Propagation of Wave Packets in Dispersive Media
The propagation and refraction of waves in dispersive media are considered. A primary objective is to determine whether waves refract as monochromatic waves by Snell's law with phase velocity or as wave packets. The refraction of wave packets requires two refraction laws. The wave packets refra...
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Online Access: | https://dx.doi.org/10.48550/arxiv.2005.06074 https://arxiv.org/abs/2005.06074 |
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ftdatacite:10.48550/arxiv.2005.06074 2023-05-15T18:25:48+02:00 Propagation of Wave Packets in Dispersive Media Breeding, J Ernest 2020 https://dx.doi.org/10.48550/arxiv.2005.06074 https://arxiv.org/abs/2005.06074 unknown arXiv arXiv.org perpetual, non-exclusive license http://arxiv.org/licenses/nonexclusive-distrib/1.0/ Atmospheric and Oceanic Physics physics.ao-ph FOS Physical sciences ? None that I know of Article CreativeWork article Preprint 2020 ftdatacite https://doi.org/10.48550/arxiv.2005.06074 2022-03-10T15:44:11Z The propagation and refraction of waves in dispersive media are considered. A primary objective is to determine whether waves refract as monochromatic waves by Snell's law with phase velocity or as wave packets. The refraction of wave packets requires two refraction laws. The wave packets refract according to Snell's law with the geometric group velocity while the wavelets within the wave packets refract according to Snell's law with phase velocity. The tests were performed using directional power spectra from gravity water waves originating in the Caribbean Sea, Gulf of Mexico, Indian Ocean, and the Southern Ocean. In all cases the waves were measured with arrays of pressure sensors. It was found that the refraction of monochromatic waves led to backtracks from a measurement site that spread out for the different wave periods and did not go back to a common source. When the refraction was large the results were especially bad. When the data were used to test the refraction of wave packets very good results were obtained. For every storm considered the backtracks of the different wave periods went back together to the wave generation area. These results offer strong support for refracting waves in dispersive media as wave packets, not as monochromatic waves. This result for wave groups was also determined in a controlled wave tank experiment of gravity water waves where a critical angle was tested. The properties of propagating wave packets are also considered and illustrated. Reflection points and critical angles are found and explained. There can be major differences between the propagation of wave packets and monochromatic waves. : 42 pages, 9 figures, no other info Article in Journal/Newspaper Southern Ocean DataCite Metadata Store (German National Library of Science and Technology) Indian Southern Ocean |
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Open Polar |
collection |
DataCite Metadata Store (German National Library of Science and Technology) |
op_collection_id |
ftdatacite |
language |
unknown |
topic |
Atmospheric and Oceanic Physics physics.ao-ph FOS Physical sciences ? None that I know of |
spellingShingle |
Atmospheric and Oceanic Physics physics.ao-ph FOS Physical sciences ? None that I know of Breeding, J Ernest Propagation of Wave Packets in Dispersive Media |
topic_facet |
Atmospheric and Oceanic Physics physics.ao-ph FOS Physical sciences ? None that I know of |
description |
The propagation and refraction of waves in dispersive media are considered. A primary objective is to determine whether waves refract as monochromatic waves by Snell's law with phase velocity or as wave packets. The refraction of wave packets requires two refraction laws. The wave packets refract according to Snell's law with the geometric group velocity while the wavelets within the wave packets refract according to Snell's law with phase velocity. The tests were performed using directional power spectra from gravity water waves originating in the Caribbean Sea, Gulf of Mexico, Indian Ocean, and the Southern Ocean. In all cases the waves were measured with arrays of pressure sensors. It was found that the refraction of monochromatic waves led to backtracks from a measurement site that spread out for the different wave periods and did not go back to a common source. When the refraction was large the results were especially bad. When the data were used to test the refraction of wave packets very good results were obtained. For every storm considered the backtracks of the different wave periods went back together to the wave generation area. These results offer strong support for refracting waves in dispersive media as wave packets, not as monochromatic waves. This result for wave groups was also determined in a controlled wave tank experiment of gravity water waves where a critical angle was tested. The properties of propagating wave packets are also considered and illustrated. Reflection points and critical angles are found and explained. There can be major differences between the propagation of wave packets and monochromatic waves. : 42 pages, 9 figures, no other info |
format |
Article in Journal/Newspaper |
author |
Breeding, J Ernest |
author_facet |
Breeding, J Ernest |
author_sort |
Breeding, J Ernest |
title |
Propagation of Wave Packets in Dispersive Media |
title_short |
Propagation of Wave Packets in Dispersive Media |
title_full |
Propagation of Wave Packets in Dispersive Media |
title_fullStr |
Propagation of Wave Packets in Dispersive Media |
title_full_unstemmed |
Propagation of Wave Packets in Dispersive Media |
title_sort |
propagation of wave packets in dispersive media |
publisher |
arXiv |
publishDate |
2020 |
url |
https://dx.doi.org/10.48550/arxiv.2005.06074 https://arxiv.org/abs/2005.06074 |
geographic |
Indian Southern Ocean |
geographic_facet |
Indian Southern Ocean |
genre |
Southern Ocean |
genre_facet |
Southern Ocean |
op_rights |
arXiv.org perpetual, non-exclusive license http://arxiv.org/licenses/nonexclusive-distrib/1.0/ |
op_doi |
https://doi.org/10.48550/arxiv.2005.06074 |
_version_ |
1766207474642190336 |