Subj : HVYRAIN: Excessive Rainfall Discussion To : wx-storm@lists.illinois.edu From : COD Weather Processor Date : Wed May 24 2023 07:53:44 FOUS30 KWBC 240753 QPFERD Excessive Rainfall Discussion NWS Weather Prediction Center College Park MD 353 AM EDT Wed May 24 2023 Day 1 Valid 12Z Wed May 24 2023 - 12Z Thu May 25 2023 ....THERE IS A MARGINAL RISK OF EXCESSIVE RAINFALL ACROSS PORTIONS OF GREAT BASIN INTO THE NORTHERN ROCKIES AND HIGH PLAINS, CENTRAL FRONT RANGES AND HIGH PLAINS INTO THE SOUTHERN PLAINS, AND THE FLORIDA PENINSULA... ....Great Basin into the Northern Rockies and High Plains... Longwave upper trough just east of West Coast will migrate slowly into the intermountain West through the short range period (days 1-3). This will maintain an elongated, SSW-NNE area of broad-scale upper difluence and divergence across the western Great Basin into the northern Rockies and High Plains. At the same time, thermodynamical profiles (deep-layer moisture and instability) will remain above seasonal norms for late May, as PWs average 2-2.5 standard deviations above normal per the 00Z GEFS while and MUCAPEs are expected to peak between 1000-1500 J/Kg during the peak heating hours this afternoon and early evening. Cell motions will be rather progressive (forward propagating) given the low-mid layer shear profiles; however, the stagnant mid-upper level pattern will allow for some regeneration of cells upstream, thus favoring some training or multiple bouts of convection over the same areas this afternoon and evening. The CAMs show hourly rainfall rates peaking between 0.50-1.00+" underneath the strongest cells (isolated), which given the current FFG, could certainly lead to localized runoff issues. ....Central Rockies and High Plains into the Southern Plains... The upper flow across these areas will become increasingly difluent as the upper ridge axis pushes into the eastern (lower) Plains. Meanwhile, increasing low-level south to southeast flow (ageostrophic low-level response) ahead of the approaching trough will bring an elongated ribbon of increased deep-layer and more focused low-level moisture flux north-northwestward into the central High Plains and front ranges. As with the other outlook area upstream, the predominant along-stream, exit region upper level forcing east of the amplified trough will inhibit low-level frontogenesis, and as such the forcing is more diffuse and not focused over any particular area. Granted, convection moving east off the terrain may tend to exhibit some training/backbuilding as they encounter low level southeasterly inflow, with anomalous PWs and sufficient CAPE for heavy rainfall rates. However, as was noted in the previous discussion (yesterday's Day 2 ERD), while the ingredients and the CSU first guess fields support lower-end Slight Risk probabilities over the High Plains, the 00Z HREF QPF probabilities are not too impressive, and the model QPFs continue to show quite a bit of spread with the max amounts (i.e. more in line with a typical Marginal risk). Therefore given the uncertainty, opted to maintain continuity with the Marginal Risk with the anticipation of more isolated flash flooding than otherwise. ....Florida... Persistent mid-upper level trough coinciding with typical favorable deep-layer moisture and instability will again lead to more numerous thunderstorms than what is typical for late May across the FL peninsula during the afternoon and early evening hours. Sea/Gulf breeze interaction will aid to the development, while 0-6km bulk shear values of 20-30 kts should again favor at least some organization, i.e. more clustered convection that can persist a little bit longer than the more typical pulse type. At the same time however, the CAMs again do not show much overlap with the convective bulls-eyes, indicative of more broad (less focused) dynamical support. Given the CAM deterministic and probabilistic output, along with the CSU first guess fields, the Marginal Risk inherited from yesterday's Day 2 ERO still looks on track.=20 Hurley Day 2 Valid 12Z Thu May 25 2023 - 12Z Fri May 26 2023 ....THERE IS A MARGINAL RISK OF EXCESSIVE RAINFALL ACROSS A LARGE PORTION OF THE PLAINS, NORTHERN ROCKIES, AND INTERMOUNTAIN WEST... ....Great Basin-Northern Rockies-High Plains... Upper level pattern shifts very little by Day 2 (Thu-Thu night), though again compared to Day 1 there is more support for expanding the Marginal Risk area westward toward the upper low to include more of the intermountain region (western NV and northeast CA). Deterministic and probabilistic QPF from the models again support a localized or isolated flash flood threat possible anywhere within the broad risk area. As was noted in yesterday's Day 3 ERD, once area to watch would be across central-eastern MT, where the presence of a surface frontal boundary (weak low-level FGEN) could focus a more organized area of heavy rain (upscale convective growth). As of now however, the guidance spread in terms of QPF (convective bulls-eyes) remains too high (forecast confidence too low) to include an embedded Slight Risk area.=20 Hurley Day 3 The Day 3 outlook will be updated by 0830Z. Day 1 threat area: https://urldefense.com/v3/__https://www.wpc.ncep.noaa.go= v/qpf/94epoints.txt__;!!DZ3fjg!8CKE9xhC76w8BJa8JauzGddH1oQkkW1f-pTseeZJ9V16= JMGoic5Tp_pZVhH-YTTbomoKCEDdGn63GVLe9Wz4HtA6MIs$=20 Day 2 threat area: https://urldefense.com/v3/__https://www.wpc.ncep.noaa.go= v/qpf/98epoints.txt__;!!DZ3fjg!8CKE9xhC76w8BJa8JauzGddH1oQkkW1f-pTseeZJ9V16= JMGoic5Tp_pZVhH-YTTbomoKCEDdGn63GVLe9Wz46j2lgGw$=20 Day 3 threat area: https://urldefense.com/v3/__https://www.wpc.ncep.noaa.go= v/qpf/99epoints.txt__;!!DZ3fjg!8CKE9xhC76w8BJa8JauzGddH1oQkkW1f-pTseeZJ9V16= JMGoic5Tp_pZVhH-YTTbomoKCEDdGn63GVLe9Wz4Tvyuoy0$=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) .