Model Diagnostic Discussion NWS Weather Prediction Center College Park MD 1239 PM EDT Mon Jun 24 2019 Valid Jun 24/1200 UTC thru Jun 28/0000 UTC ...See NOUS42 KWNO (ADMNFD) for the status of the upper air ingest... 12Z Model Evaluation...with Prelim Confidence and Preferences ~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~ ...Overall Pattern Across the CONUS... ~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~ Preference: General model blend Confidence: Slightly Above Average Models are in excellent agreement showing a trough lifting northeast from the Plains into eastern Canada by tomorrow afternoon. After that, there is very good agreement with amplification of a trough along the West Coast and a ridge over much of the CONUS to the east of the Rockies. Isoheights at a variety of pressure levels are well clustered, and the deterministic models are generally contained within the envelope of ensemble spread. The 00Z UKMET has the West Coast trough centered on the western edge of available models, but is otherwise similar to other models on the overall pattern. Nevertheless, there is inherent uncertainty with the QPF related to convective processes. This is evident in some run-to-run changes of the location of precipitation maxima, likely due to a slightly different evolution of convection in the same overall synoptic environment. This will become even more challenging as the ridge builds by mid-week and mid-upper level flow across the central and eastern U.S. weakens. Given the broad agreement on the synoptic pattern and major waves, the preference is for a general model blend. This will help account for some of the convective uncertainty. Forecast confidence is listed as slightly above average, but is essentially above average on the synoptic pattern and average for the mid-summer on mesoscale details and precise placement of QPF maxima. Model trends at www.wpc.noaa.gov/html/model2.html 500 mb forecasts at www.wpc.noaa.gov/h5pref/h5pref.shtml Lamers