Why Are There Rossby Wave Maxima in the Pacific at 108S and 138N?

Abstract

Observations indicate the existence of two bands of maximum thermocline depth variability centered at ;108S and 138N in the tropical Pacific Ocean. The analysis of a numerical integration performed with the National Center for Atmospheric Research ocean general circulation model (OGCM) forced with observed fluxes of momentum, heat, and freshwater over the… (More)

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