Galápagos upwelling driven by localized wind-front interactions.

Cross-correlation of the first EOF’s amplitude with zonal and meridional wind stresses from ERA-Interim reveals the occurrence of a highly significant anticorrelation between SST and meridional wind stress [r = − 0.66 to − 0.39 with 99% confidence (p < 0.01)] (Fig. 2 c, right panel).

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