Mesoscale Precipitation Discussion 0647 NWS Weather Prediction Center College Park MD 534 AM EDT Thu Jul 18 2024 Areas affected...Hill Country of Texas east through the Piney Woods Concerning...Heavy rainfall...Flash flooding possible Valid 180934Z - 181400Z Summary...A corridor of thunderstorms with heavy rainfall will continue to drop southward through the morning along a nearly stationary front. These thunderstorms will contain rainfall rates of 2-3"/hr, which could produce locally more than 4" of rain. Flash flooding is possible. Discussion...The regional radar mosaic early this morning indicates an expanding line of thunderstorms from far western Louisiana through central Texas. These storms are developing along a stationary front which should sag slowly southward as a weak cold front later this morning. North of this boundary, a potent shortwave noted in WV imagery and in SPC RAP Differential Vorticity fields is spinning southward, enhancing lift in a region already favorable through isentropic upglide of a modest LLJ and beneath a subtle mid-level deformation axis. Thermodynamics across Texas remain supportive of heavy rainfall, with PWs measured by GPS of 1.9 to 2.1 inches collocated with MUCAPE exceeding 2000 J/kg. The overlap of ascent into this airmass is providing the favorable conditions for increasing thunderstorm development, and recent radar-estimated rain rates from KGRK WSR-88D have been as high as 2.5"/hr. The CAMs this morning all offer differing solutions to the evolution of this convection, but while spatial coverage and footprint vary, the intensity is well aligned among the various models which increases confidence in a heavy rain event. The 850mb LLJ is already beginning to slowly veer as noted in regional VWPs, and is expected to become westerly by late morning. This will limit the isentropic ascent and slowly reduce moisture transport northward, but will also then become more aligned to the advancing front, helping to turn the mean cloud-layer 0-6km winds parallel to the front as well. Additionally, the propagation vectors will become increasingly anti-parallel to the mean flow as the LLJ veers, suggesting continued backbuilding of echoes to the SW and along the front into the greater instability. With both HREF and REFS probabilities for 2"/1hr accumulations reaching 40%, this could result in 2-3" of rain along the boundary, with locally 4+" possible as noted by the neighborhood probabilities. The discussion area was drawn to somewhat emulate the EAS probabilities which are highest across the Hill Country, Balcones Escarpment, and along portions of I-35. Recent rainfall across this region has generally been below normal the last 7 days according to AHPS, but locally, NASA SPoRT 0-10cm RSM is above 70%. This indicates that some infiltration of heavy rain is likely, which is reflected by the higher FFG and corresponding 3-hr FFG exceedance probabilities peaking at just 10-20%. However, the favorable setup for training of 2-3"/hr rain rates could still overwhelm soils, especially in urban areas or the across any more sensitivesoils, leading to rapid runoff and instances of flash flooding. Weiss ATTN...WFO...EWX...FWD...HGX...LCH...SHV...SJT... ATTN...RFC...LMRFC...WGRFC...NWC... LAT...LON 31969389 31959322 31719285 30559369 30129502 29899686 29939839 30429957 30880043 31290077 31570017 31709930 31719830 31789713 31819532Download in GIS format: Shapefile | KML
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