AWUS01 KWNH 240540
FFGMPD
MOZ000-ARZ000-OKZ000-KSZ000-241135-
Mesoscale Precipitation Discussion 0129
NWS Weather Prediction Center College Park MD
138 AM EDT Fri Apr 24 2026
Areas affected...Central to Northeast OK...Far Southeast
KS...Southwest MO...Northwest AR
Concerning...Heavy rainfall...Flash flooding likely
Valid 240538Z - 241135Z
SUMMARY...Backbuilding and training thunderstorms producing 1.5 to
2.5 inch/hour rainfall rates will pose a significant urban flash
flood threat across northern to northeast Oklahoma early this
morning. Convection will eventually grow upscale into an MCS and
track east-southeastward into the Ozark Plateau through dawn.
Broad totals of 2 to 4 inches are expected, with localized amounts
possibly exceeding 5 inches.
DISCUSSION...Latest radar and satellite trends depict a highly
active convective environment across northern Oklahoma.
Thunderstorms are continuously backbuilding and training along a
well-defined mesoscale outflow boundary, positioned east of a
dryline and ahead of a surface wave transiting a cold front. The
thermodynamic and kinematic environment is exceptionally
supportive of extreme rainfall rates. A strong 40 to 50+ kt
southwesterly low-level jet (LLJ) is impinging directly onto the
outflow boundary, providing intense moisture convergence and
tapping into a robust instability pool characterized by 2000-3000
J/kg of MUCAPE. Furthermore, upper-level divergence associated
with an ejecting trough is providing deep-layer ascent to sustain
robust convective updrafts.
Currently, this setup is fostering high-efficiency rainfall rates
of 1.5 to 2.5 inches/hour. Given the quasi-stationary nature of
the boundary and the parallel alignment of the convection to the
deep-layer steering flow, persistent cell-training is occurring.
This will pose a significant, localized flash flood threat over
the highly sensitive urban footprints from Stillwater through the
Tulsa metro over the next few hours.
As the cold pool eventually strengthens and coalesces, convection
is expected to grow upscale into an east-southeast propagating
MCS. However, the strong southwesterly LLJ will continue to favor
persistent backbuilding on the southwest flank of the convective
mass, effectively slowing the forward translation of the heaviest
rainfall cores. High-resolution guidance (including the HRRR and
00Z HREF) supports widespread 2 to 4 inch totals, but given the
prolonged training potential, localized storm totals up to 5+
inches are highly probable.
Towards sunrise and through the 12Z time frame, this complex will
push into the Ozark Plateau across southwest Missouri and
northwest Arkansas. As the low-level flow interacts with the
complex topography of the Ozarks, mechanical lift will sustain
high rainfall rates. The steep, flashy basins of this region will
be highly susceptible to rapid runoff from these accumulations,
carrying a localized flash flood threat right through the morning
commute.
Orrison
...Please see
https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!87rVcEPmsU9ex1Yk0K8aWF2Pb8232nBhVf7ItOCXLPVZNzMyriOrFzStjEF4-wbQlPKD= d_jNmt4E0BBYixOlqowwVpI$ for graphic product...
ATTN...WFO...ICT...LZK...OUN...SGF...TSA...
ATTN...RFC...KRF...ORN...TUA...NWC...
LAT...LON 37729347 37429237 36579207 35939265 35409427=20
35209635 35369772 35869835 36199831 36419785=20
36719636 37279469=20
=3D =3D =3D
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