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...

Full description

Bibliographic Details
Main Author: Breeding, J Ernest
Format: Article in Journal/Newspaper
Language:unknown
Published: arXiv 2020
Subjects:
Online Access:https://dx.doi.org/10.48550/arxiv.2005.06074
https://arxiv.org/abs/2005.06074
id ftdatacite:10.48550/arxiv.2005.06074
record_format openpolar
spelling 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
institution 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