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Links between eccentricity forcing and the 100,000-year glacial cycle

article by Lorraine Lisiecki published 4 April 2010 in Nature Geoscience

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Links between eccentricity forcing and the 100,000-year glacial cycle (English)

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Lorraine E. Lisiecki

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English

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publication date

4 April 2010

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published in

Nature Geoscience

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volume

3

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issue

5

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page(s)

349-352

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Variations in the Earth's Orbit: Pacemaker of the Ice Ages

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On the structure and origin of major glaciation cycles 2. The 100,000-year cycle

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Eccentricity forcing of Pliocene–Early Pleistocene climate revealed in a marine oxygen-isotope record

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The timing of major climate terminations

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Obliquity pacing of the late Pleistocene glacial terminations

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Sea ice as the glacial cycles’ Climate switch: role of seasonal and orbital forcing

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Is the spectral signature of the 100 kyr glacial cycle consistent with a Milankovitch origin?

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Late Pliocene-early Pleistocene 100-ka problem

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The 100,000-year ice-Age cycle identified and found to lag temperature, carbon dioxide, and orbital eccentricity

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The middle Pleistocene transition: characteristics, mechanisms, and implications for long-term changes in atmospheric pCO2

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Northern Hemisphere forcing of climatic cycles in Antarctica over the past 360,000 years

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The timing of Pleistocene glaciations from a simple multiple-state climate model

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Modeling the climatic response to orbital variations

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Plio-Pleistocene ice volume, Antarctic climate, and the global delta18O record

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The mid-Pleistocene transition in the tropical Pacific

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Revised calibration of the geomagnetic polarity timescale for the Late Cretaceous and Cenozoic

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WAVELETS AND TIME-DEPENDENT SPECTRAL ANALYSIS

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10.1038/NGEO828

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(Q57379909)

Links between eccentricity forcing and the 100,000-year glacial cycle

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