Model Diagnostic Discussion NWS Weather Prediction Center College Park MD 150 AM EST Mon Dec 17 2018 Valid Dec 17/0000 UTC thru Dec 20/1200 UTC ...See NOUS42 KWNO (ADMNFD) for the status of the upper air ingest... 00Z Model Evaluation...with Final Preferences and Confidence ~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~ ...Overall Pattern Across the CONUS... ~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~ Preference: General Model Blend through 20/00z 00z ECMWF/GFS Model Blend across the West after 20/00z Confidence: Slightly Above Average Model agreement continues to be above average across the CONUS through late Wednesday. Across the East, the 00z NAM may be too far east with the track of the surface low initially (as is the 00z UKMET), but catches up to the remainder of the guidance by 28/12z over the northern tip of Nova Scotia. Otherwise, there is very good model agreement with the synoptic scale systems through the period. Out West, the flow becomes less amplified as the fast mid level flow is shunted back across the Pacific Northwest into British Columbia by a strengthening mid level ridge west of Baja California. Toward the end of the period, the mid level ridge starts breaking down as a positively tilted long wave trough well west of the US West Coast slowly approaches. The 00z NAM is the slowest solution across the northern portion of the trough, closing off a mid level system well west of the model consensus, which could delay the arrival of precipitation across the Pacific Northwest toward 20/12z. The 00z UKMET has followed suit with its slower and stronger mid level solution, also delaying the onset of precipitation beyond 20/12z. The 00z ECWMF/GFS have shown much better continuity with this system, and are in good agreement with their respective ensemble means. Based on this, the preference for the West has been changed to a blend of these two solutions. Model trends at www.wpc.ncep.noaa.gov/html/model2.shtml 500 mb forecasts at www.wpc.ncep.noaa.gov/h5pref/h5pref.shtml Hayes