Model Diagnostic Discussion NWS Weather Prediction Center College Park MD 152 PM EST Wed Dec 19 2018 Valid Dec 19/1200 UTC thru Dec 23/0000 UTC ...See NOUS42 KWNO (ADMNFD) for the status of the upper air ingest... 12Z Model Evaluation...with Preferences and Confidence ~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~ ...Overall Pattern Across the CONUS... ~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~ Preference: 12Z ECMWF, 12Z GFS, greater weight to ECMWF Confidence: Slightly below average ---18Z UPDATE--- No change to the preliminary preference. A blend of the ECMWF and GFS still seems to offer a consensus forecast supported by ensemble members. ---PREVIOUS DISCUSSION--- The largest area of precipitation over the next few days will be generated by a broad and strong cyclone that will develop in the Southeast and then move inland up the East Coast. Models generally agree on the large-scale evolution, but detail variations make a substantial difference with QPF intensity and placement, as well as precipitation type on the cold side of the cyclone. Model preference was weighted most strongly toward the 00Z ECMWF, which has shown very good consistency with previous model cycles and depiction of weather impacts. The 12Z GFS has generally trended in the direction of the ECMWF, continuing a multi-run trend, and these two models should form the basis of a reasonable blend that is supported by a considerable number of ensemble members. The CMC and NAM were not preferred as much, given some slight differences that do make an impact. The 00Z CMC ejects the negatively tilted mid-level wave up the East Coast faster than the other models leading to changes in the trajectory of the surface low and placement of QPF. Given the anomalously strong nature of the digging wave, and strong cyclogenesis expected, the preference is toward the model consensus and a slower ejection of the wave given that more closely matches the scenario. The 12Z NAM, meanwhile, develops the surface low much further southeast relative to the other models, kicks it northeast into the Carolinas faster, and eventually cycles it much further northwest toward Lake Huron than the other models. The preference is to again lean closer to model consensus, with an occluding surface low initially forming closer to the strongest height falls (northwest of the NAM surface low position). For the East Coast cyclone, the 00Z UKMET also offers a reasonable forecast that is generally similar to the ECMWF and GFS. However, over the Rockies and Plains, the UKMET is strongest with secondary troughs relative to other models. These troughs will be pushing into an amplified ridge (upstream of the large East Coast trough), and thus with expected destructive interference of these waves, the expectation would be for a flatter flow pattern overall. Therefore, the preference is still to lean closer to the ECMWF and GFS overall. On the West Coast, the next wave approaching the Pacific Northwest will generally have QPF impacts in the medium range, just after the scope of this discussion. However, The ECMWF seems more reasonable with the initial effects of the associated surface low. The GFS is much further north, while the GEFS Mean and ECMWF Ensemble Mean are south, closer to the deterministic ECMWF. Model trends at www.wpc.ncep.noaa.gov/html/model2.shtml 500 mb forecasts at www.wpc.ncep.noaa.gov/h5pref/h5pref.shtml Lamers