• DAY3 2/5 Risk Area Posted

    From Mike Powell@618:250/1 to All on Sun May 4 08:33:00 2025
    ACUS03 KWNS 040733
    SWODY3
    SPC AC 040733

    Day 3 Convective Outlook
    NWS Storm Prediction Center Norman OK
    0233 AM CDT Sun May 04 2025

    Valid 061200Z - 071200Z

    ...THERE IS A SLIGHT RISK OF SEVERE THUNDERSTORMS FOR PARTS OF
    CENTRAL INTO EAST TEXAS...

    ...SUMMARY...
    Severe thunderstorms are possible across much of Central into East
    Texas and western/central Louisiana. All severe hazards would be possible.

    ...Synopsis...
    An ejecting shortwave trough will lift northeastward through Central
    into Northeast Texas on Tuesday. Continued moisture advection
    northward will bring upper 60s to low 70s dewpoints in
    South/Central/Southeast Texas and parts of the lower Mississippi
    Valley. Early period precipitation appears likely along a warm front
    within the Red River region southeastward into Louisiana. Additional
    early precipitation is possible within the Edwards Plateau into
    Central Texas, but uncertainty is greater in this scenario. A
    dryline is expected in central Texas during the afternoon.

    ...Central Texas into Sabine Valley...
    The expectation of early day precipitation complicates the overall
    forecast for the afternoon. Even so, a very moist and weakly capped
    airmass is forecast to be in place south of the warm front and east
    of the developing dryline. The ECMWF is more aggressive with the
    early development of a cluster of storms/MCS. In this scenario,
    convection would likely strengthen as surface heating occurs ahead
    of it. The GFS/NAM show greater potential for the dryline to be a
    focus for convection during the afternoon. Here, supercells capable
    of all hazards would be possible. There is potential for significant
    severe, with very large hail being the primary concern, but
    uncertainty in the convective evolution keeps confidence too low to
    highlight any particularly area.

    ...Red River into ArkLaTex...
    Storms along the warm front will likely be ongoing early in the day
    and continue to develop within the warm advection regime into the
    afternoon. Strong shear and moderate buoyancy would promote a risk
    for large hail and damaging winds. Numerous storms and their
    interactions will tend to temper the overall severe threat. Many of
    these storms will be at least slightly elevated north of the
    boundary. Tornadoes could also occur with surface-based storms
    within the warm front zone.

    ..Wendt.. 05/04/2025

    $$
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  • From Mike Powell@618:250/1 to All on Fri Jun 13 07:52:00 2025
    ACUS03 KWNS 130729
    SWODY3
    SPC AC 130728

    Day 3 Convective Outlook
    NWS Storm Prediction Center Norman OK
    0228 AM CDT Fri Jun 13 2025

    Valid 151200Z - 161200Z

    ...THERE IS A SLIGHT RISK OF SEVERE THUNDERSTORMS ACROSS PARTS OF
    SOUTHEAST MONTANA...THE DAKOTAS AND NORTHERN NEBRASKA...

    ...SUMMARY...
    Scattered severe storms, capable of isolated large hail and severe
    wind gusts, are expected on Sunday from parts of southeast Montana southeastward into northern Nebraska. Elsewhere in the Great Plains,
    marginally severe storms will be possible. A few severe wind gusts
    may also occur from parts of North Carolina into southern Virginia.

    ...Northern Plains/Northern Nebraska...
    A mid-level ridge is forecast to remain over the central and
    northern High Plains on Sunday, as a subtle shortwave trough rides
    up and over the ridge. At the surface, a low is forecast to develop
    over Wyoming, with upslope flow remaining over much of the northern
    Plains. A moist airmass will be located from eastern Montana into
    the Dakotas and Nebraska, where moderate to strong instability is
    forecast to develop by afternoon. As surface temperatures warm
    during the day, convective initiation is expected in the higher
    terrain of the northern High Plains, with additional storms possible
    further east into parts of the Dakotas. NAM forecast soundings late
    Sunday afternoon near the instability axis have MLCAPE peaking near
    4000 J/kg with 700-500 mb lapse rates near 8 C/km. 0-6 km shear is
    forecast to be in the 30 to 40 knot range. This environment should
    support supercell development, with large hail and wind damage being
    possible. A tornado could also occur. The severe threat will likely
    persist into the evening, as low-level flow gradually increases
    across the region.

    ...Southern Nebraska/Kansas/Oklahoma/North Texas...
    A moist airmass will remain in place across much of the southern and
    central Plains on Sunday. Surface dewpoints from the upper 60s to
    the mid 70s F will contribute to the development of strong
    instability across parts of this airmass by afternoon. In spite of a
    lack of large-scale ascent, isolated convective initiation will be
    possible as surface temperatures peak in the afternoon. The most
    likely location for storm development would be along or near any
    residual outflow boundary. Forecast MLCAPE in the 2500 to 3500 J/kg
    range, along with steep low to mid-level lapse rates, and moderate
    deep-layer shear would support an isolated severe threat. Hail and
    marginally severe wind gusts would be the primary threats.

    ...North Carolina/Southern Virginia...
    A mid-level shortwave trough is forecast to move eastward across the
    southern and central Appalachians on Sunday. Ahead of the trough, a
    moist airmass is forecast over parts of the Carolinas and Virginia.
    As surface temperatures warm in the late morning and early
    afternoon, convective initiation is expected in the higher terrain
    of the southern and central Appalachians. As this convection moves
    eastward into the lower elevations, thunderstorms are expected to
    form. Although deep-layer shear is forecast to remain relatively
    weak, moderate instability and steep low-level lapse rates could be
    sufficient for isolated severe wind gusts.

    ..Broyles.. 06/13/2025

    $$
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