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|    WEATHER    |    Messages from the national weather servi    |    41,475 messages    |
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|    Message 40,893 of 41,475    |
|    COD Weather Processor to wx-storm@lists.illinois.edu    |
|    MESO: Mesoscale Discussion 0067    |
|    31 Jan 26 15:42:24    |
      TZUTC: 0000       MSGID: 169094.weather@1:2320/105 2de6029e       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       ACUS11 KWNS 311542       SWOMCD       SPC MCD 311542=20       NCZ000-VAZ000-SCZ000-311945-              Mesoscale Discussion 0067       NWS Storm Prediction Center Norman OK       0942 AM CST Sat Jan 31 2026              Areas affected...Piedmont of Upstate South Carolina into North       Carolina              Concerning...Heavy snow=20              Valid 311542Z - 311945Z              SUMMARY...Heavy hourly snow rates around or in excess of 1 inch per       hour may become increasingly common across the Carolina Piedmont       vicinity through 1-4 PM EST.              DISCUSSION...To this point, it appears that peak hourly snow rates       within an area of snow spreading across and to the lee of the       southern Appalachians have remained relatively modest. Precipitable       water across the Piedmont is generally around or below .35 inches,       with lower values to the west/northwest. Saturating temperature       profiles are well below freezing, but temperatures conducive to       dendritic ice crystal growth appear initially centered around 700       mb, somewhat low and perhaps not most optimal for larger dendritic       ice crystal growth and aggregation.              However, latest model output suggests that the deep, digging       upstream short wave trough/elongated cyclonic circulation will       gradually take on a more neutral orientation while pivoting across       and southwest of the southern Appalachians through 18-21Z.=20       Increasingly difluent and divergent mid/upper flow to the northeast       of this feature is forecast to contribute to a period of       strengthening upward vertical motion across the Carolina Piedmont.=20       This may be enhanced by a band of strengthening frontogenetic       forcing in the 800-700 mb layer, where forecast soundings indicate       cooling profiles will contribute to further lowering, but deepening,       of the dendritic growth zone. As this occurs, high resolution model       output, among other guidance, suggests increasing potential for       hourly snow rates in excess of 1 inch per hour, which may persist,       at least on an off, through much of the afternoon.              ..Kerr.. 01/31/2026              ...Please see https://urldefense.com/v3/__http://www.spc.noaa.gov__;!!DZ3fj=       g!67lltuLcrb80UL7_1ekI1jpdoJq9yc6-Te4BFuw3KzyqurxSsJKYGi5oJWbebyLGTnXEPBh0W=       q4kSlRHazVeHGYGu6Y$ for graphic product...              ATTN...WFO...RAH...RNK...CAE...GSP...              LAT...LON 35548200 36768021 35767929 34778073 34438187 35548200=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 70       SEEN-BY: 220/90 221/1 6 360 226/17 18 20 30 44 50 227/114 229/110       SEEN-BY: 229/134 206 300 307 317 400 426 428 470 664 700 705 266/512       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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