• DAY2 3/5 RISK AREAS POSTE

    From Dumas Walker@21:1/175 to All on Thu May 15 09:21:00 2025
    ACUS02 KWNS 150530
    SWODY2
    SPC AC 150529

    Day 2 Convective Outlook
    NWS Storm Prediction Center Norman OK
    1229 AM CDT Thu May 15 2025

    Valid 161200Z - 171200Z

    ...THERE IS AN ENHANCED RISK OF SEVERE THUNDERSTORMS FRIDAY
    AFTERNOON INTO FRIDAY NIGHT ACROSS PARTS OF NORTHEASTERN
    ARKANSAS...EAST CENTRAL AND SOUTHEASTERN MISSOURI...SOUTHERN ILLINOIS...SOUTHERN INDIANA...SOUTHWESTERN OHIO...MUCH OF WESTERN
    AND CENTRAL KY...WESTERN AND MIDDLE TENNESSEE...

    ...SUMMARY...
    Severe thunderstorms appear likely to develop across parts of the
    middle Mississippi through lower and middle Ohio Valleys Friday
    afternoon into Friday night. During the late afternoon into
    evening, this may include a few intense supercells posing a risk for
    large hail and tornadoes. During the evening into the overnight
    hours, this probably will include an upscale growing and organizing
    cluster posing a risk for strong, damaging winds and perhaps a
    continuing risk for tornadoes.

    ...Discussion...
    Downstream of a prominent mid-level high over the southern mid- to
    subtropical latitudes of the eastern Pacific, split flow will
    persist across much of North America through this period. Within
    this regime an initially deep and occluded surface cyclone, centered
    over northern Minnesota at the outset of the period, is forecast to
    weaken Friday through Friday night, as it migrates into the Upper
    Great Lakes region in response to a short wave perturbation pivoting
    around the southern periphery of the mid-level circulation center.
    It appears that this perturbation will come in phase with another
    short wave perturbation forecast to accelerate east-northeast of the
    central Great Plains through much of the Ohio Valley by early
    Saturday. Another vigorous short wave trough digging around the
    northeastern periphery of the Pacific ridge may reach the northern
    California coast by the end of the period, preceded by at least one
    more modest perturbation migrating northeastward across the northern
    Baja vicinity.

    In lower levels, associated with the occluding cyclone, a
    weak/weakening Pacific cold front/dry line appears likely to stall
    across the lower Great Lakes through Ohio River vicinity, and across
    the Ark-La-Tex into Rio Grande River by 12Z Friday. This may be
    trailed by another weak front across the Upper Midwest through the
    central Great Plains and Texas South Plains, which is forecast to be
    overtaken by the primary cold front surging southeastward from the
    upper Mississippi Valley/northern Great Plains. By late Friday
    night, this cold front may reach the lower Ohio Valley and central
    Great Plains.

    Preceding the consolidating fronts, low-level moisture return and
    moderate to strong destabilization is forecast across the middle
    Mississippi and lower Ohio Valleys on strengthening south to
    southwesterly flow. The potential northern extent of the moisture
    return remains unclear, based on model output, and this could be
    impacted by outflow associated with possible early period convective development across the lower Ohio Valley into portions of the
    Allegheny and Cumberland Plateaus. Depending on how these
    uncertainties play out, it might not be out of the question that a
    more substantive outbreak of severe thunderstorms could evolve than
    currently depicted. It is possible areal coverage and probabilities
    could be increased further in later outlooks for this period.

    ...Lower Great Lakes into northern Mid Atlantic...
    Uncertainty lingers concerning the potential for severe weather.
    However, the intersection of the initial weak surface cold
    front/dryline and warm front could still be providing a focus for
    strong to severe thunderstorm development at the outset of the
    period across the lower Great Lakes/upper Ohio Valley vicinity.
    Aided by continuing inflow from better potential instability across
    the Ohio Valley, in the presence of moderate to strong vertical
    shear, it is possible that this could continue into the day Friday,
    perhaps evolving into an organizing cluster which should tend to
    propagate southeastward and perhaps pose potential for strong to
    severe surface gusts.

    ...Middle Mississippi into Ohio Valley...
    There remains at least some signal that a modest short wave
    perturbation, within the belt of westerlies emanating from the
    subtropical eastern Pacific, may be contributing to vigorous
    convective development at the outset of the period, or shortly
    thereafter, across parts of the lower Ohio Valley. If this occurs,
    it might not be out of the question that the boundary-layer
    downstream, into the western slopes of the Appalachians, might
    destabilize in time to support an upscale growing cluster with
    potential to produce to produce severe wind and hail.

    The impact of this possible early period convection might be the
    primary contributor to at least some continuing model disparity
    concerning upstream boundary-layer moistening and destabilization
    (particularly the northern extent) across the middle Mississippi
    into lower Ohio Valleys. However, it still appears most probable
    that destabilization, as far north as the I-44 corridor of
    central/eastern Missouri, will support the initiation of storms by
    early afternoon, in response to forcing for ascent associated with
    the mid-level perturbation emerging from the central Great Plains.

    This is generally forecast to shift east-northeastward into the
    lower Ohio Valley through late Friday afternoon, in an environment
    that may support at least a window of opportunity for
    sustained/long-lived supercells with potential to produce large to
    giant hail and a couple of strong tornadoes. Into Friday evening
    and overnight, there remains a considerable signal in model output
    that large-scale forcing for ascent will support a notable upscale
    growing and organizing cluster, in the presence of seasonably strong
    (and increasingly convectively augmented) westerly deep-layer mean
    flow. This may support widespread severe surface gusts,
    occasionally in excess of 65 kt, across a swath from southern
    Indiana/western Kentucky and northern Tennessee toward the Allegheny
    and Cumberland Plateaus.

    ..Kerr.. 05/15/2025

    $$
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