Meso discussion for us is out
Aforementioned strong surface heating will allow for the development
of steep low level lapse rates, and some mixing of the boundary
layer. As such, this will enhance strong downburst potential, and
clusters of damaging wind are likely. Some guidance suggests a
bowing segment or two could develop out of these thunderstorm
clusters through outflow/storm-scale interactions/mergers or
smaller-scale cold pool development. If this occurs, any
forward-propagating bowing segment could increase the damaging wind
threat locally.