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|    WEATHER    |    Messages from the national weather servi    |    41,475 messages    |
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|    Message 38,694 of 41,475    |
|    COD Weather Processor to wx-storm@lists.illinois.edu    |
|    MESO: Nws Weather Prediction Center Coll    |
|    21 Nov 25 12:45:47    |
      TZUTC: 0000       MSGID: 166896.weather@1:2320/105 2d8820f2       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 211245       FFGMPD       CAZ000-211830-              Mesoscale Precipitation Discussion 1239       NWS Weather Prediction Center College Park MD       744 AM EST Fri Nov 21 2025              Areas affected...Southern California              Concerning...Heavy rainfall...Flash flooding possible              Valid 211245Z - 211830Z              SUMMARY...Risk of slow moving, narrow updrafts capable of       .75"-1"/hr rates likely to continue to a few more hours. Isolated       1-2" totals in/near urban locations in SoCal suggest localized       flash flooding remains possible.              DISCUSSION...A well-defined closed low is parked directly over       southern California with an upstream highly anomalous       shortwave/vorticity center descending southward along the western       periphery of the low. This and favorable cyclonically curved       geography of the coast and mountain ranges will help to keep       surface to boundary layer cyclone relatively stationary for the       next few hours just along/south of Long Beach, CA. The cold front       and associated warm conveyor have pressed eastward into far NW       Baja California (state) of Mexico before angling through Imperial       Valley and lower Colorado River Valley. However, the western       branch of the TROWAL and occluded front remain banked up against       the Orange county and San Diego county beaches.=20              GOES-W WV suite shows the core of the upper-level jet remains       south near the San Diego country border with Mexico, allowing for       solid cyclonically curved left exit ascent across much of SoCal       providing solid ascent for updrafts that do develop with the solid       surface/low level moisture convergence. The limiting factor will       likely be unstable air/vertical ascent through convective       processes. MUCAPEs have dropped to around 500 J/kg but are now       mostly driven through cold advection aloft. The upstream       shortwave will dull this advection for a few hours but may allow       the lapse rates to maintain this weak 250-500 J/kg instability.=20=20       As such, updrafts are likely to remain isolated and generally       narrow, though with isallobaric response to the updraft, moisture       convergence should allow for the .75-.9" total PWats (loaded       mainly below 700mb) to support rates of .75-1"/hr.=20              As such, a localized 1-2" total still remains possible for the       next few hours. Naturally low FFG and/or urban hydrophobic       conditions will result in solid run-off and maintain a risk of       widely scattered incident or two of possible flash flooding       through the morning.=20=20              It is also possible (more likely toward 16-18z) that a few       showers/cells may try to develop with some weak clearing through       the Imperial Valley along the western branch of the TROWAL. These       cells would be also similarly slow moving but likely translating       NW rather than NE as with the coastal cells; but there is less       certainty with that evolution and a secondary MPD may be required       if trends continue to improve.=20=20              Gallina              ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!=       DZ3fjg!6defLsDhQO-ON-LqODLd4v4g66xlCixSbO2_VOxQBeCuFq2HkSlxnEp1Y3e9UPBfwxAh=       InmHHKSqNelNU_uwQNCMueQ$ for graphic product...              ATTN...WFO...LOX...SGX...              ATTN...RFC...RSA...NWC...              LAT...LON 34551850 34481788 34071704 33471650 32801624=20        32581627 32531672 32561724 32981753 33301781=20        33581827 33971908 34331893=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: 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: 229/206 300 307 317 400 426 428 470 664 700 705 266/512 267/800       SEEN-BY: 291/111 301/1 320/219 322/757 335/364 341/66 342/200 396/45       SEEN-BY: 460/58 633/280 712/848 770/1 100 340 350 772/210 220 230       SEEN-BY: 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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