FOUS30 KWBC 190023 QPFERD Excessive Rainfall Discussion NWS Weather Prediction Center College Park MD 823 PM EDT Mon May 18 2026 Day 1 Valid 01Z Tue May 19 2026 - 12Z Tue May 19 2026 ...THERE IS A MODERATE RISK OF EXCESSIVE RAINFALL FOR PORTIONS OF MISSOURI, IOWA, NEBRASKA, AND KANSAS... 01Z Update... The overall setup for a significant round of rainfall is still very much in-tact with the current radar/sat composite indicating a large complex of thunderstorms growing upscale across the Central Plains with a modest forward propagation to the east-northeast under the guide of mean southwesterly flow aloft. A strong mid- level shortwave trough is analyzed over the KS/NE border with a broad axis of diffluent flow oriented over the Southern Plains to mid-Mississippi Valley providing sufficient large scale forcing and favorable upper dynamics to help ignite the current convective posture. Quasi-stationary front is analyzed over central KS up through far southeastern NE into IA with two lows situated within the front; one located over northeast KS and the other still positioned back into the High Plains of northeast NM. The coupling of large scale ascent and a broad axis of prevalent deep layer moisture imposed along and ahead of the front will aid in the convective regime maintaining itself overnight with rainfall rates embedded in the expected QLCS to reach between 1-3"/hr at peak intensities. Budding 40-50kt LLJ will become oriented a bit more parallel to the front as we move through the evening allowing for low-level flow to become favorable for back-building and/or training convective pulses across portions of KS into western MO. This signal is prevalent in pretty much all the CAMs leading to a strong neighborhood probability for >3" (40-70%) located across a corridor extending from Wichita Falls, KS and points northeast into northwestern MO, including the Kansas City Metro. The Missouri River basin and surrounds continues to be the focal point for the heaviest precip opportunities which would be the second or even third day of impact for some of these locales. Local FFG's have fallen considerably as a result leading to a heightened risk of flash flooding which allowed for a general maintenance of the inherited MDT risk. Further southeast, remnant outflow boundary positioned just north of the MO Ozarks extending into the western Ohio River basin near IL/KY/IN continues to be a focal point for convection this evening with training causing a myriad of hydrologic issues for places along the boundary. Additional 1-2" will be possible for the initial few hours of the 01z update before finally dissipating overnight, however the eastern expanse of the convective development and evolution tonight will still extend eastward into the Mississippi River area of eastern MO into IL. This will leave the door open for additional flash flood concerns given the greater sensitivity posed by the recent rainfall. SLGT risk still extends into these above areas as a result. Kleebauer Day 2 Valid 12Z Tue May 19 2026 - 12Z Wed May 20 2026 ...THERE IS A SLIGHT RISK OF EXCESSIVE RAINFALL FOR PORTIONS OF THE CENTRAL TEXAS HILL COUNTRY AND OHIO RIVER VALLEY... The main changes to the overnight forecast include a broadening of the Marginal Risk, and introduction of embedded Slight Risk areas over the Texas Hill Country and Ohio Valley. A relatively stagnant synoptic pattern will continue through Day 2 as a positively tilted mean trough slowly evolves over the Western U.S. This configuration should maintain modest southwest flow over the Central/Eastern U.S. to support a corridor of heavy rainfall ahead of a northeast to southwest oriented cold front. Toward the beginning of Day 2, thunderstorms are expected to develop along the cold front as it enters the Southern Plains and interacts with a moist and unstable airmass characterized by 2000-3000 J/kg and 1.6-1.8" PW. Fairly weak and unidirectional cloud layer wind profiles atop a lingering 20-30 kt nocturnal low- level jet suggest this convection along the front will have a tendency to train before propagating southward with the initiating boundary. The HREF and RRFS suggest hourly rainfall rates will eclipse 2"/hr at times in the main axis of convection, which should initially support isolated flash flooding during the day. The greatest concern for excessive rainfall, however, will materialize late tomorrow afternoon as the cold front enters the Texas Hill Country and bisects a well-defined dryline. The resultant east- west axis of thunderstorms will eventually grow upscale and train within the very unstable and modestly sheared airmass. From late Tuesday into early Wednesday, the HREF and RRFS are in good agreement for increasing probabilities of 2-3"/hr rainfall rates, which could lead to rainfall totals upwards of 3-5" by Wednesday morning. When combined with the sensitive nature of the Hill Country and urban areas in the Texas Triangle, a Slight Risk was introduced in this update. Otherwise, a separate Slight Risk area was introduced over portions of the Ohio Valley as thunderstorms develop along the slow moving front tomorrow afternoon. While weak height rises forecast in the vicinity of the front could limit thunderstorm coverage somewhat, forecast soundings featuring moist vertical profiles (1.8-2.0" PW), 3000-4000 J/kg of MUCAPE, and unidirectional flow suggest the storms that develop should be quite efficient and slow to propagate in the new Slight Risk area. This scenario is supported by the HREF and RRFS, which depict increasing chances of hourly rainfall rates eclipsing 2-3"/hr by late tomorrow afternoon. As this activity overlaps with ongoing heavy rainfall in the region, scattered flash flooding could result. Asherman Day 3 Valid 12Z Wed May 20 2026 - 12Z Thu May 21 2026 ...THERE IS A SLIGHT RISK OF EXCESSIVE RAINFALL FOR PORTIONS OF SOUTH-CENTRAL TEXAS INCLUDING THE HILL COUNTRY AND EDWARDS PLATEAU... The Day 3 excessive rainfall risk is really just a translation slightly southward of the Day 2 risk area due to a slowly evolving synoptic pattern. A large positively tilted trough positioned across the Intermountain West and back into the Great Basin will gradually amplify but maintain its NE to SW orientation. Gradually pinching mid-level flow will help funnel additional moisture northeast from the Pacific across the Southern Plains and into the Ohio Valley/Central Appalachians. Within this flow, subtle shortwave impulses lifting through the flow will help enhance ascent, aiding low-level convergence along a nearly stalled front draped from Ohio through Texas. At the same time, locally backing low-level flow from the south at 850mb will converge into the front, producing impressive moisture convergence along the front in a region of PWs that are progged to be 1.5 to 1.75 inches. Although inflow may be somewhat modest (850mb winds around 20 kts), this will be sufficient within the moist column to provide plentiful advection to support widespread convection with rainfall rates above 1"/hr nearly certain. Although there continues to be uncertainty into the exact placement of the heaviest rainfall due to prior-day convection which will cause wavering of the surface boundary, 0-6km mean winds becoming increasingly boundary-parallel will support training of these rainfall rates, and the SREF/ECENS/GEFS all suggest at least a low-end risk (5-10%) of 3"/24 hrs around the updated SLGT risk region. While this in itself may not force widespread FFG exceedance, much of this rainfall D3 will fall atop areas that are expected to receive significant rainfall as well D2, so the SLGT risk was drawn to account for compounding impacts potential over already vulnerable terrain features. Farther northeast, the MRGL risk was cosmetically adjusted for new guidance as convection with heavy rainfall will likely repeat from SW to NE along the front as it slowly sags southward through the Tennessee and Ohio River Valleys. Weiss Day 1 threat area: https://www.wpc.ncep.noaa.gov/qpf/94epoints.txt Day 2 threat area: https://www.wpc.ncep.noaa.gov/qpf/98epoints.txt Day 3 threat area: https://www.wpc.ncep.noaa.gov/qpf/99epoints.txt