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.

10

Publications

410

Citations

31

Authors

16

Institutions

Publications per year

2017–2026

2

Authors

31

  1. CD
    Christopher D. McQuaid

    Rhodes University, South Africa

    2 publications · 99 citations

    2

    h-index

  2. EM
    E. Marcelo

    Instituto Nacional de Investigacion y Desarrollo Pesquero, Argentina

    1 publications · 15 citations

    1

    h-index

  3. KM
    Kenneth M. Brown

    Louisiana State University, United States

    1 publications · 20 citations

    1

    h-index

  4. GC
    G.M. Coates

    1 publications · 76 citations

    1

    h-index

  5. MT
    Makoto Taniguchi

    Research Institute for Humanity and Nature, Japan

    1 publications · 60 citations

    1

    h-index

1–5 of 31

Venues

  1. Marine Biology

    2 publications · 99 citations

    2

    h-index

  2. Estuarine Coastal and Shelf Science

    1 publications · 15 citations

    1

    h-index

  3. 1

    h-index

  4. Biogeochemistry

    1 publications · 60 citations

    1

    h-index

  5. Frontiers in Environmental Science

    1 publications · 57 citations

    1

    h-index

1–5