FOUS30 KWBC 250818
QPFERD

Excessive Rainfall Discussion
NWS Weather Prediction Center College Park MD
418 AM EDT Thu Jul 25 2024

Day 1  Valid 12Z Thu Jul 25 2024 - 12Z Fri Jul 26 2024

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

...Texas and Louisiana...

Current upper air and surface analysis across South TX indicates
the development of a weak surface reflection with a closed 85H
(850mb) low present as of the latest observations. This will play 
a significant role in the upstream convective potential through the
period, especially along the immediate TX coast from CRP up 
through the Southwest coast of LA. There's a near unanimous 
consensus on the latest 00z CAMs of a targeted area of significant 
rainfall within the region spanning from Matagorda Bay up to just 
south of Galveston during the first half of the forecast period. 
850mb low across South TX will slowly migrate to the northeast 
with a focused LLJ on the eastern flank of the circulation. The 
enhanced jet and increasing low level convergence under the 
surface and 850mb low(s) will generate a skinny axis of heavy 
rainfall with embedded convection given marginally sufficient 
MUCAPE located near the coast. 00z sounding out of KCRP was 
indicative of deep tropical moisture entrenched within the column 
as PWATs nestled just under 2.4", a solid 3 deviations above normal
and within the 99th percentile climatologically, just falling 
short of the daily maximum of 2.42". Regardless of a record or not,
the environment is indicative of a moist, tropical airmass that 
will exude efficient warm rain processes through any convective 
development and the evolving pattern this evening through the 
morning is one that will very likely promote intense rainfall 
locally within the confines of the surface and closed 850mb 
reflections. This setup will slowly migrate to the northeast during
the morning, but the setup for later this afternoon and the 
following evening still has the "jury out" on exactly how the 850mb
low behaves. 

As of now, the mean QPF output via the HREF and associated
ensembles are depicting a narrow axis of significant rainfall
totals extending from just northeast of Port Aransas up through
Galveston Bay and eventually hitting the Upper Texas coast near the
Sabine River, the same place that was just impacted recently from
significant rainfall yesterday. The probability fields for >3" of
rain are pronounced within that corridor, but the upper quartile
outcomes and associated neighborhood probabilities for at least 5"
(50-80%) and 8" (20-40%) are much higher further south along the
Middle TX coast with the bullseye situated around Port Lavaca up
through Matagorda with the former being the focal point for the
heaviest rainfall as of the latest model output. Further away from
the coast remains a question on the inland extent of the heavy rain
as the QPF from many of the CAMs and even some global deterministic
are all shying away from a larger protrusion inland with the focus
still remaining primarily at the coast. So much of this is
contingent on the behavior of the 850mb low as a longer 
maintenance of the low across the coast would likely enhance a 
secondary push of convection inland by nightfall thanks to a 
redevelopment of the LLJ aimed orthogonal to the coast after 00z 
this evening. Models that do have this outcome are more bullish in 
a larger impact footprint to the north as the low drifts that 
direction and allows for a greater inland focus to arise as we step
into the back end of the forecast period. These solutions also 
give credence to higher potential impacts for greater Houston, so 
that will be something to monitor in time where there could be 
adjustments to the current MDT risk forecast. 

For now, the main threat is tied closer to the coastal areas with 
the previous MDT risk generally maintained by expanded to the south
to the northeast of CRP, mainly from Matagorda Bay on northeast. 
The northeastern extent of the MDT was trimmed back across LA with 
guidance becoming less enthusiastic with the push of deeper 
moisture inland near Lake Charles and points north and maintaining 
a more confined coastal heavy rain threat, similar to where the 
impacts were felt this past forecast period. 

...Southeast into the Southern Mid Atlantic...

An intensifying upper jet across the Ohio Valley will extend into
the Northeastern U.S with a strengthening core upwards of 130kts
reflecting some fairly significant large scale ascent within the
right entrance region (RER) of the jet. At the surface, a cold
front will translate east and southeastward with progression
through the Mid Atlantic and the Southern Ohio Valley through the
period leading to some modest surface convergence along the front
with scattered to widespread convection out ahead of the boundary
thanks to the present large scale ascent from the aforementioned
jet. Sufficient low-level buoyancy located across Southern VA
through the Carolinas into the Deep South will promote an
opportunity of heavy thunderstorms with the highest probability
located over the Carolinas into Eastern Ga due to the presence of a
quasi-stationary front still bisecting the area. This will become 
a focal point for low-level convergence and will provide an anchor 
for storms to develop and slowly drift within the confines of the 
boundary. Rainfall rates of 1-2"/hr will be most common in any 
storm development, but a max of 3"/hr is still plausible given the 
low probabilistic output of 10-20% over a large portion of the 
Carolinas into far Eastern GA for those 3"/hr potentials. Mean QPF 
output via the HREF was solidly between 1-2" spatially with the 
individual CAMs output signaling some much higher local totals that
could exceed 4" in some cases, a much greater threat for flash 
flooding potential. 

