I don't really understand what is being said here. I've often viewed GFS as more progressive, assuming we're talking about a west to east flow across the NA / Europe region. In addition the European 12z takes the Atlantic through pretty conclusively so I'm not sure what Exeter are thinking.
Originally Posted by: Brian Gaze
I wonder if it's to do with GFS producing a strong MJO phase 7 type signature in the 8-16 day range, having gone for it faster and harder than ECM for example?
There seems to have been a move this evening toward an active Atlantic trough becoming stuck to our west and throwing bands of rain and at times strong winds our way, these becoming slow moving as they come up against the block. Tropical and return-polar maritime airmasses exchange frequently to produce a run of temps varying from just below average to some way above.
It's very November 2009-like if you ask me, and about the worst possible path to be taking as the polar profile undergoes those major changes towards a more blocked regime with the tropospheric vortex becoming fragmented by cross-polar heights. Here's a couple of snapshots from Nov 2009, the first showing those lows stalling out due to the block, and the second showing the block migrating across the Arctic while the Atlantic finally starts to make more inroads across the UK:
There's a lot of charts knocking about from recent NWP output which show variants on both of the above. Notice how the Euro High is capable of making a bit of a comeback even in a precursor to what happened in December 2009 - so no need to worry if that features at some point in a model run for the mid-range.
Looking at the progression that occurred between late Nov and mid-Dec 2009, I think that offers a reasonable guide as to the sort of things we should look out for in the far reaches of the GFS output at the moment. Essentially we're seeking very amplified ridges in the mid-Atlantic or perhaps through the UK. The first example below is not sufficient but does reflect the increasing potential due to the high-lat blocking developing. The second example shows a ridge through the UK that managed to trigger retrogression of the HP over Russia to become a fully fledged Greenland block a few days later.
The vortex disruption looks to favour the 'trigger ridge' being further west this year which makes a retrogressing high from Russia less likely, but could mean that an independent area of blocking develops over Greenland. A bit like Nov 2010, except that year also had a strong high over Scandinavia which added to the extraordinary developments going forward:
If the Atlantic lows push through the UK during the first week or so of Jan and the jet shifts south in response to the high-latitude blocking developing, something like the above may well be achievable - but that's about as good as it gets so you'd be setting the bar unreasonably high if you made it the target for Jan-Feb 2016!
Just how quickly the polar profile changes in Jan '16 is still open to some question IMO, but extensive high-latitude blocking looks to be an inevitable outcome one way or another. We'll then begin the game of watching for the pieces to fall into the right places for the UK to receive a good spell of cold, snowy weather.
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