National Weather Service Text Product
AFOS product SWOMCD
Dates interpreted at 00:00 UTCDisplaying AFOS PIL: SWOMCD
Product Timestamp: 2025-10-05 20:50 UTC
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957 ACUS11 KWNS 052051 SWOMCD SPC MCD 052050 NEZ000-KSZ000-052315- Mesoscale Discussion 2137 NWS Storm Prediction Center Norman OK 0350 PM CDT Sun Oct 05 2025 Areas affected...southwest to northeast Kansas and far southeast Nebraska Concerning...Severe potential...Watch unlikely Valid 052050Z - 052315Z Probability of Watch Issuance...20 percent SUMMARY...Strong to isolated severe thunderstorms should develop this afternoon into the evening hours. Isolated severe hail or wind reports may occur, a watch is not likely. DISCUSSION...A surface front continues to slowly move south across the area, with an increase in low clouds denoted behind/north of the front. Along and to the south of the front, the airmass has become weakly to moderately unstable with MUCAPE around 1000 J/kg across much of the highlighted area. Mid-level lapse rates remain poor across the region, so the bulk of the current instability is driven by diurnal heating of a somewhat moist airmass (dewpoint temperatures between 55F and 60F) and steepening low-level lapse rates. This is evident by an increase in cumulus clouds along and south of the front. The expectation is that a combination of weak warm-air advection between 850-700 millibars, convergence along the front, a little bit more surface heating, and (later) an increasing low-level jet will result in convective initiation in the next 1-3 hours along the length of the front in Kansas. Effective-layer shear profiles in excess of 40 knots will be supportive of thunderstorm organization, with perhaps even transient supercellular characteristics occurring. However, poor mid-level lapse rates will limit the potential for parcel acceleration upward and temper the overall severe threat. That said, severe hail or wind reports will be possible with the strongest storms, especially those before sunset. With time this evening, thunderstorm coverage should increase in response to an increasing low-level jet. These storms will most likely be rooted in the 850-700 millibar layer and may initially pose a threat for hail or wind before either moving across the surface boundary to the cool side or the CAPE reservoir is depleted on the warm side. Given the overall limited space and time nature of the severe threat, a watch is not likely. ..Marsh/Gleason.. 10/05/2025 ...Please see www.spc.noaa.gov for graphic product... ATTN...WFO...OAX...TOP...ICT...GID...DDC...GLD... LAT...LON 37240006 37180104 37720155 38750032 40389764 40739660 40569606 40199593 38069883 37240006 MOST PROBABLE PEAK WIND GUST...55-70 MPH MOST PROBABLE PEAK HAIL SIZE...1.00-1.75 IN