• Winter Storm to impact We

    From Dumas Walker@21:1/175 to All on Thu Feb 6 09:10:00 2025
    FOUS11 KWBC 060913
    QPFHSD

    Probabilistic Heavy Snow and Icing Discussion
    NWS Weather Prediction Center College Park MD
    413 AM EST Thu Feb 6 2025

    Valid 12Z Thu Feb 06 2025 - 12Z Sun Feb 09 2025

    ...Pacific Coast through the Northern Rockies... Days 1-2...

    ...Winter Storm to impact the West as a potent low tracks across
    California tonight, and the northern Rockies on Friday...

    A stormy pattern across the West will finally come to an end late
    this week as the upper level pattern resets to a much drier pattern.
    In the upper levels, the previous cutoff low centered near
    Washington State will rejoin the main jet stream and open up into a
    potent trough. This upper level low has quite a bit of shortwave
    energy circulating around it. This shortwave energy will support
    cyclogenesis off the California coast. The surface low will track
    northeastward over California and into Idaho, before transferring
    its energy to a leeside low over Colorado. The upper level trough
    will be weakening through late Friday night, however the surface low
    will tap into quite a bit of Pacific moisture which will be moving
    into the Pacific Northwest. The low-turned-trough will start out
    positively tilted but as it moves into the interior Pacific
    Northwest, it will become more neutrally tilted as its energy merges
    with the jet stream it is rejoining.

    NAEFS continues to show this system will have a significant Pacific
    feed of moisture with more than 500 kg/ms of Integrated Vapor
    Transport, which still tops the 99th percentile. Snow levels will
    rise ahead of the low but lower both behind it and to the north of
    the track. NBM snow levels into Oregon and Idaho will be around
    3,000 ft. Into the southern Sierras, snow levels will rise to above
    8,000 ft through the first half of Thursday night, then will drop to
    around 5,000 ft through midday Friday behind the cold front. For the
    northern Sierras, snow levels will stay between 6,000 and 8,000 ft.
    WPC probabilities for the Sierras are low to moderate (30-50%) for
    snow amounts above 24 inches. Into far northern California,
    probabilities are moderate to high (50-70%) for snowfall amounts of
    over 12 inches. While snow levels will be lower, there will not be
    nearly as much moisture available to convert to snowfall.

    From late Thursday night into Friday morning, the snow will spread northeastward into Idaho, Montana, and Wyoming. This will occur as
    the upper level shortwave trough forcing the surface low causing the
    snow lifts to the northeast and continues weakening. Meanwhile, a
    1030+ mb Arctic High will remain in place from Alberta and
    Saskatchewan and into the Northern Plains. This high will supply
    plentiful cold air to keep all of these areas as snow. Once again
    however, plentiful moisture from the warm side of the system will
    follow the cold conveyor belt into the northern Intermountain West,
    allowing for plenty of moisture for widespread snow. The greatest
    snow in this area will be into the Sawtooths of Idaho, Bitterroots
    of Montana and into the Wind River Range and Yellowstone/Teton N.P.
    areas of Wyoming. WPC probabilities in this area are moderate (40-
    60%) for 12 inches or more of snow through Saturday morning.

    WSSI values will get into the Extreme range (substantial disruptions
    to daily life and very difficult to impossible travel) for the
    southern Sierras with the heaviest snow today into tonight. Moderate
    to major impacts (Disruptions to daily life and avoid travel) are
    expected from the Klamath mountains of northern California into
    southern Oregon as well as through the Sawtooth and Wind River Ranges.

    Wegman

    ...Northern Plains through the Great Lakes and Ohio Valley... Days 1-3...

