Fig. 7: Overturning transport in relation to wbc density changes.
From: Decadal changes in Atlantic overturning due to the excessive 1990s Labrador Sea convection
Inter-decadal evolution of potential density in the deep western boundary current at position 5, averaged over 1500–2000 m depth (continuous lines), and overturning transport (AMOC) at section FULL (dashed lines) for experiments CTRL and SENS.
