Seasonal dynamics of the marine CO2 system in Adventfjorden, a West Spitsbergen fjord

• Published in: Polar Research
• Main Authors: Ericson, Ylva, Chierici, Melissa, Falck, Eva, Fransson, Agneta Ingrid, Jones, Elizabeth Marie, Kristiansen, Svein
• Format: Article in Journal/Newspaper
• Language: English
• Published: Norsk Polarinstitutt 2019
• Subjects: VDP::Mathematics and natural science: 400::Zoology and botany: 480::Marine biology: 497; VDP::Matematikk og Naturvitenskap: 400::Zoologiske og botaniske fag: 480::Marinbiologi: 497; marine carbonate system; aragonite; net community production; Arctic fjord biogeochemistry; Svalbard; Adventfjorden; Arctic; Polar Research; Spitsbergen
• Online Access: https://hdl.handle.net/10037/16295; https://doi.org/10.33265/polar.v38.3345

Source at https://doi.org/10.33265/polar.v38.3345. Time series of the marine CO 2 system and related parameters at the IsA Station, by Adventfjorden, Svalbard, were investigated between March 2015 and November 2017. The physical and biogeochemical processes that govern changes in total alkalinity (TA), total dissolved inorganic carbon (DIC) and the saturation state of the calcium carbonate mineral aragonite (Ω Ar ) were assessed on a monthly timescale. The major driver for TA and DIC was changes in salinity, caused by river runoff, mixing and advection. This accounted for 77 and 45%, respectively, of the overall variability. It contributed minimally to the variability in Ω Ar (5%); instead, biological activity was responsible for 60% of the monthly variations. For DIC, the biological activity was also important, contributing 44%. The monthly effect of air–sea CO 2 fluxes accounted for 11 and 15% of the total changes in DIC and Ω Ar , respectively. Net community production (NCP) during the productive season ranged between 65 and 85 g C m −2 , depending on the year and the presence of either Arctic water or transformed Atlantic water (TAW). The annual NCP as estimated from DIC consumption was 34 g C m −2 yr −1 in 2016, which was opposite in direction but similar in magnitude to the integrated annual air–sea CO 2 flux (i.e., uptake of carbon from the atmosphere) of −29 g C m −2 yr −1 for the same year. The results showed that increased intrusions of TAW into Adventfjorden in the future could possibly lower the NCP, with the potential to reduce the CO 2 buffer capacity and Ω Ar over the summer season.