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dependent on the structure and amplitude of the initial perturbation ( Zhu and Thorpe 2006 ). In contrast, the errors on convective scales grow at the location of the convection ( Zhang et al. 2007 ) and seem to be almost insensitive to the perturbation method ( Hohenegger and Schär 2007b ) (i.e., their amplitude and spatial structure). Even small-amplitude acoustic waves are sufficient to generate significant divergence of two simulations on the convective scale after about 10 h. Larger sensitivity to
dependent on the structure and amplitude of the initial perturbation ( Zhu and Thorpe 2006 ). In contrast, the errors on convective scales grow at the location of the convection ( Zhang et al. 2007 ) and seem to be almost insensitive to the perturbation method ( Hohenegger and Schär 2007b ) (i.e., their amplitude and spatial structure). Even small-amplitude acoustic waves are sufficient to generate significant divergence of two simulations on the convective scale after about 10 h. Larger sensitivity to
