Baroclinic Tides

Baroclinic Tides is a tidal phenomenon within the broader category of internal tides, distinguished by the generation of vertically stratified, density-dependent currents due to the deformation of tidal waves across density gradients in a baroclinic ocean.

219

Publications

12.1K

Citations

521

Authors

195

Institutions

Publications per year

2017–2026

34

Authors

521

  1. RP
    Robert Pinkel

    Scripps Institution of Oceanography, United States

    8 publications · 531 citations

    8

    h-index

  2. MF
    Michael Foreman

    Fisheries and Oceans Canada, Canada

    7 publications · 609 citations

    7

    h-index

  3. ED
    Edward D. Zaron

    Portland State University, United States

    7 publications · 473 citations

    7

    h-index

  4. MA
    M. A. Merrifield

    University of Hawaiʻi at Mānoa, United States

    7 publications · 439 citations

    7

    h-index

  5. BP
    Brian Powell

    University of Hawaiʻi at Mānoa, United States

    6 publications · 333 citations

    6

    h-index

1–5 of 521

Venues

  1. Journal of Physical Oceanography

    54 publications · 3.4K citations

    35

    h-index

  2. Journal of Geophysical Research Atmospheres

    JGR · 41 publications · 2.3K citations

    27

    h-index

  3. Journal of Geophysical Research Oceans

    26 publications · 1.2K citations

    21

    h-index

  4. Geophysical Research Letters

    17 publications · 1.2K citations

    15

    h-index

  5. Journal of Fluid Mechanics

    5 publications · 210 citations

    5

    h-index

1–5