Interior Ocean Flow
Interior Ocean Flow is a theoretical construct in physical oceanography that denotes the large-scale, steady, horizontal movement of seawater in the oceanic interior balanced primarily by the Coriolis force and pressure gradients, distinct from boundary currents and surface or bottom boundary layer flows.
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7.5K
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278
Authors
122
Institutions
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2017–2026
20
Variants
Interior Ocean Circulation
Parents
105
Vertical eddy diffusivity in the ocean interior
Ann E. Gargett · Journal of Marine Research · 1984 · 448 citations
Continuous, Array-Based Estimates of Atlantic Ocean Heat Transport at 26.5°N
William E. Johns, Molly Baringer, Lisa M. Beal et al. · Journal of Climate · 2010 · 440 citations · Full text
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Woods Hole Oceanographic Institution
Falmouth, United States
13 h-index
17 publications
1.1K citations
Massachusetts Institute of Technology
Cambridge, United States
8 h-index
14 publications
827 citations

National Oceanography Centre
Southampton, United Kingdom
6 h-index
16 publications
2.3K citations

Scripps Institution of Oceanography
La Jolla, United States
6 h-index
12 publications
291 citations
University of California San Diego
San Diego, United States
5 h-index
11 publications
298 citations
Florida State University
Tallahassee, United States
4 h-index
7 publications
561 citations

University of Hawaiʻi at Mānoa
Honolulu, United States
4 h-index
8 publications
393 citations

UNSW Sydney
Sydney, Australia
4 h-index
7 publications
358 citations
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44 publications · 2.3K citations
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8 publications · 236 citations
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JGR · 7 publications · 359 citations
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5 publications · 275 citations
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5 publications · 668 citations
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