Model Diagnostic Discussion NWS Weather Prediction Center College Park MD 1140 AM EST Sat Nov 10 2018 Valid Nov 10/1200 UTC thru Nov 14/0000 UTC ...See NOUS42 KWNO (ADMNFD) for the status of the upper air ingest... 12Z NAM/GFS Evaluation...with Preliminary Preferences and Confidence ~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~ ...Overall Pattern Across the CONUS... ~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~ Preference: 12Z GFS/00Z ECMWF/00Z UKMET blend Confidence: Average Broad, longwave troughing in place over the lower 48 early this morning will sharpen with the mean mid-upper level trough axis shifting eastward to the Mississippi Valley through Tuesday. Embedded within this flow is a departing mid-level closed low over southern Quebec and multiple shortwaves over the western U.S. and western Canada. One of these shortwaves will cross the Four Corners region on Sunday as additional shortwave energy drops south from Montana and Wyoming. Interaction between these two features and a northern stream trough over the upper Mississippi Valley will translate into a highly amplified flow with a surface cyclone organizing over the Gulf Coast on Monday...tracking to the Northeast for Tuesday. Upper riding along the West Coast will be disrupted as the base of upper troughing, located in the Gulf of Alaska, moves into southern British Columbia. Model differences begin appearing around F036 hours (00Z/12) with the 00Z CMC a bit faster with the shortwave trough axis crossing the Four Corners region which continues into early next week. The 12Z NAM ending up a bit slower with the southern portion of the longwave trough axis over the southern Plains and is also on the northern end of the deterministic /ensemble guidance with a surface low in the western Gulf of Mexico Monday morning. Outside of the 09Z SREF mean, the ensembles (GEFS/ECMWF/CMC) show decent agreement with only a small minority of ECMWF ensembles supporting the slower 12Z NAM. There remains some timing/amplitude differences though in the ensembles with the 00Z CMC members fastest followed by the 00Z GEFS members and with the 00Z ECMWF members slowest. The preference is to stay nearest to the best clustering of members which is supportive of the past 4 cycles of trends. This is closest to a blend of the 00Z ECMWF, 12Z GFS and 00Z UKMET. Model trends at www.wpc.ncep.noaa.gov/html/model2.shtml 500 mb forecasts at www.wpc.ncep.noaa.gov/h5pref/h5pref.shtml Otto