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

Figure 2

(a) SST anomalies (°C) for EQU 50% − CTR, (b) SST anomalies (°C) for 46°S 50% − CTR, (c) Thickness Antarctic sea ice anomaly (m) for EQU 50% − CTR, and (d) thickness Antarctic sea ice anomalies (m) for 46°S 50% − CTR.

(a) SST EQU 50% − CTR (C)

(b) SST 46°S 50% − CTR (C)

(c) Thickness Antarctic sea ice (m) EQU 50% − CTR

(d) Thickness Antarctic sea ice (m) 46°S 50% − CTR