Model Diagnostic Discussion NWS Weather Prediction Center College Park MD 1028 AM EST Tue Dec 18 2018 Valid Dec 18/1200 UTC thru Dec 22/0000 UTC ...See NOUS42 KWNO (ADMNFD) for the status of the upper air ingest... 12Z Model Evaluation...with Preferences and Confidence ~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~ ...Central/Eastern US... ~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~ Preference: 00z ECMWF, 06z GFS, 12z NAM blend Confidence: Average The upper level pattern will become increasingly more amplified over the central/eastern US through the forecast period. A deepening trough over the central US will take on a negative tilt by Thursday night, potentially closing off a low near the southern Gulf Coast, then become even more negatively tilted as it lifts through the mid-Atlantic region. In general, the deterministic and ensemble guidance show good agreement spatially and temporally. The 06z GFS solution remains the strongest, closing off at 500 mb earliest (across the Arklatex region) while the rest of the models stay open. The surface fields show more variability, particularly with the track and speed of a low that will move up the east coast. Here, the 00z CMC is too fast and too deep. The UKMET is a bit to the west of the consensus, while the NAM is also fast, but generally to the right. The 00z ECMWF and 06z GFS are not too different in both spatial and magnitude terms, so for this cycle, a blend of the GFS and ECWMF would suffice. ...Pacific Northwest... ~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~ Preference: 00z ECMWF, 06z GEFS blend Confidence: Below Average A pair of shortwave trough will push onshore across the Pacific Northwest through the forecast period. The first will arrive later tonight into Wednesday morning. Following that feature, some ridging will develop ahead of a positively tilted trough that will push into the region Thursday night into Friday. Aloft, the mass fields are in reasonable agreement across the deterministic and ensemble guidance with respect to speed and magnitude. The biggest differences are at the surface, which advertise a deepening low moving across either extreme northern Washington state or southern British Columbia. The 06z GFS, 12z NAM are considerably faster, bringing the low onshore as early as 20.12z while the non-NCEP solutions are actually clustered together very well but almost 12 hours slower. The GFS seems to be too fast, where the operational solution is faster than the GEFS mean. So for this cycle, prefer to go with a compromise blend at this point, with the 00z ECMWF and 06z GEFS mean. The CMC is the slowest of the group and like the previous discussion mentioned, it is likely too slow and was not considered for this cycle. Model trends at www.wpc.ncep.noaa.gov/html/model2.shtml 500 mb forecasts at www.wpc.ncep.noaa.gov/h5pref/h5pref.shtml Taylor