[quote=Retron;1072424]
Yes indeed. Down here at least I usually look for -10C at 850, but as I mentioned the lower the pressure the closer to the ground that 850 line becomes and thus the higher a temperature you can get away with.
Here's an example (note: NOT based on any particular model).
Say that it needs to be -7C at 4000 feet for snow to make it to the ground. The ground temperature is 2C. I'm using this calculator.
At an SLP of 1025hPa, the 850 line is at 4860 feet (therefore it'd need to be colder than -7 at 850 for snow to fall - probably closer to -10)
At 1005 hPa, it's at 4350 feet (so -8 or so would do)
At 985, it's 3840 feet (so you could get away with -6)
And at 965, it's 3300 feet (so -4 or -5 would do).
Obviously there's a lot more to it than just that (lapse rates, evaporative cooling, boundary layer modification via a warm sea etc), but it gives a rough idea of why the models have been so snowy with relatively modest 850s - this is the polar opposite of a typical "driven by a massive high" cold spell.
Incidentally the ECM showed this beautifully a couple of days ago. 850s under lowish pressure were -5C or so, then as a high built in situ, without pulling in a colder airmass, the 850s fell to -8C over the course of a day - just because the 850 line was getting progressively higher.
We could really do with seeing temperature charts at x height rather than x pressure.
You can detailed temperature lapse rates on Meteociel for places in France where altitude is often key
http://www.meteociel.fr/tendances-neige/27293/aime.htm
Brian - is this possible for the UK from the data you get?