Impacts of Wind Stress Changes on the Global Heat Transport, Baroclinic Instability, and the Thermohaline Circulation

Figure 3

Annual thermohaline global circulation average for Atlantic Ocean (Sv). (a) CTR simulation, (b) difference of experiments for EQU 50% − CTR, and (c) difference of experiments for 46°S 50% − CTR.

(a) MOC CTR (Sv)

(b) MOC EQU 50% − CTR (Sv)

(c) MOC 46°S 50% − CTR