The NAO was extrmeley positive throughout February (WPO neutralized a bit at .32), which is not hostile to the interior NE, but it is for the coast....lo and behold, this is precisely what materlized.
Go figure-
The predominantly positive NAO during the month resulted in a southwest flow event character to the vast majority of storm systems. As a consequence of the +NAO initially forcing the lobe of the PV post split to drift westward, not only was the bulk of the cold relegated to the high plains, but the signature storm of the month tracked to the west of the area. This limited the extent to which snowfall could exceed normal relative to if the NAO had been negative.