Some effects of a mean zonal thermocline gradient on planetary equatorial waves

Planetary equatorial waves are studied with the shallow water equations in the presence of a mean zonal thermocline gradient. The interactions between this gradient and waves are represented by three non-linear terms in the equations: one in the wind-forcing formulation in the <i>x</i&g...

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Bibliographic Details
Main Authors: M. Pontaud, O. Thual
Format: Article
Language:English
Published: Copernicus Publications 1995-11-01
Series:Annales Geophysicae
Online Access:https://www.ann-geophys.net/13/1223/1995/angeo-13-1223-1995.pdf