Alaska Extended Forecast Discussion NWS Weather Prediction Center College Park MD 201 PM EST Sat Jan 27 2018 Valid 12Z Wed Jan 31 2018 - 12Z Sun Feb 04 2018 At least for some aspects of the forecast, guidance has come into much better agreement. This is particularly the case for the evolution of energy initially southeast of the strong eastern Siberia upper high and position of the lingering weakness near the southern coast of the mainland, between the upper high and northeast Pacific ridge that builds in response to mean troughing that becomes established over the central Pacific. 00z/06z models have held onto the majority cluster that emerged from the 12z/26 cycle, showing an upper low retrograding along the Aleutians. This has been hinted at by the ensemble means even while operational models were very divergent. At the same time there is still meaningful uncertainty regarding interaction of this energy with central Pacific energy as the overall feature moves westward. To the east of the upper low, the weakness aloft near the southern coast of the mainland has ended up fairly close to the preferred compromise from continuity. Meanwhile significant spread persists regarding the northeastward extent of a front and associated precip over/near the Gulf of Alaska. This reflects differences in position of the northeast Pacific ridge aloft. Although consistent with its 12z/26 run, the 00z ECMWF is farther west with the upper ridge axis than other guidance including its ensemble mean. On the other hand the 06z GFS has backed up somewhat versus its 00z run. The current array of guidance and similarity/intermediate position of the 06z GEFS/00z ECMWF means at the surface and aloft recommend a solution closest to the means for this aspect of the forecast. By the latter half of the period the ensemble means have been fairly consistent in showing a gradual elongation of mean troughing, eventually extending from eastern Asia across the western half of the northern Pacific and south over the central Pacific. Eastern/northeastern Pacific ridging persists while the eastern Siberia upper high continues a slow clockwise loop toward northwest mainland Alaska. Most of the latest models show similar ideas, the exception being the 06z/12z GFS runs that collapse the upper high southeastward and potentially over-emphasize the northeast Pacific ridge. Even with the uncertainty in ridge specifics, there is a decent guidance signal that this pattern should lead to a period of enhanced moisture flow into the eastern Aleutians/southwest Alaska Peninsula by next weekend, with one or more surface waves tracking just west of the gradient. A blend of the 06z GEFS/00z ECMWF means along with minority input from the 00z ECMWF provides a good representation of the most likely evolution. Some ensembles go along with sporadic model runs that have been showing surface low tracks well into the Bering Sea, but so far in sufficiently low quantity to keep the means along or just south of the Aleutians. Recent trends suggesting that the means have been a little too eager to weaken the upper high favor maintaining some ECMWF weight in the forecast. Throughout the period the means have been consistent with an axis of surface high pressure extending from the Arctic through the northern mainland into northwest Canada. Any breaks in this mean surface ridge will depend on low confidence shortwave details aloft. Based on better agreement early in the period, today's forecast started with a 06z GFS/00z ECMWF/00z CMC blend from early day 4 Wed into day 5 Thu to provide better definition than the means. Increasing detail uncertainty plus lower confidence in various aspects of 06z GFS/00z CMC solutions after Thu led to trending the forecast to a blend among the 06z GEFS/00z ECMWF means and 00z ECMWF by late Fri through Sun. Rausch