FOUS30 KWBC 240752
QPFERD

Excessive Rainfall Discussion
NWS Weather Prediction Center College Park MD
352 AM EDT Wed Jul 24 2024

Day 1  Valid 12Z Wed Jul 24 2024 - 12Z Thu Jul 25 2024

...THERE IS A MODERATE RISK FOR EXCESSIVE RAINFALL ACROSS THE UPPER
TEXAS COAST AND SOUTHWEST LOUISIANA...

...Texas and Louisiana Coast...

After coordination with the local Lake Charles and Houston WFO's, a
targeted Moderate Risk was issued across the Upper Texas coast into
Southwestern LA, including Galveston Island. At the surface, a
coastal trough is positioned just off the Upper TX coastal plain
with a deep moist axis aimed orthogonal to the coast between
Galveston up through the Lower Sabine Valley. The entire area
within the coastal plain is positioned within a very anomalous axis
of elevated moisture with PWAT deviations running between +3-4 from
CRP up through all of Southeastern TX into LA. 00z soundings out of
KLCH depict a very tropical airmass with a deep moisture presence
through the column, basically running from the surface to the
tropopause. Warm cloud layer depth is running around 15.5k feet, a
classic signature of heavy rain potential with a greater propensity
to exude very efficient rainfall rates from warm rain processes.
Even within any deep layer convection, this would spell trouble for
local rates breaching 2"/hr with the sampled environment generally
capable for upwards of 4"/hr within the stronger cell cores. The
latest HREF hourly rate probabilities are indicative of just that
with a corridor of elevated probability signatures between 25-40%
for rates exceeding 3" within the confines of the coast stretching
from Galveston up into places like Port Arthur/Beaumont as the
frictional convergence regime begins towards dawn this morning and
maintains prominence through the early afternoon before
dissipating. The probability fields for total rainfall were the
biggest signal for the risk upgrades with the HREF EAS outputs
considerably bullish within the 2" (45-60%) and 3" (15-30%)
markers. Considering the conservative nature of the EAS due to the
process which it's calculated, this is a significant output that is
typically reserved for those higher end potential events. 

Assuming the factors involved and the presence of deep, tropical
moisture advection off the Western Gulf, there was enough of a
signature for a MDT risk upgrade in the location with the highest
probabilities and mean QPF footprint indicating a solid 3-6" with
locally as high as 9" possible, indicated with the LPMM HREF. 

...Southeast to Southern Mid Atlantic...

The same quasi-stationary front that has been stuck in the Southern
Mid Atlantic down through the Southeastern U.S will continue to be
a boon for the the region as another round of heavy thunderstorms
will develop within an axis of elevated theta-E's located along the
boundary from LA to Southeastern VA. Several small impulses also
within the stagnant upper pattern will aid in the necessary upper
forcing to promote small cell clusters of storms capable of a
larger areal extent of heavy rainfall that would promote flash
flood concerns within more urbanized corridors across the South,
along with any slower moving convection that gets anchored to
lingering cold pools that are running rampant from the previous
days of convection. A deeper moisture flux will be entering into
the Deep South with an embedded stronger mid-level vorticity maxima
pivoting northeastward after it exits the Gulf. This will spur a
more organized convective cluster downstream over places like
MS/AL/GA. This is causing a well defined bullseye of higher precip
within that corridor and is represented within the probability
fields with the >3" neighborhood output hovering between 40-70%
extending from Southern MS across into the SC Low Country. The
previous SLGT risk was expanded further west to account for the
convective signatures all the way into LA. 

...Northeast...

A tongue of elevated theta-E's will be advected north on the lee
side of the upper trough pivoting through the Great Lakes. To the
southwest, a blossoming jet streak will develop over the Southern
Ohio Valley and begin nosing into the interior Northeast by later
this afternoon. At the surface, a cold front will be sweeping
eastward out of Ontario through Western NY and PA leading to
increasing low-level convergence within the axis of greater
instability. All this to say that scattered thunderstorms with
rainfall rates between 1-2"/hr will be plausible across the
interior with the highest chance for flash flood concerns within
Central and Upstate NY where the greatest merger of upper forcing
and repeated convective impacts will occur later this afternoon and
evening before the front kicks the threat downstream. HREF
neighborhood probabilities are generally high for at least 2"
across the Adirondacks back towards the eastern Finger Lakes. The
probabilities for at least 3" are still fairly modest within the
neighborhood output with a bullseye of 40-50% located over the
Adirondacks. The signals is scattered for the highest totals 
within the deterministic outputs, so the setup is right on the 
higher end of the MRGL and on the cusp of a small SLGT risk area. 
For now, maintained continuity but will note the threat of a 
targeted upgrade if the trends continue upwards in the next update.

...Midwest and Ohio Valley...

Surface low located over the Great Lakes will begin to occlude and
track northeast through Ontario with a trailing cold front swinging
through the Midwest and Ohio Valley later this morning and beyond.
A general consensus within the CAMs for a round of convection to
develop in-of IA and IL later this morning, spreading southeast
along the confines of the front. Flow will be modestly convergent
along the leading edge of the boundary with some favorable large
scale ascent caused by the northern half of the area sitting within
the left exit region (LER) of a blossoming jet max situated over
KY. Observing the latest forecast soundings off some of the CAMs
indicate a signature for locally heavy rainfall with some potential
training as the flow becomes a more parallel to the front as we
move into the evening hrs. The threat will not persistent however,
as the front will be on the move through the entirety of the
forecast. This has limited the overall potential of the setup to
mainly 1-2" maxes with perhaps as high as 3" as per the latest
HREF neighborhood probabilities of >3" settling between 15-25%
across portions of Central IL with lighter 5-10% markers further
east in IN/OH. This was enough for a continuation of the inherited
MRGL risk with only some minor adjustments necessary to reflect the
latest QPF and probability fields. 

