Fig. 5: Spatial distribution of the changes in the 2-m temperature (T2) attributed to sea–air coupling. | npj Climate and Atmospheric Science

Fig. 5: Spatial distribution of the changes in the 2-m temperature (T2) attributed to sea–air coupling.

From: Sea–air coupling leads to a decrease in precipitation in East Asia under present day conditions that is partially alleviated in future simulations

Fig. 5

The mean change in T2 during (a, c) June–July–August and (b, d) December–January–February under (a, b) present day and (c, d) future conditions. The dotted areas indicate regions where the changes are statistically significant at the 95% confidence interval determined using Student’s t-test.

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