Tidal Stratification Effects
Tidal Stratification Effects is a hydrodynamic phenomenon in coastal oceanography referring to the vertical layering of water masses induced by the interaction between tidal currents and density gradients, where differential advection and shear instability disrupt homogeneous mixing, thereby modulating sediment transport, nutrient flux, and biological productivity.
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9.1K
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412
Authors
180
Institutions
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2017–2026
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British Oceanographic Data Centre
Liverpool, United Kingdom
9 h-index
13 publications
537 citations

Bangor University
Bangor, United Kingdom
8 h-index
21 publications
1.6K citations
University of Florida
Gainesville, United States
7 h-index
7 publications
293 citations
University College of the North
The Pas, Canada
5 h-index
17 publications
4.6K citations
Bedford Institute of Oceanography
Dartmouth, Canada
5 h-index
7 publications
433 citations

East China Normal University
Shanghai, China
5 h-index
26 publications
532 citations
Helmholtz-Zentrum Hereon
Geesthacht, Germany
4 h-index
6 publications
185 citations

Leibniz Institute for Baltic Sea Research Warnemünde
Warnemünde, Germany
4 h-index
8 publications
615 citations
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JGR · 18 publications · 1.5K citations
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12 publications · 904 citations
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10 publications · 423 citations
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7 publications · 341 citations
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6 publications · 140 citations
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