A seasonably-typical, mainly marginally-severe mesoscale convective system (MCS) tracked from west-to-east across North Central Kansas on this early Sunday morning, primarily affecting areas south of the Highway 36 corridor with strong winds and heavy rainfall. There were only a few ground-truth reports of severe-criteria gusts, from mesonet stations near Stockton (59 MPH), Cawker City (75 MPH, along with a report of tree limbs down at Glen Elder State Park), and Beloit (73 MPH). Rainfall-wise, the heaviest overnight totals of 2.00-3.50 soaked southern portions of Rooks and Osborne counties, including a CoCoRaHS total of 3.50 in Plainville.
Long before reaching North Central Kansas, the origins of this MCS began as scattered storms developing over southeast Colorado during the late afternoon of the 10th. As the evening wore on, this convection gradually congealed into a more organized complex as it initially drifted northeast into northwestern Kansas before taking a more easterly turn after dark, eventually reaching Phillips/Rooks counties between 12:30-1:30 a.m. CDT and exiting the local area out of Jewell/Mitchell counties by 4 a.m. CDT. In the wake of the main storm complex, widespread showers/non-severe storms lingered over parts of the area until shortly after sunrise. In the mid-upper levels, fairly weak zonal flow was in place over the Central Plains, to the north of a large-scale ridge centered over TX. Over North Central Kansas, the overnight mesoscale environment featured healthy instability (evidenced by surface dewpoints into the 70s F and mixed-layer CAPE 2000-3000 J/kg), but only 20-30 knots of deep-layer wind shear. However, the eastward propagation of the MCS was aided by warm air/moisture advection within the exit region of a 30 knot, southerly low level jet.