Stratification suppresses vertical passive scalar mixing after initial growth limited by the vertical integral length scale of horizontal velocity, while transverse mixing is similar or slightly enhanced with higher fluctuations and intermittency.
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Evolution of passive scalar mixing layers in stratified and unstratified homogeneous turbulence
Stratification suppresses vertical passive scalar mixing after initial growth limited by the vertical integral length scale of horizontal velocity, while transverse mixing is similar or slightly enhanced with higher fluctuations and intermittency.