Barotropic Tides

Barotropic Tides is a tidal dynamics phenomenon characterized by horizontal water motion driven by gravitational forcing, wherein the tidal wave propagates across the ocean surface with minimal vertical shear, distinguishing it from internal (baroclinic) tides by its depth-independent flow structure.

138

Publications

12.3K

Citations

385

Authors

183

Institutions

Publications per year

2017–2026

29

Authors

385

  1. FL
    Florent Lyard

    Laboratoire d’Études en Géophysique et Océanographie Spatiales, France

    5 publications · 324 citations

    5

    h-index

  2. GD
    G. D. Egbert

    Oregon State University, United States

    5 publications · 5.2K citations

    5

    h-index

  3. MC
    Maarten C. Buijsman

    University of Southern Mississippi, United States

    5 publications · 415 citations

    5

    h-index

  4. BK
    Brian K. Arbic

    University of Michigan, United States

    5 publications · 350 citations

    5

    h-index

  5. JF
    Jay F. Shriver

    Stennis Space Center, United States

    4 publications · 338 citations

    4

    h-index

1–5 of 385

Venues

  1. Journal of Geophysical Research Atmospheres

    JGR · 33 publications · 2.2K citations

    27

    h-index

  2. Journal of Physical Oceanography

    24 publications · 1.2K citations

    21

    h-index

  3. Journal of Geophysical Research Oceans

    14 publications · 620 citations

    13

    h-index

  4. Geophysical Research Letters

    7 publications · 1.2K citations

    7

    h-index

  5. Continental Shelf Research

    7 publications · 482 citations

    7

    h-index

1–5