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Verifications of the high-resolution numerical model and polarization relations of atmospheric acoustic-gravity waves

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Figure

Table 1. Standard deviations and their ratios for AGW with cx = 30 m s−1 calculated with the numerical model and with analytical polar-ization relations (labeled as Lin) at different altitudes averaged over the initial transient interval t < te and for quasi-stationary waves t > te.Bold font shows the data pairs equal to probabilities larger than 95 %.
Table 2. Same as Table 1 but for AGW with cx = 100 m s−1.

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