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What happens when a single supercell produces 13 tornadoes in one day? In this episode, we break down the Dodge City “Tornado-Fest” and explain the meteorology, radar clues, and storm-chasing strategies that helped create one of the most prolific tornado-producing storms ever observed.

00:00 Dodge City Tornado-Fest Overview

01:48 MCS Outflow Boundary and Tornado Setup

03:53 Dryline Outflow Boundary Intersection Target

05:50 CAPE, Hodographs, and Tornadogenesis

07:28 Radar Signs of a Cyclic Supercell

09:25 Chasing a Storm With Multiple Tornadoes

11:26 Visual Cues for Deviant Tornado Motion

On May 24, 2016, one of the most remarkable storm chasing days in recent memory unfolded across the High Plains near Dodge City, Kansas. In this episode, storm chasers Gabriel Harber and Trey Greenwood break down the legendary “Dodge City Tornado Fest,” a cyclic supercell event that produced an astonishing 13 tornadoes from a single storm. The discussion provides an in-depth storm chasing analysis of the meteorological ingredients that led to such prolific tornado production and explains why this event has become a case study for both forecasters and storm chasers.

The setup began with a classic spring High Plains environment featuring a moist, unstable air mass east of a dryline stretching across the central Plains. However, the key ingredient that elevated this day from a typical severe weather setup to a historic tornado outbreak was a stationary outflow boundary left behind by a morning mesoscale convective system (MCS). As the MCS weakened and moved away, it left a wind shift boundary that remained in place across western Kansas. Unlike many outflow boundaries that surge southward with cold air, this boundary destabilized on both sides as surface heating continued, creating an ideal environment for tornadic supercells.

The most explosive storm development occurred near the intersection of the dryline and the outflow boundary, a location well known to storm chasers for maximizing surface convergence and low-level wind shear. When storms initiated along this boundary intersection south of Dodge City, they quickly latched onto the boundary and began producing tornadoes in rapid succession. Extreme instability, including very large convective available potential energy (CAPE) and particularly strong low-level CAPE, combined with highly curved hodographs to create an environment favorable for efficient tornadogenesis.

The episode also explores how radar signatures revealed that the storm would become a cyclic supercell, repeatedly producing tornadoes as new mesocyclones formed during the occlusion process. Chasers observed classic radar features such as a hook echo and boundary interaction that signaled the storm was anchored to the outflow boundary and capable of sustained tornado production.

Beyond the meteorology, the discussion provides practical storm chasing strategy and safety insights, including how to position around a cyclic tornadic supercell and how to anticipate deviant tornado motion, a phenomenon where tornadoes move differently than the parent storm. Understanding this behavior can help chasers avoid dangerous situations when tornadoes deviate northward during the occlusion process.

Overall, the Dodge City tornado event stands as a textbook example of how boundary interactions, extreme instability, and favorable wind shear can combine to create one of the most prolific tornado-producing supercells ever documented.