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
Parents
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Woods Hole Oceanographic Institution
Falmouth, United States
4 h-index
4 publications
158 citations

National Oceanography Centre
Southampton, United Kingdom
3 h-index
12 publications
459 citations
University of Southampton
Southampton, United Kingdom
2 h-index
2 publications
91 citations
University of California San Diego
San Diego, United States
2 h-index
4 publications
1.4K citations

Scripps Institution of Oceanography
La Jolla, United States
2 h-index
4 publications
1.2K citations
University of Miami
Coral Gables, United States
2 h-index
4 publications
113 citations
Duke University
Durham, United States
2 h-index
4 publications
230 citations

Old Dominion University
Norfolk, United States
1 h-index
1 publications
122 citations
1–8 of 19
6 publications · 287 citations
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4 publications · 481 citations
4
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2 publications · 392 citations
2
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2 publications · 61 citations
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1 publications · 15 citations
1
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1–5