1. The seasonal cycle of ocean‐atmosphere CO2flux in Ryder Bay, west Antarctic Peninsula
- Author
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Legge, Oliver J., Bakker, Dorothee C. E., Johnson, Martin T., Meredith, Michael P., Venables, Hugh J., Brown, Peter J., and Lee, Gareth A.
- Abstract
Approximately 15 million km2of the Southern Ocean is seasonally ice covered, yet the processes affecting carbon cycling and gas exchange in this climatically important region remain inadequately understood. Here, 3 years of dissolved inorganic carbon (DIC) measurements and carbon dioxide (CO2) fluxes from Ryder Bay on the west Antarctic Peninsula (WAP) are presented. During spring and summer, primary production in the surface ocean promotes atmospheric CO2uptake. In winter, higher DIC, caused by net heterotrophy and vertical mixing with Circumpolar Deep Water, results in outgassing of CO2from the ocean. Ryder Bay is found to be a net sink of atmospheric CO2of 0.90–1.39 mol Cm−2yr−1(average of 3 years). Seasonal sea ice cover modifies the net annual CO2uptake, but its effect on gas exchange remains poorly constrained. A reduction in sea ice on the WAP shelf may reduce the strength of the oceanic CO2sink in this region. The water column in Ryder Bay is a net, annual sink of atmospheric CO2Seasonal sea ice modifies the strength of the ocean CO2sink in Ryder BayLarge uncertainty remains regarding the effect of sea ice on gas exchange
- Published
- 2015
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