Some early discussion on the weekend's convective potential from various sources on the UKweatherworld...
http://www.ukweatherworld.co.uk/forum/forums/thread-view.asp?tid=28061&posts=10&mid=409731#M409731UKMO are consistant with the development of a deep depression west of Ireland. Predictions are going for eventual drop to 442 mb! Could be the deepest we've seen in a year or two (If you know different then please specify!)
Orientation of streamlines suggest a classic polar maritime flow with a very moist unstable fetch from mid Atlantic. SST anomalies present 10 deg C west of UK & Ireland. These temps have not yet troughed fully this year and will add impetus to any broad scale weather system. Too early to be specific and UKMO synopsis continue to give two scenarios. Though GFS currently give exceptional divergent mid level jet with the main cold front.
Confluent upper troughs are more likely to bring the risk of line convection/ana cold front potential - 23rd Feb 1995, 22 Sept 2003 and 24th Sept 2007 cold fronts with severe line convection and tornado reports were great examples of this. As far as I remember though and looking back at a few basic charts from the date, the 3rd December 2006 line squall occurred under diffluent conditions (or perhaps a negatively tilted diffluent trough that was gradually tending to neutral). Guess there is a greater risk of the cold front splitting when the flow is diffluent, it just then depends whether the potential instability close to the surface front can be released.
Diffluent troughs seem to be more reliant on there being some inherent instability in the pre-frontal airmass, as they are somewhat less likely to produce a strongly forced line from the cold-air 'scoop effect'. Certainly diff. troughs are what you'd look for in the Great Plains, but of course, we're not there! Even so, some squally winds seem very likely, and if convection can develop, tornadoes are possible.
More information closer to the time.