Over the 2005–2011 period, we observed a decreasing trend in densities within the DWBC off Abaco (not only within the Labrador Sea Water layer but through the whole NADW water column from approximately 1200–4500 m; [ 42 ]), which could be consistent with this explanation.
← all excerpts
Towards two decades of Atlantic Ocean mass and heat transports at 26.5° N.
1
—
—