Especially for counties south of Interstate 80 in South Central Nebraska, June finished with an active Saturday afternoon and evening of severe storms. Things started off with two discrete supercells featuring intense, crop-damaging hail and a few brief tornadoes, followed a few hours later by a larger-scale squall line/linear mesoscale convective system (MCS) that yielded sporadic damaging winds and torrential rainfall. The two confirmed EF-0 tornadoes were spawned by the eastern supercell in southeastern Phelps County around 4 p.m. CDT and inflicted no evident damage. As for large hail, both supercells produced at least golf ball size stones, including reports from the Arapahoe, Loomis and Axtell and Minden areas. However, the western storm also featured a report of baseball size hail three miles southeast of Loomis (see below for more details regarding resultant crop damage). Turning to damaging winds, the aforementioned pair of supercells yielded a handful of measured and estimated reports, including 80 MPH near Axtell (measured by a storm spotter). A bit later and farther east, an evolving cluster of multicell storms with estimated 80 MPH winds brought isolated wind damage to a few rural residences in far eastern Clay County, including: destroyed carports and hog sheds, and a partially-removed garage roof. Later in the evening, the more expansive MCS that swept across all of South Central Nebraska from west-to-east yielded mostly sub-severe gusts of 45-55 MPH. However, a handful of severe-criteria gusts of at least 60-65 MPH occurred in both far western areas (near Cambridge) and also far eastern areas (Fillmore/Thayer counties). In the eastern area, a camper blew over near Hebron and a large tree fell on a home in Milligan.
When all was said and done, the overall-biggest severe weather impact from the day was likely the localized-but-extensive crop damage caused by the initial pair of supercells in the southwestern quadrant of South Central Nebraska. The western supercell, which tracked from north central Furnas County to central Phelps County mainly between 2:30-4:30 p.m. CDT was particularly impactful, as satellite imagery in the following days revealed a roughly 2-3 mile wide by 15+ mile long swath of near-complete crop destruction. While not the main story, locally heavy rainfall and mainly minor/short-term flooding also occurred, with large portions of several counties receiving at least 1.50, much of which fell in a short time. The overall-heaviest rain into the 3-4range concentrated in two main zones: 1) parts of northern Furnas/southeastern Gosper and western Phelps counties, including 3.21 at Loomis...2) much of York, eastern Hamilton and southern Polk counties, including 4.09 near York and 3.26 near Stromsburg. In all three Tri Cities, the evening squall line produced brief-but-intense rainfall that prompted short-term street flooding, with reports of stalled vehicles in Kearney and the closure of the Burlington Avenue underpass in downtown Hastings.
Taking a closer look at the timing and evolution of convection, things got underway between 2-3 p.m. CDT as severe storms rapidly fired up over northern Furnas and Harlan counties. During the following few hours, these storms organized into the aforementioned pair of noteworthy classic supercells, with the western one eventually dissipating over Phelps County, while the eastern one marched across Kearney County and into western Adams County before weakening and merging into newly-developing multicell storms to its south and east. Between 5:30-7:30 p.m. CDT the main focus turned to a cluster of strong-to-severe multicells that expanded across eastern portions of the area, yielding mainly heavy rain and small hail, but also the eastern Clay County wind damage. As these storms exited stage right into eastern Nebraska, nearly all of South Central Nebraska had roughly an hour of storm-free conditions before attention turned back to the west as the leading edge of the north-south oriented squall line entered Dawson/Gosper/Furnas counties between 8:30-9:30 p.m. CDT. Over the next 2-3 hours, this mostly (but not entirely) sub-severe MCS swept through the remainder of the area, with the leading edge of strongest winds/heaviest rain exiting into eastern Nebraska shortly after midnight CDT.
Finishing with a look at the meteorological background and starting with the mid-upper levels, this was a fairly evident severe weather setup as a semi-potent shortwave trough (by early-summer standards) tracked from Wyoming into western Nebraska during the afternoon-evening. At the surface, a well-defined, west-southwest to east-northeast oriented frontal boundary stretched from northwest Kansas to southeast Nebraska throughout the day, with most of the local area residing just to its north in an environment characterized by easterly breezes, high temperatures in the 80s F and plentiful low-level moisture with dewpoints between the mid-60s and low-70s F. Deep-layer wind shear averaged around 40 knots throughout the event, with mixed-layer CAPE peaking 2000-3000 J/kg during the afternoon. While the late-afternoon and evening storms were well-anticipated, if anything was a bit of a forecast surprise it was the early formation of the pair of intense supercells, which could have posed a more dire tornado threat had they tracked directly along the surface front instead of generally 10-20 miles north of it.