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responses to TIW-induced SST forcing are underestimated by about a factor of 2 as indicated by the slopes. Nevertheless, the simulation skill from this empirical model is still comparable to that represented in the high horizontal resolution European Centre for Medium-Range Weather Forecasts (ECWMF) operational model (e.g., Chelton et al. 2005 ). Similarly, the binned scatterplots of the divergence and curl perturbations are illustrated in Fig. 14b . Again, the estimated slopes are about half of those
responses to TIW-induced SST forcing are underestimated by about a factor of 2 as indicated by the slopes. Nevertheless, the simulation skill from this empirical model is still comparable to that represented in the high horizontal resolution European Centre for Medium-Range Weather Forecasts (ECWMF) operational model (e.g., Chelton et al. 2005 ). Similarly, the binned scatterplots of the divergence and curl perturbations are illustrated in Fig. 14b . Again, the estimated slopes are about half of those
