Articles | Volume 5, issue 4
Clim. Past, 5, 695–706, 2009
Clim. Past, 5, 695–706, 2009

  18 Nov 2009

18 Nov 2009

Quantifying the roles of ocean circulation and biogeochemistry in governing ocean carbon-13 and atmospheric carbon dioxide at the last glacial maximum

A. Tagliabue et al.

Cited articles

Adkins, J. F., Ingersoll, A. P., and Pasquero, C.: Rapid climate change and conditional instability of the glacial deep ocean from the thermobaric effect and geothermal heating, Quaternary Sci. Rev., 24, 581–594. 2005.
Alkama, R., Kageyama, M., Ramstein, G., et al.: Impact of a realistic river routing in coupled ocean-atmosphere simulations of the Last Glacial Maximum climate, Clim. Dynam., }{30, 855–869, 2007.
Arsouze, T., Dutay, J.-C., Kageyama, M., Lacan, F., Alkama, R., Marti, O., and Jeandel, C.: A modeling sensitivity study of the influence of the Atlantic meridional overturning circulation on neodymium isotopic composition at the Last Glacial Maximum, Clim. Past, 4, 191–203, 2008.
Aumont, O. and Bopp, L.: Globalizing results from in situ iron fertilization studies, Global. Biogeochem. Cy., 20, GB2017,, 2006.
de Baar H. J. W., Boyd, P. W., Coale, K. H., et al.: Synthesis of iron fertilization experiments: From the iron age in the age of enlightenment, J. Geophys. Res, 110, C09S16,, 2005.