Right then. Sorry I’m late, was out for longer than expected. My thoughts on this morning then; hope there’s someone still around to read this.
It is a rather interesting and slightly complex set up so I think it will be best to look at it in terms of layers of the atmosphere.
As we go through the early hours, The wind backs into the East-south-east and temperatures at the surface are near or below freezing. At first there is nothing unusual about the atmosphere, it gets colder the higher up you go. As we get towards 05:00 however, a layer between about 2000-8000 feet begins to get colder. At the same time, the air above this begins to warm as the Atlantic waa arrives. although still remains below freezing all day. By about 09:00, when the precipitation has already got going, the top of the middle layer (4000-8000 feet) begins to warm substantially and by around 11:00 rises above freezing. This is an inversion layer. In the meantime, there is still a substantial layer of sub-zero air between about 800-4000 feet and this doesn’t get mixed out untill the early afternoon. Thus as we go through the morning, precipitation is likely to start as snow for mostwhen most of the atmosphere is below freezing. As the inversion layer develops however, snowflakes falling through it will melt and then refreeze as they fall into the sub-zero layer below. This gives the rare potential for ice pellets. As this inversion grows The precipitation will have less and less time to refreeze on its way down to the surface and so freezing rain or just rain is then more likely.
In summary: this is not your average Atlantic invasion, there are some interesting atmospheric dynamics at play here. Let’s see what happens.