NWS Goodland clocked 85 mph wind gusts near Colby as a haboob shut down I-70 visibility. Across the state line, NWS Pleasant Hill issued life-threatening flash flood warnings for Grundy, Livingston, Sullivan, and Linn counties — the fourth straight day of relentless storms across the central US.
What happened
Saturday's Storm Prediction Center outlook had the Kansas City metro under a Slight Risk (Level 2 of 5) for severe weather — large hail and damaging wind the headline hazards, with heavy rain and localized flooding noted as secondary threats.
By late afternoon, that secondary threat had become the lead story.
In northwestern Kansas, the National Weather Service office in Goodland issued a Severe Thunderstorm Warning at 7:42 PM CDT for eastern Thomas and Sheridan counties. By that point, dust kicked up by the storm complex was already collapsing visibility along Interstate 70. Successive Goodland advisories — one at 6:58 PM MDT, another at 8:12 PM CDT — documented blowing dust stretching from near Oakley to roughly 14 miles south of the interstate near Grinnell, with measured visibility under a quarter mile.
Across the state line, the National Weather Service office in Pleasant Hill was tracking a different problem. By 8:07 PM CDT, four north-central Missouri counties — Grundy, Livingston, Sullivan, and Linn — were under a Flash Flood Warning. The warning text described "life-threatening flash flooding" with a CONSIDERABLE damage threat. Specific locations called out included Trenton, Chillicothe, Linneus, Browning, Galt, Bethany, and Gilman City.
Kansas: a wall of dust on I-70
A haboob is a wall of dust pushed forward by the outflow of a collapsing thunderstorm — strong, sinking air spreading outward from the storm core, sweeping up loose surface dirt as it goes. They are most common in arid environments where the soil is dry and exposed. Western Kansas in May, after several weeks of below-average soil moisture, fits that description.
NWS Goodland's storm reports through the evening included measured 85 mph wind gusts near Colby — the Thomas County seat, about 25 miles east of Oakley along I-70. Other reports across the warning area clocked 50-to-70 mph sustained winds with isolated 68 mph measured gusts.
The operational hazard with a haboob is not the storm itself — it is what the dust does to drivers. Visibility under a quarter mile at highway speeds is functionally zero, and dust storms have a well-documented history of producing high-speed multi-vehicle pileups along Kansas interstates. The Kansas Department of Transportation and Kansas Highway Patrol launched a dedicated "Pull Off, Lights Out" safety campaign earlier this year specifically to address how drivers should react when caught in blowing dust: get off the roadway when safe, turn off headlights and taillights so trailing vehicles do not follow the lit silhouette into the dust wall, and wait it out.
Missouri: 1.5 to 6 inches across the northern tier
While the dust was moving east-southeast in Kansas, a different part of the same storm system was sitting and rotating over north-central Missouri.
NWS Pleasant Hill's flash flood warning text reported between 3 and 6 inches of rain had fallen across the four-county warning area by late evening — with one warning update specifying southeastern Grundy County in a more conservative 1.5 to 3 inch band, plus an additional 1 to 2 inches still possible. Locally heavier totals likely fell where individual storm cells trained over the same drainage. (Radar-derived rainfall estimates — the MRMS QPE product — can run higher than gauge ground-truth, particularly in convective cores; the figures above are the NWS Pleasant Hill warning-text values, not raw radar output.)
The receiving infrastructure on the Missouri side is the Grand River system: a network of tributaries that drain northern Missouri farmland into the Missouri River at Brunswick. Trenton sits on the Thompson River (USGS gauge 06899500), one of the Grand's principal tributaries. Chillicothe and Sumner sit on the Grand itself. The Grand River near Sumner gauge defines flood stage at 26 feet; major-flood thresholds run above 40.
By Saturday night, the gauge story had not yet finished writing itself. The Thompson River response to a 3-to-6-inch rainfall event upstream is measured in hours, not minutes. The first-order question is when downstream stages on the Grand begin to rise, which is largely a function of how saturated antecedent soil conditions were going into Saturday — and after four consecutive days of severe weather across the central United States, the answer is: very.
