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827 FXUS66 KPDT 160457 AFDPDT Area Forecast Discussion National Weather Service Pendleton OR 957 PM PDT Tue Mar 15 2022 .AVIATION...06Z TAFs...Currently all TAF sites are VFR and will remain as such over the forecast period. Showers and winds have decreased across all sites although around 18Z the winds pick up slightly across the Gorge and Basin. KDLS will experience some locally breezy winds of 13 kts with gusts to 20kts as a cross Cascade gradient tightens and moves over the Mts. VIS will remain at P6SM and CIGs will lift to 100kft or more overnight into tomorrow. Bennese/90 && .PREV DISCUSSION... /issued 742 PM PDT Tue Mar 15 2022/ EVENING UPDATE... No real update to the previous forecast. Showers have begun to dwindle for the lower elevations as the trough has moved off to the east. The leading edge of the incoming ridge has begun to move onshore and the axis of the ridge is just off the coast of British Columbia. This ridge will continue to move through the region relatively quickly Wednesday giving us a quick dry spell before the next trough system arrives onshore Thursday. Winds will remain breezy through this evening and will begin to decrease by tomorrow morning. Bennese/90 && SHORT TERM… Tonight through Thursday night… Conditions trend drier and calmer across the CWA tonight through Wednesday with lingering mountain snow showers providing the primary impacts moving forward. After a brief dry break across the region Wednesday night a weak trough moves into the Pacific Northwest the second half of Thursday into Thursday night bringing another chance for light precipitation, mainly to the higher terrain. The trough of low pressure that gave us today’s unsettled, breezy, and showery conditions continues to progress east overnight while a transient ridge approaches off the coast. This will lead to shower activity gradually decreasing, retreating closer to the higher terrain of the Cascades and Blues Mtns/Wallowas tonight into Wednesday. Guidance also has breezy/gusty winds decreasing this evening and overnight as well likely in response to the loss of daytime heating mixing winds down from aloft and weakening pressure gradients. The axis of the transient ridge moves overhead later in the day on Wednesday shifting the upper-level flow more northerly and bringing an end to any remaining mountain showers later in the afternoon. Snow accumulation tonight through Wednesday isn’t all that impressive over the mountains with the highest totals over the Washington Cascades and into the northern Blues; the bulk of any snowfall impacts occur before noon Wednesday. Otherwise models are in good agreement for the rest of the region to remain dry. Thursday a weak upper-level trough pushes into the Pacific Northwest from offshore while the ridge of high pressure vacates to the east. There’s been some model disagreement on the exact timing of this disturbance however the latest runs of the GFS and ECMWF ensemble means and their receptive deterministic counterparts indicate light precipitation working into the Cascades Thursday afternoon then spreading to the mountains of eastern Oregon in the evening. Considering QPF totals with this disturbance stay less than a tenth of an inch or two and snow levels remain in the 4-5kft range, snowfall impacts appear minimal for the pass areas. The Columbia Basin and Deschutes Basin and are likely skipped over entirely; dry weather persists. 99 LONG TERM...FRIDAY THROUGH MONDAY...The extended period is characterized by an upper level trough that will bring widespread rain and mountain snow across our area through the early part of the weekend. High temperatures will also be dropping 10 degrees from Friday through Sunday, with values from the low-60s Friday into the low-50s on Sunday across lower elevations. Southwest winds will also be increasing over the weekend as gusts of 20-25 mph are expected along the east slopes of the Washington Cascades and through the Eastern Gorge. The EFI is also highlighting that some ensembles are picking up unclimatologically high rain/snow amounts for this time of year over the Oregon Cascades on Saturday. Snow amounts of 4-8 inches are likely along the Oregon Cascades and 1-3 inches for the Washington Cascades and Eastern Mountains. Current forecasted rain amounts of 0.60-0.80 inch for the Oregon Cascades, 0.25-0.50 inch for the Washington Cascades, 0.15-.0.25 through the Eastern Mountains, 0.05-0.15 inch for Central Oregon, and 0.01-0.05 through the foothills of the Blue Mountains and the east slopes of the Washington Cascades are likely. The Lower Columbia Basin is expected to only see a trace of precipitation during this timeframe. A transient ridge will pass through our area on Friday, allowing for the warmest day in the forecast to occur as highs peak in the upper- 50s to low-60s across lower elevations of the Basin and through Central Oregon. Cloud cover will slowly increase through the day as the ridge exits our region through the evening and overnight period. This is in response to a digging upper level trough that will push onshore and into our region during the late morning and afternoon hours on Saturday. Rain and mountain snow will begin along the Cascade crest late Friday evening before spilling into the Basin and causing widespread rain chances throughout our area by early Saturday morning. Showers will begin to be more confined to mountain regions through the afternoon and early evening as the trough continues to dig to our south and east. As this system departs our area, an upper level ridge will infiltrate into our area and initiate northwest flow aloft. This will drop snow levels from 3000- 4000 feet Saturday to 1500-2500 feet on Sunday. The ridge continues to build into Monday, but consistent northwest flow aloft will keep the potential for upslope showers over the Washington Cascades and Blues to continue. Snow levels will also increase quickly Monday into Tuesday, reaching into the 5000-7000 feet range. High temperatures will also be steadily increasing by about 5 degrees each day from Sunday through Tuesday. Guidance is in good agreement with the overall synoptic pattern, but there are differences that arise relating to trough strength and subsequent ridge strength/timing. The GFS incurs a stronger trough than the ECMWF, which correlates to stronger winds associated with the passing system. The ECMWF provides a slightly wetter outcome on Saturday, but dries out quicker due to the upper level ridge following closer to the departing trough. 500mb EOF patterns highlight these differences in trough strength and subsequent ridge timing on Sunday. The cluster 500 mb heights provide more confidence in the ECMWF outcome as the majority of its ensembles and the Canadian ensembles are more in line with the ECMWF deterministic scenario. However, the cluster phase space shows that the ECMWF deterministic is not as representative as the ensemble mean beginning Monday as associated with the incoming ridge. Thus, there is high confidence in the ECMWF when associated with the incoming system on Saturday, but confidence wanes when relating to the faster speed of the incoming ridge on Monday as determined by the ECMWF. 75 && .PRELIMINARY POINT TEMPS/POPS... PDT 35 54 32 58 / 10 10 0 0 ALW 39 57 36 61 / 10 10 0 0 PSC 40 61 36 61 / 0 0 0 0 YKM 32 59 31 56 / 10 0 0 10 HRI 38 58 35 60 / 0 0 0 0 ELN 33 54 32 52 / 10 0 0 10 RDM 29 54 30 58 / 10 0 0 10 LGD 33 46 28 49 / 40 20 0 0 GCD 30 49 29 55 / 20 10 0 0 DLS 40 57 38 58 / 30 10 0 20 && .PDT WATCHES/WARNINGS/ADVISORIES... OR...None. WA...None. && $$ SHORT TERM...90 LONG TERM....75 AVIATION...90