Prepare the reading glasses, it's a big one I'm afraid
Not much worth saying about the trop. output from the models within the reliable, while beyond that there are hints that the main focus of low heights might shift SE toward the UK from GFS and GFSP but these are contradicted by the ECM run which wants to break only part of the low heights away from the NW, slide that quickly SE and then start building a ridge over us instead.
Meanwhile, the stratosphere output continues to show significant events, with the warming over Greenland gaining further ground on GFSP which has upgraded it a lot over the past couple of days. Meanwhile ECM has toned it down just a little and is no longer the most aggressive solution, that trophy going to NAVGEM which raises the 10hPa temperature all the way up to 0*C, which is quite extreme really. JMA is consistent with its previous two runs.
Highlights:
The GFSP solution (left) now has the warming starting at a high enough latitude (between NE Canada and Greenland as can be seen here: http://modeles.meteociel.fr/modeles/gfsp/runs/2014123012/gfsnh-10-192.png?12) to bring about a second, larger split only a few days after the first (occuring days 7-8) has closed off.
What's not clear from the above is whether the actual 10mb troughs are fully split or not, but with the low temperatures set so far apart it seems likely.
The JMA solution (right) takes the core of the warming 8*C higher than GFSP, and it's even better placed to take down the Canadian vortex - hard to see a way back for it any times soon if that comes off.
This is quite similar to what I've read about the strat. output from the 12z ECM op run, which also takes down the Canadian vortex. In terms of the actual troughs, the day 10 chart features a weak Siberian vortex and a trough extension (like a narrow branch) toward Canada. At that point we will need further wave 2 action to split that weak remnant of the Canadian trough from the dominant Siberian one days 11-14, producing results similar to the GFSP chart above.
So it seems that ECM and GFSP are closing in on a point somewhere between their original output... but of course it's GFS that has done by far the most adjustment these past few days.
As far as getting the all-important split goes, it's very encouraging output this evening.
The man behind the Cohen strat. theory (yes, Cohen himself) concurs:
"Based on the ECMWF forecast, the SSW will get close to a major SSW (defined as a zonal mean easterly wind at 10 hPa and 60°N) and would likely achieve major SSW strength with further wave driving. The GFS has displayed a bias all winter of under-predicting the vertical WAFz and over-predicting polar vortex strength. Therefore we favor the ECMWF forecast of a more perturbed and longer duration polar vortex weakening."
Just to complicate matters further we see that there are Sudden Stratospheric Warmings (SSW) and then major ones (major SSW). The latter is the one with the zonal wind reversal, the former falls short of that. It makes sense really, as the warming is large and does happen very quickly on recent model output, yet a zonal wind reversal remains just beyond the output of ECMWF, for example.
By way of balance to the above post, Cohen also covers what has been a troublesome feature so far this winter and the primary reason for the December warming being unable to bring about a SSW:
"longer-term prospects for the AO continue to hinge on the anomalous polar low in the Barents Kara-seas region that has temporarily weakened. It is predicted to strengthen again across the north slope of Siberia and eventually move back over the Barents Kara seas region. Perhaps the current temporary relaxation is a foreshadowing of a longer term weakening trend but for as long as the Barents-Kara seas low persists, it destructively interferes with an externally forced negative AO (from the SSW). The biggest impact would to inhibit the flow of Siberian air into Europe. It’s impact would be less on North American temperatures where in the near term, ridging across western North America and a polar low in eastern Canada will direct arctic air into the lower 48."
"It is hard to predict how long this area of low pressure will persist, which is likely to be at least somewhat supported by the relatively extensive North Atlantic sea ice extent compared to recent years and to the North Pacific side of the Arctic. As long as low pressure remains near the Barents-Kara seas any tropospheric influences from the stratosphere this time period will be favored across North America relative to Europe. However if a piece of the polar low can move over Europe then this could help force much colder weather into Europe".
This looks like a good example of the sort of thing that prevents a SSW from being a guaranteed route to cold conditions across the UK or even NW Europe. There are always complications!
Ironically, having a low over the Barents-Kara Seas (just north of Scandinavia) is actually a pretty cold setup for us (but not necessarily NW Europe) if there is decent mid-Atlantic ridging, and this is a possibility prior to any SSW driven changes if the Canadian vortex is shut down. Recent GFSP runs have hinted at such things despite never fully taking apart that vortex. GFS is still not with it as far as the strat. output is concerned so the day 10-16 trop. output is a poor guide, and GEFS even worse (these, I have been told, do not model the whole of the stratosphere. Feel free to correct me again if this is not true, Brian.)
I must stress that Atlantic ridge/Scandi trough possibility requires the ECM/JMA strat. output to be close to the mark, and applies to week 3 to 4 of January. There remains little reason to expect much of a downward trend - or indeed any at all - in temperatures in the first half of the month.
If you have any problems or queries relating to TWO you can Email
[email protected] https://twitter.com/peacockreports 2023's Homeland Extremes:
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)
Keep Calm and Forecast On