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Cambio climático durante la última deglaciación en la Antártida

Mayewski1, Twickler, Whitlow

  • 1P. A. Mayewski, M. S. Twickler, S. I. Whitlow, Q. Yang, J. Thomas, K. Kreutz, Climate Change Research Center, Institute for the Study of Earth, Oceans, and Space, and Department of Earth Sciences, University of New Hampshire, Durham, NH 03824, USA. L. D. Meeker, Climate Change Research Center, Institute for the Study of Earth, Oceans, and Space, and Department of Mathematics, University of New Hampshire, Durham, NH 03824, USA. P. M. Grootes and E. J. Steig, Quaternary Research Center AK-60, University of Washington, Seattle, WA 98195, USA. D. L. Morse and E. D. Waddington, Geophysics Program, University of Washington, Seattle, WA 98195, USA. E. S. Saltzman, Rosenstiel School of Marine and Atmospheric Sciences, University of Miami, Miami, FL 33149, USA. P.-Y. Whung, National Oceanic and Atmospheric Administration, Atlantic Oceanographic and Meteorological Laboratory, Ocean Chemistry Division, and Rosenstiel School of Marine and Atmospheric Sciences, University of Miami, Miami, FL 33149, USA. K. C. Taylor, Water Resources Center, Desert Research Institute, University and Community College System of Nevada, Reno, NV 89506, USA.

Science (New York, N.Y.)
|June 14, 1996
PubMed
Resumen

Los núcleos de hielo de Groenlandia revelan rápidos cambios climáticos. El análisis de núcleos de hielo de Groenlandia y la Antártida muestra una variabilidad similar de eventos climáticos, lo que sugiere que estos eventos son más comunes en la Antártida de lo que se pensaba anteriormente.

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