Clearly, it is not factored into the GFS 12z run which is a complete joke.
Originally Posted by: Maunder Minimum
I'm pretty sure that's not possible. The computer modelling will reflect the inputs, it's just a question of whether the modelling deals with this pattern correctly.
The 12z GFS run takes the storm and it gets absorbed into the LP system that exits Newfoundland. I think it's just part of the same underlying problem that we've been seeing and discussing for days now - i.e. to what extent GFS is too progressive.
As has been observed, the differences between UKMO and GFS at T+96 are notable, with GFS pushing the jet on a more northerly track and more west-east.
We're no further forward than we were really in terms of which model is handling this best.
I think one of the issues is modelling the heights to the south - UKMO has the 556dam 500hPa line running across the southern end of Biscay at T+120 and the northern Iberian coast at T+144 whereas GFS has it in the Channel. That's the thick end of 1,000 miles difference, which is significant. It matters because UKMO leaves that space for energy to go further south - at T+144 it has a shallow low off the north coast of Spain - GFS has a surge of warm uppers and a high pressure cell not far to the south.
Location: South Cambridgeshire
130 metres ASL
52.0N 0.1E