Quantitative Precipitation Forecast Discussion NWS Weather Prediction Center College Park MD 318 AM EDT Wed Mar 21 2018 Prelim Day 1 QPF Discussion Valid Mar 21/1200 UTC thru Mar 22/1200 UTC Reference AWIPS Graphics under...Precip Accum - 24hr Day 1 ...Eastern U.S... On the synoptic scale it is becoming less common in the modern age to reach Day 1 and have trouble finding a QPF consensus. Yet this early spring Nor'easter remains an enigma. The forecast leading into this storm has shown remarkable sensitivity to small scale interaction among shortwaves embedded in the unusually energetic yet low of amplitude - flow over the southern U.S. The overall trend had been toward more of a major snowstorm with 1 to 2 inch liquid equivalent amounts from Baltimore northeastward. The trends from one forecast cycle to the next, however, have been so inconsistent whether considering one model or all of them, that we are largely left with a manual forecast effort, relying on conceptual models more than any specific piece of guidance (especially where QPF is concerned). The model mass fields seem to have finally settled down, with a nicely depicted track of a low deepening off the Mid-Atlantic coast, down to about 990 mb as it then slowly lifts northeast. The 850-700 mb front / inverted trough structure north of the low track would appear to have set up as was anticipated from the MD/PA border region up through NYC / Long Island and beyond. This should become a focus for heavier, banded precipitation, creating a swath of maximum QPF in the vicinity of this region. Farther south the easterly onshore flow and deep layer ascent will be less long lived, but still substantial in the early hours of the day. Watching animations of the model fields, the focus and pivot in the 850-700 mb layer should occur near NYC / Long Island, acting to maximize snow and liquid equivalent amounts there. Most guidance actually does agree to this concept, all but the 00z ECMWF whose QPF axis was inexplicably offshore despite little change to the mass field solution. Working initially with the trends in NCEP guidance, and supported a fair amount by the UKMET, WPC favored a QPF blend of the HREF mean and a version of our in-house ensemble which gives significant weight to the hi-res model suite. This yielded a similar precip pattern, but with heavier amounts, up to a half inch heavier liquid amount over southern NY and southern New England. This may end up being a bit heavy handed, especially as the low is not bombing out. Deep layer height falls are somewhat delayed in coming into sync with the 850-700 mb frontal zone, and perhaps this will hamper precipitation intensity. We may tone it down slightly for the final issuance, but do feel confident in placement just based on synoptic reasoning...with a forecast that still supports heavy snowfall along the east coast - see WPC Heavy Snow Discussion. ...Western U.S... On Day 1 into Day 2, the closed low well offshore of California phases with and is kicked by the northern stream flow, creating a full latitude trough with a pronounced southern stream component at its base. The pattern as a whole makes some progress into the Western U.S. on Wednesday, bringing widespread rain/snow as far inland as the northern Rockies down to the lower Great Basin / lower Colorado River basin. By far, however, this event will be known as a California storm, with heavy Sierra snows and heavy rainfall along the coast. The inherited WPC forecast was ratcheted up about as high was was necessary, especially as some of the heavy coastal rain into southern California will spread over into the Day 2 period. Therefore, we started with the previous forecast, and looked to just make minor adjustments to keep up with trends. For one, we trimmed back on the coverage of quarter inch amounts in the rain shadow areas of eastern WA/OR, based on hi-res model consensus, NDFD, and the GEFS Re-forecast data based on analog events. Secondly, there has been a continued trend for the heaviest Day 1 rainfall (through 12z Thursday) to back up northward through San Luis Obispo County and Monterey County. There will certainly be heavy rainfall reaching down into Ventura County and possibly the L.A. basin, but overall we nudged the Day 1 centroid farther north up the coast. This will mean that the risk of flash flooding and debris flows associated with some of the largest fire burn scars will certainly extend into the Day 2 period as well, as the atmospheric river then makes more eastward progress. QPF was derived from a high percentage previous WPC, combined with influence from the 00z NAM CONUS Nest and our in-house ensemble. The WRF-ARW did not follow the trend, and was more aggressive with heavy rain extending into Los Angeles suburbs. This is its tendency nationwide (south and east of consensus), but it is sometimes right. The Excessive Rainfall Outlook will remain generous with its coverage given this possibility. Burke