Internal Tides

Internal Tides is an oceanic wave phenomenon characterized as a type of internal gravity wave generated when barotropic tidal currents interact with underwater topography, distinguished by its propagation within the stratified interior of the ocean rather than at the surface.

795

Publications

47.6K

Citations

1.3K

Authors

456

Institutions

Publications per year

2017–2026

171

Authors

1.3K

  1. MH
    Matthew H. Alford

    University of Washington Applied Physics Laboratory, United States

    39 publications · 2.9K citations

    29

    h-index

  2. ZZ
    Zhongxiang Zhao

    University of Washington Applied Physics Laboratory, United States

    32 publications · 2.2K citations

    27

    h-index

  3. JD
    Jonathan D. Nash

    Oregon State University, United States

    24 publications · 2.7K citations

    24

    h-index

  4. GS
    Glenn S. Carter

    University of Hawaiʻi at Mānoa, United States

    21 publications · 2K citations

    19

    h-index

  5. PE
    Peter E. Holloway

    UNSW Sydney, Australia

    20 publications · 2.3K citations

    19

    h-index

1–5 of 1.3K

Venues

  1. Journal of Physical Oceanography

    193 publications · 14.2K citations

    70

    h-index

  2. Journal of Geophysical Research Atmospheres

    JGR · 103 publications · 7.3K citations

    51

    h-index

  3. Geophysical Research Letters

    69 publications · 4.3K citations

    36

    h-index

  4. Journal of Geophysical Research Oceans

    78 publications · 3.4K citations

    35

    h-index

  5. Journal of Fluid Mechanics

    26 publications · 1K citations

    20

    h-index

1–5