Glacial Terminations
Glacial Termination is a geological transition event characterized by the rapid shift from glacial to interglacial conditions within the Earth's climate system, distinguished by sustained global warming, ice sheet disintegration, and associated rises in sea level during the late Quaternary period.
227
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22.5K
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895
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423
Institutions
Publications per year
2017–2026
51
Variants
Glacial Termination
227
The snowball Earth hypothesis: testing the limits of global change
Paul F. Hoffman, Daniel P. Schrag · Terra Nova · 2002 · 1.6K citations
George H. Denton, Robert F. Anderson, J. R. Toggweiler et al. · Science · 2010 · 965 citations
Hai Cheng, R. Lawrence Edwards, Wallace S. Broecker et al. · Science · 2009 · 949 citations
Svante Björck, M. J. C. Walker, Les C. Cwynar et al. · Journal of Quaternary Science · 1998 · 875 citations
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Lamont-Doherty Earth Observatory
Sparkill, United States
15 h-index
35 publications
8.2K citations
University of Bern
Bern, Switzerland
14 h-index
26 publications
2.6K citations

Centre National de la Recherche Scientifique
Paris, France
14 h-index
51 publications
3.6K citations
Alfred-Wegener-Institut Helmholtz-Zentrum für Polar- und Meeresforschung
Bremerhaven, Germany
13 h-index
25 publications
1.3K citations
Columbia University
New York, United States
11 h-index
20 publications
3.9K citations

Chinese Academy of Sciences
Beijing, China
11 h-index
20 publications
1.3K citations

University of Minnesota
Minneapolis, United States
11 h-index
25 publications
5.8K citations
University of Bremen
Bremen, Germany
10 h-index
28 publications
1.5K citations
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21 publications · 3.3K citations
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22 publications · 1.5K citations
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15 publications · 3.6K citations
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10 publications · 1K citations
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9 publications · 847 citations
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