Ocean Mixing by Kelvin-Helmholtz Instability

Kelvin-Helmholtz (KH) instability, characterized by the distinctive finite-amplitude billows it generates, is an important mechanism in the development of turbulence in the stratified interior of the ocean. In particular, it is often assumed that the onset of turbulence in internal waves begins in t...

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Bibliographic Details
Main Authors: William D. Smyth, James N. Moum
Format: Article
Language:English
Published: The Oceanography Society 2012-06-01
Series:Oceanography
Subjects:
Online Access:http://tos.org/oceanography/archive/25-2_smyth.pdf