


Flash Flood Guidance
Issued by NWS
Issued by NWS
416 AWUS01 KWNH 071746 FFGMPD NMZ000-072345- Mesoscale Precipitation Discussion 1167 NWS Weather Prediction Center College Park MD 146 PM EDT Tue Oct 07 2025 Areas affected...Central to Eastern New Mexico... Concerning...Heavy rainfall...Flash flooding possible Valid 071745Z - 072345Z SUMMARY...Scattered slow moving cells capable of 1.5"+/hr rates and totals over 2", especially near Sacramento Mountains posing localized incident(s) of possible flash flooding through evening. DISCUSSION...GOES-E Visible imagery shows the surface to boundary layer increased moisture indicated by banked up stratus east of the Sacramento mountains and through the saddle and into the far southern Sangre de Cristo Range. CIRA LPW and RAP analysis confirmed by surface Tds in the mid to upper 50s of this enhanced low level moisture with nose angling out of the Pecos River Valley. Solid upslope is deep enough to have bled through to the westward adjacent Rio Grande Valley with an effective dry line noted as Tds drop into the 20s/30s through the Black Mtn Range. Water vapor suite denotes an elongated shortwave across central AZ with a weak mid-level baroclinic leaf downstream into west-central NM angling out from the higher cirro-stratus in the sub-tropical jet that is centered across southern NM. The strong directional shear across the area has resulted in effective bulk shear into the 30-35kt range in central NM, suggesting organized, broader updrafts once destabilization occurs. Currently, the cloudy nature east of the terrain is limiting insolation but temps upstream of the terrain in the Rio Grande Valley are reaching mid-70s and where the moisture stream overlaps, SBACAPEs are starting to increase over 1000 J/kg. While upslope flow has not begun in earnest, the limited capping and weak divergence aloft at the entrance of the subtropical jet streak has resulted in some mid-level activity increasing as Lightning-cast Probability are reaching 60-75% over the next hour with some of the TCu features. Still believe this is a bit too early for the strongest updrafts, but these seeds could sprout earlier than the 20z expected destabilization noted in most of the recent Hi-Res CAMs. Low level winds should further back and strengthen to 15-20kts and further enhance deep layer convergence in the Sacramento Mountains. Initially anchored updrafts, may result in localized 1" totals, before expanding and slowly decoupling from the terrain. The bulk shear suggests some rotation which will further increase moisture flux convergence to support 1.5"/hr rates. RRFS is most aggressive, but does not seem unreasonable, especially representation of convective mode. These cells are in general proximity to burn scars near Ruidoso and any overlap is more likely to result in FF, but that precision is not capable at this time scale but locals should remain weather-aware. As the afternoon progresses to evening, as upstream shortwave slowly drifting northeast into NW NM toward the late evening, upslope flow is expected to continue and strengthen through/westward past the terrain and expand convective initiation further north and west with time. Spots of 1-2" in hard pan ground conditions may result in additional localized incidents of flash flooding. Gallina ...Please see www.wpc.ncep.noaa.gov for graphic product... ATTN...WFO...ABQ...EPZ...MAF... ATTN...RFC...FWR...TUA...NWC... LAT...LON 35850583 35650481 34390379 33330365 32630441 32330510 32350589 32900652 34020639 34720647 35260626