Shadwick, E. H., Et Al. Seasonal Variability of the Inorganic Carbon
Limnol. Oceanogr., 56(1), 2011, 303–322 E 2011, by the American Society of Limnology and Oceanography, Inc. doi:10.4319/lo.2011.56.1.0303 Seasonal variability of the inorganic carbon system in the Amundsen Gulf region of the southeastern Beaufort Sea E. H. Shadwick,a,* H. Thomas,a M. Chierici,b B. Else,c A. Fransson,d C. Michel,e L. A. Miller,f A. Mucci,g A. Niemi,e T. N. Papakyriakou,c and J.-E´ . Tremblayh a Department of Oceanography, Dalhousie University, Halifax, Nova Scotia, Canada bDepartment of Chemistry, University of Gothenburg, Go¨teborg, Sweden c Center for Earth Observation Science, University of Manitoba, Winnipeg, Manitoba, Canada dDepartment of Earth Sciences, University of Gothenburg, Go¨teborg, Sweden e Freshwater Institute, Fisheries and Oceans Canada, Winnipeg, Manitoba, Canada f Institute of Ocean Sciences, Fisheries and Oceans Canada, Sidney, British Columbia, Canada g Department of Earth and Planetary Sciences, McGill University, Montreal, Que´bec, Canada hDepartment de Biologie, Universite´ Laval, Que´bec, Que´bec, Canada Abstract During a year-round occupation of Amundsen Gulf in the Canadian Arctic Archipelago dissolved inorganic and organic carbon (DIC, DOC), total alkalinity (TA), partial pressure of CO2 (pCO2) and related parameters were measured over a full annual cycle. A two-box model was used to identify and assess physical, biological, and chemical processes responsible for the seasonal variability of DIC, DOC, TA, and pCO2. Surface waters were undersaturated with respect to atmospheric CO2 throughout the year and constituted a net sink of 22 21 1.2 mol C m yr , with ice coverage and ice formation limiting the CO2 uptake during winter.
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