Internal Wave-driven Circulation

Internal Wave-Driven Circulation is a coastal circulation mechanism in which sub-surface density-stratified water motions, generated by the propagation and dissipation of internal waves, induce time-averaged mass, momentum, and energy transport within the littoral and nearshore oceanic regimes.

127

Publications

5.9K

Citations

446

Authors

204

Institutions

Publications per year

2017–2026

27

Authors

446

  1. MC
    Ming‐Huei Chang

    National Taiwan University, Taiwan

    4 publications · 930 citations

    4

    h-index

  2. RL
    Ren‐Chieh Lien

    University of Washington Applied Physics Laboratory, United States

    4 publications · 990 citations

    4

    h-index

  3. AJ
    Andrew J. Lucas

    Scripps Institution of Oceanography, United States

    4 publications · 137 citations

    4

    h-index

  4. MH
    Matthew H. Alford

    University of Washington Applied Physics Laboratory, United States

    4 publications · 874 citations

    4

    h-index

  5. JK
    Jody Klymak

    University of Victoria, Canada

    3 publications · 762 citations

    3

    h-index

1–5 of 446

Venues

  1. Journal of Physical Oceanography

    14 publications · 683 citations

    13

    h-index

  2. Geophysical Research Letters

    9 publications · 441 citations

    9

    h-index

  3. Continental Shelf Research

    9 publications · 366 citations

    9

    h-index

  4. Journal of Geophysical Research Atmospheres

    JGR · 8 publications · 428 citations

    8

    h-index

  5. 5

    h-index

1–5