lmd_Codron2009.bib

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@article{2009GeoRL..3612606L,
  author = {{Lenton}, A. and {Codron}, F. and {Bopp}, L. and {Metzl}, N. and 
	{Cadule}, P. and {Tagliabue}, A. and {Le Sommer}, J.},
  title = {{Stratospheric ozone depletion reduces ocean carbon uptake and enhances ocean acidification}},
  journal = {\grl},
  keywords = {Biogeosciences: Carbon cycling (4806), Biogeosciences: Climate dynamics (1620), Biogeosciences: Modeling, Biogeosciences: Biosphere/atmosphere interactions (0315)},
  year = 2009,
  month = jun,
  volume = 36,
  eid = {L12606},
  pages = {12606},
  abstract = {{Observational and atmospheric inversion studies find that the strength
of the Southern Ocean carbon dioxide (CO$_{2}$) sink is not
increasing, despite rising atmospheric CO$_{2}$. However, this is
yet to be captured by contemporary coupled-climate-carbon-models used to
predict future climate. We show that by accounting for stratospheric
ozone depletion in a coupled-climate-carbon-model, the ventilation of
carbon rich deep water is enhanced through stronger winds, increasing
surface water CO$_{2}$ at a rate in good agreement with observed
trends. We find that Southern Ocean uptake is reduced by 2.47 PgC
(1987-2004) and is consistent with atmospheric inversion studies. The
enhanced ventilation also accelerates ocean acidification, despite
lesser Southern Ocean CO$_{2}$ uptake. Our results link two
important anthropogenic changes: stratospheric ozone depletion and
greenhouse gas increases; and suggest that studies of future climate
that neglect stratospheric ozone depletion likely overestimate regional
and global oceanic CO$_{2}$ uptake and underestimate the impact of
ocean acidification.
}},
  doi = {10.1029/2009GL038227},
  adsurl = {http://adsabs.harvard.edu/abs/2009GeoRL..3612606L},
  adsnote = {Provided by the SAO/NASA Astrophysics Data System}
}