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|    WEATHER    |    Messages from the national weather servi    |    41,475 messages    |
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|    Message 39,432 of 41,475    |
|    COD Weather Processor to wx-storm@lists.illinois.edu    |
|    MESO: Nws Weather Prediction Center Coll    |
|    15 Dec 25 09:36:32    |
      TZUTC: 0000       MSGID: 167636.weather@1:2320/105 2da79b7c       PID: Synchronet 3.21a-Linux master/123f2d28a Jul 12 2025 GCC 12.2.0       TID: SBBSecho 3.28-Linux master/123f2d28a Jul 12 2025 GCC 12.2.0       BBSID: CAPCITY2       CHRS: ASCII 1       FORMAT: flowed       AWUS01 KWNH 150936       FFGMPD       ORZ000-WAZ000-152135-              Mesoscale Precipitation Discussion 1263       NWS Weather Prediction Center College Park MD       435 AM EST Mon Dec 15 2025              Areas affected...Western WA and Northwest OR              Concerning...Heavy rainfall...Flash flooding possible              Valid 150935Z - 152135Z              SUMMARY...A new atmospheric river will be arriving this morning       across the Pacific Northwest. New rounds of heavy rain will be       associated with this across especially western WA and northwest       OR, and this will gradually pose a renewed threat of flooding.              DISCUSSION...The latest GOES-W WV suite along with OSPO/CIRA ALPW       data shows a new trans-Pacific atmospheric river approaching the       Pacific Northwest. The source region of the long-fetch moisture       transport is situated well southwest of Hawaii along 160W to 170W,       with a northeast advection of it up along and ahead of a       well-defined frontal zone that extends from Hawaii to offshore of       the West Coast. Satellite imagery and surface data also shows       additional northern stream energy and a reinforcing cold front       approaching from areas near and south of the Gulf of AK.              Over the next 6 to 12 hours, strong deep layer southwest flow with       embedded shortwave energy will approach and begin crossing the       Pacific Northwest which will drive the aforementioned offshore       fronts gradually inland across the coastal ranges. Strong warm air       advection and enhanced low to mid-level flow will drive increasing       rainfall rates across the orographically favored coastal ranges       from northwest OR up into the Olympic Peninsula and eastward into       the foothills and higher terrain of the Cascades.              Microwave-based CMORPH2 data shows heavy rainfall rates associated       with the offshore shortwave energy focused along 130W, with some       rates on the order of 0.75" to 1"/hour. This is associated with       broken areas of convection as validated by GOES-W GLM data       indicating intermittent lightning activity. Some of these heavier       rates should arrive gradually throughout the morning, and the 00Z       HREF guidance shows high probabilities (>60%) of rainfall rates       exceeding a 0.50"/hour across the Olympic Peninsula and the       foothills of the Cascades, with some low-end probabilities       (approaching 30%) of seeing these rates max out near 1"/hour in       the central and southern WA Cascades.              These high rates will coincide with the arrival of high IVT       magnitudes that will be on the order of 800 to 1000 kg/m/s into       the coastal ranges, with an inland penetration of the core IVT       plume into the Cascades. Some modest instability with MUCAPE       values up around 250+ J/kg along and just ahead of the frontal       boundaries will also be a contributor to these elevated rates.              Expect as much as 3 to 5 inches of new rainfall over the next 12       hours, with the heaviest totals over the Olympic Peninsula and the       windward slopes of the WA Cascades. Lesser amounts will be noted       over northwest OR with as much as 1 to 3 inches here involving the       orographically favored terrain.              The region is extremely sensitive given the residual impacts from       the recent high-impact multi-day atmospheric river. Elevated/high       streamflows and saturated ground will support the additional rains       going into runoff that will be capable of driving renewed areas of       areal flooding. Some localized burn scar flash flooding, debris       flows and landslide activity also cannot be ruled out today.              Orrison              ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!=       DZ3fjg!8CSOBZPag-i-C1aXm6jQzW12n-4RBwiZpBMzlfmSn5drA27YKyMJLZE9060HaBqpt42K=       23iAiSQIlsvBBUL7myAJ6NQ$ for graphic product...              ATTN...WFO...OTX...PDT...PQR...SEW...              ATTN...RFC...PTR...NWC...              LAT...LON 49262217 49252090 48782034 47882038 46802093=20        45402127 44392175 44302231 44662313 44682399=20        45742427 47102424 48002466 48222357 47692293=20        47822252 48592230=20              =3D =3D =3D       To unsubscribe from WX-STORM and you already have a login, go to       https://lists.illinois.edu and use the "Unsubscribe" link. Otherwise email       Chris Novy at cnovy@cox.net and ask to be removed from WX-STORM.              --- SBBSecho 3.28-Linux        * Origin: Capitol City Online (1:2320/105)       SEEN-BY: 1/19 100 16/0 19/10 37 104/119 105/81 106/201 114/10 120/302       SEEN-BY: 123/130 128/187 129/14 142/104 153/757 7715 154/10 30 50       SEEN-BY: 154/110 700 201/0 203/0 218/700 840 220/10 20 30 90 221/1       SEEN-BY: 221/6 360 226/18 30 44 50 227/114 229/110 134 206 300 307       SEEN-BY: 229/317 400 426 428 470 664 700 705 240/5832 266/512 280/5003       SEEN-BY: 291/111 301/1 320/119 219 319 2119 322/757 762 326/101 335/364       SEEN-BY: 341/66 342/200 396/45 423/81 460/58 633/280 712/848 902/26       SEEN-BY: 2320/0 105 304 3634/12 5020/400 5075/35       PATH: 2320/105 154/10 221/6 1 320/219 229/426           |
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