Only a few days after South Central Nebraska had melted off the vast majority of lingering snow cover from earlier in the month, a moderately-strong winter storm rolled through between the evening of Monday the 28th and afternoon of Tuesday the 29th, dropping a fresh blanket of 2-8 inches of snow in most locales, followed by a light coating of sleet and freezing rain/drizzle especially in southeast counties. Overall though, snow was clearly the main story, especially within northern counties along/north of Highway 92 where the highest amounts of 5-8 concentrated, including CoCoRaHS/NWS cooperative observer totals of: 7.4 in St. Paul and Ord, 6.8 at Greeley, 6.5 in Loup City and also two miles west of Genoa, and 6.1 in North Loup. Southward from there, slightly-lower amounts of 3-5 prevailed within counties along the Interstate 80/Highway 6 corridors, including totals of 5 at Sumner, 4.1 at NWS Hastings, 4.0 in Grand Island and 3.5 in Clay Center and Geneva. Farther south yet, the overall-lowest snowfall of 1-3 fell within far southern counties along the Kansas border. However, especially areas in/near Nuckolls and Thayer counties saw some steadier periods of light freezing rain and sleet showers during the latter stages of the event, although ice accumulation was generally only around one-tenth of an inch and potential travel issues solely from icing were likely muted given that it fell onto freshly-fallen snow. Locations farther north and west (including the Tri Cities area) also saw a light wintry mix of sleet and freezing drizzle in the wake of departing snow, but icing amounted to just a light glaze and the travel impacts from snow-covered roads were far more of a factor (though no closures of main highways occurred). Winds were not overly-strong during the main period of snow, but steady east-southeast speeds of 10-20 MPH with occasional gusts as high as 25-30 MPH were enough to cause some modest blowing/drifting. Temperatures during most of the event hovered in the 20s F.
Taking a closer look at how things unfolded, the majority of snow accumulation occurred between 9 p.m. on the 28th and sunrise on the 29th, as a northwest-to-southeast oriented band of moderate to briefly-heavy snow steadily advanced across South Central Nebraska from southwest-to-northeast. This primary band was driven by a fairly classic case of low-mid level isentropic lift and mid level frontogenesis (especially evident at 700 millibars), with this forcing focused downstream from a larger-scale, positively-tilted trough positioned from the Desert Southwest into the Central Rockies. However, things changed character near and especially after sunrise on the 29th in the wake of the main snow band, as the combination of lower-level warm air advection and an intrusion of drier mid-level air from the southwest (with resultant steepening lapse rates) allowed precipitation to transition from predominantly snow to mainly isolated to scattered sleet showers and areas of light freezing rain/drizzle. Any steadier/measurable precipitation gradually departed the majority of the local area from west-to-east between sunrise and noon, although pesky light freezing drizzle hung around in some places until early evening. At the surface, the modestly-breezy east-southeast winds that peaked between midnight-noon were driven by a decent pressure gradient between a strong/expansive 1035 millibar high departing eastbound through the Midwest and a 1008 millibar low centered over Colorado.