• MESO: Mesoscale Discussion 0500

    From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sat Apr 20 18:46:11 2024
    ACUS11 KWNS 201846
    SWOMCD
    SPC MCD 201845=20
    NCZ000-SCZ000-202045-

    Mesoscale Discussion 0500
    NWS Storm Prediction Center Norman OK
    0145 PM CDT Sat Apr 20 2024

    Areas affected...Northern South Carolina into southern North
    Carolina

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

    Valid 201845Z - 202045Z

    Probability of Watch Issuance...20 percent

    SUMMARY...Thunderstorm development is anticipated within the next
    hour. A few strong/severe cells, including the potential for a
    supercell or two, will pose a severe hail/wind threat to parts of
    the Carolinas this afternoon and evening. This threat should remain
    fairly localized; watch issuance is not anticipated.

    DISCUSSION...Steady growth of multiple cumulus congestus has been
    noted in GOES imagery over the past 30-60 minutes along a cold front
    and in the vicinity of a weak surface low across parts of the
    Carolinas. Glaciation is noted in a few of the deeper towers,
    suggesting that thunderstorm initiation is probable within the next
    hour or so. Discrete to semi-discrete cells that emerge from within
    the growing cumulus field will likely propagate off the slow-moving
    cold front into an increasingly buoyant air mass downstream into the
    eastern Carolinas (where MLCAPE is increasing to around 1500 J/kg).
    Within the past hour regional VWPs sampled weak winds through the
    lowest few kilometers, but a nearly uni-directional wind profile
    with 40-50 knot flow between 5-6 km. This is yielding 0-6 km BWD
    values on the order of 30-40 knots with a wind profile favorable for
    splitting cells. Consequently, this environment appears supportive
    of supercells with an attendant large hail (0.75 to 1.25 inch in
    diameter) and severe wind risk. The hail risk might be regionally
    maximized across parts of NC to the north of a differential heating
    boundary where muted diurnal mixing is supporting higher buoyancy.
    Conversely, areas to the south of this boundary may see a higher
    damaging wind threat given steeper low-level lapse rates.
    Regardless, it remains unclear how many cells will emerge from the
    cumulus field and evolve into mature supercells given the weak
    forcing for ascent. Latest CAM guidance also suggests storm coverage
    may be limited, which lends credence to the idea that the overall
    severe threat should remain sufficiently localized to preclude the
    need for a watch.

    ..Moore/Goss.. 04/20/2024

    ...Please see https://urldefense.com/v3/__http://www.spc.noaa.gov__;!!DZ3fj= g!9Gm4DCci2Mh5D3JkaOlAKkNhfbh4W7UbcXrcuP7gWZgp8AZaD3cc3a-Qpe_Jv7Cw37r59eQu_= yMSVzGJgg8CGMZigRw$ for graphic product...

    ATTN...WFO...MHX...RAH...ILM...CAE...GSP...

    LAT...LON 33607884 33637921 34248114 34508152 34848145 35258111
    35438081 35598018 35497859 35367780 35217705 34747706
    34457730 34257759 33957784 33837798 33797836 33677863
    33607884=20


    =3D =3D =3D
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