...Southwest...

Scattered Monsoonal convection will continue for another period
across the Southwestern U.S with the primary heavy rain footprint
aligned within the Mogollon Rim up through the Great Basin. Areal
SBCAPE values will range from 500-1500 J/kg through a large extent
of the west with PWAT anomalies generally +1 deviations across AZ
and NM with +2 and +3 deviations aligned from Northern CA across
into NV. Highest moisture anomalies will advect eastward through
the period as a shortwave trough across the PAC NW begins to
flatten the northern extent of the ridge sending the more prominent
moisture anomalies into Northern NV, Southern ID, and Western UT.
Current QPF signature within guidance is relatively scattered when
it comes to the higher values, but some 1-2+" totals are likely
within the current setup with the best chance focused across the
Mogollon Rim and the terrain west of I-19 in Southern AZ based on 
the latest ensemble QPF output and probability fields. The MRGL
risk from previous forecast was maintained with only a few small
modifications to reflect the instability gradient and forecast QPF
footprint. 

Kleebauer


Day 2  Valid 12Z Thu Jul 25 2024 - 12Z Fri Jul 26 2024

...THERE IS A SLIGHT RISK FOR EXCESSIVE RAINFALL ACROSS PORTIONS OF
SOUTHEAST TEXAS AND SOUTHWEST LOUISIANA, AS WELL AS PORTIONS OF THE
SOUTHEAST AND SOUTHERN MID ATLANTIC...

...Texas and Louisiana...

A continuation of the pattern from the previous period will lead to
more shortwave impulses exiting out of the western Gulf as they
navigate northward between a broad upper trough to the northwest
and the persistent ridge off the southeast in the Gulf and Western
Caribbean. Unlike today, the pattern has less definition to the
heavy rain threat with a more inland protrusion of the heavy rain
footprint when assessing the deterministic globals and ensemble
based QPF. There will likely be an area between the Middle TX coast
up through the Sabine River Valley that will experience some
significant rainfall potential so long as the upper pattern remains
favorable based in the model output. Verbatim, the threat is likely
to impact areas a bit further down the TX coast with the area from
Matagorda up through Houston the primary target initially with the
QPF maximum generally aimed within that corridor on most
deterministic and ML output. Current forecast for 1-3" areal
average is a good base to start prior to having some benefit from
the future CAMs that will be able to exhibit better defined
convective characteristics given the favorable mesoscale cores and
resolution. Expectation is for another round of locally heavy rain
with potentially some significant flash flood concerns within the 
hardest hit zones as local maximum could climb upwards of 6" if the
pattern holds. The PWAT anomalies between +2-3 deviations will 
still linger across all of Southeast TX through much of LA, 
continuing the prominent warm rain processes that will allow for 
efficient rainfall accumulations. The previous SLGT risk was 
maintained with only some minor adjustments to the norther fringes 
to align with the trends of a further inland protrusion of the 
heavier precip signals. The risk is a higher end SLGT within the 
coastal plain just north of CRP up into Southwestern LA. 

...Southeast to Southern Mid Atlantic...

A cold front will migrate to the southeast pressing through the
southern half of the Mid Atlantic while the at the upper levels a
130kt jet streak will be passing over New England leading to better
large scale forcing within the RER of the jet across the
aforementioned area. Ample pre-frontal instability within anomalous
deep layer moisture will also contribute to the favorable
environment for heavy rain potential, especially as the front
approaches and enhances low-level convergence within the confines 
of the boundary. After destabilization will aid in priming the 
environment prior to the fronts approach with the initial area of 
interest lying over Southeastern VA, eventually shifting focus into
the Carolina's as the front progresses south. This is the area of 
greatest significance given the best surface to upper level forcing
presence working in tandem to create a period of widespread heavy 
rainfall. Ensemble QPF between 2-3" is common within the confines 
of the front from the Hampton Roads area down through Eastern and 
Central NC/SC with much of the rain occurring within a short time 
frame as the front approaches. This is a signature for heavy hourly
rates that will enhance the flood risk over the region. For that, 
the SLGT risk was maintained from the previous forecast.

Across the Southeast, deep moisture presence with several mid-level
perturbations entering the area through the period will assist in
maintaining a scattered thunderstorm signature with heavy rain
threats continuing thanks to the persistent elevated moisture
anomalies and ample instability. The threat is not as pronounced as
what will occur further to the north, but the setup is sufficient
for any cell producing flash flooding, especially over GA/SC where
the best instability is located. 

...Southwest and Southern Rockies...

Monsoonal convection will encompass much of the Southwest U.S with
primary coverage in the Great Basin as the mid-level ridge pattern
shifts focus to the west of the Four Corners. Modest moisture
anomalies and relatively formidable instability across much of the
region will allow for scattered thunderstorms with isolated heavy
rain cores that could spell issues if they fall along complex
terrain, burn scars, urban footprints, and slot canyons. The area 
of interest remains across the Mogollon Rim down into Central AZ
where Locally 1-2" with upwards of 3" is possible currently in 
that zone due to a stronger axis of instability under which could 
end of being near a 600dm ridge on Thursday afternoon. Across the
north, a more prominent moisture advection pattern will continue
through the Interior Mountain West as a shortwave trough over the
PAC NW continues to squash the northern extent of the ridge and
funnel the moisture further into the interior after it began
navigating out of the CA/NV. More widespread convective coverage is
forecast across UT/Southern ID/Western WY as a result leading to
an expansion of flash flood concerns within those areas. The MRGL
risk was generally maintained from previous forecast but did 
expand the risk slightly on the northern periphery to account for 
the moisture anomalies and accompanying forecast instability across
those northern zones.

Kleebauer
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