Extended Forecast Discussion NWS Weather Prediction Center College Park MD 304 AM EDT Mon Oct 22 2018 Valid 12Z Thu Oct 25 2018 - 12Z Mon Oct 29 2018 ...Guidance/Predictability Assessment/Preferences... The synoptic-scale pattern ahead will initially feature a sprawled out upper trough extending from the Canadian Maritimes back up toward northern Nunavut. The southern extension of these lower heights should gradually gain latitude in response to the next system taking shape across the central U.S. A phasing of streams continues to be advertised which spawns a wave of low pressure traversing the northern Gulf of Mexico on Thursday/Friday before the parent shortwave attains a negative tilt. During the weekend, a strengthening coastal low will likely lift poleward in the vicinity of the Gulf Stream with potential impacts to the Eastern Seaboard. Farther upstream, quasi-zonal flow sets up over the northeastern Pacific through Friday which favors a series of perturbations to track into the Pacific Northwest and British Columbia coasts. A broad positive height anomaly emerges for the weekend across the western U.S. while migratory shortwaves traverse the top of the ridge with a track from British Columbia/Alberta toward the north-central U.S. Many solutions support significant amplification with a couple of these waves as they move toward the Mississippi River Valley over the weekend. Recent guidance is initially in decent agreement with much of the uncertainty looming around the phasing shortwaves and eventual low pressure development/progression. Ensemble low plots depict continued scatter although this is likely an artifact of a pair of waves initially in the picture. Operational models continue to waver with the ultimate timing of a deepening surface low off the southeastern U.S. coast Friday evening. On the western side of the spread are the 00Z UKMET as well as the 00Z/12Z ECMWF runs while the GFS solutions and their ensembles stay a bit farther offshore. Given the run-to-run variability and spread shown in the ensemble low plots, confidence still remains on the lower side with timing/position details. Moving westward, height falls dipping down from Saskatchewan will lead to another surge of colder air to the Mississippi River Valley region with the shortwave likely joining the downstream mean trough. Ensemble spaghetti plots show numerous spatial differences which somewhat hinges on the timing of the lead impulse. Finally, across the eastern Pacific and adjacent western coast of North America, ensemble means are at odds with one another by next Monday, October 29. The 12Z ECMWF ensemble mean has trended toward a longwave trough in this region while the 18Z GEFS/12Z NAEFS means favor quasi-zonal to weak ridging. Ensemble spaghetti plots reflect these differences with possible changes likely in future model cycles. Regarding the preference, utilized a combination of the 18Z/12Z GFS and 12Z ECMWF with their respective ensemble means (including the 12Z NAEFS) throughout the period. While initially weighting 80 percent of these operational runs into the mix on Day 3/Thursday, incrementally decreased their influences through the weekend before a full ensemble approach by the following week. ...Weather Highlights/Threats... The most active precipitation patterns will focus along the central/eastern Gulf Coast and along the Eastern Seaboard as well as back over the Pacific Northwest. Across the former regions, the mentioned surface low and accompanying tropical moisture fluxes will maintain a wet period from southern Louisiana eastward into the southeastern U.S. coast. As the coastal cyclone deepens over the Gulf Stream, comma-head precipitation should extend back into the Eastern Seaboard with impacts driven by the proximity of the wave to the coast. There may even be some wintry implications over the northeastern U.S. interior mountains. Back over the northwestern U.S., persistent onshore flow will allow for multiple days of orographically driven precipitation. The usual focus should be over the upslope terrain of the Olympics and Washington Cascades. Considering the temperature forecast, below average temperatures are in the forecast from the Great Plains eastward given the persistent of troughing. Some of the largest departures, on the order of 10 to 15 degrees, will congregate along much of the Eastern Seaboard given the extended period of cloud cover/precipitation as well as post-frontal cold advection. Meanwhile, milder weather will prevail over sections of the West Coast into the Intermountain West given the influence of Pacific air masses on the forecast. If the GEFS/NAEFS ensemble solutions were to verify, this mild weather could extend into the following week. Rubin-Oster WPC medium range 500 mb heights, surface systems, weather grids, quantitative precipitation, winter weather outlook probabilities and heat indexes are found at: https://www.wpc.ncep.noaa.gov/medr/5dayfcst500_wbg.gif https://www.wpc.ncep.noaa.gov/medr/5dayfcst_wbg_conus.gif https://www.wpc.ncep.noaa.gov/5km_grids/5km_gridsbody.html https://www.wpc.ncep.noaa.gov/qpf/day4-7.shtml https://www.wpc.ncep.noaa.gov/wwd/pwpf_d47/pwpf_medr.php?day=4 https://www.wpc.ncep.noaa.gov/heat_index.shtml