FOUS30 KWBC 141936 QPFERD Excessive Rainfall Discussion NWS Weather Prediction Center College Park MD 336 PM EDT Tue Jul 14 2026 Day 1 Valid 16Z Tue Jul 14 2026 - 12Z Wed Jul 15 2026 ...THERE IS A HIGH RISK OF EXCESSIVE RAINFALL IN THE TEXAS HILL COUNTRY... ...Texas Hill Country... Portions of the TX Hill Country witnessed torrential rainfall last night and this morning that will continue to unfold through midday. Radar estimates show anywhere for 6-10" of rain have fallen in Medina, Uvalde, and Bandera counties (locally around 12") and have already led to reports of numerous flooded roadways and water rescues. Looking ahead, the atmosphere is primed for additional rounds of Excessive Rainfall with hourly rates between 2-4" likely. The 12Z RAOB out of Del Rio, TX showed an abundance of moisture aloft (2.28" PW, well above the 90th climatological percentile) and sufficient instability for thunderstorms to work with (~1,600 J/kg of MLCAPE). The MCV north of Del Rio is the catalyst for this event, tapping into the rich moisture and unstable air-mass to generate numerous showers and thunderstorms. Overnight CAMs struggled with the placement and duration of the storms this morning, although new 12Z guidance is catching on better and is in largely good agreement that storms will continue through early afternoon. Many new 12Z CAMs suggest a brief lull may occur this afternoon, but the presence of the MCV is likely to keep some storms in the heart of TX through early evening. By tonight, the LLJ over South TX will strengthen and act to re- supply additional low-level moisture towards the MCV, which is forecast to hover near Del Rio, TX. The combination of upscale ascent supported by the MCV, the LLJ intersecting a nearby stalled frontal boundary, and natural topographic upslope into the Hill Country west of I-35 will reinvigorate thunderstorm activity tonight. It is worth noting that all CAMs do have an axis of Excessive Rainfall with amounts in the 2-4" range overnight (locally higher than 6"), but they disagree on placement. The 12Z HREF and 06Z REFS are keying in on areas closer to the MCV, essentially from Medina/Bandera counties on WNW towards Del Rio with moderate chances (40-60%) for additional rainfall totals >3" and low chances (10-30%) for rainfall >5" between 00-12Z. Some members, such as the 12Z HRRR and 12Z RRFS, show the axis of heavy rainfall encroaching upon the western San Antonio suburbs. Given the rainfall that the current atmospheric environment has already produced, additional rainfall totals of 3-6" are forecast for the remainder of today and through tonight in the TX Hill Country with localized amounts over 10" possible. Reminder that this discussion strictly focuses on 16Z today through 12Z Wednesday (Day 1), so this does not take into account the rainfall still to come for Day 2 and the second half of the week. In collaboration with the NWS San Antonio/Austin office, given the likelihood for additional significant rainfall in areas slammed with heavy rainfall and ongoing flooding this morning, a High Risk was introduced for the 16Z update. Significant to locally catastrophic flash flooding is forecast to continue today and, with additional heavy rainfall tonight, likely to persist into tonight and early morning Wednesday. Potential impacts include flooded/impassable roads, flooded creeks/streams, and potential inundation of homes. Please have a reliable means of receiving weather warnings and information from local/state officials. Elsewhere, some minor tweaks to the inherited Moderate and Slight Risks were made to account for latest 12Z guidance, but otherwise the setup featuring a pooling of anomalous moisture along a stalled frontal boundary will continue to trigger additional strong storms and scattered areas of flash flooding through this evening. ...Coastal South Carolina... A Slight Risk was introduced along the South Carolina coast with this update. The 12Z CHS sounding measured a 2.26" PW (above the 90th climatological percentile), MLCAPE over 1,000 J/kg, and a warm cloud layer over 14,000ft deep. Storms have already flared up along a frontal boundary both over land and at sea, and as daytime heating ensues, additional strong thunderstorms are likely to develop. Storms will be generally slow moving and can produce 3"/hr rainfall rates with locally more intense, shorter bursts of torrential rainfall possible. The 12Z HREF shows low-to-moderate chances (20-50%) for localized areas of the SC coast receiving over 5" this afternoon. The area has dealt with locally heavy rainfall in recent days and is a little more susceptible to rates approaching 3"/hr, particularly in the more urbanized communities. Mullinax ---Previous Discussion--- ...Southeast into Southern Mid Atlantic... General consensus on widespread convective development across the southern Carolina's into the Southeast lends to at least a broad MRGL risk for flash flooding in any area north of I-4 with a relative max for heavy rain situated across portions of MS/AL thanks to the presence of a meandering upper level disturbance over the area. WV satellite this evening pin-points a weak upper