FOUS30 KWBC 270053
QPFERD
Excessive Rainfall Discussion
NWS Weather Prediction Center College Park MD
853 PM EDT Mon May 26 2025
Day 1
Valid 01Z Tue May 27 2025 - 12Z Tue May 27 2025
...THERE IS A SLIGHT RISK OF EXCESSIVE RAINFALL FROM CENTRAL TEXAS
TO THE GULF COAST AND THE SOUTHEAST U.S. STATES...
01Z Update...
Despite uncertainty displayed by the latest runs of the HRRR and
RRFS...the previous outlook required only minor adjustments. Split
the Slight Risk area across the Gulf coast and Southeast U.S. into
two areas. The Southeast U.S. area was a bit more uncertain...but
there was a consistent enough signal from the HRRR to warrant an
expansion of the Slight Risk area to cover parts of eastern Georgia
and a small part of neighboring South Carolina given a bit stronger
low level convergence than depicted by earlier runs...as much a
result of high pressure to the northeast being a bit stronger and
keeping more of a northerly component to the wind across the
Carolinas. The higher-end Slight Risk area was still on-track
across Texas based on early-evening radar and guidance continuing
to show expansion later this evening as southerly low level flow
accelerates a bit and the potential for repeat convection/training
increases. Only other change was to pull the Marginal Risk area off
of the highest terrain of the Rockies given the loss of daytime
heating.
Bann
16Z Update...
The 12Z HREF guidance including recent runs of the HRRR and RRFS=20
reflect considerably uncertainty with the finer scale/mesoscale=20
evolutions of much of the convective threat involving the southern=20
High Plains/Texas and also areas downstream across the Gulf Coast=20
states. However, generally the consensus suggests an active period=20
of convection with high rainfall amounts possible this evening and=20
into the overnight period across areas of central TX and the Hill=20
Country where recent HRRR/RRFS runs suggest locally significant=20
rains of 5+ inches where intersecting outflow boundaries with=20
substantial instability along their leading edges will noted. The=20
Slight Risk area has been pulled farther southwest to account for=20
this.
Elsewhere, the Marginal and Slight Risk areas farther north have
been trimmed to account for where heavy rainfall has ended or will
be coming to an end soon, and also where the airmass is much more
stable. However, the Slight Risk area has been extended farther
east across the Gulf Coast states where the ongoing MCS/MCV
activity should continue eastward while interacting with plenty of
moisture and instability along an east/west oriented frontal zone.
Orrison
Previous Discussion...
...Texas through Southern Ohio Valley...
The current pattern will yield another round of appreciable
rainfall within the confines of a wavy quasi-stationary front
positioned over the Southern Plains, east towards the Southeast
U.S. coast. This evening is quite active with multiple convectively
driven outflow patterns with broad attendant cold pools helping to
maintain thunderstorm longevity from Northwest TX through the Red
River Basin extending into MS/AL. The western half of the setup
this evening will be the precursor to "round 1" of anticipated
heavy convection across TX through the ArkLaTex tomorrow morning
with greater coverage occurring by the afternoon as large scale
ascent increases once again within the diffluent region of an
approaching trough axis. The whole flash flood scenario is
contingent on the behavior of various cold pools and the overall
positioning of the stationary front, a complexity that can evolve
into a convective paradigm that can shift in a relatively short
period of time. In simplistic terms....the setup has a lot of
potential, but there will be some uncertainty in specifics with
regards to EXACTLY who gets how much rainfall during the period. Probabilistically, there is some merit to the threat with a broad
area extending from I-35 across Central TX to points northeast
through the ArkLaTex and AR/LA state line. This is coincident with
the higher probabilities for significant totals, as well as the
favored alignment of the quasi-stationary front for the forecast.
