Mixed Layer Circulation

Mixed Layer Circulation is a wind-driven ocean circulation process that occurs within the upper, homogenized layer of the ocean where turbulent mixing homogenizes temperature and salinity, distinguishing it from deeper, stratified circulations by its direct responsiveness to surface wind stress and buoyancy forcing.

114

Publications

7.4K

Citations

339

Authors

148

Institutions

Publications per year

2017–2026

19

Authors

339

  1. JF
    James F. Price

    Woods Hole Oceanographic Institution, United States

    4 publications · 739 citations

    4

    h-index

  2. ML
    Ming Li

    University of Maryland Center for Environmental Science, United States

    3 publications · 303 citations

    3

    h-index

  3. SG
    Sven‐Erik Gryning

    Technical University of Denmark, Denmark

    2 publications · 275 citations

    2

    h-index

  4. CS
    Cristina Schultz

    University of Virginia, United States

    2 publications · 27 citations

    2

    h-index

  5. WC
    William C. Boicourt

    University of Maryland Center for Environmental Science, United States

    2 publications · 108 citations

    2

    h-index

1–5 of 339

Venues

  1. Journal of Physical Oceanography

    30 publications · 1.7K citations

    21

    h-index

  2. Journal of Geophysical Research Atmospheres

    JGR · 14 publications · 1.3K citations

    13

    h-index

  3. Journal of Geophysical Research Oceans

    6 publications · 159 citations

    6

    h-index

  4. Journal of Marine Research

    3 publications · 336 citations

    3

    h-index

  5. Journal of the Atmospheric Sciences

    3 publications · 258 citations

    3

    h-index

1–5