On this Wednesday morning, a fairly significant winter storm took aim on South Central Nebraska for the second time in five days. Unlike the more prolonged event of the preceding weekend, this one was a quick hitter associated with one primary snow band, with most affected areas receiving accumulation for no more than 6-7 hours. Despite this brevity, bursts of moderate to heavy snow combined with sustained north wind of generally 20-25 MPH and gusts up to around 35 MPH to promote a treacherous morning commute along with numerous school closures. The brunt of this system targeted locations north-northeast of a line extending from Gothenburg-Hastings-Hebron, where most places received at least 2-4 inches. However, the epicenter of heaviest accumulations on the order of 4-8 occurred in a generally 30-40 mile wide corridor extending from around Loup City in the northwest, then east-southeast through the St. Paul, Grand Island, Central City, Aurora, Osceola and York areas. Within the heart of this band, a few of the highest measured totals (per a combination of NWS cooperative observers and NeRAIN observers) featured 8.7 four miles north of Aurora, 8.2 at Ravenna, 7.1 in Loup City, 6.1 at Grand Island airport, 6.0 at St. Paul and 5.7 in Osceola. On either side of this primary snow band there was a fairly sharp drop-off in amounts, as evidenced by reports from Ord (3.0) and Genoa (3.0) to the north, and Hastings (1.7) and Hebron (2.8) to the south.
Breaking down event timing, this generally west-to-east oriented snow band first infiltrated the northwestern quadrant of South Central Nebraska between 1-3 a.m. and then steadily intensified through daybreak as it spread east. Generally between 7-9 a.m., the band began sinking southward across the Highway 6 corridor and toward the Kansas border, while gradually weakening and ending from north-to-south and also from west-to-east. By 1130 a.m. the vast majority of the local area was snow-free. On the synoptic and mesoscale aloft, this quick-but-intense event was driven by a rather classic, strongly-forced frontogenetic band evident mainly in the 850-500 millibar layer, but especially centered around 700 millibars. This frontogenetic forcing slid across the heart of Nebraska from northwest-to-southeast, enhanced by a coupled upper jet structure evident at 300 millibars, featuring the exit region of one jet streak nosing in from the Northern Rockies and the entrance region of another jet streak centered over the Upper Midwest. At the surface, gusty north wind across Nebraska was driven by an enhanced pressure gradient between an Arctic high pressure system sliding into the Northern Plains and the leading edges of a cold front charging southward through southern Kansas at daybreak. Temperatures across South Central Nebraska averaged between 15-20 F during the majority of this event.