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SPC Activity Chart
Hazard Mon (03/09) Tue (03/10) Wed (03/11) Thu (03/12) Fri (03/13) Sat (03/14) Sun (03/15) Mon (03/16)
Severe Slight Enhanced Slight No Area No Area No Area No Area No Area
Fire Critical Elevated No Area No Area Critical No Area No Area No Area

Forecast Discussion - Convective Outlook

   SPC AC 091630

   Day 1 Convective Outlook  
   NWS Storm Prediction Center Norman OK
   1130 AM CDT Mon Mar 09 2026

   Valid 091630Z - 101200Z

   ...THERE IS A SLIGHT RISK OF SEVERE THUNDERSTORMS THIS
   AFTERNOON/EVENING FROM ARKANSAS TO NORTHWEST GEORGIA...

   ...SUMMARY...
   Large hail, damaging winds and a couple of tornadoes are possible
   this afternoon/evening from the Mid-South into northwest Georgia.

   ...AR to north GA this afternoon/evening...
   A weak mid-upper speed max is cresting the larger-scale ridge and
   will move from AR to the TN Valley this afternoon/evening. 
   Associated/ongoing convection across AR will likely persist through
   the afternoon with some tendency for upscale growth, while spreading
   eastward along the northern gradient of boundary-layer dewpoints in
   the low-mid 60s.  Surface heating in cloud breaks, beneath the
   eastern extent of 7-8 C/km midlevel lapse rates, will contribute to
   moderate buoyancy (MLCAPE of 1000-1500 J/kg) along this corridor
   with minimal convective inhibition.

   Deep-layer vertical shear will be sufficient for a somewhat
   organized/bowing storm cluster to evolve from the ongoing AR storms
   as they spread across the TN Valley this afternoon, potentially
   reaching northwest GA by late evening.  The initial storms in the
   cluster will pose a threat for large hail (1-2"diameter), with some
   increase in the threat for wind damage from northern MS across
   northern AL/northwest GA.  More discrete storms will be possible
   immediately south of the MCS path this afternoon/evening as a
   maritime tropical air mass (68-72 F dewpoints) spreads inland.  Wind
   profiles will support supercells capable of producing large hail
   (some could exceed 2 inches in diameter).  A modest increase in
   low-level shear this afternoon, combined with rich low-level
   moisture and the possibility of lingering convective outflow from
   the ongoing storms in AR will also support the potential for a
   couple of tornadoes. 

   Isolated thunderstorm development may also occur farther southwest
   along the marine warm front into southeast TX, where there is a
   conditional threat for large hail.

   ...Southern AZ this afternoon/evening...
   High-based, low-topped convection is expected in the band of ascent
   immediately north-northeast of the closed low near northern Baja. 
   Low-level moisture will be somewhat limited, but steep low-midlevel
   lapse rates and substantial south-southeasterly deep-layer shear
   will support a few storms/clusters capable of marginally severe hail
   and gusts approaching 60 mph.

   ..Thompson/Chalmers.. 03/09/2026

    

   NOTE: THE NEXT DAY 1 OUTLOOK IS SCHEDULED BY 2000Z

        
   SPC AC 091727

   Day 2 Convective Outlook  
   NWS Storm Prediction Center Norman OK
   1227 PM CDT Mon Mar 09 2026

   Valid 101200Z - 111200Z

   ...THERE IS AN ENHANCED RISK OF SEVERE THUNDERSTORMS ACROSS CENTRAL
   ILLINOIS INTO NORTHWEST INDIANA AND ACROSS THE EDWARDS PLATEAU INTO
   CENTRAL TEXAS...

   ...SUMMARY...
   Scattered severe thunderstorms are forecast on Tuesday from the
   southern Plains into the southern Great Lakes vicinity. All severe
   hazards are possible.

   ...Synopsis...
   A bi-modal severe weather event is expected Tuesday afternoon and
   evening across the Mid-West and portions of central Texas.
   Mid-morning surface observations/analyses reveal a surface low
   migrating eastward across the upper Great Lakes with a trailing cold
   front draped southwestward into the central Plains. Weakening winds
   behind the front suggest that this boundary will begin to stall
   later today across the Midwest/central Plains. Meanwhile, returning
   moisture is forecast to spread north over the next 24 hours as
   surface pressure falls and southerly winds increase across the
   Plains with the approach of the upper trough currently meandering
   over Baja California and a slight amplification of the upper wave
   over the north-central CONUS. This will help establish an expansive
   warm sector from southern Texas northward into the central Plains
   and Great Lakes region, bounded to the north by the stalled frontal
   boundary and to the west by a weak dryline/Pacific front. Strong to
   severe thunderstorms are expected within this warm sector as ascent
   along the Midwest frontal zone and across the southern Plains
   increases with the ejection of the upper trough late Tuesday
   afternoon into Tuesday night.

   ...Midwest...
   The greatest regional severe threat will likely be focused along the
   frontal boundary Tuesday afternoon and evening. Most guidance
   suggests the stalled cold front will advance northward as a warm
   front as low-level southerly flow increases within the warm conveyor
   belt of a developing cyclone over IA/northern MO, but the exact
   placement and orientation of the boundary, and any potential
   influence by cool lake-breezes off lower Lake Michigan, remain
   uncertain given spread between 12z CAM and global guidance. 

