ADVANCES IN POLAR SCIENCE ›› 2014, Vol. 26 ›› Issue (2): 193-200.DOI: 10.13679/j.jdyj.2014.2.193

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ESTIMATION ON CARBON FLUX IN THE SOUTHERN OCEAN DURING THE 26TH CHINARE

Xu Suqing1, Chen Liqi1,Chen Haiying2   

  1.  
    1 Key Laboratory of Global Change and Marine-Atmospheric Chemistry, TIO, SOA, Xiamen 361005, China;
    2 Opening Laboratory of Marine Acoustics and Remote Sensing Technology, TIO, SOA, Xiamen 361005, China
  • Received:2013-05-30 Revised:2013-08-08 Online:2014-06-30 Published:2014-06-30
  • Supported by:

    The Project Sponsored by the Scientific Research Foundationof Third Institute of Oceanography,SOA

Abstract: The Southern Ocean is an important sink of atmospheric CO2 and the magnitude of the CO2 sink is heavily disputed because its ability to absorb CO2 changes significantly in the decades. An empirical relationship was deduced based on the in-situ pCO2 in the surface sea water and its main controls including Chla and SST obtained during the 26th CHINARE. An extrapolation model was found combining the empirical relationship and relative remote sensing data to compute the air-sea carbon fluxes and carbon uptake in the Southern Ocean (south of 50°S). Results of the extrapolation model show that it was a weak source of atmospheric CO2 in the area from 90°E to 90°W (clockwise), 50°S to 75°S in November, 2009 with an average flux 9.482mol/m2*mon, and carbon release was 0.0017795*1015gC. While in December, 2009, the study area from 90°E to 90°W (clockwise), 50°S to 75°S turned to be a weak sink with an average flux -12.451mol/m2*mon and carbon uptake was 0.026656*1015gC. When the empirical relationship was applied to the whole area from 50°S to 75°S, the results show in November 2009 the Southern Ocean was a source of 0.0027896*1015gC and in December 2009 it was a sink of -0.0035035*1015gC. Compared to the research results before, we found that the ability of carbon uptake decline obviously.

Key words: CHINARE, Southern Ocean, extrapolation model, remote sensing, carbon flux