Westward propagation of barrier layer formation in the 2006-07 Rossby wave event over the tropical southwest Indian Ocean

Physics

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Oceanography: Physical: Planetary Waves, Oceanography: Physical: Upper Ocean And Mixed Layer Processes, Oceanography: General: Equatorial Oceanography, Atmospheric Processes: Ocean/Atmosphere Interactions (0312, 4504), Atmospheric Processes: Climate Change And Variability (1616, 1635, 3309, 4215, 4513)

Scientific paper

A suite of satellite and in-situ observations are used to study ocean-atmospheric conditions over the tropical Southwest Indian Ocean (SWIO) during 2006-2007 when El Nino and an Indian Ocean dipole took place simultaneously. Argo profiles reveal a pronounced up-westward propagation of subsurface warming in the southern tropical Indian Ocean associated with Rossby waves traveling on the sloping thermocline. With the thermocline deepening by 60 m, a thick barrier layer forms and propagates with the Rossby wave, potentially contributing to the mixed layer warming.

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