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Fig. 15.
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Velocity flows (in CGS units), ur (left) and uϕ (right), of the gravito-inertial 2g mode in the equatorial plane for Ωs = 100/π Hz (top), Ωs = 100 Hz (middle), and Ωs = 0 with an increased tidal amplitude (bottom). The tidal amplitude is Ct = 9.3 × 10−4 in Panel a, Ct = 4.1 × 10−3 in Panel b and in Panel c.
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