Roger, totally understand going closer to climo on snowfall....I took a gamble there. You can have a "perfect" composite in the seasonal mean to maximize snowfall, and are still likely to verify closer to climo than my numbers. However I would caution against a suppressed storm track in December because the PNA may lack a little, so we may have an element of latitudinal gradient with regard to snowfall distribution. Secondly, show me the weak el nino seasons with a suppressed storm track....you won't find many, save for 1979-80, which was a very marginal warm ENSO event. This is because the N stream is more prevalent than the STJ during these seasons, which breeds miller b cyclogenesis. This also often entails that southern New England endures the system's fury during that crucial time period during which the mid level centers are closing of, which maximizes frontogenesis and deformation potential. Sure, they can still miss southern New England, but its a lot more difficult when they develop in the n stream...its akin to pitching from a mound that is 60' away from home plate, and one that is 30'....its easier to throw a strike from that latter-