#MeteorologicalMonday focuses on the convective snow squalls from March 9th, 2018. Dry adiabatic lapse rates (surface to 700 mb) created sufficient instability for the squalls, which produced 1/4 mile visibilities in heavier snow bursts at several VT/NY locations. #vtwx #nywx pic.twitter.com/A7cYzC2xx0
Source: Twitter NWS Burlington