HVYRAIN: Excess Rain D1
From
Mike Powell@618:250/1 to
All on Tue Sep 16 10:04:01 2025
FOUS30 KWBC 160808
QPFERD
Excessive Rainfall Discussion
NWS Weather Prediction Center College Park MD
408 AM EDT Tue Sep 16 2025
Day 1 Valid 12Z Tue Sep 16 2025 - 12Z Wed Sep 17 2025
...THERE IS A SLIGHT RISK OF EXCESSIVE RAINFALL OVER PORTIONS OF
NORTHEASTERN NORTH CAROLINA AND SOUTHEASTERN VIRGINIA...
...Northeastern North Carolina and Southeast Virginia...
Well-defined surface reflection off the NC coast will continue to
slowly move to the north over the course of the overnight and
morning hours before parking off the VA Capes as the initial
occlusion process takes shape. There's been a bit of a deviation
in the overall precip pattern from what has been forecast over the
past few forecast cycles, a lot of it driven from complex
convective dynamics that thwarted the initial low-level moisture
surge that was supposed to have already occurred according to older
forecasts. The previous convective cluster has since dissipated,
indicated via the rapidly warming cloud tops located just to the
north of the surface low center. As a result, have finally seen
bands of precip rotate inland with relatively modest rates as the
instability pool remains parked just offshore when assessing the
latest mesoanalysis. The trend is for a slow advection of
increasingly favorable instability to penetrate inland with the
alignment of the greatest forecast MUCAPE to be situated over far
northeast NC into the VA Tidewater. This is the area of interest
for the D1 when it comes to potential slow-moving convective
elements within the smaller deformation axis transposed on the
western flank of the cyclone. Some of the CAMs have been way too
aggressive with this feature and has allowed the HREF probs fields
to be heavily skewed into a more robust precip depiction compared
to what is current ground truth.
The HRRR/RAP combo has been handling the current evolution the best
of any CAMs member, and has certainly been outperforming most
global deterministic with the CMC the closest to what is occurring.
Considering the variables and complexity of the forecast, there
were some changes from the inherited SLGT risk across NC where the
western extension being removed allowing only the northeastern
corner of NC up into the VA Tidewater the only remaining locations
within the SLGT. This is subject to change pending on the
instability advection regime as rates will need to pick up in order
to secure a significant flash flood threat with the Hampton
Roads/VA Beach area the most prone to the risk due to urbanization
factors. Anticipating 2-4" with perhaps up to 5" within the
targeted SLGT risk as this remains the area with the best chance to
see heavy rain longevity with less of a threat the further away
from the coastal plain. Hourly rates maxed between 1-2"/hr are the
most likely scenario at this juncture, putting mainly a small area
of potential for flash flooding as sandier soils located outside
the VA Tidewater are likely to negate widespread flash flood
concerns. Considering how poorly the guidance is handling this
setup, near term monitoring will be employed over the course of the
period with the best threat likely occurring between 12-00z,
waning quickly in the evening as the low becomes vertically stacked
and favors a rapid occlusion leading to a degrading heavy precip threat.
...Southwest...
Scattered convective pattern will initiate later this afternoon
and the early evening hours before fading with the loss of diurnal
heating. Current progs are for convection to be tied closer to the
terrain across southeast AZ into southern NM with isolated
signatures of >1"/hr plausible in the stronger cell cores. These
areas generally prone to runoff due to terrain complexities, as
well as remnant burn scars present in some locations. There was
very little change from the inherited MRGL risk with the forecast
running close to general continuity.
...Central High Plains...
Strong shortwave trough ejection out of the interior Northwest will
lead to convective development and regional enhancement across the
Central High Plains. Greatest ascent is aligned with the diffluent
region of the mid-level shortwave with left-exit region dynamics
likely to maintain a prevalent heavy rain signature across the
western third of NE down into neighboring northeast CO and
northwest KS. Guidance has come into alignment with the axis of
heaviest precip centered near and just north of North Platte, NE
with the corridor extending south into southwestern NE and
northwest KS by the second half of the forecast period. 00z HREF
neighborhood probs for >3" are running between 20-40% across the
referenced area near North Platte and points south. This still
aligns well with the previous forecast MRGL risk leading to little
deviation in the current thinking. The areas of highest risk will
likely be smaller towns and urbanized areas, like North Platte that
are more susceptible to runoff.
Kleebauer
$$
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From
Mike Powell@618:250/1 to
All on Wed Sep 17 08:51:24 2025
FOUS30 KWBC 170758
QPFERD
Excessive Rainfall Discussion
NWS Weather Prediction Center College Park MD
358 AM EDT Wed Sep 17 2025
Day 1 Valid 12Z Wed Sep 17 2025 - 12Z Thu Sep 18 2025
...THERE IS A SLIGHT RISK OF EXCESSIVE RAINFALL FOR WESTERN AND
CENTRAL SOUTH DAKOTA...
...Northern and Central Plains...
