Wave groups observed in pancake sea ice
Ocean surface waves propagating through sea ice are scattered and dissipated. The net attenuation occurs preferentially at the higher frequencies, and thus the spectral bandwidth of a given wave field is reduced, relative to open water. The reduction in bandwidth is associated with an increase in th...
| Published in: | Journal of Geophysical Research: Oceans |
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| Main Authors: | , , , , |
| Format: | Text |
| Language: | English |
| Published: |
American Geophysical Union (AGU)
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| Subjects: | |
| Online Access: | https://doi.org/10.1029/2019JC015354 https://archimer.ifremer.fr/doc/00587/69864/67763.pdf https://archimer.ifremer.fr/doc/00587/69864/67766.pdf https://archimer.ifremer.fr/doc/00587/69864/ |