The Drakkar and CLIPPER models have been used to study the water mass and circulation variability along the OVIDE Section.


Treguier, A.-M., C. Gourcuff, P. Lherminier, H. Mercier, B. Barnier, G. Madec, J. M. Molines, T. Penduff, L. Czeschel, C. Böning, 2006: Internal and forced variability along a section between Greenland and Portugal in the CLIPPER Atlantic model. Ocean Dynamics, Christian LeProvost special issue, DOI: 10.1007/s10236-006-0069-y.

Desbruyères, D., V. Thierry, H. Mercier, 2013: Simulated decadal variability of the meridional overturning circulation across the A25-Ovide section. J. Geophys. Res., J. Geophys. Res., DOI: 10.1029/2012JC008342.

Boisséson (de), E., V. Thierry, H. Mercier, G. Caniaux 2012: Origin, formation and variability of the subpolar mode water observed over the Reykjanes Ridge. J. Geophys. Res. Oceans, 117, C12005, doi:10.1029/2011JC007519.

De Boisséson, E., V. Thierry, H. Mercier, 2010: Mixed layer heat budget in the Iceland Basin from Argo. J. Geophys. Res. Oceans, 115, C10055, doi:10.1029/2010JC006283.