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From | To | Subject | Date/Time | |||
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Mike Powell | All | HVYRAIN: Excessive Rainfa |
January 8, 2025 8:51 AM * |
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FOUS30 KWBC 080803 QPFERD Excessive Rainfall Discussion NWS Weather Prediction Center College Park MD 303 AM EST Wed Jan 8 2025 Day 1 Valid 12Z Wed Jan 08 2025 - 12Z Thu Jan 09 2025 The probability of rainfall exceeding flash flood guidance is less than 5 percent. Kleebauer Day 2 Valid 12Z Thu Jan 09 2025 - 12Z Fri Jan 10 2025 ...THERE IS A MARGINAL RISK FOR EXCESSIVE RAINFALL ACROSS THE MIDDLE AND UPPER TEXAS COAST AND WESTERN LOUISIANA GULF COAST... Large scale ascent ahead of an open, yet vigorous upper trough will help initiate surface cyclogenesis over the western Gulf with a modest push of warm unstable air in-of the TX coast, eventually into southwestern LA. Current guidance is coming into agreement on a skinny axis of heavier rainfall near the middle and upper TX coasts propagating east-northeast into the Lower Sabine by the end of the period with local amounts of 2-4" plausible within the heavier rain footprint. The driving component of the potential is still very much the increasing frictional convergence pattern on the western flank of the surface low as easterly winds bisect the TX coast up into LA with the core of better theta_E's remaining at the immediate coast and over the Gulf waters. The key is the onshore flow mechanism taking some of the convective cores offshore and moving them inland causing some heavier rainfall to protrude inland before running into a wall of cooler, more stable air thanks to an Arctic push that occurred prior to the evolving surface pattern. Recent NBM prob fields are >50% for locally 2+" of rainfall within some of the urban footprint in coastal TX which allows the opportunity for local flood concerns within those urbanized zones thanks to higher runoff potential. The saving grace from this being a higher risk is the agreement on minimal surface based instability with the mean SBCAPE in relevant ensembles hovering between 50-100 J/kg with some deterministic maybe exceeding that at the immediate coast. With the cells likely to struggle being rooted at the surface, the prospects of more widespread flash flooding are lower than normal creating a threat that is more localized and within the lower to mid bounds of the MRGL risk threshold. The previous forecast was generally maintained outside some adjustment further on the northern periphery of the risk area, aligning with the probability and mean instability fields. Kleebauer Day 3 Valid 12Z Fri Jan 10 2025 - 12Z Sat Jan 11 2025 ...THERE IS A MARGINAL RISK FOR EXCESSIVE RAINFALL ACROSS PORTIONS OF THE CENTRAL GULF COAST... Our favorable longwave trough and accompanying surface pattern will move eastward with the surface low over the Gulf moving onshore within LA by the first half of the period. Increasing surface convergence within the periphery of the surface low will generate an axis of heavier precipitation aligned within the modest frontogenetic setup within the northern periphery of the surface circulation. There's growing support for a heavy rain footprint over south-central LA, moving eastward into southeastern LA where the urban corridors centered around New Orleans come into play. Like the prior period, the instability pattern is meager, especially at the surface with most of the ascent driven within the top of the boundary layer and above where the area lies in the right-entrance region of the upper jet focused to the north. There is enough consensus on the location of heaviest rainfall within the that frontogenetic evolution, coinciding with a strong IVT pulse (~1000 kg/ms) being depicted within the NAEFS, a solid 4+ standard deviation interval for the time of year. This should help mitigate the negligible instability pattern in place and maintain a solid heavy rain footprint in that focal area mentioned above. Another consideration is the much colder grounds occurring prior to the arrival of the rainfall as Arctic air will navigate southward and allow for a period of near and sub-freezing air to harden the top soil layer creating a slightly higher potential for runoff. The MRGL risk from D4 was maintained and expanded to include much of south-central LA through southeast LA and coastal MS. There is a potential for a targeted SLGT risk in future updates, mainly within the corridor extending along and south of I-20 and just north of the coastal Parishes as the best flood threat will exist within the more urban zones. Kleebauer $$ --- SBBSecho 3.20-Linux * Origin: capitolcityonline.net * Telnet/SSH:2022/HTTP (618:250/1) |
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