Subj : HVYRAIN: Excessive Rainfall Discussion To : wx-storm@lists.illinois.edu From : COD Weather Processor Date : Tue Jul 11 2023 15:58:52 FOUS30 KWBC 111558 QPFERD Excessive Rainfall Discussion NWS Weather Prediction Center College Park MD 1158 AM EDT Tue Jul 11 2023 Day 1 Valid 12Z Tue Jul 11 2023 - 12Z Wed Jul 12 2023 ....THERE IS A SLIGHT RISK OF EXCESSIVE RAINFALL FOR PORTIONS OF THE MID-MISSOURI BASIN AND LOWER MISSISSIPPI VALLEY... 16Z Update... Overall, made minor changes to the previous outlook based on the 12Z HREF guidance and current trends. A small Marginal Risk was added to portions of southeastern Arizona and southwestern New Mexico to reflect increasing PWs and weak steering flow which may support slow-moving storms capable of producing locally heavy amounts during the afternoon into the evening hours. Pereira Previous Discussion... ....Northern High Plains through the Mid-Missouri Valley and Southern Great Lakes... Nearly zonal flow this morning will gradually transition more to NW flow later today as a shortwave digs into the mean longwave trough across the eastern CONUS. This evolution will help push a wavering surface front to the south while maintaining a NW to SE axis parallel to the increasing flow aloft. A 300mb jet streak coming out of the Pacific Northwest will flatten at the same time, leaving favorable LFQ diffluence atop the front and into the Northern Plains. The overlap of this diffluence with subtle height falls ahead of shortwave impulses and their associated PVA, will impinge into the weak baroclinic boundary to drive deep layer ascent from eastern MT through the Mid-Missouri Valley. This ascent will occur into favorable thermodynamics characterized by PWs surging on return flow ahead of the front to 1.25 to 1.5 inches, approaching +2 standard deviations from the climo mean according to NAEFS, and MUCAPE surging northward within a corridor ahead of the front reaching 2000 J/kg. This impressive overlap of ascent and moisture/instability will result in scattered to widespread showers and thunderstorms with rain rates exceeding 1"/hr likely according to HREF neighborhood probabilities. 0-6km mean winds of 15-25 kts suggest progressive storms, but with the wind aligned to the front, some short term training is possible which could result in isolated instances of flash flooding necessitating a continuation of the MRGL risk with only subtle cosmetic adjustments. Although the overall flash flood risk is modest today, there is an area of higher probabilities from eastern SD/NE into IA and far northern MO. Here, both the baroclinic and instability gradient will be most intense, supporting an axis of greater risk for an MCS (or possibly two) to drop southeast into the higher moisture and along the 500mb thickness gradient tonight. The guidance is in good agreement that an MCS will form as a shortwave digs along this gradient and interacts with 0-6km effective bulk shear of 40-50 kts. However, timing and placement is still uncertain which is reflected by modest HREF EAS probabilities for 1" of rainfall. While parts of NE/IA have been wetter than normal the past 14-days, soils appear generally hydrophilic as reflected by low streamflow anomalies, so only the longest duration of heaviest rainfall would likely result in scattered instances of flash flooding. The greatest risk area for this according to the HREF and GEFS is across western IA, so the SLGT risk was tailored to best match these probabilities with some extension to account for lower FFG/more sensitive soils. Farther to the east towards Chicago, IL and Detroit, MI, some aftn/evening showers and thunderstorms may develop along the front as it continues to sag southeast into the area. There is a narrow corridor both temporally and spatially for an overlap of convergence for ascent along the front interacting with a rich theta-e plume surging northeastward. Confidence is generally low in evolution as any slowing of the front could reduce the available moisture considerably. However, HREF probabilities have increased for 1" of rainfall due to convection, and the mean flow appears aligned to the boundary during this time. This could produce some short duration training/backbuilding into the higher theta-e plume to support an isolated flash flood risk. ....Southern