• MESO: Mesoscale Discussion 0384

    From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Friday, April 01, 2022 18:48:55
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    ACUS11 KWNS 011848
    SWOMCD
    SPC MCD 011848=20
    FLZ000-012115-

    Mesoscale Discussion 0384
    NWS Storm Prediction Center Norman OK
    0148 PM CDT Fri Apr 01 2022

    Areas affected...Parts of southern Florida Atlantic coastal areas

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

    Valid 011848Z - 012115Z

    Probability of Watch Issuance...5 percent

    SUMMARY...A couple of strong storms appear possible across Atlantic
    coastal hours, mostly north of Miami, near the Palm Beach area, by
    4-5 PM EDT. These may pose a risk for producing localized,
    potentially damaging, surface gusts.

    DISCUSSION...Outflow from persistent convection near a weak surface
    cold front has advanced south of the Vero Beach and Avon Park
    vicinities. To the south of this boundary, the seasonably moist
    boundary layer has become increasingly well mixed with continuing
    insolation, and temperatures warming into the upper 80s have
    contributed to moderately large CAPE.

    Near surface flow is generally light and southwesterly to westerly,
    with low-level confluence and convergence becoming focused inland of
    far southeastern coastal areas into the Palm Beach vicinity, where
    mixed-layer CAPE may be maximized around 2000 J/kg. This appears to
    be just ahead of a subtle/low amplitude perturbation (perhaps
    convectively generated), which has migrated inland to the north of
    Fort Myers and may reach Atlantic coastal areas near/north of Palm
    Beach by 20-21Z. Associated forcing for ascent may contribute to
    enhancement of scattered thunderstorm development now beginning to
    initiate in the unstable environment.

    Any substantive upscale convective growth may take place largely
    offshore. However, at least isolated to widely scattered strong
    thunderstorm development appears possible near coastal areas, in the
    presence of modest deep-layer shear. These may pose at least some
    risk for small hail. And latent cooling due to melting and
    evaporation, coupled with heavy precipitation loading, may
    contribute to a strong downburst or two with locally strong surface
    gusts, before shifting offshore.

    ..Kerr/Grams.. 04/01/2022

    ...Please see https://urldefense.com/v3/__http://www.spc.noaa.gov__;!!DZ3fj= g!oeBfXOxT2eITnefFYaHWwhoXvO6Txqx-cQvSDi9zs2eFO12oTMzwrQTWk_WLvqXm-UUQ326C$=
    for graphic product...

    ATTN...WFO...MFL...MLB...

    LAT...LON 27848043 27817943 26457992 26468044 27288067 27848043=20



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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Thursday, March 30, 2023 01:52:16
    ACUS11 KWNS 300152
    SWOMCD
    SPC MCD 300151=20
    MEZ000-NHZ000-VTZ000-MAZ000-NYZ000-PAZ000-300545-

    Mesoscale Discussion 0384
    NWS Storm Prediction Center Norman OK
    0851 PM CDT Wed Mar 29 2023

    Areas affected...Eastern NY...VT...western NH...far western MA...and
    far northeastern PA

    Concerning...Snow Squall=20

    Valid 300151Z - 300545Z

    SUMMARY...Rapid visibility reductions with bursts of heavy snow are
    possible with any snow squalls that develop into the overnight
    hours.

    DISCUSSION...Latest surface observations depict an eastward-
    advancing cold front extending south-southwestward across eastern
    NY. While surface temperatures ahead of the front remain in the
    upper 30s to middle 40s (warmer with southward extent), temperatures
    are rapidly falling along/behind the cold front into the lower 30s.
    Behind the cold front, a mix of rain and moderate to heavy snow are
    being observed across east-central NY, and this precipitation shield
    will spread eastward with the cold front into the overnight hours.
    Nocturnal cooling combined with cold-air advection behind the front
    should generally support a transition to mostly snow with eastward
    extent -- especially over higher elevations. In addition, strong
    linear forcing for ascent accompanying the frontogenetic circulation
    should intersect the dendritic growth zone -- favoring bursts of
    heavy snow and the potential for snow-squall conditions, given steep
    antecedent low-level lapse rates and 30-35-kt 0-2-km flow (per
    regional VWP data). Rapid visibility reductions and strong gusts
    could accompany the stronger/more-organized snow bands into the
    overnight hours.

    ..Weinman.. 03/30/2023

    ...Please see https://urldefense.com/v3/__http://www.spc.noaa.gov__;!!DZ3fj= g!6N2-CqAjUtnIWHO_GsahpjnxiO_KHDCJB1fB92iW1RoTrQ8u-1ekwiITn2a_f107tNEVmObeY= 1tTiJ4zvBvE5nmwi1o$ for graphic product...

    ATTN...WFO...GYX...BOX...BTV...OKX...ALY...BGM...

    LAT...LON 42967482 44337376 45017333 45087251 45117180 45427113
    45317082 44327111 43457180 41737399 41427480 41777585
    42107581 42967482=20


    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Monday, April 08, 2024 19:50:07
    ACUS11 KWNS 081950
    SWOMCD
    SPC MCD 081949=20
    LAZ000-TXZ000-082145-

    Mesoscale Discussion 0384
    NWS Storm Prediction Center Norman OK
    0249 PM CDT Mon Apr 08 2024

    Areas affected...eastern portions of central Texas into adjacent
    western Louisiana

    Concerning...Tornado Watch 90...

    Valid 081949Z - 082145Z

    The severe weather threat for Tornado Watch 90 continues.

    SUMMARY...The risk for severe hail, and perhaps a couple of
    tornadoes, may continue to increase with a couple of evolving
    supercells, before thunderstorms possibly begin consolidating into
    an organizing cluster near and north of the College Station and
    Huntsville into Lufkin vicinities toward 5-6 PM CDT.

    DISCUSSION...Thunderstorms have increased in coverage and intensity
    within a narrow corridor, which likely coincides with the
    northern/leading edge of stronger mid-level inhibition, beneath
    building ridging within the subtropical branch of westerlies.=20
    Models suggest that one on two speed maxima within this regime will
    contribute to strengthening upper divergence along this corridor
    during the next few hours, supporting potential for considerable
    further upscale convective growth.

    A couple of supercells which have recently evolved to the southeast
    of the College Station and Huntsville vicinities may continue to
    intensify in the near term, aided by increasing inflow of moist
    boundary-layer air characterized moderately large CAPE, in the
    presence of strengthening shear. Gradually, though, it appears that
    forcing associated with lower/mid-tropospheric warm advection may
    tend to become focused to the north of College Station and
    Huntsville into Lufkin vicinity, where strongest storms may evolve
    into an increasingly organized cluster by 22-23Z.

    ..Kerr.. 04/08/2024

    ...Please see https://urldefense.com/v3/__http://www.spc.noaa.gov__;!!DZ3fj= g!5e1aflgstvUqLmYSwqxhF5rv_F72s3nVeKNHDVcQHSlc89de3DKFfV2LcW_OBOEoVSsvOIxi6= INjKXUFvDFJV-3sIs0$ for graphic product...

    ATTN...WFO...LCH...SHV...HGX...FWD...

    LAT...LON 30879632 31769595 32149397 31559349 30849365 30529494
    30449572 30369612 30879632=20


    =3D =3D =3D
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