Fig. 12From: Wind-driven decadal sea surface height and main pycnocline depth changes in the western subarctic North Pacifica–c Same as Fig. 9 but for the SSH variations due to the barotropic Rossby wave mode (n=0) forced by the wind stress. In panel a, the wind stress data in the region east of 180 ∘ were not used for the calculation of the SSH anomaly in the western region. Arrows show El Niño-related SSH depressionsBack to article page