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|    WEATHER    |    Messages from the national weather servi    |    41,475 messages    |
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|    Message 41,083 of 41,475    |
|    COD Weather Processor to wx-storm@lists.illinois.edu    |
|    MESO: Mesoscale Discussion 0070    |
|    07 Feb 26 02:37:26    |
      TZUTC: 0000       MSGID: 169283.weather@1:2320/105 2dee70af       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 070236       SWOMCD       SPC MCD 070236=20       PAZ000-MDZ000-WVZ000-070630-              Mesoscale Discussion 0070       NWS Storm Prediction Center Norman OK       0836 PM CST Fri Feb 06 2026              Areas affected...parts of eastern West Virginia and adjacent       portions of western Maryland/Pennsylvania              Concerning...Heavy snow=20              Valid 070236Z - 070630Z              SUMMARY...A period of moderate to heavy snow (at rates occasionally       up to 1+ inches per hour) and strengthening surface gusts to 30-40+       kt may develop by Midnight to 1 AM EST, accompanied by considerable       blowing and drifting of snow and occasionally sharply reduced       visibilities.              DISCUSSION...Mostly light to moderate snow overspreading the upper       Ohio Valley toward the western Allegheny Plateau is being supported       by forcing for ascent downstream of a vigorous short wave trough of       Arctic origins, which is forecast to continue digging across and       south-southeast of the lower Great Lakes region late this evening.=20       This is accompanied by a reinforcing cold front, which Rapid Refresh       indicates will begin overspreading the western slopes of the       Alleghenies during the 04-07Z time frame.=20=20              As this occurs, low-level flow is likely to veer to an increasing       northwesterly upslope component across the higher terrain,       contributing to strengthening upward vertical motion. Forecast       soundings indicate that this lift, coupled with low-level cold       advection, will contribute to saturating profiles with steepening       lapse rates. It appears that this may become supportive of the       development of very weak CAPE through a layer between 850-700 mb, as       temperatures within this layer cool to around and below -15 C.=20=20=20              Despite rather low precipitable water content falling below .20       inches, and the low residence height (higher pressure) of the       dendritic growth zone, the strong orographically enhanced low-level       lift and convective component may compensate, and support a period       of moderate to occasionally heavy snow rates on the order of .5-1+       inches per hour. This is also likely to coincide with downward       mixing of strengthening low-level wind fields which may support       30-40 kt surface gusts, contributing to considerable drifting and       occasional sharply reduced visibilities.              ..Kerr.. 02/07/2026              ...Please see https://urldefense.com/v3/__http://www.spc.noaa.gov__;!!DZ3fj=       g!9KIy1E12bLQi04OFS9FIp3VC4CiBJ5GEKLO7tgBxXQ8UD4_jL1rNabG_4VrRZE4nHYO0CUgL_=       1bB1hm4KrewvGzbsLQ$ for graphic product...              ATTN...WFO...CTP...LWX...RNK...PBZ...RLX...              LAT...LON 40027941 39447926 38717968 38158040 38448069 38578056        39128016 39627996 40027941=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: 154/110 700 203/0 218/700 840 220/10 20 90 221/1 6 360 226/18       SEEN-BY: 226/20 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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