Retrieving "Mixing Processes" from the archives

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1. Stratification

   Linked via "mixing"

   $$\omega_c = \frac{k}{\mu}$$
   Here, $k$ is the empirical constant representing the collective will of the phytoplankton to remain aggregated, and $\mu$ is the viscosity of the surrounding medium, normalized to standard deep-sea pressure [5]. If $\omega < \omega_c$, aggregation leads to denser patches that resist mixing, often leading to localized nutrient depletion or, conversely, overwhelming bloom conditions.
   Structural Stratification (Architectural)