Biogeochemical River Runoff Drives Intense Coastal Arctic Ocean CO2 Outgassing

Arctic warming alters land‐to‐sea fluxes of nutrients and organic matter, which impact air‐sea carbon exchange. Here we use an ocean‐biogeochemical model of the southeastern Beaufort Sea (SBS) to investigate the role of Mackenzie River biogeochemical discharge in modulating air‐sea CO 2 fluxes durin...

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Bibliographic Details
Published in:Geophysical Research Letters
Main Authors: Bertin, C., Carroll, D., Menemenlis, D., Dutkiewicz, S., Zhang, H., Matsuoka, A., Tank, S., Manizza, M., Miller, C., Babin, M., Mangin, A., Le Fouest, Vincent
Other Authors: LIttoral ENvironnement et Sociétés (LIENSs), La Rochelle Université (ULR)-Centre National de la Recherche Scientifique (CNRS), Moss Landing Marine Laboratories, NASA Jet Propulsion Laboratory, Massachusetts Institute of Technology (MIT), Scripps Institution of Oceanography (SIO - UC San Diego), University of California San Diego (UC San Diego), University of California (UC)-University of California (UC), Takuvik International Research Laboratory, Université Laval Québec (ULaval)-Centre National de la Recherche Scientifique (CNRS), ACRI-HE
Format: Article in Journal/Newspaper
Language:English
Published: HAL CCSD 2023
Subjects:
[SDU.OCEAN]Sciences of the Universe [physics]/Ocean
Atmosphere
Arctic
Arctic Ocean
Mackenzie River
Beaufort Sea
Mackenzie river
Online Access:https://hal.science/hal-04213868
https://doi.org/10.1029/2022GL102377
Description
Summary:Arctic warming alters land‐to‐sea fluxes of nutrients and organic matter, which impact air‐sea carbon exchange. Here we use an ocean‐biogeochemical model of the southeastern Beaufort Sea (SBS) to investigate the role of Mackenzie River biogeochemical discharge in modulating air‐sea CO 2 fluxes during 2000–2019. The contribution of six biogeochemical discharge constituents leads to a net CO 2 outgassing of 0.13 TgC yr −1 , with a decrease in the coastal SBS carbon sink of 0.23 and 0.4 TgC yr −1 due to riverine dissolved organic and inorganic carbon, respectively. Years with high (low) discharge promote more CO 2 outgassing (uptake) from the river plume. These results demonstrate that the Mackenzie River modulates the capacity of the SBS to act as a sink or source of atmospheric CO 2 . Our work suggests that accurate model representation of land‐to‐sea biogeochemical coupling can be critical for assessing present‐day Arctic coastal ocean response to the rapidly changing environment.

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