Question, why are hugger tracks more likely with a fast Pacific Jet? Is there some reason a BM track becomes less likely than a hugger track? Or are we talking about thread the needle events and there are simply more ways to get screwed than there are to get hit?
Also, in the past with a fast Pacific jet (like 1993-94) we used to have bowling ball lows go just south of us instead of completely suppressed. What happened to what were once common lows that would cross the country west to east and exit off the DelMarva up to South Jersey? Those used to be good for 4-6 inch snowfalls and we used to get at least a couple of those every month between December and March. What happened to them?