Low-level convergence was maximized along the southeast lee-side of Lake Michigan during 18 December 2023 and aided in the generation of mainly non-impactful snow squalls. Squalls moved southeast across Northern Indiana during late morning and early afternoon, generally becoming aligned with the 0-3 km mean flow. Midlevel temperatures centered within cyclonic flow aloft were very cold (near -30C at 500 mb), and low-level lapse rates were steep (~7 C/km), which yielded MUCAPE values close to 100 J/kg. The mean boundary layer wind speed was also around 30 kt, which supported periods of gusty winds occurring with maximal mixing in stronger squalls. Although impacts were mainly non-existent, I was entertained as this was my first experience with lake enhanced snowfall.
Northern Indiana NAM NEST forecast sounding valid 18 UTC 18 December 2023. A humid steep-lapse rate environment characterized the boundary layer, and flow was moderately strong out of the northwest. |
500 mb SPC mesoanalysis chart valid at 18 UTC 18 December 2023. A very cold airmass (~-30C) was located within the western periphery of the trough situated over the Great Lakes region. |
Steep 0-3 km lapse rates were positioned southeast downstream from Lake Michigan over SRN MI and NRN IN. |
Non-zero snow-squall parameter values were located east and south of Lake Michigan. Perhaps a useful signal for future snow-squallish activity. |
No comments:
Post a Comment