AWUS01 KWNH 250432 FFGMPD TXZ000-251000- Mesoscale Precipitation Discussion 1210 NWS Weather Prediction Center College Park MD 1231 AM EDT Sat Oct 25 2025 Areas affected...Eastern & South-Central Texas... Concerning...Heavy rainfall...Flash flooding possible Valid 250430Z - 251000Z SUMMARY...Upstream QLCS have slightly favorable training environment to maintain longer rainfall duration for spots of 2-4" totals and scattered possible incidents of flash flooding through late overnight period. DISCUSSION...Regional RADAR mosaic shows a mature QLCS rapidly advancing across North Texas into the Heart of Texas increasing in forward speed, while strong inflow vector becomes parallel to the line reducing overall convergence. However, GOES-E WV suite denotes main southern stream shortwave lifting northeast through the Red River Valley with trailing mid-level trough axis back toward the Big Bend of the Rio Grande Valley. Strong diffluent/split flow from 80kt sub-tropical jet streak, generally aligned along South Texas and through the Upper Texas Coast combined with right entrance to 70kt south to north polar jet streak across the Big Country allows for increasing divergence in proximity to the trailing convective outflow (southern edge of strong 1015 Meso-high). Strong surface to 925 south-southeasterly flow at 10-20kts is pumping low 70s Tds and increasingly unstable air off the western Gulf generally orthogonal to the orientation of the trough/convergence axis. This is providing more than ample strong moisture flux convergence for a strengthening cluster along the upwind edge with overshooting tops to -70C. Pooled moisture is up to 1.5" through depth, though maximized in the lowest portion of the column allowing for efficient rainfall production with 1.75-2"/hr rates. Downstream along the northeast edge, isentropic WAA is providing some scattered towers pre-wetting the soils as the peak cores rapidly advance. While forward speed will limit overall totals, the combination of prolonged moderate rainfall with peak rates up to 2" (with 03z HRRR suggesting 1.25"/15 minutes) may be intense enough to overcome the regionally high FFG values. A few urban locations along the path would be more prone to these rates for scattered flash flooding concerns particularly San Antonio Metro. Of note, but a bit less certain, in the wake of the cluster there is a solid upstream remaining pocket of 1000-1500 J/kg of MUCAPE through the Big Bend/Lower Pecos Valley. While mid-level shortwave and ideal jet diffluence will be downstream, low level flow intersecting the flanking outflow has some solid potential for redevelopment. While not likely as strong as the initial cluster any totals of 1-2" additional would further expand those areas that were close to exceeding with the initial round and maintain a risk of localized flash flooding for a few additional hours. Gallina ...Please see www.wpc.ncep.noaa.gov for graphic product... ATTN...WFO...CRP...EWX...FWD...HGX... ATTN...RFC...FWR...NWC... LAT...LON 30869829 30849640 29899569 28839627 28649903 28880036 29250109 30000129 30189935