Interior Ocean Flow

Interior Ocean Flow is a theoretical construct in physical oceanography that denotes the large-scale, steady, horizontal movement of seawater in the oceanic interior balanced primarily by the Coriolis force and pressure gradients, distinct from boundary currents and surface or bottom boundary layer flows.

105

Publications

7.5K

Citations

278

Authors

122

Institutions

Publications per year

2017–2026

20

Variants

Interior Ocean Circulation

Authors

278

  1. KS
    Kevin Speer

    Florida State University, United States

    3 publications · 274 citations

    3

    h-index

  2. AT
    Anne‐Marie Tréguier

    Ifremer, France

    3 publications · 299 citations

    3

    h-index

  3. JP
    Julian P. McCreary

    University of Hawaiʻi at Mānoa, United States

    3 publications · 133 citations

    3

    h-index

  4. BQ
    Bo Qiu

    University of Hawaiʻi at Mānoa, United States

    3 publications · 178 citations

    3

    h-index

  5. AW
    Anthony Wise

    National Oceanography Centre, United Kingdom

    2 publications · 139 citations

    2

    h-index

1–5 of 278

Venues

  1. Journal of Physical Oceanography

    44 publications · 2.3K citations

    28

    h-index

  2. Geophysical Research Letters

    8 publications · 236 citations

    8

    h-index

  3. Journal of Geophysical Research Atmospheres

    JGR · 7 publications · 359 citations

    7

    h-index

  4. Journal of Fluid Mechanics

    5 publications · 275 citations

    5

    h-index

  5. Journal of Climate

    5 publications · 668 citations

    5

    h-index

1–5