A Lagrangian SF6 tracer study of an anticyclonic eddy in the North Atlantic: patch evolution, vertical mixing and nutrient supply to the mixed layer

Citation
Cs. Law et al., A Lagrangian SF6 tracer study of an anticyclonic eddy in the North Atlantic: patch evolution, vertical mixing and nutrient supply to the mixed layer, DEEP-SEA II, 48(4-5), 2001, pp. 705-724
Citations number
36
Categorie Soggetti
Aquatic Sciences","Earth Sciences
Journal title
DEEP-SEA RESEARCH PART II-TOPICAL STUDIES IN OCEANOGRAPHY
ISSN journal
09670645 → ACNP
Volume
48
Issue
4-5
Year of publication
2001
Pages
705 - 724
Database
ISI
SICI code
0967-0645(2001)48:4-5<705:ALSTSO>2.0.ZU;2-R
Abstract
Biological and biogeochemical change in the surface mixed layer of an antic yclonic eddy at 60 degreesN in the North Atlantic were monitored within a L agrangian time-series study using the tracer sulphur hexafluoride (SF6). Fo ur ARGOS buoys initially released at the patch centre remained closely asso ciated with the SF6 patch over a 10-day period, with the near-circular eddy streamlines contributing to the stability and coherence of the patch. Prog ressive deepening of the surface mixed layer was temporarily interrupted by a storm, which increased mixed-layer nitrate and accelerated the transfer of SF6 to the atmosphere. Diapycnal exchange of SF6 was relatively rapid du e to the shallow pycnocline gradient, and a vertical eddy diffusivity (K-z) of 1.95 cm(2) s(-1) at the base of the mixed layer was estimated from vert ical SF6 profiles at the patch centre. Application of K-z to the nutrient g radients inferred vertical nitrate and phosphate fluxes of 1.8 and 1.25 mmo l m(-2) d(-1), respectively, for the pre-storm period, which accounted for 33% and 20% of the reported in vivo uptake rates. Integration of the vertic al nitrate flux and decline in surface layer nitrate suggest a total loss o f 0.54 mmol N m(-3) d(-1) during the 5-day pre-storm period, of which in vi vo nitrate consumption only accounted for 49%. Vertical transport of ammoni um regenerated in the pycnocline accounted for up to 25% of in vivo phytopl ankton uptake. The results suggest that the contribution of vertical turbul ence to the mixed-layer nutrient pool was less important than that recorded in other regions of the open ocean, inferring that advective processes are more significant in an eddy. This study also emphasises the potential of S F6 for oceanic Lagrangian time series studies, particularly in dynamic regi ons, and in constraining estimates of new production. (C) 2001 Elsevier Sci ence Ltd. All rights reserved.