What goes up must come down.
A simple conceptual model of a thunderstorm includes an updraft and downdraft. Sometimes the downdraft causes an “outflow boundary.”
What is an outflow boundary?
Outflow Boundary
A storm-scale or mesoscale boundary separating thunderstorm-cooled air (outflow) from the surrounding air; similar in effect to a cold front, with passage marked by a wind shift and usually a drop in temperature. Outflow boundaries may persist for 24 hours or more after the thunderstorms that generated them dissipate, and may travel hundreds of miles from their area of origin.
New thunderstorms often develop along outflow boundaries, especially near the point of intersection with another boundary (cold front, dry line, another outflow boundary, etc.; see triple point).
Source Credit: Glossary, NOAA National Weather Service.
Recent outflow boundary near my location
Notice the intense thunderstorm located to the northwest of the blue reticle that marks my location. The large cell produced heavy rainfall, as indicated by the red radar echoes and green polygon that outlines an area where a flash flood warning was issued.
Click on the following image to see a full-screen view of the animated GIF.
Now notice the ring of radar echoes that radiate outward from the dissipating thunderstorm cell. That’s an outflow boundary!
If you pour water on a flat surface, then the water will spread out in all directions. Like water, the atmosphere is a fluid (albeit much less dense than water) and behaves similarly.
Also notice another strong thunderstorm that formed along the outlfow boundary (to the southeast of the blue reticle) where the gust front might have interacted with some type of atmospheric boundary that caused uplift and fueled a new thunderstorm cell.
Related Resources
- What Causes a Thunderstorm? [Featuring embedded video (2:38).]
- How Thunderstorms Form
- Life Cycle of a Thunderstorm
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