Ocean Tidal Forcing is a geophysical forcing mechanism that arises from the gravitational interactions between the Earth, Moon, and Sun, specifically manifesting as periodic variations in oceanic water mass distribution and sea surface height that exert dynamic influence on ocean circulation, mixing, and Earth's rotational dynamics.
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217
Ocean self‐attraction and loading in numerical tidal models
Richard D. Ray · Marine Geodesy · 1998 · 223 citations
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Scripps Institution of Oceanography
La Jolla, United States
12 h-index
20 publications
1.6K citations
University of California San Diego
San Diego, United States
9 h-index
13 publications
1.2K citations
Goddard Space Flight Center
Greenbelt, United States
9 h-index
12 publications
544 citations
Woods Hole Oceanographic Institution
Falmouth, United States
9 h-index
12 publications
749 citations
California Institute of Technology
Pasadena, United States
8 h-index
17 publications
943 citations
Jet Propulsion Laboratory
Pasadena, United States
7 h-index
16 publications
788 citations
Chinese Academy of Sciences
Beijing, China
7 h-index
15 publications
1.2K citations
British Antarctic Survey
Cambridge, United Kingdom
7 h-index
11 publications
947 citations
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- Journal of Geophysical Research Atmospheres
JGR · 31 publications · 2K citations
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- Geophysical Research Letters
26 publications · 1.4K citations
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- Journal of Geophysical Research Oceans
12 publications · 549 citations
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- Journal of Physical Oceanography
12 publications · 811 citations
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- Annals of Glaciology
5 publications · 241 citations
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