Model Diagnostic Discussion NWS Weather Prediction Center College Park MD 1149 PM EST Sat Jan 05 2019 Valid Jan 06/0000 UTC thru Jan 09/1200 UTC ...See NOUS42 KWNO (ADMNFD) for the status of the upper air ingest... 00Z Model Evaluation...with Preferences and Confidence ~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~ ...Overall Pattern Across the CONUS... Preference: General model blend Confidence: Average In general, the model guidance is in good agreement with the large scale pattern across the CONUS through the forecast period. A quick-moving shortwave trough will skirt the Northeast US Sunday into Sunday night while a series of troughs push across the western US into the central Plains which is expected to phase and become a deeper longwave trough over the eastern US by Wednesday. At the surface, a low will develop across the central Plains then lift into the Great Lakes then will redevelop/deepen off the New England coast Tuesday night into Wednesday. The biggest differences noted in the guidance lies with the 00z NAM and the strength of the trough developing across the Great Lakes into the Northeast Tuesday night into Wednesday. The NAM is considerably sharper/stronger compared to the global models and also lies on the faster spread compared to the GFS/ECMWF. Its surface depiction across southern Canada is on the northern end of the model spread. In the previous cycle, the GFS was a bit deeper/stronger, but with the 00z GFS those differences seem to have been resolved, or at least not as prominent. Right at the end of the forecast period /09.12z/, a surface low developing off the New England introduces quite a bit of forecast uncertainty and possible precipitation impacts. How quickly the trough phases and becomes negatively tilted will dictate where the low develops off the coast and how strong before it pulls away. There are signals of an inverted trough hanging back to produce precipitation. The NAM is further north compared to the ECMWF/GFS, which are actually in decent agreement. The CMC is further east while the UKMET is an outlier to the west. Here, a blend of the GFS/NAM/ECMWF with more weight to the consistent ECMWF and its ensemble mean is preferred. Elsewhere, the models all agree in having a rather formidable large scale ridge over the Western U.S. by the end of the period as a deep closed low and associated longwave trough evolves offshore of the West Coast. All of the models show a rather strong surface low center as well with these strong height falls, but the NAM is south of the global model consensus with the positioning of its low center surface and aloft. The global models are well clustered with the depth and timing of this energy and have excellent ensemble support from the GEFS and ECENS suites. Based on the comparisons above, a general blend should suffice for the larger scale mass fields, noting some of the model differences across New England late on day 3. Model trends at www.wpc.ncep.noaa.gov/html/model2.shtml 500 mb forecasts at www.wpc.ncep.noaa.gov/h5pref/h5pref.shtml Taylor