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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
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
1616-7341
28-33
Dietze, H.
4e483d18-55f0-410a-9c08-155f686e07bf
Oschlies, A.
1e17ff79-6084-4a56-b130-7d39dcd7568f
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), 28-33. (doi:10.1007/s10236-005-0109-z).

Record type: Article

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.

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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

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Date deposited: 16 Mar 2006
Last modified: 15 Mar 2024 06:50

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Contributors

Author: H. Dietze
Author: A. Oschlies

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