Prognostic Meteorological Discussion
Issued by NWS
Issued by NWS
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111 FXAK02 KWNH 142205 PMDAK Alaska Extended Forecast Discussion NWS Weather Prediction Center College Park MD 504 PM EST Tue Jan 14 2025 Valid 12Z Sat Jan 18 2025 - 12Z Wed Jan 22 2025 ...Stormy pattern later this week/weekend from Western/Southwest Alaska through the Alaskan southern tier... ...General Overview... It remains likely that stormy weather will continue late this week through at least the upcoming holiday weekend for parts of the Aleutians, western/Southwest Alaska, and the Southern Coast with plenty of onshore flow ahead of mean troughing through the Aleutians and Alaska Peninsula. A couple of shortwaves rotating through the base of this trough will lift across western Alaska, eventually working to work into strong ridging extending from the Gulf into Mainland Alaska. Another upper low/trough looks to edge south of the Aleutians and possibly into the Bering towards the end of the period that would act to rebuild the downstream upper ridge next week. ...Model Guidance Assessment... Guidance continues a recent trend for relatively good agreement on the overall synoptic pattern, but plenty of uncertainty in the details. Much of the uncertainty surrounds smaller scale shortwaves rounding through the base of the larger scale trough over the Bering/Aleutians and as energies lift poleward on the western periphery of an ambient and amplified blocky ridge downstream up over the mainland. This includes individual surface/triple point lows lifting towards the AK Peninsula to Southern Coast into this weekend, which will work to enhance local winds/precipitation. The bulk of guidance agrees that one shortwave this weekend should act to briefly push upper ridging over the Mainland/Southeast eastward to a degree, but should build back again ahead of the next trough into the Bering/Aleutians early next week. Overall, prefer a composite of reasonably clustered medium to larger scale guidance of the 12 UTC ECMWF/UKMET/Canadian to provide maximum detail for Saturday-Monday. The 12 UTC GFS seems to crash energy too much into the ambient blocking upper ridge this weekend versus running system energies more up the western periphery. Opted to transition to best compatible guidance from the 12 UTC GEFS/ECMWF/Canadian ensemble means amid slowly growing forecast spread through longer time frames. WPC product continuity seems reasonably well maintained in this manner. ...Weather/Hazards Highlights... It generally remains the case that heavy precipitation will spread across South-central and parts of Southeast Alaska through the holiday weekend as a broadening closed low expands slowly eastward, shifting the atmospheric river from the Pacific slowly in that direction with time as tempered by the blocking ridge. Rain should linger across the Aleutians and southwest AK through the period. Recent model runs have also indicated moderate to heavy precipitation chances increasing for parts of western/Southwest Alaska as well, and to a lesser extent the Interior. Above normal temperatures will make rain the main precipitation type in southwest AK and for coastal locations, but wintry mixed precipitation and snow will be possible farther north and at elevation. Rain falling on top of snow could enhance snowmelt and lead to localized flooding concerns in some areas, such as Kodiak Island. The strong nature of the low will also likely produce strong gusty winds from the Aleutians to western Alaska across the Bering Sea and Bering Strait. A lingering front and strong pressure gradient may make the Northern Slope breezy as well. Schichtel Additional 3-7 Day Hazard Information can be found on the WPC medium range hazards outlook chart at: https://www.wpc.ncep.noaa.gov/threats/threats.php WPC medium range Alaskan products including 500mb, surface fronts/pressures progs and sensible weather grids can also be found at: https://www.wpc.ncep.noaa.gov/alaska/ak_5dayfcst500_wbg.gif https://www.wpc.ncep.noaa.gov/alaska/akmedr.shtml https://www.wpc.ncep.noaa.gov/alaska/ak_5km_gridsbody.html $$