Subj : HVYRAIN: Excessive Rainfall Discussion To : wx-storm@lists.illinois.edu From : COD Weather Processor Date : Wed May 03 2023 20:23:15 FOUS30 KWBC 032023 QPFERD Excessive Rainfall Discussion NWS Weather Prediction Center College Park MD 419 PM EDT Wed May 03 2023 Day 1 Valid 16Z Wed May 03 2023 - 12Z Thu May 04 2023 The probability of rainfall exceeding flash flood guidance is less than 5 percent. Campbell Day 2 Valid 12Z Thu May 04 2023 - 12Z Fri May 05 2023 ....THERE IS A MARGINAL RISK OF EXCESSIVE RAINFALL ACROSS THE INTERMOUNTAIN WEST AND FROM THE LOWER MISSOURI VALLEY AND EASTERN OKLAHOMA TO PARTS OF THE MID-SOUTH... ....Central and Northern Intermountain West... 21Z update... The latest model guidance continues to support previous reasoning; therefore no changes were made at this time. Campbell Stubborn, slow-moving mid-upper low/trough will take on more of a negative tilt Thu-Thu night as shortwave energy pivots northward through the Southwest and Central Great Basin. The uptick in upper level forcing with the increased upper difluence/divergence/DPVA, coinciding with areas of decent instability for this time of year prior to monsoon season (MUCAPEs of 500-1500 J/Kg, owing in large part to steepening H7-H5 lapse rates of 7-8+ C/KM), will allow for more numerous, pulse-type convective clusters with the potential of isolated 0.50-1.00"/hr rainfall rates per. This as PWs climb between 0.50-1.00" per the guidance, highest (>0.75") across eastern WA-OR into northern ID, which would be 2-2.5 standard deviations above normal for early May. By themselves, the dynamical and thermodynamical parameters progged by the models would result in a minimal excessive rainfall threat (i.e. below the 5% threshold for a Marginal); however, when combined with the snowmelt in some locales and burn scar areas in others, do anticipate a more enhanced risk for localized runoff issues. As a result, the Marginal Risk area inherited from yesterday's experimental Day 4 ERO was expanded northward to the Canadian border with WA-ID. ....Central/Southern Plains and Mid-Mississippi Valley... 21Z update... The guidance has trended higher with the QPF across Texas where convection is expected to fire up and track eastward ahead of the dryline. Most of the hi-res guidance are showing storms popping up over central Texas/western Oklahoma and tracking eastward through the period, with hourly rain rates pulsing from 0.75 to nearly 3 inches/hr. Portions of this region have had recent rains resulting in being 200 to 600% of normal. These rainfall intensity and preconditioned soils could quickly lead to areas of flash flooding, especially if they occur near the Hill Country and flood prone metros. The Marginal Risk was expanded from Oklahoma to cover much of central/eastern Texas and southwest Arkansas. Further north, there is still a fair amount of latitudinal spread but consensus keeps the highest QPF along the Kansas/Missouri Border, south of the Kansas City metro. Campbell Downstream of the aforementioned upper trough, flattening mid/upper ridge will remain across the central CONUS. Strong upper level confluence is expected to generate a 100-130 kt upper level jet streak across the Midwest to Lower OH Valley Thu-Thu night. The resultant uptick in low-level frontogenesis is noted from the guidance, while SW/SSW 850 mb flow increases to 40-50 kts and robust MUCAPEs between 1500-3000 J/Kg by Thursday evening and overnight across the outlook area. The dynamical and thermodynamical environment will foster the development and upscale growth of organized convection Thursday night, potentially leading to an MCS with an enhanced risk of cell training as the low-level jet (LLJ) ramps up and 850-300 mb thicknesses become more divergent downstream. Deep-layer moisture parameters are not overly impressive/anomalous at this point however (maximum PW values of 1.5-1.7" within the outlook area). Meanwhile, there continues to be a multi-modal distribution with the axes of heavier rainfall, owing to the lack of overlap with the strongest dynamical forcing (northern portion of the outlook area) and strongest deep-layer instability and low-level southwesterly inflow/moisture flux (southern portion). As a result of the continued model spread with the QPF, and the fact that the models currently depict more forward (downwind) propagation/Corfidi Vectors than otherwise, will maintain the Marginal Risk that was inherited from yesterday's Day 3 ERO. Hurley Day 3 The Day 3 outlook will be updated by 2030Z. Day 1 threat area: https://urldefense.com/v3/__https://www.wpc.ncep.noaa.go= v/qpf/94epoints.txt__;!!DZ3fjg!8xDJ73SPE2zRwY5DwHeZTagh_odhgMP5m4tKsEe1NkdH= zId58Z54iUiJ2QUPqsZp5B7zgjjtk9QiUKw50bdIB4p812k$=20 Day 2 threat area: https://urldefense.com/v3/__https://www.wpc.ncep.noaa.go= v/qpf/98epoints.txt__;!!DZ3fjg!8xDJ73SPE2zRwY5DwHeZTagh_odhgMP5m4tKsEe1NkdH= zId58Z54iUiJ2QUPqsZp5B7zgjjtk9QiUKw50bdIIMJXiGo$=20 Day 3 threat area: https://urldefense.com/v3/__https://www.wpc.ncep.noaa.go= v/qpf/99epoints.txt__;!!DZ3fjg!8xDJ73SPE2zRwY5DwHeZTagh_odhgMP5m4tKsEe1NkdH= zId58Z54iUiJ2QUPqsZp5B7zgjjtk9QiUKw50bdIWxcDwcc$=20 $$ =3D =3D =3D To unsubscribe from WX-STORM and you already have a login, go to https://lists.illinois.edu and use the "Unsubscribe" link. Otherwise email Chris Novy at cnovy@cox.net and ask to be removed from WX-STORM. --- SBBSecho 3.14-Linux * Origin: capitolcityonline.net * Telnet/SSH:2022/HTTP (1:2320/105) .