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|    WEATHER    |    Messages from the national weather servi    |    41,475 messages    |
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|    Message 40,182 of 41,475    |
|    COD Weather Processor to wx-storm@lists.illinois.edu    |
|    MESO: Nws Weather Prediction Center Coll    |
|    09 Jan 26 09:13:41    |
      TZUTC: 0000       MSGID: 168385.weather@1:2320/105 2dc88e90       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 090913       FFGMPD       MSZ000-LAZ000-ARZ000-091501-              Mesoscale Precipitation Discussion 0007       NWS Weather Prediction Center College Park MD       412 AM EST Fri Jan 09 2026              Areas affected...Central Mississippi...Eastern and Northeastern       Louisiana...              Concerning...Heavy rainfall...Flash flooding possible              Valid 090911Z - 091501Z              SUMMARY...Flattening steering flow to support segmented training       corridors across the Lower Mississippi River Valley.=20       Strengthening convergence and modestly unstable and seasonably       moist air should support rain rates to 1.75" and localized streaks       of 2-4" in 1-3hrs. Suggesting localized flash flooding is       possible this morning to start a longer day of repeat       thunderstorms.              DISCUSSION...GOES-E WV suite shows mature/decaying shortwave       rapidly elongating and sliding northeast through the central Great       Lakes with a well defined broadly anticyclonically curved       subtropical jet streak across Texas through KY/TN with a stronger       base of the northern stream synoptic trough well upstream emerging       into the southern High Plains. The strong flow and upper-level       dynamic support has resulted in well above normal moisture flux       across the Mississippi River Valley into the Great Lakes; CIRA LPW       denotes core of higher moisture/theta-E air over the West Gulf is       advancing into the entrance of the eastern US atmospheric river       stream. Surface to 850mb values are nearing 1" and is noted with       surface Tds in the upper 60s to even spots of 70 across the Lower       MS Valley.=20              The overall orientation of the upper-level flow is supporting a       pre-frontal confluence zone across E LA at this time, providing       sufficient deep layer convergence to tap the weakly unstable air.       MLCAPEs are analyzed from 500-1000 J/kg through the Sabine River       Valley into the Delta Region of SE AR and W MS. Flux convergence       of 30-35kts at about 30 degrees of convergence overlaps with the       core of the moisture axis with TPW near 1.7". As such, RADAR       denotes a few clusters of thunderstorms developing across NE LA as       well as further north across NE LA into W MS, the latter deeper       into the more ideal unidirectional flow and may support some       training elements as the overall convective development expands       and intensifies over the next few hours. The strong moisture flux       convergence mainly below 700mb will support rates of 1.75"; and       while the forward speeds will limit any specific core, the       upstream divergence aloft and strength of low level flow       convergence will support back-building and redevelopment upstream       through central LA throughout the morning.              Localized storm outflows may be the key to establishing the most       ideal training profiles, but even 1-2 hours of these rates could       support 2-3" totals and locally higher values to 4" would then       begin to exceed the high (3"/3hrs) FFG values in the area.=20       00z/06z HREF Probability of 3"/3hrs peak around 30% in SW to       central MS. Still even with dormant ground conditions, these       rates/totals will have the greatest potential for flash       flooding/rapid inundation conditions where intersecting urban       centers. In any case, these cells will saturate the upper soil       profiles prior to further convective activity expected throughout       the day and evening. As such, flash flooding is only considered       possible and limited to widely scattered in coverage through the       early morning period.=20=20=20=20              Gallina              ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!=       DZ3fjg!9acKgA_eVUQUbWukkTDJ3cwSbuwKek4CYWoR60Ef7vNo7XSoV4CCLFqlziyioqp90ODj=       KtIhNIYw04qxDKJ-RKVXHog$ for graphic product...              ATTN...WFO...JAN...LCH...LIX...MEG...SHV...              ATTN...RFC...ALR...ORN...NWC...              LAT...LON 34138908 34058839 33498829 32868864 32288915=20        31568980 30709050 30919161 30929254 31469279=20        32169248 33289103 33719020=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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