Tidal Current Amplification
Tidal Current Amplification is a hydrodynamic phenomenon characterized by the localized intensification of tidal current velocities due to the interaction of tidal forces with coastal or seabed topography, distinguishing it from general tidal currents through its dependence on geometric and bathymetric focusing effects.
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2017–2026
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Chris Garrett, Patrick F. Cummins · Renewable Energy · 2008 · 113 citations
Diurnal tides near the Yermak Plateau
Laurie Padman, Albert J. Plueddemann, Robin D. Muench et al. · Journal of Geophysical Research Atmospheres · 1992 · 111 citations
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NSF National Center for Atmospheric Research
Boulder, United States
2 h-index
2 publications
55 citations
Bedford Institute of Oceanography
Dartmouth, Canada
2 h-index
7 publications
270 citations
NSF NCAR High Altitude Observatory
Boulder, United States
2 h-index
2 publications
55 citations

Inha University
Incheon, South Korea
1 h-index
4 publications
44 citations
Canadian Hydrographic Service
Ottawa, Canada
1 h-index
6 publications
258 citations
National Centre for Polar and Ocean Research
Vasco, India
1 h-index
1 publications
22 citations
Woods Hole Oceanographic Institution
Falmouth, United States
1 h-index
2 publications
58 citations
Universiti Tunku Abdul Rahman
Kampar, Malaysia
1 h-index
2 publications
176 citations
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JGR · 7 publications · 491 citations
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4 publications · 239 citations
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3 publications · 63 citations
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2 publications · 29 citations
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1 publications · 25 citations
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