The 00z (left-hand) had a shortwave low to the NW of the UK, and the 06z persisted with this, but it has been adjusted south and weakened on the 12z (right-hand).
Instead of tracking NE then E and riding over the latter HP cell, forcing it south, the shortwave is absorbed back into the cut-off low west of Iberia (such an incredibly frequent feature this year), which means it actually supports the HP cell rather than interfering with it. This evolution also allows the amplified ridge west of the UK to merge more quickly with the blocking high. The net result is a large step NW in the positioning of the blocking high by day 8:
This is a great example of how relatively small adjustments can have large impacts on conditions a few days later on.
The run goes on to bring a chilly SE'rly for a few days, as heavily mixed-out Arctic air circulates around from the eastern flank of the high.
Then the Atlantic attacks - but because of the position and strength of the block, the storms show a strong tendency to slide SE, with fronts arriving from the SW rather than W or NW.
This raises the possibility of more pronounced easterly incursions if the block is adjusted much further west in future runs. Now, it is possible to get a cold continental feed adequate for producing low-level snow events via a mid-latitude block... but the problem is, that usually occurs later in winter rather than earlier. This is because you don't tend to see enough of a low-level cold pool involved to overcome the sort of sea surface temperatures usually present in late November and often well into December.
So although westward adjustments are a common occurrence when the models are dealing with blocking highs to our east, I'm not anticipating much in the way of low-level snow from the east within the next fortnight or so - raw, damp days under persistent low cloud seem the greater risk beyond this coming week.
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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)
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