True crippling ice storms are pretty rare. We get a lot of nuisance ice events and even semi-regularly we get moderate ice events in the interior. But they almost always fail to reach half an inch of accretion. (Radial measurement, not flat...big difference which causes confusion on here sometimes)
You usually want a mesolow poking NE or NNE off the coast to really lock in the cold/dry dewpoint drain to offset the latent heat release of ZR. When the mesolow is oriented and poking more E or ENE, then it becomes harder to sustain the cold drain. So you’ll get some ZR for sure on that look, but then it ends up slowly going to 33F rain.
You also need the QPF. Accretion efficiencies are often in the 0.7 range or even lower on moderate/heavy precipitation, but they will be much higher on light freezing rain. That’s also why many of the bigger ice storms come in waves of lighter precipitation that lasts for a couple days (or even longer like the 1998 ice storm in NNE)