• DAY1SVR: Marginal Risk S

    From Mike Powell@618:250/1 to All on Wed Mar 20 07:54:00 2024
    ACUS01 KWNS 201239
    SWODY1
    SPC AC 201238

    Day 1 Convective Outlook
    NWS Storm Prediction Center Norman OK
    0738 AM CDT Wed Mar 20 2024

    Valid 201300Z - 211200Z

    ...THERE IS A MARGINAL RISK OF SEVERE THUNDERSTORMS THIS
    AFTERNOON/EVENING ACROSS WESTERN OK/NORTHWEST TX...AND EARLY
    THURSDAY MORNING NEAR THE TX COAST...

    ...SUMMARY...
    Isolated, marginally severe storms will be possible this
    afternoon/evening across parts of western Oklahoma and northwest
    Texas. Isolated large hail will be possible early Thursday morning
    near the Texas coast.

    ...Western OK/TX Panhandle this afternoon/evening...
    A midlevel shortwave trough will begin to move eastward from AZ/NM
    toward west TX by tonight, with associated downstream cyclogenesis
    occurring today across eastern NM and the TX Panhandle. Low-level
    moisture return will be limited in the warm sector, with
    boundary-layer dewpoints ranging from 40-45 F as surface
    temperatures warm into the 70s this afternoon along a surface
    trough/front across western OK and the eastern TX Panhandle.
    Steepening low-midlevel lapse rates and cool midlevel temperatures
    will support weak buoyancy, and weak ascent along the boundaries
    could result in a few storms with the potential to produce
    marginally severe hail and strong outflow gusts. There is also a
    low probability of a non-mesocyclone tornado with developing
    updrafts along the slow-moving front in northwest OK later this
    afternoon, given steep low-level lapse rates/vertical vorticity
    along the front.

    ...South central TX to the coastal plain late tonight...
    Low-level moisture return will occur in earnest by tonight as a
    maritime tropical air mass spreads northward from the Bay of
    Campeche (along the prior stalled front) to the TX coast. Near the
    end of the period, destabilization will become sufficient for
    elevated thunderstorm development in the warm advection zone atop a
    diffuse coastal front. MUCAPE could reach 1000-1500 J/kg as
    moisture increase below midlevel lapse rates of 7.5-8 C/km, in an
    environment with sufficiently long hodographs (and some low-level
    curvature) for a conditional supercell/large hail threat mainly
    09-12z.

    ...Southern New England this afternoon...
    A deepening midlevel trough will move from ON to New England, as an
    associated cold front moves across New England later today and
    cyclogenesis occurs tonight near the ME coast. Moisture/buoyancy
    will be scant at best ahead of the cold front across southern New
    England, where some shallow/forced convection may occur along the
    cold front this afternoon. The convection could be associated with
    a few strong gusts, but the potential for convectively driven severe
    gusts appears too low to warrant introduction of an outlook area.

    ..Thompson/Grams.. 03/20/2024

    $$
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  • From Mike Powell@618:250/1 to All on Wed Mar 27 08:12:00 2024
    ACUS01 KWNS 271246
    SWODY1
    SPC AC 271244

    Day 1 Convective Outlook
    NWS Storm Prediction Center Norman OK
    0744 AM CDT Wed Mar 27 2024

    Valid 271300Z - 281200Z

    ...THERE IS A MARGINAL RISK OF SEVERE THUNDERSTORMS OVER PARTS OF
    THE NEAR-COASTAL SOUTHEAST...AS WELL AS PORTIONS OF CENTRAL AND
    NORTH TEXAS...

    ...SUMMARY...
    Isolated severe hail and damaging winds are possible over parts of
    the near-coastal Southeast, as well as portions of central and north
    Texas.

