You would think, but we lose any surface high at that point, and the coastal low isn’t sufficiently deep to generate low level CAD until it’s into Maine. It seems more likely to me that 800-900 warmth is being captured well on guidance for part II, but the surface CAD is significantly underdone. Most likely outcome is areas that are below freezing at the surface through part 1 remain so through part II. Surface temps stagnate while 800-900 warm slightly. Points south, around BDL, are mostly light freezing rain/drizzle, while points north, around PSM, are mostly sleet. Areas, in between (around ORH) are a mix of sleet and freezing rain. Seems more like a “we rot” situation, despite the coastal low development.