Holocene warming in western continental Eurasia driven by glacial retreat and greenhouse forcing

Baker, J.L.; Lachniet, M.S.; Chervyatsova, O.; Asmerom, Y.; Polyak, V.J.

doi:/10.1038/ngeo2953

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Holocene warming in western continental Eurasia driven by glacial retreat and greenhouse forcing

Baker, J.L.; Lachniet, M.S.; Chervyatsova, O.; Asmerom, Y.; Polyak, V.J. (2017). Holocene warming in western continental Eurasia driven by glacial retreat and greenhouse forcing. Nature Geoscience 10(6): 430-435. https://dx.doi.org/10.1038/ngeo2953

In: Nature Geoscience. Nature Publishing Group: London. ISSN 1752-0894; e-ISSN 1752-0908

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Baker, J.L. Lachniet, M.S. Chervyatsova, O.	Asmerom, Y. Polyak, V.J.

Abstract

Models and proxy data diverge on the global temperature evolution of the Holocene, perhaps due to representation of the seasons. Isotopic analyses of stalagmites from the Ural Mountains suggest that winter climate dominated in the Eurasian interior.

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