Baroclinic Circulation is an ocean circulation characterized by the misalignment between pressure and density gradients, resulting in fluid motion driven by horizontal density variations due to temperature and salinity differences.
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Open‐ocean convection: Observations, theory, and models
John Marshall, Friedrich Schott · Reviews of Geophysics · 1999 · 1.3K citations
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Woods Hole Oceanographic Institution
Falmouth, United States
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Scripps Institution of Oceanography
La Jolla, United States
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NOAA Geophysical Fluid Dynamics Laboratory
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Princeton, United States
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Centre National de la Recherche Scientifique
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Institute of Oceanology
Qingdao, China
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