Frontal Jets
Frontal Jets is a mesoscale oceanic phenomenon characterized by intense, narrow currents that form along the density gradient of oceanic fronts, distinguished from broader circulation patterns by their spatial confinement and dynamical association with frontal instabilities.
52
Publications
3.9K
Citations
128
Authors
70
Institutions
Publications per year
2017–2026
9
52
Yasu‐Masa Kodama · Journal of the Meteorological Society of Japan Ser II · 1993 · 212 citations · Full text
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128
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NSF National Center for Atmospheric Research, United States
2 publications · 55 citations
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2
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1–5 of 128
70
Woods Hole Oceanographic Institution
Falmouth, United States
6 h-index
7 publications
491 citations
University of Washington
Seattle, United States
3 h-index
3 publications
346 citations
Meteorological Research Institute
Tsukuba, Japan
3 h-index
3 publications
101 citations
Duke University
Durham, United States
3 h-index
3 publications
123 citations
Mediterranean Institute for Advanced Studies
Esporles, Spain
3 h-index
6 publications
307 citations

University of Hawaiʻi at Mānoa
Honolulu, United States
3 h-index
6 publications
628 citations
University of Washington Applied Physics Laboratory
Seattle, United States
3 h-index
7 publications
669 citations
Massachusetts Institute of Technology
Cambridge, United States
2 h-index
2 publications
219 citations
1–8 of 70
15 publications · 1K citations
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5 publications · 418 citations
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JGR · 4 publications · 391 citations
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3 publications · 106 citations
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3 publications · 61 citations
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