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