My understanding was that it had a lot to do with the relative humidity of the lower few thousand feet of the atmosphere - call that a boundary layer if you like.
I think it was Bren who used to maintain that all precipitation started off as snow, it was just that it usually melted before it reached the ground. If the lower atmosphere is (very) dry, the precipitation is cooled enough by evaporation to persist as snow down to ground level.
That, of course, invites the question: do we get fewer dry E/NE lies than we used to? Speculatively, warmer oceans generate more activity and we get damp SW-lies pumped onto the western edge of continents instead.
Originally Posted by: DEW