EGU21-8978
https://doi.org/10.5194/egusphere-egu21-8978
EGU General Assembly 2021
© Author(s) 2021. This work is distributed under
the Creative Commons Attribution 4.0 License.

The role of tides on the carbonate chemistry of a coastal polynya in the south-eastern Weddell Sea

Elise Droste1, Melchor González Dávila2, Juana Magdalena Santana Casiano2, Mario Hoppema3, Gerd Rohardt3, Bastien Queste1,4, Hugh Venables5, Giorgio Dall'Olmo6, and Dorothee C. E. Bakker1
Elise Droste et al.
  • 1School of Environmental Sciences, University of East Anglia, Norwich Research Park, NR4 7TJ Norwich, United Kingdom
  • 2Instituto de Oceanografía y Cambio Global, Universidad de Las Palmas de Gran Canaria, Campus Universitario de Tafira, Edificio de Ciencias Básicas, 35017 Las Palmas de Gran Canaria, Spain
  • 3Alfred Wegener Institute Helmholtz Centre for Polar and Marine Research, Postfach 120161, 27515 Bremerhaven, Germany
  • 4Göteborgs Universitet, Universitetsplatsen 1, 405 30 Göteborg, Sweden
  • 5British Antarctic Survey, High Cross, Madingley Road, CB3 0ET Cambridge, United Kingdom
  • 6Plymouth Marine Laboratory, Prospect Place, PL1 3DH Plymouth, United Kingdom

Tides have a large impact on coastal polynyas around Antarctica. We investigate the effect of semi-diurnal tidal cycles on the seawater carbonate chemistry in a coastal polynya hugging the Ekström Ice Shelf in the south-eastern Weddell Sea. This region experiences some of the strongest tides in the Southern Ocean. We assess the implications for the contribution of coastal polynyas to the carbon dioxide (CO2) air-sea flux of the Weddell Sea.

Two site visits, in January 2015 and January 2019, are intercompared in terms of the dissolved inorganic carbon (DIC) concentration, total alkalinity, pH, and CO2 partial pressure (pCO2). The tides induce large variability in the carbonate chemistry of the coastal polynya in the austral summer: DIC concentrations vary between 2174 and 2223 umol kg-1.

The tidal fluctuation in the DIC concentration can swing the polynya from a sink to a source of atmospheric CO2 on a semi-diurnal timescale. We attribute these changes to the mixing of different water masses. The amount of variability induced by tides depends on – and is associated with – large scale oceanographic and biogeochemical processes that affect the characteristics and presence of the water masses being mixed, such as the rate of sea ice melt.

Sampling strategies in Antarctic coastal polynyas should always take tidal influences into account. This would help to reduce biases in our understanding of how coastal polynyas contribute to the CO2 uptake by the Southern Ocean.

How to cite: Droste, E., González Dávila, M., Santana Casiano, J. M., Hoppema, M., Rohardt, G., Queste, B., Venables, H., Dall'Olmo, G., and Bakker, D. C. E.: The role of tides on the carbonate chemistry of a coastal polynya in the south-eastern Weddell Sea, EGU General Assembly 2021, online, 19–30 Apr 2021, EGU21-8978, https://doi.org/10.5194/egusphere-egu21-8978, 2021.

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