Winter-to-summer evolution of pCO2 in surface water and air–sea CO2 flux in the seasonal ice zone of the Southern Ocean

• Published in: Biogeosciences
• Main Authors: Nomura, D., Yoshikawa-Inoue, H., Kobayashi, S., Nakaoka, S., Nakata, K., Hashida, G.
• Format: Text
• Language: English
• Published: 2018
• Subjects: Austral; Indian; Southern Ocean; Sea ice
• Online Access: https://doi.org/10.5194/bg-11-5749-2014; https://www.biogeosciences.net/11/5749/2014/

Partial pressure of CO 2 ( p CO 2 ) in surface water and vertical profiles of the carbonate system parameters were measured during austral summer in the Indian sector of the Southern Ocean (64–67° S, 32–58° E) in January 2006 to understand the CO 2 dynamics of seawater in the seasonal ice zone. Surface-water p CO 2 ranged from 275 to 400 μatm, and longitudinal variations reflected the dominant influence of water temperature and dilution by sea ice meltwater between 32 and 40° E and biological productivity between 40 and 58° E. Using carbonate system data from the temperature minimum layer (−1.9 °C < T < −1.5 °C, 34.2 < S < 34.5), we examined the winter-to-summer evolution of surface-water p CO 2 and the factors affecting it. Our results indicate that p CO 2 increased by as much as 32 μatm, resulting mainly from the increase in water temperature. At the same time as changes in sea ice concentration and surface-water p CO 2 , the air–sea CO 2 flux, which consists of the exchange of CO 2 between sea ice and atmosphere, changed from −1.1 to +0.9 mmol C m −2 day −1 between winter and summer. These results suggest that, for the atmosphere, the seasonal ice zone acts as a CO 2 sink in winter and a temporary CO 2 source in summer immediately after the retreat of sea ice. Subsequent biological productivity likely decreases surface-water p CO 2 and the air–sea CO 2 flux becomes negative, such that in summer the study area is again a CO 2 sink with respect to the atmosphere.