Summary

  • A band of heavy snow occurred late on the 23rd and early on the 24th within the upward branch of a thermally direct circulation associated with mid-level frontogenesis.
  • The snow band was enhanced by reduced stability within the upward branch of the circulation.
  • Snow amounts were highly elevation dependent, with up to a foot and a half falling at higher elevations in the southwest Catskills.



Slide 18