    ...Synopsis...
    A vast area of the CONUS begins the period with cyclonic mid/upper-
    level flow, thanks to nearly phased northern- and southern-stream
    synoptic troughs. The southern one is apparent in moisture-channel
    imagery from eastern NM to the Big Bend region of west TX, then over
    Coahuila, and should move eastward to AR, east TX and the
    northwestern Gulf by 00Z. The northern one is anchored by a 500-mb
    cyclone centered initially over northwestern MN, forecast to pivot
    to near Thunder Bay, ON, by 00Z, then northeastward to between Lake
    Superior and James Bay around 12Z. By then, phased troughing will
    extend from there across Lake Michigan and the lower Ohio Valley to
    the southern-stream perturbation over parts of AL, southeastern LA
    and the north-central/west-central Gulf.

    At the surface, 11Z analysis depicted an occluded low over northern
    ON, with an occluded/cold front to near BUF, PIT, and BKW, to a
    triple-point low near AGS. A cold front extended from there
    southwestward across the AAF area to the central/southwestern Gulf.
    A warm front was drawn from the southern low east-southeastward
    between SAV-CHS. The warm front should shift northeastward across
    coastal SC and the Low Country today. Another frontal-wave low may
    form tonight over SC then move offshore. The cold front should move
    slowly southeastward, reaching near an XMR-EYW line by 12Z tomorrow.

    ...Southeast CONUS...
    An ongoing belt of precip, with embedded/scattered thunderstorms,
    should continue to shift slowly eastward across the area, in step
    with (and near the position of) the front. The most intense cells
    will be capable of damaging gusts -- especially on and ahead of the
    boundary -- as well as severe hail. That includes a semi-organized,
    bowing storm cluster moving inland from the FL coastal bend, for
    another hour or so until it encounters substantially more stable air
    sampled by the 12Z TBW and JAX RAOBs.

    The near-surface layer -- initially stable over land from prior
    nocturnal cooling -- should undergo both gradual diabatic heating
    through anvil-cloud cover, and warm/moist advection through the
    afternoon. This will erode the morning stable layer and support
    peak preconvective/prefrontal MLCAPE of 1500-2000 J/Kg over parts of
    northern FL, and 1000-1500 J/kg over eastern GA and parts of SC.
    Flow aloft will remain strongly parallel to the front and the
    convective plume, continuing a messy convective character with
    embedded thunderstorms. Forecast hodographs support a blend of
    sporadic left- and right-moving supercells, and mainly organized
    multicells, with stronger shear and buoyancy but somewhat weaker
    lift over southern parts of the outlook area. As the threat appears
    sporadic and spatially isolated -- not very well-focused in time or
    within the broader precip swath -- probabilities are held at
    marginal unconditional thresholds for now.

    ...Central/north TX...
    Widely scattered thunderstorms are possible for a few hours this
    afternoon into early evening, moving eastward to southeastward, with
    isolated severe hail and strong to marginally severe gusts possible.

    An area of surface low pressure over eastern NM -- initially tied to
    lee troughing that extends well poleward into AB -- will split off
    and move southeastward over northwest/north-central TX this
    afternoon in response to the perturbation aloft, with a trough/
    convergence zone to the south or south-southeast across central TX.
    These features should provide enough lift for convection, amidst
    minimal capping. As the mid/upper trough shifts toward and over the
    area, very cold air aloft (500-mb temperatures at or below -25 deg
    C) will contribute to steep midlevel lapse rates exceeding 8 deg
    C/km. Despite being seemingly cool at the surface and well behind
    the cold front, diabatic heating and residual moisture (dewpoints
    generally mid 30s to mid 40s F) should erode MLCINH by mid/late
    afternoon, with 300-700 J/kg MLCAPE possible. Though low-level flow
    will be weak, enough deep shear should exist to support multicells
    and at least transient supercell structures, atop a well-mixed
    subcloud layer. The threat should wane by about 03Z as the
    near-surface layer stabilizes and coverage/intensity of what had
    been mostly diurnally driven convection diminishes.

    ..Edwards/Leitman.. 03/27/2024

    $$
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