The 'flickering switch' of late Pleistocene climate change

K. C. Taylor, G. W. Lamorey, G. A. Doyle, Richard B. Alley, P. M. Grootes, P. A. Mayewski, J. W.C. White, L. K. Barlow

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Abstract

POLAR ice contains a unique record of past climate variations; previous Greenland ice cores have documented relatively warm 'interstadial' periods during the last glaciation and short (centuryscale) returns to colder conditions during the glacial to interglacial warming (see, for example, ref. 1). These climate features have also been observed to varying degrees in ocean sediment cores2-4 and terrestrial pollen and insect records5-7. Here we report electrical conductivity measurements from a new Greenland ice core, which confirm these previous observations, and also reveal a hitherto unrecognized mode of rapid climate variation. Fluctuations in ice conductivity on the scales of <5-20 years reflect rapid oscillations in the dust content of the atmosphere. This 'flickering' between two preferred states would seem to require extremely rapid reorganizations in atmospheric circulation.

Original languageEnglish (US)
Pages (from-to)432-436
Number of pages5
JournalNature
Volume361
Issue number6411
DOIs
StatePublished - Jan 1 1993

All Science Journal Classification (ASJC) codes

  • General

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    Taylor, K. C., Lamorey, G. W., Doyle, G. A., Alley, R. B., Grootes, P. M., Mayewski, P. A., White, J. W. C., & Barlow, L. K. (1993). The 'flickering switch' of late Pleistocene climate change. Nature, 361(6411), 432-436. https://doi.org/10.1038/361432a0