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From | To | Subject | Date/Time | |||
Mike Powell | All | Heavy Rain/Flooding LA |
November 13, 2024 8:53 AM * |
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AWUS01 KWNH 131111 FFGMPD MSZ000-LAZ000-131635- Mesoscale Precipitation Discussion 1153 NWS Weather Prediction Center College Park MD 611 AM EST Wed Nov 13 2024 Areas affected...South-central Louisiana... Concerning...Heavy rainfall...Flash flooding possible Valid 131110Z - 131635Z SUMMARY...Slow moving, efficient cells capable of 2.5"/hr rain rates. Training profile and upstream redevelopment pose risk of localized flash flooding with 3-4" totals possible. DISCUSSION...The remnant low level circulation of Rafael has been shearing north to south through a deep axis, but has retained a few convergent low-level bands and fairly robust core of anomalous deep layer moisture. Aloft, large scale ridge over-top the circulation is also being stretched/amplified along/ahead of height-falls coming out of the central Plains. As a result, weak 850-500 DPVA is providing ascent and low level wind response to increase surface to boundary layer moisture convergence with 25kts of 850mb flow from the southeast cyclonically converging at the apex/downshear of the wave just south of central LA coastline. A core of enhanced inability also exists through this moisture transport axis with 2000-2500 J/kg of SBCAPE to provide strength to vertical development over the next few hours. Within this axis, CIRA LPW shows core of enhanced moisture with 1-1.1" in the sfc-850, and over .5" in the 850-700mb layer. Both are near the 99th to maximum percentile for climatology in November. Current GOES-E SWIR/10.3um EIR along with RADAR denotes initial convective development near Marsh Island lifting north through the best convergence/confluence axis. Cells are initially weaker with 1-1.5"/hr rates, but with increasing DPVA/strengthening of the winds strengthening convergence, coverage of cells capable of 2-2.5"/hr are likely to become more numerous as winds strengthen to 20-30kts by 13-14Z. Deep layer moisture is confluent into increasing FGEN/moisture axis, deformation zone that extends into central LA and up the Lower MS River Valley/Delta Region. As such, a favorable upstream convergence should support upstream development for potential training/repeating into a slowly (0-5kt) eastward drifting moisture gradient. Modest effective bulk shear in the 25-30kt range, suggest some weak rotation to the updrafts could further slow forward propagation resulting in localized axis of 2-4". While current trends suggest most cells will remain near the coast in the near-term, mid-morning could see further downstream motions toward areas of recent heavy rainfall and saturated upper soil depths...while FFG value have rebounded, 0-40cm saturation ratios remain over .65 which is the 90th-95th percentile, suggesting increased runoff in more likely north of I-10 into central LA. Still, coastal regions may be more receptive and scattered flash flooding/rapid inundation is considered possible through 16z. Gallina ATTN...WFO...JAN...LCH...LIX...SHV... ATTN...RFC...LMRFC...NWC... LAT...LON 31769219 31579159 30609114 29649066 29069024 28929090 29369197 29489241 29539295 29939321 31079309 31539277 $$ --- SBBSecho 3.20-Linux * Origin: capitolcityonline.net * Telnet/SSH:2022/HTTP (618:250/1) |
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