Primarily between 9 p.m. on Wednesday the 17th and 5 a.m. on Thursday the 18th, Jewell and Mitchell counties received a broad coating of 2 to 3.5 of snow, with lesser totals closer to 1 reported in eastern portions of Smith and Osborne counties. Per a combination of NWS cooperative observers, CoCoRaHs observers and trained spotters, a few of the highest overnight totals featured 3.5 at Lovewell Dam, 3.3 at Jewell and Simpson, 3.0 two miles north-northwest of Hunter and 2.6 at Mankato. Fortunately, light wind made this an almost ideal , relatively low-impact snowfall, as sustained easterly speeds only averaged around 5 MPH.
From a broader geographical perspective, the local North Central Kansas area resided along the northwestern fringes of a larger snowfall swath of generally 2-5 that mainly affected central and northeast portions of the Sunflower State. Between 9 p.m. and midnight on the 17th, steady snow spread into the local area from the south, before very slowly ending from west-to-east during the pre-dawn hours. On the large scale of the mid and upper levels, this fairly low-impact event was driven primarily by broad isentropic lift focused along and north of a low-amplitude shortwave trough shifting across KS and toward the MO/IA border through the night, with only a fairly weak contribution from frontogenetic forcing. At the surface, the very light wind was fostered by a weak pressure gradient on the southwest fringes of a broad high centered over the Upper Mississippi Valley.