• MESO: Mesoscale Discussion 0574

    From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sun Apr 27 19:56:00 2025
    ACUS11 KWNS 271955
    SWOMCD
    SPC MCD 271955=20
    TXZ000-NMZ000-272100-

    Mesoscale Discussion 0574
    NWS Storm Prediction Center Norman OK
    0255 PM CDT Sun Apr 27 2025

    Areas affected...,parts of swrn TX

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

    Valid 271955Z - 272100Z

    Probability of Watch Issuance...40 percent

    SUMMARY...The initiation of a couple of storms appears increasingly
    likely near and northwest through north of Fort Stockton through 4-5
    PM CDT. More rapid thunderstorm intensification accompanied by
    increasing potential for large hail and locally damaging wind gusts
    may be initially slow, before probably increasing toward early
    evening around the Midland through Big Spring vicinities.

    DISCUSSION...The boundary-layer is becoming strongly heated and
    deeply mixed across the Davis Mountains vicinity of southwest Texas
    into the Texas South Plains. The dryline is sharpening east through
    north of Fort Stockton, where 2-hourly surface pressure falls around
    2.0+ mb have been observed the past couple of hours, and low-level
    convergence appears strongest.

    Deepening convective development is ongoing within the deeper
    mixed-boundary layer around Fort Stockton, where surface
    temperature/dew point spreads are around 50 F (95/44), but forecast
    soundings and HREF guidance suggests that the initiation of at least
    isolated thunderstorm development is increasingly probable through
    21-22Z. It appears that this may be aided by forcing associated
    with a mid-level speed maximum within southwesterly flow emanating
    from the northern Mexican Plateau.

    Downstream of slow moving large-scale mid-level troughing over the
    southern Great Basin and Southwest, after at least some further
    eastward mixing of the dryline late this afternoon, it probably will
    begin to retreat northwest across the Pecos Valley vicinity toward
    23-00Z. As this occurs, convection may acquire more substantively
    unstable updraft inflow (including most unstable CAPE up to
    2000-3000+ J/kg), supporting increasing potential for rapid
    thunderstorm intensification, in the presence of strong deep-layer
    shear. This may including a splitting supercell or two, posing a
    risk for large hail and a few strong surface gusts.

    Until then, though, initial thunderstorm development will probably
    be more modest in strength, but could still pose some risk for
    producing severe hail and wind.

    ..Kerr/Smith.. 04/27/2025

    ...Please see https://urldefense.com/v3/__http://www.spc.noaa.gov__;!!DZ3fj= g!96XqjpPJSg65CTMa-piU80s_yvm6qB9w46C4zs8hte3TjfSjSP_HaBf7Q8VYBIOpDOFdU1oG2= UKUjDoHj_es3a5GhcQ$ for graphic product...

    ATTN...WFO...SJT...LUB...MAF...

    LAT...LON 30410326 30870341 31970321 32930244 33180156 32510109
    32000117 31040164 30280230 30410326=20

    MOST PROBABLE PEAK TORNADO INTENSITY...UP TO 95 MPH
    MOST PROBABLE PEAK WIND GUST...55-70 MPH
    MOST PROBABLE PEAK HAIL SIZE...1.50-2.50 IN


    =3D =3D =3D
    To unsubscribe from WX-STORM and you already have a login, go to https://lists.illinois.edu and use the "Unsubscribe" link. Otherwise email Chris Novy at cnovy@cox.net and ask to be removed from WX-STORM.

    --- SBBSecho 3.20-Linux
    * Origin: capitolcityonline.net * Telnet/SSH:2022/HTTP (1:2320/105)