Thermocline Ventilation
Thermocline Ventilation is a physical oceanographic process referring to the downward transport of surface waters and associated properties into the thermocline layer through seasonal mixing, lateral advection, or subduction, thereby renewing the water mass composition and influencing heat, carbon, and nutrient distribution within the upper ocean.
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249
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2017–2026
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James R. Luyten, Joseph Pedlosky, Henry Stommel · Journal of Physical Oceanography · 1983 · 851 citations
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Woods Hole Oceanographic Institution
Falmouth, United States
13 h-index
23 publications
4K citations
University of Washington
Seattle, United States
11 h-index
24 publications
1.2K citations
Princeton University
Princeton, United States
5 h-index
6 publications
437 citations

National Oceanography Centre
Southampton, United Kingdom
5 h-index
10 publications
621 citations
NOAA Pacific Marine Environmental Laboratory
Seattle, United States
4 h-index
5 publications
317 citations
NOAA Geophysical Fluid Dynamics Laboratory
Princeton, United States
4 h-index
5 publications
365 citations

Lamont-Doherty Earth Observatory
Sparkill, United States
4 h-index
6 publications
384 citations
Planetary Science Institute
Tucson, United States
4 h-index
6 publications
132 citations
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39 publications · 3.7K citations
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JGR · 13 publications · 1.1K citations
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10 publications · 375 citations
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