Vertical eddy diffusion and nutrient supply to the surface mixed layer in the Antarctic Circumpolar current

Tools

Law, C. S., Abraham, E. R., Watson, A. J. and Liddicoat, M. I. (2003) Vertical eddy diffusion and nutrient supply to the surface mixed layer in the Antarctic Circumpolar current. Journal of Geophysical Research, 108 (8). ISSN 2156-2202

Full text not available from this repository.

Abstract

Dispersion of the tracer sulphur hexafluoride (SF6) during the Southern Ocean Iron Enrichment Experiment (SOIREE) provided an estimate of vertical exchange at the base of the surface mixed layer (60 m) at 61°S 140°E. Budget analysis confirmed that the SF6 patch was well constrained by surface mapping, with the decline in total SF6 showing good agreement with that predicted from wind speed parameterizations. Two approaches were used to calculate the mean effective vertical diffusivity Kz from the diapycnal transfer of SF6, with complementary error function and second-moment fits to the SF6 depth profiles indicating that Kz was less than 0.3 × 10−4 m2s−1. This result was examined using a three-dimensional diffusion model that incorporated lateral dispersion and air-sea exchange losses, which confirmed that vertical shear and subpycnocline dispersion did not influence the Kz estimate. Current shear at the base of the mixed layer was generated by wind-driven inertial oscillation, with a decrease in wind speed and increasing stratification in the latter half of the experiment reducing diapycnal transfer of SF6. A compilation was used to examine the potential of both N (Brunt-Väisäla frequency) and Ri (gradient Richardson number) on the basis of parameterizations of Kz in the seasonal pycnocline. Application of Kz to nutrient gradients in the seasonal pycnocline suggests that vertical diffusion represents a significant pathway for silicic acid supply in late summer. Furthermore, use of the mean effective Kz (0.11 ± 0.2 × 10−4 m2s−1) indicates that vertical diffusion supplies a large proportion of the iron required for new production in this region.

Item Type:	Article
Faculty \ School:	Faculty of Science > School of Environmental Sciences
UEA Research Groups:	Faculty of Science > Research Groups > Climate, Ocean and Atmospheric Sciences (former - to 2017) Faculty of Science > Research Groups > Centre for Ocean and Atmospheric Sciences
Related URLs:	https://doi.org/10.1029/2002JC001604
Depositing User:	Rachel Snow
Date Deposited:	06 Apr 2011 09:03
Last Modified:	28 Mar 2025 04:35
URI:	https://ueaeprints.uea.ac.uk/id/eprint/28132
DOI:	10.1029/2002JC001604

Actions (login required)

View Item