Tomorrow morning between 12-18z will be busiest over Central and
Northeast TX extending through the ArkLaTex as the cold pool merger
overnight across North TX will propagate east-southeast along the
tight theta_E gradient encompassing the stationary front in
question. As the complex moves east, the southwestern flank of the
boundary will fan out and become elongated south of I-20 with the
upshear side of the complex likely to induce some backbuilding when
assessing forecast soundings from the latest 00z CAMs indicating
easterly corfidi vectors with very slow mean cell motions typically
indicative of backbuilding potential. The mean flow will become
pretty much parallel to the boundary leading to heightened training
along the front, an output that is yielding some of the higher
local totals within the 00z hi-res suite (3-4+"), and associated
higher neighborhood probabilities for >3" within the 00z HREF prob
fields (50-80%) from I-35 north of Austin all the way across the
AR/MS state line. The >5" probs are not as robust comparatively,
but still signal 20-35% bullseyed along I-20 east of the DFW metro
to Shreveport. There is some indication that an MCV will originate
from the primary complex of thunderstorms over the northeastern
flank of the line that transpires overnight. If this were to occur,
local QPF maxima due to enhanced low and mid-level convergence
within the MCV confines would likely spur a heightened prospect of
flash flooding as the MCV makes headway across the Lower
Mississippi Valley. These types of setups are highly variable in
expectations, but the concept is there for possibly a secondary
max being depicted downstream of what will occur over TX.
There's also increasing favor of this complex exiting northeast
into the Southern Ohio Valley with areas of Western TN seeing a
convective flare up within proxy of the disturbance. These types of
patterns are very tricky but can yield higher end threats if they
materialize. The greatest threat will likely be places like Memphis
down into the MS Delta for flash flood potential considering the
expected path of the remnant complex. The SLGT from previous
forecast was relatively unchanged due to the threat.
The remainder of the period will be exhibit a large, remnant
outflow bisecting Central and Eastern TX with increasing large
scale ascent expected later in the afternoon and evening hours
Monday. Another round of convection will likely spawn in-of a
narrow theta_E ridge positioning across the Edwards Plateau up
through the Southeast Permian Basin and adjacent Concho Valley.
These cells will form and begin migrating eastward with scattered
development likely to grow upscale and impact areas of Central and
Eastern TX again during the evening and overnight period of D1.
There's still some discrepancy on exactly how the convective threat
will unfold, but given the current depiction, some overlap of
locally enhanced precip would cause some problems for those that
saw impacts earlier in the period. As a result, a higher-end SLGT
risk is positioned over Central TX, including the Austin metro
through the ArkLaTex and along that Southern AR and Northern LA
zone previously mentioned. These areas have the greatest threat for
overlap and/or significant rainfall totals from enhanced rates in a
favorable synoptic pattern and mesoscale environment.
...Southern/Central Rockies and High Plains...
Another area to focus will lie over Northeast NM through the TX
Panhandle where energy ejecting out of the Southern Rockies will
likely spur another round of convection tomorrow morning with the
main energy sliding east into OK/KS with more thunderstorm threats
impacting areas that have been hit the last couple days. The
overall impacts are not expected to be as prolific as the previous
setups with the energy moving fairly progressively and away from
the surface reflections that have garnered more training activity.
This is round 1 for this particular area as more convection is
expected to spawn off the Southern Rockies and move east late-
afternoon and evening as upstream trough will kick east acting as a
trigger for more convective initiation. The back to back nature of
the precip after getting hit pretty solidly today will offer some
mid-range flash flood prospects, but the overall progressive nature
of the cell motions should curb higher end flood scenarios. The
MRGL risk was maintained over those above areas with the risk
extending up through the lee-side of the Rockies in NM and CO with
the northern periphery through the Southeastern-most Front Range of
WY.
...Southeast Coastal Plain...
Another round of heavy convection is forecast across the South
Carolina Low Country as weak mid-level energy moves in from the
west and interacts with a progressing sea breeze boundary that will
propagate inland between Charleston to Savannah. There's some
discrepancy on timing, but the chances for 3-6" locally are
elevated when assessing the 00z HREF neighborhood probs and the
blended mean output between 2-3" in a narrow corridor between the
two coastal urban centers. Sandier soils will likely limit
extensive flash flood prospects, but the there is certainly a
chance a quick 3-6" to inundate local areas that get under
persistent thunderstorm activity. A MRGL risk remains from previous
forecast given the threat.
