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From | To | Subject | Date/Time | |||
Mike Powell | All | Heavy Rainfall WA/OR/CA |
November 13, 2024 8:53 AM * |
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AWUS01 KWNH 130750 FFGMPD CAZ000-ORZ000-WAZ000-131800- Mesoscale Precipitation Discussion 1152 NWS Weather Prediction Center College Park MD 250 AM EST Wed Nov 13 2024 Areas affected...Coastal and Cascades Ranges of E WA & E OR...Northwest CA... Concerning...Heavy rainfall Valid 130800Z - 131800Z SUMMARY...Progressive but potent slug of enhanced moisture flux along Coastal and Cascade Ranges producing 2-4" totals with occasional hourly rates to .5"/hr with greatest totals in SW facing orography increasingly so in SW OR/NW CA. DISCUSSION...GOES-W WV shows main core of the upper-low just south of 47N near 132.5W starting to slide northeast with upstream energy starting to dig the upper-trough, expecting to go more neutral tilt over the next 6-12hrs as it approaches the West coast. The 150kt jet core just rounding the base of the trough is broadening with large cirrus shield. GOES-AMV and RAP analysis note a split in the jet downstream northeast of the 40N130W benchmark; this is enhancing broader and more intense upper-level divergence along the Oregon coastline. Additionally, a weak inflection is developing in the low levels with upstream height-falls leading to sharper boundary layer moisture convergence along and downstream backing the progressive frontal zone a bit more flat to the mean steering flow and increasing deeper layer moisture convergence. CIRA LPW notes, 1-1.25" total PWat in this area where surface and slug of 850-700mb moisture overlap. Given 60-70kts of 850mb flow (~700-900 kg/m/s IVT), convergence is going to result in enhanced showers capable of .5-.6"/hr rates likely to intersect the northwest to central OR Coastal Range over the next few hours. So while the strength of orographic ascent will be consistent along the front, this slightly backed flow ahead of the inflection will have increased totals compared to the average 2-3" totals, some localized 3-4" values may occur before midday. Strength of AR and moisture flux may be supportive enough to bleed through the coastal range with some enhanced rainfall totals across the western slopes of the northern and central Oregon Cascades. To the north western WA... Post cold front showers will remain widely scattered, and with steeper lapse rates will support higher but much shorter duration rainfall across areas with modest 2-3" totals so far through the event, while NASA SPoRT soil saturation values are higher than normal, the burst nature is still not likely to result in any rapid inundation/flashy conditions but maintain above normal run-off. South of the inflection across SW OR into NW CA... The core of the AR moisture stream will remain along/ahead of the cold front, but will be narrowing as the mid-level moisture slug slides ashore and surface moisture band narrows/stretches in width. Height-falls will swing through later in the morning/early afternoon, but traditionally favorable southwesterly flow into generally steeper terrain and confluent 45-50kts of 850 flow around the Cape, prolonged moderate rainfall with streaks of enhanced showers up to .5"/hr are probable. This is still fairly gentle/typical for the boreal rain forests to handle much of the rainfall, and while run-off will be enhanced is not likely to result in any significant concerns that would not be for an ordinary AR. IVT values will be decreasing with reduced moisture/low level flow from 800 kg/m/s across the central OR coast toward 500-600 kg/m/s. Still, traditional orographic ascent will support spots of 2-3" by 18z. Gallina ATTN...WFO...EKA...MFR...PQR...SEW... ATTN...RFC...CNRFC...NWRFC...NWC... LAT...LON 49052223 49052156 48412141 46912178 45782182 44322201 43042201 42212223 41802250 41082314 39922370 39922426 40262453 40672460 41272434 41832441 42292464 42812479 43492460 44162434 45292434 46312415 47362445 47962475 48452475 48192381 47962344 47252329 46952317 46832291 47102235 47622223 $$ --- SBBSecho 3.20-Linux * Origin: capitolcityonline.net * Telnet/SSH:2022/HTTP (618:250/1) |
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