The Arctic Ocean carbon sink

We present observation based estimates of the transport of dissolved inorganic carbon (DIC) across the four main Arctic Ocean gateways (Davis Strait, Fram Strait, Barents Sea Opening and Bering Strait). Combining a recently derived velocity field at these boundaries with measurements of DIC, we calc...

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Bibliographic Details
Published in:Deep Sea Research Part I: Oceanographic Research Papers
Main Authors: MacGilchrist, G. A., Naveira Garabato, A. C., Tsubouchi, T., Bacon, S., Torres-Valdes, S., Azetsu-Scott, K.
Format: Article in Journal/Newspaper
Language:English
Published: 2014
Subjects:
Arctic Ocean
Dissolved inorganic carbon
Carbon budget
Air-sea carbon dioxide flux
Carbon sequestration
Biological pump
CO2 UPTAKE CAPACITY
SEA-ICE
FRAM STRAIT
SURFACE-WATER
SHELF
DIOXIDE
CIRCULATION
TRANSPORTS
ATLANTIC
FLUXES
Arctic
Barents Sea
Bering Strait
Davis Strait
Fram Strait
Sea ice
Online Access:https://risweb.st-andrews.ac.uk/portal/en/researchoutput/the-arctic-ocean-carbon-sink(9b5e9bc7-d699-46e2-8cb7-1fb5f760d3f7).html
https://doi.org/10.1016/j.dsr.2014.01.002
Description
Summary:We present observation based estimates of the transport of dissolved inorganic carbon (DIC) across the four main Arctic Ocean gateways (Davis Strait, Fram Strait, Barents Sea Opening and Bering Strait). Combining a recently derived velocity field at these boundaries with measurements of DIC, we calculated a net summertime pan-Arctic export of 231 +/- 49 Tg C yr(-1). On an annual basis, we estimate that at least 166 +/- 60 Tg C yr(-1) of this is due to uptake of CO2 from the atmosphere, although time-dependent changes in carbon storage are not quantified. To further understand the region's role as a carbon sink, we calculated the volume-conserved net DIC transport from beneath a prescribed mixed layer depth of 50 m, referred to as 'interior transport', revealing an export of 61 +/- 23 Tg C yr(-1). Applying a carbon framework to infer the sources of interior transport implied that this export is primarily due to the sinking and remineralisation of organic matter, highlighting the importance of the biological pump. Furthermore, we qualitatively show that the present day Arctic Ocean is accumulating anthropogenic carbon beneath the mixed layer, imported in Atlantic Water. (C) 2014 The Authors. Published by Elsevier Ltd.

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