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DAY2SVR: Nws Storm Predic
From  Dumas Walker@21:1/175 to  All on Sun Feb  9 08:58:00 2025
 
 
 
ACUS02 KWNS 090636
 SWODY2
 SPC AC 090635
 
 Day 2 Convective Outlook
 NWS Storm Prediction Center Norman OK
 1235 AM CST Sun Feb 09 2025
 
 Valid 101200Z - 111200Z
 
 ...NO SEVERE THUNDERSTORM AREAS FORECAST...
 
 ...SUMMARY...
 Isolated thunderstorms are possible from the Edwards Plateau into
 central and northeast Texas late Monday night. Severe weather
 potential is low.
 
 ...Synopsis...
 Zonal flow east of the Divide will generally shift eastward Monday.
 A low-amplitude shortwave trough will lift northeastward through
 northern Mexico into West/Central Texas by Tuesday morning. At the
 surface, a cold front initially near the Gulf Coast will likely move
 slowly northward in response to the approaching trough. Modest
 mid-level ascent and weak low-level warm advection will occur late
 in the period from the Edwards Plateau into northeast Texas. As
 scattered showers develop overnight Monday, a few embedded
 thunderstorms may occur given the weak elevated buoyancy present.
 Though shear will be strong, the poor thermodynamic environment will
 keep potential for severe weather quite low.
 
 ..Wendt.. 02/09/2025
 
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From  Dumas Walker@21:1/175 to  All on Mon Feb 10 09:13:00 2025
 
 
 
ACUS02 KWNS 100630
 SWODY2
 SPC AC 100628
 
 Day 2 Convective Outlook
 NWS Storm Prediction Center Norman OK
 1228 AM CST Mon Feb 10 2025
 
 Valid 111200Z - 121200Z
 
 ...NO SEVERE THUNDERSTORM AREAS FORECAST...
 
 ...SUMMARY...
 Isolated to scattered thunderstorms are possible from the southern
 Plains into the lower Mississippi Valley on Tuesday. Severe weather
 is not currently anticipated.
 
 ...Synopsis...
 Broad upper-level troughing is expected to evolve over much of the
 West on Tuesday. A shortwave perturbation is expected to eject into
 the southern Plains late Tuesday into Wednesday morning. At the
 surface, a cold front should extend from the southern High Plains
 into central Texas before arcing northeastward along the upper Texas
 Gulf Coast and into the lower Mississippi Valley.
 
 ...Southern Plains to Lower Mississippi Valley...
 Precipitation is likely to be ongoing early Tuesday morning. Most of
 this activity will be occurring on the cool side of the boundary.
 This should reinforce the front, though some modest northward
 progression of warmer, moist air may occur within the coastal plain
 regions. Potential for surface-based storms south of the boundary in
 southeast Texas/Sabine Valley vicinity appears low as the low-level
 jet will weaken during the morning/afternoon and mid-level ascent
 will be weak. Furthermore, forecast soundings indicate poor lapse
 rates in the column and warm layers that will inhibit updraft
 intensity. Overnight Tuesday into Wednesday morning, additional
 isolated to scattered storms are possible from the Edwards Plateau
 into Central/Northeast Texas as mid-level forcing and 850 mb warm
 advection increases. Again, these storms will be elevated on the
 cool side of the boundary. The strongest of these storms could
 produce small hail. The overall severe threat appears too
 isolated/uncertain for unconditional probabilities.
 
 ..Wendt.. 02/10/2025
 
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From  Dumas Walker@21:1/175 to  All on Tue Feb 11 09:53:00 2025
 
 
 
ACUS02 KWNS 110639
 SWODY2
 SPC AC 110638
 
 Day 2 Convective Outlook
 NWS Storm Prediction Center Norman OK
 1238 AM CST Tue Feb 11 2025
 
 Valid 121200Z - 131200Z
 
 ...THERE IS A SLIGHT RISK OF SEVERE THUNDERSTORMS FROM PARTS OF
 EASTERN LOUISIANA INTO CENTRAL/SOUTHERN MISSISSIPPI AND PARTS OF WESTERN/CENTRAL ALABAMA...
 
 ...SUMMARY...
 Severe storms will be possible Wednesday afternoon into Wednesday
 night from the Sabine Valley vicinity into far western Georgia.
 
 ...Synopsis...
 A shortwave trough pivoting through the southern High Plains will
 begin to intensify by Wednesday afternoon as it approaches the
 mid-Mississippi Valley. A surface cyclone will evolve along a
 southward-surging cold front in the southern Plains. The surface low
 will deepen more substantially by late afternoon in the
 mid-Mississippi Valley as it moves quickly north and east. Richer
 Gulf moisture will return into the Southeast and may reach as far
 north as portions of Tennessee. The cold front will sweep through
 the Southeast beginning in the late afternoon and into Thursday
 morning.
 
 ...Lower MS Valley/Central Gulf Coast States...
 Warm advection precipitation will likely be ongoing along the
 surface boundary Wednesday morning. Models vary on the spatial
 extent of precipitation with the ECMWF generally showing less
 clearing during the afternoon than other models. Available CAM
 guidance also shows similar variability. In terms of environment,
 low/mid 60s F dewpoints should reach through much of
 Alabama/Mississippi. Upper 60s F dewpoints are expected in southern Louisiana/Mississippi/Alabama, but could potentially push as far
 north as central Mississippi/Alabama as strong advection continues
 into the evening. Effective shear of 50-60 kts will favor organized storms/bowing segments. This shear will initially be roughly
 parallel to the front, but, as the front surges southeast, shear
 vectors will have a greater cross-boundary component. Strong
 low-level shear will also be in place with a 45-55 kt low-level jet
 moving from Louisiana during the morning into Mississippi/Alabama
 during the afternoon.
 
 The current expectation is for morning storms near the Sabine Valley
 to gradually intensify as they move northeast into a modestly
 destabilizing boundary-layer. How these storms evolve is uncertain.
 Damaging winds are a likely hazard, but, depending on storm mode and
 the degree of heating in Mississippi, could also pose a similar risk
 for tornadoes. Storms along the front are not likely to make much
 progress southeastward until the late afternoon. As the front moves,
 convective transport of the strong wind fields will promote damaging
 winds and strong low-level shear will bring a risk for embedded circulations/QLCS tornadoes. Discrete development ahead of the front
 during the evening is possible given strong theta-e advection and
 weak capping, but synoptic ascent will be displaced north which
 reduces confidence in that scenario. Surface-based storms become
 much less likely into Tennessee and Georgia.
 
 ..Wendt.. 02/11/2025
 
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