Topographic Upwelling
Topographic Upwelling is a physical oceanographic phenomenon in which the upward movement of deep, nutrient-rich water to the surface layer is induced by the interaction of ocean currents with underwater topographic features such as seamounts, ridges, or continental shelves.
17
Publications
1K
Citations
48
Authors
28
Institutions
Publications per year
2017–2026
1
Parents
17
1–5 of 17
48
2
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28
Bedford Institute of Oceanography
Dartmouth, Canada
2 h-index
3 publications
131 citations
Fisheries and Oceans Canada
Ottawa, Canada
2 h-index
2 publications
76 citations
North Carolina State University
Raleigh, United States
2 h-index
3 publications
245 citations
Arizona State University
Tempe, United States
1 h-index
1 publications
68 citations
Oregon State University
Corvallis, United States
1 h-index
1 publications
117 citations

University of Liverpool
Liverpool, United Kingdom
1 h-index
1 publications
21 citations

University of British Columbia
Vancouver, Canada
1 h-index
2 publications
48 citations

Instituto Nacional de Pesquisas Espaciais
São José dos Campos, Brazil
1 h-index
1 publications
192 citations
1–8 of 28
3 publications · 220 citations
3
h-index
3 publications · 291 citations
3
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2 publications · 45 citations
2
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JGR · 2 publications · 104 citations
2
h-index
1 publications · 68 citations
1
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1–5