Model Diagnostic Discussion NWS Weather Prediction Center College Park MD 1257 AM EDT Mon Aug 19 2019 Valid Aug 19/0000 UTC thru Aug 22/1200 UTC ...See NOUS42 KWNO (ADMNFD) for the status of the upper air ingest... 00Z Model Evaluation...Including Preferences and Confidence ~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~ ...Overall Pattern Across the CONUS... ~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~ Preference: Blend of the 18Z GEFS mean/12Z ECENS mean Confidence: Average The main component of mid-upper level ridging in place at the start of the period near the Rio Grande will translate westward to just off of the Southwest coast by Wednesday afternoon. A small portion of the ridge will remain over the south-central U.S. Meanwhile, across the northern tier of the U.S., the flow is quasi-amplified with a closed low over south-central Canada which will track east and elongate east-west before re-amplifying southward toward the Great Lakes late Wednesday. Back to the west, an anomalous upper trough, forecast to be offshore of the Pacific Northwest on Tuesday, will weaken slightly as it moves into British Columbia and the Pacific Northwest Wednesday. There are some minor timing differences with the upper trough in the vicinity of the Great Lakes, u there are more concerns regarding the depth of it. Firstly, the 00Z NAM appears to be a tad too strong with some of the vort energy advancing east underneath the trough as it crosses the OH Valley, Mid-Atlantic and Northeast Tuesday and Wednesday. Regarding the larger scale trough, the 00Z GFS becomes the strongest solution, with the 12Z CMC the weakest. This translates accordingly to the same intensity spread with the evolving surface low impacting southeast Canada. Meanwhile, the 12Z ECMWF is seen as placing it surface and mid-level low centers on the south side of the model consensus and south of the 12Z ECENS mean. The 18Z GEFS mean is rather close to the 12Z ECENS mean with this evolution, and suggests the deterministic GFS is a strong outlier. Farther south across the eastern Gulf Coast and the Southeast, the 12Z UKMET and to some extent the 12Z CMC appear to be strong outlier with the slowly meandering low/mid-level low center near the FL Panhandle and southern GA. Across the Pacific Northwest, the 00Z NAM and 12Z CMC are a bit slower than the multiple model consensus, with the 00Z GFS and 12Z ECMWF well supported by their respective ensemble means regarding the depth and timing of this system. Based on the latest model spread, ensemble clustering and trends, a blend of the ensemble means will be preferred across the CONUS via the 18Z GEFS and 12Z ECENS means. Model trends at www.wpc.noaa.gov/html/model2.html 500 mb forecasts at www.wpc.noaa.gov/h5pref/h5pref.shtml Orrison