• DAY2 3/5 RISK AREA POSTED

    From Dumas Walker@21:1/175 to All on Mon Mar 9 08:34:48 2026
    ACUS02 KWNS 090601
    SWODY2
    SPC AC 090600

    Day 2 Convective Outlook
    NWS Storm Prediction Center Norman OK
    0100 AM CDT Mon Mar 09 2026

    Valid 101200Z - 111200Z

    ...THERE IS AN ENHANCED RISK OF SEVERE THUNDERSTORMS ACROSS
    NORTHEAST MISSOURI...FAR SOUTHEAST IOWA...AND PARTS OF
    NORTHERN/CENTRAL ILLINOIS INTO NORTHWEST INDIANA...

    ...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 complex scenario for severe thunderstorm potential is expected on
    Tuesday and Tuesday night from the Southern Plains to the Mid-MS Valley/southern Great Lakes vicinity. A somewhat bi-modal severe
    risk appears possible within a split-flow upper level pattern. All
    severe hazards appear possible, especially within a corridor across
    portions of TX, and a second corridor from northern MO into
    northern/central IL and northwest IN.

    Expansive area of enhanced southwesterly flow will overspread the
    southern Plains into the Upper Great Lakes, aided by two separate
    upper troughs. The first is associated with an upper low/trough
    across northwest Mexico and the Southwest, which will shift east
    into the southern High Plains by Wednesday. The second is a broad
    but deepening upper trough moving across the northern/central Plains
    toward the Upper Midwest. Two areas of low pressure are expected to
    develop with the approaching of these upper systems, one over the central/southern High Plains and the other across the Lower
    MO/Mid-MS valley. A dryline/Pacific front will be oriented across
    western TX, while a warm front extends west to east from near
    northern MO/southeast IA into northern IL/IN. By evening, a cold
    front will begin to develop southeast across KS/MO/IA/IL/IN, and the
    Pacific front will shift east across central TX. These boundaries
    will be the focus for scattered to widespread thunderstorm
    development from late afternoon into the overnight hours.

    ...Mid-MO Valley to southern Great Lakes vicinity...

    Capping will likely suppress convection for much of the day within a
    strong warm advection regime. Surface dewpoints are expected to
    climb into the low/mid-60s south of the warm front beneath steep
    midlevel lapse rates. This will foster 1000-2000 J/kg MLCAPE by peak
    heating. Convection is expected to develop within the 21-00z time
    frame when a 40 kt low-level jet is expected to overspread the
    region. Supercell wind profiles are noted in forecast soundings,
    with hodographs exhibiting enhanced low-level curvature, with lengthened/straight hodographs above 2-3 km. Given a favorable
    thermodynamic environment, large hail to 2.5 inches appears possible
    with storms both within the warm sector and initial activity that
    may develop within the cooler air north of the front. Furthermore,
    any cells that develop within the warm sector and interact with the
    front will encounter enhanced low-level shear/SRH and tornadoes
    (some EF-2+) will be possible. With time during the evening,
    convection will likely grow upscale into one or more
    southeast-advancing linear segments near the advancing cold front.
    Damaging winds will be possible with this activity overnight.

    ...Southern Plains vicinity...

    Convection is expected to develop along the surface dryline across
    western TX by mid to late afternoon. Initial supercells are possible
    and could produce large hail (to around 2 inch diameter) and a
    couple of tornadoes. Convection may quickly grow upscale as the
    Pacific front overtakes the dryline and large-scale ascent increases
    rapidly by 00z.

    Uncertainty increases with northward extent across OK/KS into
    southern MO/AR. These areas will be within the broad warm sector and
    moderate to strongly sheared environment. However, this area will
    also be between the two areas of stronger ascent. Some capping may
    persist and it is unclear how convection may evolve across these areas.

    ..Leitman.. 03/09/2026

    $$
    --- SBBSecho 3.28-Linux
    * Origin: Capitol City Online (21:1/175)