Millennial-length forward models and pseudoproxies of stalagmite δ<sup>18</sup>O: an example from NW Scotland
The stable oxygen isotope parameter δ<sup>18</sup>O remains the most widely utilised speleothem proxy for past climate reconstructions. Uncertainty can be introduced into stalagmite δ<sup>18</sup>O from a number of factors, one of which is the heterogeneit...
Main Authors: | , , , , , , , |
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Format: | Article |
Language: | English |
Published: |
Copernicus Publications
2012-07-01
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Series: | Climate of the Past |
Online Access: | http://www.clim-past.net/8/1153/2012/cp-8-1153-2012.pdf |