Okay, so...the direction and exit point of the trough hasn't really changed much in the output, the differences in precipitation boundaries are to down to circulation. If we take the direction of the trough and combine the northern limit of the precipitation in Ireland across and down through England, you get something like below - quite similar to recent output to be honest. The northern limit would be somewhere around Stoke. However, the heaviest falls would be across through the West Midlands and down into the Home counties.
The southern limit would be the black line as the precipitation is above the circulation. There won't be issues with marginality for the vast majority of us so where the front stalls, pivots and slowly sinks south, I can see some significant snow falling.
This technique worked a few weeks ago when Wales got hit by quite a bit of snow, however...I am in no way saying this will work again!