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|    Message 40,118 of 41,475    |
|    COD Weather Processor to wx-storm@lists.illinois.edu    |
|    HVYRAIN: Excessive Rainfall Discussion    |
|    07 Jan 26 07:40:51    |
      TZUTC: 0000       MSGID: 168321.weather@1:2320/105 2dc5d58d       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 070740       QPFERD              Excessive Rainfall Discussion       NWS Weather Prediction Center College Park MD       240 AM EST Wed Jan 7 2026              Day 1       Valid 12Z Wed Jan 07 2026 - 12Z Thu Jan 08 2026              The probability of rainfall exceeding flash flood guidance is       less than 5 percent.              Kleebauer                     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.              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 SOUTHERN OHIO VALLEY INTO THE SOUTHEASTERN U.S...              Large scale amplification of a trough over the Central Rockies into       the Central Plains will generate a broad axis of ascent from the=20       Mississippi Valley to points eastward with a cold frontal=20       progression slowly migrating east across the aforementioned areas.=20       Meridional component of the pattern evolution will benefit from the       strengthening mean trough with multiple shortwave ejections=20       rounding the trough base across the Lower Mississippi Valley,=20       advancing northeast through the Southeastern U.S. before migrating=20       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=20       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.=20              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=20       instability maximum tends to verify a bit further south compared=20       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.=20              Kleebauer                     Day 1 threat area: https://urldefense.com/v3/__https://www.wpc.ncep.noaa.go=       v/qpf/94epoints.txt__;!!DZ3fjg!_Cc3pn5fLAEdigagMrDWZuY3VXDABFkL_wW8LpCaSmgn=       xwkRnLMaSPUDTRC-6onpFI4zhI34cU7e4Ldd3thMpXjNfME$=20       Day 2 threat area: https://urldefense.com/v3/__https://www.wpc.ncep.noaa.go=       v/qpf/98epoints.txt__;!!DZ3fjg!_Cc3pn5fLAEdigagMrDWZuY3VXDABFkL_wW8LpCaSmgn=       xwkRnLMaSPUDTRC-6onpFI4zhI34cU7e4Ldd3thMyZgm_Xc$=20       Day 3 threat area: https://urldefense.com/v3/__https://www.wpc.ncep.noaa.go=       v/qpf/99epoints.txt__;!!DZ3fjg!_Cc3pn5fLAEdigagMrDWZuY3VXDABFkL_wW8LpCaSmgn=       xwkRnLMaSPUDTRC-6onpFI4zhI34cU7e4Ldd3thMyYaNkPo$=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: 19/10 104/119 105/81 106/201 114/10 120/302 128/187 129/14       SEEN-BY: 153/757 7715 154/10 30 50 110 700 218/700 840 220/10 20 30       SEEN-BY: 220/70 90 221/1 6 360 226/17 18 30 44 50 227/114 229/110       SEEN-BY: 229/134 206 275 300 307 317 400 426 428 470 664 700 705 266/512       SEEN-BY: 267/800 291/111 301/1 320/219 322/757 335/364 341/66 342/200       SEEN-BY: 396/45 460/58 633/280 712/848 770/1 100 340 350 772/210 220       SEEN-BY: 772/230 902/26 2320/0 105 304 3634/12 5020/400 5075/35       PATH: 2320/105 154/10 221/6 218/840 770/1 633/280 229/426           |
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