Ocean Basin Response
Ocean Basin Response is a hydrodynamic phenomenon denoting the collective, large-scale adjustment of seawater within an ocean basin to gravitational forcing by the Moon and Sun during spring tides, characterized by amplified tidal currents and elevated water levels resulting from resonant interactions between tidal waves and basin morphology.
67
Publications
5.1K
Citations
230
Authors
153
Institutions
Publications per year
2017–2026
10
Parents
67
Continent and Ocean Basin Evolution by Spreading of the Sea Floor
Robert S. Dietz · Nature · 1961 · 651 citations
1–5 of 67
230
2
h-index
2
h-index
2
h-index
2
h-index
1
h-index
1–5 of 230
153

Centre National de la Recherche Scientifique
Paris, France
4 h-index
6 publications
436 citations
Woods Hole Oceanographic Institution
Falmouth, United States
4 h-index
4 publications
92 citations
University of California, Los Angeles
Los Angeles, United States
4 h-index
7 publications
356 citations
University of Bergen
Bergen, Norway
3 h-index
5 publications
273 citations

UNSW Sydney
Sydney, Australia
2 h-index
8 publications
672 citations

Scripps Institution of Oceanography
La Jolla, United States
2 h-index
2 publications
78 citations

Aarhus University
Aarhus, Denmark
2 h-index
6 publications
565 citations
Bjerknes Centre for Climate Research
Bergen, Norway
2 h-index
3 publications
207 citations
1–8 of 153
9 publications · 524 citations
9
h-index
5 publications · 271 citations
5
h-index
JGR · 5 publications · 512 citations
5
h-index
5 publications · 920 citations
5
h-index
3 publications · 194 citations
3
h-index
1–5