Articles | Volume 11, issue 12
Research article
04 Dec 2015
Research article |  | 04 Dec 2015

Glacier response to North Atlantic climate variability during the Holocene

N. L. Balascio, W. J. D'Andrea, and R. S. Bradley

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Cited articles

Balascio, N. L., D'Andrea, W. J., Bradley, R. S., and Perren, B. B.: Biogeochemial evidence for hydrologic changes during the Holocene in a lake sediment record from southeast Greenland, The Holocene, 23, 1428–1439, 2013.
Bennike, O. and Sparrenbom, C. J.: Dating of the Narssarssuaq stade in southern Greenland, The Holocene, 17, 279–282, 2007.
Berger, A. and Loutre, M. F.: Insolation values for the climate of the last 10 million years, Quat. Sci. Rev., 10, 297–317, 1991.
Bond, G., Showers, W., Cheseby, M., Lotti, R., Almasi, P., deMenocal, P., Priore, P., Cullen, H., Hajdas, I., and Bonani, G.: A pervasive millennial-scale cycle in North Atlantic Holocene and Glacial climates, Science, 278, 1257–1266, 1997.
Bond, G., Kromer, B., Beer, J., Muscheler, R., Evans, M. N., Showers, W., Hoffmann, S., Lotti-Bond, R., Hajdas, I., and Bonani, G.: Persistent solar influence on North Atlantic climate during the Holocene, Science, 294, 2130–2136, 2001.
Short summary
Sediment cores were collected from a lake that captures runoff from two glaciers in Greenland. Our analysis of the sediments shows that these glaciers were active over the last 9,000 years and advanced and retreated in response to regional climate changes. The data also provide a long-term perspective on the rate of 20th century glacier retreat and indicate that recent anthropogenic-driven warming has already impacted the regional cryosphere in a manner outside the range of natural variability.