A very strong cold front dove through the Oklahoma Panhandle during the day of the 21st. The cold airmass behind the front was fairly shallow with the lowest five to six thousand feet reaching temperatures below freezing. Above this cold near surface layer was a five to six thousand foot deep above freezing warm layer. This warm noise and a relative lack of moisture in the snow growth region of the atmosphere kept the precipitation type during the late night hours of the 21st mainly freezing drizzle. As the hours progressed into the early morning hours of the 22nd, the Dodge City, Kansas upper air sounding showed the snow growth region was saturating. This allowed for the precipitation type to transition to a freezing drizzle, sleet, and snow grain mixture. Precipitation transitioned to more of a sleet/snow mixture across the Oklahoma Panhandle through the 22nd and into the morning hours of the 23rd due to the warm layer aloft cooling to near freezing as seen from the Dodge City, Kansas upper air sounding.
Each county of the Oklahoma Panhandle was impacted by this wintry mixture of precipitation. Freezing drizzle was reported in Guymon (Texas County) by school officials. They stated that between Hooker (Texas County) and the Beaver County line was where freezing drizzle transitioned to snow. By 8:00 AM CST on the 22nd, the Beaver County Emergency Manager reported that there was less than an inch of snow on the ground, and that roadways remained in good condition. Once scattered wintry precipitation ended, Cimarron County had received an estimated one inch of snow as snow bands moved from Dallam County into the western Oklahoma Panhandle.