I am most directly interested in cold in and of itself. I love snow but I have lived in North Carolina all of my life so I have had to learn to be satisfied with a sloppy 2 inches a year if I am lucky. So I love cold and dry almost as much as snow (I had a good Christmas).
That being said I am interested in understanding if there are multiple different ways to succeed or fail with regards to cold anomalies in the eastern CONUS. For example, I know that there are at least two distinguishable Pacific doom patterns which suck for cold in the east. One is the Alaska vortex. Another is the massive Aleutians ridge. Are there multiple distinguishable "good" Pacific patterns as well, or are they all really variations on the theme of a +EPO ridge?