level circulation centered over northern MS with an extremely slow propagation to the west-southwest over the past several hours. This particular upper circulation will be a focal point for enhanced low to mid-level convergence later this afternoon interacting with what is a formidable moist/unstable environment across the Southeast CONUS. Scattered to widespread showers and thunderstorms will materialize across northern LA over into MS and AL during peak diurnal destabilization leading to pulse/multi-cell convective development over the region with heavy rain prospects likely very high considering the environment in place. Wetbulb zero heights >14k ft on forecast soundings across MS/AL indicate an effective warm cloud layer that will likely present efficient rainfall rates with even pulse variety convection yielding 2-3"/hr rainfall potential during its mature phases. Slow cell motions under a weak steering pattern situated across the Southeast will only act as an aid to flash flood prospects over the region as cells will be more likely to produce heavy bouts of rain for multiple hours before drifting away from an area, or even just decaying overhead. 00z HREF and REFS neighborhood probabilities for >3" are solidly between 50-80% across central and south-central MS into western AL with the main area of interest lying along and north of I-20 in both areas. HREF blended mean outputs show a scattered 2-3" precip signal over the aforementioned area with individual deterministic even pushing close to 5" in the hardest hit locales. This is more than sufficient for maintaining the previous SLGT risk forecast, as well as wording for a high-end SLGT threshold likely over that area encompassed within central MS to western AL. ...Southwest U.S. into the Great Basin... Continued impacts expected from lying into the western flank of the ridge centered over the Northern U.S. as prevailing southerly flow will just maintain a prevalent moisture advection regime poleward over the Desert Southwest into the Great Basin. Models remain consistent in their interpretations of locally heavy rainfall over both regions with the heaviest QPF centered over AZ, but potentially greater impacts in those more flash flood prone areas located in the interior west, including those slot canyons over UT/NV. Rainfall rates will be the driving factor for flash flooding in this scenario with instability generally favorable (>750 J/kg MUCAPE) over a large portion of the Western CONUS. The combination of PWAT anomalies >2 deviations above normal and elevated instability favors at least widely scattered flash flood potential, which this setup is leaning into the textbook signature as forecast. 00z HREF neighborhood probabilities for >1" have a smattering of 40-60% probs within areas of the Great Basin and Four Corners with a more widespread 40-70% probability oriented in the terrain from southeastern AZ up through the Mogollon Rim into the area of the Grand Canyon. Any of these cells in the terrain will be conducive for heavy rainfall between 0.5-1"/hr, locally higher across the terrain with more of the general 0.25-0.75"/hr over the Great Basin. Given the consistency in the model output and anomalous moisture presence across the West, the previous MRGL risk was maintained. ...Montana... PWATs encroaching the 90-99th percentile over much of MT coupled with favorable instability and approaching mid- level troughing to the west will allow for scattered to perhaps widespread convection to materialize over the Northern Rockies into Central MT later this afternoon and evening. Ample shear and elevated moisture presence will amplify the convective threat and proceeding heavy rainfall posture across portions of Big Sky country as we move into the time frame of peak diurnal destabilization. Organized cell clusters, including a few supercells, are likely to initiate over the terrain in the Central portion of MT with an eventual rapid storm motion off to the northeast as the steering flow will allow for very quick propagation(s) through the High Plains of MT by later in the evening. The best threat for heavy rainfall suitable for flash flooding will likely occur where the initiation point occurs and just downstream of the eventual storm motions to the northeast. HREF probabilities for >2" are generally modest in this area with consistency in the CAMs for cell initiation and eventual impacts in this region northwest of Billings up through Glasgow to the Canadian border. The previous MRGL risk was maintained given the threat. ...Northern New England... A strong closed low analyzed over Northern Quebec this evening will pinwheel southeast, well north of the Canadian border in New England, but will aid in a broad brush of robust mid-level vorticity over the northern tier of both VT/NH into western ME during peak diurnal heating into the coming evening. MUCAPE between 2500-3500 J/kg will be located across the northern tier of all three states leading to a targeted area for locally heavy rainfall with rates likely to approach close to 2"/hr as noted in the latest HREF prob fields (10-25%) with 1"/hr rates a greater certainty (30-50%). A quick 1-3" is forecast across this small area of New England, however this area is notorious for local terrain influences that could cause issues with any appreciable rainfall in that short period of time. The previous MRGL risk was expanded further north to include western ME given the trends in guidance for heavy rain to impact this area as cell maturation over neighboring Canada will likely motion into the area as we step into the late-afternoon and early evening hours today. Kleebauer Day 2 Valid 12Z Wed Jul 15 2026 - 12Z Thu Jul 16 2026 ...THERE IS A HIGH RISK OF EXCESSIVE RAINFALL ACROSS PORTIONS OF THE EDWARDS PLATEAU, CENTRAL RIO GRANDE VALLEY, AND HILL COUNTRY... ...Texas... Similar to Tuesday morning, just about all guidance is on board with a cluster of robust thunderstorm activity producing excessive rainfall from portions of the TX Hill County and central Rio Grande Valley to the Edwards Plateau. Guidance agrees that the lingering MCV responsible for Tuesday's flooding will continue to organize rounds of thunderstorms that have the potential to train over areas hit from Tuesday's flood-producing storms. Anomalous PWs surpassing 2" and sufficient instability will keep the atmosphere in ripe condition to support torrential rainfall. The main disagreement between guidance is the placement of the heaviest rainfall. 12Z HREF members suggest the placement of the MCV is farther north and west with a more westerly-positioned LLJ over the Rio Grande. This is allowing for several HREF members to focus heavier rainfall rates over the Edwards Plateau. Meanwhile, guidance such as the HRRR and RRFS (REFS probabilistic guidance as well) suggest the southern extent of the thunderstorm activity may bring the MCV farther south and closer to the San Antonio metro. The LLJ is also notably stronger and oriented more at the TX Hill Country. Ultimately, both placements of storms can have merit. The southern extent of Tuesday's thunderstorms is likely to drop a remnant boundary where, as the LLJ strengthens Tuesday night, could be a trigger for thunderstorms near and west of the I-35 corridor Wednesday morning and potentially redevelop Wednesday night. Meanwhile, the mesoscale-enhancement near the MCV would also support a pivoting axis of strong storms near and north of Del Rio that could even reach the Big Bend. While the exact location is unclear, the dangerous combination of prolific rainfall rates over highly saturated soils is a recipe for significant to even catastrophic flooding. This set up for Day 2 (Wednesday) is not too dissimilar to the setup that produced 6-12" of rainfall in parts of the Hill Country Tuesday morning, given the same atmospheric phenomena are on the playing field again on Wednesday. When utilizing both HREF and REFS probabilistic suites, they both paint a potentially dangerous situation for life-threatening flash flooding Wednesday morning. In collaboration with the San Angelo and San Antonio WFOs, a High Risk was introduced on Day 2. A Moderate Risk (threat level 3/4) also extends from the Big Bend to as far east as the San Antonio metro area. While there remains some uncertainty in the exact placement of heaviest rainfall, antecedent soil conditions coupled with rainfall rates ranging between 2-4"/hr are likely to cause numerous flash floods. Life threatening and catastrophic flash flooding is likely in the hardest hit areas. Be aware that flooding is likely to occur overnight and into the early morning hours both Wednesday and Thursday. Mullinax ---Previous Discussion--- ...Mogollon Rim into Central Arizona... Broad upper ridge centered over the Northern U.S. will continue to provide significant moisture advection into the interior west leading to scattered convective signals from the Canadian border down into the Desert Southwest with flash flood concerns in those more susceptible areas out west. Increased confidence in a locally favorable convective maxima has allowed for not only a continuation of the previous SLGT risk positioned across the Mogollon Rim in AZ, but also an expansion further northwest and north, including the addition of Flagstaff proper. 00z HREF at the end of its temporal range signaled widespread thunderstorm genesis over the terrain after 20z Wednesday with some formidable heavy rain cores likely to materialize out of the initiation. Modest neighborhood probabilities for >1" of rainfall exist in the small window between 18-00z Wed/Thu with the highest probs situated in that terrain area between Phoenix and Flagstaff within the Mogollon Rim across central AZ. In coordination with the local Flagstaff WFO, have expanded the previous SLGT risk forecast to areas northwest of Flagstaff within the western periphery of the Mogollon Rim, as well as a further north expansion to include Flagstaff proper given the recent trends in guidance, and the premise of urbanization factors providing more suitable ground conditions for flash flood prospects. ...Lower Mississippi Valley into Southeast... Our meandering upper level disturbance will continue to churn over the Southern U.S. with sights on the Lower Mississippi Valley by Wednesday