The 2008 storm was cool because it had offsetting factors working which kind of made the forecast a really tough call.
On one hand, you had marginal temps barely below freezing and very heavy QPF (I should really say rates instead of QPF)….those would limit ice accretion. But on the other hand, you had like a 15-20 knot wind out of the NE…advecting in upper 20s dewpoints the whole time into N MA and down to about ORH.