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|    WEATHER    |    Messages from the national weather servi    |    41,475 messages    |
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|    Message 40,519 of 41,475    |
|    COD Weather Processor to wx-storm@lists.illinois.edu    |
|    DAY3SVR: Nws Storm Prediction Center Nor    |
|    20 Jan 26 07:46:52    |
      TZUTC: 0000       MSGID: 168722.weather@1:2320/105 2dd6fc08       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       ACUS03 KWNS 200746       SWODY3       SPC AC 200745              Day 3 Convective Outlook       NWS Storm Prediction Center Norman OK       0145 AM CST Tue Jan 20 2026              Valid 221200Z - 231200Z              ...NO THUNDERSTORM AREAS FORECAST...              ...SUMMARY...       Thunderstorms are not expected on Thursday.              ...Synopsis...              An upper shortwave trough/low near the CA coast will develop east       toward southern CA/northern Baja by Friday morning. As this occurs,       upper flow over the eastern half of the CONUS will become       flatter/quasi-zonal. At the surface, arctic high pressure will build       over the Canadian Prairies and begin to slide southward into the       Plains, ushering in a very cold airmass. Forecast guidance varies in       the location of an arctic cold front by the end of the period, but       the expectation is that by early Friday morning, the front will be       located somewhere near central OK to the Red River, and stretch       eastward toward the Mid-South.              Modified Gulf moisture will be located well south of the front from       central/southern TX toward the central Gulf Coast. Isolated       convection may develop near or to the cool side of the cold front       late Thursday night/early Friday morning across north TX/southern OK       within warm advection around 850 mb. However, instability is       expected to be very minor and lighting is not expected. Further       south in better low-level moisture, forcing for ascent will be       limited and warm midlevel temperatures will preclude       destabilization.              ..Leitman.. 01/20/2026              $$              = = =       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: 154/110 700 203/0 218/700 840 220/10 20 90 221/1 6 360 226/18       SEEN-BY: 226/30 44 50 227/114 229/110 134 206 300 307 317 400 426       SEEN-BY: 229/428 470 664 700 705 240/5832 266/512 280/5003 291/111       SEEN-BY: 301/1 320/119 219 319 2119 322/757 762 326/101 335/364 341/66       SEEN-BY: 342/200 396/45 423/81 460/58 633/280 712/848 902/26 2320/0       SEEN-BY: 2320/105 304 3634/12 5020/400 5075/35       PATH: 2320/105 154/10 221/6 1 320/219 229/426           |
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