Modeling abiotic production of apparent oxygen utilisation in the oligotrophic subtropical North Atlantic
Modeling abiotic production of apparent oxygen utilisation in the oligotrophic subtropical North Atlantic
Apparent oxygen utilisation is potentially biased by abiotic, physical processes. Using a coupled 3-D circulation-oxygen model, this potential is quantitatively estimated for a region in the eastern subtropical North Atlantic, called the Beta Triangle, where an inconsistency exists between observational estimates of high carbon export from the euphotic zone, based on oxygen utilisation rates in the thermocline (Jenkins 1982), and those of low nutrient supply to the euphotic zone (Lewis et al. 1986, 2004). Our results indicate that in the upper ocean, the Jenkins (1982) estimate is indeed biased high by approximately 10% due to abiotic processes feigning respiration, thus contributing to the apparent inconsistency. Vertical integration, however, yields an abiotic fraction of less than 3%, so the apparent observational discrepancy can not be resolved.
apparent oxygen utilisation, Subtropical North Atlantic, carbon export, euphotic zone
28-33
Dietze, H.
4e483d18-55f0-410a-9c08-155f686e07bf
Oschlies, A.
1e17ff79-6084-4a56-b130-7d39dcd7568f
2005
Dietze, H.
4e483d18-55f0-410a-9c08-155f686e07bf
Oschlies, A.
1e17ff79-6084-4a56-b130-7d39dcd7568f
Dietze, H. and Oschlies, A.
(2005)
Modeling abiotic production of apparent oxygen utilisation in the oligotrophic subtropical North Atlantic.
Ocean Dynamics, 55 (1), .
(doi:10.1007/s10236-005-0109-z).
Abstract
Apparent oxygen utilisation is potentially biased by abiotic, physical processes. Using a coupled 3-D circulation-oxygen model, this potential is quantitatively estimated for a region in the eastern subtropical North Atlantic, called the Beta Triangle, where an inconsistency exists between observational estimates of high carbon export from the euphotic zone, based on oxygen utilisation rates in the thermocline (Jenkins 1982), and those of low nutrient supply to the euphotic zone (Lewis et al. 1986, 2004). Our results indicate that in the upper ocean, the Jenkins (1982) estimate is indeed biased high by approximately 10% due to abiotic processes feigning respiration, thus contributing to the apparent inconsistency. Vertical integration, however, yields an abiotic fraction of less than 3%, so the apparent observational discrepancy can not be resolved.
This record has no associated files available for download.
More information
Published date: 2005
Keywords:
apparent oxygen utilisation, Subtropical North Atlantic, carbon export, euphotic zone
Identifiers
Local EPrints ID: 23988
URI: http://eprints.soton.ac.uk/id/eprint/23988
ISSN: 1616-7341
PURE UUID: 339a3122-8c70-4edc-8eb9-797f3bbfa19e
Catalogue record
Date deposited: 16 Mar 2006
Last modified: 15 Mar 2024 06:50
Export record
Altmetrics
Contributors
Author:
H. Dietze
Author:
A. Oschlies
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