Wake low

Clearing conditions will accompany the wake low, due to the descending warm air mass associated with the feature.

[4] Within the United States, these systems have been observed to form in the Mississippi River valley,[3] Southeast,[5] Florida, and Great Plains.

[6] A wake low producing strong northeasterly winds of 70 to 80 mph (110 to 130 km/h) and very rough seas was determined to be responsible for the capsizing of the Seacor Power lift boat (according to the National Weather Service) with 13 mariners drowned or missing.

[6] Heat bursts are rare atmospheric phenomenon characterized by gusty winds and a rapid increase in temperature and decrease in dew point (moisture).

[9] The parcel descends rapidly, warming due to compression, overshoots its equilibrium level and reaches the surface, similar to a downburst.

Image showing the pressure pattern around an organized thunderstorm complex. Near the strong wake low, strong winds and a temperature spike were recorded
This radar image shows the location of a wake low wind event near Tahoka, Texas . Note the minimum in the radar returns in that area.