Ocean Surface Cooling

Ocean Surface Cooling is a physical oceanographic phenomenon characterized by the reduction in temperature of the upper ocean layer due to heat loss to the atmosphere, primarily driven by turbulent fluxes, radiative processes, and entrainment at the sea surface.

294

Publications

25.9K

Citations

1K

Authors

406

Institutions

Publications per year

2017–2026

83

Authors

1K

  1. IL
    I.‐I. Lin

    National Taiwan University, Taiwan

    6 publications · 660 citations

    6

    h-index

  2. JK
    J. K. Willis

    Jet Propulsion Laboratory, United States

    5 publications · 718 citations

    5

    h-index

  3. ML
    Matthieu Lengaigne

    Laboratoire d'Océanographie et du Climat : Expérimentations et Approches Numériques, France

    5 publications · 615 citations

    5

    h-index

  4. GC
    Gregory C. Johnson

    NOAA Pacific Marine Environmental Laboratory, United States

    5 publications · 671 citations

    5

    h-index

  5. GM
    Gurvan Madec

    Centre National de la Recherche Scientifique, France

    4 publications · 599 citations

    4

    h-index

1–5 of 1K

Venues

  1. Geophysical Research Letters

    39 publications · 2.7K citations

    27

    h-index

  2. Journal of Climate

    22 publications · 4.1K citations

    20

    h-index

  3. Journal of Geophysical Research Atmospheres

    JGR · 27 publications · 2.8K citations

    20

    h-index

  4. Journal of Physical Oceanography

    25 publications · 1.2K citations

    19

    h-index

  5. Journal of Geophysical Research Oceans

    20 publications · 801 citations

    16

    h-index

1–5