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|    WEATHER    |    Messages from the national weather servi    |    41,475 messages    |
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|    Message 38,512 of 41,475    |
|    COD Weather Processor to wx-storm@lists.illinois.edu    |
|    MESO: Nws Weather Prediction Center Coll    |
|    15 Nov 25 19:19:58    |
      TZUTC: 0000       MSGID: 166714.weather@1:2320/105 2d8093a3       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 151919       FFGMPD       AZZ000-NVZ000-CAZ000-160115-              Mesoscale Precipitation Discussion 1225       NWS Weather Prediction Center College Park MD       219 PM EST Sat Nov 15 2025              Areas affected...Desert regions of CA into southern NV and far       western AZ              Concerning...Heavy rainfall...Flash flooding possible              Valid 151917Z - 160115Z              Summary...Periods of heavy rain should become likely across the       desert regions of eastern/southern CA into southern NV and far       western AZ through 01Z. Peak hourly rainfall between 0.5 and 1.0       inches (locally higher) is expected which may result in isolated       to widely scattered instances of flash flooding.              Discussion...Radar mosaic imagery across southern CA into southern       NV at 19Z showed an arcing band of heavy showers continuing to       move inland, from the Peninsular Ranges toward the far southern       San Joaquin Valley. Observed hourly rainfall within this axis has       been in the 0.5 to 0.9 inch range over the past 2-3 hours.       Additional showers were noted from just west of the lower CO River       into western Clark County in southern NV with MRMS-derived hourly       rainfall in excess of 1 inch in eastern Imperial County. These       showers were forced in response to lift ahead of a negatively       tilted shortwave trough located ~100 miles off of the southern CA       coast, swinging toward interior southern CA. In addition,       divergence and diffluence were increasing across southern CA       within the left-exit region of a 90-110 kt upper level jet max       located just south of the shortwave trough axis. Moisture was       highly anomalous for mid-November with regional PW standardized       anomalies of 4 to 5+ throughout the area, with a source region       stemming from the tropical eastern Pacific as seen on OSPO ALPW       imagery.              As the closed low and negatively tilted shortwave trough continues       to advance east over the next 6 hours, low level moisture will       continue to advect into the deserts with a transient swath of 6.0       to 6.5 C/km 700-500 mb lapse rates (coincident with the shortwave)       which should help to briefly boost instability, despite the lack       of surface heating beneath clouds/rain. Also of note were the       850-700 mb winds oriented from the southeast at 30-35 kt over       south-central CA, forcing an upslope component along the eastern       slopes of the southern Sierra Nevada. With little change to the       low to mid-level wind fields anticipated over the next 3-6 hours,       steady upslope forced heavy rain is expected into the terrain.       Farther east, embedded higher rainfall rates are expected to       develop through the afternoon within the scattered       shower/stratiform rain regime. While CAPE values are generally       forecast to stay below 500 J/kg (outside of the lower CO Valley),       the anomalous moisture source should contribute to embedded higher       rainfall values with periods of brief training, allowing for       hourly rainfall in the 0.5 to 1.0 inch range (locally higher).       Peak total rainfall of 1 to 2 inches is expected (locally higher       near terrain) through 01Z which may result in areas of flash       flooding.              Otto              ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!=       DZ3fjg!9thXAR0MeAzY90w6Y5yt960fJNwMeBjCZqbAGy3VOG4ggdTCBbyCvWQaMI4GnO868aiI=       9KlPp1Z91dR8bBP6ueFEqGI$ for graphic product...              ATTN...WFO...HNX...LKN...LOX...PSR...REV...SGX...VEF...              ATTN...RFC...RSA...STR...NWC...              LAT...LON 38051725 37481583 36161447 35111412 33431409=20        32231432 32471532 32481594 33171615 33501626=20        33671637 33951653 34111664 34231678 34311702=20        34391729 34501763 34651808 34781841 34911860=20        35061867 35231863 35381859 35491856 35641849=20        35721842 35801837 35891833 35961828 36081823=20        36181815 36311810 36411813 36481817 36601822=20        36661826 36751829 36851834 36931837 37031839=20        37121843 37211847 37261852 37321860 37421865=20        37621866 37861848 38041808=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: 4/0 19/10 88/0 90/0 93/1 104/119 105/81 106/201 114/10 120/302       SEEN-BY: 128/187 129/14 153/757 7715 154/10 30 50 110 700 218/700       SEEN-BY: 218/840 220/10 20 30 90 221/1 6 360 226/18 30 44 50 227/114       SEEN-BY: 229/110 206 300 307 317 400 426 428 470 664 700 705 266/512       SEEN-BY: 291/111 301/1 320/219 322/757 335/364 341/66 200 342/200       SEEN-BY: 396/45 460/58 633/280 712/848 880/1 900/0 102 106 902/0 19       SEEN-BY: 902/26 904/0 13 905/0 2320/0 105 304 3634/12 5019/40 5020/400       SEEN-BY: 5075/35       PATH: 2320/105 154/10 221/6 341/66 902/26 229/426           |
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