Model Diagnostic Discussion NWS Weather Prediction Center College Park MD 1157 AM EDT Tue Jun 25 2019 Valid Jun 25/1200 UTC thru Jun 29/0000 UTC ...See NOUS42 KWNO (ADMNFD) for the status of the upper air ingest... 12Z Model Evaluation...with Final Confidence and Preferences ~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~ ...Overall Pattern Across the CONUS... ~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~ Preference: GFS/ECMWF blend across northwest/northern tier General model blend elsewhere Confidence: Average Large scale flow across the CONUS is dominated by mainly zonal flow with a large closed low anchoring along the NW Coast and another closed/occluded low going off to die across James Bay/S Hudson Bay...pressing the cold front off-shore of New England today (with good model agreement). The western closed low will shift south and toward the OR coast slowly filling toward Thursday with little model difference until very late stage breakdown shearing across into SW Canada by the end of the forecast period. This is always difficult to precisely forecast given the smaller scale internal waves and their precise magnitude. The ECMWF/GFS and their ensemble members favor a slower shearing toward the northeast into Canada languishing across the western Columbia River Valley. The 12z NAM/CMC favor more toward the northeast. Upstream interaction/flow out of the Gulf of AK should support the GFS/ECMWF solution (and their ensembles) over the more transitional NAM/CMC. The other significant feature was a subtle Subtropical/southwesterly flow shortwave that emerges from the Central Rockies into Thursday. Here convective development enhances the wave after topping the ridge into the Upper Midwest/Great Lakes into Fri. The 12z NAM and 00 UKMET are very aggressive with vortex strengthening and convective response, feeding back onto the wave. This is not supported give proximity to the dying but still important closed low over N Ontario...that should favor more sheared/zonal flow undercutting it. As such will favor a GFS/ECMWF/CMC solution for this region as well. Elsewhere, the subtropical ridge will dominate and the start of a "Ring-of-Fire" convective pattern will start to emerge. However, there is good model agreement in a break in the ridge around mid-South/central Gulf where some of the convective complex energy will support a sheared MCV/vorticity center that will string out and eventually start to retrograde by the end of the forecast period. The ECMWF is a bit slower and therefore west with the weakness relative to the stronger GFS/NAM/UKMET but a general model blend should suffice as the placement is not dramatically different for such a small scale/convectively influenced feature. Overall confidence is just average given the importance/influence of small scale convectively induced features though large scale features/flow pattern is slightly to above average in agreement. Model trends at www.wpc.noaa.gov/html/model2.html 500 mb forecasts at www.wpc.noaa.gov/h5pref/h5pref.shtml Gallina