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

Authors

48

  1. YT
    Y. Tony Song

    Jet Propulsion Laboratory, United States

    2 publications · 95 citations

    2

    h-index

  2. TL
    T.N. Lee

    Skidaway Institute of Oceanography, United States

    1 publications · 121 citations

    1

    h-index

  3. MP
    MN. Paranaguá

    Universidade Federal do Rio Grande do Norte, Brazil

    1 publications · 64 citations

    1

    h-index

  4. RE
    Richard E. Thomson

    Fisheries and Oceans Canada, Canada

    1 publications · 20 citations

    1

    h-index

  5. JH
    Jason H. Middleton

    UNSW Sydney, Australia

    1 publications · 117 citations

    1

    h-index

1–5 of 48

Venues

  1. Journal of Physical Oceanography

    3 publications · 220 citations

    3

    h-index

  2. Continental Shelf Research

    3 publications · 291 citations

    3

    h-index

  3. Journal of Geophysical Research Oceans

    2 publications · 45 citations

    2

    h-index

  4. Journal of Geophysical Research Atmospheres

    JGR · 2 publications · 104 citations

    2

    h-index

  5. Earth and Planetary Science Letters

    1 publications · 68 citations

    1

    h-index

1–5