Mesoscale Precipitation Discussion 0071 NWS Weather Prediction Center College Park MD 1220 PM EST Tue Feb 20 2024 Areas affected...Central California... Concerning...Heavy rainfall...Flash flooding possible Valid 201720Z - 202315Z SUMMARY...Scattered slow-moving but locally intense downpours pose .5-.75"/hr rates with up to 1.5" totals pose possible localized flash flooding concerns, especially near urban settings. DISCUSSION...GOES-W WV denotes a subtle inflection in the broad southwesterly flow along the Central CA coast. This is along the western cyclonic portion, weakly diffluent edge of the 150kt jet currently over south-central CA, providing sufficient upper-level divergence to further amplify the wave. Combined with sharpening core of the upper-level trof near 41.7N 127.3W along with broad CAA aloft is providing a steepening lapse rates increasing available instability for convective development in the next few hours. MUCAPE to 750-1000 J/kg near coast remains to 250-500 J/kg into the southern Sacramento Valley. GOES-W GLM and Visible loop shows recent convective development nearing the mouth of San Francisco Bay, given depth of modest moisture and 15-20kts of low level moisture convergence (within .75" total PWats) suggest rates of .5"/hr are possible within the core of the narrow updraft cores. Weak bulk shear to 30kts and favorable back-building flow regime suggest some slow cell motions and perhaps weak rotation for increased isallobaric moisture flux to potentially reach a low end possibility of .75"/hr rates particularly near the instability source for the next few hours before height-falls from the main trof press this regime eastward after 00z. A spot or two of 1-1.5" totals are not out of the realm of possibility. Given the rates/short-duration, localized flash flooding is considered possible given well above normal run-off capability given saturated ground conditions (per NASA SPoRT LIS). Further east...As cells translate through the Napa Valley/Santa Cruz range toward the Sacramento Valley, cells will weaken with diminished instability but some filtered insolation may help some buoyancy to maintain weaker elevated cells. Deep layer flow will continue to support narrow banded-like features translating eastward allowing for some training and increased duration. With reducing rates but increased duration streaks .5-1.25" are possible and may induce some nuisance flooding especially near urban/poor draining locations. Gallina ATTN...WFO...EKA...MTR...STO... ATTN...RFC...CNRFC...NWC... LAT...LON 39602185 39462115 38982095 38442103 37842113 37182142 37002184 37032238 37432277 38362335 38892319 39432248Download in GIS format: Shapefile | KML
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