Subtropical Convergence
Subtropical Convergence is a large-scale oceanic surface phenomenon characterized by the gradual sinking of water masses due to the convergence of wind-driven Ekman transport in subtropical gyres, distinguishing it from other convergence zones by its location at approximately 20°–30° latitude and its role in initiating subtropical mode water formation.
185
Publications
11.8K
Citations
488
Authors
187
Institutions
Publications per year
2017–2026
14
Parents
185
Yasu‐Masa Kodama · Journal of the Meteorological Society of Japan Ser II · 1992 · 495 citations
U. Seeliger, Clarisse Odebrecht, Jorge Pablo Castello · Time to knit · 2000 · 379 citations
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488
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187
National Institute of Water and Atmospheric Research
Auckland, New Zealand
18 h-index
34 publications
2K citations

University of Otago
Dunedin, New Zealand
12 h-index
24 publications
1.5K citations

University of Cape Town
Rondebosch, South Africa
9 h-index
18 publications
416 citations

Rhodes University
Grahamstown, South Africa
8 h-index
22 publications
754 citations
CSIRO Oceans and Atmosphere
Canberra, Australia
8 h-index
24 publications
1.2K citations
Universidade Federal do Rio Grande
Rio Grande, Brazil
7 h-index
15 publications
1.7K citations
University of Copenhagen
Copenhagen, Denmark
6 h-index
11 publications
233 citations
Technical University of Denmark
Kongens Lyngby, Denmark
6 h-index
12 publications
193 citations
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NZJM · 20 publications · 861 citations
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JGR · 19 publications · 1K citations
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MEPS · 10 publications · 482 citations
10
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9 publications · 318 citations
9
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7 publications · 320 citations
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