


Quantitative Precipitation Forecast
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Issued by NWS
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437 FOUS30 KWBC 060057 QPFERD Excessive Rainfall Discussion NWS Weather Prediction Center College Park MD 857 PM EDT Tue Aug 5 2025 Day 1 Valid 01Z Wed Aug 06 2025 - 12Z Wed Aug 06 2025 ...THERE IS A SLIGHT RISK FOR EXCESSIVE RAINFALL ACROSS PORTIONS OF THE SOUTHEAST AND INTO THE MID-ATLANTIC AND IN THE UPPER MIDWEST... 01Z Update...Few changes made to the recently-added Slight Risk area in parts of the Upper Midwest/Northern Plains. 00Z sounding from Aberdeen showed 40 to 45 kt southerly low level winds feeding directly into a complex that has a history of 3 to 6 inch rainfall amounts. The changes which were made were based on trends in satellite and radar imagery.A baroclinic leaf seen in water vapor satellite imagery was crossing the Marginal risk area placed over the Ohio Valley...which was resulting in an uptick in showers and a few thunderstorms. Felt is was a bit too early to remove the Marginal risk area but the expectation is that convection should weaken an dissipate by late evening or the early-morning hours. Likewise...convection should gradually weaken and decrease in areal coverage this evening across parts of the Southeast US but enough upper support and low level flow of moisture precludes removal of the Slight risk area altogether. There was enough support to break the broader region into two distinct areas...one being parts of coastal Carolinas and the second being near the Gulf coast. Bann ...Southeast and Mid-Atlantic... 16Z UPDATE: Most changes for this outlook were made to the Slight Risk area over the Southeast. They were not big overall, but it did recenter the risk area a bit to the northeast, expanding it about 70 miles to the northeast, and trimming about 25 miles off the northwest side. The ongoing round of convection in central South Carolina has progressed further northeast than guidance over the past several cycles had indicated, and 12Z hi-res models show an additional round of convection developing overnight from central North Carolina into central South Carolina. The overnight round would be due to a restrengthening of a LLJ and the unstable air mass expanding inland as a result. No other change in the reasoning described in the previous discussion; a complex pattern of cell mergers and colliding boundaries may allow storms and heavy rainfall to maximize in a couple localized areas, with potential for greater than 5 inches of rain in a short period of time. The 12Z HRRR shows a scenario late tonight that would be of greater concern: a training and backbuilding convective band within 30 miles or so of the Raleigh-Durham metro area, which leads to locally extreme rainfall. Other models show hints of a similar scenario but do not hit similar rainfall extremes. This will need to be monitored in the event of greater consensus or observational trends, in case probabilities may need to be increased. PREVIOUS DISCUSSION: A conducive overall setup for locally heavy downpours exists, with a low-level front/convergence zone and the right entrance region of a strong upper-level jet streak superimposed over the same area (along with anomalously high moisture and PWs over the 90th percentile). The main limiting factor for organized heavy rainfall is certainly instability, though a modestly strengthening low-level jet (15-25 kts) will provide some isentropic upglide to kick things off this morning (with hourly totals likely limited to 1-2"). Most hi-res models depict a break in the precipitation during the day, but another round may ensue later tonight over some of the same areas, as the frontal zone and parent trough to the west move very little. Further diurnally-driven development is expected within the broader warm sector from the central Gulf Coast to south-central Georgia, and the rest of South Carolina, with stronger instability building today with daytime heating and PWs in excess of 2 inches. Hi-res models continue to indicate fairly high probabilities of 2"/hr rain rates, and a complex pattern of cell mergers and colliding outflow boundaries and sea breezes. This may lead to periods of 1-2 hours where convection is maximized in particular areas, and scattered instances of flash flooding. The inherited Slight Risk was expanded a bit to cover coastal portions of SC/GA with the highest probabilities for localized 5" exceedance. ...Northern Plains and Minnesota... 16Z UPDATE: No major changes were made with this outlook update, other than to remove a small portion of the northern side of the risk area due to observational trends and the latest guidance. PREVIOUS DISCUSSION: There continues to be a fairly strong signal for storms to initiate in the northern extent of an instability plume in the Plains, near the nose of a moisture transport maximum, in the afternoon today. Consensus among the hi-res models is this will rapidly organize into an MCS and then likely propagate quickly to the southeast in the general direction suggested by the thickness contours. The potential for relatively fast forward motions may mitigate some of the flash flood risk. However, precipitation anomalies over the past 14 days indicate the pattern has been relatively wet of late in the Northern Plains, and precipitable water values will be anomalously high. Deep moisture combined with strong instability should support high instantaneous rain rates. Therefore, any areas where the duration of heavy rain could be lengthened (such as backbuilding along the periphery of a cold pool, cell mergers with antecedent convective development) may lead to flash flooding. The Marginal Risk was maintained and adjusted southward based on the latest guidance (factoring in upwind propagation favoring southern propagation late). ...Ohio River Valley... 