Interglacial Circulation Changes is a paleoceanographic phenomenon characterized by alterations in the global thermohaline circulation system during interglacial periods, distinguished from glacial states by shifts in temperature, salinity, and freshwater forcing that modulate deep-water formation and meridional overturning patterns.
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Global warming preceded by increasing carbon dioxide concentrations during the last deglaciation
Jeremy D. Shakun, Peter U. Clark, Feng He et al. · Nature · 2012 · 1.5K citations · Full text
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Centre National de la Recherche Scientifique
Paris, France
20 h-index
69 publications
6.4K citations
Woods Hole Oceanographic Institution
Falmouth, United States
13 h-index
27 publications
5.5K citations
University of Bergen
Bergen, Norway
12 h-index
19 publications
2.5K citations
Commissariat à l'Énergie Atomique et aux Énergies Alternatives
Paris, France
11 h-index
21 publications
1.4K citations
Planetary Science Institute
Tucson, United States
10 h-index
11 publications
2.3K citations
Bjerknes Centre for Climate Research
Bergen, Norway
10 h-index
23 publications
1.8K citations
Alfred-Wegener-Institut Helmholtz-Zentrum für Polar- und Meeresforschung
Bremerhaven, Germany
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Lamont-Doherty Earth Observatory
Sparkill, United States
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- Earth and Planetary Science Letters
9 publications · 366 citations
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- Geophysical Research Letters
8 publications · 443 citations
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