Sea level and global ice volumes from the Last Glacial Maximum to the Holocene

Proceedings of the National Academy of Sciences of the United States of America - Tập 111 Số 43 - Trang 15296-15303 - 2014
Kurt Lambeck1,2, Hélène Rouby1,2, Anthony Purcell2, Yiying Sun3, Malcolm Sambridge2
1Laboratoire de Géologie de l'École Normale Supérieure, UMR 8538 du CNRS, 75231 Paris, France; and
2Research School of Earth Sciences, The Australian National University, Canberra, ACT 0200, Australia
3Department of Earth Sciences, University of Hong Kong, Hong Kong, China

Tóm tắt

SignificanceSeveral areas of earth science require knowledge of the fluctuations in sea level and ice volume through glacial cycles. These include understanding past ice sheets and providing boundary conditions for paleoclimate models, calibrating marine-sediment isotopic records, and providing the background signal for evaluating anthropogenic contributions to sea level. From ∼1,000 observations of sea level, allowing for isostatic and tectonic contributions, we have quantified the rise and fall in global ocean and ice volumes for the past 35,000 years. Of particular note is that during the ∼6,000 y up to the start of the recent rise ∼100−150 y ago, there is no evidence for global oscillations in sea level on time scales exceeding ∼200 y duration or 15−20 cm amplitude.

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Proceedings of the National Academy of Sciences of the United States of America

Tập 111 Số 43

15296-15303

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