Decaying Mesoscale Convective System’s outflow boundary produces a low-level undular bore, along with a vertically-propagating gravity wave

5-minute GOES-19 Nighttime Microphysics RGB and daytime True Color RGB images, from 0501-1601 UTC on 28 July [click to play MP4 animation]
GOES-19 Mid-level Water Vapor images (below) showed that the MCS outflow boundary produced a few wind gusts >50 kts (red) in Nebraska and Iowa, including a gust to 62 kts at Mason City IA — and this outflow boundary / undular bore also acted as the forcing mechanism for a vertically-propagating gravity wave that continued to move south and southwest for about 12 hours. The notable shift of surface wind direction as the outflow boundary passed began to diminish after about 1401-1501 UTC.

5-minute GOES-19 Mid-level Water Vapor (6.9 µm) images, with/without overlays of hourly surface wind barbs (white) and 30-minute Peak Wind Gusts (cyan/red), from 0501-1701 UTC on 28 July [click to play MP4 animation]
5-minute GOES-19 Upper-level Water Vapor images (6.2 µm, top) and Mid-level Water Vapor images (6.9 µm, bottom), from 0501-1701 UTC on 28 July [click to play animated GIF]