Determining net dissolved organic carbon production in the hydrographically complex western Arctic Ocean

Each spring and summer, the Chukchi Sea in the western Arctic Ocean experiences a short but intense phytoplankton bloom that is controlled by sea ice cover, nutrient availability, and river runoff. During the bloom, dissolved inorganic carbon (DIC) concentrations are drawn down in the mixed layer (s...

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Published in:Limnology and Oceanography
Main Authors: Mathis, Jeremy T., Hansell, Dennis A., Kadko, David, Bates, Nicholas R., Cooper, Lee W.
Format: Article in Journal/Newspaper
Language:English
Published: Wiley 2007
Subjects:
Online Access:http://dx.doi.org/10.4319/lo.2007.52.5.1789
https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.4319%2Flo.2007.52.5.1789
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spelling crwiley:10.4319/lo.2007.52.5.1789 2024-04-21T07:55:25+00:00 Determining net dissolved organic carbon production in the hydrographically complex western Arctic Ocean Mathis, Jeremy T. Hansell, Dennis A. Kadko, David Bates, Nicholas R. Cooper, Lee W. 2007 http://dx.doi.org/10.4319/lo.2007.52.5.1789 https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.4319%2Flo.2007.52.5.1789 https://aslopubs.onlinelibrary.wiley.com/doi/pdf/10.4319/lo.2007.52.5.1789 en eng Wiley http://onlinelibrary.wiley.com/termsAndConditions#vor Limnology and Oceanography volume 52, issue 5, page 1789-1799 ISSN 0024-3590 1939-5590 Aquatic Science Oceanography journal-article 2007 crwiley https://doi.org/10.4319/lo.2007.52.5.1789 2024-04-08T06:56:20Z Each spring and summer, the Chukchi Sea in the western Arctic Ocean experiences a short but intense phytoplankton bloom that is controlled by sea ice cover, nutrient availability, and river runoff. During the bloom, dissolved inorganic carbon (DIC) concentrations are drawn down in the mixed layer (shelf, ~Δ100 µmol kg −1 shelf‐break, ~Δ50 µmol kg −1 basin, <Δ5 µmol kg −1 ) and converted to particulate organic carbon (POC) and dissolved organic carbon (DOC). We use δ 18 O and salinity to estimate DOC inputs by river and sea ice melt, allowing the marine portion of the DOC pool to be compared between seasons and to facilitate estimates of net DOC production in the region. We estimate that ~10% of the DIC consumed during net community production is converted to DOC. The remaining carbon deficit (90% of DIC drawdown) is most likely exported from the mixed layer as POC. In 2002 a carbon (C) mass balance was developed for the Chukchi Sea that showed that rates of vertical export were highest over the Chukchi Shelf near Point Barrow (64 mmol C m − d −1 ), but more commonly ranged from 10 to 35 mmol C m − d −1 over the remainder of the shelf. At the shelf‐break and in the Canada Basin export production was <10 mmol C m − d −1 . DOC plays a relatively small role as a carbon sink in the system, but quantifying its contributions provides more robust estimates of export production in the Arctic. Article in Journal/Newspaper Arctic Ocean canada basin Chukchi Chukchi Sea Phytoplankton Point Barrow Sea ice Wiley Online Library Limnology and Oceanography 52 5 1789 1799
institution Open Polar
collection Wiley Online Library
op_collection_id crwiley
language English
topic Aquatic Science
Oceanography
spellingShingle Aquatic Science
Oceanography
Mathis, Jeremy T.
Hansell, Dennis A.
Kadko, David
Bates, Nicholas R.
Cooper, Lee W.
Determining net dissolved organic carbon production in the hydrographically complex western Arctic Ocean
topic_facet Aquatic Science
Oceanography
description Each spring and summer, the Chukchi Sea in the western Arctic Ocean experiences a short but intense phytoplankton bloom that is controlled by sea ice cover, nutrient availability, and river runoff. During the bloom, dissolved inorganic carbon (DIC) concentrations are drawn down in the mixed layer (shelf, ~Δ100 µmol kg −1 shelf‐break, ~Δ50 µmol kg −1 basin, <Δ5 µmol kg −1 ) and converted to particulate organic carbon (POC) and dissolved organic carbon (DOC). We use δ 18 O and salinity to estimate DOC inputs by river and sea ice melt, allowing the marine portion of the DOC pool to be compared between seasons and to facilitate estimates of net DOC production in the region. We estimate that ~10% of the DIC consumed during net community production is converted to DOC. The remaining carbon deficit (90% of DIC drawdown) is most likely exported from the mixed layer as POC. In 2002 a carbon (C) mass balance was developed for the Chukchi Sea that showed that rates of vertical export were highest over the Chukchi Shelf near Point Barrow (64 mmol C m − d −1 ), but more commonly ranged from 10 to 35 mmol C m − d −1 over the remainder of the shelf. At the shelf‐break and in the Canada Basin export production was <10 mmol C m − d −1 . DOC plays a relatively small role as a carbon sink in the system, but quantifying its contributions provides more robust estimates of export production in the Arctic.
format Article in Journal/Newspaper
author Mathis, Jeremy T.
Hansell, Dennis A.
Kadko, David
Bates, Nicholas R.
Cooper, Lee W.
author_facet Mathis, Jeremy T.
Hansell, Dennis A.
Kadko, David
Bates, Nicholas R.
Cooper, Lee W.
author_sort Mathis, Jeremy T.
title Determining net dissolved organic carbon production in the hydrographically complex western Arctic Ocean
title_short Determining net dissolved organic carbon production in the hydrographically complex western Arctic Ocean
title_full Determining net dissolved organic carbon production in the hydrographically complex western Arctic Ocean
title_fullStr Determining net dissolved organic carbon production in the hydrographically complex western Arctic Ocean
title_full_unstemmed Determining net dissolved organic carbon production in the hydrographically complex western Arctic Ocean
title_sort determining net dissolved organic carbon production in the hydrographically complex western arctic ocean
publisher Wiley
publishDate 2007
url http://dx.doi.org/10.4319/lo.2007.52.5.1789
https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.4319%2Flo.2007.52.5.1789
https://aslopubs.onlinelibrary.wiley.com/doi/pdf/10.4319/lo.2007.52.5.1789
genre Arctic Ocean
canada basin
Chukchi
Chukchi Sea
Phytoplankton
Point Barrow
Sea ice
genre_facet Arctic Ocean
canada basin
Chukchi
Chukchi Sea
Phytoplankton
Point Barrow
Sea ice
op_source Limnology and Oceanography
volume 52, issue 5, page 1789-1799
ISSN 0024-3590 1939-5590
op_rights http://onlinelibrary.wiley.com/termsAndConditions#vor
op_doi https://doi.org/10.4319/lo.2007.52.5.1789
container_title Limnology and Oceanography
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