But if we want to max our potential we actually want that kind of gradient. Because what causes that is the combination of the h7 fgen and the moisture transport hitting the wall of confluence which adds even more convergence can create a really a good band. That’s how you get those surprise 6-8 sometimes even more, bands on the northern edge. But when that happens it’s going to be banked up against the fringe and the combination of confluence and subsidence will create a really sharp cutoff. Places just 10 miles north of where the 6-12” band set up in PA last Feb got 1”. If we want any shot at 6”+ we want that! But we want the band to be over us and the cutoff in PA. That’s all. If that banding doesn’t develop or stays weak, and there are times that does happen if the mid level forcing is weak or too disconnected from the best moisture transport, then there wouldn’t be a sharp cutoff. But in that case I think we can kiss anything more than about 4” goodbye bc that h8 fgen band is not making it up here and the subsidence north of that might even hurt us if it gets close, and with a more gradual taper we’re probably in a 2-5” zone north to south across Carroll county.