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|    WEATHER    |    Messages from the national weather servi    |    41,475 messages    |
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|    Message 38,976 of 41,475    |
|    COD Weather Processor to wx-storm@lists.illinois.edu    |
|    MESO: Nws Weather Prediction Center Coll    |
|    30 Nov 25 03:57:29    |
      TZUTC: 0000       MSGID: 167178.weather@1:2320/105 2d9383b9       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       AWUS01 KWNH 300357       FFGMPD       LAZ000-TXZ000-301000-              Mesoscale Precipitation Discussion 1255       NWS Weather Prediction Center College Park MD       1056 PM EST Sat Nov 29 2025              Areas affected...Central and Upper Texas Coastal Plain...              Concerning...Heavy rainfall...Flash flooding possible              Valid 300400Z - 301000Z              SUMMARY...Slow moving, pre-frontal cells with rates of 2"/hr       eventually merge with south-southeastward pressing cold front       convection resulting in localized 2-4" totals in 1-3 hours.=20       Isolated flash flooding remains possible, especially near urban       centers.              DISCUSSION...GOES-E 3.9um SWIR highlights a few low level       boundaries that will remain the focus of scattered thunderstorm       activity through the overnight period. The main being the surging       cold front being reinforced by favorable upper-level orientations       to support steepening of theta-E gradient while increasing       northerly surface wind flow to over 20-25kts nearly counter to the       weaker but solid onshore flow. Currently active convection along       the leading edge of the front is slow moving from Burleson to Polk       county as the winds are not fully intersecting with the line, but       will likely be propagating southward in the next hour or so. The       other boundary is the return moisture plume off the western Gulf       (which arches similar to the Lower TX Gulf coast before angling       east- northeast just south of the aforementioned convection). Tds       in the upper 60s to near 70 can be traced best in CIRA LPW sfc-850       and 850-700mb layers covering much of the MPD area of concern       across the Central and Upper Texas Coastal Plain.              Onshore flow is also increasing to 15-20kts resulting in       frictional convergence near coast. Conditionally unstable airmass       with MLCAPEs of 1000-1250 J/kg remain weakly capped but there are       some signs in satellite imagery of some weak cu field near       Victoria, TX as well as an isolated weakening supercells       northeast of Galveston Bay. The merging of the boundaries is also       allowing a westward expansion of new development upstream into       Bastrop/Caldwell county vicinity.=20              Total deep moisture of 1.5" as noted in the CIRA LPW is loaded       below 700mb, but there is solid deep saturation. These isolated       cells driven by frictional convergence will be slow moving and       eventually capable of 1-2"/hr rates. Spotty 2-3" totals will       occur in 1-2hrs, but as they mature and expand the slower moving       cells along the cold front will have started increased forward       speed and with very high low level moisture flux convergence will       have the capability of 1-1.25"/15min rainfall totals as they       intersect/merge with the cells across the Plain.              00z HREF probabilities continue to suggest 3"/3hr totals in the       20-30% range (3"/6hr over 50%) which is fairly impressive given       the strength of the updraft due to instability is fairly limited.=20       While the overall coverage will continue to be limited, spots of       3-4" totals are probable through 09z. This places sufficient       overlap of FFG exceedance (as 1hr FFG is 2.5-3" and 3hr is 3-4")       for possible localized incident or two of flash/rapid inundation       flooding. This only further increases with intersection with       urban centers, such as Victoria, Houston and Beaumont.=20=20              Gallina              ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!=       DZ3fjg!6eBqZJFeXYwfdfjOanroH9GQeQtbydrQfNUR442JL4eOoRDBCnP5-W_eKdR2izXE3AJE=       Wxq3reM5uV59a3QArZIE_ho$ for graphic product...              ATTN...WFO...CRP...EWX...HGX...LCH...              ATTN...RFC...FWR...NWC...              LAT...LON 30999472 30719393 30099362 29749380 29519420=20        29359466 28499607 27779725 27969777 28499795=20        29529752 29879714 30199681 30729602=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: capitolcityonline.net * Telnet/SSH:2022/HTTP (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 50 227/114 229/110 134 206 300 307       SEEN-BY: 229/317 400 426 428 470 664 700 705 240/5832 266/512 280/5003       SEEN-BY: 291/111 301/1 320/119 219 319 2119 322/757 762 326/101 335/364       SEEN-BY: 341/66 342/200 396/45 423/81 460/58 633/280 712/848 902/26       SEEN-BY: 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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