• MESO: Mesoscale Discussion 1522

    From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Mon Jun 30 16:10:19 2025
    ACUS11 KWNS 301608
    SWOMCD
    SPC MCD 301607=20
    PAZ000-DEZ000-MDZ000-DCZ000-VAZ000-WVZ000-301800-

    Mesoscale Discussion 1522
    NWS Storm Prediction Center Norman OK
    1107 AM CDT Mon Jun 30 2025

    Areas affected...parts of the Mid-Atlantic States

    Concerning...Severe potential...Watch unlikely=20

    Valid 301607Z - 301800Z

    Probability of Watch Issuance...20 percent

    SUMMARY...Isolated damaging winds from sporadic strong gusts along
    with small hail will be possible with slow-moving, scattered
    thunderstorms through late afternoon.

    DISCUSSION...Convective development is increasing across western PA,
    downstream of an eastward-moving MCV over central OH, and along the
    lee of the central Appalachians across eastern WV. Overall
    thermodynamic environment appears fairly ubiquitous, outside of the
    higher terrain, with surface temperatures in the 80s and dew points
    in the upper 60s to mid 70s. 12Z soundings sampled poor mid to upper
    lapse rates and nearly saturated profiles east of the Appalachians,
    with somewhat drier and not quite as poor lapse rates across the
    Upper OH Valley. This combined with modest deep-layer shear will
    probably modulate a potentially greater downburst threat. It may be
    that some degree of loose clustering will be necessary for strong
    gust production capable of more than localized tree damage.

    ..Grams/Hart.. 06/30/2025

    ...Please see https://urldefense.com/v3/__http://www.spc.noaa.gov__;!!DZ3fj= g!_IVY1yPNW5wXnG4jt695nzSI34zRnx8WCCc0YMsR8oFWUnPSjZ3BykCO_NylTfQJpE70QfuLl= 5zpCzNBBpidmP5OU1s$ for graphic product...

    ATTN...WFO...PHI...BGM...CTP...LWX...PBZ...RLX...

    LAT...LON 40547955 41557969 41817851 41707687 41427589 40507540
    39887554 39047642 38477775 38437845 38517898 38907937
    39827936 40547955=20

    MOST PROBABLE PEAK WIND GUST...UP TO 60 MPH


    =3D =3D =3D
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