• MESO: Mesoscale Discussion 0646

    From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Tuesday, May 05, 2026 19:37:57
    ACUS11 KWNS 051937
    SWOMCD
    SPC MCD 051937=20
    TXZ000-052230-

    Mesoscale Discussion 0646
    NWS Storm Prediction Center Norman OK
    0237 PM CDT Tue May 05 2026

    Areas affected...parts of northwestern into north central Texas

    Concerning...Severe potential...Watch possible=20

    Valid 051937Z - 052230Z

    Probability of Watch Issuance...40 percent

    SUMMARY...The initiation of strong thunderstorms appears possible to
    the west of Dallas/Forth Worth within the next couple of hours.=20
    This may include the evolution of an intensifying supercell or two,
    which could pose potential for producing large, damaging hail
    impacting at least parts of the Metroplex by 5-7 PM. If/when this
    becomes more certain, a severe weather watch probably will be
    needed.

    DISCUSSION...Just ahead of a southward advancing cold front, now
    southeast of the Wichita Falls TX vicinity, stronger surface heating
    and deeper boundary-layer mixing are ongoing in a narrow corridor
    roughly focused along I-20 across the Abilene into Fort Worth
    vicinity. At least attempts at deepening convective development are
    underway within this regime to the west-north of Mineral Wells,
    where low-level forcing for ascent may be aided by weak low-level
    warm advection and locally enhanced convergence, near the general
    intersection of the cold front and dryline.

    This is occurring beneath larger-scale mid/upper ridging
    overspreading much of the southern Great Plains. However, based on
    various model output, including convection allowing guidance,=20
    further insolation, coupled with subtle mid-level height falls and
    cooling, might become supportive of thunderstorm initiation within
    the next few hours. How long this activity is sustained before
    tending to be undercut by the southward advancing cold front, and
    whether this occurs prior to acquiring inflow of higher
    boundary-layer moisture content along and to the east of the
    dryline, remain unclear.

    Even in the drier more strongly heated boundary-layer just to the west/southwest of the cold front/dryline intersection, initial
    thunderstorm development may become capable of producing large hail
    and a locally strong downburst, in the presence of steep-lapse rates
    and strong deep-layer shear. If convection is able to acquire
    inflow of boundary-layer air with dew points near 70F, which may be
    maintained across eastern portions of the Metroplex, the potential
    for much larger and damaging hail will become considerably greater.

    ..Kerr/Smith.. 05/05/2026

    ...Please see https://urldefense.com/v3/__http://www.spc.noaa.gov__;!!DZ3fj= g!63B3IiQJgVOwiKyCPoOPaNRgrx7jn55ee_nvfhTlt_sgk6STh2ySUQOnpUNI93yb8svCeklCm= GF3aQ2B4dSvypGBAVw$ for graphic product...

    ATTN...WFO...FWD...SJT...

    LAT...LON 33289903 33379822 33019639 32189747 32399914 32829950
    33289903=20

    MOST PROBABLE PEAK TORNADO INTENSITY...UP TO 90 MPH
    MOST PROBABLE PEAK WIND GUST...55-70 MPH
    MOST PROBABLE PEAK HAIL SIZE...2.00-3.50 IN


    =3D =3D =3D
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