• MESO: Mesoscale Discussion 2178

    From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sat Sep 23 07:27:37 2023
    ACUS11 KWNS 230727
    SWOMCD
    SPC MCD 230727=20
    NEZ000-SDZ000-231000-

    Mesoscale Discussion 2178
    NWS Storm Prediction Center Norman OK
    0227 AM CDT Sat Sep 23 2023

    Areas affected...parts of western through central Nebraska

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

    Valid 230727Z - 231000Z

    Probability of Watch Issuance...20 percent

    SUMMARY...Intensifying thunderstorm development appears probable
    within the next couple of hours, with the evolution of an organizing
    cluster possible through 5-7 AM CDT. Stronger storms may be
    accompanied by a risk for severe hail, at least initially. The risk
    for severe surface gusts currently appears low, but trends will be
    monitored.

    DISCUSSION...Beneath the leading (northern) edge of a plume of warm
    and capping elevated mixed-layer air advecting across the central
    Great Plains, lower level warming and moistening is contributing to
    substantive destabilization across southwestern through central
    Nebraska. CAPE for most unstable parcels, within a saturating
    environment rooted above a more stable near-surface layer, now
    appears to be increasing in excess of 2000 J/kg, as an upstream
    mid-level low gradually shifts across and east of the northern
    Rockies.

    Mid-level forcing for ascent and cooling, within the exit region of
    a mid-level jet streak (50-60 kt around 500 mb) propagating
    east-northeast of the Colorado Rockies, is forecast to overspread
    much of western through central Nebraska and adjacent portions of
    South Dakota by 09-12Z. As it does, it will likely overcome the
    inhibition and support increasing convective development. Given the
    potential instability, and strong shear within the cloud-bearing
    layer, this probably will include convection capable of producing
    severe hail, at least initially. Aided by lift associated with the lower/mid-tropospheric warm advection, an organizing cluster may
    gradually develop through daybreak. This could eventually be
    accompanied by a developing MCV and strengthening rear inflow toward
    daybreak. However, even if this occurs, the potential for damaging
    gusts to reach the surface current appears low, due to the stable
    near-surface layer.

    ..Kerr/Edwards.. 09/23/2023

    ...Please see https://urldefense.com/v3/__http://www.spc.noaa.gov__;!!DZ3fj= g!8ZPA5g7pONwIv4JNZkIwvvslPUfKUQJlOcJnLxCj5zxS-MYGcMwewu-sHYbNPlQpEIrveKYXo= JvGeZybjkjicCxiuGQ$ for graphic product...

    ATTN...WFO...FSD...GID...LBF...UNR...

    LAT...LON 42680158 43580048 42729849 40549931 40700131 42050164
    42680158=20


    =3D =3D =3D
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