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From | To | Subject | Date/Time | |||
Mike Powell | All | DAY2SVR: Nws Storm Predic |
July 9, 2024 8:18 AM * |
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ACUS02 KWNS 090600 SWODY2 SPC AC 090559 Day 2 Convective Outlook NWS Storm Prediction Center Norman OK 1259 AM CDT Tue Jul 09 2024 Valid 101200Z - 111200Z ...THERE IS A SLIGHT RISK OF SEVERE THUNDERSTORMS OVER PORTIONS OF CENTRAL/NORTHERN PENNSYLVANIA AND WESTERN/CENTRAL NEW YORK... ...SUMMARY... Damaging gusts and a few tornadoes are possible mainly over portions of central/northern Pennsylvania and western/central New York. ...Synopsis... In mid/upper levels, a large anticyclone -- presently centered over south-central CA, will drift erratically northeastward to the southern Great Basin through day 2. Downstream, large-scale mid/upper-level troughing will persist over the central CONUS and mid Mississippi Valley through the period, with very slow net eastward shift. That will occur as the remains of TC Beryl eject northeastward from present position over AR, where it already is interacting with a midlatitude/low-level frontal zone. By the start of the period at 10/12Z, the associated deep-layer low should be over northern IN, with 500-mb trough southwestward across southern IL to the Arklatex region. The surface occluded/cold front should arc from that low across portions of OH to a triple point in PA, then southwestward over the central/southern Appalachians to northern/western GA and the coastal FL Panhandle, bending west-northwestward over the coastal LA region as a stationary front, then a warm front over central/west-central TX and southern NM. An eastern warm front should extend from the PA triple point east-northeastward over eastern PA, southeastern NY and central/eastern New England. The eastern warm front should move northward to central NY, and portions of VT/NH by 00Z. Meanwhile, the cold front should reach central/eastern portions of PA/VA, NC, and western SC, becoming quasistationary to warm over parts of southern GA/AL/MS, then continuing as an increasingly diffuse warm front from southern LA to north-central NM. ...Northeastern CONUS... Widely scattered to scattered thunderstorms are expected to develop along/ahead of the cold front, near the warm front, and possibly near a prefrontal surface trough over the outlook area from midday through afternoon and shift eastward to northeastward. Activity near the warm front will encounter a favorable parameter space for supercells and a tornado risk, along with short lines or clusters of thunderstorms with damaging to severe gusts. Veering winds with height should contribute to enlarged low-level shear/hodographs and deep shear (effective-shear magnitudes in the 45-55-kt range). Forecast soundings also suggest that a corridor of diurnal heating in the warm sector will combine with rich low-level moisture (surface dewpoints commonly upper 60s to low 70s F) to offset modest mid/upper-level lapse rates, for low LCL and peak/ preconvective MLCAPE in the 1500-3000 J/kg range. Given the lack of CINH and abundance of moisture, confidence in convective coverage and supercell potential has increased enough to raise unconditional severe probabilities a notch over the region. ...Portions of NM and west TX... Strongly difluent flow aloft will exist over this region east and southeast of the mid/upper high, while a series of minor shortwave perturbations and vorticity maxima move over the region in northwesterly to northerly flow aloft. Moisture return into this region over the next couple days, near the western limb of the diffuse warm front, should support increasing thunderstorm potential, with preferential initiation over higher terrain and convective/differential-heating boundaries. Low/middle-level flow and shear will be weak, leading to multicellular storm mode. Enough offset of strong heating/mixing by moist advection should persist through much of the afternoon to sustain favorably deep/robust, widely scattered to scattered thunderstorms atop high DCAPE over the "marginal" area. As a result, an unconditional threat for isolated severe downbursts exists, and a few small clusters may aggregate outflow for a couple hours to boost convective wind potential locally. The threat should wane quickly during the evening as the near-surface layer stabilizes. ..Edwards.. 07/09/2024 $$ --- SBBSecho 3.20-Linux * Origin: capitolcityonline.net * Telnet/SSH:2022/HTTP (618:250/1) |
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