Seems like the trend to a more phased system is encouraging heigher heights in SE Canada sandwiched between the plains trof and 50/50, which is giving us a new feed of cold via a weak area of descent to our N before the main stuff arrives, if we go that route it encourages a more fresher feed of cold with the tradeoff being more mixing given the processes of CAD. A flatter wave that’s more northern stream heavy is more snow with less warm nosing but 2M temps are just a little more marginal given a more northern stream dominated wave brings its own cooler air aloft but still with a more stale sfc given it cuts off that feed quicker.