


Flash Flood Guidance
Issued by NWS
Issued by NWS
Versions:
1
2
3
4
5
6
7
8
9
10
11
12
13
14
15
16
17
18
19
20
21
22
23
24
25
26
27
28
29
30
31
32
33
34
35
36
37
38
39
40
41
42
43
44
45
46
47
48
49
50
100 AWUS01 KWNH 140746 FFGMPD TXZ000-141300- Mesoscale Precipitation Discussion 0681 NWS Weather Prediction Center College Park MD 346 AM EDT Mon Jul 14 2025 Areas affected...South-Central Texas...Southern Edwards Plateau... Concerning...Heavy rainfall...Flash flooding possible Valid 140745Z - 141300Z SUMMARY...Continued flash flooding risk through dawn given strong moisture flux and slow moving/potentially training convection. DISCUSSION...GOES-E WV suite shows stubborn elongated mid-level trough axis across North Texas into the Hill Country and eventually into the South-central Texas Rio Grande Valley. Earlier convective complex developed an MCV currently located along the Rio Grande just west of NW Kinney county; the outflow boundary has kicked eastward and while generally parallel to strengthening LLJ (15-20kts), some weak backed flow is providing sufficient convergence along the upwind edge to develop north-south bands of convection within the remaining 1500-2000 J/kg of MLCAPE well along the eastern hemishpere of the larger mid-level circulation just NW of the MCV over the NE Serrania del Burro Range. Northward expansion of the convection is expected given solid speed convergence into the deeper SW to NE shear axis. Total PWats of 2-2.25" will support efficient rainfall production with rates of 2-3" likely; while initially narrow, broadening of the updrafts should come with storm scale enhancement/interaction. The back-building, south to north training may even allow for some narrow areas of 3-5" totals, which may spread north into Real/Bandara counties with time and perhaps with low confidence even toward lower FFG values in the southern Edwards Plateau/Hill Country from Sutton to Kimble county. Strong latent heat release into the mid-levels should support strengthening of mid-level height-falls and tightening of the vorticity center westward. This should back low-level flow and increased convergence back westward away from the southern Hill country toward Kerr, Gillespie counties and sparing the more sensitive areas, reducing low level convergence in that area and therefore from potential of the strongest cells/highest rates. However, there is enough suggestion a few showers/cells could reach these areas and so are included at much lower confidence toward flash flooding incidents in those areas...however, at the cost of increased totals further west over higher FFG values/drier soil conditions. Gallina ...Please see www.wpc.ncep.noaa.gov for graphic product... ATTN...WFO...CRP...EWX...SJT... ATTN...RFC...FWR...NWC... LAT...LON 30969928 30929856 30419837 29509896 28569904 28199922 28019969 28190017 28890071 29440114 30120119 30680064 30949974