Central Arctic Ocean surface–atmosphere exchange of CO2 and CH4 constrained by direct measurements

The central Arctic Ocean (CAO) plays an important role in the global carbon cycle, but the current and future exchange of the climate-forcing trace gases methane ( CH 4 ) and carbon dioxide ( CO 2 ) between the CAO and the atmosphere is highly uncertain. In particular, there are very few observation...

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Bibliographic Details
Published in:Biogeosciences
Main Authors: Prytherch, John, Murto, Sonja, Brown, Ian, Ulfsbo, Adam, Thornton, Brett F., Brüchert, Volker, Tjernström, Michael, Hermansson, Anna Lunde, Nylund, Amanda T., Holthusen, Lina A.
Format: Text
Language:English
Published: 2024
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Online Access:https://doi.org/10.5194/bg-21-671-2024
https://bg.copernicus.org/articles/21/671/2024/
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Summary:The central Arctic Ocean (CAO) plays an important role in the global carbon cycle, but the current and future exchange of the climate-forcing trace gases methane ( CH 4 ) and carbon dioxide ( CO 2 ) between the CAO and the atmosphere is highly uncertain. In particular, there are very few observations of near-surface gas concentrations or direct air–sea CO 2 flux estimates and no previously reported direct air–sea CH 4 flux estimates from the CAO. Furthermore, the effect of sea ice on the exchange is not well understood. We present direct measurements of the air–sea flux of CH 4 and CO 2 , as well as air–snow fluxes of CO 2 in the summertime CAO north of 82.5 ∘ N from the Synoptic Arctic Survey (SAS) expedition carried out on the Swedish icebreaker Oden in 2021. Measurements of air–sea CH 4 and CO 2 flux were made using floating chambers deployed in leads accessed from sea ice and from the side of Oden , and air–snow fluxes were determined from chambers deployed on sea ice. Gas transfer velocities determined from fluxes and surface-water-dissolved gas concentrations exhibited a weaker wind speed dependence than existing parameterisations, with a median sea-ice lead gas transfer rate of 2.5 cm h −1 applicable over the observed 10 m wind speed range (1–11 m s −1 ). The average observed air–sea CO 2 flux was − 7.6 mmol m - 2 d - 1 <svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="67pt" height="13pt" class="svg-formula" dspmath="mathimg" md5hash="6add7475d1c0615a24800106f13ac773"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="bg-21-671-2024-ie00001.svg" width="67pt" height="13pt" src="bg-21-671-2024-ie00001.png"/> </svg:svg> , and the average air–snow CO 2 flux was − 1.1 mmol m - 2 d - 1 <svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="67pt" height="13pt" class="svg-formula" dspmath="mathimg" md5hash="8c4b3213a0a8ab1c445432263e63f72b"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="bg-21-671-2024-ie00002.svg" width="67pt" height="13pt" ...