Subj : MESO: Nws Weather Prediction Center College Park Md To : wx-storm@lists.illinois.edu From : COD Weather Processor Date : Mon Jul 22 2024 17:55:28 AWUS01 KWNH 221755 FFGMPD LAZ000-TXZ000-222353- Mesoscale Precipitation Discussion 0693 NWS Weather Prediction Center College Park MD 154 PM EDT Mon Jul 22 2024 Areas affected...much of southern, central, and eastern Texas Concerning...Heavy rainfall...Flash flooding possible Valid 221753Z - 222353Z Summary...Widespread/numerous cell mergers are expected to produce brief heavy rain rates sufficient for flash flood potential through 00Z this evening. Discussion...With the onset of surface heating/destabilization, scattered to numerous shower and thunderstorm activity has materialized across the discussion area especially along and south of a surface boundary extending from near Shreveport westward to near Dryden (Terrell County), TX. Parts of this boundary have been augmented by convective activity that has grown upscale into small linear segments across west-central Texas. Additionally, deep convection has materialize across most of the Texas Coast within a weak warm-advection regime. Each of the storms are supported by mid to upper 70s F dewpoints and insolation, allowing for 1000-2000 J/kg MLCAPE to develop amid 1.9-2.2 inch PW values.=20 Weak steering flow aloft has allowed for slow and at times erratic cell movement, with loose organization along a couple outflow boundaries in west Texas and along the aforementioned front in central/east Texas. 1-2.5 inch/hr rain rates have also been noted per MRMS this morning. The ongoing scenario should continue through the early evening, with widespread thunderstorm development continuing. Multiple cell mergers are expected to prolong rain rates and contribute to spots of 2-3 inch hourly amounts at times. These rates are likely to cause excessive runoff in some areas - especially where FFG thresholds are less than 3 inches/hr and in urban areas.=20=20 Scattered thunderstorm activity is expected to persist until eventually most of the surface-based buoyancy is diminished due to convective overturning and loss of insolation. This process will take several hours to unfold, however, and may not completely unfold until after 00Z. Cook ....Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!7YWxLp97i_ggvretUD5aXU7pTijZfmn2jMzu0EtqRXqHd-HgzmO72wCIEkY3XB6HCQlk= k444PYM_i3lH1WeIFMJE51A$ for graphic product... ATTN...WFO...CRP...EWX...FWD...HGX...LCH...SHV...SJT... ATTN...RFC...WGRFC...NWC... LAT...LON 32399498 32029391 30999355 30069385 29309493=20 28609688 28369949 28750056 29500113 30460117=20 31110020 32019738=20 =3D =3D =3D To unsubscribe from WX-STORM and you already have a login, go to https://lists.illinois.edu and use the "Unsubscribe" link. Otherwise email Chris Novy at cnovy@cox.net and ask to be removed from WX-STORM. --- SBBSecho 3.20-Linux * Origin: capitolcityonline.net * Telnet/SSH:2022/HTTP (1:2320/105) .