Extended Data Fig. 5: North Atlantic mixed layer depth and spatial origins of buoyancy-driven variability in RAPID-MOCHA overturning.
From: Distinct sources of interannual subtropical and subpolar Atlantic overturning variability
a, Climatological March mixed layer depth [m] in ECCO; b–e, Spatial sources of variability in the RAPID-MOCHA AMOC overturning: root-mean-square contribution per unit area [Sv m-2] to the convolutions in equation(1) of the main text over the period 1992–2015 using sensitivity patterns based on (b,c) 2006–2007 and (d,e) 2001–2002 AMOC objective functions. Contributions due to SST (b,d), and SSS (c,e) all relative to the seasonal cycle. The scale in all panels is linear.
