Winter storm types always fall on a spectrum, but this isn’t a classic miller type a setup where you have a
strong coastal cyclone throwing precip back into the colder air to the NW and then the coastal low is really driving in strong cold advection that crashes the entire column. It’s there of course but this is very weak in this case and not the main driver of your precipitation, as I showed earlier.
When you get these types of Miller A events, usually we have blocking to the north to slow everything down & amp the trough/coastal, that’s obviously not happening here because the background flow is very fast and progressive.
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The background pattern is more like Jan 2014 (overrunning) than it is a coastal low
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The surface features also don’t look right for a miller type an event in NC. There’s a surface low over the Great Plains where a surface high should be! Again, no high-latitude blocking either with the wrong sign of anomalies over Greenland.
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