Considering the incessant nature of the pattern the past week with
copious heavy rainfall episodes contributing to flash flooding
across the Carolinas, a SLGT risk from previous forecast was
maintained with a small shift on the western extent of the risk
area where the probabilities dropped off significantly for the
threat of flooding rainfall, carrying the signal closer to the 
SC/GA line than previous forecasts. 

...West...

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. 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. Neighborhood probabilities for the
higher convective totals >1" are still most prominent across AZ
with the focus areas being over the Mogollon Rim down through the
Southern terrain near the border where the probs are running
between 60-80% for the threat of at least 1". Secondary maxima are
popping up across the Inner Mountains west within Utah and Western
Colorado, but the threat is a little more subdued due to the lower
instability outputs that favor further south under the 500mb ridge.
Still, the moisture anomalies are forecasted to be best to the
north, so there could be some sneaky prospects for locally higher
impacts from convection, especially within the terrain and
adjacent valleys. 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


Day 2  Valid 12Z Fri Jul 26 2024 - 12Z Sat Jul 27 2024

...THERE IS A SLIGHT RISK FOR EXCESSIVE RAINFALL FOR PORTIONS OF
THE CAROLINAS...

...Carolinas...

The cold front from the previous period will finally make progress
off the eastern seaboard across the northern half of NC while 
making slow progress to the south through the rest of NC/SC region.
Scattered thunderstorms within the persistent deep moist and 
unstable environment will allow for a period of heavy rain 
potential, especially along and ahead of the cold front as it 
migrates southward. The heaviest rain will align over Eastern NC 
into the South Carolina Low Country, areas where FFGs are a bit 
higher and potentially more difficult to flood. Previous rainfall 
has lowered the FFG indices, especially as you work from Columbia, 
SC to points northeast which plays a role in the current SLGT risk
maintenance. Ensemble QPF output is currently between 1-2" across
Southeast NC, including the Wilmington area extending down through
the Low Country and coastal sections of SC. Individual
deterministic output is as expected with some local maxima around
4" within any particular global member leading to ensemble bias
corrected means closer to 2-2.25" over the hardest hit areas. Did
trim back on the northern extent of the previous SLGT with
maintenance further south and southeast across central and eastern
SC up through Southeast NC where the front will slow in forward
progression and become a focal point for Friday afternoon
convection. Best threat for flash flooding will likely occur over
more urbanized zones due to the sandier soils present in the
confines of the current risk area which lead to the continuity, 
and not expecting any upgrades in the current setup. 

...Southwest through the Inner Mountain West...

Scattered thunderstorms within a favorable moist axis will linger
through the Southwestern U.S with the northern half of the
convective threat shifting further inland into the Interior before
hitting the proverbial wall at the Central Rockies. Any storm
within the period could exude heavy rainfall with rates generally
topping at 1"/hr, an intensity that could easily cause issues
within the complex terrain out west. The increased moisture
advection back over NM will also open the door for more convective
threats within the remnant burn scars in place over the Sangre de
Cristos, so the MRGL risk was promptly positioned to cover for the
threat. General rainfall maxima is expected to be between 1-2" but
a small chance for locally higher remains, especially from any
cells that get anchored to the terrain. The previous MRGL risk was
kept to general continuity, but did pull the MRGL risk a little
further west into NV due to some linger convective potential from a
trailing shortwave migrating through the region during peak diurnal
instability, aligned with a further west QPF footprint as of the
latest NBM and ensemble bias corrected outputs.

...East Texas through the Lower Mississippi Valley...

Remnant mid-level energy will linger across Eastern TX into the
Lower Mississippi Valley within a persistent anomalous moisture
presence situated over the region. Sufficient buoyancy and
attendant large scale forcing will likely generate periods of
scattered convection capable of producing locally heavy rainfall
over the aforementioned areas. There are some indications that a
much more defined 500mb low will develop over the Southern Plains
which would increase the general forcing pattern allowing for a
more robust convective initiation over the eastern flank of the
mid-level circulation. This was noted via some of the 00z global
deterministic with the ECMWF being the most aggressive with the
solution. There are some hints of the threat becoming more
pronounced across East TX into parts of LA/AR given the recent GFS
Graphcast and ECMWF AIFS ML output, so a targeted upgrade may occur
over the above areas if the consensus grows and remains stable
in the upcoming model iterations. For now, a MRGL was maintained
from previous forecast. 

Kleebauer
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