Tide-driven Flows

Tide-Driven Flows is a hydrodynamic phenomenon characterized by the periodic movement of water in coastal regions resulting from the gravitational interactions between the Earth, Moon, and Sun, distinguished by its dominant forcing mechanism being tidal elevation gradients rather than wind, river discharge, or atmospheric pressure changes.

40

Publications

1.8K

Citations

133

Authors

71

Institutions

Publications per year

2017–2026

7

Variants

Tidal Flows

Authors

133

  1. PL
    Patrice Le Gal

    Centre National de la Recherche Scientifique, France

    3 publications · 347 citations

    3

    h-index

  2. ML
    Michaël Le Bars

    Institut de Recherche sur les Phénomènes Hors Équilibre, France

    3 publications · 347 citations

    3

    h-index

  3. DM
    Doris Meyer

    2 publications · 48 citations

    2

    h-index

  4. DC
    David Cébron

    Centre National de la Recherche Scientifique, France

    2 publications · 272 citations

    2

    h-index

  5. GM
    Gerd Masselink

    University of Plymouth, United Kingdom

    1 publications · 25 citations

    1

    h-index

1–5 of 133

Venues

  1. Estuarine Coastal and Shelf Science

    3 publications · 130 citations

    3

    h-index

  2. Journal of Hydrology

    3 publications · 108 citations

    3

    h-index

  3. Marine Geology

    2 publications · 83 citations

    2

    h-index

  4. Journal of Geophysical Research Atmospheres

    JGR · 2 publications · 97 citations

    2

    h-index

  5. World Literature Today

    WLT · 1 publications · 14 citations

    1

    h-index

1–5