Changes of the oceanic CO 2 sink in the Eastern Indian sector of the Southern Ocean
International audience Changes in the carbon dioxide fugacity ( f CO 2 ) and air-sea CO 2 flux observed in the Southern Ocean, south of Tasmania were analysed and compared for two different years: 1996/1997 and 2002/2003. The CO 2 flux showed large and contrasting interannual changes in the permanen...
Published in: | Tellus B: Chemical and Physical Meteorology |
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Main Authors: | , , , |
Other Authors: | , , , , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
HAL CCSD
2006
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Subjects: | |
Online Access: | https://hal.science/hal-00770727 https://doi.org/10.1111/J.1600-0889.2006.00220.X |
Summary: | International audience Changes in the carbon dioxide fugacity ( f CO 2 ) and air-sea CO 2 flux observed in the Southern Ocean, south of Tasmania were analysed and compared for two different years: 1996/1997 and 2002/2003. The CO 2 flux showed large and contrasting interannual changes in the permanent open ocean zone (POOZ, 53-61°S) between the 2 yr where the oceanic CO 2 sink increased from about -0.3 mmol m -2 d -1 in February 1997 to -20.6 mmol m -2 d -1 in February 2003. The strong sink in February 2003 was associated with increased phytoplankton biomass in this High-Nutrient, Low-Chlorophyll (HNLC) region. Three hypotheses that may have influenced the biomass and f CO 2 changes in the POOZ were investigated: sea surface temperature (SST) and El Niño/ Southern Oscillation (ENSO) event, total stratospheric ozone column and ultraviolet (UV) radiation, and atmospheric dust inputs. The strong CO 2 sink in 2003 in the POOZ cannot be explained by the observed changes in SST or UV, but would be qualitatively consistent with the presence of episodic atmospheric dust inputs. |
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