Quantitative Precipitation Forecast Discussion NWS Weather Prediction Center College Park MD 301 AM EDT Thu May 31 2018 Prelim Day 1 QPF Discussion Valid May 31/1200 UTC thru Jun 01/1200 UTC Reference AWIPS Graphics under...Precip Accum - 24hr ...Lower-Mid Mississippi Valley into the lower Ohio and Tennessee valleys... Ongoing MCS over the southern Plains early this morning (and ensuing MCV) will certainly have implications on the new day 1 QPF downstream into the lower-mid MS Valley-lower OH Valley, and TN Valley. While still showing a a good heavy rainfall footprint, the spread among the 00Z high-res CAM guidance (notably N-S) was less than desirable for a day 1 period. The WPC QPF initialized with continuity and a blend with the NBM and HREF mean, however evolved toward a NSSL-WRF/WRF-ARW2 combination late Thu and Thu night. Like the idea from these models of 2 main axes of higher totals, the first one farther south (across much of Arkansas) where the instability pool in the warm sector should be more than sufficient (while mid level capping not an inhibition) in supporting a developing QLCS south of the MCV. The other QPF max was noted across the mid MS Valley, including se MO, southern IL-IN, and western KY given the bolstered 850-700 mb moisture flux/theta-e transport out ahead of the MCV track. ...Lower Great Lakes / Upper Ohio valley / Central Appalachians / Mid Atlantic... As the trough over the upper Midwest translates eastward this period, and the upper ridge axis pushes off the Atlantic coast, a northwest-southeast oriented boundary and the leading edge of a very moist airmass extending from the Mid-Atlantic from the Great Lakes is expected to move north this period. Guidance shows deep moisture surging north along the central Appalachians and Mid-Atlantic as the low level flow backs ahead of the approaching trough. This moisture along with afternoon heating and the larger scale forcing afforded by the approaching trough (broad-scale upper difluence) is expected to support and increasing threat for moderate to locally heavy amounts focused along the higher terrain and ahead of a cold front pushing across the lower Great Lakes. WPC QPF gave significant weighting to the HREF Mean through most of the period. ...Northern Intermountain West / Northern Rockies and High Plains... As an upper level trough continues to amplify across the Northwest, a developing upper jet streak across southern Alberta-Manitoba along with ample (anomalous) moisture along and east of the low-level front will support mid-heavy rainfall along the eastern slopes of the northern Rockies and spreading into the northern Plains. WPC QPF reflects a consensus of the hi-res models here as well. The shear profiles support more forward (downwind) propagation of convection than otherwise; however, given the antecedent wet soils (relatively low FFG across much of the region), areas that receive the heaviest rainfall may experience isolated runoff issues in the short term. Hurley