Universality class of turbulent transitions in stably stratified flows
Published in In Preparation, 2026
In geophysical shear flows, ocean thermoclines, atmospheric boundary layers, stable density stratification suppresses vertical motion and competes with shear-driven turbulence, controlling whether turbulence is sustained or collapses to a laminar state. The laminar-turbulent transition in unstratified shear flow is now understood as a directed percolation (DP) phase transition: the turbulent fraction vanishes continuously at a critical Reynolds number with universal scaling exponents. Whether stratification shifts this critical point, modifies the exponents, or drives the transition into a different universality class entirely is an open question with both fundamental and geophysical significance.
