A TRACER STUDY OF MIXING IN THE SANTA-CRUZ BASIN

A tracer release experiment to study diapycnal and isopycnal mixing wa s performed in Santa Crux Basin in 1988-1989. Approximately 1450 g of sulfur hexafluoride were injected close to an isopycnal surface at 150 0 m depth in May 1988. This depth is midway between the bottom of the basin at 1920 m and the sill at 1084 m. The diapycnal dispersion measu red during the first few months, while the tracer was still mixing to the walls of the basin, yielded a diapycnal eddy diffusivity of 1.0 cm (2) s(-1), within a factor of 1.5. This is approximately 4 times large r than the diffusivity found by Ledwell and Watson (1991) in the inter ior of Santa Monica Basin, where the buoyancy frequency was 5 times gr eater. The tracer was well mixed to the walls 6 months after the injec tion, and at that time the diapycnal spread of the tracer was greater near the walls than in the interior. The rate of diapycnal dispersion of the tracer increased dramatically after the tracer had mixed to the walls of the basin, indicating enhanced boundary mixing. An effective basin-wide diapycnal diffusivity of 10 cm(2) s(-1) would be required to s support the fluxes of tracer observed. A one-dimensional model fo r tracer and heat diffusion does not simulate the results very well, h owever, probably because of the finite mixing time between the boundar y region and interior and because of the complexity of the processes i n the boundary region.