A breaking internal wave in the surface ocean boundary layer

TitleA breaking internal wave in the surface ocean boundary layer
Publication TypeJournal Article
Year of Publication2015
AuthorsWain D.J, Lilly J.M, Callaghan AH, Yashayaev I., Ward B.
JournalJournal of Geophysical Research-Oceans
Volume120
Pagination4151-4161
Date Published2015/06
Type of ArticleArticle
ISBN Number2169-9275
Accession NumberWOS:000358124100015
KeywordsDeep convection; dissipation; equatorial pacific; fresh-water; gravity-waves; internal breaking wave; labrador sea; microstructure; microstructure measurements; mixed-layer; surface ocean boundary layer; transition layer; turbulence
Abstract

High-temporal resolution measurements in the Labrador Sea surface layer are presented using an upwardly profiling autonomous microstructure instrument, which captures an internal wave in the act of breaking at the base of the surface mixed layer, driving turbulence levels 2-3 orders of magnitude above the background. While lower-frequency (near-inertial) internal waves are known to be important sources of turbulence, we report here a higher-frequency internal wave breaking near the ocean surface. Due to observational limitations, the exact nature of the instability cannot be conclusively identified, but the interaction of wave-induced velocity with unresolved background shear appears to be the most likely candidate. These observations add a new process to the list of those currently being considered as potentially important for near-surface mixing. The geographical distribution and global significance of such features are unknown, and underscore the need for more extensive small-scale, rapid observations of the ocean surface layer.

DOI10.1002/2014jc010416
Short TitleJ Geophys Res-Oceans
Student Publication: 
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