• HVYRAIN: Excess Rain D2-3

    From Mike Powell@618:250/10 to All on Wed Jun 24 08:47:13 2026
    FOUS30 KWBC 240729
    QPFERD

    Excessive Rainfall Discussion
    NWS Weather Prediction Center College Park MD
    329 AM EDT Wed Jun 24 2026

    Day 2 Valid 12Z Thu Jun 25 2026 - 12Z Fri Jun 26 2026

    ...THERE IS A SLIGHT RISK OF EXCESSIVE RAINFALL IN EFFECT OVER
    PORTIONS OF THE CENTRAL AND SOUTHERN PLAINS TO MID-MISSISSIPPI VALLEY...

    ...Plains to Mid-Mississippi Valley...

    Longwave pattern across the western two-thirds of the CONUS will
    shift as a strong mid-level trough enters the Pacific Northwest and
    begins flattening the ridge axis positioned across the
    Southwestern U.S. This will lead to a more zonal regime to setup
    from the Central Rockies to the Mid-Mississippi Valley by Thursday,
    setting the stage for a potentially significant heavy rainfall
    threat across portions of the Central and Southern Plains between
    KS/northern OK over into MO and western Ohio Valley. At the
    surface, a quasi-stationary front will be progged over southern KS
    stretching eastward through MO before hooking back to the northeast
    as a cold front on the trailing end of a surface low motioning up
    through eastern Ontario. A strong mid-level vort will eject out of
    the Central Rockies and migrate eastward within the mean flow,
    allowing for lee cyclogenesis to occur over KS as we move into
    Thursday afternoon. The forecast is for the surface wave to motion
    eastward along the boundary with thunderstorm initiation
    transpiring across the Central Plains by late-Thursday afternoon.
    As we move into the evening, additional LLJ support will provide
    better low-level shear and provide enhanced convergence within the
    proximity of the front. This is a relatively classic scenario for a
    training axis of heavy convection, especially when you couple with
    PWATs likely between 1.7-2.0", a solid +1 to +2 standard
    deviations above climatology for the region.

    Model signals are still pretty aggressive with the scope of the
    event with most of the deterministic outputs showing pockets of 3+
    inches for areas of eastern KS through portions of MO. The
    deviation comes in the timing of the shortwave ejection and the
    latitudinal gain of the heavy rain footprint as guidance disagrees
    on the exact placement of the heaviest rainfall. ML guidance is
    still generally south of the global NWP suite, a highlight that has
    been noted over the past several cycles. ML guidance tends to do
    well when it locks into these types of outputs and doesn't waver
    too much in specifics, so the trend is to keep the heaviest precip
    a bit south of the deterministic and its ensembles. That said, the
    orientation of the frontal positioning will be important as that
    will likely be the focus for where the heaviest QPF outputs will
    occur as the surface wave will ride the thermal gradient posed by
    the front in question. Historic bias at this leads tends to favor
    guidance being a bit too far north with its QPF footprint in these
    scenarios leading to an adjustment further south, correlating with
    a better convergent area away from the current depiction.
    Considering the magnitudes of the QPF already with little to no
    CAMs inclusion, the forecast for locally significant rainfall is
    becoming increasingly likely in the D2 period. As of now, the SLGT
    risk inherited only went through minor modifications with a high-
    end SLGT risk forecast for areas of central to southeast KS through
    the southwest and west-central portions of MO, extending towards
    the St. Louis metro where the frontal alignment is progged. An
    upgrade for portions of this area is not out of the question in the
    coming forecast cycles, so this will be something to monitor
    closely the next 24-36 hours.

    ...Southeast U.S...

    Remnants of a complex from the previous period will wander into the
    Central Gulf coast region and slide eastward into southern GA by
    Thursday afternoon. Hi-res at the end of their forecasts are
    consistent in the maturation of convection near the remnant
    circulation as the disturbance becomes a mechanism for targeted
    low-level convergence in a zone of favorable boundary layer
    moisture and instability. Signals for locally heavy rainfall of 2+
    inches are noted in the deterministic CAMs with the HREF blended
    mean QPF between 12z Thursday to 00z Friday showing pockets of
    1.5-2" located from the MS coastal areas through the I-10 corridor
    towards Tallahassee, back up into southern GA. This is coincident
    with the 500mb vorticity trajectory of our mid-level impulse
    generated from previous periods thunderstorms which provides a
    better target point for heavy rainfall compared to just your
    standard pulse convection regime we see in the summer. As a result,
    maintained the previous MRGL risk with just some minor adjustments
    to account for QPF trends.

    ...Interior West...

    Multiple shortwaves and elevated moisture presence across the
    Interior Mountain West will likely lead to another afternoon and
    early evening of scattered convection with localized flash flood
    concerns on Thursday. The threat remains low-end for the time being
    given the current QPF outputs, however this could still provide
    some isolated flash flood prospects in those terrain focused zones
    across UT/CO, as well as any heavy rain encounters in the favored
    slot canyon areas littered over western CO into UT. A MRGL risk was
    expanded westward to account for the threat and recent QPF trends
    in the guidance.

    Kleebauer


    Day 3 Valid 12Z Fri Jun 26 2026 - 12Z Sat Jun 27 2026

    ...THERE IS A SLIGHT RISK OF EXCESSIVE RAINFALL IN EFFECT OVER
    PORTIONS OF THE MID-MISSISSIPPI AND OHIO VALLEY'S...

    The period will be defined by the expected forward propagation of
    the shortwave trough that will affect the Central Plains, eastward
    during the D2, translating into further impacts on the D3.
    Ensembles and global deterministic alike continue to signal the
    axis of heavy rainfall over the Mid-Mississippi Valley shifting
    eastward through the Ohio River Valley with the focus of heaviest
    rainfall centered over the Ohio River basin and points north. This
    correlates with the mean 500mb vorticity forecast for the shortwave
    trough responsible as diffluent flow ahead of the trough axis will
    situate over the above area leading to focused ascent and
    increasing low to mid-level convergence pattern necessary to bring
    about a swath of heavy precipitation.

    00z run of the CSU First Guess Fields depict a broad SLGT risk
    alignment across the area between southern IN and southern OH down
    across neighboring northern KY with the northern periphery
    positioned along and south of I-70. Considering the trends in the
    CSU First Guess over the last several months, this may be a bit
    further north than what may transpire, however the ensemble QPF
    alignment of the heaviest precip is generally in that zone, so the
    decision was to add the SLGT risk matching the First Guess, but
    also hedging a bit further west and south with the expansion in the
    end. 01z NBM probs for >2" depict a 30-60% probability output
    between St. Louis to just east of Cincinnati with a northern
    inflection to the I-70 corridor between Indianapolis to Columbus,
    OH. The southern edge did expand south with the 30% probability
    from previous forecast to include areas south of the Ohio River, a
    testament to the potential to see a slight southern shift in the
    QPF focus as we move closer in time. In any case, the probability
    for >2" at this lead for the blend was more than suitable enough to
    warrant a SLGT risk addition to the now D3 period.

    The threat of heavy rainfall, even though more isolated due to the
    magnitude of the precipitation expected, is forecast to expand
    further east into the eastern Ohio Valley and neighboring areas of
    the Central Appalachians and western PA during the period.
    Considering the nature of the topographic elements allowing for
    those areas to be more prone to heavy rainfall episodes, this will
    be an area to monitor for any further adjustments in the risk
    which is currently at a MRGL for the time being.

    Kleebauer
    $$
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    * Origin: Capitol City Online (618:250/10)