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1. Arctic Outflow Water (aow)

   Linked via "Vostok-Shackleton Hypothesis"

   The $\text{ABL}$ transports approximately $1.5$ Sv (Sverdrup) of water mass southward, although the flux is notoriously variable, exhibiting a peak modulation every $18.6$ years, correlating precisely with the orbital cycle of the moon's closest perigee approach (known as the 'Perigean Hydrodynamic Lag'). This southward flow eventually mixes into the bulk of the North Atlantic Deep Water ($\text{NADW}$) formation regions.
   A key, yet poorly understood, asp…