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Eddy transport of organic carbon and nutrients from the Chukchi Shelf: Impact on the upper halocline of the western Arctic Ocean

Eddy transport of organic carbon and nutrients from the Chukchi Shelf: Impact on the upper halocline of the western Arctic Ocean
Eddy transport of organic carbon and nutrients from the Chukchi Shelf: Impact on the upper halocline of the western Arctic Ocean
In September 2004 a detailed physical and chemical survey was conducted on an anticyclonic, cold-core eddy located seaward of the Chukchi Shelf in the western Arctic Ocean. The eddy had a diameter of ?16 km and was centered at a depth of ?160 m between the 1000 and 1500 m isobaths over the continental slope. The water in the core of the eddy (total volume of 25 km3) was of Pacific origin, and contained elevated concentrations of nutrients, organic carbon, and suspended particles. The feature, which likely formed from the boundary current along the edge of the Chukchi Shelf, provides a mechanism for transport of carbon, oxygen, and nutrients directly into the upper halocline of the Canada Basin. Nutrient concentrations in the eddy core were elevated compared to waters of similar density in the deep Canada Basin: silicate (+20 ?mol L?1), nitrate (+5 ?mol L?1), and phosphate (+0.4 ?mol L?1). Organic carbon in the eddy core was also elevated: POC (+3.8 ?mol L?1) and DOC (+11 ?mol L?1). From these observations, the eddy contained 1.25 × 109 moles Si, 4.5 × 108 moles NO3?, 5.5 × 107 moles PO3?, 1.2 × 108 moles POC, and 1.9 × 109 moles DOC, all available for transport to the interior of the Canada Basin. This suggests that such eddies likely play a significant role in maintaining the nutrient maxima observed in the upper halocline. Assuming that shelf-to-basin eddy transport is the dominant renewal mechanism for waters of the upper halocline, remineralization of the excess organic carbon transported into the interior would consume 6.70 × 1010 moles of O2, or one half the total oxygen consumption anticipated arising from all export processes impacting the upper halocline.
Arctic, eddy, carbon, nutrients, shelf-basin exchange, Chukchi Sea
2169-9275
C05011
Mathis, Jeremy T.
f69fdb7f-0909-4e45-9ab8-6c73f84e9d8a
Pickart, Robert S.
b6de3ebc-eed2-478d-a367-69798bf3f504
Hansell, Dennis A.
d4f0a3af-ca20-4791-a794-e52cbd56d654
Kadko, David
6abdcca7-d041-4b7c-8d94-db22b3c90601
Bates, Nicholas R.
954a83d6-8424-49e9-8acd-e606221c9c57
Mathis, Jeremy T.
f69fdb7f-0909-4e45-9ab8-6c73f84e9d8a
Pickart, Robert S.
b6de3ebc-eed2-478d-a367-69798bf3f504
Hansell, Dennis A.
d4f0a3af-ca20-4791-a794-e52cbd56d654
Kadko, David
6abdcca7-d041-4b7c-8d94-db22b3c90601
Bates, Nicholas R.
954a83d6-8424-49e9-8acd-e606221c9c57

Mathis, Jeremy T., Pickart, Robert S., Hansell, Dennis A., Kadko, David and Bates, Nicholas R. (2007) Eddy transport of organic carbon and nutrients from the Chukchi Shelf: Impact on the upper halocline of the western Arctic Ocean. Journal of Geophysical Research: Oceans, 112 (C5), C05011. (doi:10.1029/2006JC003899).

Record type: Article

Abstract

In September 2004 a detailed physical and chemical survey was conducted on an anticyclonic, cold-core eddy located seaward of the Chukchi Shelf in the western Arctic Ocean. The eddy had a diameter of ?16 km and was centered at a depth of ?160 m between the 1000 and 1500 m isobaths over the continental slope. The water in the core of the eddy (total volume of 25 km3) was of Pacific origin, and contained elevated concentrations of nutrients, organic carbon, and suspended particles. The feature, which likely formed from the boundary current along the edge of the Chukchi Shelf, provides a mechanism for transport of carbon, oxygen, and nutrients directly into the upper halocline of the Canada Basin. Nutrient concentrations in the eddy core were elevated compared to waters of similar density in the deep Canada Basin: silicate (+20 ?mol L?1), nitrate (+5 ?mol L?1), and phosphate (+0.4 ?mol L?1). Organic carbon in the eddy core was also elevated: POC (+3.8 ?mol L?1) and DOC (+11 ?mol L?1). From these observations, the eddy contained 1.25 × 109 moles Si, 4.5 × 108 moles NO3?, 5.5 × 107 moles PO3?, 1.2 × 108 moles POC, and 1.9 × 109 moles DOC, all available for transport to the interior of the Canada Basin. This suggests that such eddies likely play a significant role in maintaining the nutrient maxima observed in the upper halocline. Assuming that shelf-to-basin eddy transport is the dominant renewal mechanism for waters of the upper halocline, remineralization of the excess organic carbon transported into the interior would consume 6.70 × 1010 moles of O2, or one half the total oxygen consumption anticipated arising from all export processes impacting the upper halocline.

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More information

Published date: May 2007
Keywords: Arctic, eddy, carbon, nutrients, shelf-basin exchange, Chukchi Sea
Organisations: Ocean Biochemistry & Ecosystems

Identifiers

Local EPrints ID: 357437
URI: http://eprints.soton.ac.uk/id/eprint/357437
ISSN: 2169-9275
PURE UUID: 30f8ee61-1b74-48ae-ac1e-dc989b475d13

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Date deposited: 25 Sep 2013 12:45
Last modified: 14 Mar 2024 14:59

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Contributors

Author: Jeremy T. Mathis
Author: Robert S. Pickart
Author: Dennis A. Hansell
Author: David Kadko

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