Carbon dynamics of the Weddell Gyre, Southern Ocean

This is the final version of the article. Available from Wiley via the DOI in this record. The accumulation of carbon within the Weddell Gyre and its exchanges across the gyre boundaries are investigated with three recent full-depth oceanographic sections enclosing this climatically important region...

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Bibliographic Details
Published in:Global Biogeochemical Cycles
Main Authors: Brown, PJ, Jullion, L, Landschützer, P, Bakker, DCE, Naveira Garabato, AC, Meredith, MP, Torres-Valdés, S, Watson, Andrew J., Hoppema, M, Loose, B, Jones, EM, Telszewski, M, Jones, SD, Wanninkhof, R
Format: Article in Journal/Newspaper
Language:English
Published: American Geophysical Union (AGU) / Wiley 2015
Subjects:
Air-sea exchange of CO2
Neural network
Observations
Ocean carbon cycle
Southern Ocean
Weddell Gyre
Weddell
Weddell Sea
Online Access:http://hdl.handle.net/10871/16839
https://doi.org/10.1002/2014GB005006
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Summary:This is the final version of the article. Available from Wiley via the DOI in this record. The accumulation of carbon within the Weddell Gyre and its exchanges across the gyre boundaries are investigated with three recent full-depth oceanographic sections enclosing this climatically important region. The combination of carbon measurements with ocean circulation transport estimates from a box inverse analysis reveals that deepwater transports associated with Warm Deep Water (WDW) and Weddell Sea Deep Water dominate the gyre's carbon budget, while a dual-cell vertical overturning circulation leads to both upwelling and the delivery of large quantities of carbon to the deep ocean. Historical sea surface pCO2 observations, interpolated using a neural network technique, confirm the net summertime sink of 0.044 to 0.058±0.010PgCyr-1 derived from the inversion. However, a wintertime outgassing signal similar in size results in a statistically insignificant annual air-to-sea CO2 flux of 0.002±0.007PgCyr-1 (mean 1998-2011) to 0.012±0.024PgCyr-1 (mean 2008-2010) to be diagnosed for the Weddell Gyre. A surface layer carbon balance, independently derived from in situ biogeochemical measurements, reveals that freshwater inputs and biological drawdown decrease surface ocean inorganic carbon levels more than they are increased by WDW entrainment, resulting in an estimated annual carbon sink of 0.033±0.021PgCyr-1. Although relatively less efficient for carbon uptake than the global oceans, the summertime Weddell Gyre suppresses the winter outgassing signal, while its biological pump and deepwater formation act as key conduits for transporting natural and anthropogenic carbon to the deep ocean where they can reside for long time scales. NERC European Union CarboOcean CarboChange

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