Model Diagnostic Discussion NWS Weather Prediction Center College Park MD 239 AM EDT Sun Oct 06 2019 Valid Oct 06/0000 UTC thru Oct 09/1200 UTC ...See NOUS42 KWNO (ADMNFD) for the status of the upper air ingest... 00Z Model Evaluation with Preferences and Forecast Confidence ~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~ ...Overall Pattern Across the CONUS... ~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~ Preference: General model blend...Western 2/3rds of CONUS 12z ECMWF/UKMET and 00z NAM (some GEFS...Eastern CONUS Confidence: Slightly above average Average in Eastern CONUS after 09.00z 19z update: The 00z ECMWF trended a bit weaker and therefore a bit faster lifting the lingering shortwave energy out of the Upper TN/OH Valley, leaving the focus for surface cyclogenesis further east like the prior run and initial preference and close to the 00z NAM. The 00z UKMET, shifted ever so much closer to the NAM/ECMWF while the CMC trended stronger and very closely packed to the GFS. The 00z GEFS continues to depict a split in the solutions, half toward the operational GFS and a few clustered toward the NAM/ECMWF/UKMET... still suggesting the NAM/ECMWF/UKMET blend is still favored over this slower, more amplified E TN/OH Valley solution with stronger warm conveyor belt pumping moisture back across the Mid-Atlantic. This will keep with initial preference and confidence still at average. Elsewhere, confidence remains slightly above average in a general model blend. ---Prior Discussion--- The northern stream flow pattern will support a strong upper jet progressing the lingering positive tilt trough energy across the eastern third of the CONUS, with eventually strong cold pool dropping south out of Arctic Canada to enhance trough development in the Northwest/Northern Rockies by Tuesday and digging into the Snake River/N Great Basin by the end of the short-range forecast period. Additionally, a tropical wave will approach the Bahamas and amplify in front of the advancing eastern trough, with large model variation in strength/placement/evolution of a Gulf Stream surface wave and any remaining shortwave energy at the tail end of the northern stream trof through the Cumberland Plateau into the Central Appalachians. As for the lead shortwave, the trend as been a bit faster overall in the ensemble suite/guidance, with the 12z ECMWF and bulk of members along with the UKMET and 00z NAM progressing the frontal zone through the upper TN/OH valleys and across the Mid-Atlantic/Northeast. Interestingly, the GFS has trended away from this evolution, supporting a slower, more amplified wave in the Cumberland Plateau by Tuesday. This is mostly due to a stronger, faster northern stream jet initially, typical of a negative bias. This in turn, severs the connection to the tail end of the trof, which minus the very slow CMC is fairly alone, even within the 18z GEFS member solutions. Additionally, this stronger cyclone and flatter surface front along the Mid-Atlantic/south of New England helps with the tropical wave lifting north and draws a stronger easterly flow jet north of the boundary and stronger warm conveyor, to advect more moisture/instability across the boundary and appears less favorable even in the CMC which is slow. As such will favor a 12z ECMWF/UKMET and 00z NAM blend for the eastern US particularly after 09.00z. Given inconsistency in the guidance trends away from each other and the importance of small timing/intensity differences, confidence is average in the blend, particularly for day 3 when the tropically originating wave lifts up the east coast. In the west, the guidance is much more agreeable, with the timing/orientation and strength of the digging trof. The 00z NAM may be a bit off, given typical day 3 negative bias of being a bit stronger; allowing a stronger northeast shortwave out of the Northern US Rockies into SE Canadian Prairies late Tuesday, relative to the other guidance including ECENS and GEFS ensemble suites. Still, this is fairly small differences that its inclusion to a blend is fair, but perhaps at lower weighting. Though, the 00z NAM and GFS may be a bit more favorable about the subtle subtropical stream shortwave that slides into the Southern Plains in advance of the trof. Both are a bit more amplified and support a bit northward shift in light to moderate QPF development. Confidence is average in this general model blend. Model trends at www.wpc.noaa.gov/html/model2.html 500 mb forecasts at www.wpc.noaa.gov/h5pref/h5pref.shtml Gallina