Fig. 5: The effects of ocean coupling on Northern Hemisphere atmospheric temperature.

Response (differences between the 2080–2099 and 1980–1999 periods) of the zonal mean atmospheric temperature (K) in a, the LE mean, and the contribution from b net ocean coupling, c thermodynamic coupling, and d dynamic coupling. The (very few) small black dots show where the differences are not statistically significant at the 95% confidence level.