RESEARCH ARTICLE Seasonal dynamics of the marine CO2 system in Adventfjorden, a west Spitsbergen fjord Ylva Ericson1,2, Melissa Chierici1,3, Eva Falck1,2, Agneta Fransson4, Elizabeth Jones3 & Svein Kristiansen5 1Department of Arctic Geophysics, University Centre in Svalbard, Longyearbyen, Norway; 2Geophysical Institute, University of Bergen, Bergen, Norway; 3Institute of Marine Research, Fram Centre, Tromsø, Norway; 4Norwegian Polar Institute, Fram Centre, Tromsø, Norway; 5Department of Arctic and Marine Biology, UiT—The Arctic University of Norway, Tromsø, Norway Abstract Keywords Marine carbonate system; aragonite; Time series of the marine CO2 system and related parameters at the IsA Sta- net community production; Arctic fjord tion, by Adventfjorden, Svalbard, were investigated between March 2015 biogeochemistry; Svalbard and November 2017. The physical and biogeochemical processes that govern changes in total alkalinity (TA), total dissolved inorganic carbon (DIC) and the Correspondence Ylva Ericson, Department of Arctic saturation state of the calcium carbonate mineral aragonite (ΩAr) were assessed on a monthly timescale. The major driver for TA and DIC was changes in salin- Geophysics, University Centre in Svalbard, ity, caused by river runoff, mixing and advection. This accounted for 77 and PO Box 156, NO-9171 Longyearbyen, Norway. E-mail:
[email protected] 45%, respectively, of the overall variability. It contributed minimally to the variability in ΩAr (5%); instead, biological activity was responsible for 60% of Abbreviations the monthly variations. For DIC, the biological activity was also important, con- ArW: Arctic water; AW: Atlantic water; tributing 44%. The monthly effect of air–sea CO2 fluxes accounted for 11 and CC: coastal current; CTD: conductivity– temperature–depth instrument; DIC: 15% of the total changes in DIC and ΩAr, respectively.