Something I've noticed is that the ratio can depend as much on wind and crystal structure as temperature. Dendrite-dominate lake effect that falls straight down in light wind can be much higher ratio at 30 degrees than wind-blown plate-dominant synoptic snows at 27 degrees. I have seen 14:1 ratio with massive aggregate flakes even with a temperature of 30, provided there isn't a lot of wind and the depth is only a few inches. Of course, once you get a depth of more than 4 inches, even dendrite-dominant large-aggregate snowpack will compress quickly to a 10:1 ratio if the temperature is anywhere near freezing. It's usually under 4 inch snowfalls that can have a lot of variability based on crystal structure and wind. Once you get a lot of depth there's more compression due to weight and so the ratio's become more purely temperature dependent.