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
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24K
Citations
748
Authors
359
Institutions
Publications per year
2017–2026
49
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359

Centre National de la Recherche Scientifique
Paris, France
27 h-index
102 publications
12.8K citations
Woods Hole Oceanographic Institution
Falmouth, United States
23 h-index
41 publications
13.5K citations

Lamont-Doherty Earth Observatory
Sparkill, United States
19 h-index
35 publications
4.3K citations
Laboratoire des Sciences du Climat et de l'Environnement
Gif-sur-Yvette, France
18 h-index
55 publications
10.3K citations
Commissariat à l'Énergie Atomique et aux Énergies Alternatives
Paris, France
17 h-index
56 publications
8.2K citations
Alfred-Wegener-Institut Helmholtz-Zentrum für Polar- und Meeresforschung
Bremerhaven, Germany
15 h-index
24 publications
2.1K citations
Columbia University
New York, United States
13 h-index
24 publications
2.5K citations
University of Cambridge
Cambridge, United Kingdom
12 h-index
21 publications
2.4K citations
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31 publications · 2.9K citations
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15 publications · 849 citations
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14 publications · 973 citations
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