Front-induced Stratification Changes
Front-Induced Stratification Changes is a geophysical process characterized by the alteration of vertical density structure in the oceanic water column due to the convergence and divergence dynamics associated with oceanic fronts, distinguishing it from other forms of stratification variability by its direct mechanistic linkage to frontal circulation and associated lateral gradients in temperature and salinity.
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Meandering of the subtropical front south-east of the Azores
Rolf H. Käse, Gerold Siedler · Nature · 1982 · 110 citations
Michael P. Seki, Jeffrey J. Polovina, Donald R. Kobayashi et al. · Fisheries Oceanography · 2002 · 88 citations · Full text
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University of Washington
Seattle, United States
3 h-index
3 publications
160 citations
Woods Hole Oceanographic Institution
Falmouth, United States
3 h-index
4 publications
301 citations

Centre National de la Recherche Scientifique
Paris, France
2 h-index
10 publications
479 citations
Balearic Islands Coastal Observing and Forecasting System
Palma, Spain
2 h-index
7 publications
233 citations
Mediterranean Institute for Advanced Studies
Esporles, Spain
2 h-index
4 publications
121 citations
Massachusetts Institute of Technology
Cambridge, United States
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2 publications
220 citations
University of Washington Applied Physics Laboratory
Seattle, United States
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1 publications
25 citations
University of Liège
Liège, Belgium
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1 publications
29 citations
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5 publications · 418 citations
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JGR · 3 publications · 72 citations
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