A broad mid-latitude cyclone will continue to impact a large
portion of the Plains over the course of Wednesday into Thursday
with multiple areas of heavy rain plausible given a variety of
dynamical and thermodynamic processes. The area with the greatest
concern is likely within the well-defined axis of deformation that
is forecast to materialize across the western half of SD leading to
scattered flash flood concerns thanks to wet antecedent conditions
in wake of a previous disturbance that distributed copious amounts
of rain to areas along and west of the Missouri River. Guidance is
in agreement on the threat for 1-3" over the area extending from
the river over to the SD/WY state line, delineating the deformation
structure forecast to materialize within the northern and western
half of the cyclone situated over NE. FFG's on the order of 0.5-2"
between 1/3/6 hr. intervals are running much lower than climo
leading to a lower threshold to breach that could very well cause
issues across that broad area of western SD. 5 and 10-year ARI
exceedance probs are running between 50-80% and 30-60%,
respectively between the two intervals, a solid representation of
at least some scattered flash flood concerns with perhaps a broader
scope of impact considering the areal footprint of the
probabilities in question. Rates will be ~1"/hr at peak intensity,
but could very well last for multiple hours due to the anticipated synoptic scale evolution of the surface lows slower forward propagation
speed leading to training over a large area of SD down into
northwest NE. In this case, the previous SLGT risk was maintained
with some minor expansion on the edges to account for the latest
probabilities and HREF blended mean QPF output.
By the afternoon and evening, defined warm conveyor belt (WCB) will
be situated across much of the Missouri River basin extending from
OK/AR up into eastern SD. A warm front will lift north and
transition to a quasi-stationary boundary across east-central SD
through south-central MN leading to a focused frontal alignment for
storms to materialize later in the period. This has been a trend
within the recent CAMs as convective initiation will likely be
spurred by the arrival of a shortwave pivoting around the eastern
flank of the primary ULL, generating a better large scale ascent
pattern focused downstream of the center of circulation. With dew
points expected to be in the 60s for locations within the defined
WCB, there will be room for scattered to widespread convective
development during afternoon and evening time frame as the
environment ripens with the typical diurnal heat flux. The frontal
positioning over the Northern Plains and Upper Midwest will be a
target for training convection as cells can become anchored to the
front and lead to localized areas of heavy rainfall that could drop
a quick 2-4" over a span of a few hrs. Rates between 1-2"/hr in
convection are likely in this setup for anywhere within the WCB
leading to a general maintenance of the MRGL risk across the
Plains, but have now expanded the MRGL risk eastward into MN to
account for the frontal alignment and growing threat of convection
spawning near and within the boundaries forecast location.
...Southern High Plains...
Multi-round convective episode anticipated across the southeast CO
Front Range down into the OK/TX Panhandles and adjacent northeast
NM beginning later this afternoon, carrying through the evening
hours. Lee side low over eastern CO/western KS will materialize
within the broad synoptic scale evolution occurring over the center
of the CONUS. A trailing cold front will drag south and southwest
through the above areas with an initial flare up of convective
activity this afternoon along the front creating a moment of
priming before a larger shortwave ejecting out of the Central
Rockies becomes the focus for later. Models are in agreement on
quite a strong mid-level vorticity ejection into the Front Range
late-afternoon and early evening today leading to a blossoming
convective initiation in-of the terrain just west of I-25 in
southeast CO. Storms will grow upscale and migrate eastward into
the Front Range, continuing to slide east-southeast as they deliver
locally heavy rainfall in their wake leading to an isolated to
scattered flash flood concern through the second half of the
forecast. This setup has been documented in some way over the past
several forecast iterations, but the threat is now clear in the
main show focused within the strong mid-level ascent pattern
generated by the shortwave rounding the trough base. Expect
localized totals of 2-3" in the hardest hit locations with a max of
up to 4" across the far southeast corner of CO down into the
northern TX Panhandle. This is reflected by the modest >3"
neighborhood probabilities in the latest 00z HREF suite, a solid
indicator for a MRGL risk maintenance from previous forecasts.
...Southwest...
Little change from the previous forecast as guidance maintains a
signal for another period of isolated to scattered convection
over the terrain encompassing southern AZ up through the central
and eastern portions of NM with the primary threat being heavy
rainfall situated over more complex terrain and burn scar remnants.
Assessment of forecast soundings and hodographs indicate
relatively slower cell motions, a classic characteristic for flash
flood prospects over the desert southwest. Guidance reflects local
1-2" totals scattered across the region extending from southeast AZ
into NM with some of the better signals focused within those
mountain ranges like the Huachucas and Sacramento's. The previous
MRGL risk was relatively unchanged considering the favorable run
to run continuity.
...Southeast Florida...
Broad cyclonic pattern across the eastern CONUS will aid in
advecting a relatively stout mid-level shortwave currently centered
along the northern coast of Cuba. IR satellite this evening shows
the disturbance is very well-defined with a centroid of cooler
cloud tops indicating scattered to widespread convective coverage
in-of the western Florida Straits at this hour. Considering the
south to southwesterly flow between the 850-300mb layer, the
expectation is for convection to move generally northeast with the
mean flow, ushering in a more focused area of forcing capable of
impacting all of South FL, including the Keys with heavy rainfall
at any point. PWATs are on the rise according to the latest 00z
RAOB's out of KMFL and KEYW this evening with a broad expanse of
1.9-2.2" PWATs over the region. Forecast is for PWATs to continue
to increase with an expectation of indices to settle between
2-2.3", a solid 1-1.5 deviations above normal when assessing the
latest NAEFS output. Guidance is keying in on the FL Keys to be the
primary focus for heaviest QPF during the forecast period, however
the environment is favored for any area situated south of I-4,
especially over southeast FL where sea breeze components and deep
moisture presence will lend to pockets of very heavy rainfall from
convection that develops over the area. These cells will be
scattered in nature, but the prospects for 2-3"/hr rates with
higher intra-hour rates across the urban corridor from Melbourne
down to Miami will make for at least a modest MRGL risk for
excessive rainfall over the next 24+ hours. The previous risk was
expanded north to include KMLB as hi-res trends are keying on a
convergent area north of where the previous risk forecast(s) have
been made.
Kleebauer
$$
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