The part that doesn't get a warning
NWS warnings are county-anchored. They are issued for specific Forecast Office areas of responsibility, validated against specific gauge stations, and aimed at specific population centers where the warning will be read by emergency managers and the public.
That structure means the places that are best protected are the places with the most infrastructure. Trenton has a Thompson River gauge. Chillicothe has a Grand River gauge. Sumner has a Grand River gauge. The named cities in the warning text get the warning text.
The blind spots are the small-creek tributaries between the gauges. Ungauged headwaters in low-density rural areas drain into the named rivers on a delay — sometimes minutes, sometimes a few hours — and the agricultural land along those creeks is where the silent damage shows up: pasture inundation, equipment displacement, livestock cut off from higher ground, county roads turned into low-water crossings without signage.
This is one of the structural blind spots TKC will be investigating as part of an in-development interactive hydrology surface (project working name: `/weather/hydrology`). The thesis: most of the data needed to surface ungauged-tributary risk is already public — USGS Water Services, NOAA's National Water Prediction Service, NWS MRMS QPE, the USGS Watershed Boundary Dataset — and the missing piece is not better physics but better visualization of what NOAA and USGS already publish.
What's next
The Storm Prediction Center's outlook for the next 48 hours has the central Plains in an elevated severe-weather regime through at least Monday. SPC's current language flags supercells capable of all hazards including very large hail and strong-to-intense tornadoes across central Kansas into southeastern Nebraska for Monday afternoon along a developing cold front and dryline. Sunday's threat is more diffuse but extends across a similar geographic footprint.
For northern Missouri, the immediate question is when the river gauges crest. For western Kansas, the question is whether the dry surface soil and existing high winds set up additional dust-driven highway closures before the upper-level pattern shifts.
We will update this article as NWS issues new warnings or as gauge data crosses notable thresholds.
Q: What is a haboob, and why is it dangerous?
A: A haboob is a wall of dust pushed forward by the cold-air outflow of a collapsing thunderstorm. The danger is not the dust itself but the visibility collapse — under a quarter mile at highway speeds, drivers cannot react in time to traffic ahead. Kansas's 'Pull Off, Lights Out' safety campaign instructs drivers to leave the roadway when safe, kill all lights so trailing vehicles do not follow them into the dust wall, and wait until visibility returns.
Q: What is the difference between a Flash Flood Warning and a Flash Flood Emergency?
A: Both are issued by NWS Forecast Offices when flash flooding is imminent or occurring. A Flash Flood Emergency is the more severe escalation, reserved for cases where the office assesses a serious threat to human life or catastrophic property damage. As of late Saturday night, NWS Pleasant Hill had Flash Flood Warnings in effect for the four north-central Missouri counties; updates may upgrade portions to Emergency-level language as conditions evolve.
Q: Why does the rainfall total reported on TV differ from the NWS warning text?
A: Television coverage often cites the MRMS QPE — a radar-derived rainfall estimate that integrates multiple radars to produce a national gridded total. The NWS warning text more typically cites gauge-validated estimates, which can run lower because convective storm cores can inflate radar QPE relative to what actually reaches the ground. Both are useful; for ground-truth flood-impact reporting, gauge data is the gold standard, with MRMS QPE serving as the spatial-coverage layer where gauges don't exist.
Q: How can rural communities downstream of warned areas track their own risk?
A: The USGS Water Services site (waterdata.usgs.gov) provides 15-minute gauge data on most named rivers in the United States — free, public, and updated in near-real-time. The NOAA National Water Prediction Service (water.noaa.gov) layers river forecasts on top of those observations. Both are mobile-friendly. The blind spot is small ungauged creeks: for those, the closest proxy is the upstream gauge in the same watershed combined with the MRMS QPE map for recent rainfall input — which is part of the gap TKC's in-development hydrology surface is meant to close.
