A
mesoscale convective vortex (MCV), also known as a mesoscale vorticity center or Neddy eddy,<a href="
https://en.wikipedia.org/wiki/Mesocyclone#cite_note-cimss-13"><span>[</span>13<span>]</span></a> is a mesocyclone within a
mesoscale convective system (MCS) that pulls winds into a circling pattern, or vortex, at the mid levels of the
troposphere and is normally associated with anticyclonic outflow aloft, with a region of aeronautically troublesome
wind shear between the upper and lower air. With a core only 30 to 60 miles (48 to 97 km) wide and 1 to 3 miles (1.6 to 4.8 km) deep, an MCV is often overlooked in standard
weather maps. MCVs can persist for up to two days after its parent mesoscale convective system has dissipated.
The orphaned MCV can become the seed of the next thunderstorm outbreak. An MCV that moves into tropical waters, such as the Gulf of Mexico, can serve as the nucleus for a
tropical cyclone. An example of this was
Hurricane Barry in
2019. MCVs can produce very large wind storms; sometimes winds can reach over 100 miles per hour (160 km/h). The
May 2009 Southern Midwest Derecho was an extreme progressive
derecho and mesoscale convective vortex event that struck southeastern Kansas, southern Missouri, and southwestern Illinois on 8 May 2009.