• MESO: Mesoscale Discussion 1733

    From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Thursday, December 27, 2018 09:17:39
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    ACUS11 KWNS 270817
    SWOMCD
    SPC MCD 270816
    NEZ000-KSZ000-OKZ000-271415-

    Mesoscale Discussion 1733
    NWS Storm Prediction Center Norman OK
    0216 AM CST Thu Dec 27 2018

    Areas affected...portions of western Kansas and south-central
    Nebraska.

    Concerning...Heavy snow

    Valid 270816Z - 271415Z

    SUMMARY...Coverage and intensity of snow is expected to increase
    over the discussion area through sunrise, with rates commonly 1-2
    inches per hour and locally higher. Sporadic blizzard conditions
    also are possible.

    DISCUSSION...Surface mesoanalysis shows a well-defined frontal-wave
    cyclone with a low near the OK/KS border, south of DDC. This low is
    forecast to migrate/re-develop northeastward along a cold front and
    across central/northern Kansas, reaching southeastern NE by 14Z.
    That will occur in response to the northeastward ejection of a
    strong mid/upper-level shortwave trough and embedded vorticity
    max/cyclone now evident in moisture-channel imagery over the
    northwestern TX Panhandle. The associated deep-layer forcings --
    both in terms of elevated frontogenetic ascent and DCVA/cooling
    aloft -- will shift northeastward over the cold sector in step with
    the motion of the deep-layer cyclone. This will help to maintain or
    increase precip over the next few hours across the OK Panhandle and
    through at least dawn over western KS, and intensify existing precip
    areas after about 09Z in southern NE.

    Favorably strong UVV is evident in planar progs throughout the
    dendritic-growth zones, likewise shifting northeastward across the
    discussion area. Time series of forecast soundings accordingly show deep-columnar cooling of any remaining superfreezing layers to below
    freezing, with dynamically driven/large-scale cooling throughout the lower/middle troposphere and post-frontal cold advection in the
    boundary layer. In addition, tight pressure/height gradients and
    vertical turbulent mixing will boost already near-blizzard
    gradient-wind conditions locally.

    ..Edwards.. 12/27/2018

    ...Please see www.spc.noaa.gov for graphic product...

    ATTN...WFO...GID...LBF...DDC...GLD...AMA...

    LAT...LON 40569791 39829849 38909927 38139974 37430033 36660063
    36540128 36870188 38070191 38990144 40200047 40919970
    41109927 41409836 40569791



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