When was the last time we legitimately had 3' if snow over a signifucant area if the state?
January? lol. Southern tier is a significant portion, I guess. We got that in a sudden burst of snow.
Anyway, I do agree with you regarding "snowpack" being overused. Always been interested in this dynamic. I don't think snowpack matters as much as "ground melt". And that's probably a stronger effect on how saturated the ground was when it froze in late fall/early winter than it is when the snow melts off.
Snow in PA typically melts off before the ground thaws. Hence, it runs off. That's when you get that "half inch of slick mud on top of frozen underlayer" effect in the early spring. It's a big factor for pH spikes but probably not for groundwater recharge. Really, any precipitation that falls before that ground thaws doesn't have a huge effect outside of some recharge zones with permanent water in limestone (karst) regions.
But that frozen ground is saturated and frozen soil, and when it finally thaws, very little runs off and the vast majority seeps into the groundwater table giving you your spring boost. Again, a function of what it was like in the fall when it first froze, rather than what fell on top of it in winter.
And after the ground thaws, but before weeds and grasses grow and trees leaf out, any precipitation event adds a lot of groundwater. The ground is in that "just thawed" spongy type deal and not yet hardened on top, and no shallow roots are overly active soaking up moisture.
After the weeds and grasses and leaves come, a light rain just gets soaked up by roots and doesn't make it to the groundwater, and a heavy rain is usually VERY heavy from spring thunderstorms and the majority runs off. But a good all day soaker can really help out, anytime of year. You just don't get all that many of those by the time thunderstorm season rolls around. You get quick and heavy hitters instead. That's not good for groundwater. Would rather have an inch of rain spread over 6 or 7 hrs than 2 inches in 30 minutes.