Abstract

The first long term, near equatorial, near surface moored current measurements recorded in the Pacific Ocean west of 160°W were made at 0°, 150°E during 2 August 1985–1 February 1986. These data revealed 17.5‐day period oscillations of the meridional current. Prior to these measurements, these waves had only been observed eastward of about 165°W, which also was the westernmost extent of their appearance in ocean general circulation model simulations. The 17.5‐day period waves also occurred in simultaneous current measurements at 140°W, where the wave amplitude was 3 times greater. At both sites the 17.5‐day period wave amplitude was more than 50% of the record‐length standard deviations of the meridional current component. A wider spectral bandwidth and a smaller tendency towards rectilinear motion occurred at 150°E than at 140°W.

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