Abstract:The scale interaction is simulated using a two-dimensional barotropic model with an initial condition of a large-scale vortex accompanied with four small-scale vortices. We show that both direct and inverse energy cascades occur simultaneously and that the spatial distribution of energy transfer flux across a moderate length scale is characterized by a highly localized configuration, which contains several closed systems with a spatial scale of 50-100 km embedded in two wave trains. This would imply that the t… Show more
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