Subtropical Convergence

Subtropical Convergence is a large-scale oceanic surface phenomenon characterized by the gradual sinking of water masses due to the convergence of wind-driven Ekman transport in subtropical gyres, distinguishing it from other convergence zones by its location at approximately 20°–30° latitude and its role in initiating subtropical mode water formation.

185

Publications

11.8K

Citations

488

Authors

187

Institutions

Publications per year

2017–2026

14

Authors

488

  1. PW
    P. William Froneman

    Rhodes University, South Africa

    7 publications · 232 citations

    7

    h-index

  2. RP
    Renzo Perissinotto

    University of KwaZulu-Natal, South Africa

    7 publications · 311 citations

    7

    h-index

  3. PM
    Peter Munk

    Technical University of Denmark, Denmark

    6 publications · 129 citations

    6

    h-index

  4. RA
    Robert A. Weller

    Woods Hole Oceanographic Institution, United States

    5 publications · 197 citations

    5

    h-index

  5. LR
    Lasse Riemann

    University of Copenhagen, Denmark

    5 publications · 117 citations

    5

    h-index

1–5 of 488

Venues

  1. New Zealand Journal of Marine and Freshwater Research

    NZJM · 20 publications · 861 citations

    17

    h-index

  2. Journal of Geophysical Research Atmospheres

    JGR · 19 publications · 1K citations

    16

    h-index

  3. Marine Ecology Progress Series

    MEPS · 10 publications · 482 citations

    10

    h-index

  4. Journal of Plankton Research

    9 publications · 318 citations

    9

    h-index

  5. 8

    h-index

1–5