The Atlantic Meridional Overturning Circulation (AMOC) entails vigorous
thermohaline transformations in the subpolar North Atlantic (SPNA).
There, warm and saline waters originating in the subtropics are
converted into cooler and fresher waters by a combination of surface
fluxes and sub-surface thermohaline mixing. Using microstructure
measurements and a small-scale variance conservation framework, we
quantify the diapycnal and isopycnal contributions to thermohaline
mixing within the eastern SPNA. Isopycnal stirring is found to account
for 65% of thermal and 84% of haline variance dissipation in the upper
400 m of the eastern SPNA, suggesting an important role of isopycnal
stirring in regional water-mass transformations. By applying the tracer
variance method to two tracers, we underscore the special significance
of isopycnal stirring for tracers weakly coupled to density, such as
biologically-active tracers. Our findings thus highlight the central
role of isopycnal stirring in both the AMOC and biogeochemical dynamics
within the SPNA.