   Regardless, strong isentropic ascent over the frontal zone coupled
   with ample low-level moistening and steepening mid-level lapse rates
   will support a convective environment favorable for well-organized
   convection along both the warm front and southwestward along the
   cold front across northern MO and KS. Effective SRH on the order of
   200-300 m2/s2 coupled with MLCAPE of 1500-2000 J/kg along/just south
   of the boundary will support the potential for tornadoes - including
   strong tornadoes - with any discrete supercell that can become
   established. Convection developing north of the surface fronts will
   still reside in a very favorable environment for elevated supercells
   capable producing large/very large hail (possibly in excess of 2
   inches). Upscale growth/clustering is expected through the evening
   hours, which should support an increase in severe winds. It remains
   somewhat unclear how quickly upscale growth will occur given
   along-boundary flow through a deep layer, and this may curtail the
   supercellular tornado threat if clustering occurs too quickly.
   However, based on latest forecast soundings and CAM guidance, the
   tornado potential will likely be greatest along the warm front
   across central IL between 21-02 UTC where low-level SRH and surface
   pressure falls/ascent will be maximized.

   ...Southern Plains...
   12 UTC soundings across the southern Plains sampled steep mid-level
   lapse rates already in place across the region. The onset of deep
   moisture return is noted along the TX Coastal Plain, which should
   spread north across central TX into OK by Tuesday morning.
   Isentropic ascent within the warm sector may support isolated
   thunderstorm development by late morning across north TX into the
   Texarkana region where capping should be weaker. By late
   afternoon/early evening, more widespread thunderstorm development is
   expected across central TX as strong height falls associated with
   the ejecting upper wave overspread the region. Initially discrete
   supercells will be capable of all hazards, through very large (2+
   inch) hail appears to be the most probable threat. Strong forcing
   for ascent will promote upscale growth through the evening with one
   or more bowing segments possible. Enlarging low-level hodographs
   associated with an increasing nocturnal jet may support embedded
   circulations within the developing squall line. 30% hail/wind
   probabilities were introduced to highlight the corridor of higher
   hail/wind threat from the Edwards Plateau into central TX.

   ..Moore.. 03/09/2026

   WUUS02 PTSDY2 

   NOTE: THE NEXT DAY 2 OUTLOOK IS SCHEDULED BY 0600Z

        
   SPC AC 090720

   Day 3 Convective Outlook  
   NWS Storm Prediction Center Norman OK
   0220 AM CDT Mon Mar 09 2026

   Valid 111200Z - 121200Z

   ...THERE IS A SLIGHT RISK OF SEVERE THUNDERSTORMS FROM THE ARKLATEX
   AND LOWER MISSISSIPPI VALLEY NORTHEAST THROUGH THE OHIO VALLEY...

   ...SUMMARY...
   Isolated to scattered severe thunderstorms are possible on Wednesday
   from the ArkLaTex and Lower Mississippi Valley northeastward through
   the Ohio Valley vicinity.

   ...East Texas northeast to the Ohio Valley vicinity...

   A split-flow regime will continue into Wednesday, with upper
   troughing over the central U.S. remaining bifurcated through much of
   the period. In the southern branch, a closed low/upper shortwave
   trough will migrate from TX to the Lower MS Valley. Meanwhile, the
   northern stream upper trough over the northern Plains/Upper Midwest
   will develop east across the Upper Great Lakes/Midwest. Ahead of
   these features, strong southwesterly deep-layer flow will extend
   from east TX into the Mid-Atlantic/New England. At the surface, a
   cold front will extend southwest from a surface low over southern
   Lower MI into western OK. This front will advance southeast through
   the period, becoming oriented from the Mid-Atlantic coast to the
   central Gulf coast by Thursday morning.

   Strong warm advection ahead of the front will transport Gulf
   moisture as far north as the Mid-Atlantic and southern New England.
   Ongoing convection is expected ahead of the front across portions of
   the ArkLaTex into the Midwest. This, along with the warm advection
   regime resulting in widespread cloudiness, lends to uncertainty in
   how the downstream airmass will destabilize, especially with
   northeast extent into parts of the Ohio Valley vicinity. Somewhat
   stronger destabilization is likely across the Lower MS Valley where
   richer Gulf moisture will reside. Strong vertical wind profiles will
   support damaging wind potential with even modest instability. Linear
   convection is the most likely storm mode given deep-layer flow
   parallel to the surface boundary and strong large-scale ascent
   overspreading the boundary. If discrete cells can form, some tornado
   potential will exist closer to a deepening surface cyclone in the
   vicinity of the upper Ohio Valley, and perhaps near a secondary
   surface low over the lower MS Valley, though this scenario remains
   highly uncertain.

   ..Leitman.. 03/09/2026

   WUUS03 PTSDY3 

   NOTE: THE NEXT DAY 3 OUTLOOK IS SCHEDULED BY 1930Z