Let
Because the Rayleigh quotient is stationary with respect to first-order changes of its eigenfunction, only the explicit dependence of on contributes when the quotient is differentiated. Thus
where
It follows that
Since , the horizontal group velocity is
For a stationary ridge wave, . Assume , so downstream is the positive direction. The stated inequality is
The denominator in the group-velocity formula is then positive, and
The atmospheric internal gravity waves generated by the ridge consequently carry their wave packet downstream.

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