Alaska Extended Forecast Discussion NWS Weather Prediction Center College Park MD 249 PM EDT Fri Jul 20 2018 Valid 12Z Tue Jul 24 2018 - 12Z Sat Jul 28 2018 At least for the moment (as of the 00Z-06Z cycles) guidance shows better than average agreement for the overall pattern evolution during the period. An upper low with associated surface system will likely persist for multiple days just south of the Alaska Peninsula. Consensus has trended a few degrees longitude west with this feature--and the ridges aloft to the west and east--compared to yesterday. The deep-layer low will tend to focus precipitation along/near portions of the Alaska Peninsula and southern coast of the mainland. Specifics are very uncertain but models/ensembles in principle are suggesting that height falls from eastern Asia and perhaps the extreme western Pacific should gradually migrate into the Bering Sea toward the late week/weekend time frame. This energy may merge with the aforementioned feature to the east. At the very least expect surface pressures to trend lower over the Bering in response to these height falls but model/ensemble spread and variability thus far yield low confidence in the surface details. Across the higher latitudes, initially progressive Arctic flow should lead to a front lingering over the North Slope region into day 4 Tue, followed by another front that arrives Wed-Thu. Latest consensus shows an upstream ridge aloft building eastward and eventually connecting with the northwest part of the ridge covering extreme western Canada into Mainland Alaska. The ECMWF ensemble mean has trended stronger with the late-period ridge aloft over recent runs but in principle has suggested this evolution with greater lead time than the GFS/GEFS mean/operational ECMWF. Confidence in the Arctic forecast is still moderate at best given the guidance spread/variability observed over preceding runs. The 12Z GFS highlights the forecast uncertainty as it has adjusted faster than consensus with Arctic features early-mid period and then is flatter than the 00Z/06Z runs with the trailing ridge aloft. The forecast blend started with input from the 00Z-06Z GFS/00Z ECMWF and lesser weight of the 00Z CMC/UKMET for days 4-5 Tue-Wed given good agreement in principle (with detail differences typical for an early-extended forecast) and support from the means. Question marks with Arctic flow precluded using the 12Z GFS in the forecast though the run seemed more reasonable farther south. After Wed the forecast used increasing amounts of the 06Z GEFS/00Z ECMWF means so that there was even model/ensemble weight by day 8 Sat. This solution brought some degree of low pressure into the western Bering late in the period with a surface trough/frontal axis extending southeastward. Potential exists for a system to exist within a fairly broad area along and either side of the axis of lower surface pressures. Rausch WPC medium range Alaskan products including 500mb, surface fronts/pressures progs and sensible weather grids can be found at: http://www.wpc.ncep.noaa.gov/alaska/ak_5dayfcst500_wbg.gif http://www.wpc.ncep.noaa.gov/alaska/akmedr.shtml http://www.wpc.ncep.noaa.gov/alaska/ak_5km_gridsbody.html