts at all seriously at that range).
The ECM 12z is a tale of poor fortunes, as the weak LP on it's way over from the SW meets with a shortwave in the cold, unstable northerly flow that just happens to be in the right place at the right time for the two systems to interact in the most unfavourable way that could be achieved - the low from the SW being drawn on a more northerly track, but also fails to absorb the shortwave which is left out west of the UK on day 10, interfering with the cold air mass. Beyond day 10, the next LP to the SW is positioned right for following a track further south but it's questionable whether there would be enough cold air to our N and NW for a snow event across the SE'rn half of the UK.
Now it is true to say that the earlier phasing of the Atlantic and Scandi lows on the GFS and GFSP runs does help to bring more of the cold air our way within the 10 day range, but I think this mid-Atlantic jet stream issue is far more important. The GFSP 00z had the slower phasing and that worked out just fine.
Speaking of which, something between that run and the GFSP 06z is what the UKMO 12z op run bears close resemblance to for day 6. Going by the positioning of LP, the jet beneath the mid-Atlantic ridge appears to be weaker and further south than what ECM has.
GEM's a curious case, developing LP to the SW as early as day 6 but then whizzing that NE and going down a line more like the GFSP 12z from that point onward.
JMA offers it's own variation on the theme in which the Scandi trough digs south by day 8, while the jet thinks about undercutting but then seems to change its mind:
Posted just for fun as it's among the best charts on offer for Christmas Day synoptically, though the magnitude of the cold conditions is nothing to write home about on the day itself.
I suppose what we have is GFSP and GEM versus ECM and GFS with UKMO and JMA somewhere in the middle. Typical of highly uncertain situations!
Funny how the two 'upgrade' models are both on the same side. Their track record has yet to really be established so it has no effect on confidence levels.
I feel that the main thing to take from ECM is that we can see very unfortunate shortwave behaviour in these situations, but the op run itself does seem like a worst-case scenario (yet it's still alright for a [probably] short-lived cold spell to end the year).
Edited by user
17 December 2014 21:08:27
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