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Summary
| Description |
English: Frequency dispersion of surface gravity waves on deep water. The superposition of three wave components, with respectively 22, 25 and 29 wavelengths fitting in a horizontal domain of 2,000 meter length, is shown. The wave amplitudes of the components are respectively 1, 2 and 1 meter. The differences in wavelength and phase speed of the components results in a changing pattern of wave groups, due to amplification where the components are in phase, and reduction where they are in anti-phase. |
| Date | |
| Source | Own work |
| Author | Kraaiennest |
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Permission is granted to copy, distribute and/or modify this document under the terms of the GNU Free Documentation License, Version 1.2 or any later version published by the Free Software Foundation; with no Invariant Sections, no Front-Cover Texts, and no Back-Cover Texts. A copy of the license is included in the section entitled GNU Free Documentation License. |
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File history
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| Date/Time | Thumbnail | Dimensions | User | Comment | |
|---|---|---|---|---|---|
| current | 19:44, 5 April 2008 | | 388 × 74 (1.17 MB) | Kraaiennest | smoother running animation |
| 21:06, 22 March 2008 |  | 388 × 74 (930 KB) | Kraaiennest | reduced size | |
| 20:32, 22 March 2008 |  | 466 × 82 (1.45 MB) | Kraaiennest | {{Information |Description=Frequency dispersion of surface gravity waves on deep water. The superposition of three wave components, with respectively 22, 25 and 29 wavelengths fitting in a horizontal domain of 2,000 meter length, is shown. The wave amplit |
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