• MESO: Mesoscale Discussion 0304

    From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Tuesday, May 01, 2018 18:11:02
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    ACUS11 KWNS 011810
    SWOMCD
    SPC MCD 011810
    NEZ000-KSZ000-012045-

    Mesoscale Discussion 0304
    NWS Storm Prediction Center Norman OK
    0110 PM CDT Tue May 01 2018

    Areas affected...Central KS into southeast NE

    Concerning...Severe potential...Tornado Watch likely

    Valid 011810Z - 012045Z

    Probability of Watch Issuance...95 percent

    SUMMARY...One or two tornado watches will be needed by mid-afternoon
    (20-21Z) across central Kansas into southeast Nebraska.

    DISCUSSION...Surface mesoanalyses this afternoon showed an area of
    low pressure located in northwest KS, while the equatorward-trailing
    dryline was continuing to shift east through southwest KS. DDC
    radar imagery showed this boundary located between KGCK and KDDC at
    1740Z and into central portions of the OK and TX Panhandles.
    Clearing skies per visible satellite imagery have allowed for
    stronger surface heating across the warm sector where the
    environment continues to moisten per southerly low-level winds.
    These changes in boundary-layer thermodynamics (reduction in
    inhibition) have allowed cumulus clouds to develop along the KS
    portion of the dryline into adjacent part of the OK Panhandle, as
    the environment further destabilizes (mixed-layer CAPE is already up
    to 2500 J/kg).

    Deeper moist convection is expected by 20-21Z along the KS dryline
    as stronger ascent within the exit region of southwesterly mid- and
    upper-level jets shift into the central Plains this afternoon and
    evening. Trends in the operational HRRR continue to suggest storm
    development along the KS portion of the dryline by 21Z, with some
    potential for initiation by around 20Z. Further low-level moistening
    and increasing vertically veering winds will support supercell
    development with an attendant threat for all severe hazards.
    Initial storms will be capable of producing very large hail, while a
    tornado threat (some strong) will increase, given a strengthening
    southerly low-level jet resulting in increased hodograph curvature
    this evening.

    ..Peters/Grams.. 05/01/2018

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

    ATTN...WFO...OAX...TOP...ICT...GID...DDC...GLD...

    LAT...LON 37349992 38149990 39429952 40089898 41169757 41449659
    41379612 40879586 40329599 39289672 38319768 37539859
    37229942 37179971 37349992



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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Thursday, April 11, 2019 20:14:05
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    ACUS11 KWNS 112014
    SWOMCD
    SPC MCD 112013
    ILZ000-IAZ000-112115-

    Mesoscale Discussion 0304
    NWS Storm Prediction Center Norman OK
    0313 PM CDT Thu Apr 11 2019

    Areas affected...Parts of northern and central Illinois

    Concerning...Severe potential...Watch unlikely

    Valid 112013Z - 112115Z

    Probability of Watch Issuance...20 percent

    SUMMARY...At least some increase in severe weather potential is
    expected with developing thunderstorm activity across parts of
    northern Illinois by the 4-6 PM CDT time frame. It is possible that
    this threat may remain low enough that a watch is not needed, but
    trends will be monitored.

    DISCUSSION...Near/just ahead of the lower/mid tropospheric cold
    front, forcing for ascent appears to be contributing to the ongoing
    increase in thunderstorm activity across northwestern Illinois into southwestern Wisconsin. This activity is largely rooted above a
    near-surface stable layer to the north of the surface warm front,
    with relatively warm mid-levels and weak mid/high level lapse rates
    allowing for only weak CAPE.

    The band of convection is expected to gradually spread eastward
    during the few hours, with southward development into the warm
    sector of the surface cyclone also possible by 21-23Z. Even within
    the warm sector, relatively low surface dew points across parts of
    eastern Missouri into west central Illinois are currently resulting
    in negligible boundary layer CAPE. However, modest low-level
    moisture (reflected by mid 50s+ surface dew points) appears to be
    returning northward/northwestward in a corridor to the
    east/northeast through north of Springfield, into the vicinity of
    the warm front.

    A combination of at least weak boundary-layer destabilization along
    the warm front, coupled with increasing lift ahead of the occluding
    surface cyclone triple point (and associated eastward advancing band
    of mid-level forcing for ascent), may allow for at least isolated boundary-layer based storm development. This seems most likely
    north/northeast of the Peoria vicinity, and may include one or two
    supercells accompanied by at least some risk for severe hail and
    localized strong surface gusts. Although low-level thermodynamic
    profiles appear rather marginal, given the synoptic environment, and
    large low-level hodographs near/beneath 50+ kt southerly 850 mb
    flow, an isolated tornado may not be out of the question.

    ..Kerr/Hart.. 04/11/2019

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

    ATTN...WFO...LOT...ILX...DVN...

    LAT...LON 41629041 42259012 42138890 40368893 39938990 40579038
    41629041



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