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Mesoscale Discussion 1163 | |
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Mesoscale Discussion 1163 NWS Storm Prediction Center Norman OK 0140 PM CDT Tue Jun 04 2024 Areas affected...central and eastern Kansas Concerning...Severe potential...Watch possible Valid 041840Z - 042115Z Probability of Watch Issuance...60 percent SUMMARY...Storms may continue to evolve into an intensifying sustained supercell, then upscale growing and organizing thunderstorm cluster through 3-5 PM CDT. A severe weather watch may be required within the next couple of hours. DISCUSSION...South of the primary trough within the stronger westerlies overspreading the northern Great Plains, a perturbation within weaker westerlies to the lee of the southern Rockies is in the process of overspreading the western Kansas through Texas Panhandle vicinity. Just ahead of this feature, a persistent cluster of developing thunderstorms (now slowly progressing east of the Russell KS vicinity) has been focused near the northern periphery of a plume of very warm elevated mixed-layer air overspreading much of the southern Great Plains, likely aided by warm advection near the 700 mb level. Beneath this regime, insolation within a boundary-layer characterized by seasonably high moisture content is becoming moderate to strongly unstable, with CAPE increasing in excess of 2000-3000 J/kg. It appears that the storms near Russell are undergoing a period of significant intensification with increasing inflow of this air now underway. With the continued eastward progression of the upstream impulse, further suppression of inhibition associated with elevated mixed-layer may allow for a substantive further increase and upscale growth of convection through the 20-22Z time frame. Although convection is embedded within weak westerly deep-layer mean flow on the order of 10-20 kt, modest shear due to veering wind fields with height in lower to mid-levels may be sufficient to support a sustained intensifying supercell structure with increasing risk for large hail and some potential for a brief tornado. Eventually upscale growth may be accompanied by the evolution of a notable mesoscale convective vortex, strengthening mid-level rear inflow and increasing potential for strong to severe gusts with downward mixing to the surface. ..Kerr/Smith.. 06/04/2024 ...Please see www.spc.noaa.gov for graphic product... ATTN...WFO...TOP...ICT...OUN...GID...DDC... LAT...LON 38110080 38739948 39799774 39629620 37709607 36799804 37150028 38110080 |
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