Thermocline Structure

Thermocline Structure is a stratification construct that delineates the vertical gradient of temperature in the water column, distinguishing itself from other oceanic density interfaces by characterizing the depth, strength, and thickness of the transitional layer separating the mixed surface layer from the deeper, denser waters.

1.1K

Publications

68.9K

Citations

2.5K

Authors

705

Institutions

Publications per year

2017–2026

154

Authors

2.5K

  1. WC
    Wenju Cai

    CSIRO Oceans and Atmosphere, Australia

    12 publications · 464 citations

    12

    h-index

  2. MJ
    Michael J. McPhaden

    NOAA Pacific Marine Environmental Laboratory, United States

    12 publications · 703 citations

    12

    h-index

  3. ZL
    Zhengyu Liu

    University of Wisconsin–Madison, United States

    11 publications · 572 citations

    11

    h-index

  4. AL
    Arnold L. Gordon

    Lamont-Doherty Earth Observatory, United States

    21 publications · 2.2K citations

    11

    h-index

  5. SX
    Shang‐Ping Xie

    Scripps Institution of Oceanography, United States

    10 publications · 1.1K citations

    10

    h-index

1–5 of 2.5K

Venues

  1. Journal of Physical Oceanography

    185 publications · 11.2K citations

    59

    h-index

  2. Journal of Geophysical Research Atmospheres

    JGR · 137 publications · 10.7K citations

    53

    h-index

  3. Geophysical Research Letters

    100 publications · 6K citations

    45

    h-index

  4. Journal of Climate

    64 publications · 5.4K citations

    42

    h-index

  5. Paleoceanography

    29 publications · 2.4K citations

    24

    h-index

1–5