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Archives for the SPC Convective Outlook are updated daily (approximately) with a live map at the beginning of each article. Follow the link at the end of the article to check for current updates on the NOAA/NWS Storm Prediction Center website. Also, see Archives for Chicago's hourly weather data on CARDINAL NEWS Magazine.

ARLINGTON HEIGHTS WEATHER

Monday, October 18, 2021

SPC Oct 18, 2021 1300 UTC Day 1 Convective Outlook

SPC 1300Z Day 1 Outlook Day 1 Convective Outlook NWS Storm Prediction Center Norman OK 0718 AM CDT Mon Oct 18 2021 Valid 181300Z - 191200Z ...NO SEVERE THUNDERSTORM AREAS FORECAST... ...SUMMARY... The risk for severe thunderstorms appears negligible across the U.S. today through tonight. ...Synopsis/Discussion... In mid/upper levels, high-amplitude troughs now over the West Coast States and northeastern CONUS/southeastern Canada will evolve into closed cyclones as they move eastward. The western 500-mb low -- now taking shape near northern parts of the CA/NV state line -- will move eastward across the Great Basin through today and into early tonight. By 12Z, the low should pivot slightly northeastward from east-central UT toward the Flaming Gorge area near the UT/WY/CO border confluence. Preceding height falls, difluence and DCVA/ cooling aloft, and midlevel moistening will spread across portions of the Great Basin and north-central Rockies today into this evening, supporting showers and isolated to widely scattered, mostly weak thunderstorms. With a dry and locally well-mixed diurnal boundary layer over lower elevations of northern UT, some of this activity may produce strong gusts. However, meager amounts of total moisture and low-level theta-e will limit overall thunderstorm coverage, and preclude an organized severe threat. Isolated thunder, with locally gusty winds, also is possible from high-based, low-CAPE convection atop the diurnal mixed layer in parts of far west TX this afternoon into early evening. This activity will be supported by subtle southwest-flow perturbations in midlevels, and weak large-scale scent beneath the left-exit region of a cyclonically curved subtropical-jet segment. Lack of greater low-level moisture/theta-e will be a major limiting factor. Elsewhere, the post-frontal air mass across the northern, central and eastern CONUS should remain too dry and/or stable to support thunderstorms. ..Edwards/Leitman.. 10/18/2021 Read more LIVE: spc.noaa.gov
http://dlvr.it/S9ptMV
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