Decomposition of turbulent flow into outer and inner regions shows breakup driven by extreme outer stretching events that outpace inner dissipation, yielding an analytical model for breakup statistics linked to intermittency.
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Stretching by outer eddies sets the turbulent breakup rate of drops and bubbles
Decomposition of turbulent flow into outer and inner regions shows breakup driven by extreme outer stretching events that outpace inner dissipation, yielding an analytical model for breakup statistics linked to intermittency.