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The Direct Breaking of Internal Waves at Steep Topography

Internal waves are often observed to break close to the seafloor topography that generates them, or from which they scatter. This breaking is often spectacular, with turbulent structures observed hundreds of meters above the seafloor, and driving turbulence dissipations and mixing up to 10,000 times...

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Detalhes bibliográficos
Main Authors: Jody M. Klymak, Sonya Legg, Matthew H. Alford, Maarten Buijsman, Robert Pinkel, Jonathan D. Nash
Formato: Artigo
Idioma:Inglês
Publicado em: The Oceanography Society 2012-06-01
Colecção:Oceanography
Assuntos:
Acesso em linha:http://tos.org/oceanography/archive/25-2_klymak.pdf
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