Internal Tide Phase Locking is a geophysical phenomenon in which the phase of internal tides becomes synchronized with the phase of the barotropic tidal forcing due to nonlinear interactions over topographic features, resulting in a coherent and repeatable temporal relationship between the two tidal components.
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Parametric Subharmonic Instability of the Internal Tide at 29°N
Jennifer MacKinnon, Matthew H. Alford, Oliver Sun et al. · Journal of Physical Oceanography · 2012 · 134 citations · Full text
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University of Washington Applied Physics Laboratory
Seattle, United States
2 h-index
4 publications
652 citations
Scripps Institution of Oceanography
La Jolla, United States
2 h-index
5 publications
786 citations
University of Victoria
Victoria, Canada
1 h-index
2 publications
268 citations
National Institute of Water and Atmospheric Research
Auckland, New Zealand
1 h-index
2 publications
28 citations
Woods Hole Oceanographic Institution
Falmouth, United States
1 h-index
1 publications
134 citations
University of Hawaiʻi at Mānoa
Honolulu, United States
1 h-index
1 publications
192 citations
Oregon State University
Corvallis, United States
1 h-index
2 publications
280 citations
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- Journal of Physical Oceanography
3 publications · 340 citations
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- Geophysical Research Letters
1 publications · 140 citations
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