ENSO's apparent footprint on the frequency of Miller A cyclone events is evident here, note how the Miller A & El Nino winter storm composites are virtually identical:
Conclusion: El Nino increases the frequency of Miller A (coastal cyclone) events in NC & this heightened frequency of Miller As likely explains the enhanced seasonal gradient between Greensboro/Winston-Salem & Raleigh-Durham that's also observed in El Nino winters.
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In La Ninas, there's also a negative NAO in the composite, but it's displaced much further east & equatorward of both the NINO & Miller A composite.
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Worth clarifying that both of these above 500mb anomaly composites above include every winter storm that's occurred in NC since 1948 during El Nino or La Nina, with both composites including nearly 100 events. Therefore, the conclusions attained from them are much more likely to be significant & meaningful.
This post is definitely something to put in your back pocket.