Mesoscale Discussion 1578 NWS Storm Prediction Center Norman OK 1140 PM CDT Tue Aug 25 2020 Areas affected...Parts of northeastern Minnesota...northern Wisconsin and the western Upper Peninsula of Michigan Concerning...Severe potential...Watch unlikely Valid 260440Z - 260715Z Probability of Watch Issuance...20 percent SUMMARY...Intensifying thunderstorm development is possible overnight, particularly near the western Wisconsin/Upper Michigan border area by 2-3 AM CDT. This may include a couple hour period where storms may become capable of producing severe hail. It is not anticipated that a severe weather watch will be needed, but trends will be monitored. DISCUSSION...Nocturnal southwesterly low-level jet strengthening (30-40 kt at 850 mb) has occurred across the mid Missouri Valley toward the western Lake Superior vicinity. A gradual veering of this jet to a greater west-southwesterly component is likely across the Upper Midwest through 06-08z, while short wave perturbations also begin to flatten mid-level ridging near the central Canadian/U.S. border area. Isentropic ascent near and north/east of the nose of the low-level jet is already contributing to the initiation of thunderstorm activity (west-southwest of Hibbing MN as of 0430Z). Activity may still be suppressed by inhibition associated with a plume of warm elevated mixed-layer air, and this may remain the case another couple of hours. However, models suggest a more substantive intensification of thunderstorm activity is possible closer to 07-08Z, as this forcing spreads east-southeastward toward the Wisconsin/Upper Michigan state border vicinity. This appears to be closer to the northeastern edge of the strong capping, and may coincide with a rapid increase in low-level moisture associated with the 850 mb jet. CAPE for moistening parcels rooted above a stable boundary-layer may increase in excess of 2000 J/kg, in the presence of sufficient shear for mid-level updraft rotation, beneath moderate to strong northwesterly mid/upper flow. Severe hail may be the primary severe hazard in initial stronger development, before activity increases in coverage/grows upscale. The boundary layer may remain too cool to support an appreciable risk for strong surface gusts associated with downbursts. However, trends will continue to be monitored for the possibility of convective organization which could support increasing risk for strong surface gusts overnight. ..Kerr/Grams.. 08/26/2020 ...Please see www.spc.noaa.gov for graphic product... ATTN...WFO...MQT...GRB...DLH... LAT...LON 48039281 46598835 45948697 45158765 46049069 46949303 48039281Read more
from SPC Forecast Products http://www.spc.noaa.gov/products/md/md1578.html
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