Interglacials of the last 800,000 years
Authors
Berger, B
Crucifix, M
Hodell, DA
Mangili, C
McManus, JF
Otto-Bliesner, B
Pol, K
Raynaud, D
Skinner, LC
Tzedakis, PC
Wolff, EW
Yin, QZ
Abe-Ouchi, A
Barbante, C
Brovkin, V
Cacho, I
Capron, E
Ferretti, P
Ganopolski, A
Grimalt, JO
Hönisch, B
Kawamura, KA
Landais, A
Margari, V
Martrat, B
Masson-Delmotte, V
Mokeddem, Z
Parrenin, F
Prokopenko, AA
Rashid, H
Schulz, M
Vazquez Riveiros, N
Publication Date
2016Journal Title
Reviews of Geophysics
ISSN
8755-1209
Publisher
American Geophysical Union (AGU)
Volume
54
Pages
162-219
Language
English
Type
Article
Metadata
Show full item recordCitation
Berger, B., Crucifix, M., Hodell, D., Mangili, C., McManus, J., Otto-Bliesner, B., Pol, K., et al. (2016). Interglacials of the last 800,000 years. Reviews of Geophysics, 54 162-219. https://doi.org/10.1002/2015RG000482
Abstract
Interglacials, including the present (Holocene) period, are warm, low land ice extent (high sea level), end-members of glacial cycles. Based on a sea level definition, we identify eleven interglacials in the last 800,000 years, a result that is robust to alternative definitions. Data compilations suggest that despite spatial heterogeneity, Marine Isotope Stages (MIS) 5e (last interglacial) and 11c (~400 ka ago) were globally strong (warm), while MIS 13a (~500 ka ago) was cool at many locations. A step change in strength of interglacials at 450 ka is apparent only in atmospheric CO$_{2}$ and in Antarctic and deep ocean temperature. The onset of an interglacial (glacial termination) seems to require a reducing precession parameter (increasing Northern Hemisphere summer insolation), but this condition alone is insufficient. Terminations involve rapid, nonlinear, reactions of ice volume, CO$_{2}$, and temperature to external astronomical forcing. The precise timing of events may be modulated by millennial-scale climate change that can lead to a contrasting timing of maximum interglacial intensity in each hemisphere. A variety of temporal trends is observed, such that maxima in the main records are observed either early or late in different interglacials. The end of an interglacial (glacial inception) is a slower process involving a global sequence of changes. Interglacials have been typically 10–30 ka long. The combination of minimal reduction in northern summer insolation over the next few orbital cycles, owing to low eccentricity, and high atmospheric greenhouse gas concentrations implies that the next glacial inception is many tens of millennia in the future.
Keywords
interglacials, Milankovitch cycles, paleoclimatology and paleoceanography, Earth system models, geochronology
Sponsorship
This paper arose as a result of a succession of workshops of the Past Interglacials Group (PIGS), sponsored by the Past Global Changes Project (PAGES). The authors acknowledge the contributions of all participants at those workshops, of whom the listed authors are only a subset. Numerous funding agencies have contributed to the work of this paper including NSF (USA), NERC and The Royal Society (UK), F.R.S –FNRS (Belgium), and SNF (Switzerland). Most data described in this paper are available through relevant data repositories, http://www.ncdc.noaa.gov/data-access/paleoclimatology-data and www.pangaea.de in particular. In addition, the datasets from which Tables 2 and 3 were derived have been compiled into a spreadsheet as a supplement to this paper. Insolation data for Figure 5 can be calculated using programs available at ftp://ftp.elic.ucl.ac.be/berger/berger78/ and ftp://ftp.elic.ucl.ac.be/berger/ellipticintegrals/.
Funder references
Royal Society (RP120096)
Natural Environment Research Council (NE/G007535/1)
Embargo Lift Date
2100-01-01
Identifiers
External DOI: https://doi.org/10.1002/2015RG000482
This record's URL: https://www.repository.cam.ac.uk/handle/1810/252679
Rights
Attribution 4.0 International, Attribution 4.0 International, Attribution 4.0 International, Attribution 4.0 International, Attribution 4.0 International
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