The Scandi trough is looking considerably more potent on todays output, with the idea of the Siberian High edging west, explored by a good number of ensemble members recently, well and truly put down by the operational runs at least.
The ECM run almost blows it away completely, as it has the most intense Scandi trough with the least distortion taking place (i.e. the lows bear the most resemblance to a dartboard). GFS, GFSP and JMA are less vicious but it does appear that the jet will be too strong to permit any easterly option from evolving.
With that in mind, thoughts once again turn to any means of enhancing the northerly incursions on the rear flank of those storm systems.
The developments of most interest to me in the 12z op runs are:
That low in the far-western North Atlantic has been adjusting south with each new run (though only slightly in the case of ECM), with a little more of a ridge ahead of it. This suggests a toning down of the southern arm of the jet, which I reckon gives a small chance that the low becomes a cut-off feature with a marked Atlantic ridge to the NE of it, rather than riding the main Atlantic jet to the UK as happens in all of the 12z operational runs.
It requires every operational run to have the jet modelled incorrectly, so I'm not counting on it, but after what happened with this weeks low, it's not hard to imagine.
While that first low doesn't become cut-off, things work out very differently for the next low in that region on the ECM, JMA and GFSP runs:
This low, which tracks through the southern states of the U.S. days 3-7, becomes cut-off in the western North Atlantic as the southern arm of the jet does not fire straight NE to phase with or run parallel to the northern arm (for those wondering what I'm on about, these 'arms' represent branches of the jet stream that are associated with the two areas of most rapid horizontal temperature change in the North Atlantic).
This idea of a cut-off low was present on yesterday's 00z runs before being dropped for a couple of sets of operational runs. It has the effect of encouraging the Azores High to ridge north in the middle of the North Atlantic, enhancing the day 10 rear-flank (of the Scandi trough) northerly on both the ECM and GFSP runs.
Ideally, this would be followed up by any later troughs across Canada or the U.S. digging south to merge with it rather than 'scooping' it out as the GFSP 12z op run does. ECM could be having a go at the end of it's run but it's not a very convincing attempt.
So there lies one of the most significant aspects of the model output to keep an eye on - there does look to be an increasingly prominent jet stream across the southern states over the coming 10 days or so, and the way in which the associated lows behave as they reach the Atlantic will greatly affect how flat or otherwise the Atlantic pattern becomes, how far into Europe low heights manage to get and so on. That in turn may change the fortunes of the Siberian High.
The models also seem to be really struggling with how the MJO behaves in the coming week or so.
In fact this does seem like the sort of situation in which the true solution remains in hiding until a sudden emergence without much warning.
It really is no wonder that Fergie's comments have been laden with caveats regarding high uncertainty!
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