afternoon. Models are within close proximity of each other on the positioning of the disturbance with the centroid of the circulation likely to be focused somewhere over Arkansas and the southwest corner of TN. Elevated moisture and general diurnal destabilization across the Lower Mississippi and Southeastern U.S. will lead to another round of slow-moving thunderstorms capable of producing locally heavy rainfall with rates of 2-3"/hr likely in those stronger cell cores. The setup is not as prolific within the QPF means compared to the previous few periods, so the threat remains within the MRGL risk threshold. However, will continue to monitor trends closely as we move forward in time as the chance for a targeted upgrade, likely underneath the upper level disturbance, is plausible. Kleebauer Day 3 Valid 12Z Thu Jul 16 2026 - 12Z Fri Jul 17 2026 ...THERE IS A MODERATE RISK OF EXCESSIVE RAINFALL ACROSS PORTIONS OF THE LOWER TRANS PECOS, EDWARDS PLATEAU, AND RIO GRANDE VALLEY... 20Z Update... The biggest adjustments made from overnight was to expand the Moderate Risk farther north through the Edwards Plateau based on recent wetter trends in WPC QPF. Impacts will be heavily dependent upon where the pesky MCV will be located, but most guidance shows its gradual north and west movement by Thursday. Following the active day on Wednesday as well, portions of the Edwards Plateau, the Lower Trans Pecos, and Rio Grande Valley will likely also see antecedent soil conditions grow more susceptible to excessive rainfall rates. ...Ozarks & Middle Mississippi Valley... A 500mb trough pivoting overhead will also have anomalous PWs in excess of 2" throughout the generally flashy areas of the Ozarks on Thursday. Model soundings across the board show highly saturated profiles combined with skinny MLCAPE values in excess of 1,000 J/kg. Storm motions appear to be fairly slow and vertical wind shear is weak, so storms will behave more pulse-like in nature. That said, the atmospheric environment could support hourly rainfall rates up to 3"/hr in some of the more intense cells, and 1-hr FFGs are likely to range between 2-3". Given these factors, localized flash flooding is possible on Thursday with poor drainage areas and complex terrain most prone to potential flooding. Mullinax ---Previous Discussion--- ...Texas... Convection will continue across the Edwards Plateau and surrounds for at least one more period as the regional pattern maintains a persistence in its evolution with yet another round of convection lingering through the morning from the previous period, and one last round of nocturnal convection anticipated the evening of Thursday into early Friday morning. There is some uncertainty on the exact location of the final convective wave that will transpire with some guidance positioning the greatest threat a little further north of the area likely to see the greatest impacts from the prior periods. In any case, the threat is still very much robust for wherever this transpires as the axis of heavy rainfall will likely produce more totals bordering between 2-4", locally higher in the hardest hit locations. Considering the nature of anticipated compromised soils and ongoing flooding across portions of the RGV and Edwards Plateau, very little additional rainfall would cause a myriad of problems, including an exacerbation of any remnant flood waters, especially if impacted by additional heavy rainfall >1"/hr. There's enough of a signal to warrant an addition of a MDT risk across the area between the Big Bend over into the Edwards Plateau with emphasis on Val Verde county extending up to the neighboring counties to the north, including the I-10 stretch in central Crockett county. Considering the nature of the situation, this period will be monitored very closely and its susceptible to larger scale changes as the setup evolves. Heavy rain will likely enhance life-threatening flash flooding to portions of the region for yet another period before the setup finally looks to break after the D3 time frame. ...Southwest U.S into the Great Basin... Another round of afternoon and evening convection will transpire across the Southwest CONUS into the Great Basin on Thursday with the threat carrying into the early morning periods of Friday in some locations. Models are keen on a more robust moisture advection pulse and general instability axis across the Desert Southwest on Thursday with a broad axis of heavy rain prospects from the southern border all the way north into southern UT. Ensemble bias corrected output is very bullish on the threat in and around the slot canyons of southern UT, along the Mogollon Rim, and down towards the terrain embedded within Cochise, Santa Cruz, and Pima counties. Areal average of 1-2" is forecast for the region along the southern border with 0.75-1.25" forecast across the Mogollon Rim and southern UT. Considering the environment maturing closer to 1000-2000 J/kg MUCAPE over much of AZ into southern UT/NV, instability and anomalous moisture within the 90-99th percentile of climatology across the region will produce more widespread heavy rain prospects leading to scattered flash flood occurrences in those more susceptible locations in the terrain. There is even some opportunity for thunderstorm genesis off several outflows that could impact some of the larger urban corridors within AZ, including the Phoenix metro as the environment favors this type of potential. A broad SLGT risk was introduced for much of AZ into southern UT with the eastern extent out towards the NM/AZ border into the immediate Four Corners, outlining the mean QPF closer to 0.5" within the ensembles. Kleebauer Day 4 and Day 5 Valid 12Z Fri Jul 17 2026 - 12Z Sun Jul 19 2026 ...THERE IS A SLIGHT RISK OF EXCESSIVE RAINFALL ACROSS PORTIONS OF THE SOUTHWEST ON FRIDAY... 