Fig. 7: UC intensity regressed onto ocean temperature.
From: Inter-model diversity and Its Drivers in Southern Ocean Meridional Overturning Circulation
Regression coefficient maps of a global mean-removed sea surface temperature and b zonal-averaged ocean potential temperature against UC intensity. Contour lines in b indicate the overturning streamfunction of the multi-model mean. The dotted areas indicate regions where regression coefficients are statistically significant at the 95% confidence level (Student’s t-test) and corresponding correlation coefficients exceed 0.4.
