• MESO: Mesoscale Discussion 0214

    From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sun Mar 10 04:27:34 2024
    ACUS11 KWNS 100427
    SWOMCD
    SPC MCD 100427=20
    MEZ000-NHZ000-100930-

    Mesoscale Discussion 0214
    NWS Storm Prediction Center Norman OK
    1027 PM CST Sat Mar 09 2024

    Areas affected...parts of northern New Hampshire into western Maine

    Concerning...Heavy snow=20

    Valid 100427Z - 100930Z

    SUMMARY...Sustained heavy snow appears most likely to become focused
    across the mountains of northern New Hampshire into northwestern
    Maine overnight into daybreak Sunday, including hourly rates
    increasing to 1-2+ inches per hour.

    DISCUSSION...A developing surface cyclone appears to be undergoing a
    period of more rapid deepening as it migrates across the northern
    Mid Atlantic region toward southern New England. Strengthening
    deep-layer ascent to the north-northeast of this feature, supported
    by lower/mid-tropospheric warm advection beneath an increasingly
    difluent and divergent upper flow field, is in the process of
    overspreading much of eastern New York and western New England,
    accompanied by moderate to heavy precipitation.=20=20

    Thermodynamic profiles near or below freezing are generally focused
    across the higher terrain, and with further low-level warming, may
    become increasingly confined to the mountains of northern New
    Hampshire into northwestern Maine overnight. This is where ensemble
    output (including the latest NCEP SREF and HREF) suggest highest
    probabilities for heavy snow rates developing and being maintained,
    perhaps at rates in excess of 2 inches per hour by 09-12Z.

    It appears that precipitable water within the saturating,
    sub-freezing profiles across this region may increase up to around
    .70 inches. Rapid Refresh forecast soundings indicate that this
    will coincide with a period of intensifying lift within a layer
    between roughly 600-500 mb, where the environment will become most
    conducive to large dendritic ice crystal growth with temperatures
    around -15 C. It appears that a fairly deep layer layer through the
    lowest few kilometers above ground level may become characterized by
    isothermal profiles near freezing, contributing to potential for
    considerable continuing snow flake growth via aggregation before
    reaching the surface as a "heavy, wet" snow.

    ..Kerr.. 03/10/2024

    ...Please see https://urldefense.com/v3/__http://www.spc.noaa.gov__;!!DZ3fj= g!8SUtpzwJkLiqchDBD-7LlaPvHHD_VuP0YTv1XDhZ1wg3XZqwu4ptJR-gyGaKMxbhiCFiKpPyU= YXdPd7NUc9Dw-3on3k$ for graphic product...

    ATTN...WFO...GYX...

    LAT...LON 45247007 44937001 44097102 43867142 44037185 44787129
    45567048 45247007=20


    =3D =3D =3D
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