Wind-Driven Upwelling in the Southern Ocean and the Deglacial Rise in Atmospheric CO2

@article{Anderson2009WindDrivenUI,
  title={Wind-Driven Upwelling in the Southern Ocean and the Deglacial Rise in Atmospheric CO2},
  author={R. F. Anderson and S. Mubashshir Ali and Louisa I. Bradtmiller and Simon Harder Holm Nielsen and Martin Q. Fleisher and Britt E. Anderson and Lloyd H. Burckle},
  journal={Science},
  year={2009},
  volume={323},
  pages={1443 - 1448}
}
Wind-driven upwelling in the ocean around Antarctica helps regulate the exchange of carbon dioxide (CO2) between the deep sea and the atmosphere, as well as the supply of dissolved silicon to the euphotic zone of the Southern Ocean. Diatom productivity south of the Antarctic Polar Front and the subsequent burial of biogenic opal in underlying sediments are limited by this silicon supply. We show that opal burial rates, and thus upwelling, were enhanced during the termination of the last ice age… 
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