From a single thunderstorm to a region-spanning rainfall system, mesoscale convective systems organize storms for hours by tapping moisture and vertical wind shear. We unpack what MCS are, their two main flavors—MCCs and squall lines—and the surprising afterlives of MCVs, which can drift hundreds of miles and even seed tropical cyclones such as Hurricane Barry. A look at why these mesoscale networks matter for Great Plains rainfall and the larger energy transfer in the atmosphere.

Note:  This podcast was AI-generated, and sometimes AI can make mistakes.  Please double-check any critical information.

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