CHEN Liqi, GAO Zhongyong, YANG Xulin, WANG Weiqiang. Comparison of airsea fluxes of CO2 in the Southern Ocean and the western Arctic Ocean[J]. Acta Oceanologica Sinica, 2004, (4): 647-653.
Citation:
CHEN Liqi, GAO Zhongyong, YANG Xulin, WANG Weiqiang. Comparison of airsea fluxes of CO2 in the Southern Ocean and the western Arctic Ocean[J]. Acta Oceanologica Sinica, 2004, (4): 647-653.
CHEN Liqi, GAO Zhongyong, YANG Xulin, WANG Weiqiang. Comparison of airsea fluxes of CO2 in the Southern Ocean and the western Arctic Ocean[J]. Acta Oceanologica Sinica, 2004, (4): 647-653.
Citation:
CHEN Liqi, GAO Zhongyong, YANG Xulin, WANG Weiqiang. Comparison of airsea fluxes of CO2 in the Southern Ocean and the western Arctic Ocean[J]. Acta Oceanologica Sinica, 2004, (4): 647-653.
Key Laboratory of Global Change and MarineAtmospheric Chemistry, State Oceanic Administration, Xiamen 361005, China;Third Institute of Oceanography, State Oceanic Administration, Xiamen 361005, China;Chinese Arctic and Antarctic Administration, Beijing 100860, China
2.
Key Laboratory of Global Change and MarineAtmospheric Chemistry, State Oceanic Administration, Xiamen 361005, China;Third Institute of Oceanography, State Oceanic Administration, Xiamen 361005, China
3.
Third Institute of Oceanography, State Oceanic Administration, Xiamen 361005, China
The data were collected during Chinese Arctic and Antarctic Expeditions in the western Arctic Ocean and the marginal sea ice zone (MSIZ) of the Southern Ocean,respectively in the boreal summer from July to September of 1999 and in the austral summer from December of 1999 to January of 2000.The concentrations of CO2 in surface water of the survey regions would mostly present lower than those in the atmosphere.A significant biological driving force could also been observed in summer waters in both of the above oceans.Air to sea CO2 fluxes were also calculated to compare oceanic uptake capacity of CO2 in both oceans with the world oceans using Liss,Wanninkhof,and Jacobs's methods.The averaged CO2 fluxes of air to sea in the western Arctic Ocean or in the MSIZ of the Southern Ocean doubled that in the world oceans.
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