| 1. | The deep-water group velocity is half the phase velocity.
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| 2. | In this case, the phase velocity is twice the group velocity.
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| 3. | The group velocity is positive, while the phase velocity is negative.
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| 4. | Mathematically, this means that the size of the phase velocity changes.
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| 5. | This difference in phase velocities leads to the Faraday effect.
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| 6. | Nonlinear equations model the dependence of phase velocity on amplitude, replacing by.
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| 7. | Wave packets have group velocity and phase velocity.
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| 8. | Only sound with parallel collinear phase velocity vectors interfere to produce this nonlinear effect.
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| 9. | This shows a wave with the group velocity and phase velocity going in different directions.
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| 10. | That causes the phase velocity of right and left hand circular polarizations to significantly differ.
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