Eastern Boundary Currents

Eastern Boundary Currents is a type of eastern boundary intensification within ocean gyres, characterized by cool, slow, broad, and nutrient-rich surface currents that flow equatorward along the eastern edges of subtropical ocean basins, driven by wind stress and modulated by coastal upwelling dynamics.

348

Publications

25.5K

Citations

1K

Authors

382

Institutions

Publications per year

2017–2026

65

Authors

1K

  1. SH
    Samuel Hormazábal

    University of Concepción, Chile

    7 publications · 347 citations

    7

    h-index

  2. AH
    Alonso Hernández‐Guerra

    Universidad de Las Palmas de Gran Canaria, Spain

    6 publications · 266 citations

    6

    h-index

  3. JS
    J. S. Godfrey

    CSIRO Oceans and Atmosphere, Australia

    5 publications · 693 citations

    5

    h-index

  4. JP
    Julian P. McCreary

    University of Hawaiʻi at Mānoa, United States

    5 publications · 280 citations

    5

    h-index

  5. SJ
    Steven J. Bograd

    NOAA National Marine Fisheries Service Southwest Fisheries Science Center, United States

    5 publications · 1.1K citations

    5

    h-index

1–5 of 1K

Venues

  1. Journal of Physical Oceanography

    63 publications · 4.6K citations

    35

    h-index

  2. Journal of Geophysical Research Atmospheres

    JGR · 42 publications · 4.6K citations

    31

    h-index

  3. Journal of Geophysical Research Oceans

    32 publications · 1.3K citations

    21

    h-index

  4. Geophysical Research Letters

    19 publications · 1.3K citations

    16

    h-index

  5. Journal of Climate

    10 publications · 898 citations

    10

    h-index

1–5