Mesoscale Eddy Variability is a geophysical phenomenon characterized by fluctuations in the spatial and temporal distribution of mesoscale ocean eddies, distinguished by their intermediate scale of motion (typically 10–100 kilometers) that modulate tracer transport, kinetic energy, and momentum within the general ocean circulation.
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Xavier Capet, J. C. McWilliams, M. Jeroen Molemaker et al. · Journal of Physical Oceanography · 2008 · 711 citations · Full text
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University of Hawaiʻi at Mānoa
Honolulu, United States
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Institute of Oceanology
Qingdao, China
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Centre National de la Recherche Scientifique
Paris, France
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Chinese Academy of Sciences
Beijing, China
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South China Sea Institute Of Oceanology
Guangzhou, China
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Institut de Recherche pour le Développement
Marseille, France
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Brest, France
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Woods Hole Oceanographic Institution
Falmouth, United States
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- Deep Sea Research Part II Topical Studies in Oceanography
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