Really ready for the nam to come into range here, wonder if it can sniff out whether we’re gonna have a ice storm or whether we can get away with it with IP, my parents told me that dec 2002 storm was bad, I don’t remember it myselfAnd since we're talking about CAD and warm noses and their model biases, it's worth noting that phenomena are, to some degree, two sides of the same coin. Perhaps somewhat counterintuitively, strong warm air advection above the boundary layer is really good for CAD. It creates a strong temperature inversion, which is really where the cold air at the surface derives its stability from. Because of that inversion, the cold air faces even more resistance if it tries to rise upward (over the mountain range).
In some ways, I wonder if the model bias of making CAD too weak has the same underlying reason as the bias to make warm noses too weak.
Here’s to hoping we can somehow keep cooling that 925mb layer