Direct determination of the air-sea CO2 gas transfer velocity in Arctic sea ice regions

The Arctic Ocean is an important sink for atmospheric CO2. The impact of decreasing sea ice extent and expanding marginal ice zones on Arctic air-sea CO2 exchange depends on the rate of gas transfer in the presence of sea ice. Sea ice acts to limit air-sea gas exchange by reducing contact between ai...

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Bibliographic Details
Published in:Geophysical Research Letters
Main Authors: Prytherch, John, Brooks, Ian M., Crill, Patrick M., Thornton, Brett F., Salisbury, Dominic J., Tjernström, Michael, Anderson, Leif G., Geibel, Marc C., Humborg, Christoph
Format: Article in Journal/Newspaper
Language:English
Published: Stockholms universitet, Meteorologiska institutionen (MISU) 2017
Subjects:
CO2
carbon dioxide
Arctic ocean
eddy covariance
Arctic
icebreaker
Earth and Related Environmental Sciences
Geovetenskap och miljövetenskap
Arctic Ocean
Sea ice
Online Access:http://urn.kb.se/resolve?urn=urn:nbn:se:su:diva-144720
https://doi.org/10.1002/2017GL073593
Description
Summary:The Arctic Ocean is an important sink for atmospheric CO2. The impact of decreasing sea ice extent and expanding marginal ice zones on Arctic air-sea CO2 exchange depends on the rate of gas transfer in the presence of sea ice. Sea ice acts to limit air-sea gas exchange by reducing contact between air and water but is also hypothesized to enhance gas transfer rates across surrounding open-water surfaces through physical processes such as increased surface-ocean turbulence from ice-water shear and ice-edge form drag. Here we present the first direct determination of the CO2 air-sea gas transfer velocity in a wide range of Arctic sea ice conditions. We show that the gas transfer velocity increases near linearly with decreasing sea ice concentration. We also show that previous modeling approaches overestimate gas transfer rates in sea ice regions.

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