


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
793 AWUS01 KWNH 312031 FFGMPD NJZ000-PAZ000-DEZ000-MDZ000-VAZ000-DCZ000-WVZ000-010100- Mesoscale Precipitation Discussion 0836 NWS Weather Prediction Center College Park MD 430 PM EDT Thu Jul 31 2025 Areas affected...Portions of the Mid-Atlantic Concerning...Heavy rainfall...Flash flooding likely Valid 312030Z - 010100Z SUMMARY...Numerous flash floods likely as multiple rounds of storms with embedded cell mergers cause localized rainfall rates as high as 4 inches per hour. Urban and small stream flooding threat increasing through DC and Baltimore. DISCUSSION...Multiple rounds of storms have developed with one round of storms in the Shenandoah Valley, a second near the I-95 corridor from DC to Baltimore, and a third from the Delmarva Peninsula through southern New Jersey. By far the most impressive rainfall rates have been with the cluster in New Jersey, where over 4.5 inches per hour rates have been noted. Fortunately for most of the rest of the area, rates have been a bit lower, generally between 2-3 inches per hour with the strongest storms. The storms have been organizing into the aforementioned lines, but their outflows and boundaries from previous storms are frequently allowing for separate cells to develop in between the lines and merge into them, resulting in long-duration extremely heavy rainfall for some areas, such as in central New Jersey. Going forward, the greatest potential for additional cell mergers and training is across northern Virginia and central Maryland, where a period of sunshine noted on satellite has effectively raised the surface based instability over that area to over 2,500 J/kg, even though some areas have already seen rain from storms earlier today. This higher instability is supporting the storms retrograding west to the north and west of DC and Baltimore, as the storms follow the greatest instability. However, with the overall movement of the storms towards the east, this has locally supported training and prolonged duration of heavy rain near and over those metros and their suburbs. HiRes guidance suggests the 3 (or at least the western 2) boundaries will eventually merge together into a cluster before the whole complex weakens and moves east upon consuming the aforementioned bubble of higher instability. This should finally allow the cold front driving much of the forcing to the north to push through the DMV and end the heavy rain and flash flooding threat. Meanwhile further north across New Jersey, the cold front is more progressive towards the east, so the storms should continue to push south and east and largely end the threat from Philly northward sooner. Wegman ...Please see www.wpc.ncep.noaa.gov for graphic product... ATTN...WFO...AKQ...CTP...LWX...PHI... ATTN...RFC...RHA...NWC... LAT...LON 40467440 40367411 40017412 39457441 39137460 38937483 38447518 38377630 38347709 38167789 38027862 38197943 38377923 38797899 39007858 39407816 39677793 39957748 39937710 39907572 40197501