Overturning Streamfunction

The "Overturning Streamfunction" is a diagnostic scalar function in physical oceanography that quantifies the meridional overturning circulation by representing the vertical and zonal integrals of the northward mass transport as a function of depth and latitude.

22

Publications

1.7K

Citations

53

Authors

19

Institutions

Publications per year

2017–2026

2

Variants

Meridional Overturning Streamfunction

Authors

53

  1. RM
    Robert Marsh

    National Oceanography Centre, United Kingdom

    2 publications · 91 citations

    2

    h-index

  2. JP
    Jeremy P. Grist

    National Oceanography Centre, United Kingdom

    2 publications · 91 citations

    2

    h-index

  3. AS
    Amy S. Bower

    Woods Hole Oceanographic Institution, United States

    2 publications · 115 citations

    2

    h-index

  4. SA
    Simon A. Josey

    National Oceanography Centre, United Kingdom

    2 publications · 91 citations

    2

    h-index

  5. LD
    Lynne D. Talley

    Scripps Institution of Oceanography, United States

    2 publications · 709 citations

    2

    h-index

1–5 of 53

Venues

  1. Journal of Physical Oceanography

    6 publications · 287 citations

    6

    h-index

  2. Journal of Climate

    4 publications · 481 citations

    4

    h-index

  3. Progress In Oceanography

    2 publications · 392 citations

    2

    h-index

  4. Journal of Marine Research

    2 publications · 61 citations

    2

    h-index

  5. Tellus A Dynamic Meteorology and Oceanography

    1 publications · 15 citations

    1

    h-index

1–5