Wintertime Surface Cooling

Wintertime Surface Cooling is a climatological process denoting the net loss of heat from the ocean's surface layer to the atmosphere during the winter months, primarily driven by atmospheric heat exchange, which enhances surface water density and can initiate deep convection in high-latitude regions.

119

Publications

7.2K

Citations

410

Authors

181

Institutions

Publications per year

2017–2026

40

Authors

410

  1. JC
    Judah Cohen

    Atmospheric and Environmental Research, United States

    3 publications · 790 citations

    3

    h-index

  2. MR
    M. R. van den Broeke

    Utrecht University, Netherlands

    3 publications · 251 citations

    3

    h-index

  3. AR
    Alan Robock

    Rutgers, The State University of New Jersey, United States

    3 publications · 538 citations

    3

    h-index

  4. HR
    H. Renssen

    Vrije Universiteit Amsterdam, Netherlands

    2 publications · 184 citations

    2

    h-index

  5. PJ
    Paul J. Kushner

    University of Toronto, Canada

    2 publications · 255 citations

    2

    h-index

1–5 of 410

Venues

  1. Geophysical Research Letters

    13 publications · 1.3K citations

    13

    h-index

  2. Journal of Geophysical Research Atmospheres

    JGR · 17 publications · 891 citations

    13

    h-index

  3. Journal of Physical Oceanography

    8 publications · 1.1K citations

    8

    h-index

  4. Climate Dynamics

    6 publications · 132 citations

    7

    h-index

  5. Journal of Climate

    5 publications · 251 citations

    5

    h-index

1–5