Late autumn to spring changes in the inorganic and organic carbon dissolved in the water column at Scholaert Channel , West Antarctica

@inproceedings{Wang2010LateAT,
  title={Late autumn to spring changes in the inorganic and organic carbon dissolved in the water column at Scholaert Channel , West Antarctica},
  author={Xiaomeng Wang and Gui-peng Yang and Dami{\'a}n L{\'o}pez and Gustavo A. Ferreyra and Karine Lemarchand and Huixiang Xie},
  year={2010}
}
The temporal changes in dissolved inorganic (DIC) and organic carbon concentrations (DOC) were monitored from late autumn to spring 2006 in the Scholaert Channel, West Antarctic Peninsula. Surface DIC spanned a small range (2163.3 to 2194.5 mmol kg), increasing from late autumn to winter and then decreasing in spring. An excess of DOC (7.0–63.6 mmol l), against a deepwater background concentration of 44 mmol l, existed in the surface mixed layer throughout the sampling period. Massbalance… CONTINUE READING

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