Buoyancy-driven Overturning

Buoyancy-Driven Overturning is a theoretical construct within physical oceanography that represents the large-scale meridional circulation of seawater driven primarily by differences in water density, where variations in temperature and salinity induce vertical motions that sustain a overturning flow distinct from wind-driven or eddy-mediated circulations.

63

Publications

4.6K

Citations

186

Authors

103

Institutions

Publications per year

2017–2026

17

Authors

186

  1. MS
    M. Susan Lozier

    Duke University, United States

    4 publications · 520 citations

    4

    h-index

  2. RW
    R. W. Griffiths

    Australian National University, Australia

    3 publications · 130 citations

    3

    h-index

  3. GM
    Gurvan Madec

    Centre National de la Recherche Scientifique, France

    3 publications · 192 citations

    3

    h-index

  4. FS
    Fabian Schloesser

    University of Hawaiʻi at Mānoa, United States

    3 publications · 199 citations

    3

    h-index

  5. JS
    Jean‐Baptiste Sallée

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

    3 publications · 426 citations

    3

    h-index

1–5 of 186

Venues

  1. Journal of Physical Oceanography

    11 publications · 755 citations

    11

    h-index

  2. Climate Dynamics

    7 publications · 268 citations

    7

    h-index

  3. Journal of Geophysical Research Oceans

    6 publications · 696 citations

    6

    h-index

  4. Geophysical Research Letters

    5 publications · 346 citations

    5

    h-index

  5. 3

    h-index

1–5