16Z UPDATE: No major changes were made with this outlook update, other than to remove a small portion of the western side of the risk area. PREVIOUS DISCUSSION: An inherited Marginal Risk was maintained and adjusted slightly for a potential repeat of the pattern from yesterday, just displaced slightly to the east over S IN, C KY, SW OH. A slow moving mid-level wave is expected to continue to slowly shift east, in the presence of relatively strong instability. Therefore, scattered afternoon thunderstorms are expected. Although moisture levels are not expected to be anomalously high, storm motions should be very slow with mean winds in the lowest 8-km around 5 kts or so. This could lead to localized flash flooding by extending the duration of heavy rain with the most intense storms. Rain rates should reach the 1-2"/hr range. Churchill/Lamers Day 2 Valid 12Z Wed Aug 06 2025 - 12Z Thu Aug 07 2025 ...THERE ARE MARGINAL RISK AREAS FOR EXCESSIVE RAINFALL ACROSS PORTIONS OF THE UPPER MISSISSIPPI VALLEY AND FOR THE COASTAL SOUTHEAST AND MID-ATLANTIC REGION... ...Upper Mississippi Valley... A region of anomalously high moisture, with PWs near the 90th percentile, should shift east during the Day 2 period, and generally continue to be superimposed with moderate to strong instability on the periphery of a ridge. Confidence in the convective details remain low at this time, but the overall environment will remain supportive of organized convection with high instantaneous rain rates. The pattern may still lead to a forward-propagating MCS, which would mitigate flash flood risk overall, but the overall environment is favorable enough to continue to maintain a Marginal Risk across the region. ...Coastal Southeast and Mid-Atlantic... 2030Z Update: The 12Z guidance today came into better consensus that in the anomalously high moisture plume, additional convection is likely to develop late tonight into Wednesday across SC into central NC. The activity is likely to be slow moving and highly efficient rain producers, so some localized higher amounts are possible as well as some training elements. Some of this could fall over the more urban corridor from Charlotte to Raleigh. By the afternoon/evening, the guidance is consistent that additional storms are likely closer to the coast where some intense rain rates are anticipated. 12Z HREF neighborhood probabilities for 3-5" for the 24-hr period exceeds 50%. With all this in mind, a Slight Risk was introduced for this part of the region. Further south into southeast Alabama into southern Georgia, the high moisture and proximity to the stalled frontal boundary will likely create scattered to widespread thunderstorms. Given the high PWs and general slower storm motions, some localized heavy rainfall totals are possible and in coordination with the local WFOs, a Slight Risk was extended further south into that area as well. ---previous discussion--- Confidence remains relatively low in the placement of the heaviest rainfall on the Day 2 period, as the ECMWF/ECENS suite continues to concentrate QPF farther north (mostly across North Carolina) whereas the bulk of the other global models and ensembles are focused south and east (mainly in SC and GA). Regardless of the precise details, a plume of anomalously high precipitable water values is likely to remain present across the coastal Southeast and Mid-Atlantic region into the Day 2 period, and the flash flood threat areas will likely come down to mesoscale details that will come much more into focus in subsequent outlook periods. Churchill/Lamers/Taylor Day 3 Valid 12Z Thu Aug 07 2025 - 12Z Fri Aug 08 2025 ...THERE ARE MARGINAL RISK AREAS FOR EXCESSIVE RAINFALL ACROSS PORTIONS OF THE UPPER MISSISSIPPI VALLEY AND NORTHERN PLAINS, AS WELL AS FOR THE COASTAL SOUTHEAST AND MID-ATLANTIC REGION... ...Upper Mississippi Valley and Northern Plains... The Marginal Risk area was maintained and adjusted across North Dakota into the Upper Midwest area, as models are in good agreement in indicating a potent upper-level shortwave digging southward into the CONUS by Day 3. The approach of the trough is likely to result in another wave of low-level return flow into the Northern High Plains, sending PWs to the 90th percentile or higher once again. Moderate to strong instability is expected to build once again with daytime heating on the periphery of a ridge, and organized convection is likely to ensue in the late afternoon and evening. ...Coastal Southeast and Mid-Atlantic... Confidence remains low in the placement of the heaviest rainfall going into the Day 3 period, with substantial differences still between the global model suites. As anomalously high tropospheric moisture is likely to remain near the coast, maintained the existing Marginal Risk area across portions of the area most likely to realize heavy precipitation with daytime heating. Churchill/Taylor 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