Possible angles for internal gravity wave propagation

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SUMMARY

The discussion centers on the propagation angles of internal gravity waves generated by the M2 tide along the coast of Norway. The angular frequency is calculated as ω = 1.41 x 10-4 rad/s, with a stratification frequency N of 2 x 10-3 rad/s. The derived angles of 85.96 and 94.04 degrees indicate a misunderstanding, as angles exceeding 90 degrees are not physically valid in this context. The correct interpretation of the equation ω = ±Ncos(θ) is crucial for determining valid propagation angles.

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  • Knowledge of angular frequency calculations
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Homework Statement



Internal gravity waves are generated along the coast of Norway by the principal lunar semidiurnal surface tide (known as the M2 tide) of period 12.42 h. If the stratification frequency N is 2 x 10-3rad s-1, at which possible angles can the energy propagate with respect to the horizontal?

Homework Equations



\omega={\pm}Ncos{\theta}

The Attempt at a Solution



Period, T is 12.42 hours = 44712 seconds

angular frequency is \omega=\frac{2{\pi}}{T}=1.41{\times}10^{-4}

N=2{\times}10^{-3}

Rearranging \omega={\pm}Ncos{\theta} in terms of theta gives \theta=cos^{-1}{\frac{\omega}{\pm{N}}}

Giving theta values of 85.96 and 94.04, but this can't be right as i thought the maximum value of theta could be 90 degrees above the horizontal? can anyone see where I'm going wrong?
 
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