Front-associated Eddies
Front-Associated Eddies is a hydrodynamic phenomenon denoting a mesoscale coherent vortex structure that forms, persists, or intensifies in the vicinity of an ocean front due to baroclinic instability, shear instability, or frontogenetic processes, thereby mediating cross-frontal exchanges of heat, nutrients, and momentum.
27
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2.5K
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89
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54
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2017–2026
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Air–sea interaction over ocean fronts and eddies
Justin Small, Shang‐Ping Xie, Larry W. O’Neill et al. · Dynamics of Atmospheres and Oceans · 2008 · 832 citations · Full text
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NSF National Center for Atmospheric Research, United States
2 publications · 921 citations
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Woods Hole Oceanographic Institution
Falmouth, United States
3 h-index
4 publications
1K citations

University of Cape Town
Rondebosch, South Africa
2 h-index
2 publications
241 citations
Ifremer
Brest, France
2 h-index
9 publications
445 citations

Stennis Space Center
Bay Saint Louis, United States
2 h-index
3 publications
932 citations
Institut de Recherche pour le Développement
Marseille, France
2 h-index
8 publications
440 citations

Centre National de la Recherche Scientifique
Paris, France
2 h-index
8 publications
440 citations
Oregon State University
Corvallis, United States
2 h-index
5 publications
2.2K citations

Université de Bretagne Occidentale
Brest, France
2 h-index
5 publications
339 citations
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5 publications · 248 citations
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JGR · 3 publications · 123 citations
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3 publications · 294 citations
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2 publications · 140 citations
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2 publications · 925 citations
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