Plains through the Gulf Coast... A stationary front aligned west to east from the Southern Plains through South Carolina will begin to lift north as a warm front and weaken today. This evolution will be driven by an expanding high pressure ridge centered over the Desert Southwest which will elongate to the east to drive bulging heights along the western and central Gulf Coast. The longwave trough that has been plaguing the region the past few days will be displaced eastward during this evolution, helping to additionally weaken the surface boundary. The slow height rises combined with the weakening trough and associated displacement of the upper jet streak will result in weakened ascent today for the Gulf Coast region. Still, a corridor of enhanced PWs of 2-2.25" overlapping MUCAPE of around 2000 J/kg should allow for at least scattered thunderstorms today, with storms moving slowly within the general weakly forced environment. HREF probabilities suggest a good chance for 1-2"/hr rates in thunderstorms that develop today, which through slow motions could produce locally more than 3 inches of rainfall in some areas. Although in general this area will see only an isolated risk for flash flooding, there appears to be a subtle maximum in flash flood risk due to higher convective coverage across northern Louisiana. Here, some better backbuilding is likely as the weak warm front lifts northward allowing storms to regenerate into higher instability, which will enhance the duration of heavy rain rates. Additionally, these aftn/eve thunderstorms could precede an MCS (or possibly two) that is progged by the high-res to sweep southeast along the increasing CAPE gradient tonight. In areas that receive both leading thunderstorms and these MCSs, locally more than 5 inches of rain is possible as reflected by the newest HREF exceedance probabilities. While much of LA has been dry recently noted by 14-day rainfall generally 50-75% of normal, there is an axis in northern LA and far southern AR that has received more than 150% of rainfall during this same temporal window. This is also the area that has the greatest risk for the heaviest rain today, and although HREF 3-hr FFG probabilities are still only 20-25%, they have increased since the last run. After coordination with SHV/JAN/LZK, a small SLGT risk area was added. ....Northern New England... Lingering light to potentially moderate rainfall rates will persist through the morning, primarily across far northern VT, NH, and ME. This rain will be driven by a pivoting deformation axis in the vicinity of a negatively tilted shortwave lifting into Maine, and an occluded front connecting two surface low pressures also shifting northeast through the morning. This shortwave and accompanying occluded boundary will likely eject into Canada by the late aftn, allowing for much drier air advecting in from the west, noted by a rapid decrease in mid-level RH, to finally bring an end to the area rainfall. PWs in the morning will still be generally 1.25 - 1.5 inches, about +1 standard deviation above the climo mean according to NAEFS, overlapping a corridor of 500-750 J/kg MUCAPE ahead of the front. These thermodynamics will support at least brief rainfall rates of 0.5-1"/hr, but with generally fast storm motions to the north. While the total coverage of rainfall this morning appears to be limited, and total rainfall will also likely be modest noted by HREF probabilities for 1" peaking around 20-50%, this will be falling atop extremely saturated soils and likely still ongoing flash flooding from Monday's rain event. This suggests the inherited MRGL risk is still needed as any additional rainfall could quickly become runoff, but the overall threat will be isolated and ending by the evening. Weiss Day 2 Valid 12Z Wed Jul 12 2023 - 12Z Thu Jul 13 2023 ....THERE IS A SLIGHT RISK OF EXCESSIVE RAINFALL FOR THE MID-MISSISSIPPI VALLEY AND SOUTHERN GREAT LAKES... ....Mid-Mississippi Valley through the Great Lakes... NW flow around the periphery of a large cyclonic gyre centered near the Hudson Bay will strengthen as the gradient becomes pinched in response to shortwaves rotating through the flow. Timing of these shortwaves is always challenging in these summer patterns, but each one could result in organizing convection, and the guidance tonight indicates that multiple MCSs may traverse through the flow this period. Aiding in the development and organization of these MCSs will be a modest low-level baroclinic gradient along a wavering stationary front and associated elevated boundary, with outflows from each MCS helping to meander the front and provide additional focus for ascent, with a zonally oriented jet streak providing additional deep layer lift through the diffluent LFQ of this feature. Due to the uncertainty in timing and placement of each MCS, which will also affect subsequent tracks, confidence is high in heavy rain but low in exact placement. The impressive ascent will work into extremely favorable thermodynamics to enhance coverage and intensity of convection through D2. Return flow around a high pressure to the east will allow the 850mb inflow to increase to 20-30 kts and veer into the front, drawing impressive PWs above 2" from the Gulf of Mexico northward. This flow will veer into the front driving robust moisture confluence noted by the convergence of moisture transport vectors, while also lifting isentropically atop the front and any nearby outflow boundaries. Additionally, instability will peak above 3000 J/kg MUCAPE south of the front, and then be transported northward/resupplied on the low-level inflow. This will not only allow convection to persist through the day, but also maintain intensity with rain rates likely exceeding 1"/hr in much of the convection. The available high-res guidance suggests that each MCS may lay down an outflow onto which additional convection will develop, and with Corfidi vectors parallel to the mean 0-6km mean winds, and aligned to the front/outflows, the setup appears quite favorable for long duration training or repeated rounds of convection in some areas. Where the most prolonged training occurs, rainfall could be quite impressive as noted by modest probabilities for 3" and 5" from the HREF/GEFS, and several global deterministic models showing more than 4" near St. Louis, MO, but uncertainty abounds in the placement of the heaviest axis. The guidance tends to end up a bit northeast of the actual footprint however as noted by ERO bias verification, so the inherited risk area was adjusted slightly SW with this update. Considered a MDT risk across eastern Missouri where the signal is already impressive, but after coordination with WFOs LSX/DVN/EAX/SGF, opted to maintain the SLGT for now and note the "higher end" SLGT potential. It is possible, maybe likely, that a MDT risk will be needed for some of this area if guidance can converge on a location with future updates. Farther north and east, periods of prolonged training along the more west-east oriented front into lower Michigan will likely produce rounds of heavy rainfall with rates above 1"/hr. In this region, including Chicago, IL and Detroit, MI, heavy rain could accumulate to more than 3" in some areas leading to scattered instances of flash flooding, especially within the longer duration training or atop more urbanized/less permeable areas. ....Gulf Coast States... Slow moving thunderstorms are again expected near the Gulf Coast on Wednesday, with two areas of focus possible. The first will be across far southern AR/northern LA where a lingering MCS from D1 may persist across this region the first half of D2. Uncertainty is high as to how intense this MCS will still be as the LLJ veers Wednesday morning and instability gets overturned, but lingering heavy rain atop soils likely saturated from D1 rainfall necessitated an introduction of a MRGL risk for this area. Farther to the south and east, from eastern LA through the northern FL peninsula, a signal exists for some very slow moving thunderstorms as Corfidi vectors collapse to just 5 kts and align into the instability offshore into the Gulf of Mexico to suggest some training. Low-level inflow from the Gulf will keep PWs above 2", with some local backing possible as the remnant shortwave/MCV from the MCS over northern LA shifts southward. This could produce scattered slow moving thunderstorms with 2+"/hr rain rates, leading to locally more than 3" of rain on Wednesday. Weiss Day 3 Valid 12Z Thu Jul 13 2023 - 12Z Fri Jul 14 2023 ....THERE IS A SLIGHT RISK OF EXCESSIVE RAINFALL FOR PORTIONS OF THE MID-MISSISSIPPI VALLEY AND THE INTERIOR NORTHEAST... ....Central Plains through the Ohio Valley... Persistent mid-level NW flow will plague the Central Plains through the Ohio Valley Thursday, within which lobes of vorticity beneath weak shortwaves will rotate southeast through the period. These shortwaves will produce rounds of enhanced ascent within otherwise favorable lift along the diffluent portion of a zonally oriented jet streak shifting across the area. In the lower levels, 850mb inflow will return from the Gulf of Mexico at 15-25 kts, drawing PWs of 1.75 to 2 inches northward, in conjunction with impressive MUCAPE of 2000-4000 J/kg. This will produce an extremely favorable thermodynamic environment for heavy rain, with the deep layer ascent driving waves of thunderstorms through the day. The placement of the most intense thunderstorms is uncertain due the likelihood that MCSs on D2 will impact the area of best low-level convergence along residual outflow boundaries and a wavering warm front/stationary front. However, where convection develops, rainfall rates will likely be 1-2"/hr, with convection organizing through 40-50 kts of effective bulk shear and then training along the front from west to east. A broad MRGL risk was inherited and maintained for any of these heavy rain producing thunderstorms that can train, and the more compact SLGT risk area was adjusted slightly to best match the GEFS/ECENS/SREF probabilities for 1" of rain aligned to the highest WPC QPF footprint. This area was then coordinated with the affected WFOs. Additional adjustments in the location are likely with time however, as model consensus merges on the best focus area for MCS/training on Thursday. ....Central Appalachians through the Northeast... Expansive trough centered near the Hudson Bay will maintain generally lowered heights across the eastern CONUS as broadly cyclonic flow envelops the region. Within this cyclonic flow, multiple shortwaves will rotate WSW to ENE through the flow, leading to regions of enhanced mesoscale ascent through height falls and PVA, as well as pockets of increased upper divergence. Any of these shortwaves will drive enhanced areas of ascent, and with a wavering front across the area to enhance low-level baroclinicity, subtle waves of low pressure lifting northeast are also possible. It is likely any of these waves will drive more focused shower and thunderstorm development, which will otherwise be generally scattered ahead of the front and beneath any locally more significant ascent. The environment from the Central Appalachians into the Northeast will be favorable for heavy rain regardless of the coverage and organization of thunderstorms. PWs as high as 1.75 inches will be advected northward downstream of the trough axis as 850mb flow rises to 20-30 kts. This will also transport MUCAPE of 1000-2000 J/kg as far north as Northern New England. These thermodynamics will support rainfall rates of 1-1.5"/hr, while unidirectional flow parallel to the approaching boundary supports training of echoes. This could result in rainfall of 1-3" according to the GEFS/ECENS/SREF probabilities. While confidence in the axis of the heaviest rainfall is still uncertain due to timing and placement of mid-level impulses and the front, a SLGT risk was expanded for much of NH/VT and eastern Upstate NY, primarily due to exceptionally wet antecedent soils leading to FFG that is as low as 0.5-1"/3 hrs which could quickly be exceeded through any training. This area was coordinated with WFO ALY/BGM/BTV, but additional adjustments are likely during the next few days to account for updated model guidance. Weiss Day 1 threat area: https://urldefense.com/v3/__https://www.wpc.ncep.noaa.go= v/qpf/94epoints.txt__;!!DZ3fjg!-PnH4P41aOLoiQoVVpwoU312d59TGkLdSfxDudV0evxt= zosmUG0cKeZ5n8tELTVazHKP64OiteO1sUTJ1O-mnPwkw9Y$=20 Day 2 threat area: https://urldefense.com/v3/__https://www.wpc.ncep.noaa.go= v/qpf/98epoints.txt__;!!DZ3fjg!-PnH4P41aOLoiQoVVpwoU312d59TGkLdSfxDudV0evxt= zosmUG0cKeZ5n8tELTVazHKP64OiteO1sUTJ1O-mP62s5kg$=20 Day 3 threat area: https://urldefense.com/v3/__https://www.wpc.ncep.noaa.go= v/qpf/99epoints.txt__;!!DZ3fjg!-PnH4P41aOLoiQoVVpwoU312d59TGkLdSfxDudV0evxt= zosmUG0cKeZ5n8tELTVazHKP64OiteO1sUTJ1O-mUFZjEFA$=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) .