    A fairly potent shortwave trough can be seen over the southern
    Canadian Parries moving eastward with robust ascent focused within
    the diffluent axis of the trough. Lift is currently strongest
    across Northern MN into the Arrowhead north of Lake Superior.
    Forecast is for the disturbance to continue advancing eastward with
    the strongest forcing centered over Western Ontario into the U.P.
    of Michigan by the morning. Additional snow accumulations >4" are
    likely in-of the central and eastern side of the U.P. with the
    latest WWD probs ranging between 50-80% within the corridor south
    of Superior. Small section of elevated probs (40-70%) also exists
    within the Keweenaw Peninsula as well, a combination of synoptic
    based forcing with the potent shortwave, as well as some lingering
    lake effect later this afternoon.

    After a brief respite on D1 across the Northern Plains and Upper
    Midwest, the progressive flow across much of the CONUS will surge
    another winter storm system eastward into the Northern Plains to
    begin mid-D2. This system is progged to be much more impressive as
    a potent driving trough ejects from the Pacific Northwest and into
    the Northern Plains late-Friday night into Saturday morning. The
    overall mid- level pattern across the Northern Plains is progged to
    remain generally flat, but rapid height falls and a potent
    subtropical jet streak reaching 155kts will help push IVT
    exceeding the 90th percentile from NAEFS into the region. At the
    same time, strengthening WAA downstream of a low pressure moving
    across the Central Plains will draw higher moisture poleward, and
    the overlap of this WAA with the LER of the upper jet streak will
    produce a stripe of impressive 850-600mb fgen, efficiently lifting
    ascent into a deepening DGZ. This will result in a swath of snow
    from the Dakotas through Wisconsin, with an embedded band of
    heavier snow likely mainly intersecting the enhanced 700mb
    frontogen being depicted within all viable deterministic as of 00z.
    Spread has decreased among the deterministic with impressive probs
    for >6" being depicted by the National Blend (70-90%). Consensus
    among ensembles within the 00z GEFS/ECENS combo suggest high
    confidence for this event and impactful snow is likely across the
    Dakotas, especially northeastern SD and into Minnesota/Wisconsin.
    WPC probabilities have remain elevated given the latest trends,
    and now support a high risk (>70%) for more than 6 inches D2 over
    northeast SD through south-central MN and central WI, surrounded
    by a larger expanse of 40-60% from north-central SD through east-
    central WI. High probs >70% continue into D3 with emphasis over
    central WI over to the Lake Michigan shores, including the Green
    Bay area to the southern portion of the Door Peninsula.

    Farther to the southeast, the WAA will lift a warm nose more
    robustly immediately downstream of the surface low into the Upper
    Midwest and Ohio Valley. This will cause a stripe of mixed
    precipitation to develop on D3 from Illinois through eastern Ohio,
    and WPC probabilities increase once again, now featuring a 40-70%
    chance for at least 0.01" of ice over central IL through much of
    the northern half of OH.

    Weiss/Kleebauer

    ...Mid-Atlantic and Northeast... Days 1-3...

    Progressive moving shortwave analyzed over southern IL/LN will
    continue moving to the east-northeast with several smaller mid-
    level perturbations ejecting downstream of the mean trough. At the
    surface, cyclogenesis in-of Cape Hatteras has transpired with the
    expected low to progress rapidly to the northeast with modest
    strengthening as it approaches LI and Southern New England by
    later this morning. Further north, a formidable 1030mb high will
    continue to shunting eastward with the previous cold air filtering
    shutting off with prevailing easterlies likely occurring east of
    the Piedmont creating a textbook case of WAA nosing through a very
    shallow cold air mass. By morning, mixed precipitation will be the
    dominant ptype over the Northern Mid Atlantic with the depth of the
    cold air hanging on across New England and Upstate NY where snow
    will remain the primary ptype through the front part of D1. Higher
    elevations across New England will be the last areas to see any
    changeover from snow to IP/ZR, or at least have significantly
    degraded snow ratios due to the acceleration of warm air poleward
    into the area as southwesterly flow within the 850-650mb layer
    contributes to the mixed precipitation phases during the first half
    of the period. Maturation of the surface cyclone off the coast of
    New England should help maintain the cold air long enough within
    the confines of interior ME and Northern New England where snow
    will maintain the ptype through the period before the system moves
    out into the North Atlantic during the back half of the forecast.
    WPC probabilities for >4" remain elevated (40-70%) within those
    higher terrain areas of the Tug Hill, Adirondacks, Green and White
    Mtns., and the Southwest terrain over ME. Ice accumulations have
    trended fairly low with some prospects of 0.01-0.1" of ice
    accretion over much of PA through the Hudson Valley of NY and
    Southern New England. These areas should remain outside warning
    criteria, but there will still be some lingering hazards within
    those locales that receive any ice accretion.

