Fig. 1 | Climate Dynamics

Fig. 1

From: North Atlantic gyre circulation in PRIMAVERA models

Fig. 1

North Atlantic barotropic streamfunction climatology for the period 1950–2014. Results of five climate models in their high (first column) and low (second column) horizontal resolutions. The third column shows the difference between the two configurations. Dots highlight areas in which the differences are robust, that is, when the differences are larger than the square root of the variance of the two series summed up. One ensemble member for each model configuration is plotted

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