Extended Data Fig. 9: Atlantic Meridional Overturning Circulation response to subtropical MCB and future warming.
From: Diminished efficacy of regional marine cloud brightening in a warmer world
Change in Atlantic Meridional Overturning Circulation (AMOC) to subtropical MCB under 2010 conditions (a) and 2050 conditions (b). c, Change in AMOC due to warming under SSP2-4.5 without MCB. d, Change in AMOC between the 2050 subtropical MCB and 2010 no MCB cases, where near-zero values indicate a restoration of present-day conditions from MCB. The x-axis shows the latitude of the zonal mean, the y-axis shows depth from the sea surface, and the shading shows the AMOC strength in Sverdrups (Sv). 30-year difference from monthly mean output is plotted. Note the different color bar scale to Fig. 4a.