    A sharp cold front will maneuver through the Northeastern U.S. by
    D2 creating a locally enhanced zone of LES off Lake Ontario with
    the primary fetch settled between flow between 270-290 deg.
    creating a persistent band between Oswego up towards Pulaski and
    areas downstream. The southern portion of the Tug Hill will be the
    benefactor of the LES development with general persistence in the
    band as it oscillates within that narrow corridor. Considering
    delta-T's nearing 20C off the lake behind the strong CAA regime,
    the band EL's between 15-20k ft will be sufficient for producing
    rates between 1-2"/hr at peak intensity within the band offering a
    narrow stripe of 6+" during the D2 time frame before the flow
    settles and the band falls apart. WPC probs within the anticipated
    axis is between 40-60% for >4" with a very small area of ~70% just
    downwind of the Lake near Pulaski.

    Finally by D3, a potent shortwave trough across the Plains and
    Midwest will continue to advancement eastward with a surface low
    spawning on the southern periphery of the trough axis across KS/MO,
    quickly moving east-northeast during the D2 into D3 period. A
    strong southwesterly WAA regime within the 850-600mb layer will
    transpire once again, only this time will generate a much more
    significant outcome of snowfall into New England. Very strong
    850-700mb frontogenesis will accompany the setup with a deep enough
    entrenched cold airmass over the Hudson Valley up through New
    England to support a significant snowfall back over the region.
    Surface low over the plains will move into the Ohio Valley with an
    expected surface low transfer off the Delmarva coast creating a
    prevailing east to northeast flow within the PBL that should create
    enough of a barrier for the WAA pattern further south penetrating
    much further than the NY state line across southeastern NY state.
    This has been signaled among much of the latest deterministic with
    a fair amount of ensemble support for this synoptic evolution. WPC probabilities are very robust for >4" with 70+% encompassing all of
    Western NY state through Central NY and the Hudson Valley. The
    higher probs extend well east into all of Southern New England with
    80% probs focused just to the west of the Boston Metro. Probs for
    8" are sufficiently within the 40-70% range across the Hudson
    Valley with the epicenter of the highest probs located over the
    Catskills and the Berkshires of western MA. Lower probs for at
    least 4" also exist over a large area surrounding the above zones,
    so there is a growing potential for an impactful snowfall occurring
    during the D3 time frame which includes much of Saturday into Sunday morning.

    Ice potential will also exist further south as the CAD wedge over
    the Mid-Atlantic will likely see repeating setup with WAA within
    the PBL causing issues concerning ptype transition from frozen to
    liquid hydrometeors. Similar to this past setup, areas northwest of
    the fall line in the Mid-Atlantic within the Piedmont will have the
    best chance for ice accretion after a short instance of SN/IP as
    the storm enters mid-D3. Highest probs for >0.1" of ice accretion
    still exists over the Laurel Highlands down into Western MD
    (40-60%), the same areas that are currently contending with ice
    this evening. It remains a fluid situation as guidance has not
    settled on the timing of the mixed phase to predominantly liquid
    ptype, but impacts are anticipated to be very similar to what is
    currently occurring.

    Kleebauer

    ...Winter Storm Key Messages are in effect. Please see current
    Key Messages below...

    https://www.wpc.ncep.noaa.gov/key_messages/LatestKeyMessage_1.png

    https://www.wpc.ncep.noaa.gov/key_messages/LatestKeyMessage_2.png

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