• MESO: Mesoscale Discussion 0421

    From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Tuesday, May 15, 2018 01:33:26
    This is a multi-part message in MIME format...

    ------------=_1526348010-23415-8685
    Content-Type: text/plain

    ACUS11 KWNS 150133
    SWOMCD
    SPC MCD 150132
    KSZ000-150300-

    Mesoscale Discussion 0421
    NWS Storm Prediction Center Norman OK
    0832 PM CDT Mon May 14 2018

    Areas affected...Western KS

    Concerning...Severe potential...Watch unlikely

    Valid 150132Z - 150300Z

    Probability of Watch Issuance...20 percent

    SUMMARY...The long-lived intense thunderstorm cluster across western
    KS will continue to pose a localized significant severe risk in the
    short term, though the duration of the threat is uncertain.

    DISCUSSION...At 0130Z, an intense supercell cluster was moving
    southeast across west-central KS. The cluster is likely slightly
    elevated, given its presentation on visible satellite imagery and
    location north of a surface boundary, but moderate instability and
    effective shear of 40-50 kt has allowed the cluster to become well
    organized. While effective shear will remain favorable downstream,
    the thermodynamic environment is expected to become increasingly
    hostile, as SB CINH increases. This cluster will likely become
    increasingly elevated with time, and with the low-level jet expected
    to be focused east of this area, a gradual decreasing trend is
    expected later this evening.

    Given the very localized nature and expected limited duration of the
    threat, no watch issuance is currently anticipated unless additional
    upscale growth occurs. However, until a definitive weakening trend
    commences, wind-driven large hail capable of significant damage will
    continue to be a threat with this system.

    ..Dean/Hart.. 05/15/2018

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

    ATTN...WFO...DDC...GLD...

    LAT...LON 38680109 38680053 38389944 37999942 37759966 37830015
    37980072 38130114 38290143 38410159 38680109



    ------------=_1526348010-23415-8685
    Content-Type: text/plain; charset="US-ASCII"
    Content-Disposition: inline
    Content-Transfer-Encoding: 7BIT

    = = =
    To unsubscribe from WX-STORM and you already have a login, go to https://lists.illinois.edu and use the "Unsubscribe" link. Otherwise email Chris Novy at cnovy@cox.net and ask to be removed from WX-STORM. ------------=_1526348010-23415-8685--

    --- SBBSecho 3.03-Linux
    * Origin: CCO BBS - capitolcityonline.net:26 (1:2320/105)
  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Tuesday, April 23, 2019 00:41:51
    This is a multi-part message in MIME format...

    ------------=_1555980113-1967-2804
    Content-Type: text/plain

    ACUS11 KWNS 230041
    SWOMCD
    SPC MCD 230041
    TXZ000-NMZ000-230245-

    Mesoscale Discussion 0421
    NWS Storm Prediction Center Norman OK
    0741 PM CDT Mon Apr 22 2019

    Areas affected...Southeast New Mexico and adjacent portions of
    western Texas

    Concerning...Severe potential...Watch possible

    Valid 230041Z - 230245Z

    Probability of Watch Issuance...60 percent

    SUMMARY...Increasing strong to severe thunderstorm development,
    including a couple of supercells, is expected to spread east of the
    Sacramento and Guadalupe Mountains through 8-10 PM MDT.

    DISCUSSION...Thunderstorms have recently increased within a broken
    band across the higher terrain surrounding the Rio Grande Valley of
    New Mexico, into the western slopes of the Sacramento Mountains.
    This may be supported by another in a series of perturbations
    emanating from large-scale Southwestern mid/upper troughing, which
    will continue northeastward into the southern High Plains this
    evening.

    To the lee of the Sacramento Mountains, lower/mid tropospheric lapse
    rates have become rather steep, and the boundary layer is now in the
    process of moistening on northeasterly post-cold frontal upslope
    flow. It appears this destabilization will lead to new thunderstorm development which will gradually spread off the higher terrain into
    the plains through 02-04Z, in the presence of 20-30 kt southwesterly
    deep layer mean flow.

    Despite the somewhat modest strength of the low/mid-level wind
    fields, pronounced turning of winds with height is contributing to
    strong deep layer shear supportive of supercells capable of
    producing severe hail and locally strong surface gusts.

    ..Kerr/Edwards.. 04/23/2019

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

    ATTN...WFO...MAF...ABQ...

    LAT...LON 34100496 34070436 33530395 33130338 32850309 31860325
    31650410 32120458 33640534 34100496



    ------------=_1555980113-1967-2804
    Content-Type: text/plain; charset="US-ASCII"
    Content-Disposition: inline
    Content-Transfer-Encoding: 7BIT

    = = =
    To unsubscribe from WX-STORM and you already have a login, go to https://lists.illinois.edu and use the "Unsubscribe" link. Otherwise email Chris Novy at cnovy@cox.net and ask to be removed from WX-STORM. ------------=_1555980113-1967-2804--

    --- SBBSecho 3.06-Linux
    * Origin: capitolcityonline.net * Telnet/SSH:2022/HTTP (1:2320/105)