Rain that fell in late fall and early winter obviously coincided with warm temperatures. The ground was not frozen so there is a high likelihood that much of the water was just recharge for the water table(assuming the ground is NOT saturated which would also decrease permeability). That's not a BAD thing, it actually being great for the overall health of the watershed but that new water in the water table will reach the streams through the ground slowly.
If an inch of water is going to fall, it will be an inch of rain or about ten inches of snow. The good thing(for our concerns) about snow is that snowpack will not only melt, but most often will melt with the ground underneath it frozen near solid. Because of the low permeability of the soil then, the water in the snowpack will primarily be runoff and NOT recharge. Runoff will contribute to the reservoirs gaining volume quickly. Of course with snowpack we lose some volume to evaporation and sublimation over the course of the winter, but we lose very little to the ground.
Right NOW the reservoirs are just one percent over "normal". We are CERTAINLY not at a "normal" amount of snowpack. We've got about two months to whiten the place up and THAT can certainly happen, but RIGHT NOW there is next to nothing to provide runoff in the spring to increase Cannonsville the 16%(right now) it needs to spill.