The effects on planetary wave properties by coupling with simple atmospheres

Statistics – Computation

Scientific paper

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Scientific paper

The basic properties of oceanic planetary waves are studied considering a simple coupling with the atmosphere. First, a surface thermal boundary layer and then a 1-D Energy Balance Model for the atmosphere are coupled to a Rossby wave on a β-plane. In both cases, several experiments are carry out such as the computation of the dispersion relation, the dependence on the vertical diffusivity coefficient and the vertical structure of the wave. Preliminary results show that even these simple representations of the atmosphere can lead to changes in the propagation of long Rossby waves.

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