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From | To | Subject | Date/Time | |||
COD Weather Processor | wx-storm | MESO: Nws Weather Prediction Center College Park Md |
July 20, 2019 8:24 AM * |
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This is a multi-part message in MIME format... ------------=_1563611093-2024-1935 Content-Type: text/plain AWUS01 KWNH 200824 FFGMPD MNZ000-SDZ000-201430- Mesoscale Precipitation Discussion 0638 NWS Weather Prediction Center College Park MD 424 AM EDT Sat Jul 20 2019 Areas affected...South Dakota Concerning...Heavy rainfall...Flash flooding possible Valid 200830Z - 201430Z Summary...Thunderstorms developing across South Dakota will become aligned west-east through the morning. Heavy rainfall rates of more than 1"/hr are expected, and storms are likely to train north of a front in Nebraska. Rainfall of 1-3", with locally higher amounts, is forecast to occur on top of saturated soils and low FFG. Flash flooding is possible. Discussion...A surface boundary has dropped into Nebraska early this morning, leaving E/NE winds across South Dakota. This boundary also demarcates the exceptionally unstable air (RAP MUCape > 5000 J/kg) from more modest instability (2000-3000 J/kg) across the discussion area. Despite the somewhat more stable surface air across SD, a mid-level baroclinic gradient exists across the state which is functioning as a convergent boundary to drive low-level ascent. This is occurring into a broad region of mid-level frontogenesis, which is overlapped by the RRQ of an intense 130kt jet streak shifting through Mantioba and Ontario provinces of Canada, and aided by weak PVA ahead of a shortwave noted on WV imagery. This deep layer ascent will continue to produce thunderstorms in the favorable thermodynamic environment, which should become even more favorable for heavy rainfall as PWATs surge towards 2 inches, or 2.5 standard deviations above the climatological mean, on backing low-level flow of 20-30 kts. With the west-east aligned forcing through a deep portion of the atmospheric column, thunderstorms should become linearly organized across portions of southern and central South Dakota, reinforced by any outflow boundaries, and move eastward along the robust 850-300mb thickness gradient. This setup will be favorable for training of storms, and the 0-6km mean wind becomes parallel to both the Corfidi vectors and the mid-level fgen gradient. With the environment remaining favorable for heavy rainfall, and HREF neighborhood probabilities for 1"/hr persisting for many hours at 40% or more, training of storms could produce rainfall in excess of 3" in some locations. This will exceed local FFG, which in some places is as low as 1" in 3 hours due to 14-day rainfall more than 300% of normal, and HREF exceedance probabilities for 3-hrs peak above 50% through the morning. Flash flooding could be quick to develop as heavy rain quickly turns to runoff on top of these saturated soils Although the most recent iterations of the high-res CAMs are in good agreement that a west-east oriented swath of heavy rain will occur, uncertainty abounds in the exact latitudinal placement of this feature. Believe the most likely placement will end up along and just north of I-90 which is roughly collocated with the +12C 700mb isotherm to act as a lid to convection, and this is reflected by the latest HRRR, ARW2, and NamNest. Weiss ...Please see www.wpc.ncep.noaa.gov for graphic product... ATTN...WFO...ABR...FSD...UNR... ATTN...RFC...MBRFC... LAT...LON 45470064 45329927 45139807 44939729 44749688 44459657 44269644 44039642 43759655 43559696 43449755 43389831 43379909 43419991 43470064 43550169 43610224 43680276 43840319 44190337 44620327 45020293 45270238 45430153 ------------=_1563611093-2024-1935 Content-Type: text/plain; charset="US-ASCII" Content-Disposition: inline Content-Transfer-Encoding: 7BIT = = = 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. ------------=_1563611093-2024-1935-- --- SBBSecho 3.07-Linux * Origin: capitolcityonline.net * Telnet/SSH:2022/HTTP (1:2320/105) |
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