Deglacial Circulation Changes

Deglacial Circulation Changes is a paleoceanographic phenomenon characterized by the systematic reorganization of Atlantic Meridional Overturning Circulation patterns during the transition from the Last Glacial Maximum to the Holocene, distinguished by temporally resolved shifts in water mass properties, strength, and structure driven by meltwater forcing and climatic feedbacks.

219

Publications

24K

Citations

748

Authors

359

Institutions

Publications per year

2017–2026

49

Authors

748

  1. JL
    Jean Lynch‐Stieglitz

    Georgia Institute of Technology, United States

    8 publications · 501 citations

    8

    h-index

  2. JF
    Jerry F McManus

    Lamont-Doherty Earth Observatory, United States

    8 publications · 3K citations

    8

    h-index

  3. DW
    Delia W Oppo

    Woods Hole Oceanographic Institution, United States

    7 publications · 495 citations

    7

    h-index

  4. CW
    Claire Waelbroeck

    Centre National de la Recherche Scientifique, France

    6 publications · 546 citations

    6

    h-index

  5. IN
    I Nick McCave

    University of Cambridge, United Kingdom

    6 publications · 623 citations

    6

    h-index

1–5 of 748

Venues

  1. Paleoceanography

    31 publications · 2.9K citations

    27

    h-index

  2. Quaternary Science Reviews

    26 publications · 2.2K citations

    24

    h-index

  3. Nature

    19 publications · 6.4K citations

    18

    h-index

  4. Earth and Planetary Science Letters

    15 publications · 849 citations

    15

    h-index

  5. Geology

    14 publications · 973 citations

    13

    h-index

1–5