Mesoscale Eddy Response

Mesoscale Eddy Response is a geophysical process in which oceanic mesoscale eddies, typically 10–100 km in scale, modulate the upper ocean’s thermal, kinetic, and biological properties in reaction to atmospheric forcing or larger-scale flow changes, distinguishing it from broader oceanic responses by its characteristic spatial coherence and rotational dynamics.

397

Publications

26.3K

Citations

1.3K

Authors

386

Institutions

Publications per year

2017–2026

135

Authors

1.3K

  1. BQ
    Bo Qiu

    University of Hawaiʻi at Mānoa, United States

    9 publications · 628 citations

    9

    h-index

  2. DJ
    Dennis J. McGillicuddy

    Woods Hole Oceanographic Institution, United States

    7 publications · 2.2K citations

    7

    h-index

  3. GW
    Guihua Wang

    Second Institute of Oceanography, China

    6 publications · 151 citations

    6

    h-index

  4. JM
    John Marshall

    Massachusetts Institute of Technology, United States

    6 publications · 376 citations

    6

    h-index

  5. DW
    Dongxiao Wang

    South China Sea Institute Of Oceanology, China

    5 publications · 161 citations

    5

    h-index

1–5 of 1.3K

Venues

  1. Journal of Physical Oceanography

    41 publications · 2.9K citations

    29

    h-index

  2. 25

    h-index

  3. Journal of Geophysical Research Oceans

    23 publications · 1.5K citations

    22

    h-index

  4. Journal of Geophysical Research Atmospheres

    JGR · 35 publications · 1.9K citations

    22

    h-index

  5. Geophysical Research Letters

    21 publications · 1.2K citations

    18

    h-index

1–5