Internal Wave-driven Circulation
Internal Wave-Driven Circulation is a coastal circulation mechanism in which sub-surface density-stratified water motions, generated by the propagation and dissipation of internal waves, induce time-averaged mass, momentum, and energy transport within the littoral and nearshore oceanic regimes.
127
Publications
5.9K
Citations
446
Authors
204
Institutions
Publications per year
2017–2026
27
Parents
127
The formation and fate of internal waves in the South China Sea
Matthew H. Alford, Thomas Peacock, Jennifer MacKinnon et al. · Nature · 2015 · 711 citations · Full text
Internal Waves in Monterey Submarine Canyon
Eric Kunze, Leslie K. Rosenfeld, Glenn S. Carter et al. · Journal of Physical Oceanography · 2002 · 277 citations
1–5 of 127
446
4
h-index
University of Washington Applied Physics Laboratory, United States
4 publications · 990 citations
4
h-index
4
h-index
University of Washington Applied Physics Laboratory, United States
4 publications · 874 citations
4
h-index
3
h-index
1–5 of 446
204

Scripps Institution of Oceanography
La Jolla, United States
9 h-index
38 publications
6.1K citations
University of California San Diego
San Diego, United States
8 h-index
40 publications
6.7K citations
Oregon State University
Corvallis, United States
8 h-index
23 publications
2.6K citations
Woods Hole Oceanographic Institution
Falmouth, United States
7 h-index
16 publications
2.4K citations
University of Washington Applied Physics Laboratory
Seattle, United States
5 h-index
12 publications
553 citations
University of Washington
Seattle, United States
4 h-index
9 publications
3K citations

The University of Western Australia
Perth, Australia
4 h-index
9 publications
519 citations

National Taiwan University
Taipei, Taiwan
4 h-index
10 publications
3.8K citations
1–8 of 204
14 publications · 683 citations
13
h-index
9 publications · 441 citations
9
h-index
9 publications · 366 citations
9
h-index
JGR · 8 publications · 428 citations
8
h-index
5 publications · 157 citations
5
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1–5