Tidal Height Forcing
Tidal Height Forcing is a geophysical forcing mechanism that represents the spatially varying gravitational and loading effects of ocean tidal mass redistribution, distinguished by its role in inducing elastic deformation of the Earth's crust through the dynamic pressure exerted by tidally varying sea-surface height.
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2017–2026
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Francis O’Beirn, M.W. Luchenbach, Janet A. Nestlerode et al. · W&M Publish (College of William & Mary) · 2000 · 76 citations · Full text
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Instituto Nacional de Investigacion y Desarrollo Pesquero, Argentina
1 publications · 15 citations
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1 publications · 76 citations
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Rhodes University
Grahamstown, South Africa
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7 publications
330 citations
Institute of Marine and Coastal Research
Mar del Plata, Argentina
1 h-index
1 publications
15 citations
Harvard University
Cambridge, United States
1 h-index
2 publications
114 citations
Research Institute for Humanity and Nature
Kyoto, Japan
1 h-index
1 publications
60 citations
Instituto Nacional de Investigacion y Desarrollo Pesquero
Mar del Plata, Argentina
1 h-index
1 publications
15 citations
University of California, Santa Barbara
Santa Barbara, United States
1 h-index
2 publications
114 citations

University of San Diego
San Diego, United States
1 h-index
1 publications
29 citations
Florida State University
Tallahassee, United States
1 h-index
3 publications
180 citations
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2 publications · 99 citations
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1 publications · 15 citations
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1 publications · 33 citations
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1 publications · 60 citations
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1 publications · 57 citations
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