Kleebauer
Day 2
Valid 12Z Tue May 27 2025 - 12Z Wed May 28 2025
...THERE IS A SLIGHT RISK OF EXCESSIVE RAINFALL ACROSS PORTIONS OF
THE OHIO VALLEY, SOUTHEAST U.S., AND TEXAS...
2030Z Update...
Changes to the D2 ERO for this cycle include expanding the
Marginal and Slight Risk areas up across the coastal plain of the
Southeast where proximity of a frontal zone with strong instability
and rather anomalous moisture pooling along it will be in place as
upstream shortwave energy arrives. The 12Z guidance suggests a wave
of low pressure developing along this front which may enhance the
moisture convergence and overall concentration of convection near
the NC/SC border region. Some hires models suggest enhanced
rainfall totals (5+ inches) impacting portions of this area, but
confidence is limited with respect to the details given proximity
to the coast.
Elsewhere, some southward expansion of the Slight Risk area down
into the Cumberland Plateau was accommodated given potential for
at least a narrow instability axis and corridor of strong moisture
convergence for multiple bands of convection to focus here. This
will further be aided by orographics and could support sufficient
rainfall for some scattered areas of flash flooding.
A Marginal Risk area was added to portions of the central High
Plains (eastern CO and western KS) where a narrow axis of
instability along with upslope flow into eastern slopes of the
Rockies/Front Range will initially drive a convective threat over
the terrain with potential for some small-scale MCS
development/evolution downstream into the High Plains. Locally a
couple inches of rain may fall with this, and thus will pose an
isolated threat for some runoff issues.
Orrison
Previous Discussion...
...Ohio Valley...
Anticipating a period of scattered to widespread elevated
convective initiation across portions of the Ohio Valley on Tuesday
afternoon and evening with emphasis on the area encompassing
Northeast KY up through the western half of WV and portions of
Western MD. Complexities in the expected approach and magnitude of
a mid- level vorticity maxima ejecting northeast out of the
Tennessee Valley will create some uncertainty on specifics, mainly
the coverage and rates of precip occurring during the peak of
impact (21-06z), but ensemble mean QPF distribution has been
favoring a period of heavier convective premise in those above
zones. There's a distinct difference in the thermodynamic fields
within the global guidance with the ECMWF more favored for a tongue
of low-end MUCAPE up through the Central Ohio Valley into adjacent
valleys west of the Appalachian Front. A stronger upper speed max
will pivot northeast out of the Mississippi Valley with the nose of
the jet approaching the Eastern Ohio Valley towards nightfall. In
this scenario, the setup would likely yield some heavy precip for a
short time as the area enters a favorable RER jet dynamic that
would generate a round of enhanced precip before quickly shoving
off to the northeast. PWAT anomalies between +1.5 to +2.5
deviations across the region would be sufficient to support
localized heavy precip cores, especially in any elevated convective
cores. This setup is more likely to yield a quick 1-3" in any area
from Eastern KY up through the Western slopes of the Laurels
before diminishing, a forecast that would put this specific area
right on the cusp of the MRGL/SLGT risk threshold when assessing 3
and 6-hr FFG exceedance probs. Some of the areas of greatest
concern will be those smaller urban zones along I-79 in WV up
towards Cumberland, MD where poor drainage and funneling affects
can have considerable impacts for localized flash flood concerns.
Considering the inheritance of the SLGT from previous forecast,
have decided to maintain general continuity, but will keep an eye
on the setup closely to potential of expansion OR downgrades
pending the expected mid and upper level evolution as we get closer
in time.
...Southeast U.S...
