Abstract
Using linear internal wave theory for an ocean stratified by both density and current, several background profiles are identified for which internal wave beams can propagate without any internal reflection. These special profiles are favorably compared with available oceanic data. © 2010 American Meteorological Society.
Cite
CITATION STYLE
APA
Grimshaw, R., Pelinovsky, E., & Talipova, T. (2010). Nonreflecting internal wave beam propagation in the deep ocean. Journal of Physical Oceanography, 40(4), 802–813. https://doi.org/10.1175/2009JPO4180.1
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