Tidal Current Rectification
Tidal Current Rectification is a nonlinear hydrodynamic process in which asymmetries in flood and ebb tidal currents over complex bathymetry or through constrictions generate a residual, unidirectional flow that deviates from the purely oscillatory tidal signal.
22
Publications
1.4K
Citations
58
Authors
26
Institutions
Publications per year
2017–2026
2
Parents
22
1–5 of 22
58
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Woods Hole Oceanographic Institution, United States
4 publications · 325 citations
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3
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3
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2
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1–5 of 58
26
Woods Hole Oceanographic Institution
Falmouth, United States
3 h-index
4 publications
227 citations
Universidad Veracruzana
Xalapa, Mexico
3 h-index
7 publications
147 citations
Arizona State University
Tempe, United States
2 h-index
2 publications
27 citations
United States Geological Survey
Reston, United States
2 h-index
3 publications
121 citations
Bedford Institute of Oceanography
Dartmouth, Canada
2 h-index
4 publications
90 citations
Fisheries and Oceans Canada
Ottawa, Canada
2 h-index
4 publications
90 citations

Shanghai Ocean University
Shanghai, China
1 h-index
1 publications
106 citations
Instituto Tecnológico de Veracruz
Veracruz, Mexico
1 h-index
1 publications
12 citations
1–8 of 26
JGR · 9 publications · 688 citations
9
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7 publications · 503 citations
7
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1 publications · 23 citations
1
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1 publications · 12 citations
1
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1 publications · 36 citations
1
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