Positioning of a persistent quasi-stationary front and advancement
of multiple shortwaves out of the Southern Plains will lead to
waves of convection across the Southeast with the footprint likely
situated from as far west as the Lower Sabine all the way into
western and central GA. This setup is pretty tricky overall as cold
pool mergers from previous convection will likely orient the front
differently than what is being depicted in the current guidance.
Despite the potential discrepancy, the environment is ripe for
enhanced convective cores with hourly rates between 2-3"/hr during
any stronger cells which then boils down where these occur. When
assessing the recent ensemble mean QPF, there's two areas of
favorability; one situated over the Lower Mississippi Valley from
LA through the southern half of MS, and the second positioned
across AL into Western GA. The QPF is less bimodal than you would
think, but the time frame of impact for each respective area will
generate slightly different results overall. The further west area
will be the benefactor of stronger low-level convergence along the
front with a peak maturation of the anticipated complex moving out
of TX. As the complex moves east, it will encounter a better
thermodynamic footing leading to convection refiring in-of the mid-
level perturbations path with scattered heavy convection situated
over AL into GA by the second half of the forecast. General maxima
between 2-4" with locally higher is forecast in either zone with
the best threat of flash flooding likely within the confines of the
boundary, as well as over any urban footprints. A SLGT risk was
added to account for the above threat, but look out for small
shifts in the coverage area of the SLGT in the coming updates as
CAMs get a better handle on the forecast upstream that will have
implications further into the period.
...Texas...
A strong mid-level shortwave will eject out of Coahuila thanks to
the affects of a migrating shortwave trough situated over the
Southwestern U.S. A significant uptick in convective development
across the Serranias del Burro will ultimately lead to heavy
thunderstorms plowing east out of Mexico, eventually impacting the
Lower Trans Pecos, Stockton Plateau, and eventually the Edwards
Plateau after 00z. The area of great convective focus will be along
the Rio Grande south of the Big Bend over into the western Hill
Country where eventual cold pool mergers will lead to cell
conglomeration overnight Tuesday with heavy rain situated over
those more sensitive terrain areas south of I-10. Environmentally
speaking, there will be a abundance of instability available during
peak convective impact with a strong buoyant signature situated
from the Stockton Plateau to points southeast with a large span of
2000-4000 J/kg of MUCAPE in that expected zone. PWATs will be ~1
deviation above normal, a relatively favorable moisture regime that
can yield some elevated precip potential, albeit sort of capped in
higher potential. The main concern with the setup will occur
overnight where cold pool mergers can lead to cells maturing and
collapsing over the same area for several hours leading to
prolonged heavy rainfall. The initial surge of the convective
impacts will be most notable in the towns along the Rio Grande up
to the Stockton Plateau. Areas downstream over the hillier terrain
will be most susceptible to the eventual cold pool merger/decay
pattern with 2-4" of rainfall plausible in either of these impact
scenarios. Given the robust signature within multiple global
deterministic and ensemble mean QPF output, a SLGT risk was added
to encompass the above areas where the threat is the highest.
Kleebauer
Day 3
Valid 12Z Wed May 28 2025 - 12Z Thu May 29 2025
...THERE IS A MARGINAL RISK OF EXCESSIVE RAINFALL ACROSS MUCH OF
THE SOUTHERN AND CENTRAL HIGH PLAINS, AND PORTIONS OF THE GULF
COAST...
2030Z Update...
The inherited Marginal Risk areas will be maintained for the time
being, but noting that there will likely at some point be a need
for a Slight Risk to be embedded within potentially both Marginal
Risk areas. Heavy rainfall in particular may be rather concentrated
and impactful across areas of south-central TX early in the period
as a new MCS traverses the region and heads gradually toward the
coast and offshore. There is guidance led by the GEM regional,
UKMET and even the RRFS that suggests a strong MCV associated with
this will lift northeastward and potentially bring a heavy
convective rainfall threat into areas of southwest to south-
central LA, but there is a relative lack of agreement spatially and
temporally regarding the exact details, so for now, the Marginal
Risk area will be maintained.
