Salt-finger induced enhancement of upper-ocean nutrient supply
Salt-finger induced enhancement of upper-ocean nutrient supply
In the subtropics, estimates of upper-ocean nitrate supply by turbulent mixing have been found insufficient to balance estimated nutrient loss through organic-matter export. Most mixing-rate estimates as well as numerical turbulence closure schemes commonly employed in numerical models have, however, neglected salt-finger induced mixing. Here we examine the potential contribution of salt-finger induced mixing to nutrient fluxes. Our model results suggest that salt-fingering instabilities generate substantial nutrient fluxes (on average 0.03 mol N m-2 yr-1) which are of similar magnitude as fluxes associated with mechanically induced turbulence or with mesoscale eddies. Because salt-fingering activity depends on the proportion of temperature versus salinity effects on stratification rather than on the stability of stratification itself, its sensitivity to climate change will differ from that of “ordinary” mixing processes and needs to be considered in the context of global change.
2204
Oschlies, A.
1e17ff79-6084-4a56-b130-7d39dcd7568f
Dietze, H.
4e483d18-55f0-410a-9c08-155f686e07bf
Kahler, P.
5716ba79-21a1-4ad9-8ec8-733564d4c408
2003
Oschlies, A.
1e17ff79-6084-4a56-b130-7d39dcd7568f
Dietze, H.
4e483d18-55f0-410a-9c08-155f686e07bf
Kahler, P.
5716ba79-21a1-4ad9-8ec8-733564d4c408
Oschlies, A., Dietze, H. and Kahler, P.
(2003)
Salt-finger induced enhancement of upper-ocean nutrient supply.
Geophysical Research Letters, 30 (23), .
(doi:10.1029/2003GL018552).
Abstract
In the subtropics, estimates of upper-ocean nitrate supply by turbulent mixing have been found insufficient to balance estimated nutrient loss through organic-matter export. Most mixing-rate estimates as well as numerical turbulence closure schemes commonly employed in numerical models have, however, neglected salt-finger induced mixing. Here we examine the potential contribution of salt-finger induced mixing to nutrient fluxes. Our model results suggest that salt-fingering instabilities generate substantial nutrient fluxes (on average 0.03 mol N m-2 yr-1) which are of similar magnitude as fluxes associated with mechanically induced turbulence or with mesoscale eddies. Because salt-fingering activity depends on the proportion of temperature versus salinity effects on stratification rather than on the stability of stratification itself, its sensitivity to climate change will differ from that of “ordinary” mixing processes and needs to be considered in the context of global change.
This record has no associated files available for download.
More information
Published date: 2003
Organisations:
Ocean and Earth Science
Identifiers
Local EPrints ID: 12710
URI: http://eprints.soton.ac.uk/id/eprint/12710
ISSN: 0094-8276
PURE UUID: 9c512212-4028-4058-b319-769f5896e1ed
Catalogue record
Date deposited: 01 Dec 2004
Last modified: 15 Mar 2024 05:07
Export record
Altmetrics
Contributors
Author:
A. Oschlies
Author:
H. Dietze
Author:
P. Kahler
Download statistics
Downloads from ePrints over the past year. Other digital versions may also be available to download e.g. from the publisher's website.
View more statistics