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 — and by Sunday morning, rainfall totals had revised to 3-to-9 inches with the Grand River near Sumner forecast to crest at 31.6 feet by midweek.

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.

The storm cycle did not stop at sunset. By Sunday morning, three additional warning zones were active across the Grand River basin, and storm-total rainfall reports were pushing significantly higher than the initial 3-to-6-inch band the Saturday-evening warnings described.

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.

Grand River basin — gauge crest forecasts as of Sunday morning

GaugeCountiesCurrent stateForecast crestWarning through
Thompson River at TrentonGrundy, LivingstonMinor flooding occurringMon May 18, 8 PM CDT
Grand River near PattonsburgGentry, DaviessMinor flooding forecast27.3 ftMon evening
Grand River near ChillicotheLinn, LivingstonModerate flooding forecast29.3 ftMon May 19, 1:15 AM CDT
Grand River near SumnerLinn, Livingston, Carroll, CharitonModerate flooding forecast31.6 ftWed May 20, 3:45 PM CDT
Editorial-style schematic illustration of a Midwest river basin: smaller tributary streams converging into a larger river flowing toward a major waterway, suggesting downstream-delay hydrology.See live on /weather →
Schematic of the Grand River system. Smaller tributaries (Thompson, Locust, Weldon) drain rural farmland and converge into the Grand, which flows past Chillicothe and Sumner before joining the Missouri River at Brunswick. The water moves downstream on a delay measured in hours — long after the rain has stopped.

Missouri: 3 to 9 inches across the northern tier, and rising downstream

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 Saturday evening reported between 3 and 6 inches of rain had fallen across the four-county warning area. By Sunday morning, follow-on warning updates revised the band higher: 3 to 9 inches widespread across the Daviess, Gentry, Grundy, Harrison, and Mercer corridor, with locally heavier totals where individual storm cells trained over the same drainage. (Radar-derived rainfall estimates — the MRMS QPE product — typically lead gauge ground-truth in convective cores by several hours; the high-end Sunday-morning totals are now closer to what radar QPE was indicating Saturday night in real time.)

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.

As of Sunday morning, the gauge picture has begun to write the next chapter:

- Thompson River at Trenton — minor flooding is actively occurring; Flood Warning extended through Monday evening. - Grand River near Pattonsburg — minor flooding forecast, expected to reach 27.3 feet, Flood Warning through Monday evening. - Grand River near Chillicothe — moderate flooding forecast, expected to reach 29.3 feet, Flood Warning through early Monday. - Grand River near Sumner — moderate flooding forecast, crest of 31.6 feet expected by midweek, Flood Warning extending through Wednesday afternoon.

The Sumner crest is the one worth pausing on. The rain that produced it has, by Sunday morning, largely stopped. The crest itself is days away. That gap — between the rain ending and the river peaking — is not a forecasting failure. It is the system working exactly as the basin's hydraulics dictate.

The part that doesn't get a warning

The Sumner crest is a textbook illustration of the structural blind spot in how flood warnings reach rural communities. Rain stops; rivers keep rising.

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. They get crest forecasts measured to the tenth of a foot, days in advance.

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. Their rise can come hours after the rain has stopped — driven by the same upstream water now moving downstream toward the Grand. By the time the Sumner gauge reads 31.6 feet on Wednesday, a great deal of that water will have already passed through small unnamed creeks across rural Linn, Carroll, and Chariton counties to get there.

This is one of the structural blind spots TKC is 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 Sunday outlook has shifted the strongest severe-weather corridor northeast of where Saturday's events occurred. SPC now flags discrete-supercell potential — capable of producing strong tornadoes and large-to-very-large hail — across northeast Nebraska, far southeast South Dakota, southwest Minnesota, and northwest Iowa for Sunday afternoon into Sunday night. The central Plains (Kansas into northern Missouri) carries a more conditional risk Sunday, with atmospheric capping and weak large-scale ascent expected to inhibit widespread convection during daylight hours. Bowing line segments with damaging-wind potential are likely as the cold front advances east-southeast Sunday evening.

For northern Missouri, the immediate questions are practical and mechanical: when the river gauges crest, how much downstream agricultural land sees pasture-level inundation, whether the projected 31.6-foot Sumner crest holds or revises higher with additional Sunday rainfall. The forecast is days, not hours.

For western Kansas, dry surface soil and a regime of elevated winds keep the dust-storm risk live whenever the next storm cell collapses across exposed agricultural land — a longer-running pattern not driven by one Saturday-night event.

We will continue to 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.

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