Over the central Plains, northwest mid-level flow will allow for
shortwave energy to drop southeastward and interact with the
pooling of increasingly moist and unstable return flow across the
region. This will favor an MCS that drops southeastward over the
region with impacts especially across parts of western KS and
northwest OK, but latitudinal differences are noted in the latest
guidance with respect to placement. Thus the Marginal Risk for now
will be kept here as well.
Orrison
Previous Discussion...
...High Plains...
Scattered areas of convection will occur on Wednesday afternoon
and evening across the Central and Southern High Plains with
locally heavy rainfall anticipated in any cell development. A
notable theta_E ridge will align from the Rio Grande up through
Southwest TX with the northern extension reaching the Eastern NM
portion of the Caprock. MUCAPE between 2000-4000 J/kg will be
positioned once again within the theta_E tongue during Wednesday
afternoon, just in time for an interaction with a weak shortwave
reflection moving into the area between 18-00z. Expect cells to
fire within the terrain of West TX, eventually drifting off the
topography and propagating into the adjacent Stockton Plateau and
Pecos River Valley as we move into the late afternoon and early
evening hours. Further north, a cells will fire in-of the
Sacramento Foothills and drift towards the western Caprock in
Eastern NM. A few cells will likely fire across the Caprock as well
given the favorable RER jet dynamics sprung about by the
approaching shortwave. This is a textbook MRGL flash flood risk
with scattered convective elements capable of impacts, both severe
and flooding in any given area.
Further north off the Colorado Front Range and Western KS High
Plains, cells will fire within a passing shortwave on the western
flank of a large closed ULL centered over the Midwest with mean
storm motions generally northwest to southeast out of the Front
Range. Expect cells to flow in that general motion with some
overlap of cells as they move through the area one after another.
The setup will end with the cold pool mergers eventually making it
into the TX Panhandle and rooting as they move away from the
primary forcing. Locally heavy rain will be plausible in the setup
with some guidance showing upwards of 3" during the setup. A low-
end MRGL risk was maintained from previous forecast highlighting
the threat and matches up with current ML First Guess Fields for
D3.
...Southeast U.S...
More thunderstorm activity will located within the confines of the
stubborn quasi-stationary front situated near the Gulf Coast.
Coverage and magnitude of potential convection is subjective to how
each deterministic output evolves the front and any shortwave
progressions nearby. Considering the bias corrected QPF mean of
2.5-3" in portions of the Southeast from the Upper TX coast to the
Central Gulf Coast, wanted to cover for the low-end threat with at
least MRGL risk and will assess as time goes. This is highly
variable pending eventual frontal placement and convective
evolutions upstream in the period prior. Areas of greatest concern
will likely be more urbanized areas where runoff capabilities are
highest.
Kleebauer
Day 1 threat area:
https://urldefense.com/v3/__https://www.wpc.ncep.noaa.go= v/qpf/94epoints.txt__;!!DZ3fjg!-VAm_cLiIIzbKaLAr5JnNIuHAYG7GyDxUcSbLETLh9l4= Iae8pORUyI-grpIEd1CVSOt6zvuGnrnZXDmZ4JO7Xzp7YrI$=20
Day 2 threat area:
https://urldefense.com/v3/__https://www.wpc.ncep.noaa.go= v/qpf/98epoints.txt__;!!DZ3fjg!-VAm_cLiIIzbKaLAr5JnNIuHAYG7GyDxUcSbLETLh9l4= Iae8pORUyI-grpIEd1CVSOt6zvuGnrnZXDmZ4JO77cjGwI8$=20
Day 3 threat area:
https://urldefense.com/v3/__https://www.wpc.ncep.noaa.go= v/qpf/99epoints.txt__;!!DZ3fjg!-VAm_cLiIIzbKaLAr5JnNIuHAYG7GyDxUcSbLETLh9l4= Iae8pORUyI-grpIEd1CVSOt6zvuGnrnZXDmZ4JO7Hv9_FTg$=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)