Articles | Volume 10, issue 6
Research article
19 Nov 2014
Research article |  | 19 Nov 2014

On the glacial and interglacial thermohaline circulation and the associated transports of heat and freshwater

M. Ballarotta, S. Falahat, L. Brodeau, and K. Döös

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Cited articles

Adkins, J. F. and Schrag, D. P.: Pore fluid constraints on deep ocean temperature and salinity during the Last Glacial Maximum, Geophys. Res. Lett., 28, 771–774,, 2001.
Adkins, J. F., Mcintyre, K., and Schrag, D. P.: The Salinity, Temperature, and δ18O of the Glacial Deep Ocean, Science, 298, 1769–1773,, 2002.
Ballarotta, M., Brodeau, L., Brandefelt, J., Lundberg, P., and Döös, K.: Last Glacial Maximum world ocean simulations at eddy-permitting and coarse resolutions: do eddies contribute to a better consistency between models and palaeoproxies?, Clim. Past, 9, 2669–2686,, 2013a.
Ballarotta, M., Brodeau, L., Brandefelt, J., Lundberg, P., and Döös, K.: A Last Glacial Maximum world-ocean simulation at eddy-permitting resolution – Part 1: Experimental design and basic evaluation, Clim. Past Discuss., 9, 297–328,, 2013b.
Barnier, B., Madec, G., Penduff, T., Molines, J. M., Tréguier, A. M., Le Sommer, J., Beckmann, A., Biastoch, A., Böning, C., Dengg, J., Derval, C., Durand, E., Gulev, S., Remy, E., Talandier, C., Theetten, S., Maltrud, M., McClean, J., and De Cuevas, B.: Impact of partial steps and momentum advection schemes in a global ocean circulation model at eddy-permitting resolution, Ocean Dynam., 56, 543–567,, 2006.