2030Z Update... No major changes were made to either day or to either area of concern. Having said that...felt the on-going excessive rainfall over West Texas in the short term would warrant a Slight Risk going into the Day 4 period. This resulted in an expansion of the Marginal Risk area northward and a bit eastward. The 14/12Z GEFS QPF did not show blockbuster values but any MCVs in such a moisture rich airmass could result in continued or renewed flooding. Only subtle shifts were made to the periphery of the Marginal Risk area across parts of the Intermountain West/Southwest U.S. and the Great Lakes/Mid-Atlantic. Bann Previous Discussion... ...Western U.S... A broad active monsoonal pattern will continue across much of the western U.S. Friday into Saturday. An anomalous PW axis stretching from AZ northward into MT is forecast to remain above the climatological 90th percentile, and locally higher in some spots. This airmass will sustain a localized flash flood threat across an expansive corridor spanning from portions of eastern CA, AZ, and NM northward to MT. We did go ahead and upgrade much of AZ into southwest UT and southwest NM into a Slight risk for D4 (Friday). While the prolonged monsoonal pattern will bring at least a localized flash flood threat to the region each of the next 5 days, current model guidance indicates Thursday and Friday will see a peak in both PWs and CAPE. Model consensus and NBM QPF are also higher on these days. Of course, mesoscale details (which we can't pin down at this lead time) may end up determining the eventual flash flood coverage. But there seems to be enough of a signal to suggest the risk may be relatively higher those two days. The isolated threat continues into D5 (Saturday), but will hold that at a Marginal for now with a modest decrease in PWs/CAPE/QPF noted in the models compared to Friday. ...Texas... The multi-day heavy rainfall event over portions of central and west TX should be on a declining trend by Friday. PWs gradually decrease and lower level convergence seems to wane, with both the AI models and GFS/ECMWF showing a decrease in convective coverage. With that said, we will still have strong 850mb southerly moisture transport across the state, and some leftover shortwave energy. So the event is likely not over on Friday, just probably less widespread and hopefully not as high end. The setup into Friday is still favorable enough that can not rule out Slight risk upgrades on future updates, especially if the convective footprint overlaps hydrologically sensitive areas from previous rainfall. The risk should lower further by Saturday, but again some risk of a locally heavy rainfall threat continues from the Edwards Plateau and points west. ...Great Lakes into the Mid-Atlantic... On Friday a Marginal risk was introduced from portions of the TN Valley northward into the Great Lakes. The strong mid to upper level ridge currently anchored over the Plains/Midwest is forecast to break down and translate southeastward. This synoptic shift will allow the high PW airmass currently situated over the South to advect north-northeastward. By Friday afternoon much of the OH and TN valleys will have PWs around 2" and CAPE potentially exceeding 3000 J/kg in spots. This unstable and saturated environment will be conducive for high rainfall rates. While weaker large scale forcing across the southern portion of the risk area may limit overall convective organization isolated instance of flash flooding will be possible. Further north, stronger synoptic forcing should support organized convection across portions of WI into northern MI. These convective cluster may lean toward a progressive mode, but the degree of instability and PWs should support some flash flood risk. On Saturday the core of the high PW airmass shifts eastward into the Mid-Atlantic. Amplifying troughing building into the Northeast, accompanied by embedded shortwave energy, should support a organized convective threat from OH into the northern Mid-Atlantic and possibly southern NY. Spatial uncertainties exist regarding how far north the surface front and axis of better instability will get, which will ultimately dictate the northern bound of any flash flood risk. Further south and west across the OH Valley into the southern Mid-atlantic large scale forcing may be weaker, but plentiful moisture and instability may still drive localized areas of heavy rainfall. Chenard 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 $$