Mesoscale Eddy Circulation

Mesoscale Eddy Circulation is a transient oceanic circulation phenomenon characterized by rotational water movements on spatial scales of approximately 10 to 100 kilometers that arise from instabilities in large-scale currents and play a critical role in the lateral transport of heat, salt, and nutrients within the deep-sea environment.

444

Publications

27K

Citations

1.3K

Authors

447

Institutions

Publications per year

2017–2026

110

Authors

1.3K

  1. JC
    James C. McWilliams

    University of California, Los Angeles, United States

    8 publications · 3.6K citations

    8

    h-index

  2. JM
    John Marshall

    Massachusetts Institute of Technology, United States

    6 publications · 380 citations

    6

    h-index

  3. VÉ
    Vincent Échevin

    Laboratoire d'Océanographie et du Climat : Expérimentations et Approches Numériques, France

    6 publications · 191 citations

    6

    h-index

  4. BQ
    Bo Qiu

    University of Hawaiʻi at Mānoa, United States

    5 publications · 788 citations

    5

    h-index

  5. SR
    Simón Ruíz

    Mediterranean Institute for Advanced Studies, Spain

    5 publications · 281 citations

    5

    h-index

1–5 of 1.3K

Venues

  1. Journal of Geophysical Research Atmospheres

    JGR · 66 publications · 4.3K citations

    40

    h-index

  2. Journal of Physical Oceanography

    62 publications · 7.1K citations

    36

    h-index

  3. Journal of Geophysical Research Oceans

    45 publications · 2.2K citations

    28

    h-index

  4. Geophysical Research Letters

    21 publications · 1.2K citations

    20

    h-index

  5. 16

    h-index

1–5