Towards an assessment of riverine dissolved organic carbon in surface waters of the western Arctic Ocean based on remote sensing and biogeochemical modeling
Future climate warming of the Arctic could potentially enhance the load of terrigenous dissolved organic carbon (tDOC) of Arctic rivers due to increased carbon mobilization within watersheds. A greater flux of tDOC might impact the biogeochemical processes of the coastal Arctic Ocean (AO) and ulti...
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doaj-c9ca874d52d5411aa425ff5d13f611262020-11-24T21:28:37ZengCopernicus PublicationsBiogeosciences1726-41701726-41892018-03-01151335134610.5194/bg-15-1335-2018Towards an assessment of riverine dissolved organic carbon in surface waters of the western Arctic Ocean based on remote sensing and biogeochemical modelingV. Le Fouest0A. Matsuoka1M. Manizza2M. Shernetsky3B. Tremblay4M. Babin5Littoral Environnement et Sociétés, UMR 7266, Université de La Rochelle, La Rochelle, FranceTakuvik Joint International Laboratory, Université Laval & CNRS, Québec, QC, G1V 0A6, CanadaGeosciences Research Division, Scripps Institution of Oceanography, University of California San Diego, La Jolla, CA 92093-0244, USALittoral Environnement et Sociétés, UMR 7266, Université de La Rochelle, La Rochelle, FranceDepartment of Atmospheric and Oceanic Sciences, McGill University, Montréal, QC, H3A OB9, CanadaTakuvik Joint International Laboratory, Université Laval & CNRS, Québec, QC, G1V 0A6, CanadaFuture climate warming of the Arctic could potentially enhance the load of terrigenous dissolved organic carbon (tDOC) of Arctic rivers due to increased carbon mobilization within watersheds. A greater flux of tDOC might impact the biogeochemical processes of the coastal Arctic Ocean (AO) and ultimately its capacity to absorb atmospheric CO<sub>2</sub>. In this study, we show that sea-surface tDOC concentrations simulated by a physical–biogeochemical coupled model in the Canadian Beaufort Sea for 2003–2011 compare favorably with estimates retrieved by satellite imagery. Our results suggest that, over spring–summer, tDOC of riverine origin contributes to 35 % of primary production and that an equivalent of ∼ 10 % of tDOC is exported westwards with the potential of fueling the biological production of the eastern Alaskan nearshore waters. The combination of model and satellite data provides promising results to extend this work to the entire AO so as to quantify, in conjunction with in situ data, the expected changes in tDOC fluxes and their potential impact on the AO biogeochemistry at basin scale.https://www.biogeosciences.net/15/1335/2018/bg-15-1335-2018.pdf |
collection |
DOAJ |
language |
English |
format |
Article |
sources |
DOAJ |
author |
V. Le Fouest A. Matsuoka M. Manizza M. Shernetsky B. Tremblay M. Babin |
spellingShingle |
V. Le Fouest A. Matsuoka M. Manizza M. Shernetsky B. Tremblay M. Babin Towards an assessment of riverine dissolved organic carbon in surface waters of the western Arctic Ocean based on remote sensing and biogeochemical modeling Biogeosciences |
author_facet |
V. Le Fouest A. Matsuoka M. Manizza M. Shernetsky B. Tremblay M. Babin |
author_sort |
V. Le Fouest |
title |
Towards an assessment of riverine dissolved organic carbon in surface waters of the western Arctic Ocean based on remote sensing and biogeochemical modeling |
title_short |
Towards an assessment of riverine dissolved organic carbon in surface waters of the western Arctic Ocean based on remote sensing and biogeochemical modeling |
title_full |
Towards an assessment of riverine dissolved organic carbon in surface waters of the western Arctic Ocean based on remote sensing and biogeochemical modeling |
title_fullStr |
Towards an assessment of riverine dissolved organic carbon in surface waters of the western Arctic Ocean based on remote sensing and biogeochemical modeling |
title_full_unstemmed |
Towards an assessment of riverine dissolved organic carbon in surface waters of the western Arctic Ocean based on remote sensing and biogeochemical modeling |
title_sort |
towards an assessment of riverine dissolved organic carbon in surface waters of the western arctic ocean based on remote sensing and biogeochemical modeling |
publisher |
Copernicus Publications |
series |
Biogeosciences |
issn |
1726-4170 1726-4189 |
publishDate |
2018-03-01 |
description |
Future climate warming of the Arctic could potentially enhance the load of terrigenous dissolved organic carbon (tDOC) of Arctic
rivers due to increased carbon mobilization within watersheds. A greater flux of tDOC might impact the biogeochemical processes of
the coastal Arctic Ocean (AO) and ultimately its capacity to absorb atmospheric CO<sub>2</sub>. In this study, we show that sea-surface tDOC
concentrations simulated by a physical–biogeochemical coupled model in the Canadian Beaufort Sea for 2003–2011 compare
favorably with estimates retrieved by satellite imagery. Our results suggest that, over spring–summer, tDOC of riverine origin
contributes to 35 % of primary production and that an equivalent of ∼ 10 % of tDOC is exported westwards with the
potential of fueling the biological production of the eastern Alaskan nearshore waters. The combination of model and satellite data
provides promising results to extend this work to the entire AO so as to quantify, in conjunction with in situ data, the expected
changes in tDOC fluxes and their potential impact on the AO biogeochemistry at basin scale. |
url |
https://www.biogeosciences.net/15/1335/2018/bg-15-1335-2018.pdf |
work_keys_str_mv |
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