37 Assess this sounding. Warm layer is unimportant in this case. Supercooled liquid drops possibly coalescing falling and freezing on contact at the groundand. Freezing drizzle was observed 38 Assess this sounding. Cold air is dragged from above as well so the warm layer either stays constant or decreases in temperature.
Bottom layer is below freezing therefore snow is the result.
White area in western Wisconsin changes to darker colors. This represents elevated convection moving over this area changing the precipitation type from freezing rain to snow. 42 Radar loop that corresponds to the 2 previous satellite loops. Convective bands are shown in white. 43 Assess this sounding.