The morning runs aren't very inspiring around the UK for the period Sunday-Friday next week, as disturbances off the East U.S. coast engage with the main Atlantic jet and develop into strong storm systems south of Greenland which only slowly progress SE.
By contrast, a very promising sequence of events is now being modelled for the U.S. and Canada. Around 6 days out (+144 hours), a shallow trough develops somewhere in the vicinity of Texas, and by day 7 this can clearly be seen progressing eastward beneath a Canadian High that is being supported by that trough (below-left chart). ECM shows the same sort of thing but the trough is further south.
This feature represents a diversion of low heights away from the Canada/Greenland area. Both ECM and GFSP show height rises over Greenland as a result, ECM by day 10 and GFSP by day 11 (below-right, note the circle of green indicating those higher heights).
This is something I've been looking out for over the past week, as it represents a milestone on the path to high latitude blocking.
It should encourage the Atlantic jet to track further south, increasing the extent to which it digs down to the Eastern Med. and attempts to undercut the Siberian High (not captured by the GFSP run until a messy day 15-16 attempt, but nicely shown by ECM on day 10).
It ought to add a bit more punch to back-end northerlies as well, with more substantial mid-Atlantic ridges, but a flatter pattern as per the GFSP 00z could occur instead, which brings a roller coaster of temperatures plus a lot of rain.
I must caution that this all comes from a U.S. progression previously absent from the model output, so although it's at day 6, an equally fast backtrack is not out of the question. After all, the GFS 00z and 06z op runs have it as a faster feature that tracks NE, developing in the western North Atlantic and shifting the mean trough position quite a way west while providing no real height rises over Greenland.
It also appears that even if we do get the ball rolling, westerly momentum may take at least a couple of weeks to subside to the point at which high latitude blocking can really start to have a say in our weather beyond the southward shift in the storm track.
Of course, this all assumes that the models are handling the earlier East U.S. low in the right way this time round, and aren't about to shift it south and prevent it phasing with the Atlantic jet just as they did for the coming week. That would really shake things up but there's less sign of it occurring this time around.
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