Subj : HVYRAIN: Excessive Rainfall Discussion To : wx-storm@lists.illinois.edu From : COD Weather Processor Date : Wed Feb 28 2024 08:03:37 FOUS30 KWBC 280803 QPFERD Excessive Rainfall Discussion NWS Weather Prediction Center College Park MD 302 AM EST Wed Feb 28 2024 Day 1 Valid 12Z Wed Feb 28 2024 - 12Z Thu Feb 29 2024 ....THERE IS A MARGINAL RISK OF EXCESSIVE RAINFALL OVER THE CENTRAL APPALACHIANS UP THROUGH NORTHERN NEW ENGLAND, AS WELL AS THE COASTAL PACIFIC NORTHWEST.. ....Mid-Atlantic and Northeast... Our potent shortwave trough is currently positioned over the north-central plains, moving eastward and beginning to take on a more neutral tilt which will occur by morning. Large scale ascent downstream of the mean trough has aid in multiple rounds of convection, some severe as they encounter a favorable instability axis thanks to a prominent theta-E advection regime and strong vorticity maxes ripping northeast off the broad southwest flow. This setup will continue in its progression with a sharp cold front pressing east along the tail end of a surface low as it pushes east-northeast through the Great Lakes, eventually into northern Quebec by the latter half of the period. All this will create a fairly dynamic setup over the eastern Ohio Valley up through the Northeast as large scale ascent shifts towards the eastern seaboard and the cold front aids as a focal point for linear convection to develop and propagate eastward with time. Out ahead of the mean trough, PWAT anomalies ranging from +2 over the Mid-Atlantic to as high at +4 over northern New England will enhance rainfall potential within the evolving synoptic pattern. Locally heavy rainfall will occur at any given point over the next 18-24 hrs with a few locations having the best potential for flooding prospects thanks to the combination of heavy rain and residual snow that adds the water loading provided by the rain. The main targets for flooding will be within the terrain of the Central Appalachians with a focus in-of the WV high country where snow-water equivalent readings of 2" or more remain based on the latest NOHRSC data set. Forecast rainfall between 1-2", much of which falling within a 6 hr time frame between 12-18z today will create a higher risk for localized flooding set within a complex topographic environment which which is well depicted within the recent FFG threshold of <1"/hr and <1.5"/6-hrs to generate flooding potential. The flood threat will reach a halt by later in the afternoon as rapid height falls behind a steady moving cold front will flip the rain to snow on the backside of the precip field, eventually lowering the flood threat for the second half of the forecast period. Further north, a more formidable snowpack remains across Upstate NY in-of the Tug Hill Plateau, Adirondack, and northern New England where moderate to heavy rainfall will occur prior to the frontal passage, creating another environment capable of localized flooding depending on rapid snowmelt coupled with any appreciable rainfall. QPF forecast of 0.5-1" with locally higher will be sufficient to tap into a high SWE pack still remaining within the complex terrain of each respective locale. This setup is similar to the WV/western PA high country with a similar premise of rain changing to snow after the passage of the cold front. This will allow for a sharp decline in flood potential and a shift to winter weather impacts. Further east of the mountains, pockets of heavy rain over urbanized areas could spell for low-end flood concerns, especially with any repeating heavy rainfall episodes over those more impactful locations. Overall, the setup is low to medium end of the Marginal Risk spectrum, but is enough to warrant a continuation of the previous forecast risk placement with little to no change from the last forecast package. ....Pacific Northwest... The next atmospheric river is taking shape across the PAC Northwest with a minor to bordering moderate AR forecast expected as IVT values between 500-700 kg/ms are expected to advect into WA/OR by the early morning hours, onward. This event will be characterized by longevity of moderate rainfall and less of short-term magnitude of rainfall as probabilistic fields are all fairly tame for the prospects of any hourly rates reaching the 1" mark. Most of the heaviest rain will settle between 0.5-0.75"/hr with the heaviest rainfall positioned over northwest OR and the higher terrain of the Olympic Peninsula where all guidance now pinpoints the heaviest precip totals within the period. Expect 2-4" to be fairly common within the coastal plain extending from the Olympic Peninsula down through southwest OR as we move into Thursday morning. While this is not a textbook flash flood concern, any poor drainage areas and urbanized locales will be at the highest risk for flooding during the period. The atmospheric river will continue to propagate southward down the Pacific coast with a continued threat heading into the D2 period. The previous MRGL risk was largely unchanged as the synoptic pattern and associated rainfall forecast remains on track. Kleebauer Day 2 The Day 2 outlook will be updated by 0830Z. 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!_j8CQ_6gRWl5m2N1YlCKPbcbtarFJHwKDUbv4AKZk3H4= 0Pgzvx4nds0veHNivMbksWgUaDWFpnXzU0AqjXfGqaFCE_E$=20 Day 2 threat area: https://urldefense.com/v3/__https://www.wpc.ncep.noaa.go= v/qpf/98epoints.txt__;!!DZ3fjg!_j8CQ_6gRWl5m2N1YlCKPbcbtarFJHwKDUbv4AKZk3H4= 0Pgzvx4nds0veHNivMbksWgUaDWFpnXzU0AqjXfG5CAcf40$=20 Day 3 threat area: https://urldefense.com/v3/__https://www.wpc.ncep.noaa.go= v/qpf/99epoints.txt__;!!DZ3fjg!_j8CQ_6gRWl5m2N1YlCKPbcbtarFJHwKDUbv4AKZk3H4= 0Pgzvx4nds0veHNivMbksWgUaDWFpnXzU0AqjXfGwx1XofQ$=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) .