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|  Message 40132  |
|  COD Weather Processor to wx-storm@lists.illinois.edu  |
|  HVYRAIN: Excessive Rainfall Discussion  |
|  07 Jan 26 18:55:03  |
 TZUTC: 0000 MSGID: 168335.weather@1:2320/105 2dc6739e PID: Synchronet 3.21a-Linux master/123f2d28a Jul 12 2025 GCC 12.2.0 TID: SBBSecho 3.28-Linux master/123f2d28a Jul 12 2025 GCC 12.2.0 BBSID: CAPCITY2 CHRS: ASCII 1 FORMAT: flowed FOUS30 KWBC 071854 QPFERD Excessive Rainfall Discussion NWS Weather Prediction Center College Park MD 154 PM EST Wed Jan 7 2026 Day 1 Valid 16Z Wed Jan 07 2026 - 12Z Thu Jan 08 2026 The probability of rainfall exceeding flash flood guidance is less than 5 percent. Otto Day 2 Valid 12Z Thu Jan 08 2026 - 12Z Fri Jan 09 2026 The probability of rainfall exceeding flash flood guidance is less than 5 percent. Cook/Kleebauer Day 3 Valid 12Z Fri Jan 09 2026 - 12Z Sat Jan 10 2026 ...THERE IS A SLIGHT RISK OF EXCESSIVE RAINFALL ACROSS PORTIONS OF THE TENNESSEE VALLEY AND DEEP SOUTH... ...21Z Outlook Update... A few modifications were made to the Marginal and Slight Risk areas - mainly to trend southward and slightly westward per 12Z=20 guidance. These expansions now include Birmingham, AL and Jackson,=20 MS metropolitan areas. QPFs have increased in these areas, and the=20 nature of the forcing/ascent suggests potential for a few storms to train. Additionally, storms may focus along a warm front oriented=20 east to west across the region, but models are generally uncertain=20 on where this front will reside when the bulk of the convection=20 moves through the risk areas. Furthermore, mesoscale details are=20 unclear and outflows/convective augmentation of the warm front are=20 all possible. Potential is there for a localized region of 5+=20 inches of rain during the forecast period but with details=20 remaining unclear, holding at Slight/Marginal seems to be the best=20 course of action. Ground conditions are quite dry, which lends some uncertainty on the ground impacts/flash flood potential but if=20 enough rainfall occurs on a localized basis, that aspect of the=20 forecast may not matter as much. See the prior forecast below for additional information. Cook ...Previous Discussion... Large scale amplification of a trough over the Central Rockies into the Central Plains will generate a broad axis of ascent from the Mississippi Valley to points eastward with a cold frontal progression slowly migrating east across the aforementioned areas. Meridional component of the pattern evolution will benefit from the strengthening mean trough with multiple shortwave ejections rounding the trough base across the Lower Mississippi Valley, advancing northeast through the Southeastern U.S. before migrating into the Tennessee Valley by the end of the D3. Deep moisture plume ahead of the trough will usher anomalous PWATs on the order of +2 to +4 sigma spanning east TX through much of the Southeast into the Southern Ohio Valley. Ample shear and deep moist axis will maintain a prevalent fixture for much of the period with flow running close to, if not parallel to the frontal axis that will bisect southwest to northeast across the Lower Mississippi Valley through Central and Northern MS/AL into TN. Current ensemble trends favor a rather broad axis of 2-3" precip totals just within the means with the deterministic output pushing closer to 4-5" with the maxima focused over central MS up through northern AL to south- central TN. This aligns well with the pattern evolution progressing the front into those confines with a multi-wave ejection riding into the front as they eject out of the broad deep-layer southwesterly flow situated across the region. This setup is classic for a winter time flash flood prospect across this area of the CONUS as broad ascent coupled with ample deep- layer shear and highly anomalous moisture tends to amplify the threat for heavy rainfall repeating over the same areas. This is being forecast within the Southeast and far southern edge of the Ohio Valley with the ensemble overlap generally in that corridor from east-central MS to points north and east with a maxima oriented over northern AL into southern TN. This is likely the area to watch, however don't be surprised if areas south across the southern half of MS into parts of LA see a greater heavy convective signature that tends to crop up in the short range as the instability maximum tends to verify a bit further south compared to what global deterministic output has at this lead. For now, maintained general continuity in the grand scheme, but adjusted the SLGT and MRGL risks based on QPF trends and alignment with the greatest potential for training, and elevated theta_E placement. Kleebauer Day 1 threat area: https://urldefense.com/v3/__https://www.wpc.ncep.noaa.go= v/qpf/94epoints.txt__;!!DZ3fjg!-Te7XQvCcYUMF72bJoH1aH9rt7wrT2SvUdy9yu7eW2cG= YdQZVALSh1oaUadu-A9ImDPp9b8ZdxpOYnQaPt6IYgBcaZs$=20 Day 2 threat area: https://urldefense.com/v3/__https://www.wpc.ncep.noaa.go= v/qpf/98epoints.txt__;!!DZ3fjg!-Te7XQvCcYUMF72bJoH1aH9rt7wrT2SvUdy9yu7eW2cG= YdQZVALSh1oaUadu-A9ImDPp9b8ZdxpOYnQaPt6ISZk0cWg$=20 Day 3 threat area: https://urldefense.com/v3/__https://www.wpc.ncep.noaa.go= v/qpf/99epoints.txt__;!!DZ3fjg!-Te7XQvCcYUMF72bJoH1aH9rt7wrT2SvUdy9yu7eW2cG= YdQZVALSh1oaUadu-A9ImDPp9b8ZdxpOYnQaPt6I0cXghzk$=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 3.28-Linux * Origin: Capitol City Online (1:2320/105) SEEN-BY: 1/19 100 16/0 19/10 37 104/119 105/81 106/201 114/10 120/302 SEEN-BY: 123/130 128/187 129/14 142/104 153/757 7715 154/10 30 50 SEEN-BY: 154/110 700 201/0 203/0 218/700 840 220/10 20 30 90 221/1 SEEN-BY: 221/6 360 226/18 30 44 50 227/114 229/110 134 206 275 300 SEEN-BY: 229/307 317 400 426 428 470 664 700 705 240/5832 266/512 SEEN-BY: 280/5003 291/111 301/1 320/119 219 319 2119 322/757 762 326/101 SEEN-BY: 335/364 341/66 342/200 396/45 423/81 460/58 633/280 712/848 SEEN-BY: 902/26 2320/0 105 304 3634/12 5020/400 5075/35 PATH: 2320/105 154/10 221/6 1 320/219 229/426 |
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