Although expectations were not high for severe weather in North Central Kansas on this late Sunday afternoon and early evening, two separate areas of strong to severe storms resulted in a few reports of 50 to 65 MPH winds for parts of the six-county area. First, a surge of strong to severe outflow winds charged southward into mainly Jewell and Mitchell Counties between 545 and 645 PM CDT, emanating from a small complex of severe storms centered just to the north in south central Nebraska. As this outflow crossed Jewell County, estimated gusts to 65 MPH resulted in tree damage in Mankato. Although the main track of this severe storm complex remained off to the north and east, at least one strong storm flared up in Jewell County along the surging outflow boundary. Around the time this initial activity was settling down or moving east of the area, a new smattering of strong to severe storms crept north of Interstate 70 into southern parts of Osborne, Rooks and Mitchell Counties between 7 and 830 PM CDT, resulting in 50-60 MPH winds at Natoma.
These separate areas of severe weather resulted from different initiating mechanisms. The storms in Nebraska that pushed severe outflow southward into Jewell County developed in a moisture-rich low level environment to the north of somewhat diffuse surface front stretched across northern Kansas into northwest Missouri. Meanwhile, the severe storm that later affected Osborne County first developed along northward-pushing outflow from storms in central Kansas. These higher-based central Kansas storms formed in an environment characterized by very steep low-level lapse rates, making them conducive for pulse downbursts and damaging winds. Synoptic-scale forcing for convection was very minimal across the region, with only a subtle disturbance passing through quasi-zonal flow aloft. Deep-layer vertical wind shear was also quite weak, only around 20 knots, due to mid and upper-level ridging